Mass Spectrometry of Acoustically Levitated Droplets

PubMed Central

Westphall, Michael S.; Jorabchi, Kaveh; Smith, Lloyd M.

2008-01-01

Containerless sample handling techniques such as acoustic levitation offer potential advantages for mass spectrometry, by eliminating surfaces where undesired adsorption/desorption processes can occur. In addition, they provide a unique opportunity to study fundamental aspects of the ionization process as well as phenomena occurring at the air–droplet interface. Realizing these advantages is contingent, however, upon being able to effectively interface levitated droplets with a mass spectrometer, a challenging task that is addressed in this report. We have employed a newly developed charge and matrix-assisted laser desorption/ionization (CALDI) technique to obtain mass spectra from a 5-μL acoustically levitated droplet containing peptides and an ionic matrix. A four-ring electrostatic lens is used in conjunction with a corona needle to produce bursts of corona ions and to direct those ions toward the droplet, resulting in droplet charging. Analyte ions are produced from the droplet by a 337-nm laser pulse and detected by an atmospheric sampling mass spectrometer. The ion generation and extraction cycle is repeated at 20 Hz, the maximum operating frequency of the laser employed. It is shown in delayed ion extraction experiments that both positive and negative ions are produced, behavior similar to that observed for atmospheric pressure matrix-assisted laser absorption/ionization. No ion signal is observed in the absence of droplet charging. It is likely, although not yet proven, that the role of the droplet charging is to increase the strength of the electric field at the surface of the droplet, reducing chargere combination after ion desorption. PMID:18582090

Effekt einer ad libitum verzehrten fettreduzierten Kost, reich an Obst, Gemüse und Milchprodukten auf den Blutdruck bei Borderline-Hypertonikern

NASA Astrophysics Data System (ADS)

Möseneder, Jutta M.

2002-01-01

In der randomisierten, multizentrischen DASH-Studie (Dietary Approaches to Stop Hy-pertension), die unter kontrollierten Bedingungen stattfand, führte eine fettreduzierte Mischkost, reich an Obst, Gemüse und Milchprodukten, bei Borderline-Hypertonikern zu einer signifikanten Blutdrucksenkung. Während der Studienphase wurden Körpermasse, Natrium-Aufnahme sowie Alkoholzufuhr aufgrund der bekannten Einflussnahme auf den Blutdruck konstant gehalten. In der eigenen Pilot-Studie sollte untersucht werden, ob das Ergebnis der DASH-Studie (i) mit deutschen Hypertonikern und (ii) unter habituellen Ernährungs- und Lebensbedingungen mit regelmäßig durchgeführter Ernährungsberatung und ad libitum Verzehr anstelle des streng kontrollierten Studienansatzes bestätigt werden kann. Eine Konstanz der Körpermasse, der Natrium-Urinausscheidung (unter diesem Studienansatz valider als die Aufnahme) und des Alkoholkonsums wurde vorausgesetzt. Die Studienpopulation setzte sich aus 53 übergewichtigen Probanden mit einer nicht medikamentös therapierten Borderline-Hypertonie und ohne Stoffwechselerkrankungen zusammen. Die Studienteilnehmer wurden randomisiert entweder der Idealgruppe mit einer fettarmen Kost reich an Milchprodukten, Obst und Gemüse (ähnlich der DASH-Idealgruppe) oder der Kontrollgruppe mit habitueller Ernährungsweise zugeteilt. Über einen Zeitraum von fünf Wochen wurde den Probanden etwa 50% ihres täglichen Lebensmittelbedarfes entsprechend ihrer Gruppenzugehörigkeit kostenfrei zur Verfügung gestellt. Gelegenheitsblutdruckmessungen und 24h-Blutdruckmessungen, Ernährungs- und Aktivitätsprotokolle, Blut- und Urinproben sowie anthropometrische Messungen wurden vor, während und fünf Wochen nach der Interventionsphase durchgeführt. Die Ergebnisse zeigen, dass in der Idealgruppe keine signifikante Blutdrucksenkung beobachtet werden konnte. Dies lässt sich durch die Tatsache erklären, dass die Lebens-mittel- und Nährstoffaufnahme der deutschen Kontrollgruppe eher der amerikanischen Idealgruppe entsprach. In der Pilot-Studie waren die Unterschiede in der Nährstoffzufuhr zwischen den beiden Gruppen viel geringer als in der DASH-Studie; für eine blutdrucksenkende Ernährungsumstellung bestand somit nur ein geringer Spielraum. Eine weitere Erklärung besteht in der unterschiedlichen Zusammensetzung der Studienpopulation. Bei DASH wurden vorwiegend farbige Probanden (40% höhere Hypertonieprävalenz) untersucht. Die Studienergebnisse lassen also den Schluss zu, dass Ernährungs- und Lebensstilgewohnheiten sowie der genetische Hintergrund der entsprechenden Bevölkerungsgruppe bei der Formulierung von nährstoff- oder lebensmittelbezogenen Empfehlungen zur Senkung des Bluthochdruckes Berücksichtigung finden müssen. The Dietary Approaches to Stop Hypertension trial (DASH), a randomized well-controlled feeding study conducted at 4 medical centers, demonstrated that a low-fat diet, rich in fruits, vegetables and dairy products is able to lower blood pressure of borderline-hypertensive people significantly. Body weight, sodium intake and alcohol consumption were kept constant during the whole study period, due to the known influence on hypertension. Aim of our study project was to investigate whether the results of the DASH study can be confirmed by (i) using a German hypertensive population and (ii) replacing the well-controlled feeding design by allowing ad libitum intake according to dietary ad-vice. The participants were asked to keep their body weight, sodium urine excretion (un-der this study design more valid than sodium intake) and their alcohol consumption con-stant. Our pilot study population consisted of 53 mainly overweight participants with borderline hypertension and without medication or any metabolic disorders. They were randomly assigned to either an ideal diet low in fat and rich in dairy products, fruits and vegetables (similar to the DASH I-group) or a habitual diet as control (C-group). During five weeks the subjects were provided 50 % of their daily intake for free according to their dietary pattern. Single and 24h-blood pressure measurements, dietary weighed and physical activity records, blood and urine samples and anthropometric measurements were collected before, during and five weeks after the intervention period. The study results indicated that no significantly reduction of blood pressure could be observed for both methods in the I-group of our trial. This is due to the fact that the baseline intake of foods and nutrients of the German subjects was nearly corresponding to the intake targeted for the DASH I-group. Therefore, it was impossible to increase the intake of these nutrients in our I-group by the same percentage as in the DASH study. Another explanation may be the different consistency of the study population. About 60% of the DASH study population were African Americans with a known higher prevalence of hy-pertension (about 40%) than Caucasians. The conclusion is that even convincing results of a controlled trial cannot be simply transferred into dietary advice for the general public. For addressing food-based dietary guidelines to reduce the risk of hypertension it is necessary to consider the genetic background as well as the dietary and the lifestyle situation of the target population carefully.

S1-Leitlinie Lipödem.

PubMed

Reich-Schupke, Stefanie; Schmeller, Wilfried; Brauer, Wolfgang Justus; Cornely, Manuel E; Faerber, Gabriele; Ludwig, Malte; Lulay, Gerd; Miller, Anya; Rapprich, Stefan; Richter, Dirk Frank; Schacht, Vivien; Schrader, Klaus; Stücker, Markus; Ure, Christian

2017-07-01

Die vorliegende überarbeitete Leitlinie zum Lipödem wurde unter der Federführung der Deutschen Gesellschaft für Phlebologie (DGP) erstellt und finanziert. Die Inhalte beruhen auf einer systematischen Literaturrecherche und dem Konsens von acht medizinischen Fachgesellschaften und Berufsverbänden. Die Leitlinie beinhaltet Empfehlungen zu Diagnostik und Therapie des Lipödems. Die Diagnose ist dabei auf der Basis von Anamnese und klinischem Befund zu stellen. Charakteristisch ist eine umschriebene, symmetrisch lokalisierte Vermehrung des Unterhautfettgewebes an den Extremitäten mit deutlicher Disproportion zum Stamm. Zusätzlich finden sich Ödeme, Hämatomneigung und eine gesteigerte Schmerzhaftigkeit der betroffenen Körperabschnitte. Weitere apparative Untersuchungen sind bisher besonderen Fragestellungen vorbehalten. Die Erkrankung ist chronisch progredient mit individuell unterschiedlichem und nicht vorhersehbarem Verlauf. Die Therapie besteht aus vier Säulen, die individuell kombiniert und an das aktuelle Beschwerdebild angepasst werden sollten: komplexe physikalische Entstauungstherapie (manuelle Lymphdrainage, Kompressionstherapie, Bewegungstherapie, Hautpflege), Liposuktion und plastisch-chirurgische Interventionen, Ernährung und körperliche Aktivität sowie ggf. additive Psychotherapie. Operative Maßnahmen sind insbesondere dann angezeigt, wenn trotz konsequent durchgeführter konservativer Therapie noch Beschwerden bestehen bzw. eine Progredienz des Befundes und/oder der Beschwerden auftritt. Eine begleitend zum Lipödem bestehende morbide Adipositas sollte vor einer Liposuktion therapeutisch angegangen werden. © 2017 The Authors | Journal compilation © Blackwell Verlag GmbH, Berlin.

Wirksamkeit und Sicherheit von Fumarsäureestern in Kombination mit Phototherapie bei Patienten mit moderater bis schwerer Plaque-Psoriasis (FAST).

PubMed

Weisenseel, Peter; Reich, Kristian; Griemberg, Wiebke; Merten, Katharina; Gröschel, Christine; Gomez, Natalie Nunez; Taipale, Kirsi; Bräu, Beate; Zschocke, Ina

2017-02-01

Die Behandlung von Psoriasis-Patienten mit einer Kombination aus Fumarsäureestern (FSE, Fumaderm ® ) und Phototherapie (UV) ist verbreitet, wurde aber im Rahmen von Studien wenig untersucht. Bisher liegen lediglich Daten aus einer kleinen Pilotstudie vor. Intention dieser Studie war, eine FSE/UV-Kombinationsbehandlung an einem größeren Patientenkollektiv mit mittelschwerer bis schwerer Psoriasis zu untersuchen. In dieser prospektiven, multizentrischen, nichtinterventionellen Studie wurden Daten von Patienten mit FSE/UV-Kombinationstherapie hinsichtlich der Wirksamkeit (PGA' PASI, DLQI, EQ-5D), Sicherheit und Dosierung über einen Zeitraum von zwölf Monaten erfasst und mit Daten einer retrospektiven Studie mit FSE-Monotherapie verglichen. Es wurden Daten von 363 Patienten ausgewertet. Unter der Kombinationstherapie verbesserten sich alle Wirksamkeitsparameter deutlich. Im Vergleich zur Monotherapie mit FSE konnte durch die Kombination mit UV ein schnellerer Wirkeintritt erzielt werden, wobei nach zwölf Monaten kein Unterschied in der Wirksamkeit bestand. Die Dauer und Art der Phototherapie zeigte keinen Einfluss auf die Wirksamkeitsparameter. Allgemein wurde die Kombinationstherapie gut vertragen. Unerwünschte Ereignisse wurden bei 7 % der Patienten berichtet. Die FSE/UV Kombinationstherapie zeigt eine gute Wirksamkeit und Verträglichkeit und kann zu einem schnelleren Wirkeintritt führen. Eine Kombinationstherapie erscheint vor allem in den ersten drei Monaten der FSE Behandlung sinnvoll. © 2017 Deutsche Dermatologische Gesellschaft (DDG). Published by John Wiley & Sons Ltd.

Implantate im Mittelohrbereich - Teil 2 (Ergänzungen 2007)

NASA Astrophysics Data System (ADS)

Stieve, M.; Lenarz, Thomas

In Deutschland leben ca. 12 Millionen Menschen, die an einer ein- oder beidseitigen Schwerhörigkeit leiden. Diese kann angeboren oder im Laufe des Lebens erworben sein. Klinisch und therapeutisch wichtig ist die Unterscheidung hinsichtlich des Schädigungsortes im Bereich des Mittelohres, d. h. eine Schalleitungsschwerhörigkeit, oder im Bereich des Innenohres, d. h. eine Schallempfindungsschwerhörigkeit, wobei hier der Schädigungsort auch am Hörnerven oder in den zentralen Hörabschnitten liegen kann. Therapeutisch lassen sich sowohl Schwerhörigkeiten im Bereich des Mittelohres als auch im Innenohr und sogar im Hirnstammbereich (Hirnstammimplantat) behandeln. 1,9 Millionen Schwerhörige haben eine Erkrankung im Mittelohrbereich, d. h. der Schall kann nur ungenügend auf das Innenohr übertragen werden. Die Ursache besteht meist in einer chronischen Mittelohrentzündung, die zu einer Zerstörung des Trommelfells und der Gehörknöchelchenkette geführt haben. Therapeutisch und damit als Prinzip der operativen Hörverbesserung steht primär der Verschluß des Trommelfells oder eine Rekonstruktion der Gehörknöchelchen. Mittelohroperationen werden mikrochirurgisch unter dem Operationsmikroskop durchgeführt, wobei zunächst durch eine sanierende Operation der Entzündungsprozeß entfernt wird und nach einer Ausheilungszeit die Gehörknöchelchenkette durch künstliche Prothesen rekonstruiert werden kann.

Prä- und perioperative Aspekte der Versorgung dermatochirurgischer Patienten.

PubMed

Müller, Cornelia S L; Hubner, Wakiko; Thieme-Ruffing, Sigrid; Pföhler, Claudia; Vogt, Thomas; Volk, Thomas; Gärtner, Barbara C; Bialas, Patric

2017-02-01

Die Dermatochirurgie nimmt hinsichtlich vieler Punkte eine Sonderstellung unter den operativen Fächern ein. Hierzu gehört in erster Linie die Tatsache, dass bis auf wenige Ausnahmen fast alle Eingriffe traditionell in Lokal- bzw. Regionalanästhesie und oft auch in räumlich-infrastruktureller Trennung von den großen Zentral-Operationssälen stattfinden können. Die peri- und postoperative Überwachung obliegt dabei dem dermatochirurgischen Operationsteam. Das sui generis kleinere OP-Team hat somit eine ganze Reihe perioperativer Notwendigkeiten zu beachten, um die sich in den "großen" chirurgischen Fächern eine Vielzahl verschiedener beteiligter Fachgruppen gemeinsam kümmern. Hierzu gehören neben Hygieneaspekten, Kenntnissen in der Überwachung der Patienten sowie dem Aspekt der surgical site infections auch Fragen zur postoperativen Schmerztherapie sowie detailliertes pharmakologisches Wissen über die zur Anwendung kommenden Lokalanästhetika und das Handling der damit assoziierten toxischen und allergischen Reaktionen. Eine interdisziplinäre Zusammenarbeit und Verantwortung für den Patienten ist notwendig und erfordert die Erarbeitung und Umsetzung qualitätsorientierter und evidenzbasierter Handlungsanweisungen, die im dermatochirurgischen OP-Setting meist weit über das eigentliche Fach hinausgehen. Ziel dieses Weiterbildungsartikels soll die komprimierte Darstellung der genannten fachübergreifenden Standpunkte bezüglich der wichtigsten perioperativen Aspekte sein. © 2017 Deutsche Dermatologische Gesellschaft (DDG). Published by John Wiley & Sons Ltd.

Ship Noise in the SW Indian Ocean Recorded by Ocean Bottom Seismic and Hydroacoustic Sensors

NASA Astrophysics Data System (ADS)

Barruol, G.; Dreo, R.; Fontaine, F. R.; Scholz, J. R.; Sigloch, K.

2016-12-01

In the frame of the RHUM-RUM project (Réunion Hotspot and Upper Mantle - Réunions Unterer Mantel, www.rhum-rum.net), a network of 57 ocean-bottom seismometers (OBS) has been installed on the ocean floor around La Réunion Island, but also on the neighbouring Southwest and Central Indian Ridges. The OBS were equipped by wide- and broad-band three-components seismic and hydroacoustic sensors. They were deployed in Nov. 2012, and depending on the configuration, they recorded for 8 to 13 months. Interestingly, part of the network was located beneath a NE-SW trending lane of very dense ship traffic connecting SE-Asia and the South-Atlantic region. By combining the vessel position - provided by AIS GPS data - and our geophysical data recorded on the ocean floor, we analyze the seismic and hydroacoustic ship signatures. From spectral analyzes, we show clear signals over the whole high-frequency range available from our instruments (between 1 and 50 Hz). The RHUM-RUM network covering latitude between 17 and 34° South, this allows to detect numerous vessels and to compare the noise characteristics (frequency content, polarization) of each vessel. We also investigate the possibility of using the polarization of the noise emitted by ships passing above an ocean-bottom seismometer, to help retrieving the orientation of the OBS horizontal components on the ocean floor in the geographic reference frame.

Protein crystal growth

NASA Technical Reports Server (NTRS)

Bugg, Charles E.

1993-01-01

Proteins account for 50% or more of the dry weight of most living systems and play a crucial role in virtually all biological processes. Since the specific functions of essentially all biological molecules are determined by their three-dimensional structures, it is obvious that a detailed understanding of the structural makeup of a protein is essential to any systematic research pertaining to it. At the present time, protein crystallography has no substitute, it is the only technique available for elucidating the atomic arrangements within complicated biological molecules. Most macromolecules are extremely difficult to crystallize, and many otherwise exciting and promising projects have terminated at the crystal growth stage. There is a pressing need to better understand protein crystal growth, and to develop new techniques that can be used to enhance the size and quality of protein crystals. There are several aspects of microgravity that might be exploited to enhance protein crystal growth. The major factor that might be expected to alter crystal growth processes in space is the elimination of density-driven convective flow. Another factor that can be readily controlled in the absence of gravity is the sedimentation of growing crystal in a gravitational field. Another potential advantage of microgravity for protein crystal growth is the option of doing containerless crystal growth. One can readily understand why the microgravity environment established by Earth-orbiting vehicles is perceived to offer unique opportunities for the protein crystallographer. The near term objectives of the Protein Crystal Growth in a Microgravity Environment (PCG/ME) project is to continue to improve the techniques, procedures, and hardware systems used to grow protein crystals in Earth orbit.

Airborne laser-spark for ambient desorption/ionisation.

PubMed

Bierstedt, Andreas; Riedel, Jens

A novel direct sampling ionisation scheme for ambient mass spectrometry is presented. Desorption and ionisation are achieved by a quasi-continuous laser induced plasma in air. Since there are no solid or liquid electrodes involved the ion source does not suffer from chemical interferences or fatigue originating from erosive burning or from electrode consumption. The overall plasma maintains electro-neutrality, minimising charge effects and accompanying long term drift of the charged particles trajectories. In the airborne plasma approach the ambient air not only serves as the plasma medium but at the same time also slows down the nascent ions via collisional cooling. Ionisation of the analyte molecules does not occur in the plasma itself but is induced by interaction with nascent ionic fragments, electrons and/or far ultraviolet photons in the plasma vicinity. At each individual air-spark an audible shockwave is formed, providing new reactive species, which expands concentrically and, thus, prevents direct contact of the analyte with the hot region inside the plasma itself. As a consequence the interaction volume between plasma and analyte does not exceed the threshold temperature for thermal dissociation or fragmentation. Experimentally this indirect ionisation scheme is demonstrated to be widely unspecific to the chemical nature of the analyte and to hardly result in any fragmentation of the studied molecules. A vast ensemble of different test analytes including polar and non-polar hydrocarbons, sugars, low mass active ingredients of pharmaceuticals as well as natural biomolecules in food samples directly out of their complex matrices could be shown to yield easily accessible yet meaningful spectra. Since the plasma medium is humid air, the chemical reaction mechanism of the ionisation is likely to be similar to other ambient ionisation techniques. Wir stellen hier eine neue Ionisationsmethode für die Umgebungsionisation (ambient ionisation) vor. Sowohl die Desorption als auch die Ionisation erfolgen hierbei durch ein laserbetriebenes Luftplasma. Die Abwesenheit fester oder flüssiger Elektroden hat zur Folge, dass die Methode weder unter chemischen Interferenzen noch unter Verschleiß durch Korrosionsbrand oder abgetragenes Elektrodenmaterial leidet. Insgesamt betrachtet herrscht in dem Plasma Elektroneutralität, wodurch Aufladungseffekte minimiert werden, die andernfalls zu einer langfristigenÄderung der Flugbahnen von Ionen während der Experimente führen kann. In dem Ansatz eine freischwebende Luftentladung bei Atmosphärendruck zu verwenden agiert die Luft nicht nur als Plasmamedium sondert dient zusätzlich als Badgas für die stoßinduzierte Kühlung der entstehenden Ionen. Die Ionisierung der Analytmoleküle erfolgt nicht unmittelbar im Plasma sondern in dessen direkter Umgebung durch Wechselwirkung mit freigesetzten ionischen Luftspezies, freien Elektronen oder Photonen im kurzwelligen ultravioletten Bereich. Jede Laserentladung erzeugt eine hörbare Stoßwelle, in welcher neu produzierte reaktive Spezies freigesetzt werden, welche sich konzentrisch ausbreiten, so dass eine Diffusion der Analytmoleküle ins heiße Innere des Plasmas verhindert wird. Daraus folgt, dass im Interaktionsvolumen zwischen Plasma und Analyt der Temperaturgrenzwert für eine thermische Dissoziation oder Fragmentierung der Moleküle nicht überschritten wird. Experimentell konnte belegt werden, dass das vorgestellte Ionisierungsschema sehr unselektiv bezüglich der chemischen Analytklasse ist und kaum Fragmentierungsprodukte beobachtet werden können. Messungen einer breitgefächerten Auswahl unterschiedlicher Testsubstanzen, wie beispielsweise polarer und unpolarer Kohlenwasserstoffe, Zuckern, niedermolekularer pharmazeutischer Wirkstoffe, sowie natürlicher Biomoleküle in Lebensmittelproben unmittelbar aus ihren komplexen Matrizes, führten zu aussagekräftigen Massenspektren. Zumal das Lasermedium feuchte Luft ist, scheint der Reaktionsmechanismus dem anderer Atmosphärendruckionisierungsmethoden zuähneln.

Electrostatic levitation facility optimized for neutron diffraction studies of high temperature liquids at a spallation neutron source

DOE PAGES

Mauro, N. A.; Vogt, A. J.; Derendorf, K. S.; ...

2016-01-01

Neutron diffraction studies of metallic liquids provide valuable information about inherent topological and chemical ordering on multiple length scales as well as insight into dynamical processes at the level of a few atoms. But, there exist very few facilities in the world that allow such studies to be made of reactive metallic liquids in a containerless environment, and these are designed for use at reactor-based neutron sources. We present an electrostatic levitation facility, NESL (for Neutron ElectroStatic Levitator), which takes advantage of the enhanced capabilities and increased neutron flux available at spallation neutron sources (SNSs). NESL enables high quality elasticmore » and inelastic neutron scattering experiments to be made of reactive metallic and other liquids in the equilibrium and supercooled temperature regime. The apparatus is comprised of a high vacuum chamber, external and internal neutron collimation optics, and a sample exchange mechanism that allows up to 30 samples to be processed between chamber openings. Two heating lasers allow excellent sample temperature homogeneity, even for samples approaching 500 mg, and an automated temperature control system allows isothermal measurements to be conducted for times approaching 2 h in the liquid state, with variations in the average sample temperature of less than 0.5%. Furthermore, to demonstrate the capabilities of the facility for elastic scattering studies of liquids, a high quality total structure factor for Zr 64Ni 36 measured slightly above the liquidus temperature is presented from experiments conducted on the nanoscale-ordered materials diffractometer (NOMAD) beam line at the SNS after only 30 min of acquisition time for a small sample ( 100 mg).« less

Crystallization kinetics in Si-1 at%Sn during rapid solidification in undercooled melt

NASA Astrophysics Data System (ADS)

Kuribayashi, K.; Ozawa, S.; Nagayama, K.; Inatomi, Y.

2017-06-01

In order to elucidate the cause of the morphological transition of crystals growing in an undercooled melt of semiconducting materials, we carried out the containerless solidification of undoped Si and Si-1 at%Sn using a CO2 laser-equipped electromagnetic levitator (EML). The crystallization of these materials was successfully achieved under controlled undercooling. The relation between the shape of growing crystals and the degree of undercooling in Si-1 at%Sn was similar to that in undoped Si; that is, plate-like needle crystals were observed at low undercooling, whereas at medium and high undercooling the shape of growing crystals changed to massive dendrites. The grain-size of as-solidified samples of Si-1 at%Sn was remarkably small compared with that of undoped Si. The surface morphologies of samples solidified by dropping the melt onto a chill plate of mirror-polished silicon consisted of typical twin-related <110> dendrites. On the other hand, samples that were dropped from the undercooled state consisted of twin-free <100> dendrites. The nucleation rate of two-dimensional nuclei calculated on the basis of two mechanisms, which are the twin-plane re-entrant edge mechanism and the twin-free mechanism, suggested that the morphological transition to twin-free <100> dendrites from twin-related <110> dendrites occurs when the degree of undercooling becomes larger than the critical value. These results indicate that the cause of the morphological transition of Si growing in the undercooled melt is not the roughening transition of the crystal-melt interface but the transition of the nucleation kinetics to the twin-free mechanism from the twin-related mechanism.

Advanced user support programme—TEMPUS IML-2

NASA Astrophysics Data System (ADS)

Diefenbach, A.; Kratz, M.; Uffelmann, D.; Willnecker, R.

1995-05-01

The DLR Microgravity User Support Centre (MUSC) in Cologne has supported microgravity experiments in the field of materials and life sciences since 1979. In the beginning of user support activities, MUSC tasks comprised the basic ground and mission support, whereas present programmes are expanded on, for example, powerful telescience and advanced real time data acquisition capabilities for efficient experiment operation and monitoring. In view of the Space Station era, user support functions will increase further. Additional tasks and growing responsibilities must be covered, e.g. extended science support as well as experiment and facility operations. The user support for TEMPUS IML-2, under contract of the German Space Agency DARA, represents a further step towards the required new-generation of future ground programme. TEMPUS is a new highly sophisticated Spacelab multi-user facility for containerless processing of metallic samples. Electromagnetic levitation technique is applied and various experiment diagnosis tools are offered. Experiments from eight U.S. and German investigator groups have been selected for flight on the second International Microgravity Laboratory Mission IML-2 in 1994. Based on the experience gained in the research programme of the DLR Institute for Space Simulation since 1984, MUSC is performing a comprehensive experiment preparation programme in close collaboration with the investigator teams. Complex laboratory equipment has been built up for technology and experiment preparation development. New experiment techniques have been developed for experiment verification tests. The MUSC programme includes thorough analysis and testing of scientific requirements of every proposed experiment with respect to the facility hard- and software capabilities. In addition, studies on the experiment-specific operation requirements have been performed and suitable telescience scenarios were analysed. The present paper will give a survey of the TEMPUS user support tasks emphasizing the advanced science support activities, which are considered significant for future ground programmes.

Commercial investments in Combustion research aboard ISS

NASA Astrophysics Data System (ADS)

Schowengerdt, F. D.

2000-01-01

The Center for Commercial Applications of Combustion in Space (CCACS) at the Colorado School of Mines is working with a number of companies planning commercial combustion research to be done aboard the International Space Station (ISS). This research will be conducted in two major ISS facilities, SpaceDRUMS™ and the Fluids and Combustion Facility. SpaceDRUMS™, under development by Guigne Technologies, Ltd., of St. John's Newfoundland, is a containerless processing facility employing active acoustic sample positioning. It is capable of processing the large samples needed in commercial research and development with virtually complete vibration isolation from the space station. The Fluids and Combustion Facility (FCF), being developed by NASA-Glenn Research Center in Cleveland, is a general-purpose combustion furnace designed to accommodate a wide range of scientific experiments. SpaceDRUMS™ will be the first commercial hardware to be launched to ISS. Launch is currently scheduled for UF-1 in 2001. The CCACS research to be done in SpaceDRUMS™ includes combustion synthesis of glass-ceramics and porous materials. The FCF is currently scheduled to be launched to ISS aboard UF-3 in 2002. The CCACS research to be done in the FCF includes water mist fire suppression, catalytic combustion and flame synthesis of ceramic powders. The companies currently planning to be involved in the research include Guigne International, Ltd., Technology International, Inc., Coors Ceramics Company, TDA Research, Advanced Refractory Technologies, Inc., ADA Technologies, Inc., ITN Energy Systems, Inc., Innovative Scientific Solutions, Inc., Princeton Instruments, Inc., Environmental Engineering Concepts, Inc., and Solar Turbines, Inc. Together, these companies are currently investing almost $2 million in cash and in-kind annually toward the seven commercial projects within CCACS. Total private investment in CCACS research to date is over $7 million. .

Electrostatic levitation facility optimized for neutron diffraction studies of high temperature liquids at a spallation neutron source

DOE Office of Scientific and Technical Information (OSTI.GOV)

Mauro, N. A., E-mail: namauro@noctrl.edu; Vogt, A. J.; Derendorf, K. S.

2016-01-15

Neutron diffraction studies of metallic liquids provide valuable information about inherent topological and chemical ordering on multiple length scales as well as insight into dynamical processes at the level of a few atoms. However, there exist very few facilities in the world that allow such studies to be made of reactive metallic liquids in a containerless environment, and these are designed for use at reactor-based neutron sources. We present an electrostatic levitation facility, NESL (for Neutron ElectroStatic Levitator), which takes advantage of the enhanced capabilities and increased neutron flux available at spallation neutron sources (SNSs). NESL enables high quality elasticmore » and inelastic neutron scattering experiments to be made of reactive metallic and other liquids in the equilibrium and supercooled temperature regime. The apparatus is comprised of a high vacuum chamber, external and internal neutron collimation optics, and a sample exchange mechanism that allows up to 30 samples to be processed between chamber openings. Two heating lasers allow excellent sample temperature homogeneity, even for samples approaching 500 mg, and an automated temperature control system allows isothermal measurements to be conducted for times approaching 2 h in the liquid state, with variations in the average sample temperature of less than 0.5%. To demonstrate the capabilities of the facility for elastic scattering studies of liquids, a high quality total structure factor for Zr{sub 64}Ni{sub 36} measured slightly above the liquidus temperature is presented from experiments conducted on the nanoscale-ordered materials diffractometer (NOMAD) beam line at the SNS after only 30 min of acquisition time for a small sample (∼100 mg)« less

Droplet Image Super Resolution Based on Sparse Representation and Kernel Regression

NASA Astrophysics Data System (ADS)

Zou, Zhenzhen; Luo, Xinghong; Yu, Qiang

2018-02-01

Microgravity and containerless conditions, which are produced via electrostatic levitation combined with a drop tube, are important when studying the intrinsic properties of new metastable materials. Generally, temperature and image sensors can be used to measure the changes of sample temperature, morphology and volume. Then, the specific heat, surface tension, viscosity changes and sample density can be obtained. Considering that the falling speed of the material sample droplet is approximately 31.3 m/s when it reaches the bottom of a 50-meter-high drop tube, a high-speed camera with a collection rate of up to 106 frames/s is required to image the falling droplet. However, at the high-speed mode, very few pixels, approximately 48-120, will be obtained in each exposure time, which results in low image quality. Super-resolution image reconstruction is an algorithm that provides finer details than the sampling grid of a given imaging device by increasing the number of pixels per unit area in the image. In this work, we demonstrate the application of single image-resolution reconstruction in the microgravity and electrostatic levitation for the first time. Here, using the image super-resolution method based on sparse representation, a low-resolution droplet image can be reconstructed. Employed Yang's related dictionary model, high- and low-resolution image patches were combined with dictionary training, and high- and low-resolution-related dictionaries were obtained. The online double-sparse dictionary training algorithm was used in the study of related dictionaries and overcome the shortcomings of the traditional training algorithm with small image patch. During the stage of image reconstruction, the algorithm of kernel regression is added, which effectively overcomes the shortcomings of the Yang image's edge blurs.

Flight Planning for the International Space Station - Levitation Observation of Dendrite Evolution in Steel Ternary Alloy Rapid Solidification (LODESTARS)

NASA Technical Reports Server (NTRS)

Flemings, Merton C.; Matson, Douglas M.; Hyers, Robert W.; Rogers, Jan R.

2003-01-01

During rapid solidification, a molten sample is cooled below its equilibrium solidification temperature to form a metastable liquid. Once nucleation is initiated, growth of the solid phase proceeds and can be seen as a sudden rise in temperature. The heat of fusion is rejected ahead of the growing dendrites into the undercooled liquid in a process known as recalescence. Fe-Cr-Ni alloys may form several equilibrium phases and the hypoeutectic alloys, with compositions near the commercially important 316 stainless steel alloy, are observed to solidify by way of a two-step process known as double recalescence. During double recalescence, the first temperature rise is associated with formation of the metastable ferritic solid phase with subsequent conversion to the stable austenitic phase during the second temperature rise. Selection of which phase grows into the undercooled melt during primary solidification may be accomplished by choice of the appropriate nucleation trigger material or by control of the processing parameters during rapid solidification. Due to the highly reactive nature of the molten sample material and in order to avoid contamination of the undercooled melt, a containerless electromagnetic levitation (EML) processing technique is used. In ground-based EML, the same forces that support the weight of the sample against gravity also drive convection in the liquid sample. However, in microgravity, the force required to position the sample is greatly reduced, so convection may be controlled over a wide range of internal flows. Space Shuttle experiments have shown that the double recalescence behavior of Fe-Cr-Ni alloys changes between ground and space EML experiments. This program is aimed at understanding how melt convection influences phase selection and the evolution of rapid solidification microstructures.

Relationship between topological order and glass forming ability in densely packed enstatite and forsterite composition glasses

PubMed Central

Kohara, S.; Akola, J.; Morita, H.; Suzuya, K.; Weber, J. K. R.; Wilding, M. C.; Benmore, C. J.

2011-01-01

The atomic structures of magnesium silicate melts are key to understanding processes related to the evolution of the Earth’s mantle and represent precursors to the formation of most igneous rocks. Magnesium silicate compositions also represent a major component of many glass ceramics, and depending on their composition can span the entire fragility range of glass formation. The silica rich enstatite (MgSiO3) composition is a good glass former, whereas the forsterite (Mg2SiO4) composition is at the limit of glass formation. Here, the structure of MgSiO3 and Mg2SiO4 composition glasses obtained from levitated liquids have been modeled using Reverse Monte Carlo fits to diffraction data and by density functional theory. A ring statistics analysis suggests that the lower glass forming ability of the Mg2SiO4 glass is associated with a topologically ordered and very narrow ring distribution. The MgOx polyhedra have a variety of irregular shapes in MgSiO3 and Mg2SiO4 glasses and a cavity analysis demonstrates that both glasses have almost no free volume due to a large contribution from edge sharing of MgOx-MgOx polyhedra. It is found that while the atomic volume of Mg cations in the glasses increases compared to that of the crystalline phases, the number of Mg-O contacts is reduced, although the effective chemical interaction of Mg2+ remains similar. This unusual structure-property relation of Mg2SiO4 glass demonstrates that by using containerless processing it may be possible to synthesize new families of dense glasses and glass ceramics with zero porosity. PMID:21873237

Supersaturated Electrolyte Solutions: Theory and Experiment

NASA Technical Reports Server (NTRS)

Izmailov, Alexander F.; Myerson, Allan S.; Na, Han-Soo

1995-01-01

Highly supersaturated electrolyte solutions can be prepared and studied employing an electrodynamic levitator trap (ELT) technique. The ELT technique involves containerless suspension of a microdroplet thus eliminating dust, dirt, and container walls which normally cause heterogeneous nucleation. This allows very high supersaturations to be achieved. A theoretical study of the experimental results obtained for the water activity in microdroplets of various electrolyte solutions is based on the development of the Cahn-Hilliard formalism for electrolyte solutions. In the approach suggested the metastable state for electrolyte solutions is described in terms of the conserved order parameter omega(r,t) associated with fluctuations of the mean solute concentration n(sub 0). Parameters of the corresponding Ginzburg-Landau free energy functional which defines the dynamics of metastable state relaxation are determined and expressed through the experimentally measured quantities. A correspondence of 96-99 % between theory and experiment for all solutions studied was achieved and allowed the determination of an analytical expression for the spinodal concentration n(sub spin), and its calculation for various electrolyte solutions at 298 K. The assumption that subcritical solute clusters consist of the electrically neutral Bjerrum pairs has allowed both analytical and numerical investigation of the number-size N(sub c) of nucleation monomers (aggregates of the Bjerrum pairs) which are elementary units of the solute critical clusters. This has also allowed estimations for the surface tension Alpha, and equilibrium bulk energy Beta per solute molecule in the nucleation monomers. The dependence of these properties on the temperature T and on the solute concentration n(sub 0) through the entire metastable zone (from saturation concentration n(sub sat) to spinodal n(sub spin) is examined. It has been demonstrated that there are the following asymptotics: N(sub c), = I at spinodal concentration and N(sub c) = infinity at saturation.

Overview: Experimental studies of crystal nucleation: Metals and colloids.

PubMed

Herlach, Dieter M; Palberg, Thomas; Klassen, Ina; Klein, Stefan; Kobold, Raphael

2016-12-07

Crystallization is one of the most important phase transformations of first order. In the case of metals and alloys, the liquid phase is the parent phase of materials production. The conditions of the crystallization process control the as-solidified material in its chemical and physical properties. Nucleation initiates the crystallization of a liquid. It selects the crystallographic phase, stable or meta-stable. Its detailed knowledge is therefore mandatory for the design of materials. We present techniques of containerless processing for nucleation studies of metals and alloys. Experimental results demonstrate the power of these methods not only for crystal nucleation of stable solids but in particular also for investigations of crystal nucleation of metastable solids at extreme undercooling. This concerns the physical nature of heterogeneous versus homogeneous nucleation and nucleation of phases nucleated under non-equilibrium conditions. The results are analyzed within classical nucleation theory that defines the activation energy of homogeneous nucleation in terms of the interfacial energy and the difference of Gibbs free energies of solid and liquid. The interfacial energy acts as barrier for the nucleation process. Its experimental determination is difficult in the case of metals. In the second part of this work we therefore explore the potential of colloidal suspensions as model systems for the crystallization process. The nucleation process of colloids is observed in situ by optical observation and ultra-small angle X-ray diffraction using high intensity synchrotron radiation. It allows an unambiguous discrimination of homogeneous and heterogeneous nucleation as well as the determination of the interfacial free energy of the solid-liquid interface. Our results are used to construct Turnbull plots of colloids, which are discussed in relation to Turnbull plots of metals and support the hypothesis that colloids are useful model systems to investigate crystal nucleation.

Recent advances in the study of the UO2-PuO2 phase diagram at high temperatures

NASA Astrophysics Data System (ADS)

Böhler, R.; Welland, M. J.; Prieur, D.; Cakir, P.; Vitova, T.; Pruessmann, T.; Pidchenko, I.; Hennig, C.; Guéneau, C.; Konings, R. J. M.; Manara, D.

2014-05-01

Recently, novel container-less laser heating experimental data have been published on the melting behaviour of pure PuO2 and PuO2-rich compositions in the uranium dioxide-plutonium dioxide system. Such data showed that previous data obtained by more traditional furnace heating techniques were affected by extensive interaction between the sample and its containment. It is therefore paramount to check whether data so far used by nuclear engineers for the uranium-rich side of the pseudo-binary dioxide system can be confirmed or not. In the present work, new data are presented both in the UO2-rich part of the phase diagram, most interesting for the uranium-plutonium dioxide based nuclear fuel safety, and in the PuO2 side. The new results confirm earlier furnace heating data in the uranium-dioxide rich part of the phase diagram, and more recent laser-heating data in the plutonium-dioxide side of the system. As a consequence, it is also confirmed that a minimum melting point must exist in the UO2-PuO2 system, at a composition between x(PuO2) = 0.4 and x(PuO2) = 0.7 and 2900 K ⩽ T ⩽ 3000 K. Taking into account that, especially at high temperature, oxygen chemistry has an effect on the reported phase boundary uncertainties, the current results should be projected in the ternary U-Pu-O system. This aspect has been extensively studied here by X-ray diffraction and X-ray absorption spectroscopy. The current results suggest that uncertainty bands related to oxygen behaviour in the equilibria between condensed phases and gas should not significantly affect the qualitative trend of the current solid-liquid phase boundaries.

Droplet Image Super Resolution Based on Sparse Representation and Kernel Regression

NASA Astrophysics Data System (ADS)

Zou, Zhenzhen; Luo, Xinghong; Yu, Qiang

2018-05-01

Microgravity and containerless conditions, which are produced via electrostatic levitation combined with a drop tube, are important when studying the intrinsic properties of new metastable materials. Generally, temperature and image sensors can be used to measure the changes of sample temperature, morphology and volume. Then, the specific heat, surface tension, viscosity changes and sample density can be obtained. Considering that the falling speed of the material sample droplet is approximately 31.3 m/s when it reaches the bottom of a 50-meter-high drop tube, a high-speed camera with a collection rate of up to 106 frames/s is required to image the falling droplet. However, at the high-speed mode, very few pixels, approximately 48-120, will be obtained in each exposure time, which results in low image quality. Super-resolution image reconstruction is an algorithm that provides finer details than the sampling grid of a given imaging device by increasing the number of pixels per unit area in the image. In this work, we demonstrate the application of single image-resolution reconstruction in the microgravity and electrostatic levitation for the first time. Here, using the image super-resolution method based on sparse representation, a low-resolution droplet image can be reconstructed. Employed Yang's related dictionary model, high- and low-resolution image patches were combined with dictionary training, and high- and low-resolution-related dictionaries were obtained. The online double-sparse dictionary training algorithm was used in the study of related dictionaries and overcome the shortcomings of the traditional training algorithm with small image patch. During the stage of image reconstruction, the algorithm of kernel regression is added, which effectively overcomes the shortcomings of the Yang image's edge blurs.

USML-1 Glovebox experiments

NASA Technical Reports Server (NTRS)

Naumann, Robert J.

1995-01-01

This report covers the development of and results from three experiments that were flown in the Materials Science Glovebox on USML-1: Marangoni convection in Closed Containers (MCCC), Double Float Zone (DFZ), and Fiber Pulling in Microgravity (FPM). The Glovebox provided a convenient, low cost method for doing simple 'try and see' experiments that could test new concepts or elucidate microgravity phenomena. Since the Glovebox provided essentially one (or possibly two levels of confinement, many of the stringent verification and test requirements on the experiment apparatus could be relaxed and a streamlined test and verification plan for flight qualification could be implemented. Furthermore, the experiments were contained in their own carrying cases whose external configurations could be identified early in the integration sequence for stowage considerations while delivery of the actual experiment apparatus could be postponed until only a few months before flight. This minimized the time fluids must be contained and reduced the possibility of corrosive reactions that could ruin the experiment. In many respects, this exercise was as much about developing a simpler, cheaper way of doing crew-assisted science as it was about the actual scientific accomplishments of the individual experiments. The Marangoni Convection in Closed Containers experiment was designed to study the effects of a void space in a simulated Bridgman crystal growth configuration and to determine if surface tension driven convective flows that may result from thermal gradients along any free surfaces could affect the solidification process. The Fiber Pulling in Microgravity experiment sought to separate the role of gravity drainage from capillarity effects in the break-up of slender cylindrical liquid columns. The Stability of a Double Float Zone experiment explored the feasibility of a quasi-containerless process in which a solidifying material is suspended by two liquid bridges of its own melt.

Kombinierte Hoch-/Niedrig-Dosis-Therapie mit systemischen Glukokor-tikoiden bei schweren Verlaufsformen der Alopecia areata im Kindesalter.

PubMed

Jahn-Bassler, Karin; Bauer, Wolfgang Michael; Karlhofer, Franz; Vossen, Matthias G; Stingl, Georg

2017-01-01

Schwere Verlaufsformen der Alopecia areata (AA) im Kindesalter sind aufgrund limitierter Optionen therapeutisch herausfordernd. Systemische, hochdosierte Glukokortikoide weisen die schnellste Ansprechrate auf, nach dem Absetzen kommt es allerdings zu Rezidiven. Eine längerfristige Hochdosis-Anwendung ist aufgrund der zu erwartenden Nebenwirkungen nicht empfehlenswert. Eine dauerhafte Steroiderhaltungstherapie unterhalb der Cushing-Schwellen-Dosis nach Bolustherapie könnte die Krankheitsaktivität ohne Nebenwirkungen längerfristig unterdrücken. Im Rahmen einer offenen Anwendungsbeobachtung wurden 13 Kinder mit schweren Formen der AA in diese Studie eingeschlossen. Bei sieben Kindern lag eine AA totalis/universalis vor, bei sechs eine multifokale AA mit Befall von mehr als 50 % der Kopfhaut. Das Therapieregime sah eine initiale Prednisolon-Dosierung von 2 mg/kg Körpergeweicht (KG) vor und wurde innerhalb von neun Wochen auf eine Erhaltungsdosierung unter der individuellen Cushing-Schwelle reduziert. Der Nachbeobachtungszeitraum betrug ein bis drei Jahre. Wir beobachteten in 62 % aller Fälle ein komplettes Nachwachsen der Haare. Die mittlere Dauer bis zum Ansprechen lag bei 6,6 Wochen und konnte mit der Erhaltungstherapie über den gesamten Beobachtungszeitraum aufrechterhalten werden. An Nebenwirkungen wurden ausschließlich eine Gewichtszunahme (1-3 kg) bei allen Behandelten sowie eine milde Steroidakne in 23 % der Fälle beobachtet. Die kombinierte Hoch-/Niedrig-Dosis-Therapie mit systemischen Glukokortikoiden mittels Prednisolon zeigte eine hohe, dauerhafte Ansprechrate ohne signifikante Nebenwirkungen. © 2017 Deutsche Dermatologische Gesellschaft (DDG). Published by John Wiley & Sons Ltd.

Zu einer inhaltsorientierten Theorie des Lernens und Lehrens der biologischen Evolution

NASA Astrophysics Data System (ADS)

Wallin, Anita

Der Zweck dieser Studie (zwecks Überblick siehe dazu Abb. 9.1) war zu untersuchen, wie die Schüler der Sekundarstufe II ein Verständnis von der Theorie der biologischen Evolution entwickeln. Vom Ausgangspunkt "Vorurteile der Schüler“ ausgehend wurden Unterrichtssequenzen entwickelt und drei verschiedene Lernexperimente in einem zyklischen Prozess durchgeführt. Das Wissen der Schüler wurde vor, während und nach den Unterrichtssequenzen mit Hilfe von schriftlichen Tests, Interviews und Diskussionsrunden in kleinen Gruppen abgefragt. Etwa 80 % der Schüler hatten vor dem Unterricht alternative Vorstellungen von Evolution, und in dem Nachfolgetest erreichten circa 75 % ein wissenschaftliches Niveau. Die Argumentation der Schüler in den verschiedenen Tests wurde sorgfältig unter Rücksichtnahme auf Vorurteile, der konzeptionellen Struktur der Theorie der Evolution und den Zielen des Unterrichts analysiert. Daraus konnten Einsichten in solche Anforderungen an Lehren und Lernen gewonnen werden, die Herausforderungen an Schüler und Lehrer darstellen, wenn sie anfangen, evolutionäre Biologie zu lernen oder zu lehren. Ein wichtiges Ergebnis war, dass das Verständnis existierender Variation in einer Population der Schlüssel zum Verständnis von natürlicher Selektion ist. Die Ergebnisse sind in einer inhaltsorientierten Theorie zusammengefasst, welche aus drei verschiedenen Aspekten besteht: 1) den inhaltsspezifischen Aspekten, die einzigartig für jedes wissenschaftliche Feld sind; 2) den Aspekten, die die Natur der Wissenschaft betreffen; und 3) den allgemeinen Aspekten. Diese Theorie kann in neuen Experimenten getestet und weiter entwickelt werden.

Gebrauch von Komplementärmedizin bei Patienten mit metastasierendem Melanom unter Therapie mit Ipilimumab innerhalb einer klinischen Studie.

PubMed

Huebner, Jutta; Mohr, Peter; Simon, Jan-Christoph; Fluck, Michael; Berking, Carola; Zimmer, Lisa; Loquai, Carmen

2016-05-01

In Deutschland wenden 40-90 % aller Krebspatienten Methoden der komplementären and alternativen Medizin (KAM) an. Bis dato gibt es kein Datenmaterial zum Einsatz der KAM bei Melanompatienten. Das Ziel unserer Studie war es, Daten über den Gebrauch, die Informationsquellen und Ziele von Patienten mit metastasierendem Melanom zu erfassen. Einhundertsechsundfünfzig Patienten aus 25 Studienzentren nahmen an der DecOG-MM-PAL Multibasket Studie teil. Die beteiligten Personen wurden auch gebeten, an einer Nebenstudie teilzunehmen, die ihren Gebrauch von KAM erfassen sollte. Dazu wurde während der Behandlung ein standardisierter Fragebogen zu genau festgelegten Zeitpunkten ausgeteilt. Insgesamt gingen 55 Fragebögen von 32 (21 %) Melanompatienten ein. Von diesen gaben 17 (53 %) ein Interesse an KAM an, und sieben (22 %) machten von KAM Gebrauch. Die Hauptinformationsquellen (31 %) waren Familienmitglieder und Freunde, gefolgt von Ärzten (19 %). Die Hauptgründe für die Anwendung von KAM waren die Stärkung des Immunsystems (41 %) und des Körpers (34 %). Nahrungsergänzungsmittel (Vitamine und Spurenelemente) wurden am häufigsten angewendet (28 %). Eine relativ hohe Anzahl an Patienten mit metastasierendem Melanom machte trotz Teilnahme an einer klinischen Studie von KAM Gebrauch. Wechselwirkungen könnten durch biologisch basierte KAM auftreten, und hier besonders bei immunmodulierenden KAM- Strategien. Um Risiken zu vermeiden, sollte die Kommunikation zwischen den Ärzten und den Patienten verbessert werden. © 2016 Deutsche Dermatologische Gesellschaft (DDG). Published by John Wiley & Sons Ltd.

Einsatz und Wirksamkeit von Systemtherapien bei Erwachsenen mit schwerer Neurodermitis: Erste Ergebnisse des deutschen Neurodermitis-Registers TREATgermany.

PubMed

Schmitt, Jochen; Abraham, Susanne; Trautmann, Freya; Stephan, Victoria; Fölster-Holst, Regina; Homey, Bernhard; Bieber, Thomas; Novak, Natalija; Sticherling, Michael; Augustin, Matthias; Kleinheinz, Andreas; Elsner, Peter; Weidinger, Stephan; Werfel, Thomas

2017-01-01

Versorgungsregister dienen der Erfassung des Einsatzes und der Wirksamkeit von Therapien unter realen Versorgungsbedingungen und sind als Basis einer evidenzbasierten Gesundheitsversorgung unverzichtbar. Das deutsche Neurodermitis-Register TREATgermany wurde als weltweit erstes Register für Patienten mit schwerer Neurodermitis 2011 initiiert. Erwachsene mit schwerer Neurodermitis (aktuelle/frühere antientzündliche Systemtherapie und/oder objektiver SCORAD ≥ 40) werden über einen Zeitraum von 24 Monaten prospektiv beobachtet. Anhand validierter Erhebungsinstrumente werden die klinische Erkrankungsschwere (EASI, SCORAD), Lebensqualität (DLQI), Symptome, globale Erkrankungsschwere sowie die Patientenzufriedenheit erfasst und die durchgeführten Therapien dokumentiert. Die vorliegende Analyse beschreibt die Charakteristika, Therapiewahl und Wirksamkeit der eingesetzten antiinflammatorischen Systemtherapien der bis Oktober 2014 eingeschlossenen Patienten. An fünf Zentren wurden insgesamt 78 Patienten (Durchschnittsalter 39 Jahre, 61 % männlich) eingeschlossen. Bei den Patienten besteht eine hohe Inanspruchnahme ambulanter und stationärer Leistungen. Ciclosporin war das am häufigsten eingesetzte Systemtherapeutikum und zeigte die höchste klinische Effektivität (EASI-50-Ansprechrate 51 %; EASI-75-Ansprechrate 34 % nach zwölfwöchiger Therapie). Azathioprin, Methotrexat (MTX), Prednisolon oral, Mycophenolat, Alitretinoin und Leflunomid wurden ebenfalls bei einzelnen Patienten eingesetzt. Die vorliegende Registerauswertung gibt wichtige Hinweise zur derzeitigen Versorgung von Erwachsenen mit schwerer Neurodermitis in Deutschland, dokumentiert die hohe Erkrankungslast, den Nutzen vorhandener Therapien und den Bedarf an weiteren, effektiven und in der Langzeitanwendung sicheren Therapieoptionen. © 2017 Deutsche Dermatologische Gesellschaft (DDG). Published by John Wiley & Sons Ltd.

Titanisierung von Implantatoberflächen

NASA Astrophysics Data System (ADS)

Zimmermann, Hanngörg; Heinlein, Markus; Guldner, Norbert W.

Titan gilt seit Jahrzehnten als einer der wichtigsten Implantatwerkstoffe in der Medizin. Neben den guten mechanischen Eigenschaften (Leichtigkeit, hohe Festigkeit etc.), besitzen Titanimplantate vor allem eine hervorragende Körperverträglichkeit, so dass die Implantate optimal in den humanen Organismus integriert werden [1]. Ist jedoch aufgrund der Anforderungen an das Implantat eine hohe Flexibilität und/ oder Elastizität gefragt, so scheidet der Werkstoff Titan aufgrund seiner spröden und unflexiblen Materialeigenschaften aus. Die Folge ist der Einsatz von Implantatmaterialien, sowohl künstlichen als auch biologischen Ursprungs, welche nicht selten eine unzureichende Biokompatibilität aufweisen und somit zu Fremdköper- und immunologischen Reaktionen und Einkapselung des Implantates führen können. Die Erhöhung der Körperverträglichkeit, eine Adaption an das biologische Umfeld und eine hohe Biokompatibilität sind demzufolge die wichtigsten Eigenschaften bei der bedarfsgerechten Herstellung von Implantaten und Implantatoberflächen. Zur Gestaltung von innovativen, biokompatiblen Oberflächen stehen unterschiedliche technische Lösungsansätze zur Verfügung. Zum einen besteht die Möglichkeit, geeignete Oberflächeneigenschaften aus dem Grundmaterial selbst zu optimieren. Dies geschieht unter anderem durch Modifikation der Werkstoffoberflächen in Form von Texturierungen und Oberflächenrauhigkeiten. Zum anderen können die Oberflächeneigenschaften unabhängig von denen des Trägermaterials gestaltet werden. Durch Funktionalisierung der Oberflächen mit geeigneten Beschichtungen oder der Zugabe von Medikamenten (Drug Eluting) werden die Kunststoffimplantate dahingehend verändert, dass eine Steigerung der Körperakzeptanz erreicht wird. Die Titanbeschichtung von Implantatoberflächen kombiniert die positiven Materialeigenschaften von Titan und Polymer.

Neue Laser und Strahlquellen - alte und neue Risiken?

PubMed

Paasch, Uwe; Schwandt, Antje; Seeber, Nikolaus; Kautz, Gerd; Grunewald, Sonja; Haedersdal, Merete

2017-05-01

Die Entwicklungen im Bereich dermatologischer Laser, hochenergetischer Blitzlampen, LED und neuer Energie- und Strahlquellen der letzten Jahre haben gezeigt, dass mit neuen Wellenlängen, Konzepten und Kombinationen zusätzliche, zum Teil über den ästhetischen Bereich hinaus gehende therapeutische Optionen für den Dermatologen erschlossen werden konnten. Wurden bisher zum Beispiel mit fraktionalen Lasern Falten behandelt, sind eben diese Systeme heute in Kombination mit Medikamenten wichtige Werkzeuge bei der Behandlung von Narben, bei Feldkanzerisierung und epithelialen Tumoren. Die Anforderungen an den die Indikation stellenden und vorzugsweise therapierenden Arzt steigen mit der immer komplexer werdenden Technik und den zunehmenden Komorbiditäten und Komedikationen einer älter werdenden Patientenklientel. Parallel etabliert wurden, zunächst für einige wenige Indikationen, Geräte für die Heimanwendung, die sich durch geringe Leistung und spezielle Sicherheitsvorkehrungen zur Vermeidung von Unfällen, Risiken und Nebenwirkungen auszeichnen. Trotz der reduzierten Effizienz solcher Selbstbehandlungsmaßnahmen steigt die Wahrscheinlichkeit einer Fehlanwendung, da die Grundvoraussetzung für eine korrekte Therapie, nämlich die exakte Diagnose und Indikationsstellung, nicht vorausgesetzt werden kann. Bei einer Haarentfernung können so Pigmenttumoren, bei einer Faltentherapie neoplastische Hautveränderungen adressiert und zu erwartende, unvorhergesehene und neue Nebenwirkungen und Komplikationen induziert werden. In diesem Szenario ist es wichtig, alle potenziellen Anwender dieser neuen Technologien vor deren Einsatz so zu qualifizieren, dass den Therapierten maximale Therapiesicherheit bei höchster Effizienz unter dem Leitbild diagnosis certa - ullae therapiae fundamentum garantiert wird. © 2017 Deutsche Dermatologische Gesellschaft (DDG). Published by John Wiley & Sons Ltd.

[Treatment of ASS-Associated Polyposis (ASSAP) with a cysteinyl leukotriene receptor antagonist - a prospective drug study on its antiinflammatory effects].

PubMed

Grundmann, T; Töpfner, M

2001-10-01

In a high rate of cases with recurrent polyposis an association with ASS-intolerance is detectable despite missing pulmonary symptoms. New examinations of a disturbed arachidonic acid metabolism lead to the development of new therapeutical options. Treatment with leukotriene-receptor antogonists (LTA) showed primarily good results in therapy of ASS-associated asthma. 18 patients with ASS-intolerance trias - diagnosed by oral provocation - were treated with the LTA Montelukast, after undergoing sinus surgery. Patients underwent a diagnostic pathway of provocation including four groups: recurrent chronic sinusitis, excessive polyposis, polyposis associated with asthma and anaphylactic symptoms after oral ASS-intake. Clinically we examined the following parameters periodically after sinus surgery: nasal and pulmonal symptoms by scoring levels, recurrency of polypoid hyperplasia by endoscopic follow-ups and serum ECP-levels. To evaluate antiinflammatory tissue effects of LTA EG1/EG2 labelled cells and cytokine levels of Interleukin 5 in mucosa samples of the lower turbinate were analysed under LTA-therapy. Under therapy with LTA we saw a beneficial effect on nasal and pulmonary symptoms and a significant reduction of recurrent polyposis in endoscopic examinations in relation to the untreated group. Results were proven by a permanent reduction of serum ECP-level. A reduction of the rate of EG2-positive cells according to decreased Interleukin 5 levels in the nasal mucosa unter LTA-treatment assumed antiinflammatory effects on ASS-associated polyposis. We could demonstrate antiinflammatory effects of Leukotriene-Receptor-Antagonists primarily during postoperative treatment of patients with ASS-associated nasal polyps.

Spirituelles Wohlbefinden und Coping bei Sklerodermie, Lupus erythematodes und malignem Melanom.

PubMed

Pilch, Michaela; Scharf, Sabina Nadine; Lukanz, Martin; Wutte, Nora Johanna; Fink-Puches, Regina; Glawischnig-Goschnik, Monika; Unterrainer, Human-Friedrich; Aberer, Elisabeth

2016-07-01

Religiös-spirituelles Wohlbefinden ist verbunden mit höherer Vitalität und verminderter Depressionsneigung. In unserer Studie untersuchten wir die Strategien zur Krankheitsbewältigung und die Rolle von Religiosität-Spiritualität (R-S) zur Verbesserung des subjektiven Wohlbefindens. 149 Patienten (107 Frauen), 44 mit systemischer Sklerodermie (SKL), 48 mit Lupus erythematodes (LE) und 57 mit malignem Melanom (MM), Stadium I-II, wurden mittels eines selbstentwickelten Fragebogens zum subjektiven Wohlbefinden, zu den mit der Erkrankung einhergehenden Umständen sowie mit dem Multidimensionalen Inventar (MI-RSB) zu R-S befragt. LE-Patienten sind zum Zeitpunkt der Diagnosestellung stärker belastet als SKL- und MM-Patienten. SKL- und LE-Patienten können erst nach Jahren die Erkrankung akzeptieren. Der Gesamtscore des religiös-spirituellen Befindens liegt bei LE-Patienten signifikant unter dem Wert der Normalbevölkerung. Fotosensitivität und Gelenksschmerzen sind bei LE-Patienten negativ assoziiert mit der Fähigkeit Vergeben zu können. SKL-Patienten mit Gesichtsveränderungen und Lungenbeteiligung zeigen höhere allgemeine Religiosität. MM-Patienten haben höhere Werte für transzendente Hoffnung. Vorträge über die Krankheit und psychologische Betreuung sind die wichtigsten Bedürfnisse von Patienten mit SKL, LE und MM an ihre Betreuer. Religiös-spirituelle Angebote zur Krankheitsverarbeitung scheinen derzeit eine untergeordnete Rolle zu spielen, könnten aber eine wichtige Ressource sein, der man in Zukunft mehr Aufmerksamkeit schenken sollte. © 2016 Deutsche Dermatologische Gesellschaft (DDG). Published by John Wiley & Sons Ltd.

Processing and Mechanical Properties of NiAl-Based In-Situ Composites. Ph.D. Thesis Final Report

NASA Technical Reports Server (NTRS)

Johnson, David Ray

1994-01-01

In-situ composites based on the NiAl-Cr eutectic system were successfully produced by containerless processing and evaluated. The NiAl-Cr alloys had a fibrous microstructure while the NiAl-(Cr,Mo) alloys containing 1 at. percent or more molybdenum exhibited a lamellar structure. The NiAl-28Cr-6Mo eutectic displays promising high temperature strength while still maintaining a reasonable room temperature fracture toughness when compared to other NiAl-based materials. The Laves phase NiAlTa was used to strengthen NiAl and very promising creep strengths were found for the directionally solidified NiAl-NiAlTa eutectic. The eutectic composition was found to be near NiAl-15.5Ta (at. percent) and well aligned microstructures were produced at this composition. An off-eutectic composition of NiAl-14.5Ta was also processed, consisting of NiAl dendrites surrounded by aligned eutectic regions. The room temperature toughness of these two phase alloys was similar to that of polycrystalline NiAl even with the presence of the brittle Laves phase NiAlTa. Polyphase in-situ composites were generated by directional solidification of ternary eutectics. The systems investigated were the Ni-Al-Ta-X (X=Cr, Mo, or V) alloys. Ternary eutectics were found in each of these systems and both the eutectic composition and temperature were determined. Of these ternary eutectics, the one in the NiAl-Ta-Cr system was found to be the most promising. The fracture toughness of the NiAl-(Cr,Al)NiTa-Cr eutectic was intermediate between those of the NiAl-NiAlTa eutectic and the NiAl-Cr eutectic. The creep strength of this ternary eutectic was similar to or greater than that of the NiAl-Cr eutectic.

Experiments on Nucleation in Different Flow Regimes

NASA Technical Reports Server (NTRS)

Bayuzick, R. J.; Hofmeister, W. H.; Morton, C. M.; Robinson, M. B.

1999-01-01

The vast majority of metallic engineering materials are solidified from the liquid phase. Understanding the solidification process is essential to control microstructure, which in turn, determines the properties of materials. The genesis of solidification is nucleation, where the first stable solid forms from the liquid phase. Nucleation kinetics determine the degree of undercooling and phase selection. As such, it is important to understand nucleation phenomena in order to control solidification or glass formation in metals and alloys. Early experiments in nucleation kinetics were accomplished by droplet dispersion methods. Dilatometry was used by Turnbull and others, and more recently differential thermal analysis and differential scanning calorimetry have been used for kinetic studies. These techniques have enjoyed success; however, there are difficulties with these experiments. Since materials are dispersed in a medium, the character of the emulsion/metal interface affects the nucleation behavior. Statistics are derived from the large number of particles observed in a single experiment, but dispersions have a finite size distribution which adds to the uncertainty of the kinetic determinations. Even though temperature can be controlled quite well before the onset of nucleation, the release of the latent heat of fusion during nucleation of particles complicates the assumption of isothermality during these experiments. Containerless processing has enabled another approach to the study of nucleation kinetics. With levitation techniques it is possible to undercool one sample to nucleation repeatedly in a controlled manner, such that the statistics of the nucleation process can be derived from multiple experiments on a single sample. The authors have fully developed the analysis of nucleation experiments on single samples following the suggestions of Skripov. The advantage of these experiments is that the samples are directly observable. The nucleation temperature can be measured by noncontact optical pyrometry, the mass of the sample is known, and post processing analysis can be conducted on the sample. The disadvantages are that temperature measurement must have exceptionally high precision, and it is not possible to isolate specific heterogeneous sites as in droplet dispersions.

Sub-ppb Oxygen Contaminant Detection in Semi-Conductor Processing

NASA Technical Reports Server (NTRS)

Man, K. F.

1995-01-01

Gaseous contaminants such as oxygen, water vapor, nitrogen and hydrocarbons are often present in the processing environment in semiconductor device fabrication and in containerless materials processing. The contaminants arise as a result of outgassing from hot surfaces or they may be part of the impurities in commercial ultra-high purity gases. Among these gaseous contaminants, oxygen is the most reactive and, therefore, has the most adverse effects on the end product. There has been an intense effort at the Jet Propulsion Laboratory to develop different types of oxygen sorbents to reduce oxygen concentration in a microgravity processing environment to sub-ppb (parts-per-billion) levels. Higher concentrations can lead to rapid surface oxide formation, hence reducing the quality of semiconductor devices. If the concentration of oxygen in a processing chamber at 1000oC is in the ppb level, it will only take approximately 10 seconds for an oxide layer to form on the surface of a sample. The interaction of oxygen with the water surface can lead to the formation of localized defects in semi-conductor devices, hence decreasing the manufacturing yield. For example, efficient production of 64 Mb RAM chips requires contaminations below ppb levels. This paper describes a technique for measuring trace quantities of oxygen contaminants by recording the monoatomic negative ions, O-, using mass spectrometry. The O- formation from the e--O2 interaction utilizes the electron dissociative attachment method that is greatly enhanced at the resonant energy (6.8 eV). The device combines a small gridded electron ionizer with a compact mass spectrometer. The concentrations of oxygen have been measured using the method of standard additions by diluting O2 in N2. The lowest detection limit obtained was 1.2 kHz (O- count rate) at a concentration of 10-10, corresponding to 0.1 ppb.

Microgravity experiments on the effect of internal flow on solidification of Fe-Cr-Ni stainless steels.

PubMed

Hanlon, Alaina B; Matson, Douglas M; Hyers, Robert W

2006-09-01

A new hypothesis has been developed to explain the effect of internal fluid flow on the lifetime of a metastable phase in solidifying Fe-Cr-Ni alloys. The hypothesis shows excellent agreement with available experimental results, but microgravity experiments are required for complete validation. Certain Fe-Cr-Ni stainless steel alloys solidify from an undercooled melt by a two-step process in which the metastable ferrite phase forms first followed by the stable austenite phase. Recent experiments using containerless processing techniques have shown that the lifetime of the metastable phase is strongly influenced by flow within the molten sample. Simulations using a commercial computational fluid dynamics (CFD) package, FIDAP, were performed to determine the time required for collision of dendrites and compared to experimental delay time. If the convective velocities are strong enough to bend the primary arms, then the secondary arms of adjacent dendrites can touch. The points of collision form low-angle boundaries and result in high-energy sites that can serve as nuclei for the transformation to the stable phase. It has been determined that the convective velocities in electrostatic levitation (ESL) are not strong enough to cause collision. However, in ground-based electromagnetic levitation (EML), the convective velocities are strong enough to cause the dendrites to deflect so that the secondary arms of adjacent dendrites collide. There is quantitative agreement between the numerically determined time to collision and the experimentally observed delay time in EML. The strong internal velocity due to convection within the EML samples is the reason for the observed difference in delay times between ESL and EML. Microgravity testing is essential because the significant change in nucleation behavior occurs between the ranges accessible by ground-based ESL and EML. Testing in microgravity using EML will permit a large range of internal convective velocities including those that are inaccessible in 1 g.

An extended laser flash technique for thermal diffusivity measurement of high-temperature materials

NASA Technical Reports Server (NTRS)

Shen, F.; Khodadadi, J. M.

1993-01-01

Knowledge of thermal diffusivity data for high-temperature materials (solids and liquids) is very important in analyzing a number of processes, among them solidification, crystal growth, and welding. However, reliable thermal diffusivity versus temperature data, particularly those for high-temperature liquids, are still far from complete. The main measurement difficulties are due to the presence of convection and the requirement for a container. Fortunately, the availability of levitation techniques has made it possible to solve the containment problem. Based on the feasibility of the levitation technology, a new laser flash technique which is applicable to both levitated liquid and solid samples is being developed. At this point, the analysis for solid samples is near completion and highlights of the technique are presented here. The levitated solid sample which is assumed to be a sphere is subjected to a very short burst of high power radiant energy. The temperature of the irradiated surface area is elevated and a transient heat transfer process takes place within the sample. This containerless process is a two-dimensional unsteady heat conduction problem. Due to the nonlinearity of the radiative plus convective boundary condition, an analytic solution cannot be obtained. Two options are available at this point. Firstly, the radiation boundary condition can be linearized, which then accommodates a closed-form analytic solution. Comparison of the analytic curves for the temperature rise at different points to the experimentally-measured values will then provide the thermal diffusivity values. Secondly, one may set up an inverse conduction problem whereby experimentally obtained surface temperature history is used as the boundary conditions. The thermal diffusivity can then be elevated by minimizing the difference between the real heat flux boundary condition (radiation plus convection) and the measurements. Status of an experimental study directed at measuring the thermal diffusivity of high-temperature solid samples of pure Nickel and Inconel 718 superalloys are presented. Preliminary measurements showing surface temperature histories are discussed.

Der Einfluss von Alitretinoin auf die Lebensqualität bei Patienten mit schwerem chronischen Handekzem: FUGETTA - Beobachtungsstudie unter Praxisbedingungen.

PubMed

Augustin, Matthias; Thaçi, Diamant; Kamps, Anja

2016-12-01

Alitretinoin ist die einzige zugelassene Behandlung für schweres chronisches Handekzem (CHE), das refraktär gegenüber potenten topischen Corticosteroiden ist. Bei dieser Studie (FUGETTA) wurde die Wirksamkeit von leitliniengerecht angewendetem oralem Alitretinoin sowie dessen Einfluss auf die Lebensqualität (LQ) bei Patienten mit schwerem refraktärem CHE beurteilt. Multizentrische, offene, nichtinterventionelle Beobachtungsstudie, durchgeführt in Deutschland. Die Patienten wurden nach Ermessen ihres behandelnden Arztes mit Alitretinoin 10 mg oder 30 mg einmal täglich über maximal 24 Wochen behandelt. Die Wirksamkeit wurde anhand des Physician Global Assessment (PGA) und des Dermatology Life Quality Index (DLQI) bewertet. Zudem wurden unerwünschte Ereignisse (UE) erfasst. Die Studienpopulation bestand aus 658 Patienten (30 mg: n = 581; 10 mg: n = 77). Bei Beobachtungsbeginn litten die meisten Patienten (83 %) gemäß PGA an einem schweren CHE. Bei Beobachtungsende war das Handekzem bei 48 % der Patienten gemäß PGA vollständig oder fast vollständig abgeheilt (30 mg: 49 %; 10 mg: 43 %). Die mittlere Verbesserung des DLQI-Scores in Woche 24 betrug 58 % (30 mg: mittlere [SD] Veränderung gegenüber dem Ausgangswert -10,4 [8,04]) und 70 % (10 mg: mittlere [SD] Veränderung gegenüber dem Ausgangswert -10,8 [7,29]). Die Gesamtinzidenz von NW war niedrig und in den beiden Gruppen ähnlich. Alitretinoin führte zu einer schnellen, deutlichen Verbesserung der LQ bei Patienten mit schwerem CHE. © 2016 Deutsche Dermatologische Gesellschaft (DDG). Published by John Wiley & Sons Ltd.

Retrospektive Analyse von Zufallsbefunden, die bei Patienten mit kutanem malignen Malignom durch (18) F-Fluordeoxyglucose-PET/CT erhoben wurden.

PubMed

Conrad, Franziska; Winkens, Thomas; Kaatz, Martin; Goetze, Steven; Freesmeyer, Martin

2016-08-01

Bei der (18) F-Fluordeoxyglucose-Positronenemissionstomographie/Computertomographie (FDG-PET/CT) ergeben sich häufig Zufallsbefunde. In der vorliegenden Studie konzentrierten wir uns auf mittels FDG-PET/CT erhaltene Zufallsbefunde bei Patienten mit kutanem Melanom und überprüften deren Relevanz hinsichtlich weiterer diagnostischer Maßnahmen und Interventionen. Die Krankenakten von 181 konsekutiven Melanom-Patienten wurden retrospektiv ausgewertet, um das Management von Zufallsbefunden zu dokumentieren. Der Schwerpunkt lag dabei auf den histologischen Befunden. Bei 33 von 181 (18 %) Patienten lagen 39 relevante Zufallsbefunde vor, und zwar im Kolorektalbereich (n = 15 Patienten), in der Schilddrüse (n = 8), der Prostata (n = 2), dem Bewegungsapparat (n = 2), in Lymphknoten (n = 2), der Parotis (n = 1), den Mandeln (n = 1), den Nieren (n = 1) und der Gallenblase (n = 1). Bei 25 Patienten schlossen sich weitere diagnostische Verfahren an, wobei in 21 Fällen ein klinisches Korrelat nachgewiesen wurde. Bei 16 von 21 Patienten ergab sich eine Neoplasie, darunter fünf maligne Läsionen (vier Kolonkarzinome und ein Prostatakarzinom). Die Malignome wurden frühzeitig diagnostiziert und in der Mehrzahl der Fälle erfolgreich entfernt. Der Einsatz der FDG-PET/CT als Routine-Diagnostik wird in den Leitlinien empfohlen und ist indiziert bei malignem Melanom ab Stadium IIC. In dieser Studie wurden auf effektive Weise ansonsten nicht erkannte Krebserkrankungen, insbesondere Kolonkarzinome, detektiert. In den meisten Fällen war eine frühe Intervention möglich. Zufallsbefunde durch FDG-PET/CT sollten, unter Berücksichtigung des Zustands und der Wünsche des Patienten, mit den geeigneten diagnostischen Maßnahmen abgeklärt werden. © 2016 Deutsche Dermatologische Gesellschaft (DDG). Published by John Wiley & Sons Ltd.

Smartes System für die Energiewende - der Übertragungsnetzbetreiber in der digitalen Zukunft

NASA Astrophysics Data System (ADS)

Pflaum, Rainer; Egeler, Tobias

Die Übertragungsnetze stellen eine zuverlässige Versorgung von Haushalt, Gewerbe und Industrie mit elektrischer Energie sicher und sind damit Grundlage einer modernen Wirtschaft und Gesellschaft. Die mittlerweile unumkehrbaren Entwicklungen der nationalen und europäischen Energiewende stellen den Übertragungsnetzbetreiber in seinen Kernaufgaben, dem Bau und Betrieb von Netzen, dem Markt- und Netzzugang und der Integration der erneuerbaren Energien vor neue und große Herausforderungen. Verbrauchsnahe dezentrale Erzeugung wie verbrauchsferne zentrale Erzeugung muss im Sinne der Gewährleistung der Systemstabilität gemanagt und in Einklang mit dem Verbrauch gebracht werden. Erneuerbare Energien müssen zudem in einem solchen System ihren Beitrag zur System- und Marktintegration leisten. All das erfordert mehr Daten, um in einem Gesamtsystem dynamische Reaktionsmöglichkeiten gewährleisten zu können. Erst die "Digitalisierung" schafft dabei die notwendigen Voraussetzungen die Komplexität zu stemmen. Die Digitalisierung stellt daher ein Kernelement dieses Wandels des Übertragungsnetzbetreibers dar, die einerseits mit zum Entstehen der neuen Herausforderungen beiträgt, andererseits aber auch hilft Werkzeuge bereitzustellen, diesen Herausforderungen zu begegnen. Im folgenden Beitrag wird aufgezeigt, wie die Digitalisierung die Aufgaben und Instrumente des Übertragungsnetzbetreibers verändern. Ausgehend von den heutigen Aufgaben eines Übertragungsnetzbetreibers und dem gültigen Rechtsrahmen werden unter dem Begriff "Notwendiges Set für morgen" smarte Elemente und Werkzeuge beschrieben, die bereits heute im Einsatz sind oder in den nächsten Jahren notwendig werden. Im Anschluss erfolgt anhand einiger Beispiele aus unterschiedlichen Bereichen eine Konkretisierung der Einsatzzwecke der Digitalisierung beim Übertragungsnetzbetreiber. Ein kurzer Ausblick mit Fokus auf den weiteren Veränderungsprozess rundet den Beitrag ab.

Factors determining growth and vertical distribution of planktonic algae in extremely acidic mining lakes (pH 2.7)

NASA Astrophysics Data System (ADS)

Bissinger, Vera

2003-04-01

In this thesis, I investigated the factors influencing the growth and vertical distribution of planktonic algae in extremely acidic mining lakes (pH 2-3). In the focal study site, Lake 111 (pH 2.7; Lusatia, Germany), the chrysophyte, Ochromonas sp., dominates in the upper water strata and the chlorophyte, Chlamydomonas sp., in the deeper strata, forming a pronounced deep chlorophyll maximum (DCM). Inorganic carbon (IC) limitation influenced the phototrophic growth of Chlamydomonas sp. in the upper water strata. Conversely, in deeper strata, light limited its phototrophic growth. When compared with published data for algae from neutral lakes, Chlamydomonas sp. from Lake 111 exhibited a lower maximum growth rate, an enhanced compensation point and higher dark respiration rates, suggesting higher metabolic costs due to the extreme physico-chemical conditions. The photosynthetic performance of Chlamydomonas sp. decreased in high-light-adapted cells when IC limited. In addition, the minimal phosphorus (P) cell quota was suggestive of a higher P requirement under IC limitation. Subsequently, it was shown that Chlamydomonas sp. was a mixotroph, able to enhance its growth rate by taking up dissolved organic carbon (DOC) via osmotrophy. Therefore, it could survive in deeper water strata where DOC concentrations were higher and light limited. However, neither IC limitation, P availability nor in situ DOC concentrations (bottom-up control) could fully explain the vertical distribution of Chlamydomonas sp. in Lake 111. Conversely, when a novel approach was adopted, the grazing influence of the phagotrophic phototroph, Ochromonas sp., was found to exert top-down control on its prey (Chlamydomonas sp.) reducing prey abundance in the upper water strata. This, coupled with the fact that Chlamydomonas sp. uses DOC for growth, leads to a pronounced accumulation of Chlamydomonas sp. cells at depth; an apparent DCM. Therefore, grazing appears to be the main factor influencing the vertical distribution of algae observed in Lake 111. The knowledge gained from this thesis provides information essential for predicting the effect of strategies to neutralize the acidic mining lakes on the food-web. Die vorliegende Dissertation beschäftigt sich mit den Faktoren, die das Wachstum und die Vertikalverteilung von Planktonalgen in extrem sauren Tagebaurestseen (TBS; pH 2-3) beeinflussen. Im exemplarisch untersuchten TBS 111 (pH 2.7; Lausitzer Revier) dominiert die Goldalge Ochromonas sp. in oberen und die Grünalge Chlamydomonas sp. in tieferen Wasserschichten, wobei letztere ein ausgeprägtes Tiefenchlorophyll-Maximum (DCM) ausbildet. Es wurde ein deutlicher Einfluss von Limitation durch anorganischen Kohlenstoff (IC) auf das phototrophe Wachstum von Chlamydomonas sp. in oberen Wasserschichten nachgewiesen, die mit zunehmender Tiefe von Lichtlimitation abgelöst wird. Im Vergleich mit Arbeiten aus neutralen Seen zeigte Chlamydomonas sp. erniedrigte maximale Wachstumsraten, einen gesteigerten Kompensationspunkt und erhöhte Dunkelrespirationsraten, was auf gesteigerte metabolische Kosten unter den extremen physikalisch-chemischen Bedingungen hinweist. Die Photosyntheseleistungen von Chlamydomonas sp. waren in Starklicht-adaptierten Zellen durch IC-Limitation deutlich verringert. Außerdem ergaben die ermittelten minimalen Zellquoten für Phosphor (P) einen erhöhten P-Bedarf unter IC-Limitation. Anschließend konnte gezeigt werden, dass Chlamydomonas sp. ein mixotropher Organismus ist, der seine Wachstumsraten über die osmotrophe Aufnahme gelösten organischen Kohlenstoffs (DOC) erhöhen kann. Dadurch ist dieser Organismus fähig, in tieferen, Licht-limitierten Wasserschichten zu überleben, die einen höheren DOC-Gehalt aufweisen. Da die Vertikalverteilung der Algen im TBS 111 jedoch weder durch IC-Limitation, P-Verfügbarkeit noch die in situ DOC-Konzentrationen abschließend erklärt werden konnte (bottom-up Kontrolle), wurde eine neue Theorie zur Entstehung der Vertikalverteilung geprüft. Grazing der phagotrophen und phototrophen Alge Ochromonas sp. auf der phototrophen Alge Chlamydomonas sp. erwies sich als herausragender Faktor, der über top-down Kontrolle die Abundanz der Beute in höheren Wasserschichten beeinflussen kann. Gemeinsam mit der Tatsache, dass Chlamydomonas sp. DOC zur Wachstumssteigerung verwendet, führt dies zu einer Akkumulation von Chlamydomonas sp. in der Tiefe, ausgeprägt als DCM. Daher erscheint grazing als der Hauptfaktor, der die beobachtete Vertikalschichtung der Algen im TBS 111 hervorruft. Die erzielten Ergebnisse liefern grundlegende Informationen, um die Auswirkungen von Strategien zur Neutralisierung der TBS auf das Nahrungsnetz abschätzen zu können.

Versuche zur Gewinnung von katalytischen Antikörpern zur Hydrolyse von Arylcarbamaten und Arylharnstoffen. (English Title: Attempts to produce catalytic antibodies for hydrolysis of arylcarbamates and arylureas)

NASA Astrophysics Data System (ADS)

Werner, Deljana

2002-05-01

Im Rahmen dieser Arbeit gelang es, katalytische Antikörper zur Hydrolyse von Benzylphenylcarbamaten sowie zahlreiche monoklonale Antikörper gegen Haptene herzustellen. Es wurden verschiedene Hapten-Protein-Konjugate unter Verwendung unterschiedlicher Kopplungsmethoden hergestellt und charakterisiert. Zur Generierung der hydrolytisch aktiven Antikörper wurden Inzuchtmäuse mit KLH-Konjugaten von 4 Übergangszustandsanaloga (ÜZA) immunisiert. Mit Hilfe der Hybridomtechnik wurden verschiedene monoklonale Antikörper gegen diese ÜZA gewonnen. Dabei wurden sowohl verschiedene Immunisierungsschemata als auch verschiedene Inzuchtmausstämme und Fusionstechniken verwendet. Insgesamt wurden 32 monoklonale Antikörper gegen die verwendeten ÜZA selektiert. Diese Antikörper wurden in groen Mengen hergestellt und gereinigt. Zum Nachweis der Antikörper-vermittelten Katalyse wurden verschiedene Methoden entwickelt und eingesetzt, darunter immunologische Nachweismethoden mit Anti-Substrat- und Anti-Produkt-Antikörpern und eine photometrische Methode mit Dimethylaminozimtaldehyd. Der Nachweis der hydrolytischen Aktivität gelang mit Hilfe eines Enzymsensors, basierend auf immobilisierter Tyrosinase. Die Antikörper N1-BC1-D11, N1-FA7-C4, N1-FA7-D12 und R3-LG2-F9 hydrolysierten die Benzylphenylcarbamate POCc18, POCc19 und Substanz 27. Der Nachweis der hydrolytischen Aktivität dieser Antikörper gelang auch mit Hilfe der HPLC. Der katalytische Antikörper N1-BC1-D11 wurde kinetisch und thermodynamisch untersucht. Es wurde eine Michaelis-Menten-Kinetik mit Km von 210 µM, vmax von 3 mM/min und kcat von 222 min-1 beobachtet. Diese Werte korrelieren mit den Werten der wenigen bekannten Diphenylcarbamat-spaltenden Abzyme. Die Beschleunigungsrate des Antikörpers N1-BC1-D11 betrug 10. Das ÜZA Hei3 hemmte die hydrolytische Aktivität. Dies beweist, dass die Hydrolyse in der Antigenbindungsstelle stattfindet. Weiter wurde zwischen der Antikörperkonzentration und der Umsatzgeschwindigkeit eine lineare Abhängigkeit festgestellt. Die thermodynamische Gleichtgewichtsdissoziationskonstante KD des Abzyms von 2,6 nM zeugt von einer sehr guten Affinität zum ÜZA. Hydrolytisch aktiv waren nur Antikörper, die gegen das Übergangszustandsanalogon Hei3 hergestellt worden waren. Es wird vermutet, dass die Hydrolyse der Benzylphenylcarbamate über einen Additions-Eliminierungsmechanismus unter Ausbildung eines tetraedrischen Übergangszustandes verläuft, dessen analoge Verbindung Hei3 ist. Im Rahmen der Generierung von Nachweisantikörpern zur Detektion der Substratabnahme bei der Hydrolyse wurden Anti-Diuron-Antikörper hergestellt. Einer der Antikörper (B91-CG5) ist spezifisch für das Herbizid Diuron und hat einen IC50-Wert von 0,19 µg/l und eine untere Nachweisgrenze von 0,04 µg/l. Ein anderer Antikörper (B91-KF5) reagiert kreuz mit einer Palette ähnlicher Herbizide. Mit diesen Antikörpern wurde ein empfindlicher Labortest, der ein Monitoring von Diuron auf Grundlage des durch die Trinkwasserverordnung festgeschriebenen Wertes für Pflanzenschutzmittel von 0,1 µg/l erlaubt, aufgebaut. Der Effekt der Anti-Diuron-Antikörper auf die Diuron-inhibierte Photosynthese wurde in vitro und in vivo untersucht. Es wurde nachgewiesen, dass sowohl in isolierten Thylakoiden, als auch in intakten Algen eine Vorinkubation der Anti-Diuron-Antikörper mit Diuron zur Inaktivierung seiner Photosynthese-hemmenden Wirkung führt. Wurde der Elektronentransport in den isolierten Thylakoiden oder in Algen durch Diuron unterbrochen, so führte die Zugabe der Anti-Diuron-Antikörper zur Reaktivierung der Elektronenübertragung. Attempts to produce catalytic antibodies for hydrolysis of arylcarbamates and arylureas: The aim of the investigations was to produce antibodies which are able to cleave herbicides resistant to naturally occuring enzymes. Structurally similar carbamate and urea derivatives were chosen for the experiments. Phosphonate derivatives were synthesized that mimick possible transition state analogues in structure and charge. Mice were immunized with 4 different derivatives after conjugating them to carrier proteins. 32 hybridomas were established that produce monoclonal antibodies binding to these derivatives. The possible cleavage of substrates was determined by immunoassays with monoclonal antibodies against the substrate and the products and with a photometric method based on dimethylaminocinammonaldehyde. The measuring of cleavage products was succeeded by an amperometric method. The enzyme sensor was based on immobilized tyrosinase which oxidizes p-chlorophenol and phenol. The antibodies N1-BC1-D11, N1-FA7-C4, N1-FA7-D12 und R3-LG2-F9 hydrolysed the benzylphenylcarbamates POCc18, POCc19 und Substance 27. The hydrolytic activity of these antibodies was also succeeded with HPLC. The catalytic antibody N1-BC1-D11 was investigated kinetically and thermodynamically. A Michaelis-Menten-Kinetic was observed (at pH 8.0 exhibited a Km 210 µM, a vmax 3 mM/min and a kcat 222 min-1). These values are in the range of the values obtained for the antibody-catalysed hydrolysis of diphenylcarbamates. The rate enhancement of N1-BC1 was 10. The reaction was completely inhibited by stoichiometric quantities of the transition state analogue Hei3. This is consistent with the affinity of the abzyme to Hei3 of 2.6 nM, determined by BIAcore assay. Only antibodies generated against Hei3 showed hydrolytic activity. The hydrolysis of benzylphenylcarbamates presumably occurs via an addition-elimination-Mechanism involving a tetrahedral intermediate. In summary, this work presents the first example of antibody-catalysed hydrolysis of benzylphenylcarbamates. Monoclonal anti-diuron antibodies were generated that bind to the herbicide diuron with an extremely low equilibrium dissociation constant. A sensitive immunoassay with a low detection limit of 0.2 nM for diuron was established. This is the most sensitive immunological method for detection of diuron known so far. These antibodies were also used in vitro and in vivo to prevent diuron-dependent inhibition of photosynthesis or to restore photosynthesis after inhibition. In isolated thylakoids prepared from spinach leaves (Spinacia oleracea L.) the diuron-inhibited Hill reaction was reconstituted immediately following the addition of the monoclonal antibodies. In an in vivo approach the photosynthetic oxygen evolution of the cell wall deficient mutant (cw 15) of the green alga Chlamydomonas reinhardtii Dangeard was monitored. The antibodies prevented the diuron-dependent inhibition of photosynthesis and restored photosynthesis after inhibition. Transgenic plants that synthesize and accumulate these antibodies or antibody fragments and are therefore diuron-resistant can be created.

Monte Carlo Simulation of Nanoparticle Encapsulation in Flames

NASA Technical Reports Server (NTRS)

Sun, Z.; Huertas, J. I.; Axelbaum, R. L.

1999-01-01

Gas-phase combustion (flame) synthesis has been an essential industrial process for producing large quantities of powder materials such as carbon black, titanium dioxide, and silicon dioxide. Flames typically produce simple oxides, with carbon black being the noted exception because the oxides of carbon are gaseous and are easily separated from the particulate matter that is formed during fuel pyrolysis. Furthermore, the powders produced in flames are usually agglomerated, nanometer-sized particles (nanoparticles). This composition and morphology is acceptable for many applications. However, the present interest in nanoparticles for advanced materials application has led to efforts to employ flames for the synthesis of unagglomerated nanoparticles (2 to 100 nm) of metals and non-oxide ceramics. Sodium-halide chemistry has proven to be viable for producing metals and non-oxide ceramics in flames. Materials that have been produced to date include Si (Calcote and Felder, 1993), TiN, TiB2, TiC, TiSi2, SiC, B4C (Glassman et al, 1993) Al, W, Ti, TiB2, AlN, and W-Ti and Al-AlN composites (DuFaux and Axelbaum, 1995, Axelbaum et al 1996,1997). Many more materials are possible. The main challenge that faces application of flame synthesis for advanced materials is overcoming formation of agglomerates in flames (Brezinsky, 1997). The high temperatures and high number densities in the flame environment favor the formation of agglomerates. Agglomerates must be avoided for many reasons. For example, when nanopowders are consolidated, agglomerates have a deleterious effect on compaction density, leading to voids in the final part. Efforts to avoid agglomeration in flames without substantially reducing particle number density and, consequently, production rate, have had limited success. Another critical challenge that faces all synthesis routes for nanopowders is ensuring that the powders are high purity and that the process is scaleable. Though the containerless, high temperature environment of a flame is excellent for producing high-purity simple compounds, ultrafine metals and non-oxide ceramic powders are inherently reactive in the presence of oxygen and/or moisture. Thus, the handling of these powders after synthesis poses a challenging problem. Impurities acquired during handling of nanoparticles have plagued the advancement of nanostructured materials technology.

Experiments on Nucleation in Different Flow Regimes

NASA Technical Reports Server (NTRS)

Bayuzick, Robert J.

1999-01-01

The vast majority of metallic engineering materials are solidified from the liquid phase. Understanding the solidification process is essential to control microstructure, which in turn, determines the properties of materials. The genesis of solidification is nucleation, where the first stable solid forms from the liquid phase. Nucleation kinetics determine the degree of undercooling and phase selection. As such, it is important to understand nucleation phenomena in order to control solidification or glass formation in metals and alloys. Early experiments in nucleation kinetics were accomplished by droplet dispersion methods [1-6]. Dilitometry was used by Turnbull and others, and more recently differential thermal analysis and differential scanning calorimetry have been used for kinetic studies. These techniques have enjoyed success; however, there are difficulties with these experiments. Since materials are dispersed in a medium, the character of the emulsion/metal interface affects the nucleation behavior. Statistics are derived from the large number of particles observed in a single experiment, but dispersions have a finite size distribution which adds to the uncertainty of the kinetic determinations. Even though temperature can be controlled quite well before the onset of nucleation, the release of the latent heat of fusion during nucleation of particles complicates the assumption of isothermality during these experiments. Containerless processing has enabled another approach to the study of nucleation kinetics [7]. With levitation techniques it is possible to undercool one sample to nucleation repeatedly in a controlled manner, such that the statistics of the nucleation process can be derived from multiple experiments on a single sample. The authors have fully developed the analysis of nucleation experiments on single samples following the suggestions of Skripov [8]. The advantage of these experiments is that the samples are directly observable. The nucleation temperature can be measured by noncontact optical pyrometry, the mass of the sample is known, and post processing analysis can be conducted on the sample. The disadvantages are that temperature measurement must have exceptionally high precision, and it is not possible to isolate specific heterogeneous sites as in droplet dispersions.

Levitation Technology in International Space Station Research

NASA Technical Reports Server (NTRS)

Guinart-Ramirez, Y.; Cooley, V. M.; Love, J. E.

2016-01-01

The International Space Station (ISS) is a unique multidisciplinary orbiting laboratory for science and technology research, enabling discoveries that benefit life on Earth and exploration of the universe. ISS facilities for containerless sample processing in Materials Science experiments include levitation devices with specimen positioning control while reducing containment vessel contamination. For example, ESA's EML (ElectroMagnetic Levitator), is used for melting and solidification of conductive metals, alloys, or semiconductors in ultra-high vacuum, or in high-purity gaseous atmospheres. Sample heating and positioning are accomplished through electromagnetic fields generated by a coil system. EML applications cover investigation of solidification and microstructural formation, evaluation of thermophysical properties of highly reactive metals (whose properties can be very sensitive to contamination), and examination of undercooled liquid metals to understand metastable phase convection and influence convection on structural changes. MSL utilization includes development of novel light-weight, high-performance materials. Another facility, JAXA's ELF (Electrostatic Levitation Furnace), is used to perform high temperature melting while avoiding chemical reactions with crucibles by levitating a sample through Coulomb force. ELF is capable of measuring density, surface tension, and viscosity of samples at high temperatures. One of the initial ELF investigations, Interfacial Energy-1, is aimed at clarification of interfacial phenomena between molten steels and oxide melts with industrial applications in control processes for liquid mixing. In addition to these Materials Science facilities, other ISS investigations that involve levitation employ it for biological research. For example, NASA's "Magnetic 3D Culturing and Bioprinting" investigation uses magnetic levitation for three-dimensional culturing and positioning of magnetized cells to generate spheroid assemblies for biomedical applications. Levitation is also used as a modeled microgravity ground analog in the NASA OsteoOmics ISS investigation, which tests whether magnetic levitation accurately simulates microgravity conditions by studying gravitational regulation of osteoblast and osteoclast genomics and metabolism. Elucidating the cellular mechanisms of bone loss in microgravity contributes to the understanding of bone loss in medical disorders on Earth, which may lead to development of preventive or therapeutic countermeasures. Thus, the ISS state-of-the-art laboratory offers various levitation capability platforms with applications for innovative research in Materials and Life Sciences disciplines, with benefits for humanity.

Small molecules as tracers in atmospheric secondary organic aerosol

NASA Astrophysics Data System (ADS)

Yu, Ge

Secondary organic aerosol (SOA), formed from in-air oxidation of volatile organic compounds, greatly affects human health and climate. Although substantial research has been devoted to SOA formation and evolution, the modeled and lab-generated SOA are still low in mass and degree of oxidation compared to ambient measurements. In order to compensate for these discrepancies, the aqueous processing pathway has been brought to attention. The atmospheric waters serve as aqueous reaction media for dissolved organics to undergo further oxidation, oligomerization, or other functionalization reactions, which decreases the vapor pressure while increasing the oxidation state of carbon atoms. Field evidence for aqueous processing requires the identification of tracer products such as organosulfates. We synthesized the standards for two organosulfates, glycolic acid sulfate and lactic acid sulfate, in order to measure their aerosol-state concentration from five distinct locations via filter samples. The water-extracted filter samples were analyzed by LC-MS. Lactic acid sulfate and glycolic acid sulfate were detected in urban locations in the United States, Mexico City, and Pakistan with varied concentrations, indicating their potential as tracers. We studied the aqueous processing reaction between glyoxal and nitrogen-containing species such as ammonium and amines exclusively by NMR spectrometry. The reaction products formic acid and several imidazoles along with the quantified kinetics were reported. The brown carbon generated from these reactions were quantified optically by UV-Vis spectroscopy. The organic-phase reaction between oxygen molecule and alkenes photosensitized by alpha-dicarbonyls were studied in the same manner. We observed the fast kinetics transferring alkenes to epoxides under simulated sunlight. Statistical estimations indicate a very effective conversion of aerosol-phase alkenes to epoxides, potentially forming organosulfates in a deliquescence event and increasing aerosol mass. Finally, we built a containerless apparatus to study aqueous processing reactions using an acoustic levitator paired with a mass spectrometer. The levitator is capable of trapping droplets with the size of 80-500 mum in diameter for over eight hours. The apparatus is also capable of drying and wetting the droplet in a controllable manner. We performed am example reaction between glyoxal and ammonium sulfate using this instrument, and showed that it could qualitatively monitor aqueous processing reactions.

[Postoperative adjuvante Therapie mit einem Mistelextrakt (Viscum album ssp. album) bei Hündinnen mit Mammatumoren].

PubMed

Biegel, Ulrike; Stratmann, Nina; Knauf, Yvonne; Ruess, Katja; Reif, Marcus; Wehrend, Axel

2017-01-01

Hintergrund: Canine Mammatumoren (CMT) sind wegen ihrer Häufigkeit und hohen Malignitätsrate eine Herausforderung für die Veterinärmedizin. Bisher ist noch keine postoperative adjuvante Therapie als wirksamer Standard etabliert und in den nächsten Jahren wohl auch nicht zu erwarten. Zusätzlich ist die Frage nach der Verträglichkeit einer adjuvanten Therapie mit Erhaltung oder Verbesserung der Lebensqualität (LQ) wichtig. Die Therapie mit Mistelextrakten (Viscum album L.; VAE) ist in der Humanonkologie nach adjuvanter Tumorbasistherapie (Chemotherapie und Bestrahlung) eine sehr häufig verwendete, zusätzliche adjuvante Behandlungsmethode. Auch bei verschiedenen Tierarten werden inzwischen Mistelpräparate in der Onkologie erfolgreich angewendet. Methoden: Überprüfung von Wirkung und Nutzen einer postoperativen, adjuvanten Misteltherapie beim CMT sowie Erfassung der LQ unter der VAE-Behandlung. Ausgewertet wurden 56 Hündinnen mit Mammaadenokarzinom, 33 ausschließlich operierte Kontrolltiere und 23 operierte Tiere, die adjuvant VAE erhielten. Ergebnisse: Die mediane Überlebenszeit (MST) aller Tiere (n = 56) betrug 32 Monate (Interquartilbereich 13-51 Monate). Im deskriptiven Vergleich der Überlebenszeiten (ST) nach Kaplan-Meier waren nach 12, 24, 36 bzw. 48 Monaten noch 24, 20, 15 bzw. 5 Hündinnen (entsprechend 72,7%, 60,6%, 45,1%, 12,4%) der Kontrollgruppe sowie 19, 14, 11 und 1 Hündin (82,6%, 60,9%, 47,8%, 4,3%) der VAE-Gruppe am Leben. Die VAE-Therapie führte zu einem geringeren Gesamtversterberisiko, das statistisch nicht signifikant war (Hazard Ratio (HR) 0,530, 95%-Konfidenzintervall (KI) 0,222-1,262; p = 0,15). Tendenziell (p = 0,07) zeigte sich eine Verringerung des tumorbedingten Sterberisikos auf 25% (HR 0,251, 95%-KI 0,056-1,122). Schlussfolgerungen: Es kann eine Tendenz zur Senkung des tumorbedingten Sterberisikos der VAE-Gruppe bei guter Verträglichkeit der Therapie angenommen werden. Die LQ der Tiere blieb über die gesamte Beobachtungszeit auf hohem Niveau stabil. © 2017 S. Karger GmbH, Freiburg.

Oberflächenstrukturierung metallischer Werkstoffe, z. B. für stents

NASA Astrophysics Data System (ADS)

Stöver, Michael; Wintermantel, Erich

Eine topologische Oberflächenmodifikation von metallischen Implantaten kann aus verschiedenen Gründen sinnvoll sein. Im Allgemeinen lassen sich zwei Hauptziele unterscheiden. Zum einen dienen Oberflächen dazu, bestimmte Zellreaktionen zu forcieren. Die Anwendungsbeispiele reichen hier von sehr rauen Oberflächen in Fällen wo eine gute Integration eines Permanentimplantates in das Gewebe erwünscht ist bis hin zu glatt polierten Oberflächen. Letztere werden in erster Linie dort eingesetzt, wo das Implantat in direktem Kontakt mit Blut ist. Ein Beispiel für die Erforderlichkeit einer hohen Rauheit (Rz > 100 μm) sind meist aus Titan gefertigte Schäfte von Gelenksimplantaten [1,2]. Die Autoren machten den Vorschlag, die Aufrauung von Titan- und Edelstahl-Stents analog der Aufrauung bei Hüftprothesenschäften zu versuchen, um eine noch bessere Biokompatibilität zu erreichen. [7, 8 ,9]. Sehr glatte Oberflächen, in der Regel mit Rz Werten von unter 0,1 μm, sind z. B. bei Herzklappenprothesen und der Innenseite von Gefäßstützen gefordert. Mittlere Rauheiten werden oft bei temporären Implantaten eingesetzt, in die in reguliertem Maße Gewebe einwachsen, allerdings keine unlösbare Verbindung bilden sollen. Sehr genau eingestellt werden müssen auch die Oberflächentopographien bei Implantaten in sehr empfindlichen Gebieten wie z. B. der Gehirnregion. Hierbei muss eine gute Verankerung im Gewebe vorhanden sein, um ein Verrutschen des Implantates zu verhindern. Zum anderen darf keine überschüssige Zellproliferation entstehen, um ein Einwachsen in sensible Regionen zu verhindern. Zum anderen werden Oberflächenmikrostrukturen genutzt, um Wirkstoffe in Implantate einzubringen, die lokal über einen bestimmten Zeitraum freigesetzt werden sollen. Als wichtigste Wirkstoffe sind hier Antibiotika und entzündungshemmende Mittel sowie im kardiovaskulären Bereich Proliferationshemmer zu nennen.

Antibakterielle In-vitro-Wirksamkeit ätherischer Öle gegen veterinärmedizinisch relevante Keime klinischer Isolate von Hunden, Katzen und Pferden.

PubMed

Bismarck, Doris; Schneider, Marianne; Müller, Elisabeth

Einleitung: Ätherische Öle sind die Grundlage der Aromatherapie. Unter anderem wird ihnen eine antibakterielle Wirkung zugeschrieben. In dieser Studie sollte die In-vitro-Wirksamkeit ätherischer Öle gegen ein breites Spektrum veterinärmedizinisch relevanter Erreger getestet werden. Methoden: Die antibakterielle Aktivität von 16 ätherischen Ölen wurde mittels Agardiffusionstest bestimmt. Getestet wurden grampositive und gramnegative Erreger, die aus klinischen Isolaten von Hunden, Katzen und Pferden aus der veterinärmedizinischen Routinediagnostik stammten. Die Einteilung der Wirksamkeit in nicht, gering-, mittel- und hochgradig wirksam erfolgte anhand der Größe der Hemmhofradien des Bakterienwachstums. Ergebnisse: Generell zeigten sich sowohl grampositive als auch gramnegative Erreger empfindlich gegen einige der getesteten ätherischen Öle. Nicht nur gegen Staphylokokken, sondern auch gegen Methicillin-resistente Stämme der Staphylokokken wiesen die ätherischen Öle in vitro eine nicht zu vernachlässigende Wirkung auf. Pasteurella multocida stellte sich als eher sensibler Keim heraus, während Pseudomonas aeruginosa als vollkommen resistenter Keim eine Ausnahme bildete. Teebaum-, Oregano-, und Bergbohnenkrautöl waren die potentesten Öle. Zusätzlich zeigten sich bei den grampositiven Erregern Lemongrasöl und bei den gramnegativen Erregern Thymianöl als gut wirksam. Schlussfolgerung: Ätherische Öle verfügen in vitro über eine antibakterielle Aktivität gegen klinische Isolate von Hunden, Katzen und Pferden. Diese Studie bietet eine Grundlage für die Anwendung ätherischer Öle in der Veterinärmedizin. Es zeichneten sich Tendenzen im Wirkspektrum einzelner ätherischer Öle bzw. im Grad der Wirksamkeit ätherischer Öle hinsichtlich einzelner Erregerspezies ab, allerdings lässt sich keine sichere Vorhersage über ihre Wirksamkeit gegen einen spezifischen Keim eines individuellen Patienten treffen. Deswegen sollte vor einer Therapie mit ätherischen Ölen deren individuelle Wirksamkeit mittels Aromatogramm getestet werden. © 2017 The Author(s). Published by S. Karger GmbH, Freiburg.

Biologie statt Philosophie? Evolutionäre Kulturerklärungen und ihre Grenzen

NASA Astrophysics Data System (ADS)

Illies, Christian

Vor über siebzig Jahren fand man in einer Höhle nahe Hohlenstein-Stadel, im heutigen Baden-Württemberg, eine Frau, die keiner bekannten Spezies und nicht einmal eindeutig den Hominiden zugeordnet werden konnte. Wegen ihres Aussehens wurde sie schon bald als "Löwenfrau“ bekannt (unterdessen wird sie als "Löwenmensch“ bezeichnet, da die in solchen Fragen Klarheit schaffenden Geschlechtsteile bei der Figur fehlen und in Zeiten von gender mainstreaming derartige Festlegungen gerne vermieden werden), denn sie hatte eine menschlich-aufrechte, unbehaarte Gestalt mit weiblichen Rundungen, aber zugleich eine Mähne, sowie Augen, Ohren und Schnauze eines Löwen. Eine sehr weitläufige Verwandte des Minotaurus, so schien es, und doch wesentlich älter als alle Bewohner des Olymps, denn vermutlich wurde die knapp 30 cm große Skulptur bereits in der Altsteinzeit vor etwa 32.000 Jahren aus Mammut-Elfenbein geschnitzt. Wir wissen nicht, ob sie kultischen Zwecken diente oder ein Kind mit ihr spielte, ob sie als Glücksbringer für die Jagd oder als Schamanin mit Löwenmaske verehrt und gefürchtet wurde. Aber die Löwenfrau legt nahe, dass der Mensch schon im Morgendämmern seiner Kultur über die eigene Nähe, aber auch Distanz zum Tier nachgedacht haben muss. Die Frage nach der menschlichen Selbstverortung begegnet uns in dieser Figur, und sie bestimmt viele Zeugnisse menschlichen Nachdenkens, welche uns die Altertumswissenschaften vorlegen. Mit dem Begriff "animal rationale“, wie er unter Bezug auf Aristoteles geprägt wurde, findet sie schließlich ihre klassische, für das Abendland lange Zeit maßgebliche Antwort: Der Mensch als Tier, dessen spezifisches Merkmal die Vernunftbegabtheit ist, die ihn zugleich von allen anderen Tieren abgrenzt und über sie stellt. Aber wo genau verläuft die Grenze? Und wie kann der Mensch beides zugleich sein? Die aristotelische Definition beantwortet diese Fragen nach der Doppelnatur nicht, sondern erhebt das offene Rätsel gleichsam zur Wesensbestimmung des Menschen.

Orienting Ocean Bottom Seismic Sensors from Ship Noise Polarization Analysis

NASA Astrophysics Data System (ADS)

Barruol, Guilhem; Dreo, Richard; Fontaine, Fabrice R.; Scholz, John R.; Sigloch, Karin; Geay, Bruno; Bouillon, Alexandre

2017-04-01

For the RHUM-RUM project (Réunion Hotspot and Upper Mantle - Réunions Unterer Mantel, www.rhum-rum.net), a network of 57 ocean-bottom seismometers (OBS) was installed on the ocean floor around La Réunion Island in the SW Indian Ocean. Part of the network happened to be located beneath a route of heavy ship traffic connecting SE-Asia and the South-Atlantic region. We analysed the ship noise recorded on the OBS and show that it can be used for determining the horizontal orientations of the seismic instruments as they were recording on the ocean floor. The OBS, provided by the German DEPAS and the French INSU OBS national pools, were equipped with wide-band or broad-band three-components seismic and hydro-acoustic sensors. They were deployed in Nov. 2012 by R/V Marion Dufresne and recovered by R/V Meteor one year later. Depending on the configuration, the OBS recorded for 8 to 13 months. By combining the trajectories of passing ships - provided by AIS (Automatic Identification system) GPS data - with our geophysical data recorded on the ocean floor, we show that both hydro-acoustic and seismic spectral analyses exhibit clear signals associated with vessels between 1 and 50 Hz, in the high-frequency range of our instruments. Large cargo vessels are detected several hours before and after their closest point of approach (CPA) and show clear Doppler effects which put quantitative constraints on their distances and speeds. By analysing the continuous noise polarization on the three seismic components, we show that the polarization of the noise emitted by ships passing in the neighbourhood of an ocean-bottom seismometer can be used for retrieving the orientation of the OBS horizontal components on the ocean floor with respect to the geographic reference frame. We find good agreement between OBS orientations thus calculated from ship noise and the OBS orientations determined independently from teleseismic body and surface wave polarization methods (Scholz et al., GJI, 2017).

Multifrequency tomography of the La Reunion mantle plume with P and S waves using ocean bottom seismometers in the Indian Ocean

NASA Astrophysics Data System (ADS)

Tsekhmistrenko, M.; Sigloch, K.; Hosseini, K.

2017-12-01

The RHUM-RUM experiment (Reunion Hotspot Upper Mantle - Reunions Unterer Mantel) investigates the presence or absence of a whole mantle plume beneath the volcanic hotspot island of La Reunion. From 2011 to 2016, RHUM-RUM instrumented a 2000 km x 2000 km area of western Indian Ocean seafloor, islands and Madagascar with broadband seismometers and hydrophones. The central component was a 13-month deployment of 57 German and French Ocean Bottom Seismometers (OBS) in 2300-5600 m depth. This was supplemented by 2-3 years deployments of 37 island stations on Reunion, Mauritius, Rodrigues, the southern Seychelles, the Iles Eparses and southern Madagascar. Two partner projects contributed another 30+ stations on Madagascar. We present results of multifrequency P- and S-waveform tomography of the entire mantle column beneath the Reunion hotspot. We use all frequency passbands that efficiently transmit body waves and rise above the considerable noise floor of OBS measurements. More than 200 teleseismic events during the 13-month long OBS deployment yielded usable measurements, and another 400 events before and after. We present our methods, discuss data yield and quality of ocean-bottom versus island/land seismometers and hydrophones. 150,000 combined cross-correlations measurements were used in multifrequency P-wave tomography, in passbands between 30 s and 2.7 s dominant period. Cross-correlation coefficients at permanent and temporal land stations are generally higher than on OBS, which are more affected by both microseismic and self-noise. Hydrophones worked more reliably, but strong reverberations from the water column mean that they are still less usable than seismograms. All measurements of the RHUM-RUM array are embedded in a global P-wave inversion. Mantle structures obtained from this new, high resolution tomographic model of the La Reunion area are compared to existing tomographies. We also compare to local and global convection models in order to understand the relation between mantle flow and the development of mantle plumes through time.

Finite frequency P-wave traveltime measurements on ocean bottom seismometers and hydrophones in the western Indian Ocean

NASA Astrophysics Data System (ADS)

Tsekhmistrenko, Maria; Sigloch, Karin; Hosseini, Kasra; Barruol, Guilhem

2016-04-01

From 2011 to 2014, the RHUM-RUM project (Reunion Hotspot Upper Mantle - Reunions Unterer Mantel) instrumented a 2000x2000km2 area of Indian Ocean seafloor, islands and Madagascar with broadband seismometers and hydrophones. The central component was a 13-month deployment of 57 German and French Ocean Bottom Seismometers (OBS) in 2300-5600 m depth. This was supplemented by 2-3 year deployments of 37 island stations on Reunion, Mauritius, Rodrigues, the southern Seychelles, the Iles Eparses and southern Madagascar. Two partner projects contributed another 30+ stations on Madagascar. Our ultimate objective is multifrequency waveform tomography of the entire mantle column beneath the Reunion hotspot. Ideally we would use all passbands that efficiently transmit body waves but this meets practical limits in the noise characteristics of ocean-bottom recordings in particular. Here we present the preliminary data set of frequency-dependent P-wave traveltime measurements on seismometers and hydrophones, obtained by cross-correlation of observed with predicted waveforms. The latter are synthesized from fully numerical Green's functions and carefully estimated, broadband source time functions. More than 200 teleseismic events during the 13-month long deployment yielded usable P-waveform measurements. We present our methods and discuss data yield and quality of ocean-bottom versus land seismometers, and of OBS versus broadband hydrophones. Above and below the microseismic noise band, data yields are higher than within it, especially for OBS. The 48 German OBS, equipped with Guralp 60 s sensors, were afflicted by relatively high self-noise compared to the 9 French instruments equipped with Nanometrics Trillium 240 s sensors. The HighTechInc (model HTI-01 and HTI-04-PCA/ULF) hydrophones (100 s corner period) functioned particularly reliably but their waveforms are relatively more challenging to model due to reverberations in the water column. We obtain ~15000 combined cross-correlations measurements that should be usable in multifrequency P-wave tomography, in passbands between 30 s and 2.7 s dominant period.

Das Lektin aus der Erbse Pisum sativum : Bindungsstudien, Monomer-Dimer-Gleichgewicht und Rückfaltung aus Fragmenten

NASA Astrophysics Data System (ADS)

Küster, Frank

2002-11-01

Das Lektin aus Pisum sativum, der Gartenerbse, ist Teil der Familie der Leguminosenlektine. Diese Proteine haben untereinander eine hohe Sequenzhomologie, und die Struktur ihrer Monomere, ein all-ß-Motiv, ist hoch konserviert. Dagegen gibt es innerhalb der Familie eine große Vielfalt an unterschiedlichen Quartärstrukturen, die Gegenstand kristallographischer und theoretischer Arbeiten waren. Das Erbsenlektin ist ein dimeres Leguminosenlektin mit einer Besonderheit in seiner Struktur: Nach der Faltung in der Zelle wird aus einem Loop eine kurze Aminosäuresequenz herausgeschnitten, so dass sich in jeder Untereinheit zwei unabhängige Polypeptidketten befinden. Beide Ketten sind aber stark miteinander verschränkt und bilden eine gemeinsame strukturelle Domäne. Wie alle Lektine bindet Erbsenlektin komplexe Oligosaccharide, doch sind seine physiologische Rolle und der natürliche Ligand unbekannt. In dieser Arbeit wurden Versuche zur Entwicklung eines Funktionstests für Erbsenlektin durchgeführt und seine Faltung, Stabilität und Monomer-Dimer-Gleichgewicht charakterisiert. Um die spezifische Rolle der Prozessierung für Stabilität und Faltung zu untersuchen, wurde ein unprozessiertes Konstrukt in E. coli exprimiert und mit der prozessierten Form verglichen. Beide Proteine zeigen die gleiche kinetische Stabilität gegenüber chemischer Denaturierung. Sie denaturieren extrem langsam, weil nur die isolierten Untereinheiten entfalten können und das Monomer-Dimer-Gleichgewicht bei mittleren Konzentrationen an Denaturierungsmittel auf der Seite der Dimere liegt. Durch die extrem langsame Entfaltung zeigen beide Proteine eine apparente Hysterese im Gleichgewichtsübergang, und es ist nicht möglich, die thermodynamische Stabilität zu bestimmen. Die Stabilität und die Geschwindigkeit der Assoziation und Dissoziation in die prozessierten bzw. nichtprozessierten Untereinheiten sind für beide Proteine gleich. Darüber hinaus konnte gezeigt werden, dass auch unter nicht-denaturierenden Bedingungen die Untereinheiten zwischen den Dimeren ausgetauscht werden. Die Renaturierung der unprozessierten Variante ist unter stark nativen Bedingungen zu 100 % möglich. Das prozessierte Protein dagegen renaturiert nur zu etwa 50 %, und durch die Prozessierung ist die Faltung stark verlangsamt, der Faltungsprozess ist erst nach mehreren Tagen abgeschlossen. Im Laufe der Renaturierung wird ein Intermediat populiert, in dem die längere der beiden Polypeptidketten ein Homodimer mit nativähnlicher Untereinheitenkontaktfläche bildet. Der geschwindigkeitsbestimmende Schritt der Renaturierung ist die Assoziation der entfalteten kürzeren Kette mit diesem Dimer. The lectin from Pisum sativum (garden pea) is a member of the family of legume lectins. These proteins share a high sequence homology, and the structure of their monomers, an all-ß-motif, is highly conserved. Their quaternary structures, however, show a great diversity which has been subject to cristallographic and theoretical studies. Pea lectin is a dimeric legume lectin with a special structural feature: After folding is completed in the cell, a short amino acid sequence is cut out of a loop, resulting in two independent polypeptide chains in each subunit. Both chains are closely intertwined and form one contiguous structural domain. Like all lectins, pea lectin binds to complex oligosaccharides, but its physiological role and its natural ligand are unknown. In this study, experiments to establish a functional assay for pea lectin have been conducted, and its folding, stability and monomer-dimer-equilibrium have been characterized. To investigate the specific role of the processing for stability and folding, an unprocessed construct was expressed in E. coli and compared to the processed form. Both proteins have the same kinetic stability against chemical denaturant. They denature extremely slowly, because only the isolated subunits can unfold, and the monomer-dimer-equilibrium favors the dimer at moderate concentrations of denaturant. Due to the slow unfolding, both proteins exhibit an apparent hysteresis in the denaturation transition. Therefore it has not been possible to determine their thermodynamic stability. For both proteins, the stability and the rates of association and dissociation into processed or unprocessed subunits, respectively, are equal. Furthermore it could be shown that even under non-denaturing conditions the subunits are exchanged between dimers. Renaturation of the unprocessed variants is possible under strongly native conditions with 100 % yield. The processed protein, however, can be renatured with yields of about 50 %, and its refolding is strongly decelerated. The folding process is finished only after several days. During renaturation, an intermediate is populated, in which the longer of the two polypeptide chains forms a homodimer with a native-like subunit interface. The rate limiting step of renaturation is the association of the unfolded short chain with this dimer.

Kinetics and pathways for crystallization of amorphous mullite and YAG

NASA Astrophysics Data System (ADS)

Johnson, Bradley Richard

The crystallization behavior of quenched mullite (3Al2O 3•2SiO2) and YAG (Y3Al5O 12) composition glasses (made using containerless methods) were characterized with the ultimate goal of producing single crystal, structural, ceramic oxide fibers from these materials. The kinetics for crystallization were determined from thermal analysis experiments. From the results, time-temperature-transformation (TTT) curves were calculated. The crystallization pathways were determined by examining the crystal structure, microstructure, and chemical composition of heat treated specimens using x-ray diffraction (XRD), scanning electron microscopy (SEM), and transmission electron microscopy (TEM). A machine was also designed and built to facilitate controlled crystallization of amorphous fibers. Quenched, Y3Al5O12 composition beads crystallized at temperatures as low as 840°C. The as-received specimens contained a few, small YAG crystals, in addition to a mixture of different amorphous phases. The coexistence of two different amorphous phases of the same composition, but having different densities is termed polyamorphism, and this has been reported to occur in Y3Al5O12 composition quenched melts. Although various crystallization pathways have been reported for chemically synthesized YAG precursors, these specimens crystallized directly into YAG, which was the only phase formed. Quenched, 3Al2O3•2SiO2 composition mullite beads and fibers crystallized at temperatures as low as 920°C. Due to phase separation in the quenched melts, multiple phases with slightly different compositions and different crystallization activation energies crystallized. These phases were not equilibrium, 3:2 mullite, but metastable, alumina-rich, pseudotetragonal mullite. The residual, amorphous, silica-rich phase existed as numerous, 7--10 nm sized inclusions embedded within pseudotetragonal mullite. A large amount of internal strain was detected in pseudotetragonal mullite, and the source of this strain was suggested to be the embedded, silica-rich inclusions. Pseudotetragonal mullite gradually converted to equilibrium, orthorhombic, 3:2 mullite between 1000--1400°C. This was characterized by assimilation of the embedded, silica-rich inclusions and the elimination of internal strain. Additionally, recrystallization of numerous, small, strain- and inclusion-free, 3:2 mullite grains was observed to occur as the process proceeded to completion.

High Temperature, Controlled-Atmosphere Aerodynamic Levitation Experiments with Applications in Planetary Science

NASA Astrophysics Data System (ADS)

Macris, C. A.; Badro, J.; Eiler, J. M.; Stolper, E. M.

2016-12-01

The aerodynamic levitation laser apparatus is an instrument in which spherical samples are freely floated on top of a stream of gas while being heated with a CO2laser to temperatures up to about 3500 °C. Laser heated samples, ranging in size from 0.5 to 3.5 mm diameter, can be levitated in a variety of chemically active or inert atmospheres in a gas-mixing chamber (e.g., Hennet et al. 2006; Pack et al. 2010). This allows for containerless, controlled-atmosphere, high temperature experiments with potential for applications in earth and planetary science. A relatively new technique, aerodynamic levitation has been used mostly for studies of the physical properties of liquids at high temperatures (Kohara et al. 2011), crystallization behavior of silicates and oxides (Arai et al. 2004), and to prepare glasses from compositions known to crystallize upon quenching (Tangeman et al. 2001). More recently, however, aerodynamic levitation with laser heating has been used as an experimental technique to simulate planetary processes. Pack et al. (2010) used levitation and melting experiments to simulate chondrule formation by using Ar-H2 as the flow gas, thus imposing a reducing atmosphere, resulting in reduction of FeO, Fe2O3, and NiO to metal alloys. Macris et al. (2015) used laser heating with aerodynamic levitation to reproduce the textures and diffusion profiles of major and minor elements observed in impact ejecta from the Australasian strewn field, by melting a powdered natural tektite mixed with 60-100 μm quartz grains on a flow of pure Ar gas. These experiments resulted in quantitative modeling of Si and Al diffusion, which allowed for interpretations regarding the thermal histories of natural tektites and their interactions with the surrounding impact vapor plume. Future experiments will employ gas mixing (CO, CO2, H2, O, Ar) in a controlled atmosphere levitation chamber to explore the range of fO2applicable to melt-forming impacts on other rocky planetary bodies, including the Moon and Mars. Arai et al., Rev. Sci. Instrum. 75, 2262-2265 (2004) Hennet et al., Rev. Sci. Instrum. 73, 124-129 (2001) Kohara et al., P. Natl. Acad. Sci.USA 108, 14780-14785 (2011) Macris et al., GSA Abstracts with Programs 47, 437 (2015) Pack et al., Geochem. T. 11, 1-16 (2010) Tangeman et al., Geophys. Res. Lett. 28, 2517-2520 (2001)

Solidification studies of nanocrystalline and quasicrystalline materials from the undercooled state

NASA Astrophysics Data System (ADS)

Croat, Thomas Kevin

2001-07-01

Nanocrystallization occurring during metallic glass devitrification is studied in Zr-Al-Ni-Cu bulk metallic glasses (BMGs) and Al-RE-TM (RE = rare-earth, TM = transition metal) metallic glasses. The importance of transient nucleation in BMG devitrification was established by a direct transmission electron microscopy (TEM) measurement of the grain density in two-stage annealed samples. TEM examination of low temperature annealed BMGs also suggest that amorphous phase separation is occurring prior to crystallization. Nanocrystallization of rapidly quenched Al-RE-Ni glasses was preceded by the compositional segregation of the initially homogeneous glass into Al-rich and solute-rich regions (mainly nickel-enriched) on a ≈50--100 nm length scale, suggesting amorphous phase separation. This pre-existing compositional modulation on a nanometer scale leads naturally to the development of nanocrystals. The average rare earth radius (rRE) in Al-RE-Ni alloys was altered by co-substitution of chemically similar rare earth elements. In glasses with smaller r RE, nucleation of alpha-Al occurred preferentially near the boundaries of the phase-separated regions. However, phase separation did not universally lead to alpha-Al nanocrystallization; glasses with larger rRE crystallized to metastable intermetallic phases with a 50--100 nm grain size. Kinetic analysis of the alpha-Al crystallization was performed using isothermal DSC, yielding abnormally low Avrami exponents (n = 1.0--1.5); these values were found to be consistent with the observed transformation using a model that considers the overlapping diffusion fields of the alpha-Al grains during growth within the phase separated region. Containerless solidification experiments on Ti-based quasicrystal-forming alloys have been performed using various techniques, including drop-tube solidification, electromagnetic levitation (EML) and electrostatic levitation (ESL). In Ti-Fe-Si-O, the alpha-1/1 quasicrystal approximant phase is found to nucleate directly from the liquid over the range TixFe94-xSi 4(SiO2)2 with 67 < x < 69 in EML experiments. Both the alpha-1/1 phase in Ti-Fe-Si-O and the C14 Laves phase in Ti-Zr-Ni have lower relative undercoolings than nearby crystal phases. This presumably reflects the structural similarity between these polytetrahedral phases and the undercooled liquid, which leads to smaller nucleation barriers and lower maximum undercoolings.

Investigation of upper mantle seismic discontinuities beneath the Indian Ocean using array seismology methods

NASA Astrophysics Data System (ADS)

van Driel, J.; Reiss, A. S.; Thomas, C.

2016-12-01

The topography of upper mantle seismic discontinuities can be used to constrain regional variations in composition and temperature of the Earths mantle. The 410 km discontinuity is caused by the solid-solid phase transition from olivine to wadsleyite. Due to its positive Clapeyron slope, the discontinuity is depressed in hot regimes. The phase transition from ringwoodite to bridgemanite and magnesiowüstite in contrast has a negative Clapeyron slope and therefore is elevated when hot material is present. Cold material is expected to yield an opposing topographic signature, culminating in an elevated 410 km and a depressed 660 km discontinuity. As part of the RHUM-RUM project (Réunion Hotspot and Upper Mantle - Réunions Unterer Mantel) we extract relevant geophysical parameters, by investigating the properties of upper mantle seismic discontinuities beneath the Indian Ocean. The topography of the 410 and 660 km discontinuities, which define the upper and lower bounds of the mantle transition zone, have been mapped using PP and SS underside reflections. This study has utilised over 8500 events with Mw ≥ 5.8, distributed over the entire Indian Ocean. Our robust data set yields a dense coverage of points, which are defined by consistently crossing ray paths. Array seismology methods, such as vespagrams and slowness-backazimuth analysis, are used to enhance the signal-to-noise-ratio and detect and identify weak precursor signals. The differential travel times are corrected for crustal features and converted into depth values of the discontinuities by comparing the measured travel times with theoretical ones derived from ray tracing through the 1D reference Earth model ak135. A `travel-time' stacking method has also been applied for 4° radius bins around each of the bounce points. The addition of a secondary method derives greater stability of our results and allows an enhanced error analysis procedure. In order to better constrain the mineralogical processes taking place within the mantle transition zone, amplitude ratios, polarities and velocity gradients have also been investigated.

Experimental technique for studying high-temperature phase equilibria in reactive molten metal based systems

NASA Astrophysics Data System (ADS)

Ermoline, Alexandre

The general objective of this work is to develop an experimental technique for studying the high-temperature phase compositions and phase equilibria in molten metal-based binary and ternary systems, such as Zr-O-N, B-N-O, Al-O, and others. A specific material system of Zr-O-N was selected for studying and testing this technique. The information about the high-temperature phase equilibria in reactive metal-based systems is scarce and their studying is difficult because of chemical reactions occurring between samples and essentially any container materials, and causing contamination of the system. Containerless microgravity experiments for studying equilibria in molten metal-gas systems were designed to be conducted onboard of a NASA KC-135 aircraft flying parabolic trajectories. A uniaxial apparatus suitable for acoustic levitation, laser heating, and splat quenching of small samples was developed and equipped with computer-based controller and optical diagnostics. Normal-gravity tests were conducted to determine the most suitable operating parameters of the levitator by direct observations of the levitated samples, as opposed to more traditional pressure mapping of the acoustic field. The size range of samples that could be reliably heated and quenched in this setup was determined to be on the order of 1--3 mm. In microgravity experiments, small spherical specimens (1--2 mm diameter), prepared as pressed, premixed solid components, ZrO2, ZrN, and Zr powders, were acoustically levitated inside an argon-filled chamber at one atmosphere and heated by a CO2 laser. The levitating samples could be continuously laser heated for about 1 sec, resulting in local sample melting. The sample stability in the vertical direction was undisturbed by simultaneous laser heating. Oscillations of the levitating sample in the horizontal direction increased while it was heated, which eventually resulted in the movement of the sample away from its stable levitation position and the laser beam. The follow-up on-ground experiments were conducted to study phase relations in the Zr-O-N system at high-temperatures. Samples with specific compositions were laser-heated above the melt formation and naturally cooled. Recovered samples were characterized using electron microscopy, energy-dispersive spectroscopy, and x-ray diffraction. Results of these analyses combined with the interpretations of the binary Zr-O and Zr-N phase diagrams enabled us to outline the liquidus and the subsolidus equilibria for the ternary Zr-ZrO2-ZrN phase diagrams. Further research is suggested to develop the microgravity techniques for detailed characterization of high-temperature relations in the reactive, metal based systems.

Planar millimeter wave radar frontend for automotive applications

NASA Astrophysics Data System (ADS)

Grubert, J.; Heyen, J.; Metz, C.; Stange, L. C.; Jacob, A. F.

2003-05-01

A fully integrated planar sensor for 77 GHz automotive applications is presented. The frontend consists of a transceiver multichip module and an electronically steerable microstrip patch array. The antenna feed network is based on a modified Rotman-lens and connected to the array in a multilayer approach offering higher integration. Furthermore, the frontend comprises a phase lock loop to allow proper frequency-modulated continuous wave (FMCW) radar operation. The latest experimental results verify the functionality of this advanced frontend design featuring automatic cruise control, precrash sensing and cut-in detection. These promising radar measurements give reason to a detailed theoretical investigation of system performance. Employing commercially available MMIC various circuit topologies are compared based on signal-tonoise considerations. Different scenarios for both sequential and parallel lobing hint to more advanced sensor designs and better performance. These improvements strongly depend on the availability of suitable MMIC and reliable packaging technologies. Within our present approach possible future MMIC developments are already considered and, thus, can be easily adapted by the flexible frontend design. Es wird ein integrierter planarer Sensor für 77 GHz Radaranwendungen vorgestellt. Das Frontend besteht aus einem Sende- und Empfangs-Multi-Chip-Modul und einer elektronisch schwenkbaren Antenne. Das Speisenetzwerk der Antenne basiert auf einer modifizierten Rotman- Linse. Für eine kompakte Bauweise sind Antenne und Speisenetzwerk mehrlagig integriert. Weiterhin umfasst das Frontend eine Phasenregelschleife für eine präzise Steuerung des frequenzmodulierten Dauerstrichradars. Die aktuellen Messergebnisse bestätigen die Funktionalit¨at dieses neuartigen Frontend-Designs, das automatische Geschwindigkeitsregelung, Kollisionswarnung sowie Nahbereichsüberwachung ermöglicht. Die Qualität der Messergebnisse hat weiterführende theoretische Untersuchungen über die potenzielle Systemleistungsfähigkeit motiviert. Unter Berücksichtigung von kommerziell erhältlichenMMICs werden verschiedene Schaltungstopologien auf der Grundlage des Signal-Rausch-Verhältnisses verglichen. Sowohl für sequenzielle als auch für parallele Ansteuerung der Antennenkeulen wird eine deutliche Leistungssteigerung ermittelt. Diese Verbesserungen hängen maßgeblich von der Verfügbarkeit geeigneter MMICs und einer zuverlässigen Aufbau- und Verbindungstechnik ab. Das vorliegende Frontend-Konzept kann auf Grund seiner Flexibilität leicht an derlei zukünftige Entwicklungen angepasst werden.

Superconductivity and Magnetism in LaO1-xFxFeAs

NASA Astrophysics Data System (ADS)

Buechner, Bernd

2009-03-01

Measuring ^75As, ^139La, and ^57Fe Nuclear Magnetic Resonance (NMR) as well as μSR, transport and thermodynamic properties we have determined the phase diagram of LaO1-xFxAsFe superconductors [1-6]. In my talk, I will show experimental studies of the magnetic ordering [2, 5], properties of the superconducting state [1, 3, 5] and the normal state properties [1, 4, 6] in the superconducting regions of the phase diagram. While the temperature dependence of the London penetration as determined from μSR points to an isotropic s wave state [3], our early NMR data suggest singlet pairing and nodes of the order parameter [1]. Extending the NMR work to lower temperatures we find evidence for a deviation of the T^3 behaviour of the spin lattice relaxation, which would agree with the extended s-wave symmetry suggested in recent theoretical work. In the paramagnetic normal state, NMR on all three nuclei shows that the local electronic susceptibility rises with increasing temperature. This had led to suggest the presence of a pseudogap, which I will discuss in detail. The scaling of all NMR shifts with respect to the macroscopic susceptibility indicates that there is no apparent multiband effect through preferential hyperfine couplings. Relaxation measurements indicate a similar temperature-dependence for (T1T)-1, and suggest that the dynamical susceptibility changes uniformly in q space with varying temperature. The transport properties show some striking similarities to the findings in cuprates [6] and, finally, susceptibility [4] as well as NMR studies point to the antiferromagnetic fluctuations, whose relevance is also discussed in many theoretical models of the superconducting pairing mechanism. In collaboration with Hans-Joachim Grafe, Christian Hess, R"udiger Klingeler, G"unter Behr, Agnieszka Kondrat, Norman Leps, and Guillaume Lang, IFW Dresden; Hans-Henning Klauss, TU Dresden; and Hubertus Luetkens, PSI Villigen. [4pt] References: [0pt] [1] H.-J. Grafe et al., Phys. Rev. Lett. 101, 047003 (2008) [0pt] [2] H.-H. Klauss et al., Phys. Rev. Lett. 101, 077005 (2008) [0pt] [3] H. Luetkens et al., Phys- Rev. Lett. 101, 097009 (2008) [0pt] [4] R. Klingeler et al., arXiv: 0808.0708 (2008) [0pt] [5] H. Luetkens et al., arXiv: 0806.3533 (2008) [0pt] [6] C. Hess et al., arXiv: 0811.1601 (2008)

Neue biosensorische Prinzipien für die Hämoglobin-A1c Bestimmung

NASA Astrophysics Data System (ADS)

Stöllner, Daniela

2002-06-01

Hämoglobin-A1c (HbA1c) ist ein Hämoglobin (Hb)-Subtypus, der durch nicht-enzymatische Glykierung des N-terminalen Valinrestes der Hämoglobin-beta-Kette entsteht. Das gemessene Verhältnis von HbA1c zum Gesamt-Hämoglobin (5-20 % bei Diabetikern) repräsentiert den Mittelwert der Blutglucosekonzentration über einen zweimonatigen Zeitraum und stellt zur Beurteilung der diabetischen Stoffwechsellage eine Ergänzung zur Akutkontrolle der Glukosekonzentration dar. Ziel der vorliegenden Arbeit war es, einen amperometrischen Biosensor für die Bestimmung des medizinisch relevanten Parameters HbA1c zu entwickeln. Durch Selektion geeigneter Bioerkennungselemente und deren Immobilisierung unter Erhalt der Bindungsfunktion für die Zielmoleküle Hämoglobin bzw. HbA1c wurden spezifische, hochaffine und regenerationsstabile Sensoroberflächen geschaffen. Für die Entwicklung des HbA1c-Biosensors wurden zwei Konzepte - Enzymsensor und Immunosensor - miteinander verglichen. Die enzymatische Umsetzung von HbA1c erfolgte mit der Fructosylamin Oxidase (FAO) aus Pichia pastoris N 1-1 unter Freisetzung von H2O2, welches sowohl optisch über eine Indikatorreaktion als auch elektrochemisch nach Einschluss der FAO in PVA-SbQ und Fixierung des Immobilisats vor einer H2O2-Elektrode nachgewiesen wurde. Die Kalibration des Enzymsensors mit der HbA1c-Modellsubstanz Fructosyl-Valin ergab Nachweisgrenzen, die ausserhalb des physiologisch relevanten HbA1c-Konzentrationsbereich lagen. Aus der Umsetzung von glykierten Peptiden mit einer nicht HbA1c analogen Aminosäurensequenz, z.B. Fructosyl-Valin-Glycin wurde zudem eine geringe HbA1c-Spezifität abgeleitet. Für den Immunosensor wurden zwei heterogene Immunoassay-Formate unter Verwendung von hochaffinen und spezifischen Antikörpern in Kombination mit Glucose Oxidase (GOD) als Markerenzym zum Nachweis von HbA1c untersucht. Beim indirekt-kompetitiven Immunoassay wurde anstelle des kompletten HbA1c-Moleküls das glykierte Pentapeptid Fructosyl-Valin-Histidin-Leucin-Threonin-Prolin (glkPP) als Kompetitor und Affinitätsligand immobilisiert und so eine regenerierfähige Oberfläche geschaffen. Beim Sandwich-Immunoassay wurde im ersten Schritt Gesamt-Hämoglobin an die mit Haptoglobin (Hp) modifizierte Festphase angereichert und im zweiten Schritt der gebundene HbA1c-Anteil nachgewiesen. Für die Konstruktion des HbA1c-Immunosensors wurden Affinitätsmatrizen durch Modifizierung von Cellulose-Dialysemembranen mit glkPP bzw. Hp hergestellt. Grundlegend studiert wurde die Aktivierung der Cellulose-Membranen mit 1,1'-Carbonyldiimidazol (CDI) und 1-Cyano-4-dimethylaminopyridintetrafluoroborat (CDAP) als Aktivierungsagenzien. Eine gerichtete Immobilisierung der Liganden wurde realisiert, indem glkPP über dessen C-Terminus (einzige Carboxylatgruppe) und Hp über dessen periodat-oxidiertem Kohlenhydratrest an die amino- oder hydrazidfunktionalisierte Membranen kovalent gekoppelt wurden. Mit dem Einsatz der glkPP- und Hp-modifizierten Membranen in der elektrochemischen Messzelle war erstmalig der biosensorische Nachweis von HbA1c möglich. Als Transduktor diente eine Pt-Elektrode, an der das von der GOD generierte H2O2 umgesetzt und ein mit der HbA1c-Konzentration korrelierendes Stromsignal erzeugt wurde. Die Immunosensoren zeigten Ansprechzeiten von 3 s. Mit dem Immunosensor auf Basis des indirekt-kompetitiven Testprinzips wurde eine Kalibrationskurve für HbA1c im Bereich von 0,25-30 µg/ml (3,9-465 nM, CV 3-9 %) mit Assayzeiten von 60 min und mit dem Immunosensor im Sandwich-Format eine Kalibrationskurve im Bereich von 0,5-5 µg/ml (7,8-78 nM; 5-50 % HbA1c vom Gesamt-Hb, CV 6-10 %, 3 h) aufgenommen. Hemoglobin-A1c (HbA1c) is a hemoglobin subtype formed by non-enzymatic reaction of glucose with the N-terminus of the beta-polypeptide chains. As it reflects the glycemic status of diabetics over the preceding 8-12 weeks, the determination of HbA1c has become an established procedure in the management of diabetes mellitus. It is measured as the percentage of total hemoglobin. Up to 5 % HbA1c are considered as normal whereas in diabetic subjects it could be elevated from 5-20 %. In addition to amperometric biosensors for glucose self monitoring which have been successfully applied in diabetes management, biosensors for HbA1c would be an useful supplement for a comprehensive diabetes control. Objective of this work was to develop and compare amperometric biosensors for determination of HbA1c based on enzymatic and immunochemical methods. For the enzyme based HbA1c assay a novel fructosamine oxidase (FAO) derived from marine yeast Pichia pastoris, strain N1-1 was utilized. It recognizes and oxidatively degrades fructosyl-valine (FV) which corresponds to the glycated N-terminus of the beta-chain of HbA1c and therefore is regarded as a model compound for HbA1c. Hydrogen peroxide which is liberated by the FAO during FV conversion was indicated optically in a horseradish peroxidase (POD) coupled reaction and electrochemically. For the biosensor the FAO was embedded in polyvinyl alcohol-stylbazole (PVA-SbQ) and fixed it in front of a Pt-electrode. So far, the measuring range of FV did not cover the clinically relevant range of HbA1c. Low specificity was assumed since enzyme activity also was obtained with glycated peptides, e.g. fructosyl-valine-glycine, not corresponding to the glycated N-terminus of the hemoglobin-beta-chain. For the immunosensor two immunoassays formats - heterogeneous sandwich and heterogeneous competitive - were tested. The assays were designed as follows: The competitive immunoassay was based on the immobilized synthetic glycated pentapeptide fructosyl-valine-histidine-leucine-threonine-proline (glkPP) utilized as HbA1c analogue. The peptide has an amino acid sequence corresponding to the N-terminus of the hemoglobin beta-chains and is capable for competition together with the HbA1c of the sample for the amount of a glucose oxidase (GOD)-labelled anti-HbA1c antibody. In the sandwich-type assay haptoglobin (Hp), a natural hemoglobin binding molecule with antibody characteristic properties, was used as bioreceptor for enrichment of total hemoglobin onto the surface. In a subsequent step the HbA1c fraction was quantified by a GOD-labelled HbA1c specific antibody. Cellulose dialysis membrane was used as the solid support for immobilization of Hp and glkPP near the sensor surface. For activation of the membrane two reagents, 1,1‧-carbonyldiimidazole (CDI) and 1-cyano-4-dimethylamino pyridinium tetrafluoroborate (CDAP), were compared with respect to the degree of activation and coupling efficiency. Site-directed immobilization of Hp and glkPP was achieved by coupling Hp via its carbohydrate residue and glkPP via its C-terminus to the activated membrane using a bis-amine or bis-hydrazide spacer. The affinity membranes were placed in front of a modified Clark-type hydrogen peroxide electrode in an electrochemical measuring cell and HbA1c analysis was carried out within the stirred cell. Detection of the bound GOD-label was achieved by measurement of the electrocatalytic oxidation of hydrogen peroxide at +600 mV vs. Ag/AgCl. The indication was done in only 3 s. For the competitive principle a typical inhibition curve with a linear range between 0,25-30 µg/ml (3,9-465 nM, CV 3-9 %, 60 min per sample) HbA1c was obtained. Due to the high functional stability of the peptide multiple regeneration of the affinity surface was possible without loss of binding capacity. With the sandwich assay configuration the clinically relevant range could easily be covered (calibration curve: 5-50 % HbA1c corresponding to 7,8-78 nM, CV 6-10 %, 3 h per sample).

Developing Glassy Magnets from Simulated Composition of Martian Soil for Exploration Applications

NASA Technical Reports Server (NTRS)

Ramachandran, N.; Ray, C. S.; Rogers, J. R.

2004-01-01

The long-term exploration goals of NASA include developing human habitation on Mars and conducting scientific investigations on Mars and other planetary bodies. In situ resource processing is a key objective in this area. We focus on the possibility of making magnetic glasses in situ for potential applications development. The paper will focus on ongoing work at NASA Marshall Space Flight Center on making magnetic glass from Mars soil simulants and its characterization. Analysis of the glass morphology, strength, chemistry and resulting magnetic properties will provide a fundamental understanding of the synthesized material that can be used for potential applications development. in an effort to characterize the magnetic properties of the Mars glasses, a series of tests were performed at NASA MSFC. Preliminary tests indicated that the glasses were attracted to a magnet and also had a small amount of residual magnetism. They were opaque (almost black in color). As the first step, a sample of Mars 1 glass (approx.1 mm x 1 mm x 5 mm length) was machined, weighed and its hysteresis curve was measured using a Vibration Sample Magnetometer (VSM). Next, a small furnace was designed and built and the sample was baked in a graphite (reducing agent) crucible at 800 C in an Argon atmosphere for 3 hours in the presence of a uniform, transverse (transverse to the 5mm length of the sample) magnetic field of 0.37 Tesla. The treated sample showed reddening on the outside and showed substantially increased residual magnetism. This sample was again analyzed in the VSM. The data clearly showed that some chemical change occurred during the heat treatment (color change) and that both the glasses have useful magnetic properties. Although no orientation effects of the magnetic field were considered, the data showed the following: 1. Both glass samples are primarily soft magnets and display ferromagnetic behavior (hysteresis, saturation, etc.) 2. The treated glass has improved saturation magnetism (order of magnitude increase), retentivity (factor of 6 increase) and susceptibility (order of magnitude increase) compared to the untreated glass 3. The untreated sample has higher coercivity (approx.50% that of Nickel) than the treated sample 4. Both samples have similar energy density. Results from a systematic study to quantify the effects of processing conditions such as heat treatment, atmosphere, containerless processing (by electrostatic levitation), and applications of external magnetic fields of different strengths will be discussed. Efforts on optimizing the magnetic properties of the product and the feasibility of using it for a couple of specific magnetic applications such as heat generation using an ac field and for electro forming will also be covered. The latter is an in situ manufacturing technique being studied for in-space fabrication applications at MSFC.

Spin-Up Instability of a Levitated Molten Drop in MHD-Flow Transition to Turbulence

NASA Technical Reports Server (NTRS)

Abedian, B.; Hyers, R. W.; Curreri, Peter A. (Technical Monitor)

2002-01-01

When an alternating magnetic field interacts with induced eddy currents in a conducting body, there will be a repulsive force between the body and the driving coil system generating the field. This repulsive force is the basis of electromagnetic levitation, which allows containerless processing of different materials. The eddy currents in the conducting body also generate Joule heating. Axial rotation of electromagnetically levitated objects is a common observation in levitation systems and often an undesirable side effect of such experiments on 1-g and -g. There have been recent efforts to use magnetic damping and suppress this tendency of body rotation. The first report of rotation in EML drops was attributed to a slight asymmetry of the shape and location of the levitation coils could change the axis and speed of rotation. Other theories of sample rotation include a frequency difference in the traveling electromagnetic waves and a phase difference in two different applied fields of the same frequency. All of these different mechanisms share the following characteristics: the torque is small, constant for constant field strength, and very weakly dependent on the sample's temperature and phase (solid or liquid). During experiments on the MSL-1 (First Microgravity Science Laboratory) mission of the Space Shuttle (STS-83 and STS-94, April and July 1997), a droplet of palladium-silicon alloy was electromagnetically levitated for viscosity measurements. For the non-deforming droplet, the resultant MHD flow inside the drop is inferred from motion of impurities on the surface. These observations indicate formation of a pair of co-rotating toroidal flow structures inside the spheroidal levitated drop that undergo secondary flow instabilities. As rise in the fluid temperature rises, the viscosity falls and the internal flow accelerates and becomes oscillatory; and beyond a point in the experiments, the surface impurities exhibit non-coherent chaotic motion signifying emergence of turbulence inside the drop. In this work, a background of these set of observations will be given followed by a presentation of our results on the digital particle tracking analysis that has been performed on a number of available videos. The analysis indicates that the levitated drop attains a constant rotational speed during the melting phase and formation of the co-rotating axi-symmetric laminar toroidal structures. However, the rate of axial rotation increases dramatically during the deformation of the toroidal structures anti their breakup into chaotic entities. This new data suggests an interaction between the flow inside the levitated molten drop and the driving coils in the experiments. Possible mechanisms for this interaction will be reviewed. The data will also be used to make an assessment of existing theories on droplet rotation.

Correction of clock errors in seismic data using noise cross-correlations

NASA Astrophysics Data System (ADS)

Hable, Sarah; Sigloch, Karin; Barruol, Guilhem; Hadziioannou, Céline

2017-04-01

Correct and verifiable timing of seismic records is crucial for most seismological applications. For seismic land stations, frequent synchronization of the internal station clock with a GPS signal should ensure accurate timing, but loss of GPS synchronization is a common occurrence, especially for remote, temporary stations. In such cases, retrieval of clock timing has been a long-standing problem. The same timing problem applies to Ocean Bottom Seismometers (OBS), where no GPS signal can be received during deployment and only two GPS synchronizations can be attempted upon deployment and recovery. If successful, a skew correction is usually applied, where the final timing deviation is interpolated linearly across the entire operation period. If GPS synchronization upon recovery fails, then even this simple and unverified, first-order correction is not possible. In recent years, the usage of cross-correlation functions (CCFs) of ambient seismic noise has been demonstrated as a clock-correction method for certain network geometries. We demonstrate the great potential of this technique for island stations and OBS that were installed in the course of the Réunion Hotspot and Upper Mantle - Réunions Unterer Mantel (RHUM-RUM) project in the western Indian Ocean. Four stations on the island La Réunion were affected by clock errors of up to several minutes due to a missing GPS signal. CCFs are calculated for each day and compared with a reference cross-correlation function (RCF), which is usually the average of all CCFs. The clock error of each day is then determined from the measured shift between the daily CCFs and the RCF. To improve the accuracy of the method, CCFs are computed for several land stations and all three seismic components. Averaging over these station pairs and their 9 component pairs reduces the standard deviation of the clock errors by a factor of 4 (from 80 ms to 20 ms). This procedure permits a continuous monitoring of clock errors where small clock drifts (1 ms/day) as well as large clock jumps (6 min) are identified. The same method is applied to records of five OBS stations deployed within a radius of 150 km around La Réunion. The assumption of a linear clock drift is verified by correlating OBS for which GPS-based skew corrections were available with land stations. For two OBS stations without skew estimates, we find clock drifts of 0.9 ms/day and 0.4 ms/day. This study salvages expensive seismic records from remote regions that would be otherwise lost for seismicity or tomography studies.

Sonification of acoustic emission data

NASA Astrophysics Data System (ADS)

Raith, Manuel; Große, Christian

2014-05-01

While loading different specimens, acoustic emissions appear due to micro crack formation or friction of already existing crack edges. These acoustic emissions can be recorded using suitable ultrasonic transducers and transient recorders. The analysis of acoustic emissions can be used to investigate the mechanical behavior of different specimens under load. Our working group has undertaken several experiments, monitored with acoustic emission techniques. Different materials such as natural stone, concrete, wood, steel, carbon composites and bone were investigated. Also the experimental setup has been varied. Fire-spalling experiments on ultrahigh performance concrete and pullout experiments on bonded anchors have been carried out. Furthermore uniaxial compression tests on natural stone and animal bone had been conducted. The analysis tools include not only the counting of events but the analysis of full waveforms. Powerful localization algorithms and automatic onset picking techniques (based on Akaikes Information Criterion) were established to handle the huge amount of data. Up to several thousand events were recorded during experiments of a few minutes. More sophisticated techniques like moment tensor inversion have been established on this relatively small scale as well. Problems are related to the amount of data but also to signal-to-noise quality, boundary conditions (reflections) sensor characteristics and unknown and changing Greens functions of the media. Some of the acoustic emissions recorded during these experiments had been transferred into audio range. The transformation into the audio range was done using Matlab. It is the aim of the sonification to establish a tool that is on one hand able to help controlling the experiment in-situ and probably adjust the load parameters according to the number and intensity of the acoustic emissions. On the other hand sonification can help to improve the understanding of acoustic emission techniques for training purposes (students, co-workers). On goal is to establish a real-time frequency transformation into the audio range to avoid time consuming visual data processing during the experiments. It is also the intention to analyze the signals using psycho-acoustic methods with the help of specialists from electrical engineering. Reference: Raith, Manuel (2013). "Schallemissionsanalyse bei Pulloutexperimenten an Verbunddübeln" Masterarbeit. Technische Universität München, Lehrstuhl für Zerstörungsfreie Prüfung. Malm, Fabian (2012). "Schallemissionsanalyse am humanen Femur" Masterarbeit. Technische Universität München, Lehrstuhl für Zerstörungsfreie Prüfung. Richter R. (2009): Einsatz der Schallemissionsanalyse zur Detektion des Riss und Abplatzungsverhaltens von Beton unter Brandeinwirkung. Diplomarbeit. Materialprüfungsanstalt Universität Stuttgart Keywords: Acoustic emission, bonded anchors, femur, pullout test, fire-spalling

FORS am Very Large Telescope der Europäischen Südsternwarte

NASA Astrophysics Data System (ADS)

1998-09-01

Erstes wissenschaftliches Beobachtungsinstrument liefert eindrucksvolle Bilder Entsprechend dem straffen Zeitplan wird das ESO Very Large Teleskop Projekt (VLT-Projekt) auf dem Cerro Paranal in Nord-Chile verwirklicht: die volle Betriebsbereitschaft des ersten der vier 8,2m-Einzelteleskope wird Anfang des nächsten Jahres erreicht sein. Am 15. September 1998 wurde ein weiterer wichtiger Meilenstein erfolgreich, rechtzeitig und innerhalb des Kostenplans erreicht. Nur wenige Tage nach seiner Montage am ersten 8,2m-Einzelteleskop des VLT (UT1) konnte FORS1 ( FO cal R educer and S pectrograph) als erstes einer Gruppe leistungsfähiger und komplexer wissenschaftlicher Instrumente seine Beobachtungstätigkeit beginnen. Von Anfang an konnte es eine Reihe exzellenter astronomischer Bilder aufnehmen. Dieses bedeutende Ereignis eröffnet eine Fülle neuer Möglichkeiten für die europäische Astronomie. FORS - ein Höhepunkt an Komplexität FORS1 und das zukünftige Zwillingsinstrument (FORS2) sind das Ergebnis einer der eingehendsten und fortschrittlichsten technologischen Studien, die je für ein Instrument der bodengebundenen Astronomie durchgeführt wurden. Dieses einzigartige Instrument ist nun im Cassegrain-Fokus installiert und verschwindet beinahe, trotz seiner Dimensionen von 3 x 1.5m (Gewicht 2.3t), unterhalb des riesigen 53 m 2 großen Zerodurspiegels. Um die große Spiegelfläche und die hervorragende Bildqualität von UT1 optimal auszunützen, wurde FORS speziell so konstruiert, daß es die lichtschwächsten und entferntesten Objekte im Weltall untersuchen kann. Bald wird dieses komplexe VLT-Instrument den europäischen Astronomen erlauben, die derzeitigen Beobachtungshorizonte entscheidend zu erweitern. Die beiden FORS-Instrumente sind Vielzweck-Beobachtungsinstrumente, die in mehreren unterschiedlichen Beobachtungsarten eingesetzt werden können. Beispielsweise können Bilder mit zwei verschiedenen Abbildungsmaßstäben (Vergrößerungen) sowie Spektren mit unterschiedlicher spektraler Auflösung von einzelnen oder mehreren Objekten aufgenommen werden. Dabei erlaubt der schnelle Wechsel zwischen den unterschiedlichen Beobachtungsarten z.B. zunächst die Aufnahme und direkt anschließend die Spektroskopie weit entfernter Galaxien. Damit kann dann u.a. die stellare Zusammensetzung und die Entfernung bestimmt werden. Als eines der leistungsfähigsten astronomischen Instrumente seiner Art wird FORS1 ein wahres Arbeitspferd für die Untersuchung des fernen Universums darstellen. Der Bau von FORS Das FORS-Projekt wird unter ESO-Kontrakt von einem Konsortium dreier deutscher astronomischer Institute durchgeführt, der Landessternwarte Heidelberg und den Universitäts-Sternwarten von Göttingen and München. Bis zur Beendigung des Projekts werden die beteiligten Institute Arbeit im Umfang von ca. 180 Mann-Jahren eingebracht haben. Bei der Landessternwarte Heidelberg lag die Leitung des Projekts. Hier wurde außerdem das gesamte optische System konstruiert, die Beschaffung der Komponenten der abbildenden Optik und der Zusatzoptiken für Spektroskopie und Polarimetrie durchgeführt und die spezielle Computersoftware geschrieben, mit der die von FORS gelieferten Daten verarbeitet und ausgewertet werden. Darüber hinaus wurde in der Werkstatt der Sternwarte ein Teleskopsimulator gebaut, mit dem alle wesentlichen Funktionen von FORS in Europa getestet werden konnten, bevor das Instrument zum Paranal (Chile) transportiert wurde. An der Universitäts-Sternwarte Göttingen wurden Konstruktion, Herstellung und Zusammenbau der gesamten Mechanik von FORS durchgeführt. Der größte Teil der Präzisionsteile, insbesondere der Multispalteinheit, wurde in der feinmechanischen Werkstatt der Sternwarte hergestellt. Die Beschaffung der großen Instrumentengehäuse und Flansche, die Computeranalysen für mechanische und thermische Stabilität des empfindlichen Spektrographen und die Herstellung der speziellen Werkzeuge für Handhabung, Wartung und Justierung lag ebenso in der Verantwortung dieser Sternwarte wie die Tests der zahlreichen opto- und elektromechanischen Funktionen. Die Universitäts-Sternwarte München war verantwortlich für das Projektmanagement, Integration und Test des gesamten Instruments im Labor, für Planung und Einbau aller Elektronik und Elektromechanik, sowie für Entwicklung und Test der gesamten Software, die FORS in allen Teilen vollständig per Computer steuert (z.B. Filter- und Grismräder, Verschlüsse, Spalteinheit für die Vielspaltspektroskopie, Masken, alle optischen Komponenten, Elektromotoren, Encoder usw.). Zusätzlich wurde Computersoftware geschrieben, mit der die komplexen astronomischen Beobachtungen mit FORS vorbereitet werden und das Verhalten des Instruments durch eine ständige Kontrolle der gesammelten wissenschaftlichen Daten überwacht wird. Als Gegenleistung für den Bau von FORS erhalten die Astronomen der drei beteiligten Institute des FORS-Konsortiums eine gewisse Anzahl von Nächten an "garantierter Beobachtungszeit" am VLT. In dieser Beobachtungszeit werden verschiedene Forschungsprojekte durchgeführt, deren Themen unter anderem von kleinen Körpern im äußeren Sonnensystem über Untersuchungen von Sternen im Endstadium und den von ihnen abgestoßenen Gaswolken bis zur Erforschung ferner Galaxien und Quasare reichen, die Aufschluß über die frühen Zeiten unseres Universums geben. Erste Tests von FORS1 am VLT-UT1: ein großartiger Erfolg Nach sorgfältiger Vorbereitung hat das FORS-Konsortium nun mit der Inbetriebnahme ("Commissioning") des Instruments begonnen. Dazu gehören ein eingehender Nachweis der spezifizierten Leistungsfähigkeit am Teleskop, die Überprüfung der korrekten Funktionsweise unter Softwaresteuerung vom Kontrollraum auf Paranal, und am Ende dieses Prozesses eine Demonstration, daß das Instrument seinen angestrebten wissenschaftlichen Zweck erfüllt. Während der Durchführung dieser Tests gelangen dem Commissioning-Team auf Paranal eine Reihe von Aufnahmen verschiedener astronomischer Objekte, von denen einige hier wiedergegeben sind. Sie wurden alle mit FORS in der Standardauflösung gewonnen (Bildfeldgröße 6.8 x 6.8 Bogenminuten, Pixelgröße 0.20 Bogensekunden) und zeigen einige der eindrucksvollen Möglichkeiten, die das neue Instrument bietet. Spiralgalaxie NGC 1288 ESO PR Photo 37a/98 ESO PR Photo 37a/98 [Preview - JPEG: 800 x 908 pix - 224k] [High-Res - JPEG: 3000 x 3406 pix - 1.5Mb] Farbaufnahme der Spiralgalaxie NGC 1288, aufgenommen in der ersten Beobachtungsnacht von FORS ("Nacht des ersten Lichts"). Das erste Photo zeigt eine Dreifarbenaufnahme der schönen Spiralgalaxie NGC 1288 im südlichen Sternbild Fornax. PR Photo 37a/98 umfaßt das gesamte Feld, das mit der 2048 x 2048 Pixel großen CCD-Kamera abgebildet wurde. Es wurde aus drei CCD-Aufnahmen zusammengesetzt, die bei gutem Seeing in verschiedenen Farben in der "Nacht des ersten Lichts" (15. September 1998) aufgenommen wurden. Diese Galaxie mit einem Durchmesser von rund 200000 Lichtjahren ist etwa 300 Millionen Lichtjahre entfernt, ihre Fluchtgeschwindigkeit beträgt 4500 km/sec. Technische Informationen : Photo 37a/98 ist ein Komposit von drei Aufnahmen in den drei Filtern B (420nm, 6 Minuten belichtet), V (530nm, 3 Minuten) und I (800nm, 3 Minuten) während einer Periode mit 0.7 Bogensekunden Seeing. Das gezeigte Feld ist 6.8 x 6.8 Bogenminuten groß. Norden ist links, Osten unten. Entfernter Galaxienhaufen ESO PR Photo 37b/98 ESO PR Photo 37b/98 [Preview - JPEG: 657 x 800 pix - 248k] [High-Res - JPEG: 2465 x 3000 pix - 1.9Mb] Ein ungewöhnlicher Galaxienhaufen in der Umgebung des Quasars PB5763 . ESO PR Photo 37c/98 ESO PR Photo 37c/98 [Preview - JPEG: 670 x 800 pix - 272k] [High-Res - JPEG: 2512 x 3000 pix - 1.9Mb] Vergrößerung von PR Photo 37b/98; sie zeigt mehr Einzelheiten des ungewöhnlichen Galaxienhaufens. Die nächsten Photos wurden von einer 5-minütigen Aufnahme im Nahen Infrarot reproduziert, die ebenfalls in der "Nacht des ersten Lichts" von FORS1 (15. September 1998) gewonnen wurde. PR Photo 37b/98 zeigt einen Himmelsausschnitt in der Nähe des Quasars PB5763, in dem auch ein ungewöhnlicher, sehr weit entfernter Haufen von Galaxien zu sehen ist. Er besteht aus einer großen Zahl lichtschwacher Galaxien, die bisher noch nicht eingehend untersucht wurden. Dieser Haufen ist ein gutes Beispiel für die Art von Objekten, auf die viel Beobachtungszeit mit FORS verwendet werden wird, sobald der reguläre Beobachtungsbetrieb begonnen hat. Eine Vergrößerung des gleichen Feldes ist in PR Photo 37c/98 wiedergegeben. Sie zeigt die einzelnen Mitglieder dieses Galaxienhaufens im Detail. Man beachte besonders die interessante spindelförmige Galaxie, die anscheinend einen äquatorialen Ring aufweist. Neben einer schönen Spiralgalaxie sind auch noch viele weitere lichtschwache Galaxien zu erkennen. Sie sind entweder Zwerggalaxien und Mitglieder des Haufens oder befinden sich sehr viel weiter entfernt im Hintergrund des Haufens. Technische Informationen : PR Photos 37b/98 (als Negativ reproduziert) und 37c/98 (Positiv) stammen von einer Aufnahme, die bei 0.8 Bogensekunden Seeing durch ein I-Filter (nahes Infrarot, 800nm) gewonnen wurde. Die Belichtungszeit betrug 5 Minuten, und es wurde eine Flatfield-Korrektur durchgeführt. Das gezeigte Feld ist 6.8 x 6.8 Bogenminuten bzw. 2.5 x 2.3 Bogenminuten groß. Norden ist links oben, Osten links unten. Spiralgalaxie NGC 1232 ESO PR Photo 37d/98 ESO PR Photo 37d/98 [Preview - JPEG: 800 x 912 pix - 760k] [High-Res - JPEG: 3000 x 3420 pix - 5.7Mb] Ein Farbbild der Spiralgalaxie NGC 1232, aufgenommen am 21. September 1998. ESO PR Photo 37e/98 ESO PR Photo 37e/98 [Preview - JPEG: 800 x 961 pix - 480k] [High-Res - JPEG: 3000 x 3602 pix - 3.5Mb] Vergrößerung des Zentrums von PR Photo 37d/98. Dieses spektakuläre Bild der großen Spiralgalaxie NGC 1232 (Photo 37d/98) wurde am 21. September 1998 unter guten Beobachtungsbedingungen erhalten. Es wurde aus drei Einzelaufnahmen im ultravioletten, blauen und roten Licht zusammengesetzt. Die Farben der verschiedenen Regionen sind deutlich sichtbar: Das Zentralgebiet enthält ältere, rötlich leuchtende Sterne (Photo 37e/98), während die Spiralarme von jungen, bläulichen Sternen und roten Sternentstehungsgebieten bevölkert sind. Man beachte die gestörte Begleitgalaxie am linken Rand (Photo 37d/98), die wie der griechische Buchstabe "Theta" aussieht. NGC 1232 liegt 20 Grad südlich des Himmelsäquators im Sternbild Eridanus. Obwohl die Entfernung dieser Galaxie ungefähr 100 Millionen Lichtjahre beträgt, kann man auf Grund der exzellenten Bildqualität einen unglaublichen Reichtum an Details erkennen. Bei dieser Entfernung entspricht die Kantenlänge des Bildfeldes etwa 200000 Lichtjahren oder etwa der doppelten Größe unserer Milchstraße. Technische Informationen : Photos 37d/98 und 37e/98 sind ein Komposit von drei Aufnahmen in den drei Filtern U (360nm, 10 Minuten belichtet), B (420nm, 6 Minuten) und R (600nm, 2 Minuten 30 Sekunden) während einer Periode mit 0.7 Bogensekunden Seeing. Das gezeigte Feld ist 6.8 x 6.8 Bogenminuten bzw. 1.6 x 1.8 Bogenminuten groß. Norden ist oben, Osten links. Note: [1] Diese Pressemitteilung wird gemeinsam (auf Englisch und Deutsch) von der Europäischen Südsternwarte, der Landessternwarte Heidelberg und den Universitäts-Sternwarten Göttingen und München herausgegeben. An English Version of this Press Release is also available. Zugang zu ESO Presseinformationen ESO Presseinformationen werden im World Wide Web zur Verfügung gestellt (URL: http://www.eso.org/outreach/press-rel/). ESO Pressephotos dürfen veröffentlicht werden, wenn die Europäische Südsternwarte als Urheber genannt wird.

Erzwingt die Quantenmechanik eine drastische Änderung unseres Weltbilds? Gedanken und Experimente nach Einstein, Podolsky und Rosen

NASA Astrophysics Data System (ADS)

Frodl, Peter

Von den Anfängen der Quantenmechanik bis heute gibt es Versuche, sie als statistische Theorie über Ensembles individueller klassischer Systeme zu interpretieren. Die Bedingungen, unter denen Theorien verborgener Parameter zu deterministischen Beschreibungen dieser individuellen Systeme als klassisch angesehen werden können, wurden von Einstein, Podolsky und Rosen 1935 formuliert: 1. Physikalische Systeme sind im Prinzip separierbar. 2. Zu jeder physikalischen Größe, deren Wert man ohne Störung des betrachteten Systems mit Sicherheit voraussagen kann, existiert ein ihr entsprechendes Element der physikalischen Realität.Zusammen sind sie, wie Bell 1964 gezeigt hat, prinzipiell unverträglich mit der Quantenmechanik und unhaltbar angesichts neuerer Experimente. Diese erweisen einmal mehr die Quantenmechanik als richtige Theorie. Um ihre Ergebnisse zu verstehen, müssen wir entweder die in der klassischen Physik als selbstverständlich angesehene Annahme der Separierbarkeit physikalischer Systeme aufgeben oder unseren Begriff der physikalischen Realität revidieren. Eine Untersuchung des Begriffs der Separabilität und einige Überlegungen zum Problem der Messung von Observablen zeigen, daß eine Änderung des Begriffs der physikalischen Realität unumgänglich ist. Der revidierte Realitätsbegriff sollte mit klassischer Physik und Quantenmechanik verträglich sein, um ein einheitliches Weltbild zu ermöglichen.Translated AbstractDo Quantum Mechanics Force us to Drastically Change our View of the World? Thoughts and Experiments after Einstein, Podolsky and RosenSince the advent of quantum mechanics there have been attempts of its interpretation in terms of statistical theory concerning individual classical systems. The very conditions necessary to consider hidden variable theories describing these individual systems as classical had been pointed out by Einstein, Podolsky and Rosen in 1935: 1. Physical systems are in principle separable. 2. If it is possible to predict with certainty the value of a physical quantity without disturbing the system under consideration, then there exists an element of physical reality corresponding to this physical quantity.Together they are, as was shown by Bell in 1964, incompatible in principle with quantum mechanics and no more tenable in view of recent experiments. These experiments once more corroborate quantum theory. In order to understand their results we are forced either to drop the assumption of separability of physical systems (taken for self-evident in classical physics) or to change our concept of physical reality. After investigating the notion of separability and connecting the EPR-correlations to the measurement problem we, conclude that a change of the concept of physical reality is indispensable. The revised concept should be compatible with both classical and quantum physics in order to allow a uniform view of the physical world.

Determining Ocean-Bottom Seismometer Orientations from the RHUM-RUM experiment from P-wave and Rayleigh wave polarizations

NASA Astrophysics Data System (ADS)

Scholz, John-Robert; Barruol, Guilhem; Fontaine, Fabrice R.; Sigloch, Karin

2016-04-01

To image the upper mantle structure beneath La Réunion hotspot, a large-scale seismic network has been deployed on land and at sea in the frame of the RHUM-RUM project (Réunion Hotspot and Upper Mantle - Réunions Unterer Mantel). This French-German passive seismic experiment was designed to investigate and image the deep structure beneath La Réunion, from crust to core, to precise the shape and depth origin of a mantle plume, if any, and to precise the horizontal and vertical mantle flow associated to a possible plume upwelling, to its interaction with the overlying plate and with the neighboring Indian ridges. For this purpose, 57 Ocean-Bottom Seismometers (OBS) were installed around La Réunion and along the Central and Southwest Indian ridges. Broad-band instruments were deployed with the French R/V Marion Dufresne in late 2012 (cruise MD192), and recovered 13 months later by the German R/V Meteor (cruise M101). The pool of OBS was complemented by ~60 terrestrial stations, installed on different islands in the western Indian Ocean, such as La Réunion, Madagascar, Mauritius, Seychelles, Mayotte and the Îles Éparses in the Mozambique channel. The OBS installation is a free-fall down to the seafloor, where they landed in an unknown orientation. Since seismologic investigations of crustal and upper mantle structure (e.g., receiver functions) and azimuthal anisotropy (e.g., SKS-splitting and Rayleigh waves) rely on the knowledge of the correct OBS orientation with respect to the geographic reference frame, it is of importance to determine the orientations of the OBS while recording on the seafloor. In an isotropic, horizontally homogeneous and non-dipping layered globe, the misorientation of each station refers to the offset between theoretical and recorded back-azimuth angle of a passive seismic event. Using large earthquakes (MW > 5.0), it is possible to establish multiple successful measurements per station and thus to determine with good confidence the sensor orientations. In this study, we analyzed particle motions of P-waves (P-pol) and of Rayleigh waves (R-pol) to quantify the orientation of each of the 57 OBS. We performed 213 polarization measurements based on 35 earthquakes for P-pol, and 381 polarization measurements based on 48 earthquakes for R-pol. This allowed us to successfully determine the North/South orientations for 40 out of 57 OBS: 13 stations were devoid of usable data and 4 stations were too noisy. From twice the standard deviation (95% confidence interval), we estimate the errors between 1° and 20°.

Dynamic modelling and humus balances as tools for estimating and upscaling soil carbon stock changes in temperate cropland

NASA Astrophysics Data System (ADS)

Oberholzer, Hans-Rudolf; Holenstein, Hildegard; Mayer, Jochen; Leifeld, Jens

2010-05-01

Humus balances are simple mathematical tools used by farmers for assessing the overall performance of their management in terms of soil organic matter changes. They are based on humus reproduction factors which themselves mainly depend on crop rotation, residue management, and amount and type of organic fertilization. Dynamic models, on the other hand, are typically complex and need more detailed input data and are designed to calculate the time course of soil carbon content. In both cases, thorough validation is needed to utilize their potential for estimating carbon stock changes. We compared the results of three humus balance methods SALCA-SQ (Neyroud 1997), VDLUFA method (VDLUFA 2004), Humod (Brock et al. 2008) and the RothC model with measured soil carbon stocks in a long-term experiment in Switzerland for the period 1977-2005 (Fliessbach et al 2007). The field trial comprises various minerally and organically fertilized treatments, the latter differing in the amount and composition of organics applied. All methods were able to distinguish systematic management effects on soil organic carbon (SOC). However, only those SOC trajectories calculated with the dynamic model RothC matched measured stocks quantitatively. For both, humus balances and dynamic modelling the result strongly depended on parameterization of organic fertilizers, i.e. its stability and organic matter content. Therefore, incomplete information on the amount and composition of organic fertilizer and lack of knowledge about its potential for humus reproduction is regarded an uncertainty in both dynamic modelling and humus balance calculation, and seems to be a major drawback for the reliable application of these approaches at the regional scale. Our results stress the need for more detailed and harmonized data bases of organic fertilizer composition and application rates. References Brock C., Hoyer U., Leithold G., Hülsbergen K.-J., 2008. Entwicklung einer praxisanwendbaren Methode der Humusbilanzierung im ökologischen Landbau. Abschlussbericht zum Projekt 03OE084, http://forschung.oekolandbau.de unter der BÖL-Bericht-ID 16447,184 pp. Fliessbach A, Oberholzer H.-R., Gunst L., Mäder P., 2007. Soil organic matter and biological soil quality indicators after 21 years of organic and conventional farming. Agriculture, Ecosystems and Environment 118, 273-284. Leifeld J., Reiser R., Oberholzer H.-R., 2009. Consequences of conventional vs. organic farming on soil carbon: Results from a 27-year field experiment. Agronomy Journal 101, 1204-1218. Neyroud J.-A., 1997. La part du sol dans la production intégrée 1. Gestion de la matière organique et bilan humique. Revue suisse d'agriculture, 29, 45-51. VDLUFA, 2004. VDLUFA-Standpunkt: Humusbilanzierung - Methode zur Beurteilung und Bemessung der Humusversorgung von Ackerland. Verband Deutscher Landwirtschaftlicher Untersuchungs- und Forschungsanstalten, Selbstverlag.

[Not Available].

PubMed

Hainschitz, I; Rieger, K; Siegl, H

2002-06-01

In Austria an index of 3 μg/kg of Ochratoxin A for coffee, 0,3 μg/kg for fruit juices and 0,2 μg/kg for beer is discussed. The laboratory of the food inspection authority of the state of Vorarlberg investigated the contribution of selected foodstuffs to the daily OTA intake and compared it with the recommendation of the scientific food committee of the EC. The focal point of this study was on beverages (coffee, coffee substitutes, beer and fruit juices) and their ingredients.ZUSAMMENFASSUNG: Die Untersuchungsergebnisse von Bier, Fruchtsaft und Kaffee [Diagramm 1] zeigen, dass die Mehrzahl der Proben nur sehr schwach bis gar nicht belastet waren. Die OTA-Belastung lag bei der Mehrzahl der Proben unter der Nachweisgrenze von 0,3 μg/kg bzw. 0,01μg/1. Einzelne Proben waren aber erheblich belastet, sodass bei starkem Konsum (Fruchtsaft im Sommer) eine überschreitung der vom SCF vorgeschlagenen Höchstmenge nicht auszuschließen ist. Die Ergebnisse der Kaffeemitteluntersuchung [Diagramm 2] belegen eine höhere OTA-Belastung bei mehr als der Hälfte der Proben. Wenn die vom SCF vorgeschlagene Höchstaufnahme von 5 ng pro Tag und kg Körpergewicht zu Grunde gelegt wird, resultiert für eine 60 kg schwere Person ein Wert von 0,3 μg/Tag. Das bedeutet bei einem mit 100 μg/kg OTA kontaminierten Kaffeeersatz und dem Konsum nur einer Tasse (5 - 7 g Pulver), dass alleine aus dieser Quelle diese Höchstaufnahme deutlich überschritten wird. Der Eintrag über die restliche Nahrung wie Cerealien, die für etwa die Hälfte der OTA-Aufnahme verantwortlich sind, bleibt hier unberücksichtigt. Die Untersuchungen belegen, dass die Einhaltung der in österreich vorgeschlagenen Richtwerte bei Bier, Fruchtsäften und Kaffee keine Schwierigkeiten bereitet. Für Kaffeemittel und andere Trockenfrüchte als Weintrauben [3] wurde allerdings noch kein Richtwert vorgeschlagen. Die Ergebnisse belegen aber, dass gerade für Kaffemittel und verschiedene Trockenfrüchte vor dem Hintergrund fehlender Höchstwerte ein Richtwert in der Größenordnung von 3 μg/kg bzw. 10 μg/kg hilfreich wäre, bis die Festlegung der gemeinschaftsrechtlicher Höchstgehalte erfolgt. Mit Hinblick auf die in der Einleitung beschriebene toxische Wirkung von OTA ist es im Sinne eines vorbeugenden Verbraucherschutzes wichtig, diese hochbelasteten Chargen zu erkennen und aus dem Verkehr zu nehmen. Ursache für die OTA-Kontamination ist vor allem eine mangelhafte Produktionshygiene in den Erzeugerländern. Dort liegt auch das größte Potential für eine Verringerung der OTA-Belastung. Die überprüfung der Lebensmittel auf Ochratoxin A durch die amtliche Lebensmittelkontrolle ist ein notwendiger Beitrag zum Schutz der öffentlichen Gesundheit und zur weiteren Reduktion der Aufnahme.

Experiments on Nucleation in Different Flow Regimes

NASA Technical Reports Server (NTRS)

Bayuzick, R. J.; Hofmeister, W. H.; Morton, C. M.; Robinson, M. B.

1998-01-01

The vast majority of metallic engineering materials are solidified from the liquid phase. Understanding the solidification process is essential to control microstructure, which in turn, determines the properties of materials. The genesis of solidification is nucleation, where the first stable solid forms from the liquid phase. Nucleation kinetics determine the degree of undercooling and phase selection. As such, it is important to understand nucleation phenomena in order to control solidification or glass formation in metals and alloys. Early experiments in nucleation kinetics were accomplished by droplet dispersion methods. Dilitometry was used by Turnbull and others, and more recently differential thermal analysis and differential scanning calorimetry have been used for kinetic studies. These techniques have enjoyed success; however, there are difficulties with these experiments. Since materials are dispersed in a medium, the character of the emulsion/metal interface affects the nucleation behavior. Statistics are derived from the large number of particles observed in a single experiment, but dispersions have a finite size distribution which adds to the uncertainty of the kinetic determinations. Even though temperature can be controlled quite well before the onset of nucleation, the release of the latent heat of fusion during nucleation of particles complicates the assumption of isothermality during these experiments. Containerless processing has enabled another approach to the study of nucleation kinetics. With levitation techniques it is possible to undercool one sample to nucleation repeatedly in a controlled manner, such that the statistics of the nucleation process can be derived from multiple experiments on a single sample. The authors have fully developed the analysis of nucleation experiments on single samples following the suggestions of Skripov. The advantage of these experiments is that the samples are directly observable. The nucleation temperature can be measured by noncontact optical pyrometry, the mass of the sample is known, and post-processing analysis can be conducted on the sample. The disadvantages are that temperature measurement must have exceptionally high precision, and it is not possible to isolate specific heterogeneous sites as in droplet dispersions. Levitation processing of refractory materials in ultra high vacuum provides an avenue to conduct these kinetic studies on single samples. Two experimental methods have been identified where ultra high vacuum experiments are possible; electrostatic levitation in ground-based experiments and electromagnetic processing in low earth orbit on TEMPUS. Such experiments, reported here, were conducted on zirconium. Liquid zirconium is an excellent solvent and has a high solubility for contaminants contained in the bulk material as well as those contaminants found in the vacuum environment. Oxides, nitrides, and carbides do not exist in the melt, and do not form on the surface of molten zirconium, for the materials and vacuum levels used in this study. Ground-based experiments with electrostatic levitation have shown that the statistical nucleation kinetic experiments are viable and yield results which are consistent with classical nucleation theory. The advantage of low earth orbit experiments is the ability to vary the flow conditions in the liquid prior to nucleation. The put-pose of nucleation experiments in TEMPUS was to examine.

Mixtures of Bosonic and Fermionic atoms

NASA Astrophysics Data System (ADS)

Albus, Alexander

2003-12-01

The theory of atomic Boson-Fermion mixtures in the dilute limit beyond mean-field is considered in this thesis. Extending the formalism of quantum field theory we derived expressions for the quasi-particle excitation spectra, the ground state energy, and related quantities for a homogenous system to first order in the dilute gas parameter. In the framework of density functional theory we could carry over the previous results to inhomogeneous systems. We then determined to density distributions for various parameter values and identified three different phase regions: (i) a stable mixed regime, (ii) a phase separated regime, and (iii) a collapsed regime. We found a significant contribution of exchange-correlation effects in the latter case. Next, we determined the shift of the Bose-Einstein condensation temperature caused by Boson-Fermion interactions in a harmonic trap due to redistribution of the density profiles. We then considered Boson-Fermion mixtures in optical lattices. We calculated the criterion for stability against phase separation, identified the Mott-insulating and superfluid regimes both, analytically within a mean-field calculation, and numerically by virtue of a Gutzwiller Ansatz. We also found new frustrated ground states in the limit of very strong lattices. ----Anmerkung: Der Autor ist Träger des durch die Physikalische Gesellschaft zu Berlin vergebenen Carl-Ramsauer-Preises 2004 für die jeweils beste Dissertation der vier Universitäten Freie Universität Berlin, Humboldt-Universität zu Berlin, Technische Universität Berlin und Universität Potsdam. Ziel der Arbeit war die systematische theoretische Behandlung von Gemischen aus bosonischen und fermionischen Atomen in einem Parameterbereich, der sich zur Beschreibung von aktuellen Experimenten mit ultra-kalten atomaren Gasen eignet. Zuerst wurde der Formalismus der Quantenfeldtheorie auf homogene, atomare Boson-Fermion Gemische erweitert, um grundlegende Größen wie Quasiteilchenspektren, die Grundzustandsenergie und daraus abgeleitete Größen über die Molekularfeldtheorie hinaus zu berechnen. Unter Zuhilfenahme der dieser Resultate System wurde ein Boson-Fermion Gemisch in einem Fallenpotential im Rahmen der Dichtefunktionaltheorie beschrieben. Daraus konnten die Dichteprofile ermittelt werden und es ließen sich drei Bereiche im Phasendiagramm identifizieren: (i) ein Bereich eines stabilen Gemisches, (ii) ein Bereich, in dem die Spezies entmischt sind und (iii) ein Bereich, in dem das System kollabiert. Im letzten dieser drei Fällen waren Austausch--Korrelationseffekte signifikant. Weiterhin wurde die Änderung der kritischen Temperatur der Bose-Einstein-Kondensation aufgrund der Boson-Fermion-Wechselwirkung berechnet. Verursacht wird dieser Effekt von Dichtumverteilungen aufgrund der Wechselwirkung. Dann wurden Boson-Fermion Gemische in optischen Gittern betrachtet. Ein Stabilitätskriterium gegen Phasenentmischung wurde gefunden und es ließen sich Bedingungen für einen supraflüssig zu Mott-isolations Phasenübergang angeben. Diese wurden sowohl mittels einer Molekularfeldrechnung als auch numerisch im Rahmen eines Gutzwilleransatzes gefunden. Es wurden weiterhin neuartige frustrierte Grundzustände im Fall von sehr großen Gitterstärken gefunden.

RHUM-RUM investigates La Réunion mantle plume from crust to core

NASA Astrophysics Data System (ADS)

Sigloch, Karin; Barruol, Guilhem

2013-04-01

RHUM-RUM (Réunion Hotspot and Upper Mantle - Réunions Unterer Mantel) is a French-German passive seismic experiment designed to image an oceanic mantle plume - or lack of plume - from crust to core beneath La Réunion Island, and to understand these results in terms of material, heat flow and plume dynamics. La Réunion hotspot is one of the most active volcanoes in the world, and its hotspot track leads unambiguously to the Deccan Traps of India, one of the largest flood basalt provinces on Earth, which erupted 65 Ma ago. The genesis and the origin at depth of the mantle upwelling and of the hotspot are still very controversial. In the RHUM-RUM project, 57 German and French ocean-bottom seismometers (OBS) are deployed over an area of 2000 km x 2000 km2 centered on La Réunion Island, using the "Marion Dufresne" and "Meteor" vessels. The one-year OBS deployment (Oct. 2012 - Oct. 2013) will be augmented by terrestrial deployments in the Iles Eparses in the Mozambique Channel, in Madagascar, Seychelles, Mauritius, Rodrigues and La Réunion islands. A significant number of OBS will be also distributed along the Central and South West Indian Ridges to image the lower-mantle beneath the hotspot, but also to provide independent opportunity for the study of these slow to ultra-slow ridges and of possible plume-ridge interactions. RHUM-RUM aims to characterize the vertically ascending flow in the plume conduit, as well as any lateral flow spreading into the asthenosphere beneath the western Indian Ocean. We want to establish the origin of the heat source that has been fueling this powerful hotspot, by answering the following questions: Is there a direct, isolated conduit into the deepest mantle, which sources its heat and material from the core-mantle boundary? Is there a plume connection to the African superswell at mid-mantle depths? Might the volcanism reflect merely an upper mantle instability? RHUM-RUM also aims at studying the hotspot's interaction with the neighboring ridges of the Indian Ocean. There is in particular a long-standing hypothesis, not yet examined seismically, that channelized plume flow beneath the aseismic Rodrigues Ridge could feed the Central Indian Ridge at 1000 km distance. The RHUM-RUM group (www.rhum-rum.net): * IPG Paris & Géosciences Réunion: G. Barruol, J.P. Montagner, E. Stutzmann, F.R. Fontaine, C. Deplus, M. Cannat, G. Roult, J. Dyment, S. Singh, W. Crawford, C. Farnetani, N. Villeneuve, L. Michon. V. Ferrazzini, Y. Capdeville. * Univ. Munich (LMU): K. Sigloch, H. Igel. AWI Bremerhaven: V. Schlindwein. Univ. Frankfurt: G. Rümpker. Univ. Münster: C. Thomas. Univ. Bonn: S. Miller. * Géosciences Montpellier: C. Tiberi, A. Tommasi, D. Arcay, C. Thoraval. * Mauritius Oceanography Institute: D. Bissessur. Univ. Antananarivo: G. Rambolamanana. SEYPEC Seychelles Petroleum: P. Samson, P. Joseph. * Other institutes: A. Davaille, M. Jegen, M. Maia, G. Nolet, D. Sauter, B. Steinberger.

RHUM-RUM investigates La Réunion mantle plume from crust to core

NASA Astrophysics Data System (ADS)

Sigloch, K.; Barruol, G.

2012-12-01

RHUM-RUM (Réunion Hotspot and Upper Mantle - Réunions Unterer Mantel) is a French-German passive seismic experiment designed to image an oceanic mantle plume - or lack of plume - from crust to core beneath La Réunion Island, and to understand these results in terms of material, heat flow and plume dynamics. La Réunion hotspot is one of the most active volcanoes in the world, and its hotspot track leads unambiguously to the Deccan Traps of India, one of the largest flood basalt provinces on Earth, which erupted 65 Ma ago. The genesis and the origin at depth of the mantle upwelling and of the hotspot are still very controversial. In the RHUM-RUM project, 57 German and French ocean-bottom seismometers (OBS) are deployed over an area of 2000 km x 2000 km2 centered on La Réunion Island, using the "Marion Dufresne" and "Meteor" vessels. The one-year OBS deployment (Oct. 2012 - Oct. 2013) will be augmented by terrestrial deployments in the Iles Eparses in the Mozambique Channel, in Madagascar, Seychelles, Mauritius, Rodrigues and La Réunion islands. A significant number of OBS will be also distributed along the Central and South West Indian Ridges to image the lower-mantle beneath the hotspot, but also to provide independent opportunity for the study of these slow to ultra-slow ridges and of possible plume-ridge interactions. RHUM-RUM aims to characterize the vertically ascending flow in the plume conduit, as well as any lateral flow spreading into the asthenosphere beneath the western Indian Ocean. We want to establish the origin of the heat source that has been fueling this powerful hotspot, by answering the following questions: Is there a direct, isolated conduit into the deepest mantle, which sources its heat and material from the core-mantle boundary? Is there a plume connection to the African superswell at mid-mantle depths? Might the volcanism reflect merely an upper mantle instability? RHUM-RUM also aims at studying the hotspot's interaction with the neighboring ridges of the Indian Ocean. There is in particular a long-standing hypothesis, not yet examined seismically, that channelized plume flow beneath the aseismic Rodrigues Ridge could feed the Central Indian Ridge at 1000 km distance. The RHUM-RUM group (www.rhum-rum.net): * IPG Paris & Géosciences Réunion: G. Barruol, J.P. Montagner, E. Stutzmann, F.R. Fontaine, C. Deplus, M. Cannat, G. Roult, J. Dyment, S. Singh, W. Crawford, C. Farnetani, N. Villeneuve, L. Michon. V. Ferrazzini, Y. Capdeville. * Univ. Munich (LMU): K. Sigloch, H. Igel. AWI Bremerhaven: V. Schlindwein. Univ. Frankfurt: G. Rümpker. Univ. Münster: C. Thomas. Univ. Bonn: S. Miller. * Géosciences Montpellier: C. Tiberi, A. Tommasi, D. Arcay, C. Thoraval. * Mauritius Oceanography Institute: D. Bissessur. Univ. Antananarivo: G. Rambolamanana. SEYPEC Seychelles Petroleum: P. Samson, P. Joseph. * Other institutes: A. Davaille, M. Jegen, M. Maia, G. Nolet, D. Sauter, B. Steinberger.

Grain Oriented Perovskite Layer Structure Ceramics for High-Temperature Piezoelectric Applications

NASA Astrophysics Data System (ADS)

Fuierer, Paul Anton

The perovskite layer structure (PLS) compounds have the general formula (A^{2+}) _2(B^{5+})_2 O_7, or (A^ {3+})_2(B^{4+ })_2O_7, and crystallize in a very anisotropic layered structure consisting of parallel slabs made up of perovskite units. Several of these compounds possess the highest Curie temperatures (T_{rm c} ) of any known ferroelectrics. Two examples are Sr_2Nb_2O _7 with T_{rm c} of 1342^circC, and La_2Ti_2O _7 with T_{rm c} of 1500^circC. This thesis is an investigation of PLS ceramics and their feasibility as a high temperature transducer material. Piezoelectricity in single crystals has been measured, but the containerless float zone apparatus necessary to grow high quality crystals of these refractory compounds is expensive and limited to a small number of research groups. Previous attempts to pole polycrystalline Sr_2Nb _2O_7 have failed, and to this point piezoelectricity has been absent. The initiative taken in this research was to investigate PLS ceramics by way of composition and processing schemes such that polycrystalline bodies could be electrically poled. The ultimate objective then was to demonstrate piezoelectricity in PLS ceramics, especially at high temperatures. Donor-doping of both La_2Ti _2O_7 and Sr_2Nb_2O _7 was found to increase volume resistivities at elevated temperatures, an important parameter to consider during the poling process. Sr_2Ta _2O_7 (T _{rm c} = -107 ^circC) was used to make solid solution compositions with moderately high Curie temperatures, of about 850^circC, and lower coercive fields. A hot-forging technique was employed to produce ceramics with high density (>99% of theoretical) and high degree of grain orientation (>90%). Texturing was characterized by x-ray diffraction and microscopy. Considerable anisotropy was observed in physical and electrical properties, including thermal expansion, resistivity, dielectric constant, and polarization. The direction perpendicular to the forging axis proved to be the ferroelectric "easy" direction, indicating that the polar axis lies in the plane of the plate-like grains. Hot-forged samples were poled at 40 to 50 KV/cm at 200^circC. Several compounds in the La_2Ti_2O _7-Sr_2Nb _2O_7-Sr _2Ta_2O_7 ternary system were shown to be piezoelectric. From appropriately oriented cuts, the dielectric, elastic, and piezoelectric coefficients were determined by the resonance method. Relative to commercial piezoelectric ceramics such as Pb(ZrTi)O_3, hot-forged PLS ceramics were found to have high frequency constants, low compliance, low electromechanical coupling, low piezoelectric coefficients, and high mechanical quality factors. For Sr_2(Nb_{0.5 }Ta_{0.5})_2 O_7, N_{32 } = 2216 Hz-m, s_{32} = 8.37 times 10^ {-12} m^2/N, k _{32} = 3.60%, d _{32} = 2.40 pC/N, and Q _{rm m} = 5290. This material was also shown to resist depoling when exposed to temperatures as high as 650^circC. Hot-forged PLS compounds offer a new family of ferroelectric ceramics that may prove to be useful as high temperature materials for electronic transducers or filters.

Isolation of iron bacteria from terrestrial and aquatic environments

NASA Astrophysics Data System (ADS)

Schmidt, Bertram; Szewzyk, Ulrich

2010-05-01

Bacteria, which are capable of iron oxidation or at least iron deposition are widely distributed in environments where zones of dissolved ferrous iron and oxygen gradients are overlapping [1]. They take part in the biological cycling of iron and influence other cycles of elements for example carbon [2]. Manganese can be used for similar metabolic purposes as iron, because it can be biologically oxidized by chemolithotrophs or can be reduced by respirating bacteria as well [3, 4]. Bacterial activity is responsible for the accumulation of ferric iron compounds in their surroundings. The formation of bog ore is a well known example for a soil horizon, with an extreme enrichment of biogenic ferric iron [5]. We focused on the isolation of neutrophilic iron bacteria and bacteria capable of manganese oxidation. We used samples from Tierra del Fuego (Argentina) the National Park "Unteres Odertal" (Germany) and Berlin ground water wells. Microscopic examination of the samples revealed a considerable diversity of iron encrusted structures of bacterial origin. Most of these morphologic types are already well known. The taxonomic classification of many of these organisms is based on morphologic features and is not reliable compared to recent methods of molecular biology. That is mainly due to the fact, that most of these bacteria are hardly culturable or do not show their characteristic morphologic features under culture conditions. We established a collection of more than 300 iron depositing strains. Phylogenetic analyses showed that we have many yet uncultured strains in pure culture. We obtained many isolates which form distinct branches within long known iron bacteria groups like the Sphaerotilus-Leptothrix cluster. But some of the strains belong to groups, which have not yet been associated with iron oxidation activity. The strains deposit high amounts of oxidized iron and manganese compounds under laboratory conditions. However it is unclear if these precipitations are due to biological oxidation or biological deposition of chemically oxidized iron. We examined the morphologic characteristics of selected isolates under near-natural conditions to assign them to morphologic structures which occur in native samples. Our aim for the future is to describe several strains. References: [1] Weber, K. A. ; Achenbach, L. A. ; Coates, J. D. : Microorganisms pumping iron: anaerobic microbial iron oxidation and reduction. In: Nature Reviews Microbiology 4 (2006) 752-764 [2] Van Capellen, P. ; Wang Y. : Cycling of iron and manganese in surface sediments: a general theory for the coupled transport and reaction of carbon, oxygen, nitrogen, sulfur, iron and manganese. In: American Journal of Science 296 (1996) 197-243 [3] Tebo, B. M. ; Bargar, J. R. ; Clement, B. G. ; Dick, G. J. ; Murray, K. J. ; Parker, D. Verity R. ; Webb, S. M. : Biogenic manganese oxides: properties and mechanisms of formation. In: Annual Reviews Earth Planet Science 32 (2004) 287-328 [4] Erlich, H. L. : Manganese oxide reduction as a form of anaerobic respiration. In: Geomicrobiology Journal 5 (1987) 423-431 [5] Ghiorse W. C. : Biology of iron- and manganese-depositing bacteria. In: Annual Reviews 38 (1984) 515-550

On a class of Newton-like methods for solving nonlinear equations

NASA Astrophysics Data System (ADS)

Argyros, Ioannis K.

2009-06-01

We provide a semilocal convergence analysis for a certain class of Newton-like methods considered also in [I.K. Argyros, A unifying local-semilocal convergence analysis and applications for two-point Newton-like methods in Banach space, J. Math. Anal. Appl. 298 (2004) 374-397; I.K. Argyros, Computational theory of iterative methods, in: C.K. Chui, L. Wuytack (Eds.), Series: Studies in Computational Mathematics, vol. 15, Elsevier Publ. Co, New York, USA, 2007; J.E. Dennis, Toward a unified convergence theory for Newton-like methods, in: L.B. Rall (Ed.), Nonlinear Functional Analysis and Applications, Academic Press, New York, 1971], in order to approximate a locally unique solution of an equation in a Banach space. Using a combination of Lipschitz and center-Lipschitz conditions, instead of only Lipschitz conditions [F.A. Potra, Sharp error bounds for a class of Newton-like methods, Libertas Math. 5 (1985) 71-84], we provide an analysis with the following advantages over the work in [F.A. Potra, Sharp error bounds for a class of Newton-like methods, Libertas Math. 5 (1985) 71-84] which improved the works in [W.E. Bosarge, P.L. Falb, A multipoint method of third order, J. Optimiz. Theory Appl. 4 (1969) 156-166; W.E. Bosarge, P.L. Falb, Infinite dimensional multipoint methods and the solution of two point boundary value problems, Numer. Math. 14 (1970) 264-286; J.E. Dennis, On the Kantorovich hypothesis for Newton's method, SIAM J. Numer. Anal. 6 (3) (1969) 493-507; J.E. Dennis, Toward a unified convergence theory for Newton-like methods, in: L.B. Rall (Ed.), Nonlinear Functional Analysis and Applications, Academic Press, New York, 1971; H.J. Kornstaedt, Ein allgemeiner Konvergenzstaz fü r verschä rfte Newton-Verfahrem, in: ISNM, vol. 28, Birkhaü ser Verlag, Basel and Stuttgart, 1975, pp. 53-69; P. Laasonen, Ein überquadratisch konvergenter iterativer algorithmus, Ann. Acad. Sci. Fenn. Ser I 450 (1969) 1-10; F.A. Potra, On a modified secant method, L'analyse numérique et la theorie de l'approximation 8 (2) (1979) 203-214; F.A. Potra, An application of the induction method of V. Pták to the study of Regula Falsi, Aplikace Matematiky 26 (1981) 111-120; F.A. Potra, On the convergence of a class of Newton-like methods, in: Iterative Solution of Nonlinear Systems of Equations, in: Lecture Notes in Mathematics, vol. 953, Springer-Verlag, New York, 1982; F.A. Potra, V. Pták, Nondiscrete induction and double step secant method, Math. Scand. 46 (1980) 236-250; F.A. Potra, V. Pták, On a class of modified Newton processes, Numer. Funct. Anal. Optim. 2 (1) (1980) 107-120; F.A. Potra, Sharp error bounds for a class of Newton-like methods, Libertas Math. 5 (1985) 71-84; J.W. Schmidt, Untere Fehlerschranken für Regula-Falsi Verfahren, Period. Math. Hungar. 9 (3) (1978) 241-247; J.W. Schmidt, H. Schwetlick, Ableitungsfreie Verfhren mit höherer Konvergenzgeschwindifkeit, Computing 3 (1968) 215-226; J.F. Traub, Iterative Methods for the Solution of Equations, Prentice Hall, Englewood Cliffs, New Jersey, 1964; M.A. Wolfe, Extended iterative methods for the solution of operator equations, Numer. Math. 31 (1978) 153-174]: larger convergence domain and weaker sufficient convergence conditions. Numerical examples further validating the results are also provided.

Modelling Seasonal Carbon Dynamics on Fen Peatlands

NASA Astrophysics Data System (ADS)

Giebels, Michael; Beyer, Madlen; Augustin, Jürgen; Roppel, Mario; Juszczak, Radoszlav; Serba, Tomasz

2010-05-01

In Germany more than 99 % of fens have lost their carbon and nutrient sink function due to heavy drainage and agricultural land use especially during the last decades and thus resulted in compression and heavy peat loss (CHARMAN 2002; JOOSTEN & CLARKE 2002; SUCCOW & JOOSTEN 2001; AUGUSTIN et al. 1996; KUNTZE 1993). Therefore fen peatlands play an important part (4-5 %) in the national anthropogenic trace gas budget. But only a small part of drained and agricultural used fens in NE Germany can be restored. Knowledge of the influence of land use to trace gas exchange is important for mitigation of the climate impact of the anthropogenic peatland use. We study carbon exchanges between soil and atmosphere on several fen peatland use areas at different sites in NE-Germany. Our research covers peatlands of supposed strongly climate forcing land use (cornfield and intensive pasture) and of probably less forcing, alternative types (meadow and extensive pasture) as well as rewetted (formerly drained) areas and near-natural sites like a low-degraded fen and a wetted alder woodland. We measured trace gas fluxes with manual and automatic chambers in periodic routines since spring 2007. The used chamber technique bases on DROESLER (2005). In total we now do research at 22 sites situated in 5 different locations covering agricultural, varying states of rewetted and near-natural treatments. We present results of at least 2 years of measurements on our site of varying types of agricultural land use. There we found significant differences in the annual carbon balances depending on the genesis of the observed sites and the seasonal dynamics. Annual balances were constructed by applying single respiration and photosynthesis CO2 models for each measurement campaign. These models were based on LLOYD-TAYLOR (1994) and Michaelis-Menten-Kinetics respectively. Crosswise comparison of different site treatments combined with the seasonal environmental observations give good hints for the identification of main flux driving parameters. Based on this procedure we developed a specific methane efflux model, mainly driven by the observed groundwater fluctuation and soil temperature. Depending on the observed timescale initial starting points of the model showed up to be remarkably different. We also will present suggestions for an advanced CO2 modelling as the present approaches are both based on single parameters. Generally our experiences from our field studies show that mono-parameterized models often fail in reproducing measured flux values. References: Augustin, J., Merbach, W., Käding, H., Schnidt, W. & Schalitz, G. 1996. Lachgas- und Methanemissionen aus degradierten Niedermoorstandorten Nordostdeutschlands unter dem Einfluß unterschiedlicher Bewirtschaftung. Alfed-Wegener-Stiftung (ed.): Von den Ressourcen zum Recycling: Geoanalytik-Geomanagement-Geoinformatik. Ernst & Sohn Verlag. Berlin Charman, D. 2002: Peatland and environmental change. John Wiley & Sons, LTD, Chichester Droesler, M. 2005. Trace Gas Exchange and climatic relevance of bog ecosystems, Southern Germany, phD-thesis, TU München, München Joosten, H. & Clarke, D. 2002: Wise use of mires and peatlands-background and principles including a framework for decision-making. International Mire Conservation Group and International Peat Society (eds.), Finland Kuntze 1993: Moore als Senken und Quellen für C und N, Mitt. Deutsche Bodenkundliche Gesellschaft 69, 277-280 Lloyd, J., Taylor, J. A. 1994. On the Temperature Dependence of Soil Respiration, Functional Ecology, Vol. 8, No. 3, pp. 315-323 Succow, M. & Joosten, H. 2001: Landschaftsökologische Moorkunde, 2nd edition, Schweizerbart'sche Verlagsbuchhandlung, Stuttgart

Desiccation tolerance of iron bacteria biofilms on Mars regolith simulants

NASA Astrophysics Data System (ADS)

Feyh, Nina; Szewzyk, Ulrich

2010-05-01

Iron oxidizing bacteria play an important role in the geological redox cycling of iron on earth. The redox change between Fe(II) and Fe(III) can be used for biological energy production [1]. Therefore iron oxidation in the iron rich martian soils may be or may have been microbially mediated. The microbial conversion of iron is considered to be an ancient form of metabolism [2], so it might have evolved on Mars as well. However, to exist in recent martian soils, bacteria must be able to endure dry and cold conditions. Neutrophilic iron oxidizers can be found in various iron rich aquatic environments, where they lead to the precipitation of insoluble ferric hydroxides. Some of these environments fall temporarily dry, what could have led to an adaptation to desiccation by bacteria, existing there. One strategy of iron bacteria to endure drought stress might be the formation of biofilms by excreting Extracellular Polymeric Substances (EPS). The deposition of iron hydroxides could enable them to endure dry conditions as well. For our experiments, neutrophilic iron oxidizing bacteria have been isolated from a creek in Bad Salzhausen/Hesse and temporarily drying out pools in Tierra del Fuego. Strains from aquatic environments in the national park "Unteres Odertal" and from water wells in Berlin/Brandenburg are included in the tests as well. In desiccation experiments, the capability of iron bacteria to tolerate dry conditions are investigated. The aim of our first experiment is the adaptation to dry conditions. Biofilms of 15 strains are grown on ceramic beads in liquid medium containing complexed Fe(II), established biofilms contain Fe(III) precipitates. The cultures are desiccated in a sterile airflow until the weight of the cultures remained constant. After a desiccation period of 9 h up to 7 d, the beads are transferred to fresh liquid medium. Adapted strains are used in further desiccation experiments, where biofilms are grown on two martian regolith simulants. These mineral mixtures were developed and produced by the Naturkundemuseum Berlin according to recent data of Mars research missions [3, 4, 5, 6, 7]. The minerals are attached to object slides with potassium silicate and biofilms are grown on the mineral surface. The biofilms are quantified by cell counting and the structure is evaluated by epifluorescence microscopy. After desiccation in a sterile airflow, the survival of cells is determined by fluorescence staining. Acknowledgements This research was supported by the Helmholtz Association through the research alliance "Planetary Evolution and Life". References [1] Weber, K. A. et al. (2006). Microorganisms pumping iron: anaerobic microbial iron oxidation and reduction. Nature Reviews Microbiology 4: 752-764. [2] Vargas, M. et al. (1998). Microbiological evidence for Fe(III) reduction on early Earth. Nature 395: 65-67. [3] Bibring, J.-P., Y. Langevin, et al. (2005). Mars surface diversity as revealed by the OMEGA/Mars express observations. Science 307(5715): 1576-1581. [4] Bibring, J.-P., S. W. Squyres, et al. (2006). Merging Views on Mars. Science 313(5795): 1899-1901. [5] Chevrier, V. and P. E. Mathé (2007). Mineralogy and evolution of the surface of Mars: A review. Planetary and Space Science 55(3): 289-314. [6] McCollom, T. M. and B. M. Hynek (2005). A volcanic environment for bedrock diagenesis at Meridiani Planum on Mars. Nature 438(7071): 1129-1131. [7] Poulet, F., J. P. Bibring, et al. (2005). Phyllosilicates on Mars and implications for early martian climate. Nature 438(7068): 623-627.

Effects of strains, strain crosses and environments on additive genetic and phenotypic variances in Drosophila melanogaster.

PubMed

Noor, R R; Barker, J S; Kinghorn, B P

1993-01-12

The stability of phenotypic, additive genetic and environmental variances of thorax length of Drosophila melanogaster in pure and synthetic strains was examined in two different environments. Two pure strains from different geographic locations (Melbourne and Townsville) were used, together with three synthetic populations formed from them. The existence of differences in thorax length between the Melbourne and Townsville populations, genotype by environment interaction, and heterosis in crosses between these populations indicate that they are genetically different. Thus geographic separation can cause differences in mean thorax length of flies from different populations. Both the difference in selection histories between the two localities and drift could lead to these differences. Up to the thirty fifth generation there was no evidence of any reduction in the difference between the Melbourne and Townsville populations, in either laboratory environment. The genetic differentiation of strains therefore may be maintained over many generations under new environmental conditions. The fluctuation over generations of heterosis of thorax length is possibly caused by the fluctuation of the rate of loss of favourable epistatic interaction in crossbred genotypes in combination with natural selection effects. V(p) was significantly higher in poor than in the good environment. This higher V(p) in the poor environment is most likly due to higher non additive genetic variance. V(p) was also significantly influenced by strain. In general, V(p) values of synthetic strains were higher than those of pure strains in both environments. Finally, the additive and environmental variances of thorax length were relatively stable across strains, generations and environments. ZUSAMMENFASSUNG: Wirkung von Herkünften, Kreuzungen und Umwelten auf additiv-genetische und phänotypische Varianzen in Drosophila melanogaster Die Stabilität phänotypischer, additiv-genetischer und umweltbedingter Varianzen der Thoraxlänge von Drosophila melanogaster in reinen und synthetischen Herkünften wurde in zwei verschiedenen Umwelten überprüft. Zwei reine Herkünfte von verschiedenen Gegenden (Melboune und Townsville) wurden zusammen mit drei zwischen ihnen gebildeten synthetischen Populationen untersucht. Unterschiede in Thoraxlänge zwischen Melbourne- und Townsvilleherkünften, Genotypumweltinteraktionen und Heterosis in Kreuzungen zwischen diesen Populationen zeigen, daß sie sich genetisch unterscheiden. Die geographische Trennung kann also Unterschiede in der mittleren Thoraxlänge zur Folge haben, wobei unterschiedliche Selektionsgeschichte in beiden Gegenden und Drift dies verursachen können. Bis zur 35. Generation gab es in keinem Labormilieu einen Hinweis auf eine Reduktion der Unterschiede zwischen den beiden Populationen. Die genetische Differenz der Herkünfte erhält sich daher auch unter neuen Umweltverhältnissen über viele Generationen. Die Schwankung in Heterosis für Thoraxlänge ist möglicherweise durch Schwankungen in der Verlustrate günstiger epistatischer Interaktionswirkungen in Kreuzungsgenotypen zusammen mit natürlichen Selektionswirkungen verursacht. V(p) war durch Umweltbedingungen signifikant beeinflußt und höher in schlechtem als in gutem Milieu. Der hohe Wert in schlechtem Milieu ist wahrscheinlich auf nicht-additiv-genetische Varianz zurückzuführen. V(p) wurde auch signifikant durch Herkunft beeinflußt und Werte in synthetischen Linien waren höher Linien in beiden Milieus. Additive und umweltbedingte Varianzen waren über Linie, Generationen und Umwelt relativ stabil. 1993 Blackwell Verlag GmbH.

Containerless Ripple Turbulence

NASA Astrophysics Data System (ADS)

Putterman, Seth; Wright, William; Duval, Walter; Panzarella, Charles

2002-11-01

One of the longest standing unsolved problems in physics relates to the behavior of fluids that are driven far from equilibrium such as occurs when they become turbulent due to fast flow through a grid or tidal motions. In turbulent flows the distribution of vortex energy as a function of the inverse length scale [or wavenumber 'k'] of motion is proportional to 1/k5/3 which is the celebrated law of Kolmogorov. Although this law gives a good description of the average motion, fluctuations around the average are huge. This stands in contrast with thermally activated motion where large fluctuations around thermal equilibrium are highly unfavorable. The problem of turbulence is the problem of understanding why large fluctuations are so prevalent which is also called the problem of 'intermittency'. Turbulence is a remarkable problem in that its solution sits simultaneously at the forefront of physics, mathematics, engineering and computer science. A recent conference [March 2002] on 'Statistical Hydrodynamics' organized by the Los Alamos Laboratory Center for Nonlinear Studies brought together researchers in all of these fields. Although turbulence is generally thought to be described by the Navier-Stokes Equations of fluid mechanics the solution as well as its existence has eluded researchers for over 100 years. In fact proof of the existence of such a solution qualifies for a 1 M millennium prize. As part of our NASA funded research we have proposed building a bridge between vortex turbulence and wave turbulence. The latter occurs when high amplitude waves of various wavelengths are allowed to mutually interact in a fluid. In particular we have proposed measuring the interaction of ripples [capillary waves] that run around on the surface of a fluid sphere suspended in a microgravity environment. The problem of ripple turbulence poses similar mathematical challenges to the problem of vortex turbulence. The waves can have a high amplitude and a strong nonlinear interaction. Furthermore, the steady state distribution of energy again follows a Kolmogorov scaling law; in this case the ripple energy is distributed according to 1/k 7/4. Again, in parallel with vortex turbulence ripple turbulence exhibits intermittency. The problem of ripple turbulence presents an experimental opportunity to generate data in a controlled, benchmarked system. In particular the surface of a sphere is an ideal environment to study ripple turbulence. Waves run around the sphere and interact with each other, and the effect of walls is eliminated. In microgravity this state can be realized for over 2 decades of frequency. Wave turbulence is a physically relevant problem in its own right. It has been studied on the surface of liquid hydrogen and its application to Alfven waves in space is a source of debate. Of course, application of wave turbulence perspectives to ocean waves has been a major success. The experiment which we plan to run in microgravity is conceptually straightforward. Ripples are excited on the surface of a spherical drop of fluid and then their amplitude is recorded with appropriate photography. A key challenge is posed by the need to stably position a 10cm diameter sphere of water in microgravity. Two methods are being developed. Orbitec is using controlled puffs of air from at least 6 independent directions to provided the positioning force. This approach has actually succeeded to position and stabilize a 4cm sphere during a KC 135 segment. Guigne International is using the radiation pressure of high frequency sound. These transducers have been organized into a device in the shape of a dodecahedron. This apparatus 'SPACE DRUMS' has already been approved for use for combustion synthesis experiments on the International Space Station. A key opportunity presented by the ripple turbulence data is its use in driving the development of codes to simulate its properties.

Containerless Ripple Turbulence

NASA Technical Reports Server (NTRS)

Putterman, Seth; Wright, William; Duval, Walter; Panzarella, Charles

2002-01-01

One of the longest standing unsolved problems in physics relates to the behavior of fluids that are driven far from equilibrium such as occurs when they become turbulent due to fast flow through a grid or tidal motions. In turbulent flows the distribution of vortex energy as a function of the inverse length scale [or wavenumber 'k'] of motion is proportional to 1/k(sup 5/3) which is the celebrated law of Kolmogorov. Although this law gives a good description of the average motion, fluctuations around the average are huge. This stands in contrast with thermally activated motion where large fluctuations around thermal equilibrium are highly unfavorable. The problem of turbulence is the problem of understanding why large fluctuations are so prevalent which is also called the problem of 'intermittency'. Turbulence is a remarkable problem in that its solution sits simultaneously at the forefront of physics, mathematics, engineering and computer science. A recent conference [March 2002] on 'Statistical Hydrodynamics' organized by the Los Alamos Laboratory Center for Nonlinear Studies brought together researchers in all of these fields. Although turbulence is generally thought to be described by the Navier-Stokes Equations of fluid mechanics the solution as well as its existence has eluded researchers for over 100 years. In fact proof of the existence of such a solution qualifies for a 1 M$ millennium prize. As part of our NASA funded research we have proposed building a bridge between vortex turbulence and wave turbulence. The latter occurs when high amplitude waves of various wavelengths are allowed to mutually interact in a fluid. In particular we have proposed measuring the interaction of ripples [capillary waves] that run around on the surface of a fluid sphere suspended in a microgravity environment. The problem of ripple turbulence poses similar mathematical challenges to the problem of vortex turbulence. The waves can have a high amplitude and a strong nonlinear interaction. Furthermore, the steady state distribution of energy again follows a Kolmogorov scaling law; in this case the ripple energy is distributed according to 1/k (sup 7/4). Again, in parallel with vortex turbulence ripple turbulence exhibits intermittency. The problem of ripple turbulence presents an experimental opportunity to generate data in a controlled, benchmarked system. In particular the surface of a sphere is an ideal environment to study ripple turbulence. Waves run around the sphere and interact with each other, and the effect of walls is eliminated. In microgravity this state can be realized for over 2 decades of frequency. Wave turbulence is a physically relevant problem in its own right. It has been studied on the surface of liquid hydrogen and its application to Alfven waves in space is a source of debate. Of course, application of wave turbulence perspectives to ocean waves has been a major success. The experiment which we plan to run in microgravity is conceptually straightforward. Ripples are excited on the surface of a spherical drop of fluid and then their amplitude is recorded with appropriate photography. A key challenge is posed by the need to stably position a 10cm diameter sphere of water in microgravity. Two methods are being developed. Orbitec is using controlled puffs of air from at least 6 independent directions to provided the positioning force. This approach has actually succeeded to position and stabilize a 4cm sphere during a KC 135 segment. Guigne International is using the radiation pressure of high frequency sound. These transducers have been organized into a device in the shape of a dodecahedron. This apparatus 'SPACE DRUMS' has already been approved for use for combustion synthesis experiments on the International Space Station. A key opportunity presented by the ripple turbulence data is its use in driving the development of codes to simulate its properties.

Effects of Mineral Phosphorous Fertilization and cd Loading on cd Translocation from Soil to Corn (Zea mays L.)

NASA Astrophysics Data System (ADS)

László, Márton, ,, Dr.

2010-05-01

During the last fifty years phenomenal progress has been made in several areas of ecology of different toxic elements in soils. Concerns regarding heavy metals contamination in the environment affecting all ecosystem componets, including "soil-plant-animal-human" chain (SPAHC), have been identified with increasing efforts on limiting their bioavailability. Many sites have been identified as hazardous (H) waste (W) sites (S)(HWS) because of the presence of elevated concentrations of these elements. In 2000, the main cadmium actual transfer index ("ATI" by Márton 2004) maximum and minimum values in the case of maize 4-6 foliaged phenophase ranged between +22.0- -89.2%. compared with control soils. The grain "ATI" maximum and minimum values changed between +14.4- -89.2% as opposed to unterated plants. The highest yields reached around 10 t* ha-1. These study shows maize has ability to a different degree to cadmium bioaccumulation from soil to corn and by these way for "FOOD CHAIN". Key words: Phosphorous, Fertilization, Cadmium, Translocation, Corn Introduction Nowadays, sustainable (S) precision (P) agricultural (A) production (P)(SPAP) has become the major issue following global changes in all the world over. It is well known that it has strongly established on soils. The functioning and their ability to supply nutrients, store water, release gases, modify pollutants, decrease physical degradation and produce crops is profundly influenced by their fertiliy. During the last fifty years phenomenal progress has been made in several areas of ecology of different toxic elements in soils (ATSDR 1997, 1999; ANZECC 1992; CWP 1995; COC 2004; DEFRA 2002; EDF 1998; HSC 2005; IARC 1993; ). Concerns regarding heavy metals contamination in the environment affecting all ecosystem componets, including "soil-plant-animal-human" chain (SPAHC), have been identified with increasing efforts on limiting their bioavailability (Magher 1991; NEPC 1998; NDH 1986; NTP 1991). Many sites have been identified as hazardous (H) waste (W) sites (S)(HWS) because of the presence of elevated concentrations of these elements. They will remain a threat to the environment until they are removed or immobilized. We can test and improve these situation by using different plant species, as corn (Zea mays L.) x macro nutrients as phosphorous experimental methods. Maize has a very great biomass (B) production (P) potential (P)(BPP) and important role in soil fertility by the design of plant rotation to field plant production, the animal foraging as a fodder-crop with a high carbohydrate (70%) and protein (10%) content (70%) and via pytoremediation possibilities. Cd is considered to be a nonessential element for maize, it is effectively absorbed by both the root and leaf system. By these ways a great proportion of the cadmium is to be accumulated in root tissues, even when Cd enters the plant via foliar system from the polluted air and precipitation. The most chief geobiochemical property of cadmium ions is their strong affinity for sulfhydryl groups of several compounds (OSHA 1992; Richardson 1992; RAIS 1991; Sittig 1991; TAP 1999; WA 1996; WHO 1992, 2001). Furthermore Cd shows an affinity for other side chains of protein and for phosphate groups too. The Cd content of maize is of the highest concern as a Cd reservoir and as the patway of cadmium to soil-plant-animal-man chain (FOOD CHAIN). Thus, tolerance and adaptation of corn to higher Cd levels, although important from the environmental poin of view, create a helth risc. Material and Method The phosphorus (P2O5) mineral fertilization and cadmium loading effects were studied in a long-term field experiment set up at Experimental Station of the Research Institute for Soil Science and Agricultural Chemistry of the Hungarian Academy of Sciences on a calcareous chernozem soil at Nagyhörcsök in 1977. The soil had the following agrogeochemical characteristics: pH (KCl) 7.3, humus 3.0%, ammonlactate (AL) soluble-P2O5 60-80 mg*kg-1, AL-K2O 180-200 mg*kg-1 in the plowed layer. From 1977 to 2000 the experiment consisted of 4x3x2x4=96 plots in split plot design. The gross plot size was 4.9x7=34.3 m2. The fertiliser rates in kg* ha-1 of phosphorus (P2O5) were 0, 100 (in every year from 1977), 2000 (in 1977), 4000 (in 1997) and kg*ha-1*year-1 of cadmium were 0, 70 from 1992 to 2001. Results and Discussion In 2000, the main cadmium actual transfer index ("ATI" by Márton 2004) maximum and minimum values in the case of maize 4-6 foliaged phenophase ranged between +22.0- -89.2%. compared with control soils. The grain "ATI" maximum and minimum values changed between +14.4- -89.2% as opposed to unterated plants. The highest yields reached around 10 t* ha-1. These study shows maize has ability to a different degree to cadmium bioaccumulation from soil to corn and by these way for "FOOD CHAIN". References Agency for Toxic Substances and Disease Registry (ATSDR). 1997. Toxicological Profile for Cadmium. Draft for public comment (update). US Department of Health and Human Services. Atlanta , US . Agency for Toxic Substances and Disease Registry (ATSDR). 1999. Toxicological profile for Cadmium. US department of Health and Human Services. Atlanta, US. Australian and New Zealand Environment and Conservation Council (ANZECC). 1992. Australian Water Quality Guidelines for Fresh and Marine Waters. ChemFinder WebServer Project (CWP). 1995. Cadmium Oxide (accessed, May, 1999) Department for Environment Food and Rural Affairs (DEFRA) and Environment Agency (EA). 2002. Contaminants in soil: Collation of toxicological data and intake values for humans. Cadmium. R&D Publications TOX 3. Environmental Defense Fund (EDF). 1998. Cadmium Chloride: The Chemical Scorecard: (accessed, May, 1999) Health and Safety Commission (HSC). 2005. EH40/2005 Workplace Exposure Limits. International Agency for the Research on Cancer (IARC). 1993. Beryllium, cadmium, mercury and exposures in the glass manufacturing industry. IARC monographs on the evaluation of carcinogenic risk to humans, vol 58. Lyon. Márton L. 2004. Annual Report. RISSAC. Budapest. 10 p. Meagher, D. 1991. The Macmillan Dictionary of The Australian Environment, Macmillan Education Australia Pty Ltd. National Environment Protection Council (NEPC). 1998. National Environment Protection Measure for the National Pollutant Inventory (accessed, May, 1999) New Jersey Department of Health (NDH), Right to Know Program. 1986. TRIFacts, Cadmium (accessed, May, 1999) NTP Chemical Repository, Radian Corporation, Cadmium. 1991. (accessed, May, 1999) Occupational Health and Safety Administration (OSHA). 1992. Occupational exposure to cadmium. Department of Labour. 42102-42427. Richardson, M. 1992. Dictionary of Substances and their Effects, Royal Society of Chemistry, Clays Ltd, England. Risk Assessment Information System (RAIS). 1991. Toxicity summary for cadmium. Chemical Hazard Evaluation and Communication Group, Biomedical and Environmental Information Analysis Section, Health and Safety Research Division. Sittig, M. 1991. Handbook of Toxic and Hazardous Chemicals and Carcinogens, 3rd edition, Noyes Publications, USA. Technical Advisory Panel (TAP). 1999. Final Report to the National Environment Protection Council. US Department of Health and Human Services. 1990. NIOSH Pocket Guide to Chemical Hazards, Publication No. 90-117. Worksafe Australia (WA). 1996. Exposure Standard Cadmium and compounds (as Cd) (accessed, May, 1999) World Health Organisation (WHO). 1992. Environmental Health Criteria 134 - Cadmium International Programme on Chemical Safety (IPCS) Monograph. World Health Organisation (WHO). 2001. Safety evaluation of certain food additives and contaminants. Fifty-fifth meeting of the joint FAO/WHO expert committee on feed additives, Toxicological monographs, WHO food additives series No 46. WHO. Geneva.

Entwicklung von Landnutzungsszenarien für landschaftsökologische Fragestellungen

NASA Astrophysics Data System (ADS)

Fritsch, Uta

2002-04-01

Die Landschaften Mitteleuropas sind das Resultat einer langwierigen Geschichte menschlicher Landnutzung mit ihren unterschiedlichen, z.T. konkurrierenden Nutzungsansprüchen. Durch eine überwiegend intensive Beanspruchung haben die direkten und indirekten Auswirkungen der Landnutzung in vielen Fällen zu Umweltproblemen geführt. Die Disziplin der Landschaftsökologie hat es sich zur Aufgabe gemacht, Konzepte für eine nachhaltige Nutzung der Landschaft zu entwickeln. Eine wichtige Fragestellung stellt dabei die Abschätzung der möglichen Folgen von Landnutzungsänderungen dar. Für die Analyse der relevanten Prozesse in der Landschaft werden häufig mathematische Modelle eingesetzt, welche es erlauben die Landschaft unter aktuellen Verhältnissen oder hinsichtlich veränderter Rahmenbedingungen zu untersuchen. Die hypothetische Änderung der Landnutzung, die als Landnutzungsszenario bezeichnet wird, verkörpert eine wesentliche Modifikation der Rahmenbedingungen, weil Landnutzung mageblich Einfluss auf die natürlichen Prozesse der Landschaft nimmt. Während die Antriebskräfte einer solchen Änderung überwiegend von sozio-ökonomischen und politischen Entscheidungen gesteuert werden, orientiert sich die exakte Verortung der Landnutzungsänderungen an den naturräumlichen Bedingungen und folgt z.T. erkennbaren Regeln. Anhand dieser Vorgaben ist es möglich, räumlich explizite Landnutzungsszenarien zu entwickeln, die als Eingangsdaten für die Modellierung verschiedener landschaftsökologischer Fragestellungen wie z.B. für die Untersuchung des Einflusses der Landnutzung auf den Wasserhaushalt, die Erosionsgefahr oder die Habitatqualität dienen können. Im Rahmen dieser Dissertation wurde das rasterbasierte deterministische Allokationsmodell luck (Land Use Change Scenario Kit) für die explizite Verortung der Landnutzungsänderungen entwickelt. Es basiert auf den in der Landschaftsökologie üblichen räumlichen Daten wie Landnutzung, Boden sowie Topographie und richtet sich bei der Szenarienableitung nach den Leitbildern der Landschaftsplanung. Das Modell fut auf der Hypothese, dass das Landnutzungsmuster als Funktion seiner landschaftsökologischen Faktoren beschrieben werden kann. Das Veränderungspotenzial einer Landnutzungseinheit resultiert im Modell aus einer Kombination der Bewertung der relativen Eignung des Standortes für die jeweilige Landnutzung und der Berücksichtigung von Standorteigenschaften der umliegenden Nachbarn. Die Durchführung der Landnutzungsänderung im Modell ist iterativ angelegt, um den graduellen Prozess des Landschaftswandels nachvollziehen zu können. Als Fallbeispiel für die Anwendung solcher räumlich expliziten Landnutzungsszenarien dient die Fragestellung, inwieweit Landnutzungsänderungen die Hochwasserentstehung beeinflussen. Um den Einfluss auf die Hochwasserentstehung für jede der Landnutzungskategorien – bebaute, landwirtschaftlich genutzte und naturnahe Flächen – abschätzen zu können, wird im Landnutzungsmodell luck exemplarisch für jede Kategorie ein Teilmodell für die Veränderung von Landnutzung angeboten: 1) Ausdehnung der Siedlungsfläche: Dieses Teilmodell fut auf der Annahme, dass sich Siedlungen nur in direkter Nachbarschaft bereits bestehender Bebauung und bevorzugt entlang von Entwicklungsachsen ausbreiten. Steile Hangneigungen stellen für potenzielle Standorte ein Hemmnis bei der Ausbreitung dar. 2) Stilllegung von Grenzertragsackerflächen: Gemä der Hypothese, dass sich die Stilllegung von Ackerflächen an der potenziellen Ertragsleistung der Standorte orientiert, werden in diesem Teilmodell alle Ackerstandorte dahingehend bewertet und die Flächen mit der geringsten Leistungsfähigkeit stillgelegt. Bei homogenen Gebietseigenschaften werden die Stilllegungsflächen zufällig auf die Ackerfläche verteilt. 3) Etablierung von Schutzgebieten in Ufer- und Auenbereichen: Ausgehend von der These, dass sich entlang von Flüssen sensible Flächen befinden, deren Schutz positive Folgen für das Leistungsvermögen der Landschaft haben kann, werden in diesem Teilmodell schützenswerte Ufer- und Auenbereiche auf derzeit landwirtschaftlich genutzten Flächen ausgewiesen. Die Gröe der Schutzgebietsfläche orientiert sich an der Morphologie der umgebenden Landschaft. Die drei Teilmodelle wurden hinsichtlich der implizierten Hypothesen mit vielen unterschiedlichen Ansätzen validiert. Das Resultat dieser intensiven Analyse zeigt für jedes Teilmodell eine zufriedenstellende Tauglichkeit. Die Modellierung der Landnutzungsänderungen wurden in drei mesoskaligen Flusseinzugsgebieten mit einer Fläche zwischen 100 und 500 km² durchgeführt, die sich markant in ihrer Landnutzung unterscheiden. Besonderer Wert wurde bei der Gebietsauswahl darauf gelegt, dass eines der Gebiete intensiv landwirtschaftlich genutzt wird, eines dicht besiedelt und eines vorwiegend bewaldet ist. Im Hinblick auf ihre Relevanz für die vorliegende Fragestellung wurden aus bestehenden Landnutzungstrends die Szenarien für (1) die prognostizierte Siedlungsfläche für das Jahr 2010, (2) die möglichen Konsequenzen des EU-weiten Beschlusses der Agenda 2000 und (3) die Novelle des Bundesnaturschutzgesetzes aus dem Jahr 2001 abgeleitet. Jedes Szenario wurde mit Hilfe des Modells auf die drei Untersuchungsgebiete angewendet. Dabei wurden für die Siedlungsausdehnung in allen drei Gebieten realistische Landnutzungsmuster generiert. Einschränkungen ergeben sich bei der Suche nach Grenzertragsstilllegungsflächen. Hier hat unter homogenen Gebietseigenschaften die zufällige Verteilung von Flächen für die Stilllegung zu einem unrealistischen Ergebnis geführt. Die Güte der Schutzgebietsausweisung ist mageblich an die aktuelle Landnutzung der Aue und die Morphologie des Geländes gebunden. Die besten Ergebnisse werden erzielt, wenn die Flächen in den Ufer- und Auenbereichen mehrheitlich unter derzeitiger Ackernutzung stehen und der Flusslauf sich in das Relief eingetieft hat. Exemplarisch werden für jeden Landnutzungstrend die hydrologischen Auswirkungen anhand eines historischen Hochwassers beschrieben, aus denen jedoch keine pauschale Aussage zum Einfluss der Landnutzung abgeleitet werden kann. Die Studie demonstriert die Bedeutung des Landnutzungsmusters für die natürlichen Prozesse in der Landschaft und unterstreicht die Notwendigkeit einer räumlich expliziten Modellierung für landschaftsökologische Fragestellungen in der Mesoskala. Today′s landscapes in Central Europe are the result of a long history of land-use, which is characterised by many different demands. The immediate and long-term consequences of predominantly intensive land-use have led to environmental problems in many cases. Therefore it is necessary to develop strategies for the maintenance of landscape efficiency which take into account the different claims of utilisation. In this context the estimation of possible impacts of land-use changes represents an important statement of problem. For the analysis of the relevant processes within the landscape, it is common to apply mathematical models. Such models enable the investigation of the landscape under current conditions or with regard to modified boundary conditions. A hypothetic alteration of land-use, which is termed as land-use scenario, represents a substantial modification of the boundary conditions, because land-use exerts a strong influence on the natural processes of the landscape. While the driving forces are predominantly governed by socio-economical and political decisions, the exact location of land-use changes within the landscape mainly depends on the natural conditions and follows partly transparent rules. With these presumptions it is possible to develop land-use scenarios, which can serve as input data for the modelling of different questions of landscape ecology such as the influence of land-use on the water balance, the danger of erosion or the quality of habitat characteristics. In the context of this thesis the grid-based deterministic allocation model luck (Land Use Change Scenario Kit) for the allocation of land-use changes was developed. It is based upon the types of spatial data, which are commonly used in landscape ecology, such as information on land-use, soils as well as topography. The derivation of scenarios follows the approaches of landscape planning. The model is based upon the hypothesis, that land-use structure can be described as a function of its landscape ecological factors. The potential of a site to become subject to land-use changes, results from a combination of its local qualities and the site characteristics of its neighbourhood. Land-use change is realised iteratively in order to simulate the gradual process of changes in the landscape. The influence of land-use changes on flood generation serves as a case study to demonstrate the need for spatial explicit land-use scenarios. For each land-use category – built up areas, agriculturally used areas and natural/semi-natural land – the model luck offers a submodel for investigating the effect of land-use changes on flood generation: 1) Expansion of settlement area: This submodel is based upon the assumption that settlements spread only in the neighbourhood of already existing built-up areas and preferentially along infrastructural axes of development. Steep slopes inhibit the spreading on potential locations. 2) Set-aside of marginal yield sites under agricultural use: Setting-aside of arable land is based on the hypothesis that the selection of arable land to be set-aside depends on the potential yield efficiency of the locations. Within this submodel all fields under agricultural use are valued to that effect and the ones with the least productive efficiency are selected as set-aside locations. In case of homogeneous area qualities the set-aside locations are selected randomly. 3) Establishment of protected areas in waterside and ripearian areas: This submodel takes into consideration that the protection of sensitive areas along the river courses may have positive consequences for the efficiency of the landscape. Therefore this submodel establishes protection zones on waterside and ripearian sites under currently agricultural use, that might be of value for nature conservation. The size of the protection area depends on the morphology of the surrounding landscape. The three submodels were validated with respect to the implied hypotheses by the help of many different approaches. The result of this intensive analysis shows a satisfying suitability for each of the submodels. The simulation of land-use changes was carried out for three mesoscale river catchments with an area between 100 and 500 km². Special attention was paid to the fact that these areas should be markingly different in their land-use: One study area is predominantly under intensive agricultural use, one is densely populated and the third one is covered by forest in large parts of the area. With regard to their relevance to the onhand question from existing land-use trends scenarios were derived for the prognosed settlement area for the year 2010, for the possible consequences of the EU-wide agreement of Agenda 2000 and for the amending federal conservation law dating to the year 2001, which enhances the enlargement of protected areas. Each scenario was applied to the three study areas utilizing the model luck. For the expansion of the settlement areas in all three study areas realistic land-use patterns were generated. Limitations arose only in the context of the search for marginal yield fields. Here, the random distribution of areas to be set-aside under homogeneous conditions led to unrealistic results. The quality of the establishment of protected areas in waterside and ripearian areas is substantially bound to current land-use and the morphology of the area. The best results for this submodel are achieved if waterside and ripearian areas are mainly arable land and if the river has lowered its course into the morphology. The hydrological consequences are described exemplarily for each land-use trend with a historical flood event. The interpretation of the hydrographs does not allow global statements about the influence of land-use. The study demonstrates the significance of land-use pattern for the natural processes in the landscape and underlines the necessity of spatially explicit modelling for landscape ecological questions at the mesoscale.

Seasonal Trace Gas Dynamics on Minerotrophic Fen Peatlands in NE-Germany

NASA Astrophysics Data System (ADS)

Giebels, Michael; Beyer, Madlen; Augustin, Jürgen; Minke, Merten; Juszczak, Radoszlav; Serba, Tomasz

2010-05-01

In Germany more than 99 % of fens have lost their carbon and nutrient sink function due to heavy drainage and agricultural land use especially during the last decades and thus resulted in compression and heavy peat loss (CHARMAN 2002; JOOSTEN & CLARKE 2002; SUCCOW & JOOSTEN 2001; AUGUSTIN et al. 1996; KUNTZE 1993). Therefore fen peatlands play an important part (4-5 %) in the national anthropogenic trace gas budget. But only a small part of drained and agricultural used fens in NE Germany can be restored. Knowledge of the influence of land use to trace gas exchange is important for mitigation of the climate impact of the anthropogenic peatland use. We study carbon exchanges of several fen peatland use areas between soil and atmosphere at different sites in NE-Germany. Our research covers peatlands of supposed strongly climate forcing land use (cornfield and intensive pasture) and of probably less forcing, alternative types (meadow and extensive pasture) as well as rewetted (formerly drained) areas and near-natural sites like a low-degraded fen and a wetted alder woodland. We measured trace gas fluxes with manual and automatic chambers in periodic routines since spring 2007. The used chamber technique bases on DROESLER (2005). In total we now do research at 22 sites situated in 5 different locations covering agricultural, varying states of rewetted and near-natural treatments. We present results of at least 2 years of measurements and show significant differences in their annual trace gas balances depending on the genesis of the observed sites and the seasonal dynamics. Crosswise comparison of different site treatments combined with the seasonal environmental observations give good hints for the identification of main flux driving parameters. That is that a reduced intensity in land use as a supposed mitigating treatment did not show the expected effect, though a normal meadow treatment surprisingly resulted in the lowest balances in both years. For implementing a further trace gas flux model observations will proceed at least until the end of year 2011. Regarding restoration sites we present newly installed locations of observing especially methane fluxes. To assure our results (presented at last years EGU conference, GIEBELS et al. 2009) from our in 2005 rewetted site we started observations at sites with advanced states of rewetting and alternative management respectively. I.e. one alternative aim to mitigate the heavy methane efflux after rewetting is observed at a site with removed canopy. Other experiments are conducted by freshly reforested alders and reed grass. References: Augustin, J., Merbach, W., Käding, H., Schnidt, W. & Schalitz, G. 1996. Lachgas- und Methanemissionen aus degradierten Niedermoorstandorten Nordostdeutschlands unter dem Einfluß unterschiedlicher Bewirtschaftung. Alfed-Wegener-Stiftung (ed.): Von den Ressourcen zum Recycling: Geoanalytik-Geomanagement-Geoinformatik. Ernst & Sohn Verlag. Berlin Charman, D. 2002: Peatland and environmental change. John Wiley & Sons, LTD, Chichester Droesler, M. 2005. Trace Gas Exchange and climatic relevance of bog ecosystems, Southern Germany, phD-thesis, TU München, München Giebels, M., Augustin, J., Minke, M., Halle, E., Beyer, M., Ehrig, B., Leitholdt, E., Chojnicki, B., Juszczak, R., Serba, T. 2009. Anthropogenic impact on the carbon cycle of fen peatlands in NE-Germany, EGU General Assembly 2009 Joosten, H. & Clarke, D. 2002: Wise use of mires and peatlands-background and principles including a framework for decision-making. International Mire Conservation Group and International Peat Society (eds.), Finland Kuntze 1993: Moore als Senken und Quellen für C und N, Mitt. Deutsche Bodenkundliche Gesellschaft 69, 277-280 Succow, M. & Joosten, H. 2001: Landschaftsökologische Moorkunde, 2nd edition, Schweizerbart'sche Verlagsbuchhandlung, Stuttgart

Seasonal Carbon Dynamics on Selected Fen Peatland Sites in NE-Germany

NASA Astrophysics Data System (ADS)

Giebels, Michael; Beyer, Madlen; Augustin, Jürgen; Minke, Merten; Juszczak, Radoszlav; Serba, Tomasz

2010-05-01

In Germany more than 99 % of fens have lost their carbon and nutrient sink function due to heavy drainage and agricultural land use especially during the last decades and thus resulted in compression and heavy peat loss (CHARMAN 2002; JOOSTEN & CLARKE 2002; SUCCOW & JOOSTEN 2001; AUGUSTIN et al. 1996; KUNTZE 1993). Therefore fen peatlands play an important part (4-5 %) in the national anthropogenic trace gas budget. But only a small part of drained and agricultural used fens in NE Germany can be restored. Knowledge of the influence of land use to trace gas exchange is important for mitigation of the climate impact of the anthropogenic peatland use. We study carbon exchanges of several fen peatland use areas between soil and atmosphere at different sites in NE-Germany. Our research covers peatlands of supposed strongly climate forcing land use (cornfield and intensive pasture) and of probably less forcing, alternative types (meadow and extensive pasture) as well as rewetted (formerly drained) areas and near-natural sites like a low-degraded fen and a wetted alder woodland. We measured trace gas fluxes with manual and automatic chambers in periodic routines since spring 2007. The used chamber technique bases on DROESLER (2005). In total we now do research at 22 sites situated in 5 different locations covering agricultural, varying states of rewetted and near-natural treatments. We present results of at least 2 years of measurements and show significant differences in their annual carbon balances depending on the genesis of the observed sites and the seasonal dynamics. Crosswise comparison of different site treatments combined with the seasonal environmental observations give good hints for the identification of main flux driving parameters. That is that a reduced intensity in land use as a supposed mitigating treatment did not show the expected effect, though a normal meadow treatment surprisingly resulted in the lowest CO2 balances in both years. For implementing a further trace gas flux model observations will proceed at least until the end of year 2011. Regarding restoration sites we present newly installed locations of observing especially methane fluxes. To assure our results (presented at last years EGU conference, GIEBELS et al. 2009) from our in 2005 rewetted site we started observing carbon exchange at sites with advanced states of rewetting and alternative management respectively. I.e. one alternative aim to mitigate the heavy methane efflux after rewetting is observed at a site with removed canopy. Other experiments are conducted by freshly reforested alders and reed grass. References: Augustin, J., Merbach, W., Käding, H., Schnidt, W. & Schalitz, G. 1996. Lachgas- und Methanemissionen aus degradierten Niedermoorstandorten Nordostdeutschlands unter dem Einfluß unterschiedlicher Bewirtschaftung. Alfed-Wegener-Stiftung (ed.): Von den Ressourcen zum Recycling: Geoanalytik-Geomanagement-Geoinformatik. Ernst & Sohn Verlag. Berlin Charman, D. 2002: Peatland and environmental change. John Wiley & Sons, LTD, Chichester Droesler, M. 2005. Trace Gas Exchange and climatic relevance of bog ecosystems, Southern Germany, phD-thesis, TU München, München Giebels, M., Augustin, J., Minke, M., Halle, E., Beyer, M., Ehrig, B., Leitholdt, E., Chojnicki, B., Juszczak, R., Serba, T. 2009. Anthropogenic impact on the carbon cycle of fen peatlands in NE-Germany, EGU General Assembly 2009 Joosten, H. & Clarke, D. 2002: Wise use of mires and peatlands-background and principles including a framework for decision-making. International Mire Conservation Group and International Peat Society (eds.), Finland Kuntze 1993: Moore als Senken und Quellen für C und N, Mitt. Deutsche Bodenkundliche Gesellschaft 69, 277-280 Succow, M. & Joosten, H. 2001: Landschaftsökologische Moorkunde, 2nd edition, Schweizerbart'sche Verlagsbuchhandlung, Stuttgart

A new approach to the study of therapeutic work in the transference.

PubMed

Pessier, J; Stuart, J

2000-02-01

This article proposes a new method for evaluating the effects of therapist and patient work in the transference. Work in the transference is often difficult for the patient, and may show a characteristic pattern of lag between a transference interpretation and its therapeutic effect. To account for this lag, we assessed patient responses to interpretations over the course of entire sessions. The narratives patients told about others, or Relationship Episodes (REs), were used as units of study. In a sample of three consecutive sessions taken from each of three psychodynamic cases, we identified several instances when transference work appeared to have an initial inhibitory effect, but facilitated progress over the course of the entire session. We recommend that to examine the effects of interpretations future studies use longer, more clinically meaningful segments of patient speech than have been used in the past. Dieser Beitrag propagiert eine neue Methode zur Evaluierung der Effekte von Übertragungsarbeit durch Therapeut und Patient. Arbeit in der Übertragung ist für den Patienten oftmals schwierig und zeigt häufig eine charakteristisches Muster von zeitlichen Verzögerungen bzgl. Übertragungsdeutungen und deren therapeutischen Effekten. Um diese zeitliche Verzögerung zu erklären, untersuchten wir die Reaktionen von Patienten auf derartige Deutungen im Verlauf ganzer Sitzungen. Narrative, in denen die Patienten über andere berichteten, also Beziehungsepisoden, dienten in dieser Studie als Einheit. In einter Stichprobe dreier aufeinanderfolgender Sitzugnen, die sich auf drei Fälle bezogen, identifizierten wir verschiedene Umstände, unter denen Übertragungsarbeit anfänglich einen hemmenden Affekt zu haben schien, letztlich aber den Gesamtverlauf der Sitzung günstig beeinflussten. Wir empfehlen, in Zukunft die Effekte von Übertragungsdeutungen auf der Basis längerer, klinische sinnvoller Segmente von Patientenäußerungen zu untersuchen als dies in der Vergangenheit der Fall war. Cet article propose une nouvelle méthode pour évaluer les effets du travail sur le transfert entre thérapeute et patient. Ce travail est souvent difficile pour le patient, et il peut y avoir un pattern caractéristique de délai entre une înterprétation de transfert et son effet thérapeutique. Pour expliquer ce délai, nous avons évalué les réponses des patients à des interprétatios au cours de séances entières. C'est les narrations des patients sur d'autres, ou Episodes Relationnels (ERs), qui ont constitué les unités de base de cette étude. Dans un échantillon de 3 séances consécutives venant de 3 cas psychodynamiques, nous avons identifié plusieurs moments où le traail sur le transfert semblait avoir un effet inhibitoire initial, mais favorisait le progrès en regardant la séance entière. Nous recommandons pour de futures études sur l'effet des interprétations de prendre des segments plus longs et cliniquement significatifs du récit du patient que ceux utilisés dans le passé. Este artículo propone un nuevo método para evaluar los efectos del trabajo de terapeuta y paciente en la transferencia. El trabajo en la transferencia es, con frecuencia, dificil para el paciente y puede mostrar un lapso característico entre una interpretación transferencial y sus efectos terapéuticos. Para explicar este lapso, hemos evaluado las respuestas del paciente a las interpretaciones a lo largo de sesiones enteras. Como unidad de estudio se usaron las narrativas de los pacientes acerca de otros, o sea, los episodios relacionales (REs). En una muestra de tres sesiones consecutivas tomadas de tres casos psicodinámicos, identificamos varioss casos en los que la trasferencia parecía tener un efecto inicial inhibitorio, aunque se vio que a lo largo de la sesión facilitaba el progreso. Recomendamos que, para examinar los efectos de las interpretaciones, los futuros estudios usen segmentos más largos y clínicamente más significativos del habia del paciente que los que se usaron en el pasado.

Lossless quantum data compression and secure direct communication

NASA Astrophysics Data System (ADS)

Boström, Kim

2004-07-01

This thesis deals with the encoding and transmission of information through a quantum channel. A quantum channel is a quantum mechanical system whose state is manipulated by a sender and read out by a receiver. The individual state of the channel represents the message. The two topics of the thesis comprise 1) the possibility of compressing a message stored in a quantum channel without loss of information and 2) the possibility to communicate a message directly from one party to another in a secure manner, that is, a third party is not able to eavesdrop the message without being detected. The main results of the thesis are the following. A general framework for variable-length quantum codes is worked out. These codes are necessary to make lossless compression possible. Due to the quantum nature of the channel, the encoded messages are in general in a superposition of different lengths. It is found to be impossible to compress a quantum message without loss of information if the message is not apriori known to the sender. In the other case it is shown that lossless quantum data compression is possible and a lower bound on the compression rate is derived. Furthermore, an explicit compression scheme is constructed that works for arbitrarily given source message ensembles. A quantum cryptographic protocol - the “ping-pong protocol” - is presented that realizes the secure direct communication of classical messages through a quantum channel. The security of the protocol against arbitrary eavesdropping attacks is proven for the case of an ideal quantum channel. In contrast to other quantum cryptographic protocols, the ping-pong protocol is deterministic and can thus be used to transmit a random key as well as a composed message. The protocol is perfectly secure for the transmission of a key, and it is quasi-secure for the direct transmission of a message. The latter means that the probability of successful eavesdropping exponentially decreases with the length of the message. Diese Dissertation behandelt die Kodierung und Verschickung von Information durch einen Quantenkanal. Ein Quantenkanal besteht aus einem quantenmechanischen System, welches vom Sender manipuliert und vom Empfänger ausgelesen werden kann. Dabei repräsentiert der individuelle Zustand des Kanals die Nachricht. Die zwei Themen der Dissertation umfassen 1) die Möglichkeit, eine Nachricht in einem Quantenkanal verlustfrei zu komprimieren und 2) die Möglichkeit eine Nachricht von einer Partei zu einer einer anderen direkt und auf sichere Weise zu übermitteln, d.h. ohne dass es einer dritte Partei möglich ist, die Nachricht abzuhören und dabei unerkannt zu bleiben. Die wesentlichen Ergebnisse der Dissertation sind die folgenden. Ein allgemeiner Formalismus für Quantencodes mit variabler Länge wird ausgearbeitet. Diese Codes sind notwendig um verlustfreie Kompression zu ermöglichen. Wegen der Quantennatur des Kanals sind die codierten Nachrichten allgemein in einer Superposition von verschiedenen Längen. Es zeigt sich, daß es unmöglich ist eine Quantennachricht verlustfrei zu komprimieren, wenn diese dem Sender nicht apriori bekannt ist. Im anderen Falle wird die Möglichkeit verlustfreier Quantenkompression gezeigt und eine untere Schranke für die Kompressionsrate abgeleitet. Des weiteren wird ein expliziter Kompressionsalgorithmus konstruiert, der für beliebig vorgegebene Ensembles aus Quantennachrichten funktioniert. Ein quantenkryptografisches Prokoll - das “Ping-Pong Protokoll” - wird vorgestellt, welches die sichere direkte übertragung von klassischen Nachrichten durch einen Quantenkanal ermöglicht. Die Sicherheit des Protokolls gegen beliebige Abhörangriffe wird bewiesen für den Fall eines idealen Quantenkanals. Im Gegensatz zu anderen quantenkryptografischen Verfahren ist das Ping-Pong Protokoll deterministisch und kann somit sowohl für die Übermittlung eines zufälligen Schlüssels als auch einer komponierten Nachricht verwendet werden. Das Protokoll is perfekt sicher für die Übertragung eines Schlüssels und quasi-sicher für die direkte Übermittlung einer Nachricht. Letzteres bedeutet, dass die Wahrscheinlichkeit eines erfolgreichen Abhörangriffs exponenziell mit der Länge der Nachricht abnimmt.

Large-scale hydrological modelling in the semi-arid north-east of Brazil

NASA Astrophysics Data System (ADS)

Güntner, Andreas

2002-07-01

Semi-arid areas are, due to their climatic setting, characterized by small water resources. An increasing water demand as a consequence of population growth and economic development as well as a decreasing water availability in the course of possible climate change may aggravate water scarcity in future, which often exists already for present-day conditions in these areas. Understanding the mechanisms and feedbacks of complex natural and human systems, together with the quantitative assessment of future changes in volume, timing and quality of water resources are a prerequisite for the development of sustainable measures of water management to enhance the adaptive capacity of these regions. For this task, dynamic integrated models, containing a hydrological model as one component, are indispensable tools. The main objective of this study is to develop a hydrological model for the quantification of water availability in view of environmental change over a large geographic domain of semi-arid environments. The study area is the Federal State of Ceará (150 000 km2) in the semi-arid north-east of Brazil. Mean annual precipitation in this area is 850 mm, falling in a rainy season with duration of about five months. Being mainly characterized by crystalline bedrock and shallow soils, surface water provides the largest part of the water supply. The area has recurrently been affected by droughts which caused serious economic losses and social impacts like migration from the rural regions. The hydrological model Wasa (Model of Water Availability in Semi-Arid Environments) developed in this study is a deterministic, spatially distributed model being composed of conceptual, process-based approaches. Water availability (river discharge, storage volumes in reservoirs, soil moisture) is determined with daily resolution. Sub-basins, grid cells or administrative units (municipalities) can be chosen as spatial target units. The administrative units enable the coupling of Wasa in the framework of an integrated model which contains modules that do not work on the basis of natural spatial units. The target units mentioned above are disaggregated in Wasa into smaller modelling units within a new multi-scale, hierarchical approach. The landscape units defined in this scheme capture in particular the effect of structured variability of terrain, soil and vegetation characteristics along toposequences on soil moisture and runoff generation. Lateral hydrological processes at the hillslope scale, as reinfiltration of surface runoff, being of particular importance in semi-arid environments, can thus be represented also within the large-scale model in a simplified form. Depending on the resolution of available data, small-scale variability is not represented explicitly with geographic reference in Wasa, but by the distribution of sub-scale units and by statistical transition frequencies for lateral fluxes between these units. Further model components of Wasa which respect specific features of semi-arid hydrology are: (1) A two-layer model for evapotranspiration comprises energy transfer at the soil surface (including soil evaporation), which is of importance in view of the mainly sparse vegetation cover. Additionally, vegetation parameters are differentiated in space and time in dependence on the occurrence of the rainy season. (2) The infiltration module represents in particular infiltration-excess surface runoff as the dominant runoff component. (3) For the aggregate description of the water balance of reservoirs that cannot be represented explicitly in the model, a storage approach respecting different reservoirs size classes and their interaction via the river network is applied. (4) A model for the quantification of water withdrawal by water use in different sectors is coupled to Wasa. (5) A cascade model for the temporal disaggregation of precipitation time series, adapted to the specific characteristics of tropical convective rainfall, is applied for the generating rainfall time series of higher temporal resolution. All model parameters of Wasa can be derived from physiographic information of the study area. Thus, model calibration is primarily not required. Model applications of Wasa for historical time series generally results in a good model performance when comparing the simulation results of river discharge and reservoir storage volumes with observed data for river basins of various sizes. The mean water balance as well as the high interannual and intra-annual variability is reasonably represented by the model. Limitations of the modelling concept are most markedly seen for sub-basins with a runoff component from deep groundwater bodies of which the dynamics cannot be satisfactorily represented without calibration. Further results of model applications are: (1) Lateral processes of redistribution of runoff and soil moisture at the hillslope scale, in particular reinfiltration of surface runoff, lead to markedly smaller discharge volumes at the basin scale than the simple sum of runoff of the individual sub-areas. Thus, these processes are to be captured also in large-scale models. The different relevance of these processes for different conditions is demonstrated by a larger percentage decrease of discharge volumes in dry as compared to wet years. (2) Precipitation characteristics have a major impact on the hydrological response of semi-arid environments. In particular, underestimated rainfall intensities in the rainfall input due to the rough temporal resolution of the model and due to interpolation effects and, consequently, underestimated runoff volumes have to be compensated in the model. A scaling factor in the infiltration module or the use of disaggregated hourly rainfall data show good results in this respect. The simulation results of Wasa are characterized by large uncertainties. These are, on the one hand, due to uncertainties of the model structure to adequately represent the relevant hydrological processes. On the other hand, they are due to uncertainties of input data and parameters particularly in view of the low data availability. Of major importance is: (1) The uncertainty of rainfall data with regard to their spatial and temporal pattern has, due to the strong non-linear hydrological response, a large impact on the simulation results. (2) The uncertainty of soil parameters is in general of larger importance on model uncertainty than uncertainty of vegetation or topographic parameters. (3) The effect of uncertainty of individual model components or parameters is usually different for years with rainfall volumes being above or below the average, because individual hydrological processes are of different relevance in both cases. Thus, the uncertainty of individual model components or parameters is of different importance for the uncertainty of scenario simulations with increasing or decreasing precipitation trends. (4) The most important factor of uncertainty for scenarios of water availability in the study area is the uncertainty in the results of global climate models on which the regional climate scenarios are based. Both a marked increase or a decrease in precipitation can be assumed for the given data. Results of model simulations for climate scenarios until the year 2050 show that a possible future change in precipitation volumes causes a larger percentage change in runoff volumes by a factor of two to three. In the case of a decreasing precipitation trend, the efficiency of new reservoirs for securing water availability tends to decrease in the study area because of the interaction of the large number of reservoirs in retaining the overall decreasing runoff volumes. Semiaride Gebiete sind auf Grund der klimatischen Bedingungen durch geringe Wasserressourcen gekennzeichnet. Ein zukünftig steigender Wasserbedarf in Folge von Bevölkerungswachstum und ökonomischer Entwicklung sowie eine geringere Wasserverfügbarkeit durch mögliche Klimaänderungen können dort zu einer Verschärfung der vielfach schon heute auftretenden Wasserknappheit führen. Das Verständnis der Mechanismen und Wechselwirkungen des komplexen Systems von Mensch und Umwelt sowie die quantitative Bestimmung zukünftiger Veränderungen in der Menge, der zeitlichen Verteilung und der Qualität von Wasserressourcen sind eine grundlegende Voraussetzung für die Entwicklung von nachhaltigen Maßnahmen des Wassermanagements mit dem Ziel einer höheren Anpassungsfähigkeit dieser Regionen gegenüber künftigen Änderungen. Hierzu sind dynamische integrierte Modelle unerlässlich, die als eine Komponente ein hydrologisches Modell beinhalten. Vorrangiges Ziel dieser Arbeit ist daher die Erstellung eines hydrologischen Modells zur großräumigen Bestimmung der Wasserverfügbarkeit unter sich ändernden Umweltbedingungen in semiariden Gebieten. Als Untersuchungsraum dient der im semiariden tropischen Nordosten Brasiliens gelegene Bundestaat Ceará (150 000 km2). Die mittleren Jahresniederschläge in diesem Gebiet liegen bei 850 mm innerhalb einer etwa fünfmonatigen Regenzeit. Mit vorwiegend kristallinem Grundgebirge und geringmächtigen Böden stellt Oberflächenwasser den größten Teil der Wasserversorgung bereit. Die Region war wiederholt von Dürren betroffen, die zu schweren ökonomischen Schäden und sozialen Folgen wie Migration aus den ländlichen Gebieten geführt haben. Das hier entwickelte hydrologische Modell Wasa (Model of Water Availability in Semi-Arid Environments) ist ein deterministisches, flächendifferenziertes Modell, das aus konzeptionellen, prozess-basierten Ansätzen aufgebaut ist. Die Wasserverfügbarkeit (Abfluss im Gewässernetz, Speicherung in Stauseen, Bodenfeuchte) wird mit täglicher Auflösung bestimmt. Als räumliche Zieleinheiten können Teileinzugsgebiete, Rasterzellen oder administrative Einheiten (Gemeinden) gewählt werden. Letztere ermöglichen die Kopplung des Modells im Rahmen der integrierten Modellierung mit Modulen, die nicht auf der Basis natürlicher Raumeinheiten arbeiten. Im Rahmen eines neuen skalenübergreifenden, hierarchischen Ansatzes werden in Wasa die genannten Zieleinheiten in kleinere räumliche Modellierungseinheiten unterteilt. Die ausgewiesenen Landschaftseinheiten erfassen insbesondere die strukturierte Variabilität von Gelände-, Boden- und Vegetationseigenschaften entlang von Toposequenzen in ihrem Einfluss auf Bodenfeuchte und Abflussbildung. Laterale hydrologische Prozesse auf kleiner Skala, wie die für semiaride Bedingungen bedeutsame Wiederversickerung von Oberflächenabfluss, können somit auch in der erforderlichen großskaligen Modellanwendung vereinfacht wiedergegeben werden. In Abhängigkeit von der Auflösung der verfügbaren Daten wird in Wasa die kleinskalige Variabilität nicht räumlich explizit sondern über die Verteilung von Flächenanteilen subskaliger Einheiten und über statistische Übergangshäufigkeiten für laterale Flüsse zwischen den Einheiten berücksichtigt. Weitere Modellkomponenten von Wasa, die spezifische Bedingungen semiarider Gebiete berücksichtigen, sind: (1) Ein Zwei-Schichten-Modell zur Bestimmung der Evapotranspiration berücksichtigt auch den Energieumsatz an der Bodenoberfläche (inklusive Bodenverdunstung), der in Anbetracht der meist lichten Vegetationsbedeckung von Bedeutung ist. Die Vegetationsparameter werden zudem flächen- und zeitdifferenziert in Abhängigkeit vom Auftreten der Regenzeit modifiziert. (2) Das Infiltrationsmodul bildet insbesondere Oberflächenabfluss durch Infiltrationsüberschuss als dominierender Abflusskomponente ab. (3) Zur aggregierten Beschreibung der Wasserbilanz von im Modell nicht einzeln erfassbaren Stauseen wird ein Speichermodell unter Berücksichtigung verschiedener Größenklassen und ihrer Interaktion über das Gewässernetz eingesetzt. (4) Ein Modell zur Bestimmung der Entnahme durch Wassernutzung in verschiedenen Sektoren ist an Wasa gekoppelt. (5) Ein Kaskadenmodell zur zeitlichen Disaggregierung von Niederschlagszeitreihen, das in dieser Arbeit speziell für tropische konvektive Niederschlagseigenschaften angepasst wird, wird zur Erzeugung höher aufgelöster Niederschlagsdaten verwendet. Alle Modellparameter von Wasa können von physiographischen Gebietsinformationen abgeleitet werden, sodass eine Modellkalibrierung primär nicht erforderlich ist. Die Modellanwendung von Wasa für historische Zeitreihen ergibt im Allgemeinen eine gute Übereinstimmung der Simulationsergebnisse für Abfluss und Stauseespeichervolumen mit Beobachtungsdaten in unterschiedlich großen Einzugsgebieten. Die mittlere Wasserbilanz sowie die hohe monatliche und jährliche Variabilität wird vom Modell angemessen wiedergegeben. Die Grenzen der Anwendbarkeit des Modell-konzepts zeigen sich am deutlichsten in Teilgebieten mit Abflusskomponenten aus tieferen Grundwasserleitern, deren Dynamik ohne Kalibrierung nicht zufriedenstellend abgebildet werden kann. Die Modellanwendungen zeigen weiterhin: (1) Laterale Prozesse der Umverteilung von Bodenfeuchte und Abfluss auf der Hangskala, vor allem die Wiederversickerung von Oberflächenabfluss, führen auf der Skala von Einzugsgebieten zu deutlich kleineren Abflussvolumen als die einfache Summe der Abflüsse der Teilflächen. Diese Prozesse sollten daher auch in großskaligen Modellen abgebildet werden. Die unterschiedliche Ausprägung dieser Prozesse für unterschiedliche Bedingungen zeigt sich an Hand einer prozentual größeren Verringerung der Abflussvolumen in trockenen im Vergleich zu feuchten Jahren. (2) Die Niederschlagseigenschaften haben einen sehr großen Einfluss auf die hydrologische Reaktion in semiariden Gebieten. Insbesondere die durch die grobe zeitliche Auflösung des Modells und durch Interpolationseffekte unterschätzten Niederschlagsintensitäten in den Eingangsdaten und die daraus folgende Unterschätzung von Abflussvolumen müssen im Modell kompensiert werden. Ein Skalierungsfaktor in der Infiltrationsroutine oder die Verwendung disaggregierter stündlicher Niederschlagsdaten zeigen hier gute Ergebnisse. Die Simulationsergebnisse mit Wasa sind insgesamt durch große Unsicherheiten gekennzeichnet. Diese sind einerseits in Unsicherheiten der Modellstruktur zur adäquaten Beschreibung der relevanten hydrologischen Prozesse begründet, andererseits in Daten- und Parametersunsicherheiten in Anbetracht der geringen Datenverfügbarkeit. Von besonderer Bedeutung ist: (1) Die Unsicherheit der Niederschlagsdaten in ihrem räumlichen Muster und ihrer zeitlichen Struktur hat wegen der stark nicht-linearen hydrologischen Reaktion einen großen Einfluss auf die Simulationsergebnisse. (2) Die Unsicherheit von Bodenparametern hat im Vergleich zu Vegetationsparametern und topographischen Parametern im Allgemeinen einen größeren Einfluss auf die Modellunsicherheit. (3) Der Effekt der Unsicherheit einzelner Modellkomponenten und -parameter ist für Jahre mit unter- oder überdurchschnittlichen Niederschlagsvolumen zumeist unterschiedlich, da einzelne hydrologische Prozesse dann jeweils unterschiedlich relevant sind. Die Unsicherheit einzelner Modellkomponenten- und parameter hat somit eine unterschiedliche Bedeutung für die Unsicherheit von Szenarienrechnungen mit steigenden oder fallenden Niederschlagstrends. (4) Der bedeutendste Unsicherheitsfaktor für Szenarien der Wasserverfügbarkeit für die Untersuchungsregion ist die Unsicherheit der den regionalen Klimaszenarien zu Grunde liegenden Ergebnisse globaler Klimamodelle. Eine deutliche Zunahme oder Abnahme der Niederschläge bis 2050 kann gemäß den hier vorliegenden Daten für das Untersuchungsgebiet gleichermaßen angenommen werden. Modellsimulationen für Klimaszenarien bis zum Jahr 2050 ergeben, dass eine mögliche zukünftige Veränderung der Niederschlagsmengen zu einer prozentual zwei- bis dreifach größeren Veränderung der Abflussvolumen führt. Im Falle eines Trends von abnehmenden Niederschlagsmengen besteht in der Untersuchungsregion die Tendenz, dass auf Grund der gegenseitigen Beeinflussung der großen Zahl von Stauseen beim Rückhalt der tendenziell abnehmenden Abflussvolumen die Effizienz von neugebauten Stauseen zur Sicherung der Wasserverfügbarkeit zunehmend geringer wird. --- Anmerkung: Der Autor ist Träger des von der Universitätsgesellschaft Potsdam e.V. vergebenen Wissenschaftspreises zur Förderung des wissenschaftlichen Nachwuchses für die beste Dissertation des Jahres 2002/2003 an der Universität Potsdam.

Vergleich von rekombinanten Vaccinia- und DNA-Vektoren zur Tumorimmuntherapie im C57BL/6-Mausmodell

NASA Astrophysics Data System (ADS)

Johnen, Heiko

2002-10-01

In der vorliegenden Arbeit wurden Tumorimpfstoffe auf der Basis des Plasmid-Vektors pCI, modified vaccinia virus Ankara (MVA) und MVA-infizierten dendritischen Zellen entwickelt und durch Sequenzierung, Western blotting und durchflußzytometrische Analyse überprüft. Die in vivo Wirksamkeit der Vakzinen wurde in verschiedenen Tumormodellen in C57BL/6 Mäusen verglichen. Die auf dem eukaryotischen Expressionsvektor pCI basierende DNA-Vakzinierung induzierte einen sehr wirksamen, antigenspezifischen und langfristigen Schutz vor Muzin, CEA oder beta-Galactosidase exprimierenden Tumoren. Eine MVA-Vakzinierung bietet in den in dieser Arbeit durchgeführten Tumormodellen keinen signifikanten Schutz vor Muzin oder beta-Galactosidase exprimierenden Tumoren. Sowohl humane, als auch murine in vitro generierte dendritische Zellen lassen sich mit MVA – im Vergleich zu anderen viralen Vektoren – sehr gut infizieren. Die Expressionsrate der eingefügten Gene ist aber gering im Vergleich zur Expression in permissiven Wirtszellen des Virus (embryonale Hühnerfibroblasten). Es konnte gezeigt werden, daß eine MVA-Infektion dendritischer Zellen ähnliche Auswirkungen auf den Reifezustand humaner und muriner dendritischer Zellen hat, wie eine Infektion mit replikationskompetenten Vakzinia-Stämmen, und außerdem die Hochregulation von CD40 während der terminalen Reifung von murinen dendritischen Zellen inhibiert wird. Die während der langfristigen in vitro Kultur auf CEF-Zellen entstandenen Deletionen im MVA Genom führten zu einer starken Attenuierung und dem Verlust einiger Gene, die immunmodulatorische Proteine kodieren, jedoch nicht zu einer Verminderung des zytopathischen Effekts in dendritischen Zellen. Die geringe Expressionsrate und die beobachtete Inhibition der Expression kostimulatorischer Moleküle auf dendritischen Zellen kann für eine wenig effektive Induktion einer Immunantwort in MVA vakzinierten Tieren durch cross priming oder die direkte Infektion antigenpräsentierender Zellen verantwortlich sein. Durch die Modifikation einer Methode zur intrazellulären IFN-gamma Färbung konnten in vakzinierten Mäusen tumorantigenspezifische CTL sensitiv und quantitativ detektiert werden. Die so bestimmte CTL-Frequenz, nicht jedoch die humorale Antwort, korrelierte mit der in vivo Wirksamkeit der verschiedenen Vakzinen: DNA vakzinierte Tiere entwickeln starke tumorantigenspezifische CTL-Antworten, wohingegen in MVA-vakzinierten Tieren überwiegend gegen virale Epitope gerichtete CD4 und CD8-T-Zellen detektiert wurden. Die Wirksamkeit der pCI-DNA-Vakzine spricht für die Weiterentwicklung in weiteren präklinischen Mausmodellen, beispielsweise unter Verwendung von MUC1 oder HLA-A2 transgenen Mäusen. Die Methoden zur Detektion Tumorantigen-spezifischer CTL in 96-Loch-Mikrotiterplatten können dabei zur systematischen Suche nach im Menschen immundominanten T-Zell-Epitopen im Muzin-Molekül genutzt werden. Der durchgeführte Vergleich der auf den Vektoren pCI und MVA basierenden Vakzinen und die Analyse neuerer Publikationen führen zu dem Ergebniss, daß vor allem DNA-Vakzinen in Zukunft eine wichtige Rolle bei der Entwicklung von aktiven Tumorimpfstoffen spielen werden. Rekombinante MVA-Viren, eventuell in Kombination mit DNA- oder anderen Vektoren, haben sich dagegen in zahlreichen Studien als wirksame Impfstoffe zur Kontrolle von durch Pathogene hervorgerufenen Infektionserkrankungen erwiesen. In this study, tumor vaccines based on the plasmid pCI, the attenuated vaccinia virus strain modified vaccinia virus Ankara (MVA) and MVA-infected dendritic cells were constructed and characterized by sequencing, Western blot and flow cytometric analysis. The efficiency to induce tumor immunity in vivo was compared in several C57BL/6 mouse tumor models. Naked DNA Vaccination based on the eukaryotic expression vector pCI did induce very effective, antigen-specific and long-term protection against tumor cell lines expressing mucin, CEA or beta-Gal whereas MVA vaccination did not elicit protective immunity against Mucin or beta-Gal expressing tumors. MVA does infect human or murine in vitro generated dendritic cells very efficiently compared to other viral vectors, however expression levels of the inserted antigens in dendritic cells are significantly lower than in permissive host cells (chicken embryo fibroblasts). It could be shown that the effect of MVA infection on the maturation status of dendritic cells is similar to the effects described for dendritic cells infected with replication competent vaccinia strains. In addition it was shown that the upregulation of the important costimulatory molecule CD40 through LPS stimulation is strongly inhibited in MVA infected cells. During passage in tissue culture, MVA has accumulated a number of large deletions, including a number of immunomodulatory molecules and resulting in a strong attenuation. However the strong cytopathic effect on dendritic cells is maintained. The low level of expression and the effect on dendritic cell maturation may be responsible for the failure of MVA to induce tumor immunity through either cross presentation or direct infection of antigen presenting cells. To detect and quantify tumor-antigen-specific CTL a method based on intracellular IFN-gamma staining was modified and it could be shown that the cellular – but not the humoral – response does correlate with in vivo protection: DNA but not MVA vaccines do induce high levels of tumorantigen-specific CTL whereas MVA-vaccines do induce strong and long lasting CD4 and CD8-T-cell responses against vaccinia antigens. The excellent protection induced by pCI-DNA-vaccination in different tumor models does encourage us to further investigate the elicitation of tumor immunity in MUC1 or HLA-A2 transgenic mice. In mice transgenic for human MHC-I, the IFN-gamma staining protocol could be used to systematically screen for mucin T-cell epitopes that are relevant in humans.

Robust boosting via convex optimization

NASA Astrophysics Data System (ADS)

Rätsch, Gunnar

2001-12-01

In this work we consider statistical learning problems. A learning machine aims to extract information from a set of training examples such that it is able to predict the associated label on unseen examples. We consider the case where the resulting classification or regression rule is a combination of simple rules - also called base hypotheses. The so-called boosting algorithms iteratively find a weighted linear combination of base hypotheses that predict well on unseen data. We address the following issues: o The statistical learning theory framework for analyzing boosting methods. We study learning theoretic guarantees on the prediction performance on unseen examples. Recently, large margin classification techniques emerged as a practical result of the theory of generalization, in particular Boosting and Support Vector Machines. A large margin implies a good generalization performance. Hence, we analyze how large the margins in boosting are and find an improved algorithm that is able to generate the maximum margin solution. o How can boosting methods be related to mathematical optimization techniques? To analyze the properties of the resulting classification or regression rule, it is of high importance to understand whether and under which conditions boosting converges. We show that boosting can be used to solve large scale constrained optimization problems, whose solutions are well characterizable. To show this, we relate boosting methods to methods known from mathematical optimization, and derive convergence guarantees for a quite general family of boosting algorithms. o How to make Boosting noise robust? One of the problems of current boosting techniques is that they are sensitive to noise in the training sample. In order to make boosting robust, we transfer the soft margin idea from support vector learning to boosting. We develop theoretically motivated regularized algorithms that exhibit a high noise robustness. o How to adapt boosting to regression problems? Boosting methods are originally designed for classification problems. To extend the boosting idea to regression problems, we use the previous convergence results and relations to semi-infinite programming to design boosting-like algorithms for regression problems. We show that these leveraging algorithms have desirable theoretical and practical properties. o Can boosting techniques be useful in practice? The presented theoretical results are guided by simulation results either to illustrate properties of the proposed algorithms or to show that they work well in practice. We report on successful applications in a non-intrusive power monitoring system, chaotic time series analysis and a drug discovery process. --- Anmerkung: Der Autor ist Träger des von der Mathematisch-Naturwissenschaftlichen Fakultät der Universität Potsdam vergebenen Michelson-Preises für die beste Promotion des Jahres 2001/2002. In dieser Arbeit werden statistische Lernprobleme betrachtet. Lernmaschinen extrahieren Informationen aus einer gegebenen Menge von Trainingsmustern, so daß sie in der Lage sind, Eigenschaften von bisher ungesehenen Mustern - z.B. eine Klassenzugehörigkeit - vorherzusagen. Wir betrachten den Fall, bei dem die resultierende Klassifikations- oder Regressionsregel aus einfachen Regeln - den Basishypothesen - zusammengesetzt ist. Die sogenannten Boosting Algorithmen erzeugen iterativ eine gewichtete Summe von Basishypothesen, die gut auf ungesehenen Mustern vorhersagen. Die Arbeit behandelt folgende Sachverhalte: o Die zur Analyse von Boosting-Methoden geeignete Statistische Lerntheorie. Wir studieren lerntheoretische Garantien zur Abschätzung der Vorhersagequalität auf ungesehenen Mustern. Kürzlich haben sich sogenannte Klassifikationstechniken mit großem Margin als ein praktisches Ergebnis dieser Theorie herausgestellt - insbesondere Boosting und Support-Vektor-Maschinen. Ein großer Margin impliziert eine hohe Vorhersagequalität der Entscheidungsregel. Deshalb wird analysiert, wie groß der Margin bei Boosting ist und ein verbesserter Algorithmus vorgeschlagen, der effizient Regeln mit maximalem Margin erzeugt. o Was ist der Zusammenhang von Boosting und Techniken der konvexen Optimierung? Um die Eigenschaften der entstehenden Klassifikations- oder Regressionsregeln zu analysieren, ist es sehr wichtig zu verstehen, ob und unter welchen Bedingungen iterative Algorithmen wie Boosting konvergieren. Wir zeigen, daß solche Algorithmen benutzt werden koennen, um sehr große Optimierungsprobleme mit Nebenbedingungen zu lösen, deren Lösung sich gut charakterisieren laesst. Dazu werden Verbindungen zum Wissenschaftsgebiet der konvexen Optimierung aufgezeigt und ausgenutzt, um Konvergenzgarantien für eine große Familie von Boosting-ähnlichen Algorithmen zu geben. o Kann man Boosting robust gegenüber Meßfehlern und Ausreissern in den Daten machen? Ein Problem bisheriger Boosting-Methoden ist die relativ hohe Sensitivität gegenüber Messungenauigkeiten und Meßfehlern in der Trainingsdatenmenge. Um dieses Problem zu beheben, wird die sogenannte 'Soft-Margin' Idee, die beim Support-Vector Lernen schon benutzt wird, auf Boosting übertragen. Das führt zu theoretisch gut motivierten, regularisierten Algorithmen, die ein hohes Maß an Robustheit aufweisen. o Wie kann man die Anwendbarkeit von Boosting auf Regressionsprobleme erweitern? Boosting-Methoden wurden ursprünglich für Klassifikationsprobleme entwickelt. Um die Anwendbarkeit auf Regressionsprobleme zu erweitern, werden die vorherigen Konvergenzresultate benutzt und neue Boosting-ähnliche Algorithmen zur Regression entwickelt. Wir zeigen, daß diese Algorithmen gute theoretische und praktische Eigenschaften haben. o Ist Boosting praktisch anwendbar? Die dargestellten theoretischen Ergebnisse werden begleitet von Simulationsergebnissen, entweder, um bestimmte Eigenschaften von Algorithmen zu illustrieren, oder um zu zeigen, daß sie in der Praxis tatsächlich gut funktionieren und direkt einsetzbar sind. Die praktische Relevanz der entwickelten Methoden wird in der Analyse chaotischer Zeitreihen und durch industrielle Anwendungen wie ein Stromverbrauch-Überwachungssystem und bei der Entwicklung neuer Medikamente illustriert.

Modellierung des Einflusses der Landnutzung auf die Hochwasserentstehung in der Mesoskala

NASA Astrophysics Data System (ADS)

Niehoff, Daniel

2001-10-01

Seit 1990 waren mehrere der großen Flussgebiete Mitteleuropas wiederholt von extremen Hochwassern betroffen. Da sowohl die Landoberfläche als auch die Flusssysteme weiter Teile Mitteleuropas in der Vergangenheit weitreichenden Eingriffen ausgesetzt gewesen sind, wird bei der Suche nach den Ursachen für diese Häufung von Extremereignissen auch die Frage nach der Verantwortung des Menschen hierfür diskutiert. Gewässerausbau, Flächenversiegelung, intensive landwirtschaftliche Bodenbearbeitung, Flurbereinigung und Waldschäden sind nur einige Beispiele und Folgen der anthropogenen Eingriffe in die Landschaft. Aufgrund der Vielfalt der beteiligten Prozesse und deren Wechselwirkungen gibt es allerdings bislang nur Schätzungen darüber, wie sehr sich die Hochwassersituation hierdurch verändert hat. Vorrangiges Ziel dieser Arbeit ist es, mit Hilfe eines hydrologischen Modells systematisch darzustellen, in welcher Weise, in welcher Größenordnung und unter welchen Umständen die Art der Landnutzung auf die Hochwasserentstehung Einfluss nimmt. Dies wird anhand exemplarischer Modellanwendungen in der hydrologischen Mesoskala untersucht. Zu diesem Zweck wurde das deterministische und flächendifferenzierte hydrologische Modell wasim-eth ausgewählt, das sich durch eine ausgewogene Mischung aus physikalisch begründeten und konzeptionellen Ansätzen auszeichnet. Das Modell wurde im Rahmen dieser Arbeit um verschiedene Aspekte erweitert, die für die Charakterisierung des Einflusses der Landnutzung auf die Hochwasserentstehung wichtig sind: (1) Bevorzugtes Fließen in Makroporen wird durch eine Zweiteilung des Bodens in Makroporen und Bodenmatrix dargestellt, die schnelle Infiltration und Perkolation jenseits der hydraulischen Leitfähigkeit der Bodenmatrix ermöglicht. (2) Verschlämmung äußert sich im Modell abhängig von Niederschlagsintensität und Vegetationsbedeckungsgrad als Verschlechterung der Infiltrationsbedingungen an der Bodenoberfläche. (3) Das heterogene Erscheinungsbild bebauter Flächen mit einer Mischung aus versiegelten Bereichen und Freiflächen wird berücksichtigt, indem jede Teilfläche je nach Versiegelungsgrad in einen unversiegelten Bereich und einen versiegelten Bereich mit Anschluss an die Kanalisation aufgeteilt wird. (4) Dezentraler Rückhalt von Niederschlagswasser kann sowohl für natürliche Mulden als auch für gezielt angelegte Versickerungsmulden mit definierten Infiltrationsbedingungen simuliert werden. Das erweiterte Modell wird exemplarisch auf drei mesoskalige Teileinzugsgebiete des Rheins angewandt. Diese drei Gebiete mit einer Fläche von zwischen 100 und 500 km² wurden im Hinblick darauf ausgewählt, dass jeweils eine der drei Hauptlandnutzungskategorien Bebauung, landwirtschaftliche Nutzung oder Wald dominiert. Für die drei Untersuchungsgebiete sind räumlich explizite Landnutzungs- und Landbedeckungsszenarien entworfen worden, deren Einfluss auf die Hochwasserentstehung mit Hilfe des erweiterten hydrologischen Modells simuliert wird. Im Einzelnen werden die Auswirkungen von Verstädterung, Maßnahmen zur Niederschlagsversickerung in Siedlungsgebieten, Stilllegung agrarisch genutzter Flächen, veränderter landwirtschaftlicher Bodenbearbeitung, Aufforstung sowie von Sturmschäden in Wäldern untersucht. Diese Eingriffe beeinflussen die Interzeption von Niederschlag, dessen Infiltration, die oberflächennahen unterirdischen Fließprozesse sowie, zum Beispiel im Fall der Kanalisation, auch die Abflusskonzentration. Die hydrologischen Simulationen demonstrieren, dass die Versiegelung einer Fläche den massivsten Eingriff in die natürlichen Verhältnisse darstellt und deshalb die stärksten (negativen) Veränderungen der Hochwassersituation hervorbringt. Außerdem wird deutlich, dass eine bloße Änderung des Interzeptionsvermögens zu keinen wesentlichen Veränderungen führt, da die Speicherkapazität der Pflanzenoberflächen im Verhältnis zum Volumen hochwasserauslösender Niederschläge eher klein ist. Stärkere Veränderungen ergeben sich hingegen aus einer Änderung der Infiltrationsbedingungen. Die Grenzen der entwickelten Methodik zeigen sich am deutlichsten bei der Simulation veränderter landwirtschaftlicher Bewirtschaftungsmethoden, deren mathematische Beschreibung und zahlenmäßige Charakterisierung aufgrund der Komplexität der beteiligten Prozesse mit großen Unsicherheiten behaftet ist. Die Modellierungsergebnisse belegen darüber hinaus, dass pauschale Aussagen zum Einfluss der Landnutzung auf die Hochwasserentstehung aufgrund der entscheidenden Bedeutung der klimatischen und physiographischen Randbedingungen unzulässig sind. Zu den klimatischen Randbedingungen zählen sowohl Niederschlagsintensität und -dauer als auch die Feuchtebedingungen vor einem hochwasserauslösenden Niederschlag. Die physiographischen Randbedingungen sind von der geomorphologischen und geologischen Ausstattung des Gebiets vorgegeben. Weiterhin muss der räumliche und zeitliche Maßstab, über den Aussagen getroffen werden, klar definiert sein, da sich mit steigender Einzugsgebietsgröße die relative Bedeutung sowohl der verschiedenen Niederschlagstypen als auch der physiographischen Eigenschaften verschiebt. Dies wird in der vorliegenden Arbeit im Gegensatz zu vielen anderen Untersuchungen konsequent berücksichtigt. In Abhängigkeit von Randbedingungen und räumlichen Maßstab sind aufgrund der gewonnen Erkenntnisse folgende Aussagen zum Einfluss von Landnutzungsänderungen auf die Hochwasserentstehung möglich: (1) Für intensive konvektive Niederschlagsereignisse mit tendenziell geringer Vorfeuchte ist der Einfluss der Landnutzung größer als für langanhaltende advektive Niederschläge geringer Intensität, da im ersten Fall veränderte Infiltrationsbedingungen stärker zum Tragen kommen als bei kleinen Niederschlagsintensitäten. (2) In kleinen Einzugsgebieten, wo kleinräumige Konvektivzellen zu Hochwassern führen können, ist der Einfluss der Landnutzung dementsprechend größer als in großen Flussgebieten wie dem Rheingebiet, wo vor allem langanhaltende advektive Ereignisse (unter Umständen verbunden mit Schneeschmelze) relevant sind. (3) In Gebieten mit guten Speichereigenschaften wie mächtigen, gut durchlässigen Böden und gut durchlässigem Gesteinsuntergrund ist der Einfluss der Landnutzung größer als in Gebieten mit geringmächtigen Böden und geringdurchlässigem Festgestein. Dies ist darin begründet, dass in Gebieten mit guten Speichereigenschaften bei einer Verschlechterung der Infiltrationsbedingungen mehr Speicherraum für Niederschlag verloren geht als in anderen Gebieten. Since 1990, several of the large European river basins were affected repeatedly by extreme floods. As both the landscape and the river systems in large parts of Central Europe have undergone major changes in the past, during the search for the causes of this accumulation of extreme events also the impact of human activities on flooding has been discussed. River training, surface sealing, intensive agricultural land-use, consolidation of farmland, and damages to forests are only some examples and consequences of the anthropogenic interferences with the landscape. But due to the diversity of the processes and factors involved, by now it can only be estimated how far the flood situation has changed by these interferences. Therefore, the main target of this thesis is to describe systematically in which way, to what extent and under which circumstances the land-use exerts an influence on storm-runoff generation and subsequently the discharge of rivers. This is investigated by means of exemplary model applications at the hydrological meso-scale. For this task, the deterministic and distributed hydrological model wasim-eth was chosen due to its well-balanced mixture of physically-based and conceptual approaches. In the framework of this thesis, the model has been extended in order to cope with several phenomena which are important when aiming at a characterization of the influence of land-use on flood generation: (1) Preferential flow in macropores is treated by a division of the soil into macropores and a soil matrix. This so-called double-porosity approach allows for fast infiltration and percolation beyond the hydraulic conductivity of the soil matrix. (2) Siltation expresses itself within the model as a deterioration of infiltration conditions at the soil surface, depending on precipitation intensity and the degree of vegetation covering. (3) The heterogeneous appearance of built-up areas, consisting of both sealed areas and pervious areas, is taken into account by dividing each partial area into an unsealed part and a sealed part which is connected to the sewer system. (4) Decentralized storage can be simulated for natural depressions as well as for specific infiltration measures with defined infiltration conditions. The extended model is exemplarily applied to three meso-scale tributaries of the Rhine river. These three catchments with an area of between 100 and 500 km² were chosen with regard to their prevailing land-use, one of them being heavily urbanized, one dominated by agricultural use, and one being mainly forested. For these three catchments, spatially explicit land-use and land-cover scenarios were developed. The impact of these scenarios on storm-runoff generation is being simulated using the extended hydrological model. In this context, namely urbanization, infiltration measures in settlement areas, conversion of farmland to set-aside areas, altered agricultural management practices, affor estation and storm damages in forests are taken into account. These changes influence the interception of rainfall, its infiltration into the soil, the subsurface flow processes next to the soil surface as well as, for example in the case of sewer systems, also runoff concentration. The hydrological simulations demonstrate that sealing of the soil surface is the most intensive intervention in the natural conditions among the ones which are mentioned above. Therefore it results in the strongest (negative) changes of the flooding situation in a catchment. In addition to that, the simulations show that a simple alteration in the interception capacity does not yield significant changes in catchment response, because the storage capacity of vegetation surfaces is rather low compared to the volume of storm events which normally lead to significant floods. More pronounced changes arise from modifications in the infiltration conditions. The limits of the methodology which was chosen for this thesis become obvious when simulating altered agricultural management practices. Due the complexity of the processes involved, mathematical description and parameterization is difficult and therefore afflicted with high uncertainty. In addition to that, the modelling results prove that global statements on the influence of land-use on flood generation are illegitimate because of the paramount importance of the climatic and physiographic boundary conditions. Climatic boundary conditions are precipitation intensity and duration as well as the moisture conditions before a storm event. The physiographic boundary counditions are given by the geomorphological and geological catchment properties. Furthermore, with increasing scale there is a shift in the relative importance of the different types of rainfall as well as the different geophysical catchment properties. Therefore, the spatial and temporal scale for which the results are valid have to be clearly defined. This is taken into account consequently within this thesis - in contrast to many other studies on this topic. Depending on boundary conditions and spatial scale, the findings allow the following statements regarding the influence of land-use changes on storm-runoff generation: (1) For intensive convective storm events with generally low antecedent soil moisture, the influence of land-use is greater than for long-lasting advective storm events with low rainfall intensities, because in the first case changes in the infiltration conditions are more important than during times of low precipitation intensities. (2) In small catchments, where small-scale convective cells can lead to a flood, the influence of land-use is accordingly greater than in large river basins like the Rhine basin, where long-lasting advective rainfalls (possibly in combination with snowmelt) are relevant. (3) In areas with good storage conditions like thick, permeable soils and pervious rock underneath, the influence of land-use is greater than in areas with thin soils and only slightly permeable bedrock. This is due to the fact that in case of deteriorating infiltration conditions, more storage space for precipitation is lost in areas with good storage conditions than in other areas. siehe auch: http://opus.kobv.de/ubp/volltexte/2005/398/

Herstellung von Chitosan und einige Anwendungen

NASA Astrophysics Data System (ADS)

Struszczyk, Marcin Henryk

2001-05-01

1. Die Deacetylierung von crabshell - Chitosan führte gleichzeitig zu einem drastischen Abfall der mittleren viscosimetrischen Molmasse ( Mv), insbesondere wenn die Temperatur und die Konzentration an NaOH erhöht werden. Diese Parameter beeinflussten jedoch nicht den Grad der Deacetylierung (DD). Wichtig ist jedoch die Quelle des Ausgangsmaterials: Chitin aus Pandalus borealis ist ein guter Rohstoff für die Herstellung von Chitosan mit niedrigem DD und gleichzeitig hoher mittlerer Mv, während Krill-Chitin (Euphausia superba) ein gutes Ausgangsmaterial zur Herstellung von Chitosan mit hohem DD und niedrigem Mv ist. Chitosan, das aus Insekten (Calliphora erythrocephala), unter milden Bedingungen (Temperatur: 100°C, NaOH-Konzentration: 40 %, Zeit: 1-2h ) hergestellt wurde, hatte die gleichen Eigenschaften hinsichtlich DD und Mv wie das aus Krill hergestellte Chitosan. Der Bedarf an Zeit, Energie und NaOH ist für die Herstellung von Insekten-Chitosan geringer als für crabshell-Chitosan vergleichbare Resultaten für DD und Mv. 2. Chitosan wurde durch den Schimmelpilz Aspergillus fumigatus zu Chitooligomeren fermentiert. Die Ausbeute beträgt 25%. Die Chitooligomere wurden mit Hilfe von HPLC und MALDI-TOF-Massenspektrmetrie identifiziert. Die Fermentationsmischung fördert die Immunität von Pflanzen gegen Bakterien und Virusinfektion. Die Zunahme der Immunität schwankt jedoch je nach System Pflanze-Pathogen. Die Fermentation von Chitosan durch Aspergillus fumigatus könnte eine schnelle und billige Methode zur Herstellung von Chitooligomeren mit guter Reinheit und Ausbeute sein. Eine partiell aufgereinigte Fermentationsmischung dieser Art könnte in der Landwirtschaft als Pathogeninhibitor genutzt werden. Durch kontrollierte Fermentation, die Chitooligomere in definierter Zusammensetzung (d.h. definierter Verteilung des Depolymerisationsgrades) liefert, könnte man zu Mischungen kommen, die für die jeweilige Anwendung eine optimale Bioaktivität besitzen. 3. Die aus Chitosan-Dispersionen hergestellten MCChB-Filme weisen bessere mechanische Eigenschaften (Bruchfestigkeit, Dehnung) und eine höhere Wasseraufnahmefähigkeit auf als Filme, die nach herkömmlichen Methoden aus sauerer Lösung hergestellt werden. Die Einführung von Proteinen ändert die mechanischen Eigenschaften der MCChB-Filme abhängig von der Art, der Proteine sowie des DD und der Mv des eingesetzte Chitosan. Die Zugabe von Protein beschleunigt den biologischen Abbau der MCChB-Filme. Aus den untersuchten MCChB-Filmen mit Proteinzusatz können leichte, reißfeste und dennoch elastische Materialen hergestellt werden. 4. Mit Hilfe von MCChB-Dispersion kann Papier modifiziert werden. Dadurch werden die mechanischen Eigenschaften verbessert und die Wasseraufnahme wird verringert. Die Zugabe von Proteinen verringert das Wasseraufnahmevermögen noch weiter. Ein geringes Wasseraufnahmevermögen ist der bedeutendste Faktor bei der Papierherstellung. Auch Papier, das mit einem MCChB-Protein-Komplexe modifiziert wurde, zeigt gute mechanische Eigenschaften. 5. Wird Chitosan durch unmittelbare Einführung von MCChB auf Cellulose-Fasern aufgebracht, so erhält man eine netzartige Struktur, während durch Ausfällung aufgebrachtes Chitosan eine dünne Schicht auf den Cellulose-Fasern bildet. Die netzartige Struktur erleichtert die Bioabbaubarkeit, während die Schichtstruktur diese erschwert. 6. Die guten mechanischen Eigenschaften, die geringe Wasseraufnahmefähigkeit und die mit Cellulose vergleichbare Bioabbaubarkeit von Papier, das mit MCChB modifiziert wurde, lassen MCChB für die Veredlung von Papier nützlich erscheinen. 1. Deacetylation of the crustacean chitosan causes drastically decrease in the Mv with increasing reaction temperature and time as well as the concentration of sodium hydroxide. However, the DD are relatively less affected. Pandalus borealis is a good source for production of chitosan having high Mv and low DD, whereas chitosan of medium to low Mv can ideally be prepared using krill chitin. Insect chitosan is prepared under milder condition as compared with the crustacean chitosan, showed similar Mv and DD. Moreover, the consumption of time, energy and sodium hydroxide is much lower than for crustacean chitosan used. The properties of chitin (type of source, crystallinity, DD, Mv, swelling properties, particle size) affect the deacetylated polymer parameters. 2. Fermentation of chitosan using fungus Aspergillus fumigatus resulted in a composition of oligosaccharides with controlled molecular weight and yield at least 25 wt%. The product of fermentation effectively inhibited the viral and/or bacterial infection of the plant. This method can be an excellent, inexpensive system for preparation of bioactive agent. The preliminary purified fermentation mixture due to its antiviral and antibacterial behaviour is capable to be used as a natural, plant protection agent. The controlled degradation of chitosan connected with the production of various oligosaccharides having specified molecular weight allows obtaining the product with optimum bioactivity for suitable applications. 3. The films formed form microcrystalline chitosan (MCChB) gel-like dispersion demonstrate the better mechanical properties and higher swelling behaviour than typical films prepared using acidic solution of chitosan. The introduction of proteins significantly changes the mechanical strength and swelling behaviour. Addition of proteins causes the increase in their biodecomposition. The blended films containing proteins could be the base for formation of the resistant materials showed excellent elongation at break. 4. The application of MCChB in a paper formation as a modificator of the fibre-water interactions allows producing the paper sheets indicating the high increase in the mechanical properties and significant decrease in swelling properties. The introduction of MCChB with proteins causes a slight decrease in paper mechanical strength, if determined at low relative humidity. However, the mechanical strength measured at high relative humidity differ less than for paper sheet containing only MCChB. 5. Direct introduction of MCChB to a paper pulp forms the "web-like" structure of cellulose fibres and MCChB. The "web-like" structure of MCChB enables the faster biodecomposition of formed paper sheets. The precipitation of MCChB as wells as introduction of MCChB with proteins causes the "coat-like" structure. MCChB creates a thin layers coated the cellulose fibres lowering a biodecomposition rate. 6. The properties of paper sheets modified by MCChB such as: similar to cellulose biodegradation, excellent mechanical properties at rel. high humidity and the decrease in swelling properties as well as various possibilities to introduce MCChB allow to apple microcrystalline chitosan with or without proteins as the modificator of the fibre-water interactions in paper.

Change in genetic correlation due to selection using animal model evaluation.

PubMed

Strandén, I; Mäntysaari, E A; Mäki-Tanila, A

1993-01-12

Monte Carlo simulation and analytical calculations were used to study the effect of selection on genetic correlation between two traits. The simulated breeding program was based on a closed adult multiple ovulation and embryo transfer nucleus breeding scheme. Selection was on an index calculated using multi-trait animal model (AM). Analytical formulae applicable to any evaluation method were derived to predict change in genetic (co)variance due to selection under multi-trait selection using different evaluation methods. Two formulae were investigated, one assuming phenotypic selection and the other based on a recursive two-generation AM selection index. The recursive AM method approximated information due to relatives by a relationship matrix of two generations. Genetic correlation after selection was compared under different levels of initial genetic and environmental correlations with two different selection criteria. Changes in genetic correlation were similar in simulation and analytical predictions. After one round of selection the recursive AM method and the simulation gave similar predictions while the phenotypic selection predicted usually more change in genetic correlation. After several rounds of selection both analytical formulae predicted more change in genetic correlation than the simulation. ZUSAMMENFASSUNG: Änderung der genetischen Korrelation bei Selektion mit einem Tiermodell Der Selektionseffekt auf die genetische Korrelation zwischen zwei Merkmalen wurde mit Hilfe von Monte Carlo-Simulation und analytischen Berechnungen untersucht. Ein geschlossener Adulter - MOET (Multiple Ovulation and Embryo Transfer) Zuchtplan wurde simuliert. Die Selektion gründete sich auf einen Index, der die Zuchtwertschätzung des Mehrmerkmals-Tiermodells benutzte. Analytische Formeln für die Voraussage der Änderung der genetischen (Ko)varianz unter multivariate Selektion für verschiedene Zuchtwertschätzungsmethode wurden deduziert. Zwei Formeln wurden studiert, die erste nahm phänotypische Auswahl an und die andere gründete sich auf ein wiederholte Mehrmerkmals-Tiermodell von zwei Generationen. Das wiederholte Mehrmerkmals-Tiermodell approximierte die Information aus den Verwandten mit Hilfe einer Verwandtschaftsmatrix der zwei Generationen. Die genetische Korrelation nach der Selektion aus der Simulation und den analytischen Formeln wurde mit verschiedenen reellen genetischen und umweltbedingten Korrelationen mit zwei Selektionskriterien verglichen. Sie änderte sich ähnlich bei Simulation und analytischen Formeln. Nach einem Selektionszyklus kamen das wiederholte Mehrmerkmals-Tiermodell und die Simulation zu gleichen Voraussagen, aber die phänotypische Selektion sagte mehr Änderung voraus. Nach mehreren selektierten Generationen sagten die beiden analytischen Formeln mehr Änderung in der genetischen Korrelation voraus als die Simulation. RÉSUMÉ: Changement de corrélation génétique du à la sélection en utilisant une évaluation de type modèle animal Une simulation Monte Carlo et des calculs analytiques ont été utilisés pour étudier l'effet de la sélection sur la corrélation génétique entre deux caractères. Le programme de sélection simulé a été basé sur le schéma d'un noyau de sélection adulte et fermé avec superovulation et transfert embryonnaire. La sélection portait sur un indice calculé à partir d'un modèle animal multicaractères (AM). Des formules analytiques applicables à n'importe quelle méthode d'évaluation ont été développées pour prédire le changement de (co)variance génétique du à la sélection multicaractères en utilisant différentes méthodes d'évaluation. Deux formules ont été étudiées, l'une supposant une sélection phénotypique et l'autre basée sur un index de sélection de type AM sur deux générations. La méthode AM récurrente prenait en compte l'information des apparentés de manière approximative à travers la matrice de parenté sur deux générations. La corrélation génétique après sélection a été comparée à différents niveaux de corrélations génétique et environnementale pour deux critères de sélection différents. Les changements de corrélation génétique étaient similaires dans les simulations et les prédictions analytiques. Après un cycle de sélection, la méthode récurrente AM et la simulation donnaient les prédictions similaires alors que la sélection phénotypique prédisait habituellement des changements de corrélations génétiques plus importants. Après plusieurs cycles de sélection, les deux formules analytiques prédisaient des changements de corrélation plus importants que la simulation. RÉSUMÉ: Cambio en la correlación genética debido a selección usando evaluaciones con modelo animal Se estudió el efecto de la selección sobre la correlación genética entre dos caracteres utilizando simulación de Monte Carlo y cálculos analíticos. El esquema de selección simulado estuvo basado en un núcleo adulto y cerrado de ovulación multiple y transferencia de embriones. El criterio de selección fue un indice calculado a partir de un modelo animal multicarácter (AM). Se derivaron fórmulas analíticas aplicables a cualquier método de evaluación para predecir cambios debidos a selección en las (co)varianzas genéticas bajo selección multicarácter usando distintos métodos de valoración. Se investigaron dos fórmulas, una que asumía selección fenotípica y la otra basada en un índice de selección AM recurrente con dos generaciones. El método AM recurrente aproximaba la información de parientes a través de una matriz de relaciones aditivas que contemplaba dos generaciones. La correlación genética tras la selección fue comparada bajo distintos niveles de correlación genética y ambiental iniciales con dos criterios de selección diferentes. Los cambios en correlatión genética fueron similares en las predicciones analíticas y con simulación. Tras un ciclo de selección, el método AM recurrente y la simulación produjeron predicciones similares mientras que la selección fenotípica predijo, generalmente, más cambio en la correlación genética. Después de varios ciclos de selección, las dos fórmulas analíticas predijeron más cambios en la correlación genética que la simulación. 1993 Blackwell Verlag GmbH.

The development of the Middle Triassic tectonical controlled Germanic Basin of Central Europe and the palaeoenvironmental related distribution of marine and terrestrial reptiles

NASA Astrophysics Data System (ADS)

Diedrich, Cajus G.

2010-05-01

Nine Middle Triassic paleogeographical maps comprising the uppermost Upper Bunter, Lower to Middle Muschelkalk and Upper Muschelkalk to Lower Keuper time frame (Diedrich 2008b) show the marine ingression and regression cycle of the Middle Triassic Germanic Basin (Diedrich 2010c). For bathymetrical and palaeoenvironmental interpretations especially reptiles and their footprints are used. This Germanic Basin as analogon for the Arabian Gulf (Knaust 1997), north of the Tethys, was under marine and finally terrestrial influenced sediments in a time frame (after Kozur and Bachmann 2008) between 247.2 My (Myophoria Fm, Aegean, Lower Anisian) to 237.9 My (Grabfeld Fm, Longobardian, Lower Ladinian). In a duration of 9.3 My the Germanic Basin was filled up mainly with marine carbonates and at the end by siliciclastics influenced by the northern Tethys through the Silesian, Carpathian and later the Burgundian Gates which connected the Germanic Basin to the Northern Tethys. With the marine ingression from the East via the Silesian Gate (Poland) a ten to hundred kilometers extended intertidal flat to sabkha facies belt surrounded first only the central and then the Western Germanic Basin (Winterswijk, Netherlands). Those intertidal zones were used mainly by two different small reptiles as their primary habitat. Hereby they left Millions of the small tom medium sized footprints of the ichnogenera Rhynchosauroides and Procolophonichnium (Diedrich 2005, 2008a). Larger terrestrial and beach and sabkha adapted reptiles were Tanystrophaeus antiquus and unknown archosaurs, which are recorded only by their footprints. At the beginning of the ingression at the uppermost Bunter a shallow marine invertebrate fauna and coastal reptiles appeared in the Germanic Basin which must have originated mainly from the Northern Tethys. Especially all marine reptiles immigrated from the Tethys which is proven not only by assamblaged Tethyan cephalopod Ceratite species (cf. Diedrich 2008a). The coastal intertidal zones appeared with mud cracked biolaminate and sabkha dolomites ("Biolaminate and Sabkha facies") and expanded further west and south within the Lower Muschelkalk Winterswijk Fm (Aegean/Bithynian boundary), Osnabrück Fm, and Jena Fm (Bithynian to Pelsonian) (Diedrich and Trostheide 2007, Diedrich 2008a). The intertidal zones changed their extensions several times in the Lower Muschalkalk due to the less eustatically and more tectonically controlled very shallow relief cratonic basin morphology and were more stable in the western part of the flat carbonate ramp basin (Winterswijk, Netherlands) and in coastal zones in general. In the Germanic Basin centre (Rüdersdorf to Gogolin, Germany/Poland) the conditions were all that time under very shallow carbonate sand barr (Oolithtic, Terebratula or Shell bioclastic facies) or shallow subtidal ("Wellenkalk facies") conditions, whereas even extended seagrass meadows in shallow carbonate facies types are indirectly proven by invertebrate communities, especially snails. Those algae attracted especially placodontids which were the "Triassic seacows" feeding on such algae (Diedrich, 2010a), which immigrated with Paraplacodus, Placodus and Cyamodus already with the first Lower Muschelkalk ingression sequence. Also other reptiles such as nothosaurs Nothosaurus (small species), Cymatosaurus, the pachypleurosaurids Dactylosaurus, Neusticosaurus or Serpianosaurus must have originated from the tethys and were shallow marine and even lagoonary adapted paraxial swimming smaller marine reptiles. This "Lower Muschelkalk" time was highly tectonically active represented by several seismic layers (slumps, sigmoidal shocked layers, etc.) (cf. Schwarz 1975, Rüffer 1996, Knaust 2000, Diedrich 2008a), which were also reaching the intertidal beach zones, possibly even with tsunamite hazard events (Diedrich 2008b, 2009b). Such tsunamis or quick floodings due to storm events must have had hazardous impacts on marine reptiles or fishes, and the beach inhabiting terrestrial reptiles, which could have been killed by high amounts which explains the presence of many skeletons, bonebeds, and footprint preservations in the Germanic Basin biolaminate and lagoonal facies. With a high seismic peak during the Middle Muschelkalk Karlstadt Fm (Pelsonian/Illyrian boundary) in the intertidal zones up to 19 tectonically shocked biolaminate layers (locality Bernburg, Central Germany, Diedrich 2009b) prove the beginning of the Alpine tectonics and its raise (fold belt structure: Müller et al. 1964), but also the opening of the Carpathian Gate (graben structure: Szulc 1998), from which the epicenters were estimated by two main slickenside directions. Those can be found all over the Germanic Basin "Lower Muschelkalk" sediments (Szulc 1998, Föhlisch 2007, Diedrich 2009b). This time period of the Pelsonian/Illyrian boundary gave even such extended intertidal zones, that reptiles left Millions of tracks all over those biolaminate facies types, allowing those to migrate and distribute East (Bohemian Island) - West (Rhenisch Massif, London-Brabant Massif) due to "intertidal flat bridges". Therefore chirotherid archosaur trackmakers left Chirotherium, Isochirotherium and Brachychirotherium trackways quite abundantly not anymore in the typical Bunter red sandstone facies; now they appeared in the new environments, the intertidal biolaminates such as well documented at Bernburg (Central Germany, Diedrich 2009b), but also on other Middle Triassic coast east of the Massif Central (Demathieu 1985) or the Alps (e.g. Avanzini 2002). The only surviving marine reptiles were smaller lagoonal adapted pachypleurosaurs such as the common Anarosaurus and smaller sized Nothosaurus. Placodontids disappeared with the loss of the palaeoenvironment of the macroalgae meadows and seem to have migrated to the Carpathian gate and northern Tethys, where those habitats were still present. The dramatical habitat change with terrestrial territory loss, and marginal marine beach zone extensions seem to be also the reason for the beginning of the dinosaur raise in the world. Within the Middle Muschelkalk Heilbronn and Diemel Formations a massive sea level fall caused a new extension of intertidal zones and sabkhas, but also halite and gypsum evaporates ("Domolite-evaporate facies") in the basin center including the southern Germanic Basin branch (region Tübingen/Stuttgart, Southwestern Germany). The "Middle Muschelkalk" shallow relief and lagoon to intertidal dominated period changed again drastically within a new tectonic active "Upper Muschelkalk" time and strong "ingression" of the northern Tethys into the Germanic Basin within the Illyrian time (Bad Sulza Fm, Trochitenkalk Fm). A shallow marine, with shallow water carbonates filled Germanic Basin developed again, but this time with different consequences onto the former coastal zones, in which intertidal biolaminated and sabkhas disappeared as a result of steeper coastal morphologies. Whereas in the first ingression a shallow marine reptile fauna was present (Nothosaur-Pachypleurosaur taphocoenosis, Lower Bad Sulza Fm, Diedrich in prep.). The fauna changed with the main transgression within the Upper Bad Sulza Fm to a Placodontid-Pistosaur taphocoenosis with more open marine adapted forms (Diedrich in prep.). At those time also crinoid bioherms developed massively all over the central and southern Germanic Basin in front of the costs at the "steeper coast margins" (which were still hot high angled), as a "crinoid belt" (e.g. Aigner and Bachmann 1991), which was responsible for massive crinoidal limestones (= "Trochitenkalk facies"). In this period again "Triassic seacows" seem to have populated well the entire Germanic Basin, and here again seagrass meadow areas documented by benthic invertebrate palaeocommunities (Diedrich 2009a, 2010a). The marine macroplants must have built extended meadows on the shallow marine and oxygen-rich seafloor conditions of the "Tonplatten facies" on which many different invertebrates settled in- or epifaunistic. This tectonical deepening controlled situation continued with the Meißner Fm and aequivalent Formations and its cephalopod Ceratite rich "Tonplatten facies", whereas the "maximum flooding" (if the term can be used here in a cratonic and tectonically controlled basin: cf. definition of marine cycles in: Aigner and Bachmann 1991) was in the compressus biozone (ceratite biozone, middle Meißner Fm, Anisian/Ladinian boundary, cf. Diedrich 2009a). The high stand is underlined by now full adapted marine reptiles such as nothosaurs (Nothosaurus mirabilis, Simosaurus gaillardodti), pistosaurs (Pistosaurus longaevus) and especially the open marine ichtyosaurs (Shastasaurus, Mixosaurus, Omphtalmosaurus) support the full marine and highest water level conditions. The "regression" or better suggested here "basin uplifting" started in the upper Meißner Fm with a reducing carbonate sedimentation which was overtaken slowly by terrestrial sediments already within the Warburg/Erfurt Formations (Fassanian/Longobardian boundary, Lower Ladinian). The fresh water and clay mineral influence caused a reduction of the marine benthic community biodiversity and the development of brackish lagoons, in which some invertebrate faunas and dominantly small marine reptiles pachypleurosaurs lived. At that time all placodontid reptiles disappeared, which must have been the chain reaction of the macroalgae loss and environmental changes. A change of terrestrial influence and periodic marine influence is documented in repeating intercalated massive dolomites (Alberti-Bed, Anthraconit-Bed and others) and clay layers of the Lower Keuper Erfurt and especially Grabfeld Fm (Longobardian). In this final period the Lower Keuper Germanic Basin was less and less marine influenced, finally dominated at that time on the limnic influenced costs by large amphibians such as Mastodonsaurus, Gerrhothorax or Plagiosuchus, which were found especially at southern German and Central german sites (Schoch and Wild 1999, Diedrich 2010b), including the famous southern German "Grenzbonebed" (Fassanian/Longobardian boundary) (Reif 1982, Hagdorn 1990). This bonebed already contains a strongly reduced marine reptile fauna with pachypleurosaurs and giant lagoon-adapted nothosaurs (N. giganteus, S. gaillardoti) and few marine hypersaline adapted shells such as Costatoria costata (cf. Hagdorn et al. 2009). The absence of cephalopod ceratites and rare nautilid presence are the last proves for the periodic restricted lagoon situations- being comparable in its facies and reptile fauna to the lagoon of the Northern Tethys Monte San Giorgio, Switzerland/Italy (e.g. De Zanche and Farabegoli 1988, Furrer 1995) to which the Germanic Basin was connected through the Burgundian Gate, France. The marine influence and marine sediment fill of the Germanic Basin stopped finally at the beginning of the Middle Keuper (lower Upper Triassic), diachronously more earlier in northern Germany (Warburg/Erfurt Fm, cf.: Kozur and Bachmann 2008, Diedrich 2010b) as in southern Germany (cf. Hagdorn et al. 2009) indicating a periodic marine influence from the Northern Tethys through the Burgundian Gate. At the final tectonical stage (last seismits in the Grabfeld Fm, Longobardian: cf. Bachmann and Aref 2005) no intertidal flats nor biolamnintes developed anymore in a low relief Germanic Basin morphology, which reason can be explained be the carbonate reduction, strong terrigenous clay input, and brakish-lagoonary conditions, in which cyanobacterial mats of the low-relief intertidal zones could not develop. References Aigner, T. and Bachmann, G.H. 1991. Sequence Stratigraphy of the German Muschelkalk. In: Hagdorn, H. and Seilacher, A. (Eds.): Muschelkalk. Schöntaler Symposium. 15-18. Goldschneck-Verlag, Stuttgart. Avanzini, M. 2002. Dinosauromorph tracks from the Middle Triassic (Anisian) of the Southern Alps (Valle di Non-Italy). Bolletino della Società Paleontologica Italiana, 41 (1), 37-40. Bachmann, G.H. and Aref, M.A.M., 2005. A seismite in Triassic gypsum deposits (Grabfeld Formation, Ladinian), Southwest Germany. Sedimentary Geology 180, 75-89. De Zanche, V. and Farabegoli, E. 1988. Anisian paleogeographic evolution in the Central-Western Southern Alps. Memoirs Scientifique Geologique 40, 399-411. Demathieu, G.R. 1985. Trace fossil assemblages in Middle Triassic marginal marine deposits, eastern border of the Massif Central, France. Societe Economie Paléontologie et Mineralogie, Special Publications, 35, 53-66. Diedrich, C. 2005. Actuopalaeontological trackway experiments with Iguana on intertidal flat carbonates of the Arabian Gulf - a comparison to fossil Rhynchosauroides tracks of Triassic carbonate tidal flat megatracksites in the European Germanic Basin. Senckenbergiana maritime, 35 (2), 203-220. Diedrich, C. 2008a. Millions of reptile tracks - Early to Middle Triassic carbonate tidal flat migration bridges of Central Europe. Palaeogeography, Palaeoclimatology, Palaeoecology, 259, 410-423. Diedrich, C. 2008b. Palaeogeographic evolution of the marine Middle Triassic marine Germanic Basin changements - with emphasis on the carbonate tidal flat and shallow marine habitats of reptiles in Central Pangaea. Global and Planetary Change, 65 (2009), 27-55. Diedrich, C. 2009a. The vertebrates of the Anisian/Ladinian boundary (Middle Triassic) from Bissendorf (NW Germany) and their contribution to the anatomy, palaeoecology, and palaeobiogeography of the Germanic Basin reptiles. Palaeogeography, Palaeoclimatology, Palaeoecology, 273 (2009), 1-16. Diedrich, C. 2009b. Die Saurierspuren-Grabung im basalen Mittleren Muschelkalk (Anis, Mitteltrias) von Bernburg (Sachsen-Anhalt). Archäologie in Sachsen-Anhalt, Sonderband 2009, 1-62. Diedrich, 2010a. Palaeoecology of Placodus gigas (Reptilia) and other placodontids - macroalgae feeder of the Middle Triassic in the Germanic Basin of Central Europe and comparison to convergent developed sirenia. Palaeogeography, Palaeoclimatology, Palaeoecology, (in review). Diedrich, 2010b. The vertebrate fauna of the Lower Ladinian (Middle Triassic) from Lamerden (Germany) and contribution to the palaeoecology, anatomy and palaeogeography of the Germanic Basin reptiles. Palaeogeography, Palaeoclimatology, Palaeoecology, (in review). Diedrich, 2010c. The palaeogeographic reconstructions of the Middle Triassic tectonical controlled carbonatic Germanic Basin of Central Europe - a northern Tethys connected cratonic marine Basin - coastal basin margin mappings by the use of reptile footprint rich intertidal and sabkha environments. Abstract, Fifth International Conference on the Geology of the Tethys Realm, Quena-Luxor,Egypt), 3-5. Diedrich, in prep. The shallow marine fish and sauropterygian reptile vertebrate fauna of the Germanic Basin from the atavus/pulcher Bonebeds in the Bad Sulza Fm (Illyrian, Middle Triassic) of Bad Sulza (Central Germany). Diedrich, C. and Trostheide, F. 2007. Auf den Spuren der terresten Muschelkalksaurier und aquatischen Sauropterygier vom obersten Röt bis zum Mittleren Muschelkalk (Unter-/Mitteltrias) von Sachsen-Anhalt. Abhandlungen und Berichte für Naturkunde, 30, 5-56. Föhlisch, K. 2007. Überlieferungen seismischer Aktivität im Unteren Muschelkalk. Beiträge zur Geologie Thüringens, N.F. 14, 55-83. Furrer, H. 1995. The Kalkschieferzone (Upper Meride estone Ladinian) near Meride (Canton Ticino, Southern Switzerland) and the evolution of a Middle Triassic intraplatform basin. Eclogae geolicae Helvetiae, 88(3), 827-852. Hagdorn, H. 1990. Das Muschelkalk/Keuper-Bonebed von Crailsheim. In: Weidert, W. K. (Ed.), Klassische Fundstellen der Paläontologie, Band 2. 78-88. Goldschneck-Verlag, Stuttgart. Hagdorn, H., E. Nitsch, Aigner, T. and Simon, T. 2009. Field guide 6th international Triassic field workshop (Pan-European Correlation of the Triassic) Triassic of Southwest Germany. September 7-11, 2009, www.stratigraphie.de/perm-trias_workshops.html, 1-72. Knaust, D. 1997. Die Karbonatrampe am SE-Rand des Persischen Golfes (Vereinigte Arabische Emirate) - rezentes Analogon für den Unteren Muschelkalk der Germanischen Trias? Greifswalder Geowissenschaftliche Beiträge, 5, 101-123. Knaust, D. 2000. Signatures of tectonically controlled sedimentation in Lower Muschelkalk carbonates (Middle Triassic) of the Germanic Basin. Zentralblatt für Geologie und Paläontologie, I, 1998 (9-10), 893-924. Kozur, H.W. and Bachmann, G.H. 2008. Updated correlation of the Germanic Triassic with the Tethyan scale and assigned numeric ages. Berichte der Geologischen Bundesanstalt Wien, 76, 53-58. Reif, W.E. 1982. Muschelkal/Keuper bone-beds (Middle Triassic, SW-Germany) - storm condensation in a regressive cycle. In: Einsele, G. and Seilacher, A. (Eds.), Cyclic and Event Stratification. 299-325. Springer-Verlag, Berlin-Heidelberg-New York. Müller, W. et al., 1964. Vulkanogene Lagen aus der Grenzbitumenzone (Mittlere Trias) des Monte San Giorgio in den Tessiner Kalkalpen. Eclogae geolicae Helvetiae, 57(2), 431-450. Rüffer, T. 1996. Seismite im Unteren Muschelkalk westlich von Halle (Saale). Hallesches Jahrbuch für Geowissenschaften, B 18, 119-130. Schoch, R. and Wild, R. 1999. Die Wirbeltiere des Muschelkalks unter besonderer Berücksichtigung Süddeutschlands. In: Hauschke, N. and Wilde, V. (Eds.), Trias eine ganz andere Welt. Europa im frühen Erdmittelalter. 331-342. Pfeil-Verlag, München. Schwarz, U. 1975. Sedimentary structures and facies analysis of shallow marine carbonates (Lower Muschelkalk, Middle Triassic, SW-Germany). Contributions to Sedimentology, 3, 1-100. Szulc, J. 1998. Anisian-Carnian evolution of the Germanic Basin and its eustatic, tectonic and climate controls. Zentralblatt für Geologie und Paläontologie, I, 7-8, 813-852.

Miocene climate as recorded on slope carbonates : examples from Malta (Central Mediterranean) and Northeastern Australia (Marion Plateau, ODP LEG 194)

NASA Astrophysics Data System (ADS)

John, Cédric Michaël

2003-08-01

This study investigated the slope carbonates of two Miocene carbonate systems: the Maltese Islands (in the Central Mediterranean) and the Marion Plateau (Northeastern Australia, drilled during ODP Leg 194). The aim of the study was to trace the impact of the Miocene cooling steps (events Mi1-Mi6) in these carbonate systems, especially the Mi3 event, which took place around 13.6 Ma and deeply impacted the marine oxygen isotope record. This event also profoundly impacted oceanographic and climatic patterns, eventually leading to the establishment of the modern ice-house world. In particular, East Antarctica became ice covered at that period. The rational behind the present study was to investigate the impact that this event had on shallow water systems in order to complement the deep-sea record and hence acquire a more global perspective on Miocene climate change. The Maltese Islands were investigated for trends in bulk-rock carbon and oxygen isotopes, as well as bulk-rock mineralogy, clay minerals analysis and organic geochemisty. Results showed that the mid Miocene cooling event deeply impacted sedimentation at that location by changing sedimentation from carbonate to clay-rich sediments. Moreover, it was discovered that each phase of Antarctic glaciation, not just the major mid Miocene event, resulted in higher terrigenous input on Malta. Mass accumulation rates revealed that this was linked to increased runoff during periods when Antarctica was glaciated, and thus that the carbonate sediments were “diluted” by clay-rich sediments. The model subsequently developed to explain this implies feedback from Antarctic glaciations creating cold, dense air masses that push the ITCZ Northward, thus increasing precipitation on the North African subcontinent. Increased precipitation (or stronger African monsoon) accelerated continental weathering and runoff, thus bringing more terrigenous sediment to the paleo-location of the slope sediments of Malta. Spectral analysis of carbonate content and organic matter geochemical analysis furthermore suggest that the clay-rich intervals are similar to sapropelic deposits. On the Marion Plateau, trends in oxygen and carbon isotopes were obtained by measuring Cibicidoides spp foraminifers. Moreover, carbonate content was reconstructed using a chemical method (coulometer). Results show that the mid Miocene cooling step profoundly affected this system: a major drop in accumulation rates of carbonates occurs precisely at 13.8 Ma, around the time of the East Antarctic ice sheet formation. Moreover, sedimentation changes occurred at that time, carbonate fragments coming from neritic environments becoming less abundant, planktonic foraminifer content increasing and quartz and reworked glauconite being deposited. Conversely, a surprising result is that the major N12-N14 sea-level fall occurring around 11.5 Ma did not impact the accumulation of carbonates on the slope. This was unexpected since carbonate platform are very sensitive to sea-level changes. The model developed to explain that mass accumulation rates of carbonates diminished around 13.6 Ma (Mi3 Event) instead of 11.5 Ma (N12-N14 event), suggests that oceanic currents were controlling slope carbonate deposition on the Marion Plateau prior to the mid-Miocene, and that the mid Miocene event considerably increase their strength, hence reducing the amount of carbonate being deposited on slope sites. Moreover, by combining results from deep-sea oxygen isotopes with sea-level estimates based on coastal onlaps made during Leg 194, we constrain the amplitude of the N12-N14 sea-level fall to 90 meters. When integrating isotopic results from this study, this amplitude is lowered to 70 meters. A general conclusion of this work is that the mid Miocene climatic shift did impact carbonate systems, at least at the two locations studied. However, the nature of this response was highly dependant on the regional settings, in particular the presence of land mass (Malta) and the absence of a barrier to shelter from the effects of open ocean (Marion Plateau). Im Rahmen dieser Doktorarbeit wurden die Hangkarbonate von zwei miozänen heterozoischen Karbonatsystemen näher untersucht: die Malta Inselgruppe (zentrales Mittelmeer) und das Marion Plateau (Nordost Australien, ODP Leg 194). Die Auswirkungen der mittelmiozänen Abkühlung (Mi3), die auf 13.6 Ma datiert wird und starken Einfluß auf die Sauerstoffisotopenkurve hatte, in den oben genannten Flachwassersystemen stellten das Ziel dieser Arbeit dar. Dieses Abkühlungsereignis beeinflußte außerdem sehr stark die ozeanographischen und klimatischen Muster, die im weiteren Verlauf zum modernen Eishausklima führten. So steht insbesondere die Vereisung von Ostantarktika mit diesem Ereignis in Verbindung. Diese Arbeit untersucht den Einfluß dieses Ereignisses auf Flachwassersysteme, um vorliegende Untersuchungen in Tiefwassersystemen zu ergänzen und so zum globalen Verständnis des miozänen Klimawechsels beizutragen. Die Profile auf der Maltainselgruppe wurden mit Hilfe von Kohlenstoff- und Sauerstoffisotopen Auswertungen im Gesamtgestein, Gesamtgesteinmineralogie, Tonmineralanalyse und organischer Geochemie untersucht. Durch einen Wechsel von karbonatischeren zu tonigeren Sedimenten beeinflußte das mittelmiozäne Abkühlungsereignis die Sedimentation in diesem Gebiet sehr stark. Weiterhin wurde beobachtet, daß jede Phase der antarktischen Vereisung, nicht nur das mittelmiozäne Hauptereignis, zu einem erhöhten terrigenen Eintrag in den Hangsedimenten der Maltainselgruppe führte. Akkumulationsraten zeigen, daß dieser erhöhte terrigene Eintrag den einzelnen Vereisungsperioden zusammenhängt und die karbonatischen Sedimente durch tonreiche Sedimente “verunreinigt” wurden. Das daraufhin entwickelte Modell erklärt diesen erhöhten terrigenen Eintrag mit einer nordwärtigen Verlagerung der innertropischen Konvergenzzone durch die Bildung von kalten, dichten Luftmassen, die zu verstärkten Niederschlägen in Nordafrika führten. Diese verstärkten Niederschläge (oder verstärkter afrikanischer Monsun) beeinflußten die kontinentale Verwitterung und den Eintrag, mit der Folge, daß verstärkt terrigene Sedimente im Bereich der Hangsedimente der Maltainselgruppe abgelagert wurden. Die tonreichen Intervalle weisen Ähnlichkeiten zu sapropelischen Ablagerungen auf, was mit Hilfe der Spektral analyse des Karbonatgehalts und der geochemischen Analyse des organischen Materials gezeigt wurde. Auf dem Marion Plateau wurden die Sauerstoff- und Kohlenstoffisotopenkurven anhand von Foraminiferen der Gattung Cibicidoides spp. rekonstruiert. Der Karbonatgehalt wurde mit Hilfe einer chemischen Methode (Coulometer) ermittelt. Genauso wie die Sedimente der Maltainselgruppe beeinflußte das mittelmiozäne Abkühlungsereignis (Mi3) auch die Sedimente auf dem Marion Plateau. So kam es bei 13,8 Ma, in etwa zur Zeit der Vereisung von Ostantarktika, zu einem Abfall der Karbonatakkumulationsraten. Weiterhin traten Änderungen in der Zusammensetzung der Sedimente auf, so nehmen neritische Karbonatfragmente ab, der planktische Foraminiferengehalt nimmt zu und es wurden verstärkt Quarz und Glaukonit abgelagert. Ein überraschendes Ergebnis ist die Tatsache, daß der große N12-N14 Meeresspiegelabfall um 11,5 Ma die Akkumulationsraten der Karbonate auf dem Hang nicht beeinflußte. Dieses Ergebnis ist umso erstaunlicher, da Karbonatplattformen normalerweise sehr sensitiv auf Meeresspiegeländerungen reagieren. Der Grund, warum sich die Karbonatakkumulationsraten schon um 13,6 Ma (Mi3) und nicht erst um 11,5 Ma (N12-N14) verringerten, liegt in der Tatsache, daß die ozeanischen Strömungen die Karbonatsedimentation auf dem Hang des Marion Plateau schon im Miozän kontrollierten. Das mittelmiozäne Ereignis (Mi3) erhöhte die Stärke diese Strömungen und als eine Ursache wurde die Karbonatakkumulation auf den Hängen reduziert. Die Amplitude des N12-N14 Meeresspiegelabfalls liegt bei 90 m unter der Berücksichtigung der Sauerstoffisotopendaten aus der Tiefsee und Berechnungen des Meeresspiegels anhand des “coastal onlaps”, die während Leg 194 gemacht wurden. Die Isotopendaten dieser Arbeit weisen hingegen auf einen verringerten Meeresspiegelabfall von 70 m hin. Als allgemeine Schlußfolgerung kann gesagt werden, daß der mittelmiozäne Klimaumschwung die Karbonatsysteme zumindest an den beiden untersuchten Lokalitäten beeinflußt hat. Allerdings waren die Auswirkungen sehr von den unterschiedlichen lokalen Gegebenheiten abhängig. Insbesondere wirkten sich die Anwesenheit einer Landmasse (Malta) und die Abwesenheit einer Barriere vor den Einflüssen des offenen Ozeans (Marion Plateau) stark auf die Ablagerung der Karbonate aus.

Estimation of the genetic correlations between twisted legs and growth or conformation traits in broiler chickens.

PubMed

Bihan-Duval, E L; Beaumont, C; Colleau, J J

1997-01-12

Genetic correlations between two types of leg deformities, valgus and varus angulations, and some growth or conformation traits were estimated in two commercial broiler strains. 14 264 chickens of both sexes in line A were measured for leg defects at 6 weeks and body weight at 3 (BW3) or 6 (BW6) weeks. The same measures were taken in line B on 8 164 chickens, as well as breast angle (BRA) and breast meat yield (BRM) at 6 weeks on 70% of the male birds. The multinomial logit model previously developed for the genetic analysis of valgus and varus deformities was extended to deal with the joint analysis of one unordered categorical trait and one continuous variable. The model assumed a competition between latent susceptibility variates related to the various deformities and linearly dependent on the continuous performances. Location parameters for latent susceptibilities and continuous trait were estimated by the 'Maximum A Posteriori' approach and dispersion parameters by the 'Maximum Marginal Likelihood' using a tilda-hat approximation. The genetic model took into account the effects of the sire, maternal grandsire and dam within maternal grandsire. As described in a previous study, leg deformities showed moderate heritabilities. Mean heritability estimate for both lines, based on the sire/maternal-grandsire (S/MGS) component, was equal to 0.22 for valgus and varus; when based on the dam component, mean estimates were equal to 0.37 and 0.29 for the two deformities respectively. Except for BRA, heritability of growth and conformation traits appeared to be smaller when based on S/MGS component (from 0.18 to 0.47) than on dam component (from 0.41 to 0.63). Very low genetic correlations were found between susceptibilities to leg deformities and growth performances: average estimates for both lines of the genetic correlation with BW3 were -0.03 and -0.05 for valgus and varus respectively. Respective genetic correlations with BW6 were estimated to be +0.05 and +0.01. According to a simulation study these small estimates were unlikely to be due to the negative back effects of severe disorders on growth performances. According to these results, including leg defects in breeding schemes would not delay improvement on growth through unfavourable genetic correlations. Susceptibility to valgus deformity appeared to be genetically independent of conformation traits (genetic correlation was estimated to be -0.06 and -0.08 with BRA and BRM respectively), whereas moderate unfavourable genetic correlations were found for varus (+0.16 and +0.19 with BRA and BRM respectively). Care must be taken when considering the impact of the actual intensive selection for greater conformation on the incidence of varus deformity. RÉSUMÉ: Les corrélations génétiques entre deux types de déformations osseuses, le valgus et le varus, et des caractères de croissance et de conformation ont été estimées dans deux lignées commerciales de poulet de type chair. Dans la lignée "A", 14 264 poulets des deux sexes ont été mesurés pour les problèmes de pattes à 6 semaines, ainsi que pour le poids vif aux âges de 3 et 6 semaines. Ces mêmes mesures ont été faites dans la lignée "B"sur 8 164 poulets; on disposait en plus pour un échantillon des animaux de cette lignée de la mesure de l'angle de poitrine et du rendement en filet à 6 semaines. Des développements du modèle logistique multinomial déjà utilisé pour l'analyse génétique des valgus et varus ont été réalisés pour permettre l'analyse conjointe de plusieurs caractères discrets non ordonnés et d'une variable continue. Le modèle d'analyse fait l'hypothèse d'une compétition entre plusieurs variables sous-jacentes de sensibilité aux déformations, dépendant linéairement de la performance continue. Les paramètres de position pour les sensibilités sous-jacentes et le caractère continu ont été estimés par l'approche bayésienne du "Maximum A Posteriori"et les paramètres de dispersion par une approximation de type tilde-hat du "Maximum de Vraisemblance Marginale". Le modèle génétique d'analyse comprenait les effets des père, grand-père maternel et mère intra grand-père. Comme démontré dans une étude précédente, la sensibilité aux problèmes de patte présente une héritabilité modérée. En moyenne sur les deux lignées, l'estimation obtenue par la voie père/grand-père maternel (P-GPM) est de 0.22 pour les deux déformations et celle pour la voie mère de 0.37 pour le valgus et de 0.29 pour le varus. A l'exception de l'angle de poitrine, l'héritabilité des caractères de croissance et de conformation apparaît largement supérieure par la voie mère (de 0.41 à 0.63) que par la voie P-GPM (de 0.18 à 0.47). Les corrélations génétiques entre les sensibilités aux déformations osseuses et les performances de croissance apparaissent très faibles: la moyenne des estimations de la corrélation avec le poids vif à 3 semaines est de -0.03 pour le valgus et -0.05 pour le varus. Les corrélations avec le poids à 6 semaines sont du même ordre, estimées à respectivement +0.05 et +0.01 pour les valgus et varus. Une étude par simulation a permis de vérifier que ces faibles corrélations n'étaient pas dues à des biais éventuels liés aux effets secondaires négatifs des pathologies sévères sur les performances de croissance. D'après ces rèsultats, la prise en compte en sélection de la sensibilité aux problèmes de pattes n'introdurait pas, par une corrélation génétique défavorable, de réponse indirecte négative sur le poids. Si la sensibilité au valgus apparaît génétiquement indépendante des caractères de conformation (avec des corrélations génétiques avec l'angle de poitrine et le pourcentage de filet estimées à -0.06 et -0.8 respectivement), la liaison génétique apparaît plutôt défavorable pour le varus: +0.16 et +0.19 respectivement avec l'angle et le pourcentage de filet. Ces résultats doivent inciter à surveiller l'impact sur l'incidence des varus des fortes pressions de sélection appliquées actuellement sur les caractères de conformation. ZUSAMMENFASSUNG: Genetische Korrelationen zwischen verbogenen Füßen und Wachstums- und Formmerkmalen in Broilern Genetische Korrelationen zwischen 2 Arten von Beindeformationen, Valgus und Varus Angulationen, und einigen Wachtums- und Formmerkmalen wurden bei zwei kommerziellen Broiler Herkünften geschätzt, 14 264 Hühner beiderlei Geschlechter wurden in Linie A auf Beinfehler bei 6 Wochen Alter und Körpergewicht bei 3 (BW3) und 6 Wochen (BW6) untersucht, in Linie B 8 164 Tiere, wo aber auch Brustwinkel (BRA) und Brustfleisch (BRM) von ca. 70% der Hähne erhoben worden ist. Das für die genetische Analyse von Valgus und Varus Deformationen entwickelte multinomiale logit Modell wurde für die gemeinsame Analyse eines ungeordneten kategorischen Merkmals und einer kontinuierlichen Variablen erweitert. Dieses unterstellt Kompetition zwischen latenter Anfälligkeiten für verschiedene Deformationen und lineare Beziehung zu kontinuierlich verteilter Leistung. Lokationsparameter wurden mittels "Maximum A Posteriori" Ansatz und Dispersionsparameter mittels "Maximum Marginaler Likelihood" unter Verwendung von 'tilde-hat' Approximation geschätzt. Das genetische Modell berücksichtigte Vater-, maternale Großvater- und Muttertier-innerhalb der letzteren-Wirkungen. Beindeformationen zeigen mittlere Heritabilitätswerte, 0.22 für Valgus and Varus aus Vater/maternalem Großvater Komponenten, 0.37 bez. 0.29 aus der Muttertierkomponente. Mit Ausnahme von BRA waren Heritabilitätswerte für Wachstum- und Formmerkmale aus S/MGS-Komponenten (0.18-0.47) kleiner als die aus Muttertierkomponenten (0.41-0.63). Genetische Korrelationen zwischen letzeren und Anfällikeiten waren sehr niedrig: zwischen BW3 und Valgus und Varus -0.03 bzw. -0.05, BW6 +0.05 und 0.01. Simulation zeigte, daß die niedrigen Werte kaum auf negative Rückwirkung der Defekte auf Leistung zurückzuführen sind, sodaß deren Berücksichtigung in der Selektion den Zuchtfortschritt nicht beeinträchtigen sollte. Valgusdeformation scheint genetisch unabhängig von Formmerkmalen zu sein (r(G) -0.06, -0.08 mit BRA und BRM), während Varus mäßig ungünstige Korrelationen zeigt (+0.16, -0.19 mit BRA und BRM), sodaß Selektion auf Bemuskelung dies zu beachten hat. 1997 Blackwell Verlag GmbH.

The effects of topical mesenchymal stem cell transplantation in canine experimental cutaneous wounds

PubMed Central

Kim, Ju-Won; Lee, Jong-Hwan; Lyoo, Young S; Jung, Dong-In; Park, Hee-Myung

2013-01-01

Background Adult stem cells have been widely investigated in bioengineering approaches for tissue repair therapy. We evaluated the clinical value and safety of the application of cultured bone marrow-derived allogenic mesenchymal stem cells (MSCs) for treating skin wounds in a canine model. Hypothesis Topical allogenic MSC transplantation can accelerate the closure of experimental full-thickness cutaneous wounds and attenuate local inflammation. Animals Adult healthy beagle dogs (n = 10; 3–6 years old; 7.2–13.1 kg) were studied. Methods Full-thickness skin wounds were created on the dorsum of healthy beagles, and allogenic MSCs were injected intradermally. The rate of wound closure and the degree of collagen production were analysed histologically using haematoxylin and eosin staining and trichrome staining. The degree of cellular proliferation and angiogenesis was evaluated by immunocytochemistry using proliferating cell nuclear antigen-, vimentin- and α-smooth muscle actin-specific antibodies. Local mRNA expression levels of interleukin-2, interferon-γ, basic fibroblast growth factor and matrix metalloproteinase-2 were evaluated by RT-PCR. Results Compared with the vehicle-treated wounds, MSC-treated wounds showed more rapid wound closure and increased collagen synthesis, cellular proliferation and angiogenesis. Moreover, MSC-treated wounds showed decreased expression of pro-inflammatory cytokines (interleukin-2 and interferon-γ) and wound healing-related factors (basic fibroblast growth factor and matrix metalloproteinase-2). Conclusion and clinical importance Topical transplantation of MSCs results in paracrine effects on cellular proliferation and angiogenesis, as well as modulation of local mRNA expression of several factors related to cutaneous wound healing. Résumé Contexte Les cellules souches adultes ont été largement étudiées dans les approches de bio-ingénierie pour la thérapie de réparation tissulaire. Nous évaluons l'efficacité clinique et la sécurité de l'application de cellules souches mésenchymateuses allogéniques en culture dérivées de moelle osseuse (MSCs) pour le traitement de plaies cutanées dans un modèle canin. Hypothèse La transplantation de MSC allogénique topique peut accélérer la fermeture en toute épaisseur de plaies cutanées expérimentales et atténuer l'inflammation locale. Sujets Des chiens beagles adultes sains (n = 10; 3–6 ans; 7.2–13.1 kg) ont été étudiés. Méthodes Des plaies cutanées en pleine épaisseur ont été crées sur la face dorsale des beagles sains et des MSCs allogènes ont été injectées par voie intradermique. Le taux de cicatrisation et le degré de production de collagène ont été analysés sur le plan histologique par colorations à l'hématoxyline et éosine et par trichrome. Le degré de prolifération cellulaire et d'angiogénèse ont été évalués par immunohistochimie à l'aide d'anticorps spécifiques d'antigène nucléaire de prolifération cellulaire, de vimentine et d'actine de muscle lisse α. Les taux d'expression local d'ARNm d'interleukine-2, d'interféron-γ, du facteur de croissance basique de fibroblaste et de métalloprotéinase-2 de matrice, ont été évalués par RT-PCR. Résultats Comparé avec les plaies traitées par excipient, les plaies traitées par les MSCs ont montré une plus rapide cicatrisation et une augmentation de synthèse de collagène, de prolifération cellulaire er d'angiogénèse. En outre, Les plaies traitées au MSC ont montré une expression diminuée de cytokines pro-inflammatoires (interleukine-2 et interféron-γ) et des facteurs liés à la cicatrisation (facteur de croissance basique de fibroblaste et métalloprotéinase-2 de matrice). Conclusion et importance clinique La transplantation topique de MSCs résulte en des effets paracrines de prolifération cellulaire et d'angiogénèse ainsi qu'en une modulation de l'expression locale d'ARNm de plusieurs facteurs liés à la cicatrisation cutanée. Resumen Introducción Las células madre de adultos se han estudiado extensivamente en estrategias de bioingeniería para la reparación de tejidos. Hemos evaluado el valor clínico y la seguridad de la aplicación de células madre mesenquimales (MSCs) alogenéicas derivadas de la medula ósea para tratar las heridas de la piel en un modelo canino. Hipótesis El transplante tópico alogenéico de MSCs puede acelerar la cicatrización de heridas cutáneas experimentales de todo el grosor de la piel y disminuir la inflamación local. Animales Se estudiaron perros de raza Beagle sanos adultos (n=10; de 3-6 años de edad; 7,2-13,1 kg de peso). Métodos Se crearon heridas de todo el grosor de la piel en el dorso de perros Beagle sanos, y se inyectaron MSCs alogenéicas intradérmicamente. El ritmo de reparación de la herida y el grado de producción de colágeno se analizaron histológicamente utilizando tinciones de hematoxilina-eosina y tricrómico. El grado de proliferación celular y la angiogenesis se evaluaron mediante inmunohistoquímica utilizando anticuerpos específicos para el antígeno de proliferación celular nuclear (PCNA), vimentina y α-actina de músculo liso. La expresión local de mRNA para interleuquina-2 (IL-2), interferón- γ (IFN- γ), factor básico de crecimiento de fibroblastos (BFGF) y metaloproteinasa de matriz-2 se evaluaron mediante RT-PCR. Resultados comparado con las heridas tratadas solo con el vehículo, las heridas tratadas con MSCs mostraron una reparación más rápida y un aumento en la producción de colágeno, proliferación celular y angiogenesis. Además, las heridas tratadas con MSCs mostraron una expresión aumentada de citoquinas proinflamatorias (IL-2 e IFN- γ) y factores relacionados con la reparación de la herida (BFGF y metaloproteinasa de matriz-2). Conclusión e importancia clínica El transplante tópico de MSCs resulta en efectos paracrinos en la proliferación celular y angiogenesis, así como en la modulación de la expresión de mRNA de diversos factores relacionados con la cicatrización de heridas. Zusammenfassung Hintergrund Adulte Stammzellen sind für ihre biotechnologische Verwendung bei der Wiederherstellung von Geweben bereits weit reichend erforscht. Wir haben die klinische Bedeutung und Sicherheit der Applikation von kultivierten allogenen mesenchymalen Stammzellen (MSCs) aus dem Knochenmark zur Behandlung von Hautwunden in einem caninen Modell evaluiert. Hypothese Die topische allogene MSC Transplantation kann den Wundverschluss experimenteller Hautwunden (Brandwunden Grad III) beschleunigen und die lokale Entzündung mildern. Tiere Erwachsene gesunde Beagles (n=10; 3-6 Jahre alt; 7,2-13,1kg) wurden in der Studie verwendet. Methoden Es wurden Hautwunden 3. Grades am Rücken der gesunden Beagles verursacht und allogene MSCs intradermal injiziert. Die Schnelligkeit des Wundverschlusses und das Ausmaß der Kollagenproduktion wurden histologisch mittels Hämatoxylin und Eosin Färbung und Trichromfärbung untersucht. Das Ausmaß der zellulären Proliferation und der Angiogenese wurde mittels Immunzytochemie unter Verwendung von Proliferating-Cell-Nuclear-Antigen, Vimentin und Alpha Smooth Muscle Actin-spezifischen Antikörpern evaluiert. Die lokale Exprimierung von mRNA von Interleukin-2, Interferon-γ, Basic Fibroblasten Wachstumsfaktor und Matrix Metalloproteinase-2 wurde mittels RT PCR evaluiert. Ergebnisse Im Vergleich zu den Wunden, die nur mit dem Trägermedium behandelt worden waren, zeigten die mit MSC-behandelten Wunden einen rascheren Verschluss und eine erhöhte Kollagensynthese, zelluläre Proliferation und Angiogenese. Darüber hinaus zeigten MSC-behandelte Wunden eine verminderte Exprimierung pro-entzündlicher Zytokine (Interleukin-2 und Interferon-γ) und Wundheilungsfaktoren (Basic Fibroblasten Wachstumsfaktor und Matrix Metalloproteinase-2). Schlussfolgerung und klinische Bedeutung Die topische Transplantation von MSCs resultiert in parakrinen Effekten auf die zelluläre Proliferation und Angiogenese sowie die Modulierung lokaler mRNA Exprimierung verschiedener Faktoren, die mit der Wundheilung der Haut im Zusammenhang stehen. 摘要 背景 以成体干细胞的生物工程法用于组织修复治疗已被广泛研究。将骨髓培养得到的外源性间充质干细胞(MSCs)用于犬模型上治疗皮肤创伤,我们来评估其临床价值和安全性。 假设 局部外源性MSC移植能使试验的皮肤创口全层愈合加快,并使局部炎症减轻。 动物 研究成年健康比格犬(n = 10;3–6 岁;7.2–13.1 kg)。 方法 在健康的比格犬背部创造全层皮肤创口,皮内注射外源性MSCs。使用苏木精和伊红染色法和三色染色法,从组织结构上分析伤口愈合率和胶原产生的程度。通过免疫细胞化学使用增殖细胞核抗原、维生素和α-平滑肌肌动蛋白-特定抗体,评估细胞增殖和血管生成程度。通过RT PCR评估白介素-2、γ-干扰素、基纤维母细胞生长因子和基质金属蛋白酶-2局部mRNA表达等级。 结果 与媒介物治疗创口相比,MSC治疗创口显示出更快的创口愈合,以及胶原合成、细胞增殖和血管生成增加。 此外,MSC治疗创口显示出炎性细胞因子(白介素-2和γ-干扰素)和与创口愈合相关因子(碱性成纤维细胞生长因子和基质金属蛋白酶-2)表达减少。 结论和临床价值 局部移植MSCs造成了对细胞增殖和血管生成的旁分泌作用,也同样引起几个与皮肤创伤愈合相关因子局部mRNA表达的调节。 要約 背景 成熟した幹細胞は組織修復療法に対して生物工学的なアプローチで広く研究されている。著者らは培養した骨髄由来の同種異系の間葉系肝細胞(MSCs)を犬の皮膚創傷の治療に応用し、臨床的な価値と安全性を評価した。 仮説 同種異系MSCの局所への移植は実験的な皮膚全層創傷の閉鎖と炎症の軽減を加速する可能性がある。 供与動物 成熟した健常ビーグル犬(n = 10; 3–6 歳齢; 7.2–13.1 kg)を用いた。 方法 健常ビーグルの背部に皮膚全層潰瘍を作成し、同種異系MSCを皮内に注射した。創傷閉鎖率とコラーゲン産生度をヘマトキシリン染色トリクローム染色を用いて組織学的に解析した。細胞増殖度と血管新生は核内増殖抗原−、ビメンチン−、α−平滑筋アクチン−特異的抗体を用いて免疫組織化学染色で評価した。局所のインターロイキン−2、インターフェロンγ、塩基性線維芽細胞増殖因子とマトリックスメタロプロテアーゼ2のmRNA発現レベルをRT-PCRで評価した。 結果 賦形剤のみで治療した創傷と比較し、MSCで治療した創傷はより早期に閉鎖し、コラーゲン合成の増加、細胞増殖や血管新生を示した。さらに、MSCで治療した創傷は炎症後サイトカイン(インターロイキン−2とインターフェロン−γ)と創傷治癒関連因子(塩基性線維芽細胞増殖因子とマトリックスメタロプロテアーゼ−2)の発現が減少していた。 結論と臨床的な重要性 MSCの局所への移植により細胞増殖と血管新生に対してはパラクライン効果を示すのと同時に,皮膚創傷治癒に関連する様々な因子の局所mRNA発現を調節した。 PMID:23432413

HWHAP_Ep9_ International Space Station 2 Research

NASA Image and Video Library

2017-09-08

>> HOUSTON, WE HAVE A PODCAST! WELCOME TO THE OFFICIAL PODCAST OF THE NASA JOHNSON SPACE CENTER, EPISODE 9: INTERNATIONAL SPACE STATION #2 RESEARCH. I’M GARY JORDAN AND I’LL BE YOUR HOST TODAY. SO IF YOU’RE NEW TO THE PODCAST, THIS IS THE ONE WHERE WE BRING ON EXPERTS, NASA SCIENTISTS, ENGINEERS, ASTRONAUTS, AND THEY TELL YOU EVERYTHING YOU NEED TO KNOW, ALL THE COOLEST PARTS ABOUT NASA. SO TODAY WE’RE TALKING ABOUT SPACE STATION SCIENCE WITH TARA RUTTLEY. SHE’S THE ASSOCIATE PROGRAM SCIENTIST FOR THE SPACE STATION HERE AT THE NASA JOHNSON SPACE CENTER IN HOUSTON, TEXAS, AND WE HAD A GREAT DISCUSSION ABOUT WHAT KINDS OF RESEARCH WE’RE DOING ABOARD THE ORBITING COMPLEX RIGHT NOW, WHAT WE’RE LEARNING, AND WHY IT’S IMPORTANT. SO WITH NO FURTHER DELAY, LET’S GO LIGHT SPEED AND JUMP RIGHT AHEAD TO OUR TALK WITH DR. TARA RUTTLEY. ENJOY. [ MUSIC ] >> T MINUS FIVE SECONDS AND COUNTING. MARK. [ INDISTINCT RADIO CHATTER ] >> HOUSTON, WE HAVE A PODCAST. [ MUSIC ] >> WELL THANK YOU FOR COMING ON AND FOR TAKING THE TIME TO COME ON THE PODCAST. I’M EXCITED ABOUT THIS TOPIC BECAUSE YOU THINK ABOUT THE INTERNATIONAL SPACE STATION-- GIANT, FOOTBALL FIELD-SIZED SPACESHIP, HUGE SOLAR ARRAYS-- LIKE, THAT’S COOL, BUT WHAT ARE THEY DOING INSIDE? SO THAT’S KIND OF WHAT I WANTED TO TALK ABOUT TODAY, AND YOU’RE THE PERFECT PERSON TO DO THAT AS THE ASSOCIATE PROGRAM SCIENTIST FOR THE INTERNATIONAL SPACE STATION PROGRAM. SO WELCOME, WELCOME. FIRST THING I WANT TO SAY, ESPECIALLY IN YOUR POSITION, WE DO SCIENCE-- YOU KNOW, IF SOMEONE WERE EVER TO ASK YOU, “WHAT DO YOU DO? WHAT DO YOU DO UP IN THE SPACE STATION?” YOU’D SAY, “WE DO SCIENCE. WE DO SCIENTIFIC RESEARCH,” CORRECT? IS THAT-- AM I FAIR IN SAYING THAT? >> YES, AND THEN THEY SAY, “WHY, WHY? DON’T WE HAVE LABORATORIES ON EARTH?” AND THEN I SAY, YOU KNOW, “IT’S THIS HUGE ORBITING LABORATORY! THINK OF EVERY EXPERIMENT YOU’VE EVER DONE IN SCHOOL.” >> OKAY. >> “AND YOU KNOW, YOU CAN CONTROL TEMPERATURE, AND LIGHTING, AND ALL THESE DIFFERENT THINGS. BUT THE ONE THING YOU CAN’T CONTROL IS THAT YOU ALWAYS HAVE THAT GRAVITY VECTOR THERE.” >> STUPID GRAVITY. >> --EXPERIMENTS YOU’VE EVER DONE-- SUCH A FORCE TO BE RECKONED WITH! “ANY EXPERIMENT YOU’VE EVER DONE ON EARTH, WHAT WOULD HAPPEN IF YOU COULD TAKE GRAVITY AWAY FROM THAT, AND WHAT WOULD YOU LEARN?” AND THEN THE LIGHT BULBS START TO GO OFF AND THEY GO, “OH, OKAY.” AND THE NEXT QUESTION IS WHAT WE’LL TALK ABOUT FOR THE REST OF THIS PODCAST, THIS, “WELL, WHAT DO YOU GET OUT OF IT?” >> YEAH, NO, THAT’S PERFECT. I MEAN, IF YOU COULD-- THERE’S ALWAYS-- WHEN YOU TALK ABOUT SCIENTIFIC RESEARCH, YOU HAVE CERTAIN THINGS THAT YOU JUST HAVE TO DEAL WITH, RIGHT? SO GRAVITY, I THINK, WOULD BE ONE OF THOSE THINGS. IT’S SOMETHING YOU CAN’T-- IT’S A FIXED-- I’M SORRY, I HAVEN’T TAKEN A SCIENCE CLASS IN A LONG TIME, BUT IS IT A FIXED SOMETHING VERSUS A VARIABLE? >> IT IS A FIXED-- IT’S AN INDEPENDENT VARIABLE. >> OKAY, YEAH. >> IT’S SOMETHING THAT-- WELL, AND IT’S SOMETHING THAT-- WELL, IT’S SOMETHING YOU CAN’T CHANGE. SO YOU CAN CHANGE TEMPERATURE, PRESSURE, LIGHTING, HEAT-- YEAH, ALL THOSE THINGS. YEAH, BUT GRAVITY, 9.81 METERS PER SECOND SQUARED-- BRINGING YOU BACK A LITTLE BIT-- >> ALL RIGHT, I WAS COMING BACK. >> AND WE’VE ALL-- THIS WHOLE PLANET, EVERYTHING ON IT, EVERY LIVING SYSTEM, EVERY PHYSICAL SYSTEM HAS EVOLVED AROUND THAT GRAVITY VECTOR. SO IT’S WHAT WE’RE USED TO, IT’S WHAT WE CAN PREDICT OUR THEORIES AROUND, AND IT’S WHAT WE CAN-- IT’S HOW WE KNOW WHAT’S GOING TO HAPPEN NEXT. BUT SO WHEN YOU GO UP AND YOU TRY ALL THESE DIFFERENT SCIENCE EXPERIMENTS IN THE MICROGRAVITY ENVIRONMENT, YEAH, IT’S NOT ALWAYS PREDICTABLE. AND THAT’S WHAT WE WANT TO USE THAT ENVIRONMENT OF THE SPACE STATION FOR. IT’S LIKE, WHAT HAPPENS NEXT IF WE SEND THIS UP? AND THEN, AS HUMAN BEINGS WE WANT TO FIND OUT, WELL, HOW DO WE TAKE THAT INFORMATION AND LEVERAGE IT TO OUR BENEFITS, EITHER ON EARTH OR HELP US GO EXPLORE FURTHER. >> YEAH, NO, THAT’S A PERFECT OVERVIEW. THAT’S GREAT. THAT’S AWESOME. WELL, THAT’S GREAT. I MEAN, YOU’RE IN THE PERFECT POSITION, ESPECIALLY IF YOU’RE THERE. BUT SO, WHAT’S SOMETHING-- I MEAN, JUST AS A GENERAL EXAMPLE BEFORE WE START TO GET GOING-- WHAT’S SOMETHING THAT YOU’RE LIKE, “HEY, I WONDER WHAT WOULD HAPPEN TO THIS IF WE BROUGHT IT UP TO--” WHAT’S LIKE ONE OF THE COOLER THINGS THAT YOU CAN THINK OF? WHAT WOULD HAPPEN TO BLANK? >> YOU KNOW, I’M GOING TO-- I DON’T KNOW-- I DON’T HAVE A PERSONAL-- MY HEAD RUNS THROUGH ALL KINDS OF SCENARIOS, SO I’VE NOT BEEN ABLE TO SATISFY MYSELF PERSONALLY WITH WHAT WOULD HAPPEN WITH A PARTICULAR EXPERIMENT. BUT THE ONE I GET ASKED THE MOST IS ABOUT DEVELOPMENT. DEVELOPMENT OF-- YOU KNOW, NEXT GENERATION OF A PARTICULAR LIVING ORGANISM. AND SO-- >> OH, LIVING THINGS, OKAY. >> YEAH, LIKE REPRODUCING IN SPACE, AND WHAT HAPPENS WITH THE OFFSPRING, AND DO THEY TURN OUT FUNKY, OR NORMAL, OR ANYTHING LIKE THAT? SO I MEAN, WE’RE NOT QUITE THERE, ALTHOUGH THERE HAVE BEEN A COUPLE OF WHAT WE CALL “MODEL ORGANISMS” THAT-- YOU KNOW, FRUIT FLIES, FOR EXAMPLE, WE CAN SEND UP AND HAVE REPRODUCTION, AND THEN LOOK AT THEIR OFFSPRING AND LOOK AT ANYTHING DIFFERENT THAT MIGHT BE OCCURRING. AND SO FUNDAMENTALLY, I THINK I GET ASKED THAT THE MOST, BECAUSE IT’S SOMETHING WE CAN ALL RELATE TO. IT’S KIND OF WEIRD IN ITSELF, BUT IT’S ALSO, LIKE, IT EXPLAINS A LITTLE BIT ABOUT WHO WE ARE AS LIVING ORGANISMS IN THIS ENVIRONMENT. >> IT’S SO COOL THAT WE HAVE A PLACE TO DO THAT, TOO. LIKE, YOU HAVE THAT QUESTION, LIKE, WHAT WOULD HAPPEN TO-- YOU KNOW, IF WE WERE TO HAVE LIVING THINGS REPRODUCE IN SPACE? OH, THAT’S RIGHT-- WE HAVE A LABORATORY WHERE WE CAN TEST THAT. THAT’S REALLY COOL. >> AND IT’S-- I HAVE TO SAY, YOU KNOW, I’VE BEEN A SPACE GEEK MY WHOLE LIFE, AND I’VE WATCHED ALL THE SHUTTLE EXPERIMENT MISSIONS AND THE DEVELOPMENT OF ISS. AND BEING A SCIENTIST AS I AM, I HAVE TO SAY THAT NOW IS THE GOLDEN AGE FOR SPACE RESEARCH-- MORE THAN EVER BEFORE AND PROBABLY MORE THAN WE’LL EVER SEE AGAIN. NOW IS THE TIME. >> WELL, WE’VE GOT A GIGANTIC LABORATORY TO DO IT, SO I CAN SEE WHY IT’S THE GOLDEN AGE. >> YEAH, SO BY THE WAY, FOR ANYBODY WHO’S LISTENING WHO’S A RESEARCHER OR A STUDENT, IF YOU HAVE AN IDEA FOR SOMETHING THAT YOU THINK YOU COULD DO IN SPACE, WE’RE OPEN-- WE WANT THAT RIGHT NOW. WE’RE OUT THERE TRYING TO GET THE BEST TO USE THIS PLATFORM. >> OOH, OKAY. ALL RIGHT, WE’LL HAVE TO-- AT THE VERY END OF THE PODCAST WE DO LIKE A-- WE PITCH WHERE THEY CAN GO FOR MORE INFORMATION. >> YEAH, I’LL BE HAPPY TO GIVE IT TO YOU. >> I’LL MAKE A NOTE TO SAY WHERE THEY CAN GO-- RESEARCHERS. OKAY, COOL. SO YOU KNOW, ONE OF THE EXPERIMENTS THAT I ALWAYS THINK ABOUT IS-- NOT NECESSARILY EXPERIMENTS, BUT LIKE, WHAT WOULD YOU WANT TO SEND UP TO SPACE THAT WOULD LOOK COOL? AND LIKE, THE PICTURES OF WATER UP THERE. >> OH, YEAH. >> THEY ARE JUST SO COOL. LIKE, YOU KNOW, YOU THINK WATER SPLASHING, MAYBE STICKING TO STUFF, FALLING-- WATERFALLS-- BUT IT DOESN’T FALL. IT FORMS INTO LIKE A BALL, RIGHT? >> I LOVE THAT, YEAH. SO THAT’S A GREAT EXAMPLE. THAT’S ONE OF THE MOST HIGHLY VISIBLE PHENOMENA THAT ALWAYS COMES OUT OF SPACE STATION. AND YOU’RE ALWAYS SEEING ASTRONAUTS PLAY WITH IT, MESS AROUND WITH IT, BUT THE REALLY INTERESTING THING ABOUT FLUID BEHAVIOR, WATER BEHAVIOR IN SPACE IS THAT FOR DECADES WE’VE BEEN LAUNCHING TO SPACE, BUT WE’VE NEVER HAD ANY MODELS, SOFTWARE MODELS, OR MODELS OF FLUID BEHAVIOR THAT-- BASED ON THE MICROGRAVITY ENVIRONMENT THAT WE COULD BUILD PREDICTIONS ON. SO FOR EXAMPLE, IF WE WANT-- YOU KNOW, FLUID TENDS TO HIDE-- YOU KNOW, CRAWL UP CRACKS AND CREVICES IN MICROGRAVITY. ON EARTH, IT’S GOING TO SIT IN YOUR GLASS. YOU CAN STARE AT IT AND KNOW IT’S GOING NOWHERE. >> THAT’S GOOD. >> YEAH, IT’S GOOD, YEAH. THAT’S HOW WE WORK ON EARTH, BUT IN SPACE, THAT STUFF GETS EVERYWHERE. >> RIGHT. >> AND YOU COULD POTENTIALLY LOSE, YOU KNOW, IMPORTANT PARTS OF IT. IT’S A PRECIOUS RESOURCE, FLUID, UP IN SPACE, WHETHER IT’S A PROPELLANT OR IT’S WATER. AND SO WE HAVE NEVER CREATED THE MOST EFFICIENT PROPELLANT TANKS, FOR EXAMPLE, BASED ON THE BEHAVIOR OF WATER OR PROPELLANT IN SPACE. SO WE HAD-- REALLY ONE OF MY FAVORITE EXPERIMENTS WAS A VERY ELEGANT, SIMPLE, HANDHELD EXPERIMENT DEVELOPED BY MARK WEISLOGEL OUT AT PORTLAND STATE UNIVERSITY. AND HE’S A PHENOMENON WITH FLUID BEHAVIOR. AND WHAT WE GOT FROM HIS EXPERIMENTS WAS A WHOLE NEW SET OF OPEN-SOURCE CODE, NOW, UNDERSTANDING HOW FLUID BEHAVES IN SPACE IN DIFFERENT GEOMETRIES OF CONTAINERS-- SO A SQUARE, A TRIANGLE, A HONEYCOMB-- WHATEVER. >> OH. >> HE’S GOT ALL THOSE MODELS, AND NOW, IF YOU AS A RESEARCHER-- OR ANYONE INTERESTED IN BUILDING A PROPELLANT TANK OR A FLUID TANK FOR SPACE-- HAVE A CAD MODEL. YOU CAN GO STICK YOUR DESIGN INTO THAT SOFTWARE PROGRAM AND SEE HOW FLUID’S GOING TO BEHAVE IN YOUR SYSTEM. >> WHOA. >> YEAH, AND SO FOR THE FIRST TIME EVER, WE HAVE THESE MODELS THAT WE CAN DESIGN MORE EFFICIENT PROPELLANT TANKS, MORE EFFICIENT WATER HANDLING SYSTEMS. THAT’S GOING TO HELP US EXPLORE. NOW, ALSO, BECAUSE WE ARE GETTING A BETTER HANDLE ON FLUID BEHAVIOR IN SPACE, WE’RE ALSO ABLE TO APPLY IT TO GROUND WATERING OF OUR AGRICULTURE. >> OH, COOL. >> THE WAY THAT PLANTS TAKE UP WATER IN THE SOIL, IT’S ALL THE SAME-- IT’S CAPILLARY FLOW, IT’S CAPILLARY ACTION, THE WAY THAT WATER MOVES THROUGH A MEDIUM TO GET TO ITS SOURCE. BECAUSE WE TOOK GRAVITY OUT, WE CAN REALLY FOCUS ON LOOKING AT CAPILLARY BEHAVIOR. AND NOW WE CAN APPLY IT TO GROUND-BASED WATERING SYSTEMS, WE CAN APPLY IT TO TINY LITTLE LAB ON CHIPS-- ANYTHING THAT USES FLUID MOVEMENT AND YOU DON’T WANT TO USE A BATTERY, YOU WANT TO LEVERAGE GRAVITY. I MEAN, ALL KINDS OF ADVANCEMENTS ARE COMING OUT OF THIS SIMPLE, ELEGANT SERIES OF RESEARCH THAT CAME OUT OF ISS. SO IT’S REALLY, REALLY COOL. >> THAT’S AMAZING. SO GOING BACK, THOSE CAD MODELS. IS THAT ASSUMING YOUR SYSTEM IS IN A WEIGHTLESS ENVIRONMENT, OR IS THAT FOR ANY SYSTEM? >> THAT’S ASSUMING THAT YOU’RE DESIGNING FOR A WEIGHTLESS ENVIRONMENT. >> I SEE, OKAY, COOL. >> SO IF YOU WANT TO DESIGN FOR THE NEXT VEHICLE THAT, YOU KNOW, THAT WE LAUNCH TO WHEREVER-- MARS, OR STATION, OR WHATEVER-- OR IF YOU’RE A STUDENT AND YOU WANT TO DESIGN AN EXPERIMENT FOR SPACE STATION AND IT’S GOING TO HAVE FLUID IN IT, YOU CAN TAKE YOUR MODEL AND STICK IT IN THERE AND SEE HOW IT BEHAVES. IT’S GREAT STUFF. >> THAT’S AWESOME. YEAH, I’VE SEEN SOME OF THOSE EXPERIMENTS, TOO, AND THEY’RE REALLY COOL. I MEAN, IT’S SOMETHING YOU WOULDN’T NORMALLY THINK ABOUT-- YOU KNOW, YOU PUT FUEL IN A ROCKET AND YOU LAUNCH IT, BECAUSE THE FUEL’S GOING TO GO DOWN TO THE BOTTOM. BUT IN A WEIGHTLESS ENVIRONMENT, IT’S NOT-- IT’S GOING TO FLOAT AROUND, AND ALL OF A SUDDEN YOU’VE GOT FUEL COMING OUT WHENEVER IT HAPPENS TO SNAP TO THAT SIDE, BUT YOU’VE GOT TO FIGURE OUT A PATH IN A WEIGHTLESS ENVIRONMENT TO DO THAT. >> WICKING, WICKING, WICKING. >> WICKING, YEAH. VERY COOL. SO ANOTHER ONE BEFORE WE GO ON KIND OF THE OVERALL KIND OF RESEARCH KIND OF THING IS, YOU KNOW, WHEN I SEE FIRE IN SPACE-- THOSE FIRE EXPERIMENTS THAT THEY’RE DOING, IT’S LIKE A LITTLE SPARK, AND THEN IT FORMS THIS TINY, LIKE, FAINT BLUE BALL. >> YEAH. >> SO WHAT ARE WE LEARNING FROM FIRE? >> SO, YEAH, SO ANOTHER HIGHLY VISUAL ONE-- FIRE AND WATER, OUR BASIC NEEDS. >> WELL, THOSE ARE ALSO THE FIRST ONES THAT COME TO MIND FOR ME. >> IT’S TOTALLY COOL, YEAH. SO WE DO COMBUSTION STUDIES IN SPACE BECAUSE WHEN YOU TAKE THAT GRAVITY VECTOR AWAY, YOU KNOW, THE WAY A FLAME BURNS IT’S GOT LOTS OF DIFFERENT LAYERS AND IT PUTS OFF LOTS OF DIFFERENT PARTICLES, SO TO SPEAK. AND THERE ARE PEOPLE WHO STUDY THAT ON EARTH-- LIKE, THEIR WHOLE LIVES PEOPLE ARE STUDYING FLAMES, JUST LIKE THOSE WHO ARE STUDYING BUBBLES. BECAUSE WE HERE ON EARTH WANT TO LEARN HOW TO BETTER DETECT FIRES, WE WANT TO BE ABLE TO BETTER PUT THEM OUT. >> RIGHT. >> BUT ALSO IN SPACE WE WANT TO DO THE SAME, FOR DIFFERENT REASONS. >> THAT’S FAIR, YEAH. >> AND SO HOW DO FLAMES BEHAVE IN SPACE? WELL, WE’VE BEEN STUDYING THOSE FOR DECADES-- IN FACT, WAY BEYOND-- BEFORE SPACE STATION, EVEN. BUT NOW WE HAVE THIS HUGE FACILITY DEDICATED WITHIN THE LABORATORY FOR ONGOING EXPERIMENTS. AND SO, YOU KNOW, IF YOU’VE SEEN THE IMAGES, YOU SAID, A LITTLE-- THE WAY FLAMES BURN IN TINY LITTLE BALLS, BLUE, TINY LITTLE BULBS-- YOU DON’T HAVE THAT CANDLE-LIKE PEAK AT THE TOP. >> RIGHT. >> RIGHT, BECAUSE IN SPACE THERE’S NO CONVECTION, THERE’S NO-- THERE’S NO-- THINK ABOUT IT-- THERE’S NO DENSITY, THERE’S NO MASS-- THERE’S MASS, BUT THERE’S NOT RELATIVE DENSITY. SO YOU CAN’T HAVE-- ON EARTH, YOUR HOT AIR WILL RISE IN A FLAME. >> RIGHT. >> AND THEN THE COLD AIR WILL SINK TO THE BOTTOM, AND THEN RISE UP AGAIN, RIGHT. BUT THERE’S NO SINKING IN SPACE. EVERYTHING-- THERE’S NO RELATIVE DENSITY. SO YOU DON’T HAVE CONVECTION-- THAT’S WHAT THAT IS. >> GOT IT. >> SO NOW, IN SPACE YOU DON’T HAVE HOT AIR RISING, AND YOUR FLAME BURNS IN A LITTLE BALL UNTIL IT’S EXTINGUISHED. NOW, A REALLY INTERESTING PIECE OF THAT IS WE HAVE FOUND, IN BURNING SOME OF OUR FLUID-- GASOLINE, SO TO SPEAK, OR OUR FLUID PROPELLANTS-- IN SPACE IS THAT WE’VE SEEN EXTINGUISHING, AS NORMAL. AND THEN IN SOME CASES, WE’VE SEEN ALL OF A SUDDEN A REIGNITION EVENT. >> WHOA. >> SO YOU THINK THE FIRE’S OUT, AND THEN-- BOOM-- IT’S BACK AGAIN. >> YEAH. >> AND THAT KIND OF MADE OUR RESEARCHERS SCRATCH THEIR HEAD AND OPEN UP A BRAND NEW PATH OF RESEARCH ON ISS THAT WE WEREN’T ANTICIPATING. BUT THIS KIND OF PHENOMENON IS-- THEY’VE DETERMINED-- IS CALLED A COLD FLAME. >> AH, YES. >> SO YOU HAVE THE IGNITION EVENT, WHICH IS A THERMAL HEAT FLAME, THE SECONDARY COLD FLAME EVENT IS A CHEMICAL FLAME. IT’S REALLY A RESULT OF RECOMBINING OF ELEMENTS IN THE ATMOSPHERE UNDER THOSE CERTAIN ENVIRONMENTAL CONDITIONS. AND IT’S IMPORTANT TO US TO UNDERSTAND IN SPACE BECAUSE, JEEZ, YOU THINK YOU PUT THE FLAME OUT, BUT WHAT IF YOUR PRESSURES-- AND YOU’VE STILL GOT A LITTLE BIT OF MIXING THERE. >> RIGHT. AND IS IT INVISIBLE, OR IS IT A VISIBLE FLAME? >> IT’S A VISIBLE FLAME. >> OKAY, IT IS, OKAY. >> YEAH, AND IT SHOWS UP AS THIS PRETTY TOROIDAL CLOUD-- A DIFFERENT COLOR AND EVERYTHING. >> OH, OKAY. >> HOWEVER, YOU’VE GOT A GOOD POINT-- THERE ARE SOME CAMERAS IN THAT FACILITY THAT WE USE TO LOOK AT DIFFERENT LEVELS OF THE FLAME AND WHAT WE CAN’T SEE VISUALLY AS WELL. AND ALL THOSE IMAGES GO BACK DOWN TO THE EARTH, AND THE INVESTIGATORS-- THERE’S PLENTY, PLENTY OF DATA TO LOOK AT FOR THOSE INVESTIGATORS. >> WOW. >> YEAH, IT’S REALLY FUN. >> SO I MEAN, YOU-- THESE ARE JUST A COUPLE OF THEM, RIGHT? SO JUST-- WE’RE TALKING ABOUT THE FLAME EXPERIMENT, AND WE TALKED BRIEFLY ABOUT LIFE REPRODUCING SORT OF PHENOMENON, BUT YOU KNOW, THERE’S A LOT GOING ON. AT ANY GIVEN DAY, HOW MANY EXPERIMENTS ARE GOING ON ON THE SPACE STATION? >> IT’S HARD TO SAY BY DAY, BECAUSE SOME TAKE LONGER THAN OTHERS, BUT WE TRACK THEM IN A SIX-MONTH EXPEDITION PERIOD. >> OKAY. >> AND SO THERE ARE, AT ANY ONE TIME, OVER SIX MONTH’S WORTH OF ABOUT 250 DIFFERENT INVESTIGATIONS. >> WOW. >> THAT SIX CREW MEMBERS ARE DOING ON ORBIT. AND THEY REPRESENT HUNDREDS OF SCIENTISTS ON THE GROUND, BY THE WAY. >> THAT’S AMAZING. >> YEAH, SO THAT ALWAYS GETS ME, EVERY TIME-- THOSE NUMBERS, LIKE 300-800 SCIENTISTS ON THE GROUND EVERY SIX MONTHS ARE GETTING THEIR SCIENCE REPRESENTED BY THOSE SIX CREW MEMBERS. >> WOW. >> NO PRESSURE! >> YEAH, FOR REAL. SO IS IT THE ASTRONAUTS THAT ARE WORKING ALL OF THESE EXPERIMENTS? OR ARE SOME OF THEM KIND OF RUNNING ON THEIR OWN? >> BOTH. >> OH, OKAY. >> SO BEST BET IS IF YOU’RE GOING TO CREATE AN EXPERIMENT FOR STATION, IF IT’S AUTOMATED ALL THE BETTER. >> RIGHT. >> AND THEN IF IT’S AUTOMATED, YOU AS THE INVESTIGATOR COULD PROBABLY INTEGRATE YOUR SOFTWARE INTO YOUR COMPUTERS AND WORK WITH MISSION CONTROL TO OPERATE THAT. >> WHOA. >> BUT SOME OF THESE THINGS ARE SO DELICATE, ESPECIALLY THE LIVING ORGANISMS, THAT YEAH, THEY REQUIRE CREW TIME. AND SO WE PRIORITIZE THE SCIENCE AND MAKE SURE EVERYBODY’S STUFF GETS DONE. AND WE LOG IT ALL, WE CAPTURE IT ALL, AND WE TURN OUT METRICS TO SAY, “OH, THIS MUCH GOT DONE.” >> IT’S JUST GOOD SCIENCE, RIGHT? >> YEAH, IT’S JUST GOOD SCIENCE MANAGEMENT, TOO. YES, THAT’S RIGHT. >> YEAH. >> YEAH. >> YOU’VE GOT TO DO THAT. OKAY, SO SOME OF THEM DO REQUIRE ASTRONAUT TIME. AND SO I GUESS IS THIS MOST OF AN ASTRONAUT’S DAY IS UP ON THE SPACE STATION? THEY ARE JUST GOING FROM RESEARCH EXPERIMENT TO RESEARCH EXPERIMENT-- IS THAT WHAT’S HAPPENING? >> SO IT DEPENDS ON THE CREW MEMBER, BUT YEAH, IT'S-- THE CREW IS SCHEDULED, I THINK, FOR EIGHT HOURS OF WORK DAY. AND I THINK BETWEEN ALL OF THE CREW MEMBERS ON ORBIT, THEY'LL REPRESENT ANYWHERE FROM 35-40 HOURS-- THEY'LL GET ABOUT 35-40 HOURS AS THE TARGET DONE PER WEEK OF SCIENCE. BUT WE HAVE BEEN AVERAGING-- WE HAVE HAD WEEKS OF 70 HOURS OF SCIENCE DONE, TOO. >> WHOA. >> SO IT DEPENDS ON THE VISITING VEHICLE FREQUENCY-- DO WE HAVE NEW SCIENCE COMING OR CARGO THAT'S BEING DELIVERED? DO WE HAVE CREW CHANGE-OUT WITH NEW CREW MEMBERS? >> RIGHT, YEAH, THAT CAN GET IN THE WAY. >> SOME PEOPLE ARE COMING UP TO SPEED, AND DO WE HAVE AN ANOMALY ON ORBIT THAT THEY NOW NEED TO GO DO AN EVA? >> OH, RIGHT. >> SO ALL OF THESE THINGS NEED TO BE FACTORED SO IT VARIES, BUT OUR GOAL IS ABOUT 40 HOURS A WEEK. BUT WE HAVE REPEATEDLY HIT 70, AT LEAST 70 HOURS. >> THAT'S AMAZING. AND WHAT’S COOL-- COMING UP HERE, WE’RE GOING TO HAVE A LOT MORE U.S. CREW MEMBERS, A LOT MORE TIME TO DEDICATE TO SOME OF THESE U.S. EXPERIMENTS, SO IS THAT GOING TO SKYROCKET EVEN BEYOND 70 MAYBE? >> YEAH! >> THAT’S AWESOME. >> SO WE’RE LOOKING AT AT LEAST, AT LEAST 80 HOURS. THAT’S LIKE TWO FULL TIME PEOPLE WORKING FULL TIME SCIENCE IN A WEEK, RIGHT? >> WOW. >> THAT’S AT LEAST, SO WE’RE ANXIOUS TO SEE WHAT HAPPENS THERE. >> YEAH, FOR REAL. OKAY, SO WE’VE GOT A LOT OF CREW TIME. WE’VE GOT A LOT OF EXPERIMENTS THAT WE’RE RUNNING AUTONOMOUSLY. SO IN GENERAL-- YOU KNOW, WE KIND OF HINTED AT THIS, BUT THE SPACE STATION, ONE OF THE MAIN BENEFITS IS THAT YOU CAN TAKE AWAY GRAVITY IN ONE OF YOUR EXPERIMENTS AND YOU CAN KIND OF MESS WITH THAT. BUT YOU KNOW, WHAT ARE SOME OF THE OTHER THINGS THAT MAKES THE INTERNATIONAL SPACE STATION SUCH A NICE PLACE? THE ONE THAT COMES TO MIND IS PERSPECTIVE, OBVIOUSLY. YOU’VE GOT-- YOU’RE 250 MILES ABOVE THE EARTH, SO YOU CAN LOOK DOWN, SO YOU’VE GOT SOME OBSERVATIONAL THINGS. BUT WHAT OTHER KINDS OF THINGS, YOU KNOW, IS GOOD ABOUT PUTTING RESEARCH UP THERE? >> YEAH, SO THERE’S A FEW. OUR EARTH OBSERVATION IS A GREAT EXAMPLE, BUT YOU KNOW, THEN YOU GET ASKED, “WELL, WHAT ABOUT THE OTHER SATELLITES? AREN’T THERE LOTS OF OTHER SATELLITES OBSERVING THE EARTH?” >> SURE. >> WELL, YEAH, BUT SPACE STATION IS A BIG SATELLITE WITH LOTS OF DATA CAPABILITY, AND A TRAJECTORY THAT’S DIFFERENT THAN ANY OTHER SATELLITE THAT WE WOULD CALL SYNCHRONOUS, GEOSYNCHRONOUS SATELLITES. >> OH, OKAY. >> SO STATION HAS A TRAJECTORY THAT CAN CIRCLE THE EARTH ONCE EVERY 90 MINUTES, AND BY THE TIME IT’S THROUGH A COMPLETE ROTATION, I SHOULD SAY, IT COVERS ABOUT 90% OF THE EARTH’S SURFACE. >> ALL RIGHT. >> SO 99.5% IT CAN TAKE IMAGES. THAT’S MORE THAN ANY ONE SATELLITE CAN DO ON ITS OWN. PLUS, IT’S GOT HUMAN BEINGS UP THERE LOOKING DOWN AND FINDING THINGS HAPPENING THAT, YOU KNOW, THAT SATELLITES-- YOU KNOW, THERE’S NOTHING LIKE THE HUMAN EYE TO SEE A FLOOD, OR AN OIL SPILL, OR A VOLCANIC ERUPTION BEFORE ANYTHING ELSE. >> AND THAT’S HAPPENED BEFORE, RIGHT? >> YEAH, IT HAS HAPPENED BEFORE. I HEARD A STORY OF ONE OF THE CREW MEMBERS CALLING DOWN TO USGS SAYING, “UM, I’M SEEING A VOLCANIC ERUPTION.” AND THEY’RE LIKE, “NO, I DON’T--” THEY THOUGHT IT WAS A HOAX. >> I THINK IT WAS-- I THINK IT WAS JEFF WILLIAMS. >> WILLIAMS, YEAH. >> YEAH, IT WAS, YEAH. >> OKAY, WE HEARD THE SAME STORY, YEAH, YEAH. >> AND THEN THEY WERE ABLE TO ACTUALLY COMMUNICATE ALL THAT. HE WAS LIKE, “HEY, I THINK THERE’S-- THINK THERE’S A VOLCANO ERUPTING.” BECAUSE HE TOOK A PICTURE OF IT. >> THAT’S RIGHT, AND YOU CAN GET THE MESSAGE OUT FOR THOSE DISASTER RESPONSE NETWORKS MUCH MORE QUICKLY. >> YEAH. >> BUT ALSO, ISS IS A HUGE PLATFORM FOR DATA. SO IF YOU’VE GOT SOMETHING LIKE THE ALPHA MAGNETIC SPECTROMETER THAT’S LOOKING FOR DARK MATTER-- >> OH YEAH. >> YOU KNOW-- >> LOVE THAT ONE. >> THE FACT THAT THAT-- IT’S A DATA HOG. IT’S LOOKING FOR-- IT’S, YOU KNOW, ABSORBING TONS AND TONS OF COSMIC RAYS AND SENDING I DON’T EVEN KNOW WHAT-- GIGA, TRIGA-- I DON’T KNOW-- BYTES OF DATA-- GIGATRIGABYTE, YEAH-- TEASED FOR THAT ONE. >> WELL, GIGATRIGABYTE’S AWESOME. >> BUT DOWN TO EARTH, AND ONLY ISS CAN HANDLE THAT KIND OF DATA AND POWER DEMAND TO KEEP SOMETHING UP THERE FOR SO LONG. >> OH! >> --THOSE KIND OF COSMIC BEHAVIORS. >> WOW. >> BUT ALSO, YOU CAN PUT EXPERIMENTS ON THE OUTSIDE OF SPACE STATION TO EXPOSE THEM TO ATOMIC OXYGEN, OR THE ULTRAVIOLET RADIATION, OR THE INTENSE THERMAL SWINGS. >> YEAH. >> WE HAVE PUT DIFFERENT TYPES OF MATERIAL OUT THERE BEFORE, AND GET THEM HOME, AND LOOK AT THE DAMAGE CAUSED BY EXTERNAL ENVIRONMENTS. AND FOR EXAMPLE, ONE OF THOSE WAS A PAINT THAT’S NOW BEEN USED ON THE MARS ROVER CURIOSITY, WHO’S UP THERE. IT’S PROTECTING ITS POWER, ITS CRITICAL POWER UNIT. >> RIGHT. >> THAT WAS TESTED ON STATION FIRST. >> OH, YOU PUT A BUNCH OF PAINT OUTSIDE AND SEE WHICH ONE LASTED BEST, OKAY. VERY COOL. >> AND WE DO THAT WITH SPACESUIT PIECES AND VEHICLE PIECES. >> YEAH. >> WE’VE GOT STUFF ON-- PAINT ON THE SPACEX LAUNCH VEHICLES THAT WERE TESTED ON STATION. AND WE’VE ACTUALLY FLOWN MICROORGANISMS ON THE OUTSIDE OF SPACE STATION, TOO, TO SEE HOW THEY’LL SURVIVE, AND LITTLE TYPES OF ENDOSPORES, LITTLE, YOU KNOW, LIVING ORGANISMS THAT GO INTO HIBERNATION. THEN BRING THEM HOME AND FIND OUT WHAT SPACE DID TO THEM, YOU KNOW? >> WOW. >> SO IT’S GOT THAT EXTERNAL PLATFORM UNLIKE ANYTHING OTHER. >> SO I’M GUESSING BRINGING THEM HOME IS ALSO A PRETTY GOOD THING TO DO, RIGHT, BECAUSE YOU CAN PLAY WITH SOMETHING, BUT THEN YOU CAN ALSO GET IT BACK DOWN TO EARTH-- IS THAT A UNIQUE CAPABILITY OF THE ISS? >> YEAH, SO THE ULTIMATE GOAL FOR ANY RESEARCHER IS TO GET YOUR SAMPLE HOME-- IF YOU’RE A LIFE SCIENTIST OR A PHYSICAL SCIENTIST. AND THAT IS-- THAT IS ENABLED BY THE SPACEX VEHICLE. SPACEX CAN RETURN SAMPLES. >> RIGHT, OKAY. >> BUT THERE ARE ALSO OTHER WAYS TO GET YOUR DATA. SO IF YOU’RE A TECHNOLOGIST, OR, YOU KNOW, VISUAL-- IF YOU JUST NEED IMAGES, OR VIDEO, OR ZEROES AND ONES, DATA-- >> JUST DOWNLINK IT, RIGHT? >> DOWNLINK IT FROM STATION, AND IT’S BEEN-- THOSE ARE WAYS TO DO IT, TOO. NOW, THERE WAS A TECHNOLOGY EXPERIMENT CALLED OPALS, WHICH WAS TESTED ON STATION-- I BELIEVE IT MAY HAVE JUST WRAPPED UP. THEY MET THEIR OBJECTIVES. BUT THEY’RE LOOKING AT USING LASER OPTICAL TECHNOLOGY TO SEND DATA DOWN IN THE FORM OF HIGH SPEED LASERS TO-- YEAH, RIGHT, TO THE GROUND, YEAH. >> AWESOME! >> SO THAT-- AND THEY USED A COUPLE OF DIFFERENT ISS INVESTIGATIONS AS A WAY TO PIPELINE THAT DATA AND TEST IT OUT. >> SWEET. >> SO HIGH SPEED DATA TRANSFER VIA LASERS-- YOU KNOW, COOL STUFF. ALL THAT’S HAPPENING AT THE SAME TIME. >> YEAH, THAT’S AMAZING. OKAY, SO, YOU KNOW, THERE’S A LOT OF THESE EXPERIMENTS AT ALL DIFFERENT TIMES, RIGHT? WE’RE TALKING ABOUT OBSERVATIONAL RESEARCH, TALKING ABOUT SATELLITE-- YOU GET THE BENEFIT OF COVERING THE EARTH. YOU KNOW, WHAT ARE SOME OF THE CATEGORIES OF EXPERIMENTS THAT WE’RE SENDING UP THERE? >> YEAH, SO I’LL START WITH THE FIRST ONE, WHICH IS MY FAVORITE, WHICH ARE ALL THE HUMAN EXPERIMENTS THAT HAPPEN. >> HUMANS. >> THERE’S NOTHING LIKE THE CREW MEMBERS ON STATION, RIGHT? THEY’RE NOT ROBOTS. THEY ARE THE HUMAN BEINGS THAT WILL GO AND EXPLORE FURTHER. AND SO WE’VE KNOWN FOR DECADES THERE ARE LOTS OF CHANGES THAT HAPPEN THROUGHOUT THE ENTIRE SYSTEM. BECAUSE WHY? WE’RE CREATURES OF THE GRAVITY ENVIRONMENT-- FOREVER. >> RIGHT. >> THAT’S HOW WE’VE EVOLVED. SO ANY SYSTEM IN THE HUMAN BODY THAT YOU CAN THINK OF IS-- HAS TO ADAPT TO THE SPACEFLIGHT ENVIRONMENT. THERE’S AN EFFECT. SO WE STUDY THE NEUROVESTIBULAR OR THE BALANCE SYSTEMS. WE-- BECAUSE THEY CHANGE. WE STUDY THE BONE. THEY’RE-- SINCE I WAS A KID-- I MEAN, WE’VE ALL KNOWN THERE’S BEEN BONE LOSS IF YOU DON’T USE YOUR BONES. THINK ABOUT WHY WE HAVE BONES. IT’S BECAUSE WE HAVE TO STAND UP AGAINST GRAVITY-- AND OUR MUSCLES, TOO. >> YEAH. >> IF YOU DON’T USE THAT IN SPACE, THEY’RE-- THE BODY’S PRETTY EFFICIENT AT GETTING RID OF IT. >> YEAH, YOUR BODY NEEDS TO CONSERVE ENERGY, AND IF IT DOESN’T NEED BONES, JUST GET RID OF THAT, PUT THE ENERGY SOMEWHERE ELSE. >> EXACTLY. SO WHERE DO WE GET THE ENERGY? WE KEEP-- TELL OUR BODY WE NEED ENERGY THROUGH EXERCISE. >> OH, OKAY. >> AND SO WE DO RESISTIVE EXERCISE AND CARDIOVASCULAR TRAINING ON ORBIT TO HELP MITIGATE THAT. AND VERY INTERESTING FINDING: WE’VE BEEN ABLE TO MAINTAIN BONE MINERAL DENSITY NOW, FOR THE FIRST TIME EVER, AS A RESULT OF THE WORK THAT WE’VE BEEN DOING ON STATION. >> THAT’S AMAZING. OVER THE COURSE OF A SIX-MONTH-- >> YEAH. >> EVEN, IN THE CASE OF SCOTT KELLY, A YEAR LONG, RIGHT? >> YEAH, WASN’T AS BAD AS IT COULD’VE BEEN. >> YEAH. >> YEAH, SO KUDOS TO US FOR THAT. >> VERY COOL. >> AND YOU KNOW, THE IMMUNE SYSTEM-- SO ANYTHING IN THE HUMAN BODY, RIGHT? OTHER THAN THE HUMAN BODY, THERE ARE CHANGES IN BIOLOGY, THE LIVING SYSTEMS. WE-- THE FRUIT FLIES, FOR EXAMPLE, OUR MODEL ORGANISMS THAT ARE USED IN LABORATORIES, WE CAN LOOK AT CHANGES IN THEIR GENETICS AS A RESULT OF SPACEFLIGHT, WHAT THEIR BABIES WOULD LOOK LIKE, OR HOW THEY WOULD BEHAVE. WE CAN SEND UP TINY LITTLE WORMS THAT ARE CALLED C. ELEGANS AND LOOK AT HOW THEY BEHAVE, OR EVEN INFECT THEM IN SPACE WITH A CERTAIN TYPE OF BACTERIA. >> TO SEE HOW THE IMMUNE SYSTEM WORKS OR SOMETHING? >> WELL, YOU CAN STUDY THEIR IMMUNE SYSTEM, BUT YOU CAN ALSO TRY TO FIGURE OUT WHAT MAKES THAT BACTERIA AGGRESSIVE. >> OH, SO STUDY THE BACTERIA. >> WHY DOES IT INFECT YOU IN THE FIRST PLACE? >> WOW. >> WHAT IS IT? AND SO WE’VE ACTUALLY FOUND THAT MICROGRAVITY HAS UP-REGULATED-- IS WHAT WE CALL IT-- GENES TO MAKE CERTAIN BACTERIA MORE YUCKY AND MAKE YOU SICK QUICKER. SO YOU KNOW, ALL KINDS OF-- WE SEND UP RODENTS TO LOOK AT THE BEHAVIOR IN SOME OF THE SYSTEMS IN MICE, AND SO ANY LIVING SYSTEM-- THE MICROBIOLOGY COMPONENT OF IT IS FASCINATING, TOO. WE SAMPLE THE ENVIRONMENT ON A REGULAR BASIS-- THE AIR, THE WATER, THE SURFACE. >> OH, YEAH. >> AND ANY NEW FINDINGS IN BACTERIA OR FUNGI THAT MIGHT BE SHOWING UP THAT ARE-- >> WITHIN THE ENVIRONMENT-- YEAH, WITHIN THE HABITABLE ENVIRONMENT OF THE SPACE STATION. >> AND ESPECIALLY SINCE WE SEE THAT OUR CREW MEMBERS HAVE EVIDENCE OF A SUPPRESSED IMMUNE SYSTEM, HOW DOES THAT-- IF ANYTHING WACKY SHOWS UP, HOW IS THAT GOING TO AFFECT THEIR IMMUNE SYSTEM? >> YEAH. >> SO THE INTERESTING MICROBIOTA IS REALLY FASCINATING, THOSE KIND OF STUDIES. BUT WE ALSO DO TECHNOLOGICAL STUDIES, SO TECHNOLOGY. WE USE SPACE STATION AS A PLATFORM TO TEST WHAT WE WANT TO USE TO EXPLORE FURTHER. SO FOR EXAMPLE, THE BIG ONE RIGHT NOW IS BEAM, RIGHT?? >> OH, YEAH! >> THE BIG INFLATABLE ONE THAT’S UP THERE RIGHT NOW. >> THAT’S REALLY COOL-- EXPANDABLE TECHNOLOGY, EXPANDABLE MODULES. >> YEAH. >> I LOVE THAT. >> AND THAT’S-- IT’S HUGE. >> YEAH, IT IS. AND YOU CAN GET THEM TO BE WAY BIGGER-- THAT’S THE WHOLE VALUE ADD OF THAT, RIGHT, IS YOU CAN LAUNCH SOMETHING WITH A SIMILAR WEIGHT BUT JUST KIND OF PACK IT DOWN AND THEN EXPAND IT IN SPACE SO YOU HAVE WAY MORE VOLUME. THAT’S AWESOME-- YOU CAN MAKE GIGANTIC SPACE HABITATS WITH THAT. THAT’S REALLY AWESOME. >> IT’S REALLY-- IT’S GOT GREAT POTENTIAL. SO IT’S ONE OF OUR TECHNOLOGY DEVELOPMENT INITIATIVES. BUT IT’S ALSO-- WE ALSO TEST OUT NEW GAS ANALYZERS OR AIR MONITORS UP ON ORBIT, OR WAYS TO BETTER SERVICE SATELLITES THAT END UP OUT THERE DEAD AND WERE NEVER INTENDED TO BE SERVICED-- BUT IF WE WANT TO GO TO MARS, FOR EXAMPLE, MAYBE WE WANT TECHNOLOGY TO SERVICE, YOU KNOW, STATIONS IN BETWEEN US AND MARS. >> OH, YEAH. >> RIGHT, SO YOU’VE GOT THESE LITTLE WAYPOINTS THAT GIVE YOU EXTRA FOOD OR EXTRA FUEL OR SOMETHING. >> LIKE SPACE GAS STATIONS SLASH CONVENIENCE STORES. >> YEAH, WHO KNOWS. SO WE DO SOME OF THOSE TECHNOLOGY EVALUATIONS TO CREATE NEW TOOLS AND PROCESSES THAT COULD POSSIBLY GET US THERE, TOO. SO TECHNOLOGY, BUT WE ALSO HAVE A LOT OF EDUCATION THAT HAPPENS. >> VERY IMPORTANT. >> YEAH, WE’VE GOT STUDENTS SENDING UP THEIR OWN EXPERIMENTS, AND DIFFERENT-- LOTS OF DIFFERENT OPPORTUNITIES ON ISS THROUGH NANORACKS AND STUDENT ORGANIZATIONS. HIGH SCHOOLS ARE GOING FUNDRAISING, YOU KNOW, THEIR OWN MONEY TO SEND THEIR OWN EXPERIMENTS ON ISS. IT’S THAT ACCESSIBLE. >> WOW, VERY COOL. >> AND WE’VE HAD 5th GRADERS DO THAT, TOO. THERE ARE A COUPLE OF FORMAL PROGRAMS. ONE’S CALLED THE SALLY RIDE EARTHKAM. >> EARTHKAM, RIGHT. >> LAUNCHED OUT OF THE U.S. SPACE AND ROCKET CENTER IN ALABAMA, WHERE, IF YOU’RE INTERESTED, AS JUST A REGULAR STUDENT, YOU JUST GO REGISTER WITH THAT PROGRAM AND YOU SAY, “I WANT SPACE STATION TO TAKE AN IMAGE OF X MARKS THE SPOT,” AND THEY WILL PUT YOU IN QUEUE, GET THAT IMAGE, AND CONTACT YOU WHEN IT’S AVAILABLE. >> WOW. >> AND YOU KNOW, HAM RADIO, FOR THOSE OF YOU WHO LIKE, YOU KNOW, USING THE HAM RADIO, IF YOU’RE A HAM RADIO SPECIALIST, THERE ARE CERTAIN OPPORTUNITIES TO CALL THE SPACE STATION CREW MEMBERS ON A HAM RADIO AND JUST ASK QUESTIONS. SO THAT’S ALL ONGOING, AND SOME OF THE BEST EXPERIMENTS ARE STUDENT EXPERIMENTS, BECAUSE THEY ASK THE WEIRD QUESTIONS THAT-- THE WHAT-IF QUESTIONS, RIGHT? THEY’RE STILL IN THAT PHASE OF EARLY DISCOVERY. >> RIGHT. >> SOME OF OUR ESTABLISHED RESEARCHERS HAVE THEIR OWN PATH TO RESEARCH AND THEIR OWN QUESTIONS THEY WANT TO ASK THAT HELPS BENEFIT THE RESEARCH THEY’RE DOING, WHICH WILL ULTIMATELY GET TO US HERE ON EARTH, TOO. >> SURE. >> SO THERE ARE LOTS OF OPPORTUNITY-- AND IN FACT, EVEN THE RESEARCHERS WHO DON’T HAVE A GOAL OF EDUCATION, THERE’S ALWAYS A STUDENT INVOLVED ONE WAY OR ANOTHER, WHETHER IT’S UNDERGRADUATES OR GRADUATES CRUNCHING NUMBERS, OR HAS A DISSERTATION OR THESIS, OR SOMETHING ASSOCIATED WITH THAT. SO WE ARE ALWAYS INTERACTING WITH STUDENTS. >> WOW. >> SO LOTS OF EDUCATION. THE PHYSICAL SCIENCES-- ANYTHING FROM FLAMES TO FLUIDS, TO TINY LITTLE PARTICLES CALLED COLLOIDS IN A SUSPENSION OF FLUIDS. >> OH, OKAY. >> COMPLEX FLUIDS, OR NON-NEWTONIAN FLUIDS, OR SOLIDS, ALLOY BEHAVIORS-- CAN YOU MELT TWO MATERIALS TOGETHER AND CREATE SOMETHING NEW? WE’VE GOT CAPABILITIES FOR THOSE KIND OF METALS ON SPACE STATION, TOO. WE’VE GOT FURNACES. >> OOH. >> WE CAN LEVITATE MATERIALS, TOO. >> WHAT! >> YEAH, LEVITATE THEM ON ISS, AND BASICALLY YOU HAVE CONTAINERLESS PROCESSING, SO YOU CAN PROCESS MATERIALS-- METALS OR SOLIDS-- WITHOUT IT EVER TOUCHING A CONTAINER. >> DOESN’T HAVE TO TOUCH ANYTHING, COOL. >> YEAH, SO ALL THE KINDS OF SCI-FI, WACKY STUFF YOU CAN IMAGINE HAPPENING IN MICROGRAVITY, WE’RE ALMOST DOING ALMOST ALL OF IT. >> YEAH. >> WE’RE DOING A LOT OF COOL STUFF. >> WELL, 250-- YOU’VE GOT-- I MEAN, IT’S GOT TO COME FROM SOMEWHERE, RIGHT? SO YOU’VE GOT IT FROM EVERY DIFFERENT TYPE OF SCIENCE. THAT’S JUST AMAZING, ALL THE THINGS YOU CAN ACCOMPLISH, AND I’M EXCITED TO SEE WHAT THEY’RE ALL GOING TO DO WHEN ALL THE FOUR CREW MEMBERS ARE UP THERE. >> THEY’RE NEVER BORED, I’LL TELL YOU. THOSE GUYS ARE NEVER BORED. AND THE INTERESTING THING WITH THE ASTRONAUTS, TOO, IS THEY TAKE PERSONAL OWNERSHIP OF GETTING THIS STUFF IMPLEMENTED. LIKE, THEY’RE TRAINED ON THE RESEARCH. THEY KNOW THEY’RE THE PROXY SCIENTIST FOR THE GUYS ON THE GROUND, THE GUYS AND GALS ON THE GROUND. >> YEAH. >> AND THEY ARE SERIOUS ABOUT GETTING IT DONE. >> THAT’S AWESOME. >> AND THEN THEY TAKE JOY IN THE WORK THAT THEY DO, TOO, AND OFTENTIMES WILL ASK, “CAN WE DO MORE OF THAT? CAN WE DO, YOU KNOW, MORE OF THIS, MORE OF THAT?” >> AW, VERY COOL. YEAH, I THINK ONE OF MY FAVORITES WAS WHEN KATE RUBINS DID THE DNA SEQUENCING, RIGHT? BECAUSE SHE HAS A SCIENCE BACKGROUND, AND WHEN SHE DID-- AW MAN, THAT WAS-- IT WAS JUST COOL. >> YEAH, AND THE INTERESTING THING ABOUT KATE, TOO-- WHEN SHE CAME BACK, SHE’S SHARING ALL THE KNOWLEDGE WITH THOSE OF US ON THE GROUND WHO CAN ENABLE US TO DO EVEN MORE OF WHAT SHE DID. IT’S LIKE-- WOW, WHY DIDN’T WE THINK OF THIS-- WELL, WE DID-- WE THINK WE THOUGHT OF THIS BEFORE, BUT KATE COMES BACK AND SHE’S LIKE, “NO, NO, SERIOUSLY, YOU CAN DO IT LIKE THIS. THIS IS EXACTLY HOW I DID IT.” >> WELL SHE DID IT RIGHT BECAUSE SHE HAS THE PERSPECTIVE-- SHE WAS THE ONE RUNNING IT. >> YEAH, SO UNIQUE. SO IT’S SUCH A RESOURCE WE’RE EXCITED ABOUT. >> AWESOME. >> YEAH, GOOD STUFF. >> I LOVE IT. DNA SEQUENCING, THOUGH, THAT’S A COOL ONE. THAT ONE’S-- THE PURPOSE OF THAT IS TO MAKE REAL TIME DECISION MAKING, RIGHT? >> YEAH. >> SO YOU CAN UNDERSTAND HOW GENETICS CHANGE OVER TIME, BUT REAL TIME YOU’RE STILL GETTING DATA OUT. THAT’S AWESOME. >> I MEAN, ON EARTH, IT’S JUST-- THAT WHOLE-- THE WHOLE DNA GENETICS SEQUENCING, YOU CAN’T EVEN KEEP UP BECAUSE TECHNOLOGY AND PROCESSES ARE EVOLVING SO QUICKLY. IF YOU’VE KEPT UP WITH ANY OF THAT STUFF, THE HUMAN GENOME AND NEW FINDINGS IN DNA AND RNA, AND ALL THE THINGS IN BETWEEN-- I MEAN, EVEN SINCE I’VE GRADUATED, THERE’S NEW STUFF. >> YEAH. >> AND THAT I DON’T EVEN KNOW. BUT SO NASA NOW IS ON THE CUTTING EDGE OF KEEPING UP WITH WHAT’S HAPPENING ON EARTH, OR AT LEAST WATCHING. ISS IS WATCHING AND TRYING TO FIGURE OUT WHAT’S IMPORTANT FOR RESEARCHERS, AND TRYING TO BRING THAT TO THE LABORATORY TO INVITE THOSE RESEARCHERS TO NOW DO THIS IN A MICROGRAVITY ENVIRONMENT. SO THERE’S INTERESTING CHANGES THAT CAN HAPPEN TO YOUR GENETICS THROUGHOUT YOUR LIFETIME THAT AFFECT YOUR GENES INSIDE OF YOU AS YOU LIVE, AND THEN YOU COULD PASS ON TO YOUR CHILDREN. AND SO-- >> THEY CHANGE NATURALLY? OR THEY CHANGE BECAUSE OF INFLUENCES? >> IT’S CALLED EPIGENETICS-- BECAUSE OF INFLUENCES, EXTERNAL INFLUENCES. >> INTERESTING. >> IT’S REALLY INTERESTING. >> WOW. >> EVEN THE STRESS OF AN ENVIRONMENT CAN CHANGE SOME OF YOUR GENETIC OUTCOMES, AND PASS ON TO YOUR CHILDREN. >> OH, NO WAY! >> YEAH. >> OKAY, SO I’VE GOT TO REMEMBER TO RELAX. >> RELAX, DUDE. IF YOU’VE GOT A FUTURE WITH CHILDREN, Y’ALL NEED TO RELAX. TRY TO CHILL. >> YEAH. >> BUT MICROGRAVITY COULD BE ONE OF THOSE, AND WHAT DOES THAT ALL MEAN? WELL, I DON’T KNOW. IF YOU CAN DO IT REAL TIME IN SPACE ON ISS, AND YOU CAN LOOK AT DATA FROM DNA REAL TIME, WELL, YOU KNOW WHAT IT LOOKED LIKE YESTERDAY-- NOW YOU’LL KNOW WHAT IT LOOKED LIKE TODAY. THOSE ARE ALL TOOLS THAT RESEARCHERS ARE INTERESTED IN FOR VARIOUS, LOTS OF DIFFERENT REASONS ON EARTH. >> IT’S AMAZING. >> BUT ALSO, WHAT HAPPENS WITH OUR CREW MEMBERS IS WE STAY UP LONGER AND LONGER. AND WE WANT TO GO TO MARS-- WHAT HAPPENS TO OUR GENES? >> YEAH, YOU’VE GOT TO KNOW ALL THAT STUFF. >> YEAH. >> I MEAN, THERE’S A LOT OF DIFFERENT EXPERIMENTS GOING ON LIKE WE TALKED ABOUT, BUT HOW IS EVERYONE GETTING THEM ON SPACE STATION? I KNOW THERE’S AN ORGANIZATION CALLED CASIS, RIGHT? DO THEY KIND OF HELP WITH THAT? >> YEAH, THEY KIND OF HELP. NO, THEY’RE THE BIG HELP, YES. >> THEY’RE THE BIG HELP, OKAY. >> YEAH, SO CERTAIN PARTS OF THE-- WELL, THE UNITED-- I SHOULD SAY THE UNITED STATES ASSETS ON THE SPACE STATION ARE CONSIDERED A NATIONAL LABORATORY, A UNITED STATES NATIONAL LABORATORY. THAT’S A DESIGNATION THAT MAYBE 12 OR 13 OTHER LABORATORIES IN AMERICA ARE GIVEN, AND THAT MEANS THEY’RE SPECIAL-- THERE’S SOMETHING UNIQUE ABOUT THEM THAT NOBODY ELSE CAN OFFER. BUT IT ALSO MEANS THAT NOW WE HAVE ONE IN SPACE, AND IT’S THE NATIONAL LABORATORY ON ISS. AND ITS UNIQUE RESOURCES ARE EVERYTHING I JUST EXPLAINED. >> RIGHT. >> BUT ALSO, NOW IT OPENS UP ACCESS TO NON-NASA USERS. SO RESEARCHERS FROM OTHER GOVERNMENT AGENCIES, RESEARCHERS FROM ACADEMIA, RESEARCHERS FROM COMMERCIAL INDUSTRY, STUDENT, YOU OFF THE STREET WHO HAS A REALLY GREAT IDEA THAT’S FEASIBLE-- IT’S OPEN TO ALL OF YOU TO PROPOSE YOUR RESEARCH TO GET ON THE INTERNATIONAL SPACE STATION NOW. CASIS IS THE CENTER FOR THE ADVANCEMENT OF SCIENCE IN SPACE.. >> LOVE ACRONYMS. >> YES, WE HAVE ACRONYMS-- PROBABLY WITH AN ACRONYM. >> BUT THAT’S AN ORGANIZATION, RIGHT? >> YES, THEY’RE AN ORGANIZATION THAT MANAGES THAT NATIONAL LABORATORY COMPONENT. SO WHEN YOU HAVE A GREAT IDEA, YOU GO TO WWW.ISS-CASIS.ORG AND YOU’LL FIND OUT THAT THERE’S A FLOW-- YOU GET INTO THE RESEARCH PROCESS AND YOU PROPOSE YOUR IDEAS. AND EITHER CASIS HAS OPPORTUNITIES OPEN, OR YOU PROPOSE IDEAS. AND THEY’RE LOOKING FOR ALL-- I HATE THE CLICHE “BEST AND THE BRIGHTEST,” BUT IT’S TRUE-- THAT’S WHAT WE WANT. >> YEAH. >> LIKE I SAID, TO BE ABLE TO USE THIS LABORATORY NOW IS LIKE MORE IMPORTANT THAN EVER. >> RIGHT. >> AND A LOT OF PEOPLE DON’T EVEN KNOW THAT THEY COULD DO THIS. THEY THINK SPACE IS SO INACCESSIBLE. AND I KNOW-- I GO AROUND AND I TALK TO RESEARCHERS, AND THE LOOK ON THEIR FACE IS LIKE YOUR LOOK RIGHT NOW! YOU’RE LIKE, “IT’S SO ACCESSIBLE! WHAT DO YOU MEAN I CAN JUST COME UP WITH AN IDEA?” >> WELL, HOW ABOUT THIS-- HOW ABOUT WE DO A WHOLE PODCAST EPISODE ON ISS RESEARCH AND TELL THEM HOW TO GET THERE? THAT’D BE COOL. >> YEAH, WE CAN INVITE SOME CASIS PEOPLE. >> ALL RIGHT, SOMEBODY WRITE THAT DOWN. >> YEAH, WE’VE GOT THIS-- ACTION TO US. WE’VE GOT AN ACTION. THAT’S GREAT. >> VERY COOL. OKAY, SO THEY GO THROUGH CASIS, AND CASIS MAKES IT EASY FOR THEM TO GET IT ON THE STATION, AND THEY’LL WALK THEM THROUGH THE WHOLE PROCESS, AND THEN THEY CAN USE THE NATIONAL LAB FOR WHATEVER IDEA THEY HAVE. >> THAT’S THE WHOLE POINT. >> THAT’S AWESOME. SO I MEAN, WHEN YOU TALK ABOUT ALL THIS DIFFERENT RESEARCH-- AND A LOT OF IT, LIKE YOU SAID, YOU KNOW, A LOT OF THEM-- WE WANT TO GO TO MARS, SO WE’VE GOT TO FIGURE OUT, WE’VE GOT TO PREPARE, YOU KNOW, WHAT’S THE HUMAN BODY GOING TO DO ON LONG DURATION SPACEFLIGHT? SO-- FOR WHEN WE GET THERE-- BUT YOU KNOW, WHAT-- THERE’S GOT TO BE SOME COMPONENTS THAT ARE COMING BACK DOWN TO EARTH, RIGHT? SO WHAT WE DO AND LEARN COMES BACK DOWN, AND WE CAN PUT IT INTO OUR EVERYDAY LIVES, RIGHT? >> YEAH. SO ONE GOOD EXAMPLE OF THAT IS THAT, YOU KNOW, WHEN WE LAUNCH OUR CREW MEMBERS TO ISS, NOT EVERY SINGLE ONE OF THEM IS A MEDICAL DOCTOR. AND SO WHAT IF SOMEONE HURTS THEMSELVES OR GETS SICK ON ORBIT? HOW DO WE ASSESS THAT FROM THE GROUND? WELL, WE HAVE AN IMAGING CAPABILITY ON ORBIT WHICH IS THE ULTRASOUND. AND THAT’S REALLY THE ONLY IMAGING CAPABILITY WE HAVE. WE DON’T HAVE X-RAYS OR ANY OF THAT STUFF. >> MM-HMM. >> AND SO NOW THE GOAL IS TO USE THE ULTRASOUND-- NOW YOU’VE GOT TO TRAIN NON-CLINICIANS TO USE THIS CLINICAL TOOL TO ASSESS, RIGHT, AND SEND INFORMATION DOWN TO THE DOCS. >> BECAUSE THEY DON’T-- YEAH. >> BECAUSE THEY CAN’T ASSESS ON ORBIT. >> RIGHT. >> AND SO WE’VE HAD AN ULTRASOUND THAT WE SENT TO ISS. IT WAS SLIGHTLY MODIFIED WITH SOME SOFTWARE. IT WAS-- WE USED IT TO TRAIN THE CREW MEMBERS UP BEFORE THEY LAUNCH. AND OUR UNIQUE SOFTWARE AND TRAINING PROGRAMS WERE SO WIDELY RECOGNIZED NOW BY THE ACADEMY OF SURGEONS ON THE GROUND THAT IT’S BEING TAUGHT TO UP-AND-COMING SURGEONS. LIKE, OUR TRAINING PROGRAM AND OUR SOFTWARE SYSTEMS ARE BEING TAUGHT TO NEW CLINICIANS TO USE THAT ON THE GROUND. BECAUSE WHEN YOU THINK IN TERMS OF TELEMEDICINE, YOU CAN DEPLOY THESE ULTRASOUNDS EVERYWHERE. AND IT IS BEING DONE THAT WAY. MORE AND MORE TELEMEDICINE IS HAPPENING, RIGHT, FOR OUR TROOPS WHO ARE IN A PLACE WHERE THEY CAN’T GET ACCESS TO HOSPITALS, OR TO COMMUNITIES THAT DON’T HAVE ACCESS TO CLINICAL FACILITIES. >> SO A DOCTOR COMES TO THEM REMOTELY, SORT OF. >> TELEMED-- YEAH, REMOTELY. SO THE IDEA IS NOW YOU’VE GOT THIS ULTRASOUND OUT THERE, YOU’VE GOT SOMEONE WHO’S BEEN TRAINED UP ON HOW TO USE IT. EVEN IF THEY’RE NOT A DOCTOR, YOU’VE GOT PEOPLE WHO CAN USE IT, SEND THE INFORMATION BACK TO THE DOCTORS WHEREVER THEY ARE, AND THE DOCTOR CAN MAKE A DIAGNOSIS. SO THOSE KINDS OF BENEFITS WE DON'T HEAR A LOT ABOUT, BECAUSE THEY DON'T-- ULTRASOUND DOESN’T AFFECT OUR EVERYDAY LIVES. >> YEAH. >> BUT THEY'RE ALSO-- BECAUSE OUT OF PURE, BASIC NEED, WE STARTED LOOKING AT SPECIFIC TISSUES ON ISS THAT YOU WOULD NOT NORMALLY USE AN ULTRASOUND TO LOOK AT. YOU WOULD USE SOMETHING LIKE AN X-RAY OR AN MRI, BUT WE HAVE GOTTEN NEED-DRIVEN, AND SO UNIQUELY USEFUL AT THIS ULTRASOUND TECHNIQUE. >> YEAH. >> IT’S NOW DRIVING CLINICAL DECISIONS ON WHEN TO USE AN ULTRASOUND VERSUS AN MRI, VERSUS AN X-RAY, AND ALL THESE DIFFERENT COMPONENTS. SO NEW TECHNIQUES COMING OUT OF ULTRASOUND. >> YEAH, SO NOT NECESSARILY IN YOUR HOUSE, A BENEFIT, BUT YOU KNOW, YOUR HEALTH. >> YOUR HEALTH, YEAH. >> YOUR DOCTOR DOES A BETTER JOB. YEAH, THAT'S COOL. >> YEAH, MAYBE THE DOCTOR CAN ORDER AN ULTRASOUND INSTEAD OF AN MRI, AND GET YOU SOME BETTER RESULTS, OR DIFFERENT RESULTS OR FASTER RESULTS. WHO KNOWS? >> VERY COOL. >> ANOTHER BENEFIT IS THAT THIS LABORATORY-- THIS SET OF LABORATORY SCIENTISTS HAVE USED SPACE STATION-- AGAIN, THINKING ABOUT THE FLUID BEHAVIOR IN SPACE-- >> MM-HMM. >> --TO ADVANCE SOME OF THE TREATMENT TOOLS THAT THEY'RE GOING TO DESIGN FOR POSSIBLY TREATING CERTAIN DISEASES INCLUDING CANCER. SO THIS TEAM SENT UP-- THEY'RE TRYING TO IMPROVE ON WHAT'S CALLED "MICROBALLOONS" OR "MICROENCAPSULATION." SO YOU TAKE THIS TINY, LITTLE BALL THAT YOU'VE CREATED, AND YOU PUT A BUNCH OF CHEMICALS IN THERE, WHETHER IT'S TREATING CANCER CHEMICALS, OR SOME GOOD AGENT. WHERE YOU WANT IT TO GO, YOU TARGET IT DIRECTLY TO THE POINT-- MAYBE IT'S A TUMOR-- AND YOU TREAT IT THAT WAY. >> OH, OKAY. >> RATHER THAN MAYBE A SYSTEMIC EFFECT OF CHEMOTHERAPY. SO THESE LITTLE MICROBALLOONS CAN BE DELIVERED ANYWHERE IN THE BODY, DO PRETTY MUCH WHATEVER YOU TELL THEM TO DO. BUT IT'S NOT PERFECT. WE'VE NEVER, EVER, IN THE HISTORY OF MICROENCAPSULATION, BEEN ABLE TO USE IT CLINICALLY. SO THIS-- BECAUSE OF DIFFERENT REASONS. IT'S JUST NOT EFFECTIVE. IT'S NOT TARGETING RIGHT. >> I SEE. >> SO THIS GROUP SENT A NEW MACHINE TO SPACE STATION, TRIED TO LEVERAGE THE MICROGRAVITY ENVIRONMENT TO CREATE NEW MICROBALLOONS BASED ON DIFFERENT FLUID BEHAVIOR, AND GOT A RESULT THAT SHOWED IMPROVEMENTS IN LABORATORY TUMORS. NOW, THIS PARTICULAR GROUP IS IN THE PATH OF GETTING TO FDA APPROVAL FOR USE AS A TREATMENT OF CANCER. >> OH! >> BUT WE'RE NOT QUITE THERE YET, RIGHT? >> OKAY. >> AND SO, WE'RE NOT SAYING STATION’S GOING TO SOLVE-- CURE CANCER-- >> YEAH. >> BUT SOME OF THE TECHNIQUES THAT HAVE COME OUT OF SPACE STATION ARE ON THE PATH TO FDA APPROVAL, AND WE MAY SEE SOME OF THAT COMING OUT IN THE NEXT SEVERAL YEARS OR SO. >> WOW! VERY IMPORTANT STEP. >> YEAH, AND THOSE KINDS OF THINGS TAKE TIME, TOO, SO THAT'S ANOTHER THING TO REMEMBER. WE'RE SEEING-- YOU KNOW, WE'RE STILL SEEING RESULTS FROM APOLLO COME IN, RIGHT? >> OH, WOW! >> AND WHEN YOU TALK ABOUT REALLY CRITICAL RESULTS AND BENEFITS TO THOSE ON EARTH, ANY LABORATORY CAN TAKE A WHILE, DEPENDING ON WHETHER YOU'VE GOT FDA APPROVAL OR WHETHER IT'S A QUICK TURN-AROUND TYPE OF INVESTIGATION. SOME OF THEM GO QUICKER THAN OTHERS. AND THE LIFE SCIENCES ARE TYPICALLY THE LONGEST BECAUSE IT'S SO COMPLICATED. >> YEAH. >> YEAH, YEAH. BUT IN THE MEANTIME, IF YOU GO TO WWW.NASA.GOV I THINK IT’S /STATIONBENEFITS, WE HAVE A WHOLE PAGE DEDICATED TO THESE TWO EXAMPLES, PLUS TONS OF OTHERS THAT YOU CAN LEARN, "WHAT HAS STATION DONE FOR ME, LIKE IN MY DAILY LIFE, NOW?" >> COOL. >> AND EVERYTHING FROM BRAIN SURGERY, ROBOTICALLY, BECAUSE IT WAS DESIGNED BASED ON THE CANADARM THAT WE USE ON THE SPACE STATION, TO IDENTIFICATION OF LOST BOATS, YOU KNOW, SHIPS ON THE OCEAN, THANKS TO SOME OF THE SIGNALS THAT SPACE STATION WAS ABLE TO PICK UP. SO, THERE'S LOTS OF GOOD STORIES THERE. >> WOW, THAT'S AMAZING. >> YEAH! >> SO, A LOT OF THINGS BEING BROUGHT DOWN TO EARTH TO BENEFIT US, LIKE TO BENEFIT HUMANKIND. AND THAT'S A VERY, VERY IMPORTANT PART OF ISS, RIGHT? >> YES. >> SO THAT'S WHY WE LIKE TO SAY, "OFF THE EARTH, FOR THE EARTH." >> YUP, THAT'S RIGHT. >> THAT'S COOL. SO, I MEAN, GOING AWAY FROM EARTH TOWARDS TO MARS, WHAT ARE WE LEARNING-- I KNOW WE'RE TALKING ABOUT THE HUMAN BODY AND SOME OTHER STUFF, BUT WHAT ARE WE LEARNING SPECIFICALLY ON ISS THAT'S REALLY GOING TO HELP US GET TO MARS, BOOTS ON THE GROUND? >> YEAH, SO A COUPLE OF THINGS. WE'VE GOT TECHNOLOGY DEVELOPMENT. MINIATURIZED, MOST EFFICIENT SYSTEMS FOR MAINTAINING HUMANS. EVERYTHING EVOLVES AROUND MAINTAINING THE HUMANS, RIGHT? >> YEAH, RIGHT. >> WE ARE THE ONES GOING TO MARS, SO EVERY SYSTEM NEEDS TO COOPERATE WITH THAT. AND SO, KEEPING HUMANS ALIVE, HOW MUCH FOOD DOES A HUMAN NEED? CAN WE MINIATURIZE IT? IS IT AFFECTED BY RADIATION? CAN WE EXTEND SHELF-LIFE OF THAT? PLUS PHARMACEUTICALS-- WHAT ABOUT ALL THE MEDICAL CAPABILITIES? HOW ARE THEY GOING TO BE TRAINED? LET'S SEE-- RADIATION EFFECTS. OH... HOW OUR GENETICS CHANGE, BEHAVIOR EVEN OF ONE THAT YOU SENT ME AN EXAMPLE ON, WHICH IS THE STRATA INVESTIGATION. >> YEAH. >> I THOUGHT IT WAS COOL BECAUSE I WAS LIKE, "WHAT IS THAT?" BUT NO, THAT'S STUDYING HOW DUST BEHAVES, OR REGULAR DUST BEHAVES IN A MICRO-GRAVITY ENVIRONMENT. WELL, YEAH, RIGHT? THAT'S A GOOD THING TO KNOW BEFORE YOU GO TO MARS. >> BECAUSE PEOPLE ARE GOING TO INTERACT WITH IT, RIGHT? SO YOU’VE GOT TO KNOW WHAT IT DOES. >> YOU’LL LAND THERE-- AND I HEAR FROM STORIES ABOUT THE MOON, IT'S PRETTY-- IT'S A DRIVER. IT IS A MAJOR FORCE TO CONTEND WITH. SO ANY SYSTEM INVOLVING THE HUMANS, ANY SYSTEM INVOLVING AIR, WATER, RECYCLING, PLANET-- YOU KNOW, SPACESHIP EARTH-- THAT'S WHAT WE'RE DOING ON THE INTERNATIONAL SPACE STATION, AND IN EVERY DIFFERENT DIRECTION. >> THAT'S AMAZING. >> YEAH. >> I MEAN, THAT'S COOL. >> THERE'S A LOT. >> IT'S GOING, IT'S GOING-- THINKING ABOUT MARS, WE’RE THINKING ABOUT OTHER PLANETS, YOU KNOW, WHAT WE'RE LEARNING, YOU KNOW, THE REGOLITH ON THE MOON OBVIOUSLY IS A CONSIDERATION. THAT'S WHY WE PUT IT ON ISS, BROUGHT IT BACK DOWN TO EARTH. THIS RESEARCH GOES EVERYWHERE. >> YEAH. >> SO THAT'S AMAZING. >> YEP. >> SO, IS THERE ANYTHING-- IS THERE ANYTHING THAT WE'VE INVESTIGATED ON THE ISS THAT WE DIDN'T REALLY KNOW, OR SOME KIND OF STORY WHERE, YOU KNOW, THERE'S SOMETHING THAT WAS DISCOVERED THROUGH TRYING TO DISCOVER SOMETHING ELSE, OR SOMETHING NEW THAT HAS COME UP, YOU KNOW? >> YEAH, I THINK THE MOST-- ONE OF THE MOST INTRIGUING THINGS TO ME IS THE FACT THAT AS OUR CREW MEMBERS STAY ON ORBIT, THEIR BODIES START TO EXHIBIT LOTS OF SYMPTOMS-- I WOULD CALL IT SYMPTOMS-- BUT PROJECTIONS OF WHAT WE SEE IN OUR AGING POPULATION ON EARTH, AND THEY DO IT AT A VERY ACCELERATED RATE. >> OH, OKAY. >> SO THERE'S A COROLLARY BETWEEN WHAT WE SEE IN THE HUMAN IMMUNE SYSTEMS, THE BONE LOSS-- THE BONE LOSS HAPPENS AT A RATE OF-- IF IT'S NOT TREATED, AT THE RATE OF POST-MENOPAUSAL WOMEN, OR EVEN FASTER, WHICH IS 1-2% PER MONTH. >> JUST FROM BEING IN SPACE, WOW! >> YEAH, AND THE IMMUNE SYSTEM STARTS TO-- A LOT OF THE CHANGES IN THE TINY MOLECULES OF THE IMMUNE SYSTEM STARTS TO REPRESENT THE AGE-- WHAT WE SEE IN THE AGING POPULATIONS. THERE'S ALSO WOUND HEALING THAT SEEMS TO BE A LITTLE BIT SLOWER IN SPACE. SO I KEEP GOING BACK TO THE HUMAN BODY BECAUSE TO ME, IT’S THE MOST FASCINATING, AND EVERYTHING WE DO IS BECAUSE WE WANT TO EXPLORE. SO SOME OF THE MOST INTERESTING FINDINGS COME FROM THAT, AND ESPECIALLY THE AGING POPULATION. NOW, WHEN WE FIGURE OUT HOW TO TREAT OUR ASTRONAUTS-- OR, I WOULDN'T SAY "TREAT," BUT MITIGATE SOME OF THE EFFECTS THAT WE SEE WITH SPACEFLIGHT, THOSE HAVE BEEN ABLE TO BE APPLIED TO THE AGING POPULATIONS HERE ON EARTH. SO FOR EXAMPLE, BONE LOSS, I MENTIONED, BUT IT'S BECAUSE THEY'RE DOING THEIR RESISTIVE EXERCISE. THAT'S BECAUSE THEY'RE TAKING THEIR HIGH DOSES OF VITAMIN D, AND THEY'RE EATING ALL THEIR CALORIES. WELL, BEFORE YOU’RE OSTEOPOROTIC, AND YOU GET TO JUST THAT POINT, YOUR DOCTOR'S ALREADY TELLING YOU: "WELL, WE THINK RESISTIVE EXERCISE IS A GOOD IDEA, AND CALCIUM AND VITAMIN D." BUT WE CAN SHOW, ON SPACE STATION IN A SHORT TIME-- >> YOU HAVE THE DATA. >> YEAH, THE DATA. AND SO IT'S AMAZING TO ME HOW THE CREW MEMBERS ARE AN ACCELERATED MODEL FOR EVERYTHING THAT WE ARE INTERESTED IN. DISEASE POPULATIONS OR AGING POPULATIONS ON EARTH. >> WOW. >> AND THEY'RE GREAT, BECAUSE YOU KNOW WHAT THEIR HISTORY IS. >> YEAH. >> SO THEY’RE KIND OF A CLEAN MODEL TO LOOK AT. >> OH, WOW. I MEAN, THAT'S KIND OF-- A LOT OF ASTRONAUTS DESCRIBE PART OF THEIR JOB AS BEING GUINEA PIGS, RIGHT? >> YEAH, YEAH. >> BECAUSE LIKE YOU SAID, YOU KNOW, THE HUMAN BODY IS ONE OF THE TOP RESEARCH INVESTIGATIONS ON THE INTERNATIONAL SPACE STATION. YOU WANT TO KNOW WHAT HAPPENS TO THE HUMAN BODY OVER TIME IN SPACE-- WHEN IT'S IN SPACE FOR THAT LONG. >> WANT A GOOD TEST. >> YOU KNOW, THIS IS-- WE'RE IN A TIME WHERE THIS IS A NORMAL THING, RIGHT? >> YEAH. >> ANYONE BORN PAST THE YEAR 2000, RIGHT? >> RIGHT! >> --HAS NEVER KNOWN A TIME WHEN THERE HASN'T BEEN SOMEONE LIVING IN SPACE. >> MY DAUGHTER'S TEN. SHE'S LIKE, "WHAT DO YOU MEAN? WHAT? YES, OF COURSE THERE ARE PEOPLE LIVING IN SPACE. THERE'S ALWAYS BEEN PEOPLE LIVING IN SPACE." >> ISN'T IT WEIRD THAT IT'S LIKE A NORMAL THING NOW? IT'S JUST LIKE, "OH, YEAH, THERE'S PEOPLE IN SPACE." >> YEAH, AND THE THING IS, WE'RE NOT SENDING-- WE'RE GOING TO BE DONE SENDING ROBOTS-- YOU KNOW, NOT DONE, BUT WE'RE GOING TO GET PAST JUST SENDING ROBOTS TO MARS. IT'S THE HUMAN EXPERIENCE, SO WE'RE VERY COMPLICATED MACHINES. >> YEAH. SO TO YOU, WHAT IS THE BENEFIT OF SENDING HUMANS TO MARS? >> I THINK IT'S THAT PERSONAL JUDGEMENT. >> YEAH. >> IT'S SOMETHING THAT NO AMOUNT OF CIRCUITRY PROGRAMMING, AT LEAST IN MY MIND-- I'M NOT A SCIENCE FICTION READER, BUT-- SO MAYBE SOMEONE CAN CORRECT ME, BUT THERE'S NOTHING LIKE DISCERNMENT FROM A HUMAN BEING MAKING A JUDGEMENT CALL. IT COULD BE HARD, IT COULD BE A LITTLE EASIER, IT COULD BE TRICKY. >> YEAH. >> “HUMAN IN THE LOOP” IS THE CLICHE THAT I HATE TO USE, BUT IT'S TRUE. THERE'S NOTHING LIKE PEOPLE. >> MM-HMM. WE GET TO-- YOU KNOW, AND THAT'S WHAT HAPPENED WHEN WE LANDED ON THE MOON, RIGHT? YOU KNOW, YOU CAN TAKE PICTURES OF THE MOON ALL YOU WANT. >> YEAH. >> WE ACTUALLY HAD A COUPLE MISSIONS AROUND THE MOON. WE HAD ROBOTIC MISSIONS LAND ON THE MOON. >> THAT'S RIGHT. >> BEFORE THEY EVEN GOT THERE. NO ONE CARED. BUT ONCE THERE'S A HUMAN ACTUALLY SET FOOT, WE CAN-- WE CAN-- ALL OF THE SUDDEN, WE WERE PART OF THE EXPERIENCE. >> YES. >> WE COULD ALL SHARE. >> AND COMING BACK IS A BIG PART OF IT, BECAUSE THOSE PEOPLE COME BACK, AND THEY SHARE THEIR UNIQUE EXPERIENCES, AND THEY INSPIRE OTHERS, AND THE LESSONS LEARNED, AND YOU KNOW, WE WANT THAT INFORMATION BACK. AND THAT’S A-- THAT BECOMES A NATIONAL RESOURCE, YOU KNOW. SO, YEAH, THERE'S NOTHING LIKE IT. THAT WAS A REALLY GOOD EXAMPLE. >> YEAH. I MEAN, I JUST CAN'T WAIT. I CAN'T WAIT TILL SOMEONE LANDS. >> SOMEONE'S GOING TO DO IT. >> I WANT-- I WANT TO HEAR THEIR STORY. SOMEONE'S GOING TO DO IT, RIGHT, SO-- >> AND ISS WILL HELP GET THEM THERE. >> YEAH, ABSOLUTELY. SO WHAT'S ONE OF YOUR TOP INVESTIGATIONS GOING ON THE INTERNATIONAL SPACE STATION, EITHER RIGHT NOW, OR IN THE PAST? SOMETHING THAT YOU JUST THINK THAT REALLY STANDS OUT? AND IT COULD BE A PART OF THE HUMAN BODY, BUT ANYTHING THAT'S REALLY JUST, YOU KNOW, REALLY STUCK WITH YOU, OR YOU ALWAYS GO BACK TO OR REFER TO? >> MAN. >> IT'S A HARD ONE. IT'S LOADED. >> YEAH, I'M GOING TO TRY TO GET OFF THE HUMAN RESEARCH ONE, AND TALK ABOUT AMS, THE ALPHA MAGNETIC SPECTROMETER. >> OH, RIGHT. >> I AM NOT AN ASTROPHYSICIST, BUT AGAIN, IT'S SEARCHING FOR, YOU KNOW, THESE COSMIC PARTICLES, THIS DARK MATTER, THIS DARK ENERGY. I THINK I READ, AT SOME POINT, THAT, YOU KNOW, EVERYTHING THAT WE PERCEIVE, IS ONLY 5%, VISIBLY, 5% OF WHAT'S REALLY ACTUALLY OUT THERE. SO IF WE'RE ONLY SEEING 5% OF WHAT'S REALLY OUT THERE-- >> I CAN'T EVEN THINK-- I CANNOT-- >> WHAT IS IN FRONT OF ME RIGHT NOW? >> RIGHT! >> --THAT WE CAN'T SEE? AND SO I KNOW IT'S MORE COMPLICATED THAN THAT, BUT-- >> RIGHT, RIGHT. >> PHILOSOPHICALLY, I THINK AMS SPEAKS TO ME IN TERMS OF WHERE DID-- WHAT ARE THE ORIGINS OF THE UNIVERSE? WHERE DO WE COME FROM? >> YEAH. >> YOU KNOW, AND-- >> I THINK THOSE ARE REALLY THE ULTIMATE QUESTIONS. >> YEAH. >> WHAT IS THE ORIGIN OF THE UNIVERSE? WHERE DO WE COME FROM? ARE WE ALONE? YOU KNOW, THESE BIG QUESTIONS. >> AND WE HUMANS ARE DESIGNING BIG TOOLS LIKE AMS TO TRY AND FIND THESE QUARK-Y THINGS, THEY'RE CALLED QUARKS, OR NEUTRALINOS, OR THINGS THAT WE THINK EXISTS, AND WE CAN RELICATE ON EARTH-- WE CAN CREATE THEM ON EARTH, BUT HOW DO THEY EXIST NATURALLY? AND THEN, IF THEY DO EXIST, THAT PROVES SOME THEORY-- IT HELPS PROVE THEORIES OF WHERE WE CAME FROM. SO THAT WHOLE VERY COMPLICATED, DESIGNED INSTRUMENT IS ALL-- JUST AN EXTENSION-- IT'S A TOOL THAT EXTENDS OUR HUMAN SENSES IN A WAY THAT WE CAN'T DO, AND SO THAT JUST FASCINATES ME AS AN EXTENSION OF US. >> I JUST THINK-- I THINK THAT INTERNATIONAL SPACE STATION AND AMS, YOU KNOW, ALL THESE THINGS-- THE FACT THAT THESE EXIST, THE FACT THAT THEY ARE-- THEY'RE ACTUALLY UP IN SPACE, THAT WE ARE ACTUALLY DOING THEM, THAT WE ASK THESE QUESTIONS AND PURSUE THEM THROUGH TECHNOLOGY, THINGS THAT WE INVENT, AND WE COME UP WITH AN IDEA IN ORDER TO OBSERVE-- IT JUST PROVES WE ARE VERY CURIOUS BEINGS. >> YES. >> WE REALLY WANT TO KNOW WHAT'S GOING ON. >> AND CAPABLE. >> AND WE WILL DO ANYTHING-- AND CAPABLE. CURIOUS AND CAPABLE. >> WE WILL STOP AT NOTHING. >> WE WILL STOP AT NOTHING! >> NOT EVEN BUDGETS. >> OH, MY GOSH! IT'S JUST A FASCINATING CONCEPT JUST TO THINK ABOUT IT. >> I'M REALLY LUCKY TO BE WORKING WHERE I AM NOW. >> YEAH. >> I WOULD HAVE NEVER DREAMT UP THIS CAREER FOR MYSELF. QUITE HONESTLY, IT'S EVERYTHING I'VE EVER LOVED-- I GET TO DO EVERYDAY. >> YEAH. >> SO, I COULDN'T HAVE CREATED IT. JUST REALLY FASCINATED. A FASCINATING PLACE TO WORK. >> IT REALLY IS, IT REALLY IS. THE THINGS WE HAVE TO THINK ABOUT ALL DAY ARE JUST-- IT'S JUST-- YOU KNOW, YOU THINK ABOUT SPACE, YOU THINK ABOUT, YOU KNOW, WHAT COULD WE DO-- WHERE ARE GOING TO GO NEXT? HOW ARE WE GOING TO GET THERE? IT’S JUST-- >> YEAH, HOW DO WE MAKE THE MOST OUT OF WHAT WE HAVE? >> OH, MAN. I WISH WE COULD DO A TWO-HOUR LONG EPISODE, BUT TARA, I'M SORRY. I THINK THAT'S ABOUT ALL THE TIME WE HAVE. >> AHH. >> SO, FOR THE LISTENERS, STAY TUNED UNTIL AFTER THE MUSIC HERE, AND LEARN ABOUT SOME OF THOSE SITES. WE'RE GOING TO REITERATE THOSE SITES THAT TARA WAS TALKING ABOUT SO YOU CAN GO VISIT THEM, ESPECIALLY IF YOU'RE A RESEARCHER LISTENING TO THIS PODCAST AND WANT TO KNOW WHERE TO SUBMIT YOUR RESEARCH AND ACTUALLY TAKE IT TO SPACE, GO TO THE INTERNATIONAL SPACE STATION. IT’S VERY, VERY COOL-- AND LEARN SOME OF THOSE BENEFITS, SOME OF THE ONES-- WE KIND OF SKIMMED OVER THEM BECAUSE, YOU KNOW, WE REALLY DO HAVE A SHORT AMOUNT OF TIME, BUT IF YOU REALLY WANT TO LEARN ABOUT THEM, JUST STAY AFTER. YEAH, FOR SURE. SO TARA, THANKS AGAIN SO MUCH FOR COMING ON THE SHOW. I FEEL LIKE WE HAVE A GOOD GRASP OF-- I MEAN, WE HAVE-- I WOULDN'T SAY A GOOD GRASP, BUT LIKE, YEAH, AT LEAST A GOOD PLACE TO START, AN OVERARCHING KNOWLEDGE OF ALL THE RESEARCH GOING ON ABOARD THE SPACE STATION. BUT IT IS VERY CONTINUOUS, AND THANK YOU FOR COMING ON TODAY. >> I HOPE I'VE INSPIRED A COUPLE OF YOU OUT THERE, SO-- >> YOU INSPIRED ME, SO I THINK IT WAS WORTH IT FOR AT LEAST THAT. >> THANK YOU. >> SO, THANKS AGAIN. >> AH, SURE. [ MUSIC ] [ INDISTINCT RADIO CHATTER ] >> HOUSTON, WELCOME TO SPACE. >> HEY, THANKS FOR STICKING AROUND. SO TODAY WE TALKED ABOUT SPACE STATION SCIENCE WITH DR. TARA RUTTLEY. AND IF YOU WANT TO KNOW WHAT’S GOING ON ONBOARD THE SPACE STATION RIGHT NOW, JUST GO TO NASA.GOV/ISS. BUT WE WERE TALKING MAINLY ABOUT SPACE STATION SCIENCE. IF YOU WANT TO GO THERE, JUST GO TO NASA.GOV/ISS-SCIENCE. THAT’S ACTUALLY WHERE YOU CAN FIND ALL THE RESEARCH THAT’S GOING ON ABOARD RIGHT NOW. WE ALSO SORT OF ALLUDED TO SOME OF THE BENEFITS THAT ARE GOING ON ON STATION THAT YOU CAN BRING DOWN RIGHT TO EARTH. SO IF YOU GO TO NASA.GOV/STATIONBENEFITS THAT’S THE ONE WHERE THE EXPERIMENTS THAT WE’RE DOING ABOARD THE INTERNATIONAL SPACE STATION, THE ONES THAT ACTUALLY HELP US OUT HERE ON THE GROUND. AND YOU CAN ALSO FIND A LOT OF THIS STUFF ON THE SPINOFF MAGAZINE. THOSE ARE SOME TECHNOLOGIES THAT HAVE BEEN SPINNED OFF FROM NASA TECHNOLOGY RIGHT HERE INTO OUR EVERYDAY LIVES, AND IT’S REALLY COOL. I WOULD DEFINITELY RECOMMEND CHECKING IT OUT. AND SO IF YOU’RE A RESEARCHER OR A STUDENT AND YOU WANT TO SEND SOME OF YOUR RESEARCH ABOARD THE INTERNATIONAL SPACE STATION, JUST GO TO YOUR FAVORITE BROWSER AND JUST TYPE IN CASIS-- THAT’S C-A-S-I-S. OR YOU CAN GO TO WWW.ISS-CASIS.ORG. ONE OF THOSE WILL TAKE YOU TO THE ORGANIZATION THAT WILL ACTUALLY HELP YOU GET YOUR RESEARCH ABOARD THE INTERNATIONAL SPACE STATION, AND IT IS REALLY COOL. YOU CAN GET SOME REALLY COOL STUFF WHEN YOU SEND YOUR EXPERIMENTS ABOARD. WE HAVE STUDENTS THAT DO STUFF LIKE-- ONE OF MY FAVORITES IS SPHERES. THEY’RE ACTUALLY TINY LITTLE ROBOTS THAT STUDENTS CAN ACTUALLY PROGRAM CONTROLS, AND THEN THEY ACTUALLY FLY AROUND THE INSIDE OF THE SPACE STATION. YOU CAN GET SOME GREAT IMAGERY OF YOUR EXPERIMENTS THERE. SO IF YOU WANT TO FOLLOW US ON SOCIAL MEDIA, ANY OF THE INTERNATIONAL SPACE STATION SITES WILL HELP YOU OUT. THERE’S THE INTERNATIONAL SPACE STATION FACEBOOK PAGE. ON TWITTER, IT’S @SPACE_STATION AND INSTAGRAM IT’S @ISS. BUT WE ALSO HAVE RESEARCH ACCOUNTS, TOO-- JUST TYPE IN “ISS RESEARCH.” I’M PRETTY SURE THEY’RE VERIFIED ON ALL THOSE DIFFERENT PLATFORMS-- FACEBOOK, TWITTER, AND INSTAGRAM. USE THE HASHTAG #ASKNASA ON YOUR FAVORITE PLATFORM TO SUBMIT AN IDEA TO THE PODCAST. MAYBE YOU HAVE A QUESTION OR MAYBE YOU HAVE AN IDEA OF AN EPISODE THAT WE SHOULD DO-- AND MAKE SURE TO MENTION IT’S FOR “HOUSTON, WE HAVE A PODCAST.” SO THIS PODCAST WAS RECORDED ON JUNE 21st. THANKS TO ALEX PERRYMAN, JOHN STOLL, GREG WEISMAN, AND DAN HEWITT FOR HELPING TO SET UP, AND OF COURSE, THANKS TO DR. TARA RUTTLEY FOR COMING ON THE SHOW TODAY. WE’LL SEE YOU NEXT WEEK.