Radioactivity of phosphate ore, superphosphate, and phosphogypsum in Abu-Zaabal phosphate plant, Egypt

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

Hussein, E.M.

1994-09-01

A measurement of the radioactivity content of phosphate ore material, phosphatic fertilizer (superphosphate), and by-product phosphogypsum in the Abu-Zaabal phosphate plant, Egypt, has been carried out. According to the results of gamma-ray spectroscopy analysis, {sup 238}U was found in concentrations of 523, 473, and 134 Bq kg{sup {minus}1}; {sup 226}Ra in concentrations of 514, 301, and 411 Bq kg{sup {minus}1}; {sup 232}Th in concentrations of 37, 24, and 19 Bq kg{sup {minus}1}; and {sup 40}K in concentrations of 19, 3, and 16 Bq kg{sup {minus}1} for the analyzed materials, respectively. The data are discussed and compared with those given inmore » the literature for some other countries in light of permissible radiation dose rates. 11 refs., 3 tabs.« less

40 CFR 63.620 - Applicability.

Code of Federal Regulations, 2010 CFR

2010-07-01

... requirements of this subpart apply to the following emission points which are components of a granular triple... to the following emission points which are components of a granular triple superphosphate storage... emission points which are components of a diammonium and/or monoammonium phosphate process line: reactors...

40 CFR 63.620 - Applicability.

Code of Federal Regulations, 2011 CFR

2011-07-01

... requirements of this subpart apply to the following emission points which are components of a granular triple... to the following emission points which are components of a granular triple superphosphate storage... emission points which are components of a diammonium and/or monoammonium phosphate process line: reactors...

40 CFR 60.4 - Address.

Code of Federal Regulations, 2010 CFR

2010-07-01

... Fertilizer Industry: Wet Process Phosphoric Acid Plants X X X X U Phosphate Fertilizer Industry: Superphosphoric Acid Plants X X X X V Phosphate Fertilizer Industry: Diammonium Phosphate Plants X X X X W Phosphate Fertilizer Industry: Triple Superphosphate Plants X X X X X Phosphate Fertilizer Industry...

40 CFR 60.242 - Standard for fluorides.

Code of Federal Regulations, 2010 CFR

2010-07-01

... 40 Protection of Environment 6 2010-07-01 2010-07-01 false Standard for fluorides. 60.242 Section... Industry: Granular Triple Superphosphate Storage Facilities § 60.242 Standard for fluorides. (a) On and... atmosphere from any affected facility any gases which contain total fluorides in excess of 0.25 g/hr/megagram...

40 CFR 60.242 - Standard for fluorides.

Code of Federal Regulations, 2011 CFR

2011-07-01

... 40 Protection of Environment 6 2011-07-01 2011-07-01 false Standard for fluorides. 60.242 Section... Industry: Granular Triple Superphosphate Storage Facilities § 60.242 Standard for fluorides. (a) On and... atmosphere from any affected facility any gases which contain total fluorides in excess of 0.25 g/hr/megagram...

Nitrogen Isotopes as an Indicator of Long-Term N Cycling in a Grazed Temperate Pasture Receiving Different Rates of Superphosphate Fertilizer and Irrigation for ~50 Years

NASA Astrophysics Data System (ADS)

Mudge, P. L.; Schipper, L. A.; Ghani, A.; Baisden, W. T.; Dodd, M.

2010-12-01

Pastoral agriculture is the dominant land use in New Zealand and intensification (as a result of fertilizer inputs and in some areas irrigation) has led to increased nitrogen (N) losses to the wider environment. An indicator that could identify soils which are vulnerable to N loss would be useful for the development of management practices and regulations aimed at reducing unwanted N losses. The natural abundance of 15N relative to 14N (δ15N) in soils is one potential indicator. Most N cycle processes associated with N losses (e.g. nitrification, denitrification, and volatilisation) discriminate against 15N and therefore soil δ15N could provide an indication of cumulative N losses. In this study we measured δ15N in archived soils from two long-term field trials receiving different rates of superphosphate fertilizer and irrigation. Both trials were in mid-Canterbury, New Zealand and were grazed by sheep. The fertilizer trial began in 1952, and treatments used were the control (nilP), 376 kg superphosphate ha-1 y-1 (376PA) and a treatment where 376 kg superphosphate ha-1 y-1 was applied between 1952 and 1957, no fertilizer from 1958 to 1979 and then 250 kg superphosphate ha-1 y-1 from 1980 to 2009 (376-0-250PA). The irrigation trial was initiated in 1949 and ceased in 2002. The dryland treatment and treatments irrigated when soil moisture was 10% and 20% were used in this study. From 1958, soil samples (0-75 mm depth) were taken annually from each trial, air dried and archived. Soil samples at four year intervals were analysed for this study. Pasture production varied considerably between treatments, with higher rates of fertilizer and irrigation promoting greater pasture growth and therefore higher grazing intensities. Initially δ15N was about the same (3.3‰) in all treatments of both trials. δ15N in the 376PA treatment of the fertilizer trial increased gradually with time and by 2009 was 4.5‰. In the 376-0-250PA treatment, δ15N stayed constant until about 1980 and then increased rapidly, which coincided with re-commencement of P fertilizer application. δ15N in the nilP treatment initially declined slightly and then remained relatively constant. In the irrigation trial, δ15N stayed constant (~3.3‰) in all three treatments up until around 1985 and then increased. After 1985 there was a separation between treatments with δ15N in the 20% treatment increasing marginally more than the 10% treatment and considerably more than the dryland treatment. We had anticipated an increase and divergence in δ15N values from the start of the irrigation trial. In general soil δ15N scaled with intensity of grazing, which suggests that N losses were greater under more intensive systems. δ15N therefore shows potential as an indicator of the vulnerability of soils to N loss. Further work will investigate the relationship between changes in δ15N and total C and N at these two trials, and future work will seek to directly relate soil δ15N to cumulative N losses via leaching and gaseous emissions.

Nitrogen fertilization stimulates germination of dormant pin cherry seed

Treesearch

L.R. Auchmoody

1979-01-01

Nitrogen fertilizers triggered germination of dormant Prunus pensylvanica L. seed naturally buried in the forest floor of 60-year-old Allegheny hardwood stands. Neither triple superphosphate nor muriate of potash applied with urea increased germination over that which occurred with urea alone. Rates as low as 56 kg/ha N from urea and calcium...

Nitrogen Fertilization Increases Cottonwood Growth on Old-Field Soil

Treesearch

B. G. Blackmon; E. H. White

1972-01-01

Nitrogen (150 lb ./acre as NH4N03 ) applied to a 6-year-old eastern cottonwood plantation in an old field on Commerce silt loam soil increased diameter, basal area, and volume growth by 200 percent over untreated controls. The plantation did not respond to 100 pounds P per acre from concentrated superphosphate.

Current content of selected pollutants in moss, humus, soil and bark and long-term radial growth of pine trees in the Mezaparks forest in Riga.

PubMed

Pīrāga, Dace; Tabors, Guntis; Nikodemus, Oļģerts; Žīgure, Zane; Brūmelis, Guntis

2017-05-01

The aim of this study was to evaluate the use of various indicators in the assessment of environmental pollution and to determine the response of pine to changes of pollution levels. Mezaparks is a part of Riga that has been subject to various long-term effects of atmospheric pollution and, in particular, historically from a large superphosphate factory. To determine the spatial distribution of pollution, moss, pine bark and soil O and B horizons were used as sorbents in this study, as well as the additional annual increment of pine trees. The current spatial distribution of pollution is best shown by heavy metal accumulation in mosses and the long-term accumulation of P 2 O 5 pollution by the soil O horizon. The methodological problems of using these sorbents were explored in the study. Environmental pollution and its changes could be associated with the tree growth ring annual additional increment of Mezaparks pine forest stands. The additional increment increased after the closing of the Riga superphosphate factory.

40 CFR 60.232 - Standard for fluorides.

Code of Federal Regulations, 2010 CFR

2010-07-01

... 40 Protection of Environment 6 2010-07-01 2010-07-01 false Standard for fluorides. 60.232 Section... Industry: Triple Superphosphate Plants § 60.232 Standard for fluorides. On and after the date on which the... gases which contain total fluorides in excess of 100 g/megagram (Mg) of equivalent P2O5 feed (0.20 lb...

40 CFR 60.232 - Standard for fluorides.

Code of Federal Regulations, 2011 CFR

2011-07-01

... 40 Protection of Environment 6 2011-07-01 2011-07-01 false Standard for fluorides. 60.232 Section... Industry: Triple Superphosphate Plants § 60.232 Standard for fluorides. On and after the date on which the... gases which contain total fluorides in excess of 100 g/megagram (Mg) of equivalent P2O5 feed (0.20 lb...

Bedding and Fertilization Influence on Slash Pine Development in the Florida Sandhills

Treesearch

James B. Baker

1973-01-01

A field study on the infertile and droughty Lakeland sands of west Florida indicated that bedding or fertilization (134 kg P /ha as ordinary superphosphate and 90 kg N/ha as ammonium nitrate) or both increased early growth of planted slash pine ( Engelm.). Throughout the 6-year study, best growth was obtained when the treatments were...

Accumulation of lead and arsenic by peanut grown on lead and arsenic contaminated soils amended with broiler litter ash or superphosphate

USDA-ARS?s Scientific Manuscript database

Lead and arsenic are toxic metals that can be harmful to humans when inhaled or ingested via the consumption of drinking water or of crops grown on lead and arsenic contaminated soils. Lead and arsenic in the environment comes from industrial activities and the use of arsenical herbicides and insec...

40 CFR 60.242 - Standard for fluorides.

Code of Federal Regulations, 2012 CFR

2012-07-01

... atmosphere from any affected facility any gases which contain total fluorides in excess of 0.25 g/hr/megagram (Mg) of equivalent P2O5 stored (5.0 × 10 −4 lb/hr/ton of equivalent P2O5 stored). (b) No owner or... Industry: Granular Triple Superphosphate Storage Facilities § 60.242 Standard for fluorides. (a) On and...

40 CFR 60.242 - Standard for fluorides.

Code of Federal Regulations, 2013 CFR

2013-07-01

... atmosphere from any affected facility any gases which contain total fluorides in excess of 0.25 g/hr/megagram (Mg) of equivalent P2O5 stored (5.0 × 10 −4 lb/hr/ton of equivalent P2O5 stored). (b) No owner or... Industry: Granular Triple Superphosphate Storage Facilities § 60.242 Standard for fluorides. (a) On and...

40 CFR 60.242 - Standard for fluorides.

Code of Federal Regulations, 2014 CFR

2014-07-01

... atmosphere from any affected facility any gases which contain total fluorides in excess of 0.25 g/hr/megagram (Mg) of equivalent P2O5 stored (5.0 × 10 −4 lb/hr/ton of equivalent P2O5 stored). (b) No owner or... Industry: Granular Triple Superphosphate Storage Facilities § 60.242 Standard for fluorides. (a) On and...

Structural characterization of anion-calcium-humate complexes in phosphate-based fertilizers.

PubMed

Baigorri, Roberto; Urrutia, Oscar; Erro, Javier; Mandado, Marcos; Pérez-Juste, Ignacio; Garcia-Mina, José María

2013-07-01

Fertilizers based on phosphate-metal-humate complexes are a new family of compounds that represents a more sustainable and bioavailable phosphorus source. The characterization of this type of complex by using solid (31)P NMR in several fertilizers, based on single superphosphate (SSP) and triple superphosphate (TSP) matrices, yielded surprising and unexpected trends in the intensity and fine structure of the (31)P NMR peaks. Computational chemistry methods allowed the characterization of phosphate-calcium-humate complexes in both SSP and TSP matrices, but also predicted the formation of a stable sulfate-calcium-humate complex in the SSP fertilizers, which has not been described previously. The stability of this complex has been confirmed by using ultrafiltration techniques. Preference towards the humic substance for the sulfate-metal phase in SSP allowed the explanation of the opposing trends that were observed in the experimental (31)P NMR spectra of SSP and TSP samples. Additionally, computational chemistry has provided an assignment of the (31)P NMR signals to different phosphate ligands as well as valuable information about the relative strength of the phosphate-calcium interactions within the crystals. Copyright © 2013 WILEY-VCH Verlag GmbH & Co. KGaA, Weinheim.

JPRS Report, Soviet Union, Economic Affairs

DTIC Science & Technology

1988-06-28

reducing the application of melamine formaldehyde resins which are used for the final finishing processes of fabrics since a harmful sub- stance...superphosphate and urea for private plots. Many letters arrive from Siberia, the Urals, Moldavia and from the Moscow region. Even in Moscow itself...Progressive types of rolled metal, including galvanized steel sheet, as well as efficient plastics, resins , polymers, timber products etc., are being

Immobilization of Pb and Cu in polluted soil by superphosphate, multi-walled carbon nanotube, rice straw and its derived biochar.

PubMed

Rizwan, Muhammad Shahid; Imtiaz, Muhammad; Huang, Guoyong; Chhajro, Muhammad Afzal; Liu, Yonghong; Fu, Qingling; Zhu, Jun; Ashraf, Muhammad; Zafar, Mohsin; Bashir, Saqib; Hu, Hongqing

2016-08-01

Lead (Pb) and copper (Cu) contamination in croplands pose severe health hazards and environmental concerns throughout soil-food chain transfer. In the present study, BCR, TCLP, CaCl2, and SBET techniques were employed to evaluate the simultaneous effectiveness of rice straw (RS) and its derived biochar (BC), multiwall carbon nanotube (MWCNT), and single superphosphate (SSP) to immobilize the Pb and Cu in co-contaminated soil. The BCR sequential extraction results suggested that with increasing BC and SSP amount, the acid-soluble fractions decreased while oxidizable and residual proportions of Pb and Cu were increased significantly. Compared to SSP, the application of BC amendment substantially modified partitioning of Cu from easily exchangeable phase to less bioavailable residual bound fraction. The immobilized Pb and Cu were mainly transformed to reducible forms. The TCLP and CaCl2-extracted Pb and Cu were reduced significantly by the addition of BC compared to RS and MWCNT, whereas the bio-accessibility of Pb significantly reduced with RS addition. SSP showed better results for Pb immobilization while marginal for Cu in co-contaminated soil. Overall, the addition of BC offered the best results and could be effective in both Pb and Cu immobilization thereby reducing their mobility and bioavailability in the co-contaminated soil.

Comparative Analysis between Ecotoxicity of Nitrogen-, Phosphorus-, and Potassium-Based Fertilizers and Their Active Ingredients

PubMed Central

Simplício, Nathan de Castro Soares; Muniz, Daphne Heloísa de Freitas; Rocha, Fernanda Regina Moreira; Martins, Denis Cavalcanti; Dias, Zélia Malena Barreira; Farias, Bruno Pereira da Costa; Oliveira-Filho, Eduardo Cyrino

2016-01-01

This study aimed to analyze the ecotoxicity of nitrogen-, phosphorus-, and potassium-based compounds to organisms of two different trophic levels in order to compare the toxic effect between high-purity substances and these substances as components of fertilizers. Dilutions were made with the fertilizers’ potassium chloride, potassium nitrate, superphosphate, urea, and their equivalent reagents, to conduct assays to establish the acute lethal concentration for half of the population (LC50). Ten individuals of the benthic snail Biomphalaria glabrata and the fish Danio rerio were exposed to each concentration of tested compounds. As a result, the toxicity levels of potassium chloride, potassium nitrate, and urea were obtained for B. glabrata and D. rerio, with the fish being more susceptible to potassium chloride in the fertilizer and the snail to potassium nitrate and urea, in both commercial and reagent forms. Regarding superphosphate, no significant toxicity was found. This study concluded that among the tested substances, KNO3 and KCl were the most toxic substances and urea the least toxic. It was not possible to establish the most sensitive species since, for KCl, the fish were more susceptible to the fertilizer and the snail to the reagent, while for KNO3 the opposite was observed. PMID:29051434

Interactions between organic amendments and phosphate fertilizers modify phosphate sorption processes in an acid soil

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

Sckefe, C.R.; Patti, A.F.; Clune, T.S.

2008-07-15

To determine how organic amendments and phosphate fertilizers interact to modify P sorption processes, three phosphate fertilizers were applied to lignite- and compost-amended acid soil and incubated for either 3 or 26 days. The fertilizers applied were potassium dihydrogen phosphate, triple superphosphate, and diammonium phosphate (DAP). After 3 days of incubation, sorption of all three P sources was decreased in the lignite-amended treatments, whereas P sorption was increased in the compost-amended treatments. Increased incubation time (26 days) resulted in significantly decreased P sorption when DAP was added to lignite-amended treatments. Addition of triple superphosphate increased P sorption in lignite- andmore » compost-amended treatments and decreased solution pH compared with DAP application. In addition to the effect of P source, differences in P sorption between the lignite- and compost-amended treatments were driven by differences in solution chemistry, predominantly solution pH and cation dynamics. Soil amendment and fertilizer addition also increased microbial activity in the incubation systems, as measured by carbon dioxide respiration. It is proposed that the combination of lignite and DAP may contribute to decreased P sorption in acid soils, with the positive effects likely caused by both chemical and biological processes, including the formation of soluble organic-metal complexes.« less

PROCESS FOR THE RECOVERY OF URANIUM FROM PHOSPHATIC ORE

DOEpatents

Long, R.L.

1959-04-14

A proccss is described for the recovery of uranium from phosphatic products derived from phosphatic ores. It has been discovered that certain alkyl phosphatic, derivatives can be employed in a direct solvent extraction operation to recover uranium from solid products, such as superphosphates, without first dissolving such solids. The organic extractants found suitable include alkyl derivatives of phosphoric, pyrophosphoric, phosof the derivative contains from 4 to 7 carbon atoms. A diluent such as kerosene is also used.

Interaction of Endomycorrhizal Fungi, Superphosphate, and Meloidogyne incognita on Cotton in Microplot and Field Studies.

PubMed

Smith, G S; Roncadori, R W; Hussey, R S

1986-04-01

Microplot and field experiments were conducted to determine the effects of two vesicular-arbuscular mycorrhizal (VAM) fungi, Glomus intraradices (Gi) and Gigaspora margarita (Gm), and dicalcium phosphate (P) on Meloidogyne incognita (Mi) reproduction and seed cotton yield of the Mi-susceptible cotton cultivar, Stoneville 213. In 1983 population densities of Mi juveniles were significantly lower 60 and 90 days after planting in microplots receiving Gi. Mycorrhizal fungi reduced the severity of yield losses to Mi, whereas P fertilization increased yield losses to Mi. In 1984 microplot yields were reduced linearly as nematode inoculum densities increased in treatments of Mi alone, Gm, or P, but the response was curvilinear with Gi. Yield suppressions in the 1984 field experiment occurred only in plots infested with Mi alone. In the 1984 microplots, numbers of Mi juveniles penetrating seedling roots increased Iinearly with increasing nematode inoculum densities and was favored when mycorrhizal fungi or superphosphate were added. Juvenile penetration of roots was negatively correlated with yields in all treatments (r = -0.54 to -0.81) except Gm and with number of bolls in Mi alone (r = -0.85) and P (r = -0.81) treatments. Mycorrhizal fungi can increase host tolerance to M. incognita in field conditions and may function as important biological control agents in soils infested with high population densities of efficient VAM species.

[Effects of superphosphate addition on NH3 and greenhouse gas emissions during vegetable waste composting].

PubMed

Yang, Yan; Sun, Qin-ping; Li, Ni; Liu, Chun-sheng; Li, Ji-jin; Liu, Ben-sheng; Zou, Guo-yuan

2015-01-01

To study the effects of superphosphate (SP) on the NH, and greenhouse gas emissions, vegetable waste composting was performed for 27 days using 6 different treatments. In addition to the controls, five vegetable waste mixtures (0.77 m3 each) were treated with different amounts of the SP additive, namely, 5%, 10%, 15%, 20% and 25%. The ammonia volatilization loss and greenhouse gas emissions were measured during composting. Results indicated that the SP additive significantly decreased the ammonia volatilization and greenhouse gas emissions during vegetable waste composting. The additive reduced the total NH3 emission by 4.0% to 16.7%. The total greenhouse gas emissions (CO2-eq) of all treatments with SP additives were decreased by 10.2% to 20.8%, as compared with the controls. The NH3 emission during vegetable waste composting had the highest contribution to the greenhouse effect caused by the four different gases. The amount of NH3 (CO2-eq) from each treatment ranged from 59.90 kg . t-1 to 81.58 kg . t-1; NH3(CO2-eq) accounted for 69% to 77% of the total emissions from the four gases. Therefore, SP is a cost-effective phosphorus-based fertilizer that can be used as an additive during vegetable waste composting to reduce the NH3 and greenhouse gas emissions as well as to improve the value of compost as a fertilizer.

Commercial fertilizers 1992

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

Berry, J.T.; Montgomery, M.H.

1992-12-01

Fertilizer consumption information in the USA for 1992 submitted by state regulatory officials is presented. This includes total sales or shipments for farm and non-farm use. Liming materials were excluded. Materials used for manufacture or blending of reported fertilizers or for use in other fertilizers are excluded to avoid double-counting. The consumption of multiple-nutrient and single-nutrient fertilizers is listed. Dry bulk, fluid, and bagged classes are given. Typical fertilizers include: anhydrous ammonia, aqua ammonia, nitrogen solutions, urea, ammonium nitrates, ammonium sulfates, phosphoric acid, superphosphates, potassium chlorides, and potassium sulfates.

Determination of Cd, Cr and Pb in phosphate fertilizers by laser-induced breakdown spectroscopy

NASA Astrophysics Data System (ADS)

Nunes, Lidiane Cristina; de Carvalho, Gabriel Gustinelli Arantes; Santos, Dario; Krug, Francisco José

2014-07-01

A validated method for quantitative determination of Cd, Cr, and Pb in phosphate fertilizers by laser-induced breakdown spectroscopy (LIBS) is presented. Laboratory samples were comminuted and homogenized by cryogenic or planetary ball milling, pressed into pellets and analyzed by LIBS. The experimental setup was designed by using a Q-switched Nd:YAG at 1064 nm with 10 Hz repetition rate, and the intensity signals from Cd II 214.441 nm, Cr II 267.716 nm and Pb II 220.353 nm emission lines were measured by using a spectrometer furnished with an intensified charge-coupled device. LIBS parameters (laser fluence, lens-to-sample distance, delay time, integration time gate, number of sites and number of laser pulses per site) were chosen after univariate experiments with a pellet of NIST SRM 695 (Trace Elements in Multi-Nutrient Fertilizer). Calibration and validation were carried out with 30 fertilizer samples from single superphosphate, triple superphosphate, monoammonium phosphate, and NPK mixtures. Good results were obtained by using 30 pulses of 50 J cm- 2 (750 μm spot size), 2.0 μs delay time and 5.0 μs integration time gate. No significant differences between Cd, Cr, and Pb mass fractions determined by the proposed LIBS method and by ICP OES after microwave-assisted acid digestion (AOAC 2006.03 Official Method) were found at 95% confidence level. The limits of detection of 1 mg kg- 1 Cd, 2 mg kg- 1 Cr and 15 mg kg- 1 Pb and the precision (coefficients of variation of results ranging from 2% to 15%) indicate that the proposed LIBS method can be recommended for the determination of these analytes in phosphate fertilizers.

Field studies of the effect of chemical fertilizers on the quality of ground- and drainage waters

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

Kondratas, A.R.

1988-01-01

This article describes a field study of the effect of a variety of fertilizers--superphosphates, potassium chlorides, and ammonium nitrates--used in the cultivation of corn on the ground and runoff waters comprising a regional water resource. The experiment establishes that the fertilizers have a substantial effect on runoff waters--the formation of their chemical composition and mineralization--and a lesser effect on ground water. The study accounts for meteorological factors as well as dispersion behavior of the water in the soil and its eventual transport to the water resource and supply system. Conservation measures are indicated based on the results.

Improving Water Use Efficiency of Lettuce (Lactuca sativa L.) Using Phosphorous Fertilizers.

PubMed

Alkhader, Asad M F; Abu Rayyan, Azmi M

2013-01-01

A greenhouse pot experiment was conducted to evaluate the effect of phosphorous (P) fertilizers application to an alkaline calcareous soil on the water use efficiency (WUE) of lettuce cultivar "robinson" of iceberg type. Head fresh and dry weights, total water applied and WUE were affected significantly by the P fertilizer type and rate. P fertilizers addition induced a significant enhancement in the WUE and fresh and dry weights of the crop. A local phosphate rock (PR) applied directly was found to be inferior to the other types of P fertilizers (Mono ammonium phosphate (MAP), Single superphosphate (SSP), and Di ammonium phosphate ((DAP)). MAP fertilizer at 375 and 500 kg P2O5/ha application rates recorded the highest significant values of head fresh weight and WUE, respectively.

Degree of Phosphorus Saturation and Soil Phosphorus Thresholds in an Ultisol Amended with Triple Superphosphate and Phosphate Rocks

PubMed Central

Gikonyo, E. W.; Zaharah, A. R.; Hanafi, M. M.; Anuar, A. R.

2011-01-01

Soil phosphorus (P) release capability could be assessed through the degree of P saturation (DPS). Our main objective was to determine DPS and, hence, P threshold DPS values of an Ultisol treated with triple superphosphate (TSP), Gafsa phosphate rocks (GPR), or Christmas Island phosphate rocks (CIPR), plus or minus manure. P release was determined by the iron oxide—impregnated paper strip (strip P), while DPS was determined from ammonium oxalate—extractable aluminum (Al), iron (Fe), and P. Soils were sampled from a closed incubation study involving soils treated with TSP, GPR, and CIPR at 0–400 mg P kg-1, and a field study where soils were fertilized with the same P sources at 100–300 kg P ha-1 plus or minus manure. The DPS was significantly influenced by P source x P rate, P source x manure (incubated soils), and by P source x P rate x time (field-sampled soils). Incubated soil results indicated that both initial P and total strip P were related to DPS by exponential functions: initial strip P = 1.38exp0.18DPS, R2 = 0.82** and total strip P = 8.01exp0.13DPS, R2 = 0.65**. Initial strip P was linearly related to total P; total P = 2.45, initial P + 8.41, R2 = 0.85**. The threshold DPS value established was about 22% (incubated soil). Field soils had lower DPS values <12% and strip P was related to initial DPS and average DPS in exponential functions: strip P = 2.6exp0.44DPS, R2 = 0.77** and strip P = 1.1DPS2 — 2.4DPS + 6.2, R2 = 0.58**, respectively. The threshold values were both at ≈8% and P release was 11–14 mg P kg-1. Results are evident that DPS can be used to predict P release, but the threshold values are environmentally sensitive; hence, recommendations should be based on field trials. PMID:21805012

Degree of phosphorus saturation and soil phosphorus thresholds in an ultisol amended with triple superphosphate and phosphate rocks.

PubMed

Gikonyo, E W; Zaharah, A R; Hanafi, M M; Anuar, A R

2011-07-28

Soil phosphorus (P) release capability could be assessed through the degree of P saturation (DPS). Our main objective was to determine DPS and, hence, P threshold DPS values of an Ultisol treated with triple superphosphate (TSP), Gafsa phosphate rocks (GPR), or Christmas Island phosphate rocks (CIPR), plus or minus manure. P release was determined by the iron oxide-impregnated paper strip (strip P), while DPS was determined from ammonium oxalate-extractable aluminum (Al), iron (Fe), and P. Soils were sampled from a closed incubation study involving soils treated with TSP, GPR, and CIPR at 0-400 mg P kg-1, and a field study where soils were fertilized with the same P sources at 100-300 kg P ha-1 plus or minus manure. The DPS was significantly influenced by P source x P rate, P source x manure (incubated soils), and by P source x P rate x time (field-sampled soils). Incubated soil results indicated that both initial P and total strip P were related to DPS by exponential functions: initial strip P = 1.38exp0.18DPS, R2 = 0.82** and total strip P = 8.01exp0.13DPS, R2 = 0.65**. Initial strip P was linearly related to total P; total P = 2.45, initial P + 8.41, R2 = 0.85**. The threshold DPS value established was about 22% (incubated soil). Field soils had lower DPS values <12% and strip P was related to initial DPS and average DPS in exponential functions: strip P = 2.6exp0.44DPS, R2 = 0.77** and strip P = 1.1DPS2 ¨C 2.4DPS + 6.2, R2 = 0.58**, respectively. The threshold values were both approximately equal to 8% and P release was 11-14 mg P kg-1. Results are evident that DPS can be used to predict P release, but the threshold values are environmentally sensitive; hence, recommendations should be based on field trials.

Effects of fluorides on metabolism and visible injury in cut-flower crops and citrus

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

Woltz, S.S.; Waters, W.E.; Leonard, C.D.

1971-01-01

Fluoride taken up by gladiolus roots caused foliar damage only when soil pH was low and F/sup -/ containing superphosphate was applied in relatively excessive amounts. This damage to leaves occurred more to leaf interior than to margins and tips as in F/sup -/ fumigation. Fluoride in leaves was found to move passively with the transpirational stream of water and accumulated at the terminus of translocation. Rose and gladiolus cut-flowers were damaged by low concentrations of F/sup -/ in vase water whereas the chrysanthemum was less affected. De novo chlorophyll synthesis in Vigna sinensis seedling leaves was inhibited by F/supmore » -/ absorbed by detached seedling tops. Yield of Valencia orange fruit was depressed by air-borne F/sup -/. Valencia leaves (a) were reduced in size, (b) had decreased photosynthetic rates and (c) had decreased chlorophyll content in response to increasing levels of airborne F/sup -/. 11 references, 6 tables.« less

Effects of anabolic and catabolic nutrients on woody plant encroachment after long-term experimental fertilization in a South African savanna

PubMed Central

Milewski, Antoni V.; Snyman, Dirk; Jordaan, Jorrie J.

2017-01-01

The causes of the worldwide problem of encroachment of woody plants into grassy vegetation are elusive. The effects of soil nutrients on competition between herbaceous and woody plants in various landscapes are particularly poorly understood. A long-term experiment of 60 plots in a South African savanna, comprising annual applications of ammonium sulphate (146–1166 kg ha-1 yr-1) and superphosphate (233–466 kg ha-1 yr-1) over three decades, and subsequent passive protection over another three decades, during which indigenous trees encroached on different plots to extremely variable degrees, provided an opportunity to investigate relationships between soil properties and woody encroachment. All topsoils were analysed for pH, acidity, EC, water-dispersible clay, Na, Mg, K, Ca, P, S, C, N, NH4, NO3, B, Mn, Cu and Zn. Applications of ammonium sulphate (AS), but not superphosphate (SP), greatly constrained tree abundance relative to control plots. Differences between control plots and plots that had received maximal AS application were particularly marked (16.3 ± 5.7 versus 1.2 ± 0.8 trees per plot). Soil properties most affected by AS applications included pH (H2O) (control to maximal AS application: 6.4 ± 0.1 to 5.1 ± 0.2), pH (KCl) (5.5 ± 0.2 to 4.0 ± 0.1), acidity (0.7 ± 0.1 to 2.6 ± 0.3 cmol kg-1), acid saturation (8 ± 2 to 40 ± 5%), Mg (386 ± 25 to 143 ± 15 mg kg-1), Ca (1022 ± 180 to 322 ± 14 mg kg-1), Mn (314 ± 11 to 118 ± 9 mg kg-1), Cu (3.6 ± 0.3 to 2.3 ± 0.2 mg kg-1) and Zn (6.6 ± 0.4 to 3.7 ± 0.4 mg kg-1). Magnesium, B, Mn and Cu were identified using principal component analysis, boundary line analysis and Kruskal-Wallis rank sum tests as the nutrients most likely to be affecting tree abundance. The ratio Mn/Cu was most related to tree abundance across the experiment, supporting the hypothesis that competition between herbaceous and woody plants depends on the availability of anabolic relative to catabolic nutrients. These findings, based on more than six decades of experimentation, may have global significance for the theoretical understanding of changes in vegetation structure and thus the practical control of invasive woody plants. PMID:28662068

Improvement of nutritional quality of greenhouse-grown lettuce by arbuscular mycorrhizal fungi is conditioned by the source of phosphorus nutrition.

PubMed

Baslam, Marouane; Pascual, Inmaculada; Sánchez-Díaz, Manuel; Erro, Javier; García-Mina, José María; Goicoechea, Nieves

2011-10-26

The improvement of the nutritional quality of lettuce by its association with arbuscular mycorrhizal fungi (AMF) has been recently reported in a previous study. The aim of this research was to evaluate if the fertilization with three P sources differing in water solubility affects the effectiveness of AMF for improving lettuce growth and nutritional quality. The application of either water-soluble P sources (Hewitt's solution and single superphosphate) or the water-insoluble (WI) fraction of a "rhizosphere-controlled fertilizer" did not exert negative effects on the establishment of the mycorrhizal symbiosis. AMF improved lettuce growth and nutritional quality. Nevertheless, the effect was dependent on the source of P and cultivar. Batavia Rubia Munguía (green cultivar) benefited more than Maravilla de Verano (red cultivar) in terms of mineral nutrients, total soluble sugars, and ascorbate contents. The association of lettuce with AMF resulted in greater quantities of anthocyanins in plants fertilized with WI, carotenoids when plants received either Hewitt's solution or WI, and phenolics regardless of the P fertilizer applied.

Relation of pH and other soil variables to concentrations of Pb, Cu, Zn, Cd, and Se in earthworms

USGS Publications Warehouse

Beyer, W.N.; Hensler, G.L.; Moore, J.

1987-01-01

Various soil treatments (clay, composted peat, superphosphate, sulfur, calcium carbonate, calcium chloride, zinc chloride, selenous acid) were added to experimental field plots to test the effect of different soil variables on the concentrations of 5 elements in earthworms (Pb, Cu, Zn, Cd, Se). Concentrations of the 5 elements were related to 9 soil variables (soil Pb, soil Cu, soil Zn, pH, organic matter, P, K, Mg, and Ca) with linear multiple regression. Lead concentrations in earthworms were positively correlated with soil Pb and soil organic matter, and negatively correlated with soil pH and soil Mg, with an R2 of 64%. Se concentrations were higher in earthworms from plots amended with Se, and Zn concentrations were higher in earthworms from plots amended with Zn. However, none of the other soil variables had important effects on the concentrations of Cu, Zn, Cd and Se in earthworms. Although some significant statistical relations were demonstrated, the values of r2 of all relations (> 20%) were so low that they had little predictive value.

Assessing phytotoxicity of heavy metals in remediated soil.

PubMed

Branzini, A; Zubillaga, M S

2010-01-01

Copper (Cu), zinc (Zn) and chromium (Cr) are pollutants that usually are accumulated in soils. Their toxicity can be decreased by applying amendments. We proposed to evaluate changes in Cu, Zn, and Cr availability, due to the application of amendments, through chemical analysis and phytotoxicity tests. The phytotoxicity test was carried out using species belonging to Sesbania genus; plant parameters were measured 48, 72, 96, and 168 hours after the start of incubation. The treatments included enriched soil, in addition to biosolid compost and triple superphosphate. Cu and Zn amounts were higher in treatments without amendments, indicating immobilization on the part of these. The amounts of Cr tended to decrease with amendments application. The amendments increased pH values and decreased EC; however, this had no impact on the results. No relationship was found among pH, EC, and plant parameters. Different behaviors were observed. S. virgata showed germination seed delay. In addition, while in S. virgata the IG increased during the assay, in S. punicea it diminished. The application of compost, fertilizer or both combined could be of interest for contaminated soils remediation. The use of chemical analysis and phytotoxicity tests allowed to estimate heavy metal availability and the effect on both Sesbania species.

Improving Phosphorus Availability in an Acid Soil Using Organic Amendments Produced from Agroindustrial Wastes

PubMed Central

Ch'ng, Huck Ywih; Ahmed, Osumanu Haruna; Majid, Nik Muhamad Ab.

2014-01-01

In acid soils, soluble inorganic phosphorus is fixed by aluminium and iron. To overcome this problem, acid soils are limed to fix aluminium and iron but this practice is not economical. The practice is also not environmentally friendly. This study was conducted to improve phosphorus availability using organic amendments (biochar and compost produced from chicken litter and pineapple leaves, resp.) to fix aluminium and iron instead of phosphorus. Amending soil with biochar or compost or a mixture of biochar and compost increased total phosphorus, available phosphorus, inorganic phosphorus fractions (soluble inorganic phosphorus, aluminium bound inorganic phosphorus, iron bound inorganic phosphorus, redundant soluble inorganic phosphorus, and calcium bound phosphorus), and organic phosphorus. This was possible because the organic amendments increased soil pH and reduced exchangeable acidity, exchangeable aluminium, and exchangeable iron. The findings suggest that the organic amendments altered soil chemical properties in a way that enhanced the availability of phosphorus in this study. The amendments effectively fixed aluminium and iron instead of phosphorus, thus rendering phosphorus available by keeping the inorganic phosphorus in a bioavailable labile phosphorus pool for a longer period compared with application of Triple Superphosphate without organic amendments. PMID:25032229

Increased Phosphorus Uptake by Wheat and Field Beans Inoculated with a Phosphorus-Solubilizing Penicillium bilaji Strain and with Vesicular-Arbuscular Mycorrhizal Fungi.

PubMed

Kucey, R M

1987-12-01

Greenhouse and field experiments were conducted to test the effect of a P-solubilizing isolate of Penicillium bilaji on the availability of Idaho rock phosphate (RP) in a calcareous soil. Under controlled greenhouse conditions, inoculation of soils with P. bilaji along with RP at 45 mug of P per g of soil resulted in plant dry matter production and P uptake by wheat (Triticum aestivum) and beans (Phaseolus vulgaris) that were not significantly different from the increases in dry matter production and P uptake caused by the addition of 15 mug of P per g of soil as triple superphosphate. Addition of RP alone had no effect on plant growth. Addition of vesicular-arbuscular mycorrhizal fungi was necessary for maximum effect in the sterilized soil in the greenhouse experiment. Under field conditions, a treatment consisting of RP (20 kg of P per ha of soil) plus P. bilaji plus straw resulted in wheat yields and P uptake equivalent to increases due to the addition of monoammonium phosphate added at an equivalent rate of P. RP added alone had no effect on wheat growth or P uptake. The results indicate that a biological system of RP solubilization can be used to increase the availability of RP added to calcareous soils.

Potential negative consequences of adding phosphorus-based fertilizers to immobilize lead in soil

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

Kilgour, Douglas W.; Moseley, Rebecca A.; Savage, Kaye S

2008-09-01

A study of the potential negative consequences of adding phosphate (P)-based fertilizers as amendments to immobilize lead (Pb) in contaminated soils was conducted. Lead-contaminated firing range soils also contained elevated concentrations of antimony (Sb), a common Pb hardening agent, and some arsenic (As) of unknown (possibly background) origin. After amending the soils with triple superphosphate, a relatively soluble P source, column leaching experiments revealed elevated concentrations of Sb, As, and Pb in the leachate, reflecting an initial spike in soluble Pb and a particularly dramatic increase in Sb and As mobility. Minimal As, Sb, and Pb leaching was observed duringmore » column tests performed on non-amended control soils. In vitro extractions tests were performed to assess changes in Pb, As, and Sb bioaccessibility on P amendment. Lead bioaccessibility was systematically lowered with increasing P dosage, but there was much less of an effect on As and Sb bioaccessibility than on mobility. Our results indicate that although P amendments may aid in lowering the bioaccessibility of soil-bound Pb, it may also produce an initial increase in Pb mobility and a significant release of Sb and As from the soil, dramatically increasing their mobility and to a lesser extent their bioavailability.« less

Phytoremediation of arsenic contaminated soil by Pteris vittata L. I. Influence of phosphatic fertilizers and repeated harvests.

PubMed

Mandal, Asit; Purakayastha, T J; Patra, A K; Sanyal, S K

2012-12-01

A greenhouse experiment was conducted to evaluate the effectiveness of diammonium phosphate (DAP), single superphosphate (SSP) and two growing cycles on arsenic removal by Chinese Brake Fern (Pteris vittata L.) from an arsenic contaminated Typic Haplustept of the Indian state of West Bengal. After harvest of Pteris vittata the total, Olsen's extractable and other five soil arsenic fractions were determined. The total biomass yield of P. vittata ranged from 10.7 to 16.2 g pot(-1) in first growing cycle and from 7.53 to 11.57 g pot(-1) in second growing cycle. The frond arsenic concentrations ranged from 990 to 1374 mg kg(-1) in first growing cycle and from 875 to 1371 mg kg(-1) in second growing cycle. DAP was most efficient in enhancing biomass yield, frond and root arsenic concentrations and total arsenic removal from soil. After first growing cycle, P. vittata reduced soil arsenic by 10 to 20%, while after two growing cycles Pteris reduced it by 18 to 34%. Among the different arsenic fractions, Fe-bound arsenic dominated over other fractions. Two successive harvests with DAP as the phosphate fertilizer emerged as the promising management strategy for amelioration of arsenic contaminated soil of West Bengal through phyotoextraction by P. vittata.

Removal of sewage phosphorus by adsorption and mineral precipitation, with recovery as a fertilizing soil amendment.

PubMed

Jowett, Craig; Solntseva, Irina; Wu, Lingling; James, Chris; Glasauer, Susan

2018-05-01

Clear sand adsorbs 15-35% total phosphorus (P) from septic tank effluent, but P is mobilized when low-P effluent is applied. Amorphous P compounds formed by alkali aluminate chemical addition may also be subject to leaching. Crystalline mineralization is the desired end effect that isolates P thoroughly from the water resource. Using new low-energy iron electrochemistry (EC-P process), dissolved ferrous iron reacts with sewage phosphate ions (PO 4 ) and precipitates onto filtration medium as vivianite [Fe 3 (PO 4 ) 2 ·8H 2 O], as identified by scanning electron microscopy and X-ray diffraction and predicted from Eh-pH-aHPO 4 2- phase relations. Removal rates of 90-99% in sand, soil and synthetic foam filters are obtained. The precipitation of vivianite demonstrates that P can be immobilized quickly and without intermediary adsorption phases, as with Fe-rich soils. Vitreous silicate material (VSM) or rockwool that traps and precipitates mineral P after EC-P treatment was investigated as a means of P reuse as a fertilizing soil amendment. Comparative soil leaching and growth studies using corn plants demonstrate that the VSM alone reduces P losses from soils, and that VSM which has received EC-P effluent is equivalent to or better than commercial superphosphate fertilizer.

Characterization and obtainment of phosphate rock concentrates of Turmequé, Boyacá

NASA Astrophysics Data System (ADS)

Zanguña, S. Quijano; Lozano Gómez, L. F.; Pineda Triana, Y.

2017-12-01

The work focuses on the use and exploitation of the mineral concentrates from phosphate rock (PR) coming from mines with a low percentage of phosphorus. The procedure was based on the collection of a source of phosphate rock from the department of Boyacá (municipality of Turmequé), using a randomized design with three replications. The samples were initially milled and sifted using meshes between 140 and 200 US standard, homogenizing them and improving the process of solubility of the phosphorus in the soil. We conduced Z-potential tests, which show that by performing a prior wash on the mineral and maintaining certain concentrations and pH defined, better results are achieved in terms of the buoyancy of the particles in the flotation process. The results obtained from the microflotation tests; both direct and inverse, and the results of chemical composition, with X-Ray Fluorescence (XRF) and X-Ray Diffraction (XRD), before and after the microflotation process, were carried out to obtain of commercial laws grade phosphate rock concentrate, confirm that the protocol used increases by 9% the value of total phosphorus in the collected sample. These concentrates from phosphate rock, could be used in the future for the attainment of simple superphosphate (SSP), with the help of sulphuric acid and ammonium thiosulphate mixtures.

Response of Sugarcane in a Red Ultisol to Phosphorus Rates, Phosphorus Sources, and Filter Cake

PubMed Central

Prado, Renato de Mello; Campos, Cid Naudi Silva; Rosatto Moda, Leandro; de Lima Vasconcelos, Ricardo; Pizauro Júnior, João Martins

2015-01-01

We evaluated the effect of phosphorus application rates from various sources and in the presence or absence of filter cake on soil phosphorus, plant phosphorus, changes in acid phosphatase activity, and sugarcane productivity grown in Eutrophic Red Ultisol. Three P sources were used (triple superphosphate, Araxa rock phosphate, and Bayovar rock phosphate) and four application rates (0, 90, 180, and 360 kg ha−1 of P2O5) in the presence or absence of filter cake (7.5 t ha−1, dry basis). The soil P, the accumulated plant P, the leaf acid phosphatase activity and straw, the stalk productivity, the concentration of soluble solids in the juice (Brix), the juice sucrose content (Pol), and the purity were the parameters evaluated. We found that P applications increased levels of soil, leaf, and juice phosphorus and led to higher phosphorus accumulation and greater stalk and straw productivity. These levels were highest in the presence of filter cake. Acid phosphatase activity decreased with increasing plant phosphorus concentration. Phosphate fertilization did not show effect on sugarcane technological quality. We concluded that P application, regardless of source, improved phosphorus nutrition and increased productivity in sugarcane and, when associated with filter cake, reduced the need for mineral fertilizer. PMID:26078993

Effect of phosphoric fertilizer and starter rates of nitrogen fertilizers on the phosphatase activity in the rhizosphere soil and nonlignified soybean roots under drought conditions

NASA Astrophysics Data System (ADS)

Emnova, E. E.; Daraban, O. V.; Bizgan, I. V.; Toma, S. I.

2014-02-01

In a small-plot field experiment, two soybean ( Glycine max L.) cultivars were grown on a calcareous chernozem under the drought conditions of 2012 with the preplanting application of simple superphosphate (Ps) at 60 kg/ha, urea (Nu) at 10 and 20 kg/ha, and ammonium nitrate (Nan) at 20 kg/ha. The phosphatase activity was measured in the rhizosphere soil (0- to 20-cm layer) and the fine nonlignified roots of soybean plants at the blossoming and pod-formation stages (the soil water content was 19 and 33% of the total water capacity, respectively). The maximum content of available phosphorus in the rhizosphere of both soybean cultivars (4.3-4.8 mg/100 g dry soil) was found at the simultaneous application of Ps and Nu20. Higher activities of the predominant phosphatases (alkaline phosphatase in the rhizosphere and acid phosphatase in the roots) were observed in the root-inhabited zone of the soil under the Indra cultivar compared to the Aura cultivar, which correlated with the lower content of available phosphorus in the rhizosphere soil (especially at the simultaneous application of Ps and Nu20) and the higher productivity of this cultivar in this treatment.

Agronomic efficiency of phosphate fertilizers produced by the re-use of a metallurgical acid residue.

PubMed

Barreto, Matheus Sampaio Carneiro; Mattiello, Edson Marcio; Santos, Wedisson Oliveira; Melo, Leônidas Carrijo Azevedo; Vergütz, Leonardus; Novais, Roberto Ferreira

2018-02-15

The production of fertilizers with industrial wastes reduces the environmental impacts of waste disposal and improves environmental sustainability by generating added-value products. Our objective with this study was to evaluate the agronomic performance and potential soil/plant contamination with heavy metals of alternative phosphate (P) fertilizers, obtained from the acidulation of phosphate rocks (PR) by a metallurgical acidic waste. Seven P fertilizers were evaluated: three PR (Araxá, Patos, and Bayóvar), their respective acidulated products (PAPR), and triple superphosphate fertilizer (TSP). A greenhouse trial was carried out to test the agronomic performances of fertilizers in a sequentially cultivated maize-soybean-white oat. The reaction of PR with acid waste was effective to increase their solubility and improve plant yield and P uptake compared to their natural PR. There was a cumulative recovery by plants of 1.4 and 8.1% of added P via PR and PAPR, respectively. No increase in heavy metal (Cd, Pb, Cr, and Ni) availability in soil or accumulation in shoots was observed, indicating that the PAPR were environmentally safe. The usage of acid waste to produce P fertilizers therefore represents a strategic way to employ marginal products for the production of fertilizers. Copyright © 2017 Elsevier Ltd. All rights reserved.

Novel Applications for Oxalate-Phosphate-Amine Metal-Organic-Frameworks (OPA-MOFs): Can an Iron-Based OPA-MOF Be Used as Slow-Release Fertilizer?

PubMed Central

Anstoetz, Manuela; Rose, Terry J.; Clark, Malcolm W.; Yee, Lachlan H.; Raymond, Carolyn A.; Vancov, Tony

2015-01-01

A porous iron-based oxalate-phosphate-amine metal-organic framework material (OPA-MOF) was investigated as a microbially-induced slow-release nitrogen (N) and phosphorus (P) fertilizer. Seedling growth, grain yields, nutrient uptake of wheat plants, and soil dynamics in incubated soil, were investigated using OPA-MOF vs standard P (triple-superphosphate) and N (urea) fertilizers in an acidic Ferralsol at two application rates (equivalent 120 and 40 kg N ha-1). While urea hydrolysis in the OPA-MOF treatment was rapid, conversion of ammonium to nitrate was significantly inhibited compared to urea treatment. Reduced wheat growth in OPA-MOF treatments was not caused by N-deficiency, but by limited P-bioavailability. Two likely reasons were slow P-mobilisation from the OPA-MOF or rapid P-binding in the acid soil. P-uptake and yield in OPA-MOF treatments were significantly higher than in nil-P controls, but significantly lower than in conventionally-fertilised plants. OPA-MOF showed potential as enhanced efficiency N fertilizer. However, as P-bioavailability was insufficient to meet plant demands, further work should determine if P-availability may be enhanced in alkaline soils, or whether central ions other than Fe, forming the inorganic metal-P framework in the MOF, may act as a more effective P-source in acid soils. PMID:26633174

Liming induces carbon dioxide (CO2) emission in PSB inoculated alkaline soil supplemented with different phosphorus sources.

PubMed

Adnan, Muhammad; Shah, Zahir; Sharif, Muhammad; Rahman, Hidayatur

2018-04-01

Agricultural land is a major sink of global organic carbon (C). Its suitable management is crucial for improving C sequestration and reducing soil CO 2 emission. Incubation experiments were performed to assess the impact of phosphate solubilizing bacterial (PSB) inoculation (inoculated and uninoculated) and soil calcification (4.78, 10, 15, and 20% crushed CaCO 3 ) with phosphorus (P) sources [single superphosphate (SSP), rock phosphate (RP), farm yard manure (FYM), and poultry manure (PM)] in experiment 1 and with various rates of PM (4, 8, and 12 kg ha -1 ) in experiment 2 on cumulative soil respiration. These experiments were arranged in three factorial, complete randomize design (CRD) with three replications. Interactively, lime with P sources (at day 1 and 3) and lime with PSB (at day 1) significantly expedited soil respiration. Mainly, PSB inoculation, liming, PM fertilization, and its various rates significantly enhanced soil respiration with time over control/minimum in alkaline soil at all incubation periods. Higher CO 2 emission was detected in soil supplemented with organic P sources (PM and FYM) than mineral sources (SSP and RP). CO 2 emission was noted to increase with increasing PM content. Since liming intensified CO 2 discharge from soil, therefore addition of lime to an alkaline soil should be avoided; instead, integrated approaches must be adopted for P management in alkaline calcareous soils for climate-smart agriculture.

Phosphorus availability and microbial immobilization in a Nitisol with the application of mineral and organo-mineral fertilizers.

PubMed

Morais, Francisco A; Gatiboni, Luciano C

2015-01-01

The aim of this study was to evaluate P availability, P and C contained in the microbial biomass, and enzymatic activity (acid phosphatases and β-glucosidases) in a Nitisol with the application of mineral and organo-mineral fertilizers. The experiment was performed in a protected environment with control over air temperature and soil moisture. The experimental design was organized in a "5 x 4" factorial arrangement with five sources of P and four times of soil incubation. The sources were: control (without P), triple superphosphate, diammonium phosphate, natural Arad reactive rock phosphate, and organo-mineral fertilizer. The experimental units consisted of PVC columns filled with agricultural soil. The columns were incubated and broken down for analysis at 1, 20, 40, and 60 days after application of the fertilizers. In each column, samples were taken at the layers of 0-2.5, 2.5-5.0, and 5.0-15.0 cm below the zone of the fertilizers. The application of soluble phosphates and organo-mineral fertilizer temporarily increased P availability in the zone near the fertilizers (0-2.5 cm), with maximum availability occurring at approximately 32 days. Microbial immobilization showed behavior similar to P availability, and the greatest immobilizations occurred at approximately 30 days. The organo-mineral fertilizer was not different from soluble phosphates.

Influence of amendments on soil arsenic fractionation and phytoavailability by Pteris vittata L.

PubMed

Yan, Xiulan; Zhang, Min; Liao, Xiaoyong; Tu, Shuxin

2012-06-01

Increasing availability of soil arsenic is of significance for accelerating phytoremediation efficiency of As-polluted sites. The effects of seven amendments, i.e., citrate, oxalate, EDTA, sodium polyacrylate (SPA), phosphate rock (PR), single superphosphate (SSP), and compost on fractionation and phytoavailability of soil As were investigated in lab culture experiment. The results showed that the addition of PR, SPA, EDTA or compost to soils significantly increased the concentration of NaHCO(3)-extractable As over a 120 d incubation period compared with the control (amendment-free) soil. Then, the four amendments were selected to add to As-contaminated soil growing Pteris vittata. It was concluded that As accumulation by the fern increased significantly under the treatments of PR and SPA by 25% and 31%, respectively. For As fractionation in soil, SPA increased Fe-As significantly by 51% and PR increased Ca-As significantly by 18%, while both the two amendments reduced occluded-As by 16% and 19%, respectively. Adding PR and SPA in soil increased the activities of urease and neutral phosphatase resulting from the improvement the fertility and physical structure of the soil, which benefits plant growth and As absorption of P. vittata. The results of the research revealed that both PR and SPA were effective amendments for improving phytoremediation of As-contaminated sites by P. vittata. Copyright © 2012 Elsevier Ltd. All rights reserved.

Impacts of delayed addition of N-rich and acidic substrates on nitrogen loss and compost quality during pig manure composting.

PubMed

Jiang, Jishao; Kang, Kang; Chen, Dan; Liu, Ningning

2018-02-01

Delayed addition of Nitrogen (N)-rich and acidic substrates was investigated to evaluate its effects on N loss and compost quality during the composting process. Three different delayed adding methods of N-rich (pig manure) and acidic substrates (phosphate fertilizer and rotten apples) were tested during the pig manure and wheat straw is composting. The results showed that delayed addition of pig manure and acidic materials led two temperature peaks, and the durations of two separate thermophilic phase were closely related to the amount of pig manure. Delayed addition reduced total N loss by up to 14% when using superphosphate as acidic substrates, and by up to 12% when using rotten apples as acidic substrates, which is mainly due to the decreased NH 3 emissions. At the end of composting, delayed the addition of pig manure caused a significant increase in the HS (humus substance) content, and the highest HS content was observed when 70% of the pig manure was applied at day 0 and the remaining 30% was applied on day 27. In the final compost, the GI in all treatments almost reached the maturity requirement by exceeding 80%. The results suggest that delayed addition of animal manure and acidic substrates could prevent the N loss during composting and improve the compost quality. Copyright © 2017 Elsevier Ltd. All rights reserved.

Bioremediation of kerosene I: A case study in liquid media.

PubMed

Gouda, Mona K; Omar, Sanaa H; Chekroud, Zohra A; Nour Eldin, Hemdan M

2007-11-01

The ability of different local isolates in addition to some isolates from Germany to degrade kerosene in liquid medium was studied. The results showed that the percent of kerosene degradation varied among the different organisms and that 59-94% of kerosene was degraded after 21d. Two local isolates (Pseudomonas sp. AP and Pseudomonas sp. CK) and one German isolate (Gordonia sp. DM) were selected for this study. The addition of wheat bran, as co-substrate, stimulated the kerosene degradation by the two local strains, while glucose inhibited the degradation rate using the three organisms with different rates. Ammonium nitrate and urea was the best nitrogen sources. The use of superphosphate (as phosphorus source) in the presence of urea stimulates the degradation rate. It was also observed that the addition of 1% surfactants, like Triton X-100, Igepal, Tergitol, or Tween 20 and 80 enhanced the kerosene degradation. The degradation percent lied between 94% and 98%. The ability of the tested organisms to degrade kerosene concentration from 2% to 8% was evaluated. It was found that the three organisms degraded about 65-85% from 8% kerosene after 21d. The use of rice straw-immobilized cells reduced the time of degradation and enhanced the degradation ability of the organisms. The sodium dodecyl sulphate-polyacrylamide gel electrophoresis revealed the presence of a common protein band when the tested organisms were grown on kerosene.

Novel Applications for Oxalate-Phosphate-Amine Metal-Organic-Frameworks (OPA-MOFs): Can an Iron-Based OPA-MOF Be Used as Slow-Release Fertilizer?

PubMed

Anstoetz, Manuela; Rose, Terry J; Clark, Malcolm W; Yee, Lachlan H; Raymond, Carolyn A; Vancov, Tony

2015-01-01

A porous iron-based oxalate-phosphate-amine metal-organic framework material (OPA-MOF) was investigated as a microbially-induced slow-release nitrogen (N) and phosphorus (P) fertilizer. Seedling growth, grain yields, nutrient uptake of wheat plants, and soil dynamics in incubated soil, were investigated using OPA-MOF vs standard P (triple-superphosphate) and N (urea) fertilizers in an acidic Ferralsol at two application rates (equivalent 120 and 40 kg N ha(-1)). While urea hydrolysis in the OPA-MOF treatment was rapid, conversion of ammonium to nitrate was significantly inhibited compared to urea treatment. Reduced wheat growth in OPA-MOF treatments was not caused by N-deficiency, but by limited P-bioavailability. Two likely reasons were slow P-mobilisation from the OPA-MOF or rapid P-binding in the acid soil. P-uptake and yield in OPA-MOF treatments were significantly higher than in nil-P controls, but significantly lower than in conventionally-fertilised plants. OPA-MOF showed potential as enhanced efficiency N fertilizer. However, as P-bioavailability was insufficient to meet plant demands, further work should determine if P-availability may be enhanced in alkaline soils, or whether central ions other than Fe, forming the inorganic metal-P framework in the MOF, may act as a more effective P-source in acid soils.

Phycocyanin extraction in Spirulina produced using agricultural waste

NASA Astrophysics Data System (ADS)

Taufiqurrahmi, N.; Religia, P.; Mulyani, G.; Suryana, D.; Ichsan; Tanjung, F. A.; Arifin, Y.

2017-06-01

Phycocyanin is a pigment-protein complex synthesized by blue-green microalgae such as Arthrospira (Spirulina) platensis. This pigment is used mainly as natural colouring in food industry. Previous studies have demonstrated the potential health benefits of this natural pigment. The price of phycocyanin is a vital factor that dictates its marketability. The cost of culturing the algae, particularly from the substrate used for growth, is one of the main factors that determine the price of phycocyanin. Another important factor is the growth yield of the algae. In our research, agricultural waste such as charcoal produced from rice husk was utilized for the algae cultivation to replace the synthetic chemicals such as urea and triple superphosphate used the mineral medium. The use of this low cost substrate increases the cell concentration by 60 % during 8 days’ cultivation to reach 0.39 g/l. The phycocyanin extraction was performed using water at the different biomass-to-solvent ratio and shaking rates. The phycocyanin concentration and purity (A615/A280) obtained were 1.2 g/l and 0.3. These values are 40 % and 20 % lower than the value obtained from the algae produced using the synthetic chemicals. Further purification produced the extract purity required for food grade. The biomass-solvent ratio does not significantly affect the extract purity; however, the higher shaking rate during extraction reduces the purity. This finding demonstrates the potential of using rice husk as an alternative substrate to cultivate algae for phycocyanin extraction.

Phosphate Treatment of Lead-Contaminated Soil: Effects on ...

EPA Pesticide Factsheets

Water quality threats associated with using phosphate-based amendments to remediate Pb-contaminated soils are a concern, particularly in riparian areas. This study investigated the effects of P application rates to a Pb-contaminated alluvial soil on Pb and P loss via surface water runoff, Pb accumulation in tall fescue (Festuca arundinacea Schreb; Kentucky 31), and Pb speciation. An alluvial soil was treated with triple superphosphate at P to Pb molar ratios of 0:1(control), 4:1, 8:1, and 16:1. After a 6- mo reaction period, rainfall simulation (RFS) studies were conducted, followed by tall fescue establishment and a second set of RFS studies (1 yr after treatment). Results from the first RFS (unvegetated) demonstrated that the total Pb and P concentrations in the effluents of 8:1 and 16:1 (P:Pb molar ratio) treatment levels were significantly greater (p 55%. X-ray absorption near-edge structure spectroscopy data showed that pyromorphite [Pb5(PO4)3OH,Cl,F] abundance ranged from 0% (control) to 32% (16:1 P:Pb; 1 yr after treatment) of the total soil Pb. Although P treatment stimulated pyromorphite formation, pyromorphite abundance was comparable between the P-treated soils. These findings suggest that a 4:1 (P:Pb molar ratio) P treatment may be a sufficient means of reducing Pb bioavailability while minimizing concerns related to P loss in an alluvial setting. The purpose of the current research was to examine the feasability of using phosphate based ammend

[Effects of nitrogen preserving agent on composting process and nitrogen loss of Eichhornia crassipes].

PubMed

Li, Sen; Luo, Xue Mei; Tu, Wei Guo; Fan, Hua; Gou, Xiao Lin; DU, Yu Long; Li, Ling; Wang, Qiong Yao

2017-04-18

To study the effects of nitrogen preserving agent (NPA) on composting process and nitrogen loss of Eichhornia crassipes, an aerobic composting was conducted for 35 days using four treatments. The NPA was prepared by mixing ferrous sulfate, humic acid sodium, and superphosphate (M:M:M=75:20:5). Four treatments were included with different mass ratios of NPA, including 0% (CK), 1% (PN1), 2% (PN2), and 3% (PN3). The physical and chemical properties, N fraction concentrations, ammonia volatilization, and N loss rates were measured and explored during composting process. The results showed that the pile temperature of NPA treatments were higher than that of CK in thermophillic period, however their water contents were significantly (P＜0.05) lower than that in CK in cooling period. At the end of composting, the concentrations of total nitrogen and organic nitrogen increased significantly in NPA treatments (P＜0.05), and their highest concentrations in the PN3 treatment were 16.3% and 13.2% higher than those in CK, respectively. The ammonia volatilization losses of PN1, PN2 and PN3 treatments were 25.9%, 31.5% and 42.4% lower than that of CK, respectively, however, their nitrogen fixation rates reached 31.3%, 40.7% and 72.2% respectively. Therefore, adding NPA could accelerate start-up speed, shorten composting time, and also could effectively reduce ammonia volatilizations and nitrogen loss in the composting process of E. crassipes. Therefore, PN3 showed the best effects of nitrogen preserving.

L-asparaginase and L-glutaminase activities in submerged rice soil amended with municipal solid waste compost and decomposed cow manure.

PubMed

Bhattacharyya, P; Chakrabarti, K; Tripathy, S; Chakraborty, A; Kim, K; Kim, S H

2007-01-01

The field study was conducted to evaluate the effect of municipal solid waste compost (MSWC) as a soil amendment on L-asparaginase (LA) and L-glutaminase (LG) activities. Experiments were conducted during the wet seasons of 1997, 1998 and 1999 on rice grown under a submerged condition, at the Agriculture Experimental Farm, Calcutta University at Baruipur, West Bengal, India. The treatments consisted of control, no input; MSWC, at 60 Kg N ha(- 1); well-decomposed cow manure (DCM), at 60 Kg N ha(- 1); MSWC (30 Kg N ha(- 1)) + Urea (U) (30 Kg N ha(- 1)); DCM (30 Kg N ha(- 1)) + U (30 Kg N ha(- 1)) and Fertilizer, (at 60:30:30 NPK kg ha(- 1)) through urea, single superphosphate and muriate of potash respectively). LA and LG activities alone and their ratio with organic-C (ratio index value, RIV), straw and grain yield were higher in DCM than MSWC-treated soils, due to higher amount of biogenic organic materials like water-soluble organic carbon, carbohydrate and mineralizable nitrogen in the former. The studied parameters were higher when urea was integrated with DCM or MSWC, compared to their single applications. The heavy metals in MSWC did not detrimentally influence the above-measured activities of soil. In the event of long term MSWC application, changes in soil quality parameters should be monitored regularly, since heavy metals once entering into soil persist over a long period.

Recycling slaughterhouse waste into fertilizer: how do pyrolysis temperature and biomass additions affect phosphorus availability and chemistry?

PubMed

Zwetsloot, Marie J; Lehmann, Johannes; Solomon, Dawit

2015-01-01

Pyrolysis of slaughterhouse waste could promote more sustainable phosphorus (P) usage through the development of alternative P fertilizers. This study investigated how pyrolysis temperature (220, 350, 550 and 750 °C), rendering before pyrolysis, and wood or corn biomass additions affect P chemistry in bone char, plant availability, and its potential as P fertilizer. Linear combination fitting of synchrotron-based X-ray absorption near edge structure spectra demonstrated that higher pyrolysis temperatures decreased the fit with organic P references, but increased the fit with a hydroxyapatite (HA) reference, used as an indicator of high calcium phosphate (CaP) crystallinity. The fit to the HA reference increased from 0% to 69% in bone with meat residue and from 20% to 95% in rendered bone. Biomass additions to the bone with meat residue reduced the fit to the HA reference by 83% for wood and 95% for corn, and additions to rendered bone by 37% for wood. No detectable aromatic P forms were generated by pyrolysis. High CaP crystallinity was correlated with low water-extractable P, but high formic acid-extractable P indicative of high plant availability. Bone char supplied available P which was only 24% lower than Triple Superphosphate fertilizer and two- to five-fold higher than rock phosphate. Pyrolysis temperature and biomass additions can be used to design P fertilizer characteristics of bone char through changing CaP crystallinity that optimize P availability to plants. © 2014 Society of Chemical Industry.

Phosphorus Amendment Efficacy for In Situ Remediation of ...

EPA Pesticide Factsheets

A validated method is needed to measure reductions of in vitro bioaccessible (IVBA) Pb in urban soil remediated with amendments. This study evaluated the effect of in vitro extraction solution pH and glycine buffer on bioaccesible Pb in P-treated soils. Two Pb-contaminated soils (790-1300 mg Pb kg-1), one from a garden and one from a city lot in Cleveland, OH, were incubated in a bench scale experiment for 1 yr. Six phosphate amendments, including bone meal, fish bone, poultry litter, monoammonium phosphate, diammonium phosphate, and triple superphosphate, were added to containers at two application rates. Lead IVBA was assessed using USEPA Method 1340 and three modified versions of this method. Modifications included using solutions with pH 1.5 and 2.5 as well as using solutions with and without 0.4 mol L-1 glycine. Soil amendments were effective in reducing IVBA Pb in these soils as measured by pH 1.5 with glycine buffer. The greatest reductions in IVBA Pb, from 5 to 26%, were found using pH 2.5 extractions. Lead mineral results showed several soil amendments promoted Pb phosphate formation, an indicator of remediation success. A significant negative linear relationship between reduction in IVBA Pb and Pb-phosphate formation was found only for pH 2.5 without glycine extraction solution. A modified USEPA Method 1340 without glycine and using pH 2.5 has the potential to predict P soil treatment efficacy and reductions in bioavailable Pb. Developing mana

Solid Cattle Manure Less Prone to Phosphorus Loss in Tile Drainage Water.

PubMed

Wang, Y T; Zhang, T Q; Tan, C S; Qi, Z M; Welacky, T

2018-03-01

Forms (e.g., liquid and solid) of manure influence the risk of P loss after land application. The objective of this study was to investigate the effects of P-based application of various forms of cattle manure (liquid, LCM; or solid, SCM) or inorganic P as triple superphosphate (IP) on soil P losses in tile drainage water. A 4-yr field experiment was conducted in a clay loam soil with a corn ( L.)-soybean [ (L.) Merr.] rotation in the Lake Erie basin. Over the 4 yr, the dissolved reactive P (DRP) flow-weighted mean concentration (FWMC) in tile drainage water was greater under SCM fertilization than under either IP or LCM fertilization. Despite its lower value on an annual basis, DRP FWMC rose dramatically immediately after LCM application. However, the differences in DRP FWMC did not result in detectable differences in DRP loads. Regarding particulate P and total P losses during the 4 yr, they were 68 and 47%, respectively, lower in the soils amended with SCM than in those with IP, whereas both values were similar between IP and LCM treatments. Overall, the P contained in solid cattle manure was less prone to P loss after land application. Accordingly, the present results can provide a basis for manure storage and application of best management practices designed to reduce P losses and improve crop growth. Copyright © by the American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America, Inc.

Treatment of alumina refinery waste (red mud) through neutralization techniques: A review.

PubMed

Rai, Suchita; Wasewar, K L; Agnihotri, A

2017-06-01

In the Bayer process of extraction of alumina from bauxite, the insoluble product generated after bauxite digestion with sodium hydroxide at elevated temperature and pressure is known as 'red mud' or 'bauxite residue'. This alumina refinery waste is highly alkaline in nature with a pH of 10.5-12.5 and is conventionally disposed of in mostly clay-lined land-based impoundments. The alkaline constituents in the red mud impose severe and alarming environmental problems, such as soil and air pollution. Keeping in view sustainable re-vegetation and residue management, neutralization/treatment of red mud using different techniques is the only alternative to make the bauxite residue environmentally benign. Hence, neutralization techniques, such as using mineral acids, acidic waste (pickling liquor waste), coal dust, superphosphate and gypsum as amenders, CO 2 , sintering with silicate material and seawater for treatment of red mud have been studied in detail. This paper is based upon and emphasizes the experimental work carried out for all the neutralization techniques along with a comprehensive review of each of the processes. The scope, applicability, limitations and feasibility of these processes have been compared exhaustively. Merits and demerits have been discussed using flow diagrams. All the techniques described are technically feasible, wherein findings obtained with seawater neutralization can be set as a benchmark for future work. Further studies should be focused on exploring the economical viability of these processes for better waste management and disposal of red mud.

Natural radioactivity levels and heavy metals in chemical and organic fertilizers used in Kingdom of Saudi Arabia.

PubMed

El-Taher, A; Althoyaib, S S

2012-01-01

The present work deals with identifying and determining the activity levels of natural occuring radionuclides, (226)Ra and (232)Th series, their decay products and (40)K, in chemical and organic fertilizers used in Kingdom of Saudi Arabia. A total of 30 samples: 20 phosphatic fertilizers (single super-phosphate SSP and triple super-phosphate,TSP) and 10 organic fertilizers (cow, sheep and chicken) collected from markets and farms. The gamma-ray spectrometer consists of NaI(Tl) detector and its electronic circuit was used for measuring γ-ray spectra. The ranges of radioactivity levels of (226)Ra, (232)Th and (40)K in chemical fertilizers are 51.5±5.2-106.3±7.5, 5.1±1.6-9.9±3.2. and 462.6±21-607.3±14Bqkg(-1), respectively. The activities of (226)Ra, (232)Th and (40)K in natural fertilizers (cow, sheep and chicken) are lower than the activities in chemical fertilizers. The obtained data are compared with available reported data from other countries in literature. The Ra(eq) in chemical fertilizer ranges from 100.37 to 161.43Bqkg(-1) and in organic fertilizer ranges from 34.07 to 102.19Bqkg(-1), which are lower than the limit of 370Bqkg(-1) adopted from NEA-OECD (1979). The average heavy metal (Pb, Cd, Ni, Co and Cr) contents of the fertilizers marketed in the Kingdom of Saudi Arabia are also determined and within the limits of those used worldwide. Copyright © 2011 Elsevier Ltd. All rights reserved.

Phosphorus runoff from incorporated and surface-applied liquid swine manure and phosphorus fertilizer.

PubMed

Daverede, I C; Kravchenko, A N; Hoeft, R G; Nafziger, E D; Bullock, D G; Warren, J J; Gonzini, L C

2004-01-01

Excessive fertilization with organic and/or inorganic P amendments to cropland increases the potential risk of P loss to surface waters. The objective of this study was to evaluate the effects of soil test P level, source, and application method of P amendments on P in runoff following soybean [Glycine max (L.) Merr.]. The treatments consisted of two rates of swine (Sus scrofa domestica) liquid manure surface-applied and injected, 54 kg P ha(-1) triple superphosphate (TSP) surface-applied and incorporated, and a control with and without chisel-plowing. Rainfall simulations were conducted one month (1MO) and six months (6MO) after P amendment application for 2 yr. Soil injection of swine manure compared with surface application resulted in runoff P concentration decreases of 93, 82, and 94%, and P load decreases of 99, 94, and 99% for dissolved reactive phosphorus (DRP), total phosphorus (TP), and algal-available phosphorus (AAP), respectively. Incorporation of TSP also reduced P concentration in runoff significantly. Runoff P concentration and load from incorporated amendments did not differ from the control. Factors most strongly related to P in runoff from the incorporated treatments included Bray P1 soil extraction value for DRP concentration, and Bray P1 and sediment content in runoff for AAP and TP concentration and load. Injecting manure and chisel-plowing inorganic fertilizer reduced runoff P losses, decreased runoff volumes, and increased the time to runoff, thus minimizing the potential risk of surface water contamination. After incorporating the P amendments, controlling erosion is the main target to minimize TP losses from agricultural soils.

Liming can decrease legume crop yield and leaf gas exchange by enhancing root to shoot ABA signalling

PubMed Central

Rothwell, Shane A.; Elphinstone, E. David; Dodd, Ian C.

2015-01-01

To meet future requirements for food production, sustainable intensive agricultural systems need to optimize nutrient availability to maximize yield, traditionally achieved by maintaining soil pH within an optimal range (6–6.5) by applying lime (calcium carbonate). However, a field trial that applied recommended liming rates to a sandy loam soil (increasing soil pH from 5.5 to 6.2) decreased pod yield of field bean (Vicia faba L. cv. Fuego) by ~30%. Subsequent pot trials, with liming that raised soil pH to 6.3–6.7, reduced stomatal conductance (g s) by 63, 26, and 59% in V. faba, bean (Phaseolus vulgaris), and pea (Pisum sativum), respectively. Furthermore, liming reduced shoot dry biomass by 16–24% in these species. Ionomic analysis of root xylem sap and leaf tissue revealed a decrease in phosphorus concentration that was correlated with decreased g s: both reductions were partially reversed by adding superphosphate fertilizer. Further analysis of pea suggests that leaf gas exchange was reduced by a systemic increase (roots, xylem sap, and leaves) in the phytohormone abscisic acid (ABA) in response to lime-induced suboptimal plant phosphorus concentrations. Supplying synthetic ABA via the transpiration stream to detached pea leaves, at the same xylem sap concentrations induced by liming, decreased transpiration. Furthermore, the g s of the ABA-deficient mutant pea wilty was unresponsive to liming, apparently confirming that ABA mediates some responses to low phosphorus availability caused by liming. This research provides a detailed mechanistic understanding of the physiological processes by which lime application can limit crop yields, and questions the suitability of current liming recommendations. PMID:25740925

Phosphorus-Assisted Biomass Thermal Conversion: Reducing Carbon Loss and Improving Biochar Stability

PubMed Central

Zhao, Ling; Cao, Xinde; Zheng, Wei; Kan, Yue

2014-01-01

There is often over 50% carbon loss during the thermal conversion of biomass into biochar, leading to it controversy for the biochar formation as a carbon sequestration strategy. Sometimes the biochar also seems not to be stable enough due to physical, chemical, and biological reactions in soils. In this study, three phosphorus-bearing materials, H3PO4, phosphate rock tailing (PRT), and triple superphosphate (TSP), were used as additives to wheat straw with a ratio of 1: 0.4–0.8 for biochar production at 500°C, aiming to alleviate carbon loss during pyrolysis and to increase biochar-C stabilization. All these additives remarkably increased the biochar yield from 31.7% (unmodified biochar) to 46.9%–56.9% (modified biochars). Carbon loss during pyrolysis was reduced from 51.7% to 35.5%–47.7%. Thermogravimetric analysis curves showed that the additives had no effect on thermal stability of biochar but did enhance its oxidative stability. Microbial mineralization was obviously reduced in the modified biochar, especially in the TSP-BC, in which the total CO2 emission during 60-d incubation was reduced by 67.8%, compared to the unmodified biochar. Enhancement of carbon retention and biochar stability was probably due to the formation of meta-phosphate or C-O-PO3, which could either form a physical layer to hinder the contact of C with O2 and bacteria, or occupy the active sites of the C band. Our results indicate that pre-treating biomass with phosphors-bearing materials is effective for reducing carbon loss during pyrolysis and for increasing biochar stabilization, which provides a novel method by which biochar can be designed to improve the carbon sequestration capacity. PMID:25531111

Reclamation of acidic, denuded copper basin land: Revegetation performance of phosphate rock vs other nutrient sources

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

Soileau, J.M.; Sikora, F.J.; Maddox, J.J.

1996-12-31

Open pit smelting of Copper ore about 100 years ago resulted in approximately 9,300 ha of severely eroded, very acidic (pH 4.0 to 5.0) soils at Copper Basin, Tennessee. Along with other essential nutrients, phosphorus (P) amendments are critical for long-term productivity and sustainability of vegetation on this depleted soil. A field study was conducted (1992-1995) to compare revegetation from surface-applied North Carolina phosphate rock (PR) and triple superphosphate (TSP) at 20, 59, and 295 kg P ha{sup -1}, and to determine benefits of starter NPK tree tablets. The experimental design consisted of 7.3 x 9.1 m replicated plots, eachmore » planted to 20 loblolly pine seedlings and aerially seeded with a mixture of grasses and legumes. Tree survivability was high from all treatments. Through the third year, tree height and diameter increased with increasing P to 59 kg P ha without fertilizer tablets. There were no pine growth differences between PR and TSP. Weeping lovegrass has been the dominant cover crop through 1995, with increased stimulation to tree tablets and surface P. Tall fescue (KY 31), sericea lespedeza, and black locust responded more to PR than to TSP. Surface soil pH increased, and 0.01 M SrCl{sub 2} extractable Al decreased, with increasing rate of PR. For future loblolly pine plantings in the Copper Basin, this study suggests there is no benefit to applying both tree tablets and surface P at rates above 59 kg P ha{sup -1}. For reclaiming land with high acidity and low P fertility, PR has significant benefits. In reclaiming steep, gullied land, there is great potential for aerial application of PR and/or pelletized liming agents.« less

Cadmium accumulations and bioavailability in soils from long-term phosphorus fertilization

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

Mulla, D.J.; Page, A.L.; Ganje, T.J.

1980-07-01

Soils from citrus groves that had been fertilized with the equivalent of approximately 175 kg P/ha per year (as treble superphosphate (TSP)) over a 36-year period were sampled and analyzed for total P, Cd, and Zn as well as water-soluble P and Cd. A P fertilization rate of 175 kg/ha is much higher than normal field rates, which are typically about 30 kg/ha. Concentrations of total Cd in surface soil were highly correlated (r = 0.89) with concentrations of total P. The concentrations of Cd in surface soil receiving broadcast P for 36 years averaged 1.0 ..mu..g/g, and were considerablymore » greater than those of the controls, which showed a mean concentration of 0.07 ..mu..g/g. Phosphorus in soil saturation paste extracts ranged from 0.10 ..mu..g/ml (controls) to 8.87 ..mu..g/ml in P fertilized soils. Water-soluble saturation extract Cd ranged from 0.008 ..mu..g/ml in controls to 0.017 ..mu..g/ml in fertilized soils, and was not well correlated with water-soluble P. Cadmium levels in barley (Hordeum vulgare var. U.C. 566) grain and leaves grown in the field on soil subject to long-term heavy P fertilization were not elevated above levels in barley grown on the control soil. Swiss chard (Beta vulgaris var. cicla) was grown in the greenhouse on the above surface soils collected from the field. Although Cd levels averaging 1.6 ..mu..g/g in plant tissue were significantly elevated over those on the control soil (0.26 ..mu..g/gm), no yield depression was observed.« less

Phosphorus Amendment Efficacy for In Situ Remediation of Soil Lead Depends on the Bioaccessible Method.

PubMed

Obrycki, John F; Basta, Nicholas T; Scheckel, Kirk; Stevens, Brooke N; Minca, Kristen K

2016-01-01

A validated method is needed to measure reductions of in vitro bioaccessible (IVBA) Pb in urban soil remediated with amendments. This study evaluated the effect of in vitro extraction solution pH and glycine buffer on bioaccessible Pb in P-treated soils. Two Pb-contaminated soils (790-1300 mg Pb kg), one from a garden and one from a city lot in Cleveland, OH, were incubated in a bench scale experiment for 1 yr. Six phosphate amendments, including bone meal, fish bone, poultry litter, monoammonium phosphate, diammonium phosphate, and triple superphosphate, were added to containers at two application rates. Lead IVBA was assessed using USEPA Method 1340 and three modified versions of this method. Modifications included using solutions with pH 1.5 and 2.5 as well as using solutions with and without 0.4 mol L glycine. Soil amendments were ineffective in reducing IVBA Pb in these soils as measured by pH 1.5 with glycine buffer. The greatest reductions in IVBA Pb, from 5 to 26%, were found using pH 2.5 extractions. Lead mineral results showed several soil amendments promoted Pb phosphate formation, an indicator of remediation success. A significant negative linear relationship between reduction in IVBA Pb and Pb-phosphate formation was found only for pH 2.5 without glycine extraction solution. A modified USEPA Method 1340 without glycine and using pH 2.5 has the potential to predict P soil treatment efficacy and reductions in bioavailable Pb. Copyright © by the American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America, Inc.

Environmental evaluation of the life cycle of elephant grass fertilization-Cenchrus purpureus (Schumach.) Morrone-using chemical fertilization and biosolids.

PubMed

Neves, Talles Iwasawa; Uyeda, Claudio Augusto; Carvalho, Monica; Abrahão, Raphael

2017-12-19

Law 12305/10, National Solid Waste Policy of Brazil, banned the disposal in landfills of any solid waste that could be converted to another use. Sludge produced at Industrial Wastewater Treatment Plants, which contains components characteristic of fertilizers, falls into this category. This type of sludge, also known as a biosolid, has great potential to replace commercial chemical fertilization. The use of biosolids in agriculture allows for compliance with new legislation, reducing the burden on landfills and reusing a waste product. The present paper utilizes the life cycle assessment methodology to compare the carbon footprint associated with the use of different quantities of biosolid and selected chemical fertilizers in the production of elephant grass. The IPCC 2013 GWP 100a method, which is based on data published by the Intergovernmental Panel on Climate Change, was selected as the environmental assessment method. The method expresses the emissions of greenhouse gases generated, in kilograms of CO 2 equivalent, over a time horizon of 100 years. The biosolid quantities used were based on the Brazilian Environment Council Resolution 375. The chemical fertilizer used contained urea, simple superphosphate, and potassium chloride. The use of biosolids in the amounts calculated according to Brazilian standards resulted in a carbon footprint approximately 17.7% lower than the use of the chemical fertilization mix, with similar productivity in both cases. The transportation of biosolids to the experimental area was responsible for the majority of emissions associated with the use of biosolids. Urea synthesis was the largest contributor to emissions resulting from the use of commercial chemical fertilizer, accounting for 73.6% of total emissions.

Mercury in rice (Oryza sativa L.) and rice-paddy soils under long-term fertilizer and organic amendment.

PubMed

Tang, Zhenya; Fan, Fangling; Wang, Xinyue; Shi, Xiaojun; Deng, Shiping; Wang, Dingyong

2018-04-15

High levels of mercury (Hg), especially methylmercury (MeHg), in rice is of concern due to its potential of entering food chain and the high toxicity to human. The level and form of Hg in rice could be influenced by fertilizers and other soil amendments. Studies were conducted to evaluate the effect of 24 years application of chemical fertilizers and organic amendments on total Hg (THg) and MeHg and their translocation in soil, plants, and rice grain. All treatments led to significantly higher concentrations of MeHg in grain than those from the untreated control. Of nine treatments tested, chemical fertilizers combining with returning rice straw (NPK1+S) led to highest MeHg concentration in grain and soil; while the nitrogen and potassium (NK) treatment led to significantly higher THg in grain. Concentrations of soil MeHg were significantly correlated with THg in soil (r = 0.59 *** ) and MeHg in grain (r = 0.48 *** ). Calcium superphosphate negatively affected plant bioavailability of soil Hg. MeHg concentration in rice was heavily influenced by soil Hg levels. Phosphorus fertilizer was a main source contributing to soil THg, while returning rice straw to the field contributed significantly to MeHg in soil and rice grain. As a result, caution should be exercised in soil treatment or when utilizing Hg-contaminated soils to produce rice for human consumption. Strategic management of rice straw and phosphorus fertilizer could be effective strategies of lowering soil Hg, which would ultimately lower MeHg in rice and the risk of Hg entering food chain. Copyright © 2017 Elsevier Inc. All rights reserved.

Long-Term Rock Phosphate Fertilization Impacts the Microbial Communities of Maize Rhizosphere

PubMed Central

Silva, Ubiana C.; Medeiros, Julliane D.; Leite, Laura R.; Morais, Daniel K.; Cuadros-Orellana, Sara; Oliveira, Christiane A.; de Paula Lana, Ubiraci G.; Gomes, Eliane A.; Dos Santos, Vera L.

2017-01-01

Phosphate fertilization is a common practice in agriculture worldwide, and several commercial products are widely used. Triple superphosphate (TSP) is an excellent soluble phosphorus (P) source. However, its high cost of production makes the long-term use of crude rock phosphate (RP) a more attractive alternative in developing countries, albeit its influence on plant-associated microbiota remains unclear. Here, we compared long-term effects of TSP and RP fertilization on the structure of maize rhizosphere microbial community using next generation sequencing. Proteobacteria were dominant in all conditions, whereas Oxalobacteraceae (mainly Massilia and Herbaspirillum) was enriched in the RP-amended soil. Klebsiella was the second most abundant taxon in the RP-treated soil. Burkholderia sp. and Bacillus sp. were enriched in the RP-amended soil when compared to the TSP-treated soil. Regarding fungi, Glomeromycota showed highest abundance in RP-amended soils, and the main genera were Scutellospora and Racocetra. These taxa are already described as important for P solubilization/acquisition in RP-fertilized soil. Maize grown on TSP and RP-treated soil presented similar productivity, and a positive correlation was detected for P content and the microbial community of the soils. The results suggest changes of the microbial community composition associated to the type of phosphate fertilization. Whilst it is not possible to establish causality relations, our data highlights a few candidate taxa that could be involved in RP solubilization and plant growth promotion. Moreover, this can represent a shorter path for further studies aiming the isolation and validation of the taxa described here concerning P release on the soil plant system and their use as bioinoculants. PMID:28744264

Optimization of Aspergillus niger rock phosphate solubilization in solid-state fermentation and use of the resulting product as a P fertilizer

PubMed Central

Mendes, Gilberto de Oliveira; da Silva, Nina Morena Rêgo Muniz; Anastácio, Thalita Cardoso; Vassilev, Nikolay Bojkov; Ribeiro, José Ivo; da Silva, Ivo Ribeiro; Costa, Maurício Dutra

2015-01-01

A biotechnological strategy for the production of an alternative P fertilizer is described in this work. The fertilizer was produced through rock phosphate (RP) solubilization by Aspergillus niger in a solid-state fermentation (SSF) with sugarcane bagasse as substrate. SSF conditions were optimized by the surface response methodology after an initial screening of factors with significant effect on RP solubilization. The optimized levels of the factors were 865 mg of biochar, 250 mg of RP, 270 mg of sucrose and 6.2 ml of water per gram of bagasse. At this optimal setting, 8.6 mg of water-soluble P per gram of bagasse was achieved, representing an increase of 2.4 times over the non-optimized condition. The optimized SSF product was partially incinerated at 350°C (SB-350) and 500°C (SB-500) to reduce its volume and, consequently, increase P concentration. The post-processed formulations of the SSF product were evaluated in a soil–plant experiment. The formulations SB-350 and SB-500 increased the growth and P uptake of common bean plants (Phaseolus vulgaris L.) when compared with the non-treated RP. Furthermore, these two formulations had a yield relative to triple superphosphate of 60% (on a dry mass basis). Besides increasing P concentration, incineration improved the SSF product performance probably by decreasing microbial immobilization of nutrients during the decomposition of the remaining SSF substrate. The process proposed is a promising alternative for the management of P fertilization since it enables the utilization of low-solubility RPs and relies on the use of inexpensive materials. PMID:26112323

Maize Yield Response to Water Supply and Fertilizer Input in a Semi-Arid Environment of Northeast China

PubMed Central

Yin, Guanghua; Gu, Jian; Zhang, Fasheng; Hao, Liang; Cong, Peifei; Liu, Zuoxin

2014-01-01

Maize grain yield varies highly with water availability as well as with fertilization and relevant agricultural management practices. With a 311-A optimized saturation design, field experiments were conducted between 2006 and 2009 to examine the yield response of spring maize (Zhengdan 958, Zea mays L) to irrigation (I), nitrogen fertilization (total nitrogen, urea-46% nitrogen,) and phosphorus fertilization (P2O5, calcium superphosphate-13% P2O5) in a semi-arid area environment of Northeast China. According to our estimated yield function, the results showed that N is the dominant factor in determining maize grain yield followed by I, while P plays a relatively minor role. The strength of interaction effects among I, N and P on maize grain yield follows the sequence N+I >P+I>N+P. Individually, the interaction effects of N+I and N+P on maize grain yield are positive, whereas that of P+I is negative. To achieve maximum grain yield (10506.0 kg·ha−1) for spring maize in the study area, the optimum application rates of I, N and P are 930.4 m3·ha−1, 304.9 kg·ha−1 and 133.2 kg·ha−1 respectively that leads to a possible economic profit (EP) of 10548.4 CNY·ha−1 (CNY, Chinese Yuan). Alternately, to obtain the best EP (10827.3 CNY·ha−1), the optimum application rates of I, N and P are 682.4 m3·ha−1, 241.0 kg·ha−1 and 111.7 kg·ha−1 respectively that produces a potential grain yield of 10289.5 kg·ha−1. PMID:24465896

Optimization of Aspergillus niger rock phosphate solubilization in solid-state fermentation and use of the resulting product as a P fertilizer.

PubMed

Mendes, Gilberto de Oliveira; da Silva, Nina Morena Rêgo Muniz; Anastácio, Thalita Cardoso; Vassilev, Nikolay Bojkov; Ribeiro, José Ivo; da Silva, Ivo Ribeiro; Costa, Maurício Dutra

2015-11-01

A biotechnological strategy for the production of an alternative P fertilizer is described in this work. The fertilizer was produced through rock phosphate (RP) solubilization by Aspergillus niger in a solid-state fermentation (SSF) with sugarcane bagasse as substrate. SSF conditions were optimized by the surface response methodology after an initial screening of factors with significant effect on RP solubilization. The optimized levels of the factors were 865 mg of biochar, 250 mg of RP, 270 mg of sucrose and 6.2 ml of water per gram of bagasse. At this optimal setting, 8.6 mg of water-soluble P per gram of bagasse was achieved, representing an increase of 2.4 times over the non-optimized condition. The optimized SSF product was partially incinerated at 350°C (SB-350) and 500°C (SB-500) to reduce its volume and, consequently, increase P concentration. The post-processed formulations of the SSF product were evaluated in a soil-plant experiment. The formulations SB-350 and SB-500 increased the growth and P uptake of common bean plants (Phaseolus vulgaris L.) when compared with the non-treated RP. Furthermore, these two formulations had a yield relative to triple superphosphate of 60% (on a dry mass basis). Besides increasing P concentration, incineration improved the SSF product performance probably by decreasing microbial immobilization of nutrients during the decomposition of the remaining SSF substrate. The process proposed is a promising alternative for the management of P fertilization since it enables the utilization of low-solubility RPs and relies on the use of inexpensive materials. © 2015 The Authors. Microbial Biotechnology published by John Wiley & Sons Ltd and Society for Applied Microbiology.

A lysimeter study of nitrate leaching, optimum fertilisation rate and growth responses of corn (Zea mays L.) following soil amendment with water-saving super-absorbent polymer.

PubMed

Islam, M Robiul; Mao, Sishuai; Xue, Xuzhang; Eneji, A Egrinya; Zhao, Xingbao; Hu, Yuegao

2011-08-30

Nitrate leaching and the resulting groundwater contamination from intensive cereal production has become a major concern for long-term farmland efficiency and environmental sustainability in northern China. The aim of this study was to evaluate a water-saving super-absorbent polymer (SAP) for minimising NO(3)(-) leaching from soil and optimising corn growth and yield. Thirty-six undisturbed soil lysimeters were installed in a field lysimeter facility in drought-affected northern China to study the growth and yield characteristics of summer corn (Zea mays L.) as well as the amount of NO(3)-leaching losses under different fertiliser (standard, medium or 75% and low, or 50% of conventional fertilisation rate) and SAP (control, 0; level-1, 15 kg ha(-1) and level-2, 30 kg ha(-1)) treatments. Corn yield fell by 19.7% under medium and 37.7% under low fertilisation; the application of SAP increased yield significantly by 44.4% on level-1 and 80.3% on level-2. Similarly, plant height, leaf area, number of grains as well as protein, soluble sugar and starch contents in the grain also increased with SAP treatment. Application of SAP at 30 kg ha(-1) plus half of conventional fertilisation can reduce maximum (64.1%) nitrate leaching losses from soil. Application of SAP at 30 kg ha(-1) plus only half the amount of conventional fertiliser rate (150 kg urea, and 50 kg each of superphosphate and potassium sulfate) would be a more appropriate practice both for minimising nitrate leaching and sustainable corn production under the arid and semiarid conditions of northern China. Copyright © 2011 Society of Chemical Industry.

Improving phosphorus uptake and wheat productivity by phosphoric acid application in alkaline calcareous soils.

PubMed

Akhtar, Muhammad; Yaqub, Muhammad; Naeem, Asif; Ashraf, Muhammad; Hernandez, Vicente Espinosa

2016-08-01

Low phosphorus (P) efficiency from existing granular fertilisers necessitates searching for efficient alternatives to improve wheat productivity in calcareous soil. Multi-location trials have shown that phosphoric acid (PA) produced 16% higher wheat grain over commercial P fertilisers, i.e. diammonium phosphate (DAP) and triple superphosphate (TSP). Methods of P application significantly influenced grain yield and the efficiency of methods was observed in the order: PA placement below seed > PA, DAP or TSP fertigation > DAP or TSP broadcast. The sub-surface application of PA produced highest grain yields (mean of all rates), i.e. 4669, 4158 and 3910 kg ha(-1) in Bagh, Bhalwal and Shahpur soil series, respectively. Phosphoric acid at 66 kg P2 O5 ha(-1) was found more effective in increasing gain yield over that of control. Trend in grain P uptake was found similar to that observed for grain yield. Maximum P uptake by grain was recorded at the highest P rate and the lowest at zero P. The significant increase in P uptake with P rates was generally related to the increase in yield rather than its concentration in grain. Phosphorus agronomic efficiency (PAE) and phosphorus recovery efficiency (PRE) were found higher at lower P rate (44 kg P2 O5 ha(-1) ) and decreased with P application. However, PA applied by the either method resulted in higher PAE and PRE compared to DAP and TSP. Phosphoric acid is suggested as an efficient alternative to commercial granular P fertilisers for wheat production in alkaline calcareous soils. © 2015 Society of Chemical Industry. © 2015 Society of Chemical Industry.

Effects of phosphorus fertilizer and lime on the As, Cr, Pb, and V content of soils and plants

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

Goodroad, L.L.; Caldwell, A.C.

1979-10-01

The occurrence in fertilizer material of small quantities of chemical elements not essential to plants suggests that the soil may become contaminated with these elements due to the use of fertilizers. Two experimental sites: a Nicollet clay loam fertilized with 0, 1111, 2222, 4444, and 8888 kg/ha of concentrated superphosphate (CSP) and 20.2 metric tons of lime, and a Port Byron silt loam fertilized for 19 years with 99, 73, 82, and 352 kg/ha annually of CSP, calcium metaphosphate, phosphoric acid, and southern rock phosphate, respectively, were sampled to determine if significant amounts of arsenic (As), chromium (Cr), lead (Pb),more » or vanadium (V) had been added from the use of these fertilizer materials. There was no indication of increased As, Cr, Pb, or V from the addition of P fertilizers to either the Nicollet or Port Byron soils. The addition of lime increased the Cr content of the Nicollet soil by approximately 3 ppM, but there was no increase in As, Pb, or V. There was no increase in As, Cr, Pb, or V from addition of CSP in soil samples from below the Ap horizon to a depth of 47.5 cm. Soil samples from a representative Nicollet soil suggest that higher As, Cr, Pb, and V concentrations in the A and B horizons are due to leaching of CaCO/sub 3/ into the C horizon. Corn (Zea mays L.) plant growth and grain yields were similar for all CSP and lime treatments. The results of this study indicate that the use of P fertilizers at the rates presently applied would not add substantially to the natural levels of As, Cr, Pb, and V in the soil.« less

Subsurface application of poultry litter and its influence on nutrient losses in runoff water from permanent pastures.

PubMed

Watts, D B; Way, T R; Torbert, H A

2011-01-01

Environmental pressure to reduce nutrient losses from agricultural fields has increased in recent years. To abate this nutrient loss to the environment, better management practices and new technologies need to be developed. Thus, research was conducted to evaluate if subsurface banding poultry litter (PL) would reduce nitrogen (N) and phosphorus (P) loss in surface water runoff using a four-row prototype implement. Rainfall simulations were conducted to create a 40-min runoff event in an established bermudagrass (Cynodon dactylon L.) pasture on soil types common to the Coastal Plain and Piedmont regions. The Coastal Plain soil type was a Marvyn loamy sand (fine-loamy, kaolinitic, thermic Typic Kanhapludults) and the Piedmont soil type was a Hard Labor loamy sand (fine, kaolinitic, thermic Oxyaquic Kanhapludults). Treatments consisted of surface- and subsurface-applied PL at a rate of 9 Mg ha(-1), surface broadcast-applied commercial fertilizer (CF; urea and triple superphosphate blend) at the equivalent N (330 kg N ha(-1)) and P (315 kg N ha(-1)) content of PL, and a nonfertilized control. The greatest loss for inorganic N, total N, dissolved reactive P (DRP), and total P occurred with the surface broadcast treatments, with CF contributing to the greatest loss. Nutrient losses from the subsurface banded treatment reduced N and P in surface water runoff to levels of the control. Subsurface banding of PL reduced concentrations of inorganic N 91%, total N 90%, DRP 86%, and total P 86% in runoff water compared with surface broadcasted PL. These results show that subsurface band-applied PL can greatly reduce the impact of N and P loss to the environment compared with conventional surface-applied PL and CF practices.

Effect of surface incorporation of broiler litter applied to no-till cotton on runoff quality.

PubMed

Adeli, A; Shankle, M W; Tewolde, H; Brooks, J P; Sistani, K R; McLaughlin, M R; Rowe, D E

2011-01-01

Surface application of broiler litter to no-till cotton could lead to degradation of water quality. Incorporation of broiler litter into the top surface soil (0.05 m) could alleviate this risk. A 2-yr field study was conducted on a silt loam upland soil to determine the effect of incorporation of broiler litter into the soil surface on nutrient and bacterial transport in runoff. The experimental design was a randomized complete block with four treatments and three replications. Treatments were (i) unfertilized control; (ii) surface-appliedbroiler litter at 7.8 Mg ha(-1) without incorporation; (iii) surface-applied broiler litter at 7.8 Mg ha(-1) with immediate incorporation; and (iv) inorganic fertilizer N (urea ammonium nitrate, 32% N) and inorganic fertilizer P (triple superphosphate) at the recommended rate. Phosphorus was surface appliedat 25 kg ha(-1) and N was injected at 101 kg ha(-1) into the soil using a commercial liquid fertilizer applicator. Runoff was collected from small runoff plots (2.4 m by 1.6 m) established at the bottom side of main plots (13.7 m by 6.0 m). Incorporation of broiler litter reduced total N (TN), NO3-N, water soluble P (WSP), and total P (TP) concentrations in runoffby 35, 25, 61, and 64%, respectively, and litter-associated bacteria by two to three orders of magnitude compared with unincorporated treatment. No significant difference in total suspended solids (TSS) in runoffwas obtained between incorporated and unincorporated treatments. Incorporation of broiler litter into the surface soil in the no-till system immediately after application minimized the potential risk for surface nutrient losses and bacteria transport in runoff.

Rainfall intensity and phosphorus source effects on phosphorus transport in surface runoff from soil trays.

PubMed

Shigaki, Francirose; Sharpley, Andrew; Prochnow, Luis Ignacio

2007-02-01

Phosphorus runoff from agricultural fields amended with mineral fertilizers and manures has been linked to freshwater eutrophication. A rainfall simulation study was conducted to evaluate the effects of different rainfall intensities and P sources differing in water soluble P (WSP) concentration on P transport in runoff from soil trays packed with a Berks loam and grassed with annual ryegrass (Lolium multiflorum Lam.). Triple superphosphate (TSP; 79% WSP), low-grade super single phosphate (LGSSP; 50% WSP), North Carolina rock phosphate (NCRP; 0.5% WSP) and swine manure (SM; 70% WSP), were broadcast (100 kg total P ha-1) and rainfall applied at 25, 50 and 75 mm h-1 1, 7, 21, and 56 days after P source application. The concentration of dissolved reactive (DRP), particulate (PP), and total P (TP) was significantly (P<0.01) greater in runoff with a rainfall intensity of 75 than 25 mm h-1 for all P sources. Further, runoff DRP increased as P source WSP increased, with runoff from a 50 mm h-1 rain 1 day after source application having a DRP concentration of 0.25 mg L-1 for NCRP and 28.21 mg L-1 for TSP. In contrast, the proportion of runoff TP as PP was greater with low (39% PP for NCRP) than high WSP sources (4% PP for TSP) averaged for all rainfall intensities. The increased PP transport is attributed to the detachment and transport of undissolved P source particles during runoff. These results show that P source water solubility and rainfall intensity can influence P transport in runoff, which is important in evaluating the long-term risks of P source application on P transport in surface runoff.

Phosphorus saturation and superficial fertilizer application as key parameters to assess the risk of diffuse phosphorus losses from agricultural soils in Brazil.

PubMed

Fischer, P; Pöthig, R; Gücker, B; Venohr, M

2018-07-15

In Brazil, a steady increase in phosphorus (P) fertilizer application and agricultural intensification has been reported for recent decades. The concomitant P accumulation in soils potentially threatens surface water bodies with eutrophication through diffuse P losses. Here, we demonstrated the applicability of a soil type-independent approach for estimating the degree of P saturation (DPS; a risk parameter of P loss) by a standard method of water-soluble phosphorus (WSP) for two major soil types (Oxisols, Entisols) of the São Francisco catchment in Brazil. Subsequently, soil Mehlich-1P (M1P) levels recommended by Brazilian agricultural institutions were transformed into DPS values. Recommended M1P values for optimal agronomic production corresponded to DPS values below critical thresholds of high risks of P losses (DPS=80%) for major crops of the catchment. Higher risks of reaching critical DPS values due to P accumulation were found for Entisols due to their total sorption capacities being only half those of Oxisols. For complementary information on soil mineralogy and its influence on P sorption and P binding forms, Fourier transformation infrared (FTIR) spectroscopic analyses were executed. FTIR analyses suggested the occurrence of the clay minerals palygorskite and sepiolite in some of the analyzed Entisols and the formation of crandallite as the soil specific P binding form in the investigated Oxisols. Palygorskite and sepiolite can enhance P solubility and hence the risk of P losses. In contrast, the reshaping of superphosphate grains into crandallite may explain the chemical processes leading to previously observed low dissolved P concentrations in surface runoff from Oxisols. To prevent high risk of P losses, we recommend avoiding superficial fertilizer application and establishing environmental thresholds for soil M1P based on DPS. These measures could help to prevent eutrophication of naturally oligotrophic surface waters, and subsequent adverse effects on biodiversity and ecosystem function. Copyright © 2018 Elsevier B.V. All rights reserved.

Biochar as phosphorus transporter to support the closure of the phosphorus cycle

NASA Astrophysics Data System (ADS)

Soja, Gerhard; Jagerhofer, Reinhard; Fristak, Vladimir; Pfeifer, Christoph

2017-04-01

Waste materials rich in phosphorus could partly substitute rock phosphate-based mineral fertilizers. As rock phosphate is listed as critical raw material, measures for increasing the recovery rate of phosphorus and for closing the phosphorus cycle are required. However, direct use of the waste materials as fertilizers are frequently not possible because of legal constraints, adverse side effects because of co-occurring contaminants or hygienic concerns. So this study had the objective to test the appropriateness of carbonizing P-rich residues that can be used as secondary P resources for producing P fertilizers. The resulting biochar or hydrochar products should be tested for the bioavailability of P for plant uptake. Feedstock materials tested as secondary P resources were chicken manure, animal bone flour, sewage sludge, and digestates. These materials were either pyrolyzed at different temperatures, partly with different chemical modifications, or hydrothermally carbonized. The biochar and hydrochar products were analyzed for their total and available P concentrations, and the plant bioavailability was determined with a standardized plant growth test with rye (Neubauer-test). The results showed that biochar produced from a mixture of chicken manure and saw dust was equivalent to a standard phosphate fertilizer (superphosphate) with respect to P available for plant uptake. For most materials, a pyrolysis temperature of 400 °C was slightly more beneficial for P availability than 500 °C. Pyrolytic carbonization mostly was more supportive for plant growth than hydrothermal carbonization of the tested feedstocks. For some feedstocks the addition of sodium carbonate improved the P uptake of the plants without affecting the biomass production. The results show that P-rich waste materials used as secondary resources for carbonization can effectively contribute to increased P recovery, savings in the use of mineral phosphate fertilizers and reduced P loads to non-target ecosystems. Additionally, other benefits of biochar application to agricultural soils like carbon sequestration or improvements of physical soil characteristics may supplement the fertilizer effect of P-enriched biochars or hydrochars.

Chemical fertilizers as a source of (238)U, (40)K, (226)Ra, (222)Rn, and trace metal pollutant of the environment in Saudi Arabia.

PubMed

Alshahri, Fatimh; Alqahtani, Muna

2015-06-01

The specific activities of (238)U, (226)Ra, (40)K, and (222)Rn in chemical fertilizers were measured using gamma ray spectrometer and Cr-39 detector. In this study, 21 chemical fertilizers were collected from Eastern Saudi Arabian markets. The specific activities of (238)U ranged from 23 ± 0.5 to 3900 ± 195 Bq kg(-1); (226)Ra ranged from 5.60 ± 2.80 to 392 ± 18 Bq kg(-1); and (40)K ranged from 18.4 ± 3 to 16,476 ± 820 Bq kg(-1). The radon concentrations and the radon exhalation rates were found to vary from 3.20 ± 1.20 to 1532 ± 160 Bq m(-3) and from 1.60 to 774 mBq m(-2) h(-1), respectively. Radium equivalent activities (Raeq) were calculated for the analyzed samples to assess the radiation hazards arising due to the use of these chemical fertilizers in the agriculture soil. The Raeq for six local samples (nitrogen, phosphorous, and potassium (NPK) and single superphosphate (SSP)) and one imported sample (Sulfate of Potash (SOP)) were greater than the acceptable value 370 Bq kg(-1). The total air absorbed doses rates in air 1 m above the ground (D) were calculated for all samples. All samples, except one imported granule sample diammonium phosphate (DAP), were higher than the estimated average global terrestrial radiation of 55 nGy h(-1). The highest annual effective dose was in triple super phosphate (TSP) fertilizers (2.1 mSv y(-1)). The results show that the local TSP, imported SOP, and local NPK (sample 13) fertilizers were unacceptable for use as fertilizers in agricultural soil. Furthermore, the toxic elements and trace metals (Pb, Cd, Cr, Co, Ni, Hg, and As) were determined using atomic absorption spectrometer. The concentrations of chromium in chemical fertilizers were higher than the global values.

Phosphorus, nitrogen, and radionuclide retention and leaching from a Joel sand amended with red mud/gypsum

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

McPharlin, L.R.; Jeffery, R.C.; Toussaint, L.F.

1994-01-01

The leaching of phosphorus (P), nitrogen (N), and radionuclides [sup 232]Th, [sup 226]Ra, [sup 228]Ra, and [sup 40]K from Joel sands amended with red mud/gypsum (RMG) at 9 rates (0, 2, 4, 8, 16, 32, 64, 128, and 256 t/ha) was measured using columns. Intense leaching conditions (34 mm/day for 12 days) and a high rate of applied P (320 kg/ha as superphosphate) and N (680 kg/ha as ammonium nitrate) were used to simulate extremes of irrigated vegetable production on the Swan Coastal Plain. Addition of the highest rate of RMG (256 t/ha) reduced leaching of fertiliser P and ammonium-nitrogenmore » (NH4-N) by 85% and 50%, respectively, compared with 0 t/ha after 12 days. At 64 t RMG/ha P leaching was reduced 50% compared with 0 t/ha. Nitrate-nitrogen (NO3-N) leaching was not affected by addition of RMG. Reduced leaching of NH4-N was attributed to an increase in cation exchange capacity of the soil with the addition of RMG. Bicarbonate-extractable P in the soil increased with rate of RMG to >50 [mu]g P/g soil at 256 t/ha. This indicates that soil testing of residual P could be used to reduce P inputs to vegetable crops after soils were amended with RMG. This would further reduce the impact of vegetable production on the water systems of the Swan Coastal Plain and extend the period of effectiveness of RMG amended soils. The increase in [sup 232]Th specific activity in Joel sand amended with RMG was well below statutory limits even at the highest rate. Neither [sup 40]K nor [sup 226]Ra were detectable in RMG amended sands up to 256 t RMG/ha. There was no evidence of leaching of [sup 226]Ra or [sup 228]Ra at any rate of RMG. These results suggest that the use of RMG amendment on commercial horticultural properties on the Swan Coastal Plain could be feasible. 30 refs., 7 figs., 2 tabs.« less

Effect of interactions on the nutrient status of a tropical soil treated with green manures and inorganic phosphate fertilizers.

PubMed

Bah, Abdul R; Rahman, Zaharah A; Hussin, Aminuddin

2004-06-08

Integrated nutrient management systems using plant residues and inorganic P fertilizers have high potential for increasing crop production and ensuring sustainability in the tropics, but their adoption requires in-depth understanding of nutrient dynamics in such systems. This was examined in a highly weathered tropical soil treated with green manures (GMs) and P fertilizers in two experiments conducted in the laboratory and glasshouse. The treatments were factorial combinations of the GMs (Calopogonium caeruleum, Gliricidia sepium, and Imperata cylindrica) and P fertilizers (phosphate rocks [PRs] from North Carolina, China, and Algeria, and triple superphosphate) replicated thrice. Olsen P, mineral N, pH, and exchangeable K, Ca, and Mg were monitored in a laboratory incubation study for 16 months. The change in soil P fractions and available P was also determined at the end of the study. Phosphorus available from the amendments was quantified at monthly intervals for 5 months by 33P-32P double isotopic labeling in the glasshouse using Setaria sphacelata as test crop. The GMs were labeled with 33P to determine their contribution to P taken up by Setaria, while that from the P fertilizers was indirectly measured by labeling the soil with 32P. The P fertilizers hardly changed Olsen P and exchangeable cations during 16 months of incubation. The legume GMs and legume GM+P did not change Olsen P, lowered exchangeable Ca, and increased exchangeable K about threefold (4.5 cmol[+]kg(-1) soil) in the first 4 months, even as large amounts of NH4-N accumulated (approximately 1000 mg kg soil(-1)) and soil pH increased to more than 6.5. Afterwards, Olsen P and exchangeable Ca and Mg increased (threefold) as NH4+-N and soil pH declined. The legume GMs also augmented reversibly sorbed P in Al-P and Fe-P fractions resulting in high residual effect in the soil, while fertilizer-P was irreversibly retained. The GMs increased PR-P utilization by 40 to over 80%, mobilized soil P, and markedly enhanced uptake of N, K, Ca, and Mg. Thus GMs+PRs is an appropriate combination for correcting nutrient deficiencies in tropical soils.

Phosphorus in waters from sewage sludge amended lysimeters.

PubMed

Hinesly, T D; Jones, R L

1990-01-01

In surface waters, phosphorus (P) concentrations exceeding 0.05 mg liter(-1) may cause eutrophic conditions. This study was undertaken to measure total P concentrations in runoff and tile drainage waters from land receiving either inorganic fertilizer or anaerobically digested sewage sludge. Total P was measured in runoff and tile drainage waters during 2 years of sample collections from instrumented, large-scale lysimeters planted to corn (Zea mays L.). During the 3 years prior to monitoring P concentrations, six of the lysimeter plots had been amended with anaerobically digested sewage sludge which supplied 5033 kg P per ha. Additional sludge applications supplied 1058 and 1989 kg P per ha during the first and second years of monitoring operations, respectively. Another six lysimeters were annually treated with fertilizer which included P applications amounting to 112 kg ha(-1). For years 1 and 2, respectively, annual losses from lysimeters treated with sewage sludge were 4.27 and 0.35 kg P per ha in runoff and 0.91 from 0.91 and 0.51 kg Per P per ha in drainage waters. Parallel annual losses of P from lysimeters treated with superphosphate were 2.15 and 0.17 kg ha(-1) in runoff and 0.53 and 0.35 kg ha(-1) in tile drainage waters. Sludge applications did not significantly change absolute soil contents of organic P, but did decrease the per cent of total P present in organic forms. Sludge and soil, respectively, contained 21 and 36% of their total P contents in organic forms. In sludge and soil about 85 and 64% of their respective total inorganic P contents were associated with the Al and Fe fractions. Sludge applications significantly increased soil contents of P in the saloid (water-soluble plus P extracted with 1 N NH(4)Cl), Al, Fe and reductant soluble P fractions, but contents of Ca-bound P were not changed. Total P contents of the soil below a depth of 30 cm were not affected by sludge incorporated to a depth of about 15 cm by plowing.

Radiological investigation of phosphate fertilizers: Leaching studies.

PubMed

Hegedűs, Miklós; Tóth-Bodrogi, Edit; Németh, Szabolcs; Somlai, János; Kovács, Tibor

2017-07-01

The raw materials of the phosphate fertilizer industry are the various apatite minerals. Some of these have high levels of natural radionuclides, and thus phosphate fertilizers contain significant amounts of U-238, K-40 and Ra-226. These can leach out of the fertilizers used in large quantities for resupplying essential nutrients in the soil and can then enter the food chain through plants, thereby increasing the internal dose of the affected population. In the current study, the radiological risk of eight commercially available phosphate fertilizers (superphosphate, NPK, PK) and their leaching behaviours were investigated using different techniques (gamma and alpha spectrometry), and the dose contributions of using these fertilizers were estimated. To characterize the leaching behaviour, two leaching procedures were applied and compared -the MSZ 21470-50 (Hungarian standard) and the Tessier five-step sequential extraction method. Based on the evaluation of the gamma-spectra, it is found that the level of Th-232 in the samples was low (max.7 ± 6 Bq kg -1 ), the average Ra-226 activity concentration was 309 ± 39 Bq kg -1 (min. 10 ± 8 Bq kg -1 , max. 570 ± 46 Bq kg -1 ), while the K-40 concentrations (average 3139 ± 188 Bq kg -1 , min. 51 ± 36 Bq kg -1 ) could be as high as 7057 ± 427 Bq kg -1 . The high K-40 can be explained by reference to the composition of the investigated fertilizers (NPK, PK). U concentrations were between 15 and 361 Bq kg -1 , with the average of 254 Bq kg -1 , measured using alpha spectrometry. The good correlation between P 2 O 5 content and radioactivity reported previously is not found in our data. The leaching studies reveal that the mobility of the fertilizer's uranium content is greatly influenced by the parameters of the leaching methods. The availability of U to water ranged between 3 and 28 m/m%, while the Lakanen-Erviö solution mobilized between 10 and 100% of the U content. Copyright © 2016 Elsevier Ltd. All rights reserved.

Various soil amendments and environmental wastes affect the (im)mobilization and phytoavailability of potentially toxic elements in a sewage effluent irrigated sandy soil.

PubMed

Shaheen, Sabry M; Shams, Mohamed S; Khalifa, Mohamed R; El-Dali, Mohamed A; Rinklebe, Jörg

2017-08-01

Contamination of long-term sewage effluent irrigated soils by potentially toxic elements (PTEs) is a serious concern due to its high environmental and health risk. Our scientific hypothesis is that soil amendments can cause contradictory effects on the element mobilization and phytoavailability depending on the type of element and amendment. Therefore, we aimed to assess the impact of the application (1%) of several low cost amendments and environmental wastes on the (im)mobilization, availability, and uptake of Al, Cd, Cr, Cu, Fe, Mn, Ni, and Zn by sorghum (Sorghum bicolor) in a long term sewage effluent irrigated sandy soils collected from Egypt. The used materials include activated charcoal (AC), potassium humate (KH), phosphate rock (PR), phosphogypsum (PG), triple superphosphate (TSP), phosphoric acid (PA), sulfur (S), sugar beet factory lime (SBFL), cement bypass kiln dust (CBD), egg shell (ES), bone mill (BM), brick factory residual (BFR), ceramic powder (CP), and drinking water treatment residual (WTR). The mobilization and availability of the elements in the soil were extracted using NH 4 NO 3 and ammonium bicarbonate- diethylene triamine penta acetic acid (AB-DTPA), respectively. The above-ground biomass samples were analyzed for the elements studied. The results confirmed our hypothesis and concluded that although some amendments like S, PA, and TSP can be used for reducing the plant uptake of Al, Cr, and Fe, they might be used with KH for enhancing the phytoextraction of Cd, Cu, Mn, and Ni. Moreover, several wastes such as BFR and WTR might be used for enhancing the phytoextraction of Al, Cd, Cr, Cu, Fe, and Ni and reducing the uptake of Mn from the studied soil. Although SBFL decreased the plant uptake of Al, Fe, Mn, and Zn, it's increased the plant uptake of Cd, Cu, and Ni. Therefore, the amendments which reduce the plant uptake of an element might be suitable candidates for its immobilization, while the amendments which increase the plant uptake of an element might be used for enhancing its phytoextraction when using bioenergy crops like sorghum in similar contaminated sandy soils. The studied materials offered the potential for effective and low cost media for the treatment of PTEs contaminated sewage effluent irrigated sandy soils. These results should be verified in a field study. Copyright © 2017 Elsevier Inc. All rights reserved.

Forest Soil Phosphorus Resources and Fertilization Affect Ectomycorrhizal Community Composition, Beech P Uptake Efficiency, and Photosynthesis

PubMed Central

Zavišić, Aljosa; Yang, Nan; Marhan, Sven; Kandeler, Ellen; Polle, Andrea

2018-01-01

Phosphorus (P) is an important nutrient, whose plant-available form phosphate is often low in natural forest ecosystems. Mycorrhizal fungi mine the soil for P and supply their host with this resource. It is unknown how ectomycorrhizal communities respond to changes in P availability. Here, we used young beech (Fagus sylvatica L.) trees in natural forest soil from a P-rich and P-poor site to investigate the impact of P amendment on soil microbes, mycorrhizas, beech P nutrition, and photosynthesis. We hypothesized that addition of P to forest soil increased P availability, thereby, leading to enhanced microbial biomass and mycorrhizal diversity in P-poor but not in P-rich soil. We expected that P amendment resulted in increased plant P uptake and enhanced photosynthesis in both soil types. Young beech trees with intact soil cores from a P-rich and a P-poor forest were kept in a common garden experiment and supplied once in fall with triple superphosphate. In the following summer, labile P in the organic layer, but not in the mineral top soil, was significantly increased in response to fertilizer treatment. P-rich soil contained higher microbial biomass than P-poor soil. P treatment had no effect on microbial biomass but influenced the mycorrhizal communities in P-poor soil and shifted their composition toward higher similarities to those in P-rich soil. Plant uptake efficiency was negatively correlated with the diversity of mycorrhizal communities and highest for trees in P-poor soil and lowest for fertilized trees. In both soil types, radioactive P tracing (H333PO4) revealed preferential aboveground allocation of new P in fertilized trees, resulting in increased bound P in xylem tissue and enhanced soluble P in bark, indicating increased storage and transport. Fertilized beeches from P-poor soil showed a strong increase in leaf P concentrations from deficient to luxurious conditions along with increased photosynthesis. Based on the divergent behavior of beech in P-poor and P-rich forest soil, we conclude that acclimation of beech to low P stocks involves dedicated mycorrhizal community structures, low P reserves in storage tissues and photosynthetic inhibition, while storage and aboveground allocation of additional P occurs regardless of the P nutritional status. PMID:29706979

Spatial 2D distribution of the proportion of soil phosphorus uptake by maize and soybean caused by tillage and fertilization

NASA Astrophysics Data System (ADS)

Li, Haixiao; Mollier, Alain; Ziadi, Noura; Messiga, Aimé Jean; Parent, Leon-Étienne; Morel, Christian

2017-04-01

Plant-available soil phosphorus (P) accumulates primarily in the topsoil due to P fertilization and P released from crop residues. In contrast with conventional tillage (moldboard plough, MP), conservation tillage [e.g. no-till, (NT)] often leads to higher P concentrations in the topsoil mainly due to the absence of mixing between soil, fertilizer, and crop residues. Our objective was to estimate the proportion of P uptake from a given soil mass across the soil profile under maize and soybean as the product of root surface density proportions and local plant-available soil P. This study was conducted on a long-term field experiment initiated in 1992 in southern Quebec, Canada, and established on a clay-loam soil under MP and NT systems. The experiment was factorially treated with three P doses (0, 17.5 and 35 kg P ha-1 applied as triple superphosphate on maize at 5 cm depth and at 5 cm on one side of the crop row). Soil was sampled at flowering stage at five depths (0-5, 5-10, 10-20, 20-30 and 30-40 cm) and three horizontal distances perpendicular to the crop row (5, 15 and 25 cm) in 2014 and 2015 to map a grid soil P availability to plants, e.g. phosphate ion concentrations in solution and the time-dependent amount of phosphate ions that can equilibrate- solution by diffusion, root distribution, and consequently crop P uptake, which was calculated as the fraction of plant-available soil P intercepted by surface roots. In general, NT tended to have higher soil P status in the upper soil layer and lower soil P status in the deeper soil layer compared to MP ; confirming previous results obtained from the same experimental site. This variation along the soil profile was significantly affected by sampling distance to crop row with higher concentration observed at 5-cm distance mainly because of the placement of P fertilizers. The 2D distribution of P uptake depended on tillage practice and P fertilization. There was higher proportions of P uptake from the 0-10 and 0-20 cm layers in NT (46% and 79%, respectively) compared to MP (25% and 68%, respectively). On average 8% of P uptake originated from the 30-40 cm layer irrespective of tillage, indicating that plant P uptake from deeper soil layers also influenced the P cycling in agroecosystems.

Digestate and ash as alternatives to conventional fertilisers: Benefits and threats to soil biota

NASA Astrophysics Data System (ADS)

Marshall, Rachel; Lag-Brotons, Alfonso J.; Herbert, Ben; Hurst, Lois; Ostle, Nick; Dodd, Ian C.; Quinton, John; Surridge, Ben; Aiouache, Farid; Semple, Kirk T.

2017-04-01

Recovering energy and nutrients from waste offers opportunities to tackle issues of energy and food security whilst simultaneously improving waste management. Waste materials from the bioenergy industry potentially contain valuable resources for use in agriculture and there is growing evidence to suggest that the use of digestate, from anaerobic digestion, and biomass ash from incineration processes could contribute to improving soil health and nutrition. The work presented here is part of the Adding Value to Ash and Digestate (AVAnD) project which looks at the impacts of digestate and ash blends on soil fertility, crop yields and soil health. Whilst increased crop productivity is one of the essential indicators of the success of these alternative soil amendments; it is important that the impacts on soil biological function is understood. Field and lab experiments were conducted with a number of different fertiliser treatments, including conventional fertiliser (urea and superphosphate), digestate from two contrasting feedstocks, ash material and ash-digestate blends. Looking across different biological scales from soil microbe to soil macro-fauna, this work examines the benefits and threats to soil biota arising from the use of ash-digestate fertilisers in agriculture. Measurements of microbial respiration and biomass (by chloroform fumigation) and community composition (by phospholipid fatty acid analysis) were made at different timescales (days/weeks). Data from these studies demonstrates that none of the soil amendments decreased microbial activity or biomass in the short term (t= 1 month). Additions of both conventional fertilisers and the fertilisers derived from waste stimulated microbial activity with significantly higher respiration observed from the digestate based treatments. Digestate-based treatments also resulted in higher soil microbial biomass and differential effects were observed between digestate amendments with and without ash. These results will be discussed in the context of microbial community change in response to the amendments. At the macro-fauna scale, effects of amendments on earthworm (Eisenia fetida and Lumbricus terrestris) health were assessed using 14 day toxicity assays (4 application rates between 85-340 kgN.ha-1) and with 48 hour avoidance tests. In general, the addition of digestate-based fertilisers resulted in no observable toxic effects and earthworms did not significantly avoid these materials when compared to a conventional fertiliser. However, earthworms mortality was observed with one of the ash-digestate blends applied at 340 kgN.ha-1, potentially linked to changes in soil pH and elements speciation .It is therefore crucial that the effects of the amendments on soil properties, and the implications this has for soil communities at all scales, is understood to ensure sustainable soil management in agriculture.

Mineralization of soluble P fertilizers and insoluble rock phosphate in response to phosphate-solubilizing bacteria and poultry manure and their effect on the growth and P utilization efficiency of chilli (Capsicum annuum L.)

NASA Astrophysics Data System (ADS)

Abbasi, M. K.; Musa, N.; Manzoor, M.

2015-08-01

The ability of soil microorganisms and organic manure to convert insoluble phosphorus (P) to an accessible form offers a biological rescue system for improving P utilization efficiency in soil-plant systems. Our objective was to examine the P mineralization potential of two soluble P fertilizers (SPF), i.e., single superphosphate (SSP) and diammonium phosphate (DAP), and of insoluble rock phosphate (RP) with and without phosphate-solubilizing bacteria (PSB) and poultry manure (PM) and their subsequent effect on the growth, yield and P utilization efficiency (PUE) of chilli (Capsicum annuum L.). An incubation study was carried out on a loam (slightly alkaline) soil with 12 treatments: T0 - control; T1 - RP; T2 - SSP; T3 - DAP; T4 - PM; T5 - 1/2 RP+1/2 SSP; T6 - 1/2 RP+1/2 DAP; T7 - 1/2 RP+1/2 PM; T8 - RP+PSB; T9 - 1/2 RP+1/2 SSP+PSB; T10 - 1/2 RP+1/2 DAP+PSB; and T11 - 1/2 RP+1/2 PM+PSB. Phosphorus mineralization was measured by analyzing extractable P from the amended soil incubated under controlled conditions at 25 °C for periods of 0, 5, 15, 25, 35 and 60 days. A complementary greenhouse experiment was conducted in pots with chilli (Capsicum annuum L.) as a test crop. Growth, yield, P uptake and PUE of the chilli was determined during the study. Results indicated that P mineralization in soil amended with RP was 6.0-11.5 mg kg-1, while both soluble P fertilizers resulted in 68-73 mg P kg-1 at day 0, which decreased by 79-82 % at the end of incubation. The integrated use of PSB and PM with RP in T11 stimulated P mineralization by releasing a maximum of 25 mg P kg-1 that was maintained at high levels without any loss. Use of PSB decreased soil pH. In the greenhouse experiment, RP alone or RP+PSB did not have a significant impact on plant growth. However, the combined use of RP, PM and PSB in T11 resulted in similar growth, yield and P uptake of chilli as DAP. The PUE of applied P varied from 4 to 29 % and was higher in the treatments that included PSB. We conclude that the use of PSB and PM with insoluble RP or with soluble P fertilizers could be a promising approach to enhance P availability from both low-grade RP and SPF for crop production in intensive cropping systems.

Mobility of Pb, Cu, and Zn in the phosphorus-amended contaminated soils under simulated landfill and rainfall conditions.

PubMed

Cao, Xinde; Liang, Yuan; Zhao, Ling; Le, Huangying

2013-09-01

Phosphorus-bearing materials have been widely applied in immobilization of heavy metals in contaminated soils. However, the study on the stability of the initially P-induced immobilized metals in the contaminated soils is far limited. This work was conducted to evaluate the mobility of Pb, Cu, and Zn in two contrasting contaminated soils amended with phosphate rock tailing (PR) and triple superphosphate fertilizer (TSP), and their combination (P + T) under simulated landfill and rainfall conditions. The main objective was to determine the stability of heavy metals in the P-treated contaminated soils in response to the changing environment conditions. The soils were amended with the P-bearing materials at a 2:1 molar ratio of P to metals. After equilibrated for 2 weeks, the soils were evaluated with the leaching procedures. The batch-based toxicity characteristic leaching procedure (TCLP) was conducted to determine the leachability of heavy metals from both untreated and P-treated soils under simulated landfill condition. The column-based synthetic precipitation leaching procedure (SPLP) were undertaken to measure the downward migration of metals from untreated and P-treated soils under simulated rainfall condition. Leachability of Pb, Cu, and Zn in the TCLP extract followed the order of Zn > Cu > Pb in both soils, with the organic-C- and clay-poor soil showing higher metal leachability than the organic-C- and clay-rich soil. All three P treatments reduced leachability of Pb, Cu, and Zn by up to 89.2, 24.4, and 34.3 %, respectively, compared to the untreated soil, and TSP revealed more effectiveness followed by P + T and then PR. The column experiments showed that Zn had the highest downward migration upon 10 pore volumes of SPLP leaching, followed by Pb and then Cu in both soils. However, migration of Pb and Zn to subsoil and leachate were inhibited in the P-treated soil, while Cu in the leachate was enhanced by P treatment in the organic-C-rich soil. More than 73 % P in the amendments remained in the upper 0-10 cm soil layers. However, leaching of P from soluble TSP was significant with 24.3 % of P migrated in the leachate in the organic-C-poor soil. The mobility of heavy metals in the P-treated soil varies with nature of P sources, heavy metals, and soils. Caution should be taken on the multi-metal stabilization since the P amendment may immobilize some metals while promoting others' mobility. Also, attention should be paid to the high leaching of P from soluble P amendments since it may pose the risk of excessive P-induced eutrophication.

The Chemophytostabilisation Process of Heavy Metal Polluted Soil

PubMed Central

Grobelak, Anna; Napora, Anna

2015-01-01

Industrial areas are characterised by soil degradation processes that are related primarily to the deposition of heavy metals. Areas contaminated with metals are a serious source of risk due to secondary pollutant emissions and metal leaching and migration in the soil profile and into the groundwater. Consequently, the optimal solution for these areas is to apply methods of remediation that create conditions for the restoration of plant cover and ensure the protection of groundwater against pollution. Remediation activities that are applied to large-scale areas contaminated with heavy metals should mainly focus on decreasing the degree of metal mobility in the soil profile and metal bioavailability to levels that are not phytotoxic. Chemophytostabilisation is a process in which soil amendments and plants are used to immobilise metals. The main objective of this research was to investigate the effects of different doses of organic amendments (after aerobic sewage sludge digestion in the food industry) and inorganic amendments (lime, superphosphate, and potassium phosphate) on changes in the metals fractions in soils contaminated with Cd, Pb and Zn during phytostabilisation. In this study, the contaminated soil was amended with sewage sludge and inorganic amendments and seeded with grass (tall fescue) to increase the degree of immobilisation of the studied metals. The contaminated soil was collected from the area surrounding a zinc smelter in the Silesia region of Poland (pH 5.5, Cd 12 mg kg-1, Pb 1100 mg kg-1, Zn 700 mg kg-1). A plant growth experiment was conducted in a growth chamber for 5 months. Before and after plant growth, soil subsamples were subjected to chemical and physical analyses. To determine the fractions of the elements, a sequential extraction method was used according to Zeien and Brümmer. Research confirmed that the most important impacts on the Zn, Cd and Pb fractions included the combined application of sewage sludge from the food industry and the addition of lime and potassium phosphate. Certain doses of inorganic additives decreased the easily exchangeable fraction from 50% to 1%. The addition of sewage sludge caused a decrease in fraction I for Cd and Pb. In combination with the use of inorganic additives, a mobile fraction was not detected and an easily mobilisable fraction was reduced by half. For certain combinations of metals, the concentrations were detected up to a few percent. The application of sewage sludge resulted in a slight decrease in a mobile (water soluble and easily exchangeable metals) fraction of Zn, but when inorganic additives were applied, this fraction was not detected. The highest degree of immobilisation of the tested heavy metals relative to the control was achieved when using both sewage sludge and inorganic additives at an experimentally determined dose. The sequential extraction results confirmed this result. In addition, the results proved that the use of the phytostabilisation process on contaminated soils should be supported. PMID:26115341

The Chemophytostabilisation Process of Heavy Metal Polluted Soil.

PubMed

Grobelak, Anna; Napora, Anna

2015-01-01

Industrial areas are characterised by soil degradation processes that are related primarily to the deposition of heavy metals. Areas contaminated with metals are a serious source of risk due to secondary pollutant emissions and metal leaching and migration in the soil profile and into the groundwater. Consequently, the optimal solution for these areas is to apply methods of remediation that create conditions for the restoration of plant cover and ensure the protection of groundwater against pollution. Remediation activities that are applied to large-scale areas contaminated with heavy metals should mainly focus on decreasing the degree of metal mobility in the soil profile and metal bioavailability to levels that are not phytotoxic. Chemophytostabilisation is a process in which soil amendments and plants are used to immobilise metals. The main objective of this research was to investigate the effects of different doses of organic amendments (after aerobic sewage sludge digestion in the food industry) and inorganic amendments (lime, superphosphate, and potassium phosphate) on changes in the metals fractions in soils contaminated with Cd, Pb and Zn during phytostabilisation. In this study, the contaminated soil was amended with sewage sludge and inorganic amendments and seeded with grass (tall fescue) to increase the degree of immobilisation of the studied metals. The contaminated soil was collected from the area surrounding a zinc smelter in the Silesia region of Poland (pH 5.5, Cd 12 mg kg-1, Pb 1100 mg kg-1, Zn 700 mg kg-1). A plant growth experiment was conducted in a growth chamber for 5 months. Before and after plant growth, soil subsamples were subjected to chemical and physical analyses. To determine the fractions of the elements, a sequential extraction method was used according to Zeien and Brümmer. Research confirmed that the most important impacts on the Zn, Cd and Pb fractions included the combined application of sewage sludge from the food industry and the addition of lime and potassium phosphate. Certain doses of inorganic additives decreased the easily exchangeable fraction from 50% to 1%. The addition of sewage sludge caused a decrease in fraction I for Cd and Pb. In combination with the use of inorganic additives, a mobile fraction was not detected and an easily mobilisable fraction was reduced by half. For certain combinations of metals, the concentrations were detected up to a few percent. The application of sewage sludge resulted in a slight decrease in a mobile (water soluble and easily exchangeable metals) fraction of Zn, but when inorganic additives were applied, this fraction was not detected. The highest degree of immobilisation of the tested heavy metals relative to the control was achieved when using both sewage sludge and inorganic additives at an experimentally determined dose. The sequential extraction results confirmed this result. In addition, the results proved that the use of the phytostabilisation process on contaminated soils should be supported.

Nutrient transport to the Swan-Canning Estuary, Western Australia

NASA Astrophysics Data System (ADS)

Peters, Norman E.; Donohue, Robert

2001-09-01

Catchment nutrient availability in Western Australia is primarily controlled by the disposal of animal waste and the type and rate of fertilizer application, particularly on the relatively narrow (25 km wide), sandy coastal plain. Nitrogen (N) and phosphorus (P) concentrations and fluxes during the wet season of 15 tributaries, including four urban drains to the Swan-Canning Estuary, were evaluated from 1986 to 1992 and additionally concentrations only were evaluated throughout the year from 1993 to 1996. Concentrations of filtered reactive P (FRP) and total P (TP) were generally low, with the volume-weighted means for all sites being 0·06 mg l-1 and 0·12 mg l-1 respectively. The urban drains had higher TP concentrations (volume-weighted mean of 0·21 mg l-1) than the streams (0·12 mg l-1), with the high concentrations associated with particulate matter. Total inorganic N (TIN, NH4N plus NO3N) and total N (TN), which is of interest to eutrophic status of the N-limited estuary, were likewise low, compared with other developed areas having a similar climate. Both TIN and TN were higher in the urban drains (0·76 mg l-1 and 1·5 mg l-1 respectively) than the streams (0·31 mg l-1 and 1·2 mg l-1 respectively). The Avon River, which drains 98·5% of the 121 000 km2 catchment area, contributes most of the N (0·03 kg ha-1 year-1 or 65%) and a high percentage of the P (<0·01 kg ha-1

Efforts to improve and sustain the productive utilization of dry grasslands in Armenia

NASA Astrophysics Data System (ADS)

Mezhunts, Bagrat; Navasardyan, Marine

2014-05-01

Armenia is a small mountainous country (29,743 km2) located in the South Caucasus. It lies in the sub-tropical zone and has a continental climate with hot summers (av. +250C) and cold winters (av. -60C). The average precipitation is 550 mm; in the dry-steppe zone it amounts to only 250 mm and with a rainy season in spring-early summer. Altitudinal variation (390-4,095 m) gives rise to a range of climatic zones (from semi-desert to alpine), soil types and plant communities. Besides, Armenia is situated on the crossroads of Caucasian - mesophyllous (humid) and Armeno-Iranian - xerophyllous (arid) floristic provinces, which has made it to a "biodiversity hotspot". Agriculture is important as a source of employment and for domestic food supply. The rural population (ca. 1.2 million) is largely dependent on livestock for their livelihood. The principal feed resource is extensive grasslands (60% of total agricultural lands), but past practices of uncontrolled grazing management has led to low grassland productivity and low proportion of valuable legume forages. Improvement of natural grasslands, enhancement of feed quality, prevention of soil erosion and re-establishment of vegetation cover are key socio-economic challenges and are needed to raise the livelihood of rural population in Armenia. This presentation focuses on present status and trends of dry pastureland degradation, exposed to intensive grazing, and on results from case studies to increase productivity and restore valuable forage species for sustainable use in agriculture. Three different conventional approaches have been applied in these studies including: fertilization with moderate doses of ammonium and potassium nitrate and superphosphate, over-sowing by local legume seeds and implementation of a 2-year rest period in overgrazed areas. From 1986 to 2007, the total yield (TY) in studied dry-steppe pastures decreased by 40%, while at the same time, the proportion of grasses in total yield decreased by 50%, legumes - 70%, but no changes observed in the proportion of unpalatable forbs. The studied drylands showed a high spatial mosaic of the vegetation cover as within the same sampling areas TY varied from 0.4 to 4.2 t/ha. The abovementioned approaches had different effects on total yield and botanical composition in heavily and medium trampled pastures (HTP&MTP) with higher positive biological and economic effect for the MTP. The study also revealed that a 2-year rest of overgrazed areas positively influenced above- and below- ground grass biomass. Impact was mainly determined by individual peculiarities of the studied species. In addition, yields of annual and perennial grass communities increased 1.4-1.9 and 2.4-2.9 times, respectively. It is concluded that total biomass yield itself and, in particular, the proportion of legumes and grasses, could serve as indicators to characterize the extent of dryland degradation and that the tested approaches might mitigate degradation processes caused by uncontrolled grazing management.

Nutrient transport to the Swan - Canning Estuary, Western Australia

USGS Publications Warehouse

Peters, N.E.; Donohue, R.

2001-01-01

Catchment nutrient availability in Western Australia is primarily controlled by the disposal of animal waste and the type and rate of fertilizer application, particularly on the relatively narrow (~25 km wide), sandy coastal plain. Nitrogen (N) and phosphorous (P) concentrations and fluxes during the wet season of 15 tributaries, including four urban drains to the Swan-Canning Estuary, were evaluated from 1986 to 1992 and additionally concentrations only were evaluated throughout the year from 1993 to 1996. Concentrations of filtered reactive P (FRP) and total P (TP) were generally low, with the volume-weighted means for all sites being 0.06 mg 1-1 and 0.12 mg 1-1 respectively. The urban drains had higher TP concentrations (volume-weighted mean of 0.21 mg 1-1) than the streams (0.12 mg 1-1), with the high concentrations associated with particulate matter. Total inorganic N (TIN, NH4N plus NO3N) and total N (TN), which is of interest to eutrophic status of the N-limited estuary, were likewise low, compared with other developed areas having a similar climate. Both TIN and TN were higher in the urban drains (0.76 mg 1-1 and 1.5 mg 1-1 respectively) than the streams (0.31 mg 1-1 and 1.2 mg 1-1 respectively). The Avon River, which drains 98.5% of the 121 000 km2 catchment area, contributes most of the N (0.03 kg ha-1 year-1 or 65%) and a high percentage of the P (<0.01 kg ha-1 year-1 or 32%) to the estuaries. The Avon River nutrient fluxes are much less than other tributaries closer to the estuary. The coastal plain receives significantly higher rainfall (1,200 mm year-1) and has more intense horticulture and animal production than inland areas (<300 mm year-1). Annual rainfall is seasonal, occuring primarily from May through December. The surficial aquifers on the coastal plain generally are sandy with a low nutrient retention capacity, and rapidly transmit soluble and colloidal material in subsurface flow. Ellen Brook, on the coastal plain, drains pastures treated with superphosphate and has the highest FRP (0.51 mg 1-1), TP (0.7 mg 1-1) and TN (2.1 mg 1-1) of any tributary to the estuary. The coastal plain is also undergoing urbanization, particularly in areas adjacent to the estuary. Nutrients are subsequently available for transport during the onset of seasonal wet weather. Perennial baseflow from urban areas is an important source of nutrients. Water yield from the urban areas was high, being as much as 50% of annual rainfall. The timing of the nutrients delivered by the tributaries may be an important control on estuarine ecology. Copyright ?? 2001 John Wiley and Sons, Ltd.

Adding Value to Ash and Digestate (AVAnD): Performance of Novel Soil Amendents on the Soil-Plant System Under Glasshouse Conditions

NASA Astrophysics Data System (ADS)

Lag-Brotons, Alfonso; Marshall, Rachel; Herbert, Ben; Hurst, Lois; Ostle, Nick; Dodd, Ian; Quinton, John; Surridge, Ben; Aiouache, Farid; Semple, Kirk T.

2017-04-01

Resource recovery from waste plays a central role in strategies tackling current worldwide sustainability problems. In this sense, two waste streams derived from bioenergy production (anaerobic digestion and incineration), digestate [D] and biomass ash [A], may be especially valuable within agriculture. These materials offer complementary plant nutrient profiles for alternative fertiliser production (i.e. nitrogen [N] from D and phosphorus [P] from A). In addition, incorporating these materials into the soil could impact upon several soil/plant characteristics, and have positive effects on ecosystem services (eg. nutrient cycling). Therefore, this present work assessed the effects of A/D blends on the soil-plant system under controlled conditions (glasshouse). The overarching aim of "Adding Value to Ash and Digestate [AVAnD]" project is to identify novel nutrient-recycling pathways to maximise soil quality and crop productivity utilising waste streams derived from bioenergy production. Two pot experiments of 6 weeks duration were carried out [Exp. A and Exp. B] using contrasting agricultural soils (neutral loam and sandy acidic soil) and wheat as the crop. A factorial randomised block design was selected, with fertilisation treatment and soil condition (planted/unplanted) as factors. Fertilisation treatments (n=13) were applied at a rate of 63/60 kg N/P2O5 per ha and comprised: control ([C], no fertilisation), urea [U], urea+superphosphate [U+P], fly ash [A1], bottom ash [A2], U+A1; U+A2, anaerobic digestates [D1, D2] and ash/digestate blends [D1A1, D1A2, D2A1, D2A2]. Each block (n=5) contained 8 planted and 5 unplanted pots (104 planted + 65 unplanted experimental units). At the end of the experiment, all the plants were assessed for morphometric traits, while for tissue elemental analyses the total number of replicates per treatment was randomly reduced (n=5/treatment). Soil physico-chemical properties (i.e. available nitrogen, pH) were assessed in unplanted and selected planted pots. Differences in plant growth were primarily dependant on soil type and secondarily on fertiliser type. In Exp. A, adding digestate-based treatments resulted in comparable biomass and N levels (concentration and uptake) to that of inorganic fertilisers (U+P). In Exp. B, growth was mainly related to soil pH, with higher biomass in those treatments containing A1. In relation to soil properties, the main effects were attributed to pH variation and increase of available N- / P- and EC. Based on these results, these novel materials and inorganic fertilisers induced similar effects in the soil-plant system, thus suggesting inorganic fertilisers could potentially be replaced. However, further research under field conditions, including other soil types, is required to corroborate the value of these A/D blends as land conditioners.

Refine phosphorus stratification caused by long-term tillage and P fertilisation in maize -soybean rotation in eastern Canada

NASA Astrophysics Data System (ADS)

Ziadi, Noura; Morel, Christian

2017-04-01

The use of conservation tillage for crops production worldwide has increased markedly over recent years. Nutrient distributions under no-till (NT) compared with conventional moldboard tillage (CT) management in the cold, humid region of the eastern Canada need to be assessed for future placement, quantity, and type of fertilizers to efficiently match crop demands. We determined soil-profile distributions of soil total C (TC), total N (TN), and phosphate ions concentration (CP) in soil solution to a depth of 0.4 m after 23 years of continuous CT and NT management at different P fertilization rates on a clay loam soil in eastern Canada cropped with grain maize -soybean rotation. The experimental site was initiated in 1992 in southern Quebec, Canada. In August 2014, soil samples were collected at five profiles: 0 to 5, 5 to 10, 10 to 20, 20 to 30 and 30 to 40 cm under CT and NT fertilized at three P fertilizations (0 (P0), 17.5 (P0.5), and 35 (P1) kg P ha-1 applied as triple superphosphate on maize at 5 cm depth). To refine CNP stratification analysis for NT-P0 and NT-P1, supplemental soils of the 0-5 cm layer were sampled in P0 and P1 and then cutting into 5 layers of 1 cm. Different patterns for CP in relation to P fertilization under CT and NT were observed at the five profiles. The CP values did not differ significantly within ploughed layer but increased with P fertilization, e.g. 0.031, 0.066, and 0.075 mg P L-1 for P0, P0.5 and P1, respectively. Significant decline was observed in deeper depth beyond the plough. The Cp results in NT-P0 did not differ significantly to those of MP-P0. By contrast, highly significant P stratifications were observed in NT-P0.5 and NT-P1, especially marked in NT-P1 for which the CP value in 0-5 cm layer (0.35 mg P L-1) was 50 times greater than that in 30-40 cm layer (0.007 mg P L-1). To refine the C, N, and P stratifications, supplemental sampling was carried out in the 0-5 cm to cut this layer every 1 cm depth for P0 and P1. Most dramatic changes occurred within the 0-5 cm depth. The CP value in the first cm of soil (0.20 mg P L-1) was four times greater than that in the 4-5 cm layer (0.049 mg P L-1) of soil. The main reason for the large P accumulation in the first centimeter of soil is the annual return of plant residues to the soil surface. The stratification of TC and TN within the 0-5 cm layer showed similar trends irrespective of P fertilization. Under NT, the magnitude of CNP stratifications within the 0-1 cm layer to the 4-5 cm layer is equivalent to that observed in the 0-5 cm layer to the 30-40 cm layer.

Predicting the Soil Phosphorus Dynamics of the Ploughed Layer Under Continuous Cultivation and P Fertilization

NASA Astrophysics Data System (ADS)

Morel, C.; Augusto, L.; Gallet-Budynek, A. S.

2011-12-01

One major component of the biogeochemical cycling of phosphorus (P) in soils is the plant-available soil P. Its sound management, to minimize the loss of soil P to surface waters while ensuring enough P to sustain soil fertility, requires being able to predict the long term dynamics of plant-available soil P with the P budget. We examined the ability of a simple model to predict the change in plant-available soil P of the ploughed layer for almost 3 decades of continuous cultivation and P fertilization. We used a process-based assessment of plant-availability that considers both the concentration (Cp) of phosphate ions (Pi) in solution and the time-dependent amount (Pr) of Pi bound to the soil solid phase that can diffuse towards solution that equilibrates with time Pi in solution under the effect of a gradient of concentration. Soil analyses were performed in batch experiment on soil suspensions using a 32Pi-dilution method at steady-state. The modeling considered the difference between P inputs minus P outputs. This annual P budget was partitioned between Cp and Pr for one year. Every year the P budget was calculated as the added P to soil minus the P removed in grain yields and the P that leaves the plough layer by leaching estimated as the simulated Cp value multiplied by the annual volume of drainage water. Other fluxes that can play a role in P cycling such as atmospheric deposit, preferential, subsurface and surface flows were neglected. We analyzed archived soil samples, taken up every 3-4 years from a long-term field experiment (1972-2000) on a sandy soil under temperate climate. It comprised 4 replicates and 3 annual rates of P application as commercial superphosphate: 0, 44 and 96 kg Pha-1 yr-1. The crop was a monoculture of irrigated-maize. Grain yields and their P content were determined every year for all plots. The overall corn grain yield over almost 3 decades was: 11.6 t ha-1 yr-1 (mean P content of grain = 3.0 g P kg¬-1). The starting Cp value in 1972 was 1.31 mg P L. At the end of the experiment, the measured Cp values ranged from 0.44 to 3.86 mg P L-1 due to the cumulative P budget which varied between -825 to +1400 kg-1 ha-1 including the calculated leached P beyond the plough layer (from -129 to -384 kg P ha-1). Experimental Pr values vs. Cp and time were highly and closely (r2=0.94; n=108) fitted by a single kinetic Freundlich equation, irrespective of the year of sampling. This equation was used to calculate Pr value after one year. To test the predictive capability of the model, we compared the simulated Cp values by the model to the field-observed Cp values. The model reproduced the most important patterns of the fate of soil P for the different P fertilization treatments. Simulated Cp values were not significantly different from the field-observed Cp values for the 0 and 44 kg P ha-1 yr-1 treatments, but some discrepancies were observed for the 96 kg P ha-1 yr-1 treatment. The next step in the generalization of our results would be to test the model performance in other field conditions. This investigation highlights the importance of long-term field experiments with archived soil samples and complete database on plant biomass for understanding P cycling and soil P dynamics.

The effect of copper-amended fertiliser and copper oxide wire particles on the copper status of farmed red deer (Cervus elaphus) and their progeny.

PubMed

Grace, N D; Wilson, P R; Quinn, A K

2005-02-01

To determine changes in serum and liver copper concentrations in postnatal, weaner, yearling, and mature deer after grazing pasture topdressed with copper (Cu) at two rates of application of copper sulphate (CuSO4(.)5H2O), and following oral administration of copper oxide (CuO) wire particles to some of the deer. In mid-March 2000 (Year 1), 1.1-ha paddocks (two/treatment) of ryegrass/white clover pasture received either 0 (Control), 6 (Low) or 12 (High) kg CuSO4(.)5H2O /ha applied with 250 kg potash superphosphate/ha. They were grazed by 4-month-old red deer hinds (n=11/treatment) from mid-April 2000 until early March 2001. In mid-March 2001 (Year 2), the pastures were topdressed again as for Year 1, and the original hinds, now yearlings which had grazed as a single group between studies, were returned to their respective treatments in mid-April 2001 and remained on the trial until mid-March 2002. They were mated during April/May. The pastures were also grazed by pregnant mature hinds (n=8/treatment) from mid-May 2001. As the Cu status (i.e. liver Cu concentration) of the yearling hinds on the pasture treated with 6 kg CuSO4(.)5H2O/ha was not significantly different from the untreated animals, in late July 2001 the yearling and mature deer on this treatment were treated orally with 10 g CuO wire particles. The mature hinds calved in November and the yearling hinds in December. Pasture samples were collected at about monthly intervals to determine concentrations of Cu and other minerals. In Year 1, liver biopsies and blood samples were collected at 4-6-weekly intervals for determination of Cu concentrations. In Year 2, samples were collected similarly at 6-12-weekly intervals. Liver biopsies and blood were also collected from progeny, along with milk from their dams. Liveweights were determined at 3-7-monthly intervals, as well as data on calving/mortality rates. Pasture Cu concentrations before the application of CuSO4(.)5H2O were 6-9 mg Cu/kg dry matter (DM) and remained at this level in the untreated Control paddocks throughout the study. In Year 1, 28 days after treatment, pasture Cu concentration was 25 and 35 mg Cu/kg DM for the Low and High treatments, respectively; while at the same time for the same treatments in Year 2 it was 20 and 60 mg/kg DM, respectively. A second 60 mg Cu/kg DM peak also occurred on Day 85 in Year 2 with the High treatment. The pasture Cu concentration returned to 6-9 mg/kg DM, and there were no differences between treatments at Days 80 and 150 in Years 1 and 2, respectively. In Years 1 and 2, the Low treatment had no significant effect on the Cu status of the weaner and yearling hinds, respectively, when compared with that of animals grazing the untreated Control pastures. Weaner (Year 1) and yearling (Year 2) deer on the High treatment had significantly higher mean serum and liver Cu concentrations in the late winter and spring period when compared with those on untreated Control pastures. CuO wire particles increased the mean serum Cu concentration at Days 60 and 180, and liver Cu concentration at Day 60, in yearling hinds. A similar effect was observed in mature hinds. Regardless of Cu treatment, the liver Cu concentration of the 1-4-week-old progeny was markedly greater (p<0.001) than that of their dams, and then decreased significantly until weaning in March. In progeny of treated yearling hinds, but not mature hinds, serum and liver Cu concentrations were significantly higher (p=0.013) than progeny of untreated dams. Topdressing pastures with CuSO4(.)5H2O at a rate of 12 kg/ha, but not 6 kg/ha, in mid-March was effective in increasing the Cu status of weanling hinds; while pastures topdressed with 12 kg CuSO4(.)5H2O /ha in mid-March and dosing hinds with 10 g CuO in late July were effective in increasing the Cu status of pregnant hinds, and in the case of the yearling hinds, significantly improved the Cu status of their progeny from birth to weaning.

Climate Change: Precipitation and Plant Nutrition Interactions on Potato (Solanum tuberosum L.) Yield in North-Eastern Hungary

NASA Astrophysics Data System (ADS)

László Phd, M., ,, Dr.

2009-04-01

It is widely well known that annual temperatures over Europe warm at a rate of between 0.1 0C decade-1 and 0.4 0C decade-1. And most of Europe gets wetter in the winter season between +1% and +4% decade-1. In summer there is a strong gradient of change between northern Europe (wetting of up to +2% decade-1) and southern Europe (drying of up to 5% decade-1). The droughts and the floods were experienced at Hungary in the early eighties as well as today. So among the natural catastrophes, drought and flooding caused by over-abundant rainfall cause the greatest problems in field potato production. The crop is demanding indicator plant of climate factors (temperature, rainfall) and soil nitrogen, phosphorus, potassium and magnesium status. This publication gives the results achieved in the period from 1962 to 2001 of a long term small- plot fertilization experiment set up on acidic sandy brown forest soil at Nyírlugos in the Nyírség region in North-Eastern Hungary. Characteristics of the experiment soil were a pH (KCl) 4.5, humus 0.5%, CEC 5-10 mgeq 100g-1 in the ploughed layer. The topsoil was poor in all four macronutrient N, P, K and Mg. The mineral fertilization experiment involved 2 (genotypes: Gülbaba and Aranyalma) x 2 (ploughed depths: 20 and 40 cm) x 16 (fertilizations: N, P, K, Mg) = 64 treatments in 8 replications, giving a total of 512 plots. The gross and net plot sizes were 10x5=50 m2 and 35.5 m2. The experimental designe was split-split-plot. The N levels were 0, 50, 100, 150 kg ha-1 year-1 and the P, K, Mg levels were 48, 150, 30 kg ha-1 year-1 P2O5, K2O, MgO in the form of 25% calcium ammonium nitrate, 18% superphosphate, 40% potassium chloride, and powdered technological magnesium sulphate. The forecrop every second year was rye. The groundwater level was at a depth of 2-3 m. From the 64 treatments, eight replications, altogether 512- experimental plots with 7 treatments and their 16 combinations are summarised of experiment period from 1962 to 1979. The main conclusions were as follows: 1. The experiment years (1962-1963, 1964-1965, 1966-1967, 1968-1969, 1970-1971, 1972-1973, 1974-1975, 1976-1977, 1978-1979) were characterised by frequent extremes of climate. Seven years had an average rainfall, one year had an over rainfall and one year had a very dry by Hungarian traditional and RISSAC-HAS (Márton 2001b) new potato ecological standards. 2. The unfavorable effects of climate anomalies (drought, over-abundance of water in the topsoil) on the yield formation, yield quantity of potato depended decisively on the time of year when they were experienced and the period for which they lasted. 3. Precipitation deficiency (droughts) in the winter could not be counterbalanced by average rainfall during the vegetation period, and its effect on the yield was similar to that of summer drought. 4. Yield was influenced by rainfall to a greater extent than by 0-150 kg ha-1 nitrogen and NP, NK, NPK, NPKMg combinations. 5. Drought and over rainfall negative effects were decreased by increasing N- doses and its combinations of potassium, phosphorous and magnesium from 13 to 32%. 6. It was found the polynomial correlation between rainfall and yield could be observed in the case of N: Y'=380.18-2.95x+0.0056x2, n=72, R2=0.95, NP: Y'=387.19-3.04x+0.0059x2, n=72, R2=0.96, NK: Y'=381.65-2.95x+0.0056x2, n=72, R2=0.95, NPK: Y'=390.87-3.07x+0.0060x2, n=72, R2=0.96 and NPKMg: Y'=390.45-3.06x+0.0059x2, n=72, R2=0.96 nutrition systems. The optimum yields ranges between 17-20 t ha-1 at 280-330 mm of rainfall. Key words: climate change, rainfall, potato, N, NP, NK, NPK, NPKMg, yield Introduction: Climate change was recognized as a serious environmental issue. The build up of greenhouse gases in the atmosphere and the inertia in trends in emissions means that we can expect significant changes for at least the next few decades and probably for the future time. Annual temperatures over Europe warm at a rate of between 0.1 0C decade-1 and 0.4 0C decade-1. And most of Europe gets wetter in the winter season between +1% and +4% decade-1. In summer there is a strong gradient of change between northern Europe (wetting of up to +2% decade-1) and southern Europe (drying of up to 5% decade-1). The urgent need is to understand what might be involved in adapting to the new climates. And we must increasingly get the following question: how do we respond effectivelly to prevent damaging impacts and take advantage of new climatic opportunities. This question requires detailed in information regarding expected impacts and effectíve adaptive measures. Climate change at Hungary was initiated about of 1850 (Márton 2001b). Nowadays among the natural catastrophes, drought and flooding caused by over-abundant rainfall and cause the greatest problems in field crop production in this region (László et al. 2000a, Márton et al. 2000). The droughts and the floods were experienced in the early eighties as well as today have drawn renewed attention to the analysis of this problem (László 2001, Márton 2001a, Márton 2001c). Potatoes are one of the most important crops in the agricultural systems of many World countries but little research in the field of climate change impact assessment has been undertaken. Potatoes are sensitives to the prevailing weather conditions (precipitation) and, hence, it is important to evaluate the effects of anthropogenic climate change on their production. The crop is demanding indicator plant of soil nutrient status too. Has a particularly high requirement for supply of soil nitrogen, phosphorus, potassium and magnesium (Láng 1973, Szemes és Kádár 1990, Kádár és Szemes 1994, Johnston 2000, Kádár et al. 2000, László 2000, László et al. 2000b, 2000c, Márton 2000a, 2000b). The tubers remove 1.5 times as much potassium as nitrogen and 4 or 5 times the amount of phophate. This paper describes climate change, mainly precipitation and N, NP, NK, NPK and NPKMg effects on potato yield on a acidic sandy brown forest soil at long term field experiment scale under North- Eastern Hungarian climate conditions at Nyírlugos from 1962 to 1979. Material and Method: Effects of climate changes, especially rainfall quantity and distribution on certain crop fertilization factors (N, P, K, Mg and potato yield) were studied in a long-term field experiment on acidic sandy brown forest soil at Nyírlugos in North- Eastern Hungary set up in 1962 and 2001. Ploughed layer of the experiment soil had a pH (KCl) 4.5, humus 0.5%, CEC 5-10 mgeq 100g-1. The topsoil was poor in all four macronutrient N, P, K and Mg. The mineral fertilization experiment involved 2 (Gülbaba and Aranyalma genotypes) x 2 (20 and 40 cm ploughed depths) x 16 (N, P, K, Mg fertilizations) = 64 treatments in 8 replications, giving a total of 512 plots. The gross and net plot sizes were 10x5=50 m2 and 35.5 m2. The experimental designe was split-split-plot. The N levels were 0, 50, 100, 150 kg ha-1 year-1 and the P, K, Mg levels were 48, 150, 30 kg ha-1 year-1 P2O5, K2O, MgO in the form of 25% calcium ammonium nitrate, 18% superphosphate, 40% potassium chloride, and powdered technological magnesium sulphate. The forecrop every second year was rye. The groundwater level was at a depth of 2-3 m. Ecological and experimental dates were estimated by Hungarian traditional, RISSAC-HAS (Márton 2001b) new potato standards and MANOVA. From the 64 treatments, eight replications, altogether 512- experimental plots with 7 treatments and their 16 combinations are summarised of experiment period from 1962 to 1979. Results and Discussion: The experiment years (1962-1963, 1964-1965, 1966-1967, 1968-1969, 1970-1971, 1972-1973, 1974-1975, 1976-1977, 1978-1979) were characterised by frequent extremes of climate. Seven years had an average rainfall, one year had an over rainfall and one year had a very dry. The unfavorable effects of climate anomalies (drought, over-abundance of water in the topsoil) on the yield formation, yield quantity of potato depended decisively on the time of year when they were experienced and the period for which they lasted. Droughts in the winter or summer half-year had much the same effect on yield. Precipitation deficiency in the winter could not be counterbalanced by average rainfall during the vegetation period, and its effect on the yield was similar to that of summer drought. It was also concluded that economic yields could not be achieved with poor N, P, K and Mg nutrient supply even with a normal quantity and distribution of rainfall. Yield was influenced by rainfall to a greater extent (Table 4) than by 0-150 kg ha-1 nitrogen and NP, NK, NPK, NPKMg combinations. Drought and over rainfall negative effects were decreased by increasing N- doses with combinations of potassium, phosphorous and magnesium from 13 to 32% (Table 5). And with the help of regression analysis it was found the polynomial correlation between rainfall and yield could be observed in the case of N: Y'=380.18-2.95x+0.0056x2, n=72, R2=0.95, NP: Y'=387.19-3.04x+0.0059x2, n=72, R2=0.96, NK: Y'=381.65-2.95x+0.0056x2, n=72, R2=0.95, NPK: Y'=390.87-3.07x+0.0060x2, n=72, R2=0.96 and NPKMg: Y'=390.45-3.06x+0.0059x2, n=72, R2=0.96 nutrition systems. The optimum yields ranges between 17-20 t ha-1 at 280-330 mm of rainfall. Acknowledgement: This study were supported by Research Institute for Soil Science and Agricultural Chemistry of the Hungarian Academy of Sciences (RISSAC-HAS), Budapest. References Johnston, A. E., 2000. Some aspects of nitrogen use efficiency in arable agriculture. K. Scogs-o. Lantbr. Akad. Tidskr. 139, 8. Kádár, I., Márton, L., Horváth, S., 2000. Mineral fertilisation of potato (Solanum tuberosum L.) on calcareous chernozem soil. Plant Production. 49, 291-306. Kádár, I., Szemes, I., 1994. A nyírlugosi tartamkísérlet 30 éve. MTA TAKI, Budapest, 248 p. Láng, I., 1973. Műtrágyázási tartamkísérletek homoktalajon. MTA Doktori értekezés. MTA TMB. Budapest László, M., 2000. Nutrition of potato (Solanum tuberosum L.) on Hungary on a chernozem soil. Acta Agronomica Óváriensis. 42, 81-93. László, M., 2001. Year and N- fertilizer effect on winter rye (Secale cereale L.) yield in a long term field experiment. XLIII. Georgikon Days. University of Veszprém. Keszthely László, M., Imre, K., Jose, E. M., 2000a. Effects of Crotalaria juncea L. and Crotalaria spectabilis ROTH. on soil fertility and soil conservation in Hungary. Acta Agronomica Óváriensis. In press László, M., Silva, J. B. C., José, A. B., 2000b. Ecological friendly dragée technics on different crops and vegetables seeds. Acta Agronomica Óváriensis. In press László, M., Silva, J. B. C., Jose, A. B., 2000c. Ecological friendly dragée technics to sustainable precision agriculture. Fertilization in the Third Millenium. CASISCF. Beijing Márton, L., 2000a. Effects of NPK fertilizers on potato (Solanum tuberosum L.) yield. Doctoral Ph.D Dissertation. University of Veszprém, Keszthely. Márton, L., 2000b. Effects of NPK fertilizers on potato (Solanum tuberosum L.) yield. Doctoral Ph.D Thesis. University of Veszprém, Keszthely. Márton, L., 2001a. Climate change and N, P, K, Mg fertilization effect analysis at Tisza-river basin in a long term field experiment. Szent István University, Gödöllő, 21. p. Márton, L., 2001b. Climate change effets on rye (Secale cereale L.) yield. Agrochemistry and Soil Science. In press Márton, L., 2001c. Climate change and fertilization effect analysis at the Tisza- river basin on rye yield. SZINET. University of Szent István. Gödöllő. Márton, L., Kádár, I., Estáquio, M. J., 2000. Effects of Crotalaria juncea L. and Crotalaria spectabilis ROTH on soil fertility and soil conservation. ESSC. Man and Soil at the Third Millennium. Abstract Book. 195. Valencia Szemes, I., Kádár, I., 1990. Műtrágyázás és meszezés tartamhatásának vizsgálata savanyú homoktalajon. Növénytermelés. 39: 147-155.

Climate Change and Potassium Effects Under Different N-Fertilization Input on Potato (Solanum tuberosum L.) Yield in a Long Term Field Experiment

NASA Astrophysics Data System (ADS)

László, Márton, ,, Dr.

2010-05-01

Climate change of Hungary was initiated about of 1850. Nowadays among the natural catastrophes, drought and flooding caused by over-abundant rainfall cause the greatest problems in field crop production. The droughts and the floods were experienced in the early eighties as well as today have drawn renewed attention to the analysis of this problem. The potato is demanding indicator crop of climate factors (temperature, rainfall) and soil nutrient status. Has a particularly high requirement for quantity of precipitation and for supply of soil potassium, nitrogen, phosphorus and magnesium. This paper reports the results achieved in the period from 1962 to 2001 of a long term small- plot fertilization experiment set up on acidic sandy brown forest soil at Nyírlugos in the Nyírség region in North- Eastern Hungary. Characteristics of the experiment soil were a pH (KCl) 4.5, humus 0.5%, CEC 5-10 mgeq 100g-1 in the ploughed layer. The topsoil was poor in all four macronutrient N, P, K and Mg. The mineral fertilization experiment involved 2 (genotype: Gülbaba and Aranyalma) x 2 (ploughed depth: 20 and 40 cm) x 16 (fertilizations: N, P, K, Mg) = 64 treatments in 8 replications, giving a total of 512 plots. The gross and net plot sizes were 10x5=50 m2 and 35.5 m2. The experimental designe was split-split-plot. The N levels were 0, 50, 100, 150 kg ha-1 year-1 and the P, K, Mg levels were 48, 150, 30 kg ha-1 year-1 P2O5, K2O, MgO in the form of 25% calcium ammonium nitrate, 18% superphosphate, 40% potassium chloride, and technological powdered magnesium sulphate. The forecrop every second year was rye. The groundwater level was at a depth of 2-3 m. From the 64 treatments, eight replications, altogether 512- experimental plots with 7 treatments and their 16 combinations are summarised of experiment period from 1962 to 1979. The main conclusions were as follows: 1. The experiment years (1962-1963, 1964-1965, 1966-1967, 1968-1969, 1970-1971, 1972-1973, 1974-1975, 1976-1977, 1978-1979) were characterised by frequent extremes of climate. Seven years had an average rainfall, one year had an over rainfall and one year had a very dry by Hungarian traditional and RISSAC-HAS new ecological standards. 2. The unfavorable effects of climate anomalies (drought, over-abundance of water in the topsoil) on the yield formation, yield quantity of potato depended decisively on the time of year when they were experienced and the period for which they lasted. 3. Droughts in the winter or summer half-year had much the same effect on yield. Precipitation deficiency in the winter could not be counterbalanced by average rainfall during the vegetation period, and its effect on the yield was similar to that of summer drought. 4. In vegetation periods poor in rainfall yield safety in potato can not be secured by 150 kg ha-1 potassium fertilization. It was also concluded that economic yields could not be achieved with poor N, P, K and Mg nutrient supply even with a normal quantity and distribution of rainfall. 5. Yield was influenced by rainfall to a greater extent than by 150 kg ha-1 potassium combinations (NK, NPK, NPKMg). 6. Drought and over rainfall negative effects were decreased by increasing N- doses and its combinations of potassium, phosphorous and magnesium from 13 to 32%. 7. With the help of regression analysis it was found the polynomial correlation between rainfall and yield could be observed in the case of NK (Y'=381.65-2.95x+0.0056x2, n=72, R2=0.95), NPK (Y'=390.87-3.07x+0.0060x2, n=72, R2=0.96) and NPKMg (Y'=390.45-3.06x+0.0059x2, n=72, R2=0.96) nutrition systems. The optimum yield ranges between 17-20 t ha-1 at 280-330 mm of rainfall. Key words: climate change, rainfall, potassium, potato, yield INTRODUCTION Climate change is now recognized as a serious environmental issue. The build up of greenhouse gases in the atmosphere and the inertia in trends in emissions means that we can expect significant changes for at least the next few decades and probably for the rest of this century. The urgent need is to understand what might be involved in adapting to the new climates. A decade ago, research asked the "what if " question. For example, what will be the impact if climate changes. Now, we must increasingly address the following question: how do we respond effectivelly to prevent damaging impacts and take advantage of new climatic opportunities. This question requires detailed in information regarding expected impacts and effectíve adaptive measures. Information on adaptation is required for the range of stakeholders concerned with agriculture- from the farmers and producers, to processors, supermarkets and consumers and for government and landscape planners. Not only the local effects and options, but also the spatial implications must be understood. Will yields be maintained on the present range of farms. Where will new crops be grown. Will new processing plants be required. Will there be competition for water. Climate change at Hungary was initiated about of 1850 (Márton 2001b). Nowadays among the natural catastrophes, drought and flooding caused by over-abundant rainfall cause the greatest problems in field crop production (László et al. 2000a, Márton et al. 2000). The droughts and the floods were experienced in the early eighties as well as today have drawn renewed attention to the analysis of this problem (László 2001a, László 2001b, Márton 2001a, Márton 2001c). Most recent agricultural impact studies have concentrated on the effects of mean changes in climate on crop production, whilst only limited investigations into the effects of climate variability on agriculture have been undertaken. The paucity of studies in this area is not least due to the considerable uncertainty regarding how climate variability may change in the future in response to greenhouse gas induced warming but also as a result of the uncertainty in the response of agricultural crops to changes in climate variability, effected most probably through changes in the frequency of extreme climatic events. Showed that changes in variance have a greater effect on the frequency of extreme climatic events than do changes in the mean values. Hence, it is important to attempt to include changes in variability in scenarios of climate change. Potatoes are one of the most important crops in the agricultural systems of many World countries but little research in the field of climate change impact assessment has been undertaken. Potatoes are sensitives to the prevailing weather conditions (precipitation) and, hence, it is important to evaluate the effects of anthropogenic climate change on their production. The crop is demanding indicator plant of soil nutrient status too. Has a particularly high requirement for supply of soil potassium, nitrogen, phosphorus and magnesium (Johnston 2000, Kádár et al. 2000, László 2000, László et al. 2000b, 2000c, Márton 2000a, 2000b). The tubers remove 1.5 times as much potassium as nitrogen and 4 or 5 times the amount of phophate. This paper describes climate change and mainly potassium effects on potato yield on a acidic sandy brown forest soil at long term experiment scale under Mediterranean climate conditions at North- Eastern Hungary from 1962 to 1979. MATERIAL AND METHOD The effect of climatic factors, especially rainfall quantity and distribution on certain crop fertilization factors (K, N, P, Mg and potato yield) were studied in a long-term field experiment on acidic sandy brown forest soil at Nyírlugos in North- Eastern Hungary set up in 1962 and 2001. Ploughed layer of the experiment soil had a pH (KCl) 4.5, humus 0.5%, CEC 5-10 mgeq 100g-1. The topsoil was poor in all four macronutrient N, P, K and Mg. The mineral fertilization experiment involved 2 (Gülbaba and Aranyalma genotypes) x 2 (20 and 40 cm ploughed depths) x 16 (N, P, K, Mg fertilizations) = 64 treatments in 8 replications, giving a total of 512 plots. The gross and net plot sizes were 10x5=50 m2 and 35.5 m2. The experimental designe was split-split-plot. The N levels were 0, 50, 100, 150 kg ha-1 year-1 and the P, K, Mg levels were 48, 150, 30 kg ha-1 year-1 P2O5, K2O, MgO in the form of 25% calcium ammonium nitrate, 18% superphosphate, 40% potassium chloride, and technological powdered magnesium sulphate. The forecrop every second year was rye. The groundwater level was at a depth of 2-3 m. Ecological and experimental dates were estimated by Hungarian traditional, RISSAC-HAS new standards and MANOVA. From the 64 treatments, eight replications, altogether 512- experimental plots with 7 treatments and their 16 combinations (Table 1) are summarised of experiment period from 1962 to 1979. Table 1. Experimental N, P, K, Mg treatments and combinations (Nyírlugos, 1962-1979) Treatments (kg ha-1 year-1) Control N1 = 50 P = 48 (P2O5) N2 = 100 K = 150 (K2O) N3 = 150 Mg = 30 (MgO) N, P, K, Mg combinations Control N1 N2 N3 N1P N2P N3P N1K N2K N3K N1PK N2PK N3PK N1PKMg N2PKMg N3PKMg RESULTS AND DISCUSSION The experiment years (1962-1963, 1964-1965, 1966-1967, 1968-1969, 1970-1971, 1972-1973, 1974-1975, 1976-1977, 1978-1979) were characterised by frequent extremes of climate (Table 2). Seven years had an average rainfall, one year had an over rainfall and one year had a very dry (Table 3). The unfavorable effects of climate anomalies (drought, over-abundance of water in the topsoil) on the yield formation, yield quantity of potato depended decisively on the time of year when they were experienced and the period for which they lasted. Droughts in the winter or summer half-year had much the same effect on yield. Precipitation deficiency in the winter could not be counterbalanced by average rainfall during the vegetation period, and its effect on the yield was similar to that of summer drought. In vegetation periods poor in rainfall yield safety in potato can not be secured by 150 kg ha-1 potassium fertilization. It was also concluded that economic yields could not be achieved with poor N, P, K and Mg nutrient supply even with a normal quantity and distribution of rainfall. Yield was influenced by rainfall to a greater extent (Table 4) than by 150 kg ha-1 potassium combinations (NK, NPK, NPKMg). Drought and over rainfall negative effects were decreased by increasing N- doses with combinations of potassium, phosphorous and magnesium from 13 to 32% (Table 5 and 6). With the help of regression analysis it was found the polynomial correlation between rainfall and yield could be observed in the case of NK (Y'=381.65-2.95x+0.0056x2, n=72, R2=0.95), NPK (Y'=390.87-3.07x+0.0060x2, n=72, R2=0.96) and NPKMg (Y'=390.45-3.06x+0.0059x2, n=72, R2=0.96) nutrition systems. The optimum yield ranges between 17-20 t ha-1 at 280-330 mm of rainfall. From 1962 to 1979 the weather was highly variable, with particularly frequent droughts and over rainfall resulting in yield losses of 13 to 32 percentin in this period. Thus it is important to analyse the consequences of possible future climate change on crop in Hungary. REFERENCES A.E. Johnston. 2000. Some aspects of nitrogen use efficiency in arable agriculture. K. Scogs-o. Lantbr. Akad. Tidskr. 139: 8. Kádár, I-Márton, L.-Horváth, S. 2000. Mineral fertilisation of potato (Solanum tuberosum L.) on calcareous chernozem soil. Plant Production. 49: 291-306. László, M. 2000. Nutrition of potato (Solanum tuberosum L.) on Hungary on a chernozem soil. Acta Agronomica Óváriensis. 42: 81-93. László, M. 2001a. Climate change and N, P, K, Mg fertilization effects on potato (Solanum tuberosum L.) yield and quality. EAPR. Hamburg. In press László, M. 2001b. Year and N- fertilizer effect on winter rye (Secale cereale L.) yield in a long term field experiment. XLIII. Georgikon Days. University of Veszprém. Keszthely László, M.-Imre, K.-Jose, E.M. 2000a. Effects of Crotalaria juncea L. and Crotalaria spectabilis ROTH. on soil fertility and soil conservation in Hungary. Acta Agronomica Óváriensis. 42: 99-106. László, M.-Silva, J.B.C.-José, A.B. 2000b. Ecological friendly dragée technics on different crops and vegetables seeds. Acta Agronomica Óváriensis. 42: 107-111. László, M.-Silva, J.B.C.-Jose, A.B. 2000c. Ecological friendly dragée technics to sustainable precision agriculture. Fertilization in the Third Millenium. CASISCF. Beijing Márton, L. 2000a. Effects of NPK fertilizers on potato (Solanum tuberosum L.) yield. Doctoral Ph.D Dissertation. University of Veszprém, Keszthely. Márton, L. 2000b. Effects of NPK fertilizers on potato (Solanum tuberosum L.) yield. Doctoral Ph.D Thesis. University of Veszprém, Keszthely. Márton L. 2001a. Climate change and N, P, K, Mg fertilization effect analysis at Tisza- river basin in a long term field experiment. Szent István University, Gödöllő, 21. p. Márton, L. 2001b. Climete change effets on rye (Secale cereale L.) yield. Agrochemistry and Soil Science. Budapest. In press. Márton, L. 2001c. Climate change and fertilization effect analysis at the Tisza- river basin on rye yield. SZINET. University of Szent István. Gödöllő. Márton, L.-Kádár, I.-Estáquio M.J. 2000. Effects of Crotalaria juncea L. and Crotalaria spectabilis ROTH on soil fertility and soil conservation. ESSC. Man and Soil at the Third Millennium. Abstract Book. 195. Valencia ACKNOWLEDGEMENT This study were supported by Research Institute for Soil Science and Agricultural Chemistry of the Hungarian Academy of Sciences (RISSAC-HAS) Address of author: László M., Research Institute for Soil Science and Agricultural Chemistry of the Hungarian Academy of Sciences, H-1022 Budapest, II. Herman O. u. 15., E-mail:marton@gw.rissac.hu

Liming and Fertilization Effects on Triticale (XTriticosecale W.) Yield Between 1999 and 2006

NASA Astrophysics Data System (ADS)

László Phd, M., ,, Dr.

2009-04-01

Precipitation amount, distribution and nitrogen (N)-, phosphorus (P2O5)-, potassium (K2O)-, calcium (CaO)-, and magnesium (MgO) fertilization interaction effects were studied on a sandy acidic lessivated brown forest soil; WRB: Haplic Luvisol in the 44 year old Nyírlugos Field Trial (NYFT) in a Hungarian fragile agro-ecosystem in Nyírség region (N: 470 41' 60'' and E: 220 2' 80'') on triticale (X Triticosecale W.) yield from 1999 to 2006. At the trial set up in 1962, the soil had the following agrochemical properties: pH (H2O) 5.9, pH (KCl) 4.7, hydrolytic acidity 8.4, hy1 0.3, humus 0.7%, total N 34 mg kg-1, ammonlactate (AL) soluble-P2O5 43 mg kg-1, AL-K2O 60 mg kg-1 in the plowed (0-25 cm) layer. From 1980 to 2006, the experiment consisted of 32x4=128 plots in randomised block design. The gross plot size was 10x5=50 m2. The average fertilizer rates in kg ha-1 year-1 were nitrogen 75, phosphorus 90 (P2O5), potassium 90 (K2O), calcium 437.5 (CaCO3) and magnesium 140 (MgCO3). The groundwater table has had at a depth of 2-3 m below the surface. The main results are as follows. During drought conditions the respective yield of the control areas was -25% less than for average years. The application of N alone, or of NP and NK treatments, led to yield reduction of -19.7%, while that of NPK, NPKCa, NPKMg or NPKCaMg caused an -28.3% drop during these types of years. In the wet years, the yield decreased by -22.2% on the unfertilized soils; in the case of N, NP, or NK nutrition with an -14.1%; and increased at 13.8% on NPK, NPKCa, NPKMg and NPKCaMg treated plots. In the very wettest year, the yields were dropped -43.1% on control soils, -39.3% of N, NP, or NK loadings and -35.8% on NPK, NPKCa, NPKMg and NPKCaMg treatments to those in the average year. The relationships between rainfall quantitiy during the vegetation period N, P, K, Ca and Mg nutrition and yield were characterised by polynomial correlations (control: R= 0.7212***, N: R = 0.7410***, NP: R = 0.6452***, NK: R = 0.6998***, NPK: R = 0.5555***, NPKCa: R = 0.5578***, NPKMg: R = 0.4869**, NPKCaMg: R = 0.4341**). However, the total regression coefficients ranged from 0.43 to 0.74 in depence on the different nutrient application. Maximum yields of 5.8-6.0 t . ha-1 were achieved in the rainfall range of 580-620 mm. At values above and below this domain of the precipitation the grain yield reduced quadratically. So, it can be stated that both, drought and excess rainfall conditions resulted dramatically in significant negative effects between fertilization (N, P, K, Ca, Mg) and triticale yield. Keywords: precipitation, fertilization, liming, triticale, yield Introduction: The hazards associated with climate change are depend on the interaction of several systems with many variables (Johnston, 2000). Accummulation of carbon dioxide, methane, water vapor, ozone, nitrous oxide, sulfur hexafluoride, hydrofluorocarbons, perfluorocarbons, chlorofluorocarbons (build-up of greenhouse gases) in the atmosphere and trends in their emissions suggest that we can expect significant environmental changes in the 21th century (Cynthia and Ana, 2006; Eric 2006). However, a recent consensus has emerged that between the greenhouse gases rising of atmospheric concentrations of carbon dioxide could become the more dangerous bacause it causing the global warming (Láng, 2005). Today, most researchers believe that higher temperature, drought and rainfall excess caused by climate change will depress crop yields in many places in the coming decades (Kádár et al., 2000; Jolánkai, 2005). Thus, in the last decades many agricultural investigations focused on understanding the relation between mean climate change and crop production (Runge, 1968; Várallyay, 1992). Changes in weather patterns were observed thoughout Europe including Hungary as early as 1850. Among the natural consequences of changing weather patterns, years of drought (rainfall deficit) and wet (rainfall excess) conditions, resulted in problems among plant nutrition and field crop production (EU, 2003). Triticale (Kádár et al., 1999; Márton, 2002) is a crop of worldwide importance, limited research exists about the effects of climate change on these crop. The crop is sensitive to the prevailing weather conditions (such as rainfall) and, for this reason, understanding the effects of anthropogenic climate change on it's production is important (Márton, 2006). In addition to growing season triticale conditions (e.g., soil agrochemical properties, fertilization, liming) affect the growth and yield of crop (Lobell and Asner, 2003) and cause yield variations. Understanding the fertilization, liming and rainfall effects have been a continuous endeavor toward improving farming technology and management strategy to reduce the negative impacts of fertilization, liming and rainfall and to increase crop yield (Kádár and Szemes 1994; Várallyay 1994; among others). Our main objective of this research it was study and clarify the precipitation amount and distribution and nitrogen (N)-, phosphorus (P2O5)-, potassium (K2O)-, calcium (CaO)-, and magnesium (MgO) fertilization interaction effects on a sandy acidic lessivated brown forest soil; WRB: Haplic Luvisol in the 44 year old Nyírlugos field trial in a Hungarian fragile agro-ecosystem in Nyírség region on triticale (X Triticosecale W.) yield from 1999 to 2006. Furthermore, it was our intent to emphasize that the net effect of multiple environmental changes is far more important than the effect of a single factor on the crop. Materials and Methods: The net-influence of rainfall (quantity, distribution) and mineral fertilization (N, P2O5, K2O, CaO, MgO) were studied in a long term field experiment established at the Research Institute for Soil Science and Agricultural Chemistry of the Hungarian Academy of Sciences Experiment Station (RISSAC-HAS ET) in Hungary on a Haplic Luvisol (sandy acidic lessivated brown forest soil) with triticale (X Triticosecale W.) indicator crop under fragile agro-ecological circumstances at Nyírlugos for 8 years from 1999 to 2006. The main experiment's soil agrochemical characteristics in the plowed (0-25 cm) layer are presented in Table 1. at the experimental set up in 1962 (Láng, 1973). From 1980 to 2006 the experiment consisted of 32x4=128 plots in randomized block designs. The gross plot size has been having 10x5=50 m2. The experimental treatments and combinations are shown in Table 2. The fertilizers were applied in the form of 25% calcium ammonium nitrate, 18% superphosphate, 40% potassium chloride, calcium carbonate and magnesium sulphate. The groundwater table has had at a depth of 2-3 m below the surface. The plant samples had had taken by manually at the harvest time. Rainfall amounts (deviation in rainfall from the average over many years: dry year -10 - -20%, drought year -20% over, wet year +10 - +20%, year with excess rainfall +20% over) and other related data determined on traditional Hungarian (Harnos, 1993) and Research Institute for Soil Science and Agricultural Chemistry of the Hungarian Academy of Sciences (Márton, 2004) standards, and MANOVA (Multivariate Analysis of Variance) by SPSS test (SPSS Inc., 2000). Table 1: The main soil agrochemical properties in the plowed (0-25 cm) layer at the experiment set up. (Brown forest soil, acid sand; WRB: Haplic Luvisol, Nyírség region Nyírlugos 1962) Content PH HA* Hy1 Humus Total AL** (H2O) (KCl) nitrogen P2O5 K2O 5.9 4.7 8.4 0.3 % 0.7 mg . kg-1 34 43 60 * Hydrolytic acidity, ** ammoniumlactate (AL) soluble Table 2: Fertilization and liming treatments in the experiments, kg ha-1 year-1 (Brown forest soil, acid sand; WRB: Haplic Luvisol, Nyírség region Nyírlugos) TreatmentLevels Applied kg ha-1 yr-1 N P2O5 K2O CaCO3 MgCO3 0 0 0 0 0 0 1 50 60 60 250 140 2 100 120 120 500 280 3 150 180 180 1000 - Note: In the form of Ca-ammonium-nitrate, Superphosphate, potassium cloride, powdered limestone and dolomite. Results and Discussion: During drought conditions, in conformity with Adams et al. (1995), Rosenzweig and Tubiello (1997) and McMaster (1999) the respective yield of the control areas was -25% less than for average years. The application of N alone, or of NP and NK treatments, led to yield losses of -19.6%, while that of NPK, NPKCa, NPKMg or NPKCaMg caused an -28.3% drop during these types of years. In the wet years, the yield decreased by -22.2% in the unfertilized plots; in the case of N, NP, or NK nutrition with an -14.1%; and increased at 13.8% on NPK, NPKCa, NPKMg and NPKCaMg treatments. In the very wettest year, the yields were dropped -43.1% on control soils, -39.3% of N, NP, or NK loadings and -35.8% on NPK, NPKCa, NPKMg and NPKCaMg treatments to those in the average year, reverse of Asbjorn et al. (2004). The relationships between rainfall quantitiy during the vegetation period N, P, K, Ca and Mg nutrition and yield were characterised by polynomial correlations (control: R= 0.7212***, N: R = 0.7410***, NP: R = 0.6452***, NK: R = 0.6998***, NPK: R = 0.5555***, NPKCa: R = 0.5578***, NPKMg: R = 0.4869**, NPKCaMg: R = 0.4341**). However, the total regression coefficients ranged from 0.43 to 0.74 in depence on the different nutrient application. Maximum yields of 5.8-6.0 t . ha-1 were achieved in the rainfall range of 580-620 mm. At values above and below this range the grain yield reduced quadratically. To sum up we can say climate change will gradually and, at some point, be even abruptly affects Europa and Hungary agriculture. Warming temperatures and a greather incidence and intensity of extreme weather events possible lead to significant reductions in triticale yield. Expanded ranges of crop agrochemicals and altered transmission dynamics of different irrigation solutions might exacarbate these reductions. Since farmers' strategies grow out of experience, they can find that the past will be a less reliable predictor of the future. Acknowledgements: This research was supported by Hungarian Academy of Sciences, H-Budapest and the Hungarian and Spanish Intergovernmental S & T Cooperation Project of E-2/04-OMFB-00112/2005 and Hungarian and Indian Intergovernmental S & T Cooperation Project of IND-3/03/2006. References Adams, R. M., Fleming, R. A., Chang, C. C., McCarl, B. A. and Rosenzweig, C. 1995. A reassessment of the economic effects of global climate change on U.S. agriculture. Climatic Change, Vol. 30, pp. 147-167. Asbjorn, T., Michelle, T. and Bárd, R. 2004. Climate Change Impacts on Agricultural Productivity in Norway. CICERO. Oslo Cynthia, R. & Ana, I. 2006. Potential impact of climate change on world food supply. Data sets from a major crop modeling study. Socioeconomic Data and Applications Center. Columbia University. New York Eric La F. 2006. Adapting crops for climate change. UBC Botanical Garden and Centre for Plant Researches. EU (European Union). 2003. Drought costs EU farmers euro of 11 billion. European Report, Brussels Harnos, Zs. 1993. Weather and weather-yield interaction analysis. (In Hungarian) In: Aszály 1983 (Szerk.: Baráth Cs-né., Győrffy B., Harnos Zs.). KÉE. Budapest Johnston, A. E. 2000. Some aspects of nitrogen use efficiency in arable agriculture. K. Scogs-o. Lantbr. Akad. Tidskr. 139:8. Jolánkai M. 2005. Effect of climate change on plant cultivation. (In Hungarian) In: „AGRO-21" Füzetek. 41. 47-58. Kádár I. - Németh T. - Szemes I. (1999): Triticale trágyareakciója a nyírlugosi tartamkísérletben. Növénytermelés. 48:647-661. Kádár I. - Szemes I. (1994): A nyírlugosi tartamkísérlet 30 éve. MTA Talajtani és Agrokémiai Kutató Intézete. Budapest. Láng I. (1973): Műtrágyázási tartamkísérletek homoktalajokon. Akad. Doktori Disszertáció. Kézirat. MTA. Budapest. Láng I., 2005. Weather and climate change: change-effect-response. (In Hungarian) In: „AGRO-21" Füzetek. 43. 3-10. Márton L. (2002): A csapadék és tápanyagellátottság hatásának vizsgálata a tritikale termésére tartamkísérletben. Növénytermelés. 51:687-701. Márton L. 2004. Rainfall and fertilization effects on crops yield in a global climate change. In: Proc. 4th Agroenviron Symposium. Role of Multipurpose Agriculture in Sustaining Global Environment-AGROENVIRON 2004 (Udine, 20-24 Oct., 2004). Part 3. 451-456. DPVTA. Udine Márton L. 2006. Ecological changes of rainfall and artificial fertilization on crop yield formation. ESA, Memphis, Tenesse McMaster, H. J. 1999. The potential impact of global warming on Hail Losses to winter crops in New South Wales. Climatic Change, Vol. 43, No. 2, October, pp. 455-476. Németh I. 2004. A klímaváltozás és a magyarországi mezőgazdaság. "AGRO-21" Füzetek. "AGRO-21" Kutatási Programiroda. 33:65-69. Németh, T. 2004. MTA Talajtani és Agrokémiai Kutatóintézet (MTA TAKI) tudományos programjának megvalósítására vonatkozó koncepció (2005-2010). Scientific Programme Conception of RISSAC-HAS from 2005 to 2010. MTA TAKI., Budapest Pilar, M.-Arriaga, H.-Salcedo, G.-Márton L.-Pinto, M. 2006. Diet influence on ammonia emission in lactaing dairy cows. NEIKER, Bilbao, Spain Rajendra, K. P. 2004. Foreword. In: Proc. 22nd Session of the Intergovernmental Panel on Climate Change (New Delhi, 9-11 November, 2004). 7-8. IPCC. New Delhi Reilly, J. F. T., McCarl, B., Abler, D., Darwin, R. et al. 2003. U.S. Agriculture and cimate change: New results. Climatic Change, Vol. 57, pp. 43-69. Rosenzweig, C. P., and Parry, M. L. 1994. Potential impact of climate change on world food supply. Nature, 367:133-137. Rosenzweig, C. P., Phillips, J., Goldberg, R., Caroll, J. and Hodges, T. 1996. Potential impacts of climate change on citrus and potato production in the US. Agricultural Systems, Vol. 52, pp. 455-479. Rosenzweig, C. P. and F. N. Tubiello. 1997. Impacts of global climate change on Mediterranean agriculture: Current methodologies and future directions: An introductory essay. Mitigation and Adaptation Strategies for Global Change, Vol. 1, pp. 219-232. RS (Royal Society). 2005. Climate change warming over food production. Web address: http://www.newscientist.com Runge, E. C. 1968. Effect of rainfall and temperature interaction during the growing season on corn yield. Agron. J, 60:503-507. Russell, C. M.-Jennifer, A. B. 1991. Climatic Risk in Crop Production: Models and Management for the Semiarid Tropics and Subtropics. C. A. B. International, Wallingford Semenov, M. A. and Porter, J. R. 1995. Climatic variability and modeling of crop yields. Agric. For Meteorol. 73:265-283. Seth, G. P. & Yeffrey, S. A. 2005. Crops and Environmental Change. Food Product Press. New York-London-Oxford Schulze, R. E., Gregory, A. K. and Richard, P. K. 1993. Global climate change and agricultural productivity in southern Africa. Global Environmental Change, Vol. 3, No. 4, December, pp. 330-349 Smith, W. J. 1920. Agricultural meteorology. The effect of weather on crops. Macmillan Comp., New York. Singh, B., Mustapha, E. M., Pierre A., Christopher, R. B. and Jean, P. T. 1998. Impacts of a Ghg-induced climate change on crop yields: Efects of acceleration in maturation, moisture stress and optimal temperature. Climatic change, Vol. 38, No. 1, January, pp. 51-86. SPSS. 2000. SigmaPlot for Windows. Ver. 3.2, Chicago, III.: SPSS, Inc Szász G. 2005. Climatic instability causing variability in crop output in the Carpathian Basin. (In Hungarian) In: „AGRO-21" Füzetek. 40. 33-69. Tubiello, F. N., Rosenzweig, C., Goldberg, R. A. Jagtap, S. and Jones, J. W. 2002. Effects of climate change on U.S. crop production: Simulation results using two different GCM scenarios. Part I: Wheat, potato, maize and citrus. Climate Research, Vol. 20, pp. 259-270. Uprety, D. C. 1999. Global change series. IARI, New Delhi Vesselin, A., Eitzinger, J., Vesna, C. and Michael, O. 2002. Potential impact of climate change on selected agricultural crops in north-eastern Austria. Global Change Biology. 8:372. Várallyay, Gy. 1992. Globális klímaváltozások hatása a talajra. Effect of Global Climate Change to soil. Magyar Tudomány, 9:1071-1076. Várallyay Gy.: 1994. A nyírlugosi tartamkísérlet talajszelvényeinek leírása és laborvizs-gálati eredményei. In: A nyírlugosi tartamkísérlet 30 éve. 216-226. (Kádár I.- Szemes I.) MTA Talajtani és Agrokémiai Kutató Intézete. Budapest. Várallyay Gy. 2005. Possible pedological effects of climate changes in the Kisalföld. (In Hungarian) In: „AGRO-21" Füzetek. 43. 11-23. Voss, R. E.-Hanway, J. J.-Fuller, W. A. 1970. Influence of soil management and climatic factors on the yield response by corn to N, P and K fertilizer. Agron, J, 62:736-740. Walter, R. 1973. Soil conditions and plant growth. Longman, London Weber, M. and Grant, H. 2003. A regional analysis of climate change impacts on Canadian agriculture, Canadian Public Policy, Vol. 29. No. 2, June, pp. 163-179. Wetherald, R. T.-Manabe, S. 1995. The mechanism of summer dryness induced by greenhouse warming. J. Climate, 8:3096-3108. Wigley, T. M. L. 1999. The science of climate change: Global and U.S. Perspectives. Pew Center on Global Climate Change, 48 pp. Woodruff, C. M., Mudrick, S.E. 1998. Interdecadal variations of annual precipitation in the central United States. Bull. Amer. Meteor. Soc. 79:212-219.

Climate and N-Mineral Fertilization Changes on Triticale (XTriticosecale W.) Yield

NASA Astrophysics Data System (ADS)

László, Márton, ,, Dr.

2010-05-01

Ecological quality has a well established dependence on climate-rainfall changes because the water problems are pressing. There is, therefore, growing concern about the potentially wide ranging risks that climate change would have on these key industries as the nature and extent of anticipated changes have become more evident. It also includes changes in land use and in plant production and their management. These changes are unprecedented in terms of both their rate and their spatial extent. Changes in land use (agrotechnics, soil, cultivation, fertility, quality, protection etc.) and in plant production (plant nutrition-, rotation-, protection-, etc.) are currently the main manifestations. As an interdisciplinary problem it is necessary to study such a complex matter in terms of agricultural production. Generally among natural catastrophes, droughts and floods cause the greatest problems in field crop production. The droughts and the floods that were experienced in Hungary in the early 1980's have drawn renewed attention to the analyses of these problems. New research on climate change-soil-plant systems are focused on yield and yield quality. This paper reports the climate change (rainfall) x soil (acidic sandy brown forest) x mineral N-fertilisation x plant interactions on triticale yields in a long term field experiment set up at Nyírlugos in north-eastern Hungary under temperate climate conditions in 1962. The agrochemical parameters of the soil were as follows: pH (H2O) 5.9, pH (KCl) 4.7, hydrolytic acidity 8.4, hy1 0.3, humus 0.7%, CEC 5-10 mgeq 100*g-1, total N 34 mg*kg-1, AL-P2O5 43 mg*kg-1, AL-K2O 60 mg*kg-1. From 1962 to 1980 the experiment consisted of 2x16x4x4=512 plots and from 1980 of 32x4=128 plots in split-split plot and factorial random block design. The gross plot size was 10x5=50 m2. The average fertiliser rates in kg*ha-1*year-1 were nitrogen 45, phosphorus 24 (P2O5), potassium 40 (K2O), magnesium 7.5 (MgO) until 1980 and nitrogen 75, phosphorus 90 (P2O5), potassium 90 (K2O), calcium 175 (Ca) and magnesium 40 (Mg) after 1980. Nitrogen results are summarised from 1990 to 2001. Main conclusions were as follows: 1. On the basis of "general" (Harnos 1993) and triticale-specific rainfall deficiency values (Márton 2003) the years could be classified as average (1991, 1995, 2000), dry (1993), droughty (1992, 1994, 1996), wet (1997, 1998, 2001) and over wet (1999). 2. In average years the yield of the control plots became stabilised at the 1.4 t*ha-1 level. In the fertilised treatments the highest yield (4.0 t*ha-1) was more than two times the lowest yield (1.9 t*ha-1). N fertilisation resulted in an increase of around 1.0 t*ha-1 in the main yield compared with the control. The triticale yields could only be enhanced economically by full treatment with NPK (3.3 t*ha-1) or NPKCa-, NPKMg-, NPKCaMg (3.9 t*ha-1). 3. Without fertilisation the yield in the dry and drought years was decreased 14% and 36% to that in the average year. In case of the nitrogen treatmets the yield was decreased 45% and 24%. 4. In the wet years on the unfertilised plots the yield declined 14% and in the case of the nitrogen fertilisation the yield no changed than in the average years. In the over wet year the plots yielded similar than in the average years. 5. The relationships between rainfall during the vegetation period, N, P, K, Ca and Mg fertilisation and yield were characterised by second-degree correlation depending on the level of nutrition (R: 0=0.3455**, N=0.2779+, NP=0.4722***, NK=0.3739***, NPK=0.6311***, NPKCa=0.6673***, NPKMg=0.6734***, NPKCaMg=0.6232***). The maximum yield (5.0-6.0 t*ha-1) was yielded at 550-600 mm growth period rainfall. This paper summarises quantified results of triticale research with regarding to interaction effects and relationships between climate (rainfall)-mineral nutrition-crop production changes in Hungary during a long term field experiment to agricultural sustainability. Introduction "Climate Change" are recognized as a serious environmental issues (Johnston, 2000). Presently the build up of greenhouse gases in the atmosphere and the inertia in trends in emissions means that we can expect significant changes for at least the next few decades and probably for the 21th century as well (Márton, 2001a., b). It would badly need to understand what might be involved in adapting to the new climates. A decade ago, researchers asked the "what if" question. For example, what will be the impact if climate changes. Now, we must increasingly address the following question: how do we respond effectivelly to prevent damaging impacts and take advantage of new climatic opportunities. This question requires detailed in information regarding expected impacts and effectíve adaptive measures. Information on adaptation is required for governments, landscape planners, stakeholders, farmers, producers, processors, supermarkets and consumers. Not only the local effects and options, but also the spatial implications must be understood. Will yields be maintained on the present range of farms. Where will new crops be grown. Will new processing plants be required. Will there be competition for water. Most recent agricultural impact studies have concentrated on the effects of mean changes in climate on crop production, whilst only limited investigations into the effects of climate variability on agriculture have been undertaken. The paucity of studies in this area is not least due to the considerable uncertainty regarding how climate variability may change in the future in response to greenhouse gas induced warming but also as a result of the uncertainty in the response of agricultural crops to changes in climate variability, effected most probably through changes in the frequency of extreme climatic events. Showed that changes in variance have a greater effect on the frequency of extreme climatic events than do changes in the mean values. Hence, it is important to attempt to include changes in variability in scenarios of climate change. Weather change at Hungary was started about of 1850. Among the natural catastrophes, drought and flooding caused by over-abundant rainfall cause the greatest problem in plant nutrition and in field crop production nowadays too (José et al., 2001). It is why we found it necessary to revise and to analyse this problem. The triticale is most important crop of many World countries (Márton and Pekli, 2003) but little research in the field of climate change impact assessment has been undertaken. These plant is sensitive to the prevailing weather conditions (rainfall) and, hence, it is important to evaluate the effects of anthropogenic climate change on her production. The crop is demanding indicator of soil nutrient status also. Have a particularly high requirement for supply of soil nitrogen, phosphorus, potassium, calcium and magnesium. From 1990 to 2001 this paper describes climate-rainfall-change and N-mineral fertilisation effects on triticale yield on a acidic sandy brown forest soil at long term experiment scale under temperate climate conditions at Hungary. Material and Method The effect of rainfall quantity and distribution on certain crop fertilisation factors (N, P, K, Ca, Mg and yield) were studied in a long- term field experiment on acidic sandy brown forest soil at North- Eastern Hungary set up in 1962 and 2003. The agrochemical parameters of the soil were as follows: pH (H2O) 5.9, pH (KCl) 4.7, hydrolytic acidity 8.4, hy1 0.3, humus 0.7%, CEC 5-10 mgeq 100*g-1, total N 34 mg*kg-1, AL-P2O5 43 mg*kg-1, AL-K2O 60 mg*kg-1. From 1962 to 1980 the experiment consisted of 2x16x4x4=512 plots and from 1980 of 32x4=128 plots in split-split plot and factorial random block design. The gross plot size was 10x5=50 m2. The average fertiliser rates in kg*ha-1*year-1 were nitrogen 45, phosphorus 24 (P2O5), potassium 40 (K2O), magnesium 7.5 (MgO) until 1980 and nitrogen 75, phosphorus 90 (P2O5), potassium 90 (K2O), calcium 175 (Ca) and magnesium 40 (Mg) after 1980 in the form of 25 % calcium ammonium nitrate, 18 % superphosphate, 40 % potassium chloride, calcium carbonate and magnesium sulphate. The groundwater table was at a depth of 2 - 3 m. Ecological (rainfall) and experimental data bases were estimated by Hungarian traditional (Harnos, 1993) and RISSAC-HAS (Márton, 2003) standards, MANOVA (SPSS) and regression analysis (SPSS). Results and Discussion Nitrogen results are summarised from 1990 to 2001. 1. On the basis of "general" (Harnos, 1993) and triticale-specific rainfall deficiency values (Márton, 2003) the years could be classified as average (1991, 1995, 2000), dry (1993), droughty (1992, 1994, 1996), wet (1997, 1998, 2001) and over wet (1999). 2. In average years the yield of the control plots became stabilised at the 1.4 t*ha-1 level. In the fertilised treatments the highest yield (4.0 t*ha-1) was more than two times the lowest yield (1.9 t*ha-1). N fertilisation resulted in an increase of around 1.0 t*ha-1 in the main yield compared with the control. The triticale yields could only be enhanced economically by full treatment with NPK (3.3 t*ha-1) or NPKCa-, NPKMg-, NPKCaMg (3.9 t*ha-1). 3. Without fertilisation the yield in the dry and drought years was decreased 14% and 36% to that in the average year. In case of the nitrogen treatmets the yield was decreased 45% and 24%. 4. In the wet years on the unfertilised plots the yield declined 14% and in the case of the nitrogen fertilisation the yield no changed than in the average years. In the over wet year the plots yielded similar than in the average years. 5. The relationships between rainfall during the vegetation period, N, P, K, Ca and Mg fertilisation and yield were characterised by second-degree correlation depending on the level of nutrition (R: 0=0.3455**, N=0.2779+, NP=0.4722***, NK=0.3739***, NPK=0.6311***, NPKCa=0.6673***, NPKMg=0.6734***, NPKCaMg=0.6232***). The maximum yield (5.0-6.0 t*ha-1) was yielded at 550-600 mm growth period rainfall. References Harnos, Zs. 1993. Időjárás és időjárás-termés összefüggéseinek idősoros elemzése. In: Aszály 1983 (Szerk.: Baráth, Cs-né., Győrffy, B., és Harnos, Zs.). KÉE. Budapest Johnston, A. E. 2000. Some aspects of nitrogen use efficiency in arable agriculture. K. Scogs-o. Lantbr. Akad. Tidskr. 139: 8. José, A. B., Estáquio, M. J., and Márton, L. 2001. Results of Crotalaria ssp. effects on soil conservation. In: Congress on Conservation Agriculture, (Eds Armando, M. V.), ECAF., Madrid, 5, pp 1-4. Márton, L. 2001a. Climate change and N, P, K, Mg fertilization effect analysis at Tisza-river basin in a long term field experiment. Szent István University, Gödöllő, p. 9. Márton, L. 2001b. Climate change, N-fertilisation effect on rye (Secale cereale L.) yield in a long term field experiment. In: Rural development-Ecologically farming-Agriculture, (Eds Palkovics, M.), University Veszprém, Keszthely, pp 924-929. Márton, L. 2002a. Climate-Rainfall Change (CRC) and mineral fertilisation (MF) effects on different crop production. In: Challenges of the new millennium our joint responsibility. (Eds A. Borhidi). MTA ÖBKI. Budapest. 1, pp 110-111. Márton, L. 2002b. Relationships between rainfall, nutrient supplies and the yield of winter wheat (Triticum aestivum L.). Plant Production 51: 529-542. Márton, L. 2003. Relationships between rainfall, nutrient supplies and the yield of triticale. Plant Production. In press Márton, L., and Pekli, J. 2003. Plant production under sub-arctical and temperate climate conditions. SZIU. Gödöllő Acknowledgement This research was supported by Hungarian Academy of Sciences, H-Budapest Adderss of the author Dr. Márton László Ph.D Research Institute for Soil Science and Agricultural Chemistry of the Hungarian Academy of Sciences, 1022 H-Budapest, Herman O. u. 15. E-mail:marton@rissac.hu

Environmental Change: Precipitation and N, P, K, mg Fertilization Influences on Crop Yield Under Temperate Climate Conditions

NASA Astrophysics Data System (ADS)

László Phd, Dd. M.

2009-04-01

Summary: Agroecological quality has a well estabished dependence on climate-rainfall changes because the water problems are pressing. Therefore, there is, growing concern about the potentially wide ranging risks that climate change would have on these key industries as the nature and extent of anticipated changes have become more evident. It also includes changes in land use and in plant production and their management. These changes are unprecedented in terms of both their rate and their spatial extent. Changes in land use (agrotechnics, soil, cultivation, fertility, quality, protection etc.) and in plant production (plant, nutrition, rotation, protection etc.) are currently the main manifestations. As an interdisciplinary problem it is necessary to study such a complex matter in terms of agricultural production. Generally, among natural catastrophes, droughts and floods cause the greatest problems in field crop production. The droughts and the floods that were experienced in Hungary in the early 1980s have drawn renewed attention to the analyses of these problems. New research on climate change-soil-plant systems are focused on yield and yield quality. This paper reports of the climate changes (rainfall); soil (acidic sandy brown forest) properties, mineral N, P, K, Mg fertilisation level and plant interactions on rye (Secale cereale L.), on potato (Solanum tuberosum L.) and on winter wheat (Triticum aestivum L.) yields in a long term field experiment set up at Nyírlugos in north-eastern Hungary under temperate climate conditions in 1962. Results are summarised from 1962 to 1990. Main conclusions were as follows: 1. Rye: a, Experimental years were characterised by frequent extremes of precipitation variabilities and changes. b, By an average year, at a satisfactory fertilisation level (N: 90 kg ha-1 and NP, NK, NPK, NPKMg combinations) the maximum yield reached 3.8 t ha-1. But yield was decreased by 17% and by 52% due to drought and excess rainfall, respectively. Negative effects (drought, excess rainfall) were diminished by 20-25% with Mg treatments. c, Correlation between rye yields and precipitation during vegetation seasons showed that optimum yield (4.0 t ha-1) develops in the 430-470 mm range. 2. Potato: a, Trial years were estimated by recurrent extremes of climate. b, In vegetation seasons poor in rainfall yield safety in potato cannot be secured by fertilisation (N, NP, NK, NPK, NPKMg) alone. Under this weather condition yield was decreased by 35%. c, Optimum yields range between 17-21 t ha-1 at 280-350 mm. 3. Winter wheat: a, Climate was manifested mainly by precipitation using average, drought, dry and rainy levels. b, Yields from drought year effects with N, NP and NK combinations were diminished to 48% and with NPK and NPKMg treatments fell to 51%. c, Optimum yields (3.5-4.0 t ha-1) were developed at 450-500 mm. This paper summarises quantified results of rye, potato and winter wheat research with regarding to interaction effects and relationships between climate (rainfall)-mineral nutrition-crop production changes in Hungary during a long term field experiment to agricultural sustainability. Key words: ecology, rainfall, crop, fertilization, yield Introduction: "Climate Change" are recognized as a serious environmental issues [1]. Presently the build up of greenhouse gases in the atmosphere and the inertia in trends in emissions means that we can expect significant changes for at least the next few decades and probably for the whole 21th century too [2]. It would badly need to understand what might be involved in adapting to the new climates. A decade ago, researchers asked the „what if" question. For example, what will be the impact if climate changes. Now, we must increasingly address the following question: how do we respond effectivelly to prevent damaging impacts and take advantage of new climatic opportunities [3]. This question requires detailed in information regarding expected impacts and effectíve adaptive measures. Information on adaptation is required for governments, landscape planners, stakeholders, farmers, producers, processors, supermarkets and consumers. Not only the local effects and options, but also the spatial implications must be understood. Will yields be maintained on the present range of farms. Where will new crops be grown. Will new processing plants be required. Will there be competition for water. Most recent agricultural impact studies have concentrated on the effects of mean changes in climate on crop production, whilst only limited investigations into the effects of climate variability on agriculture have been undertaken. The paucity of studies in this area is not least due to the considerable uncertainty regarding how climate variability may change in the future in response to greenhouse gas induced warming but also as a result of the uncertainty in the response of agricultural crops to changes in climate variability, effected most probably through changes in the frequency of extreme climatic events. That changes showed in variance have a greater effect on the frequency of extreme climatic events than do changes in the mean values. Hence, it is important to attempt to include changes in variability in scenarios of climate change. Weather change in Hungary was started about of 1850. Among the natural catastrophes, drought and flooding caused by over-abundant rainfall cause the greatest problem in plant nutrition and in field crop production nowadays too [4]. It is why we found it necessary to revise and to analyse this problem. Rye (Secale cereale L.), potato (Solanum tuberosum L.) and winter wheat (Triticum aestivum L.) are most important crops of many World countries [5] but little research in the field of climate change impact assessment has been undertaken. All three plant are sensitive to the prevailing weather conditions (rainfall) and, hence, it is important to evaluate the effects of anthropogenic climate change on their production. These crops are demanding indicator of soil nutrient status also. Have a particularly high requirement for supply of soil nitrogen, phosphorus, potassium and magnesium. From 1962 to 1990 this paper describes climate-rainfall-change and N, P, K and Mg-mineral fertilisation effects on rye, potato and winter wheat yield on a acidic sandy brown forest soil at long term experiment scale under temperate climate conditions at Hungary. Material and Method: The effect of rainfall quantity and distribution on certain crop fertilisation factors (N, P, K, Mg and yield) were studied in a long-term field experiment on acidic sandy brown forest soil at North-Eastern Hungary set up in 1962 and 2002. Ploughed layer of the experiment soil had a pH(KCl) 4.5, humus 0.5%, CEC 5-10 mgeq 100 g-1. The topsoil was poor in all four macronutrients N, P, K and Mg. Rye, potato and winter wheat experiments involved 2x2x16x8 = 512, 2x2x16x8 = 512 and 2x16x4 = 128 plots. The gross and net plot size was 10x5 = 50 m2 and 35.5 m2. The experimental designe was split-split-plot. Average treatments were rye N:45 kg, P2O5:24, K2O:40, MgO:7.5 kg ha-1 year-1, potato N:75 kg, P2O5:24, K2O:75, MgO:15 kg ha-1 year-1, winter wheat N:45 kg, P2O5:24, K2O:40, MgO:7.5 kg ha-1 year-1 from 1962 to 1980 and N:75 kg, P2O5:90, K2O:90, MgO:140 kg ha-1 year-1 from 1981 to 1990 in the form of 25% calcium ammonium nitrate, 18% superphosphate, 40% potassium chloride, and magnesium sulphate. The groundwater table was at a depth of 2-3 m. Ecological (rainfall) and experimental data bases were estimated by Hungarian traditional [6] and RISSAC-HAS [3] standards and MANOVA (SPSS). Results: Climate-rainfall-change and mineral fertilisation effects on rye yield a. Experimental years were characterised by frequent extremes of precipitation variabilities and changes. One year had an 450 mm average rainfall (1966), one year had a more humid (1970) and three years had a very dry (1964, 1968, 1972) character. b. Weather anomalies as drought or to much rainfall did not cause significant differences on rye yield without fertilisation (average year: 1.66 t ha-1, drought year: 1.51 t ha-1, over rainfall year: 1.47 t ha-1). c. Yields varied from 2.01 to 3.04 t ha-1 under low (N: 30 kg ha-1 and NP, NK, NPK, NPKMg combinations) fertilisation input. Yields were decreased by 14% and 10% by drought and also by excess of rainfall. d. At mean fertilisation (N: 60 kg ha-1 and NP, NK, NPK, NPKMg combinations) level the maximum yield had reached 3.6 t ha-1 in average year. In years with excess rainfall, rye yields decreased as an average of fertilisation treatments by 20%. e. By an average year, at satisfactory fertilisation (N: 90 kg ha-1 and NP, NK, NPK, NPKMg combinations) level the maximum yield reached 3.8 t ha-1. But these yields were decreased with 17% and with 52% by drought and excess rainfall weather conditions respects. Negative effects (drought, excess rainfall) were diminished with 20-25% on the Mg treatments. f. Correlations between rye yields and the sums of precipitations during vegetation period (control: R = 0.99***, N: R = 0.84***, NP: R = 0.84***, NK: R = 0.91***, NPK: R = 0.85***, NPKMg: R = 0.65**) showed that optimum yields will develop in 430-470 mm range. Under and above these range of rainfall yields will decrease. Climate-rainfall-change and mineral fertilisation effects on potato yield a. Trial years (1963, 1965, 1967, 1969, 1971) were characterised by recurrent extremes of climate under vegetation seasons of potato. Three period had average rainfall, while two were very dry. b. All in all, droughts in the winter or summer half-year had much the same effect on yields. Precipitation deficiency in the winter could not be counterbalanced by average rainfall during the vegetation period, and its effect on the yield was similar to that of summer drought. c. Yield and quality were influenced by rainfall to a greater extent than by fertilisation. d. In vegetation periods poor in rainfall yield and quality safety in potato cannot be secured by fertilisation alone, they were decreased to 35%. It was also concluded that economic yields could not be achieved with poor nutrient supply even with a normal quantity and distribution of rainfall. e. The unfavorable effects of climate anomalies (drought, over-abundance of water in the topsoil) on the yield formation, yield quantity and quality of potato depended decisively on the time of year when they were experienced and the period for which they lasted. f. With the help of regression analysis it was found the polynomial correlation between rainfall and yield could be observed in case of the control: R = 0.98***, N: R = 0.95***, NP: R = 0.96***, NK: R = 0.95***, NPK: R = 0.98***, NPKMg: R = 0.96*** nutrition systems. The optimum yield ranges between 17-20 t ha-1 at 280-350 mm of rainfall. Climate-rainfall-change and mineral fertilisation effects on winter wheat yield a. Climate-rainfall-conditions of winter wheat years were determined by mainly precipitation on-, average (1982 and 1989)-, drought (1976 and 1990)-, dry (1974) and rainy (1978 and 1980) level. b. Experimental years climate-rainfall-character were formed by winter half-years (october-march), months (october-september), pre-months of sowing (august), critical sequential month number in vegetation seasons (september-july) and critical sequential month number in experimental years (september-august). c. In average years without any mineral fertilisation wheat yield was stabilized on the level of 1.8 t ha-1. Under N, P, K and Mg fertiliser input minimum and maximum yields were 2.7 and 4.1 t ha-1. Yield was only increased by whole NPK and Mg completed NPKMg treatment. d. Without mineral fertilisation on control plots yield was decreased by drought year effect compared with average with a 39%. On N, NP and NK combinations yields were diminished to 48%. Drought damage on yield production was rised more to 51% by NPK and NPKMg application. e. But in dry years and in average years yields were similar on control plots. Yields were decreased for average year effect on N, NP, NK and NPK, NPKMg treatments with 20% and with 16%. f. Under excess rainy weather conditions without fertiliser application yields were decreased more dramaticaly (56%) than under drought seasons (39%) to case of average rainfall effects. Yield was damaged with a 47% by unfavourable (N, NP, NK) nutrition. But this negative effect of excess rainfall condition was diminished on NPK and NPKMg treatments to 41%. g. Correlations of regression analysis between yields and the sums of precipitations during vegetation seasons (control: R = 0.59***, N: R = 0.57***, NP: R = 0.76***, NK: R = 0.53**, NPK: R = 0.67***, NPKMg R = 0.70**) showed that optimum yields will develop in 450-500 mm range. Above these range of rainfall yields will decrease swiftly. This paper gives opportunities summarise quantified results of rye-potato-winter wheat researches with regarding to interaction effects and relationships between climate (rainfall)-mineral nutrition-crop production changes at Hungary in a long term field experiment system under temperate climate conditions to agricultural sustainability. Acknowledgement: This research was supported by Hungarian Academy of Sciences, H-Budapest References [1] Johnston A.E.: Some aspects of nitrogen use efficiency in arable agriculture. K. Scogs-o. Lantbr. Akad. Tidskr. 2000, 8, 139. [2] Márton L.: Climate change and N, P, K, Mg fertilization effect analysis at Tisza-river basin in a long term field experiment. Szent István University, Gödöllő 2001, 9. [3] Márton L.: Climate change, N-fertilisation effect on rye (Secale cereale L.) yield in a long term field experiment. [in:] Rural development-Ecologically farming-Agriculture, (Eds M Palkovics), University Veszprém, Keszthely 2001, 924-929. [4] José A.B., Estáquio M.J. and Márton L.: Results of Crotalaria ssp. effects on soil conservation. Congress on Conservation Agriculture (Eds Armando MV), ECAF., Madrid, 2001. 5, 1-4. [5] Kádár I., Márton L. and Horváth S.: Mineral fertilisation of potato (Solanum tuberosum L.) on calcareous chernozem soil. Plant Production, 2000, 49, 291-306. [6] Harnos, Zs.: Időjárás és időjárás-termés összefüggéseinek idősoros elemzése, [in:] Aszály 1983 (Szerk.: Baráth Cs-né, Győrffy B., Harnos Zs.). KÉE. Budapest 1993. [7] Márton L.: Climate-Rainfall Change (CRC) and mineral fertilisation (MF) effects on different crop production. [in:] Challenges of the new millennium our joint responsibility. (Eds A. Borhidi). MTA ÖBKI, Budapest 2002, 1, 110-111. [8] Márton L.: Rainfall, mineral fertilisation and winter wheat (Triticum aestivum L.) yield relations. Plant Production, 2002, 51, 529-542.

Effects of Nitrogen and Desferal Treatments on CROTALARIA's (Crotalaria juncea Roth) Biomass Production

NASA Astrophysics Data System (ADS)

László Phd, M., ,, Dr.

2009-04-01

Presently sustainable agriculture is vital to achieving food security poverty alleviation and environmental protection because land degradation and desertification has occurred in all the world over cutting across a broad spectrum of contrasts in climate, ecosystem types, land uses and socio/economic settings. For this reason improving integrated soil fertility management is appreciationed and has become a major issue of concern on the development plant nutrition and plant production agendas. On plant nutrition level mineral macronutrients so nitrogen and chelating agents of different microelements so Desferal- deferoxamin-methansulfonic are essential for plant growth and development. Crotalari juncea L. is a well-known nutrient indicator fodder and green manure crop with a high yield potential. Field experiment was carried out on a chernozem meadow soil (Kunság- region of Hungary, Kunmadaras) in partly of experiment series (6 years) in 2001. The ploughed layer of region soils contained with about 2.6-3.4% humus and 40-42% clay, had a humus stability index of 0.9-2.5 by Márton (1997), pH (H2O) of 6.5-7.7, pH (KCl) of 5.3-6.8, y1 of 6.7-13.3. The topsoil was poorly supplied with all five macronutrients (N-NO3 1 mg 100 g-1, AL-soluble P2O5 14 mg 100 g-1, AL-K2O 36 mg 100 g-1, Ca 330 mg 100 g-1, Mg 43 mg 100 g-1) and with all four micronutrients (0.5m HNO3 soluble Cu 1 mg kg-1, Zn 1 mg kg-1, Mn 9 mg kg-1, Fe 80 mg kg-1) according to soil analysis. The groundwater depth was 2-3 m. Nitrogen x Desferal (Novartis Pharma AG Basie, Switzerland, Suiza 500mg) x Genotype (Brazíl-EMBRAPA/CNPH, Brazilia-DF, India-University of Agricultural Sciences, Bangalore) x Time experiment involved 4Nx2Dx2Gx3T=48 treatments in 3 replications giving a total of 144 plots. The N levels were 0, 100, 200 and 300 kg ha-1 year-1, and desferal levels 0 and 20 kg ha-1 year-1 with a 100 kg ha-1 year-1 P2O5 and 120 kg ha-1 year-1 K2O basic fertilisation. The plot size had an area of 4x2=8 m2 with 920-920 individual plants. Experimental datas were estimated by MANOVA of SPSS. The most important results can be summarised as follows: a., As the N supplies improved the root length (cm), plant height (cm), mean scores (1-5), fresh root weight (t ha-1), green straw+leaf weight (t ha-1), total green biomass weight (t ha-1), air dry root weight (t ha-1), air dry straw+leaf weight (t ha-1), and total air dry biomass weight (t ha-1) increased with an 1.4, 1.3, 4.3, 1.3, 1.8, 1.6, 2.1, 1.9 and 2.0 times compared to the control by the start of flowering. b., As the N doses rised the root length, plant height, mean scores, fresh root weight, green straw+leaf weight, total green biomass weight, air dry root weight, air dry straw+leaf weight and total air dry biomass weight reaching 34.3 cm, 168.0 cm, 4.3, 14.8 t ha-1, 51.7 t ha-1, 66.5 t ha-1, 7.4 t ha-1, 16.5 t ha-1 and 23.9 t ha-1. c., About three-fourth of the total green biomass and total air dry biomass production at harvest was given by the straw+leaf yield, which ranged between 29.0-51.7 t ha-1 and 8.7-16.5 t ha-1, depending on the N-treatment applied. d., The root length, plant height, mean scores, fresh root weight, green straw+leaf weight, total green biomass weight, air dry root weight, air dry straw+leaf weight and total air dry biomass weight was increased in average with an 14, 15, 21, 157, 30, 63, 102, 28 and 51% by N+Desferal treatments compared to mean of N doses effects. e., By N+Desferal treatments the root length, plant height, mean scores, fresh root weight, green straw+leaf weight, total green biomass weight, air dry root weight, air dry straw+leaf weight and total air dry biomass weight achieved 37.0 cm, 173.3 cm, 4.3, 37.8 t ha-1, 64.4 t ha-1, 102.2 t ha-1, 13.8 t ha-1, 19.3 t ha-1 and 33.1 t ha-1. f., Approximately two-third of the total green biomass and total air dry biomass production at harvest was given by the straw+leaf yield, which ranged between 44.7-64.4 t ha-1 and 24.1-33.1 t ha-1, depending on the N+Desferal treatment rates. g. On the given soil the highest quantity of 300 kg ha-1 year-1 N mineral fertilizer + 20 kg ha-1 year-1 Desferal chelating agent seemed to give already over fertilization and lowered in its tendency mainly the total green biomass yield and verifiable the total air dry biomass yield. By experimental results can be summarised that we was able to increase with a great rate Crotalaria juncea L. total green biomass yield and total air dry biomass yield by N and Desferal treatments. As well as so we can show and offer our results to different sustainable farming managements with nutrition system of low, mean and high input in the next future. Keywords: nitrogen, desferal, crotalaria, soil fertility, sustainable agriculture management Introduction Presently sustainable agriculture is vital to achieving food security poverty alleviation and environmental protection because land degradation and desertification has occurred in all the world over cutting across a broad spectrum of contrasts in climate, ecosystem types, land uses and socio/economic settings. For this reason improving integrated soil fertility management is appreciationed and has become a major issue of concern on the development plant nutrition and plant production agendas. On plant nutrition level mineral macronutrients so nitrogen and chelating agents of different microelements so Desferal- deferoxamin-methansulfonic are essential for plant growth and development. Crotalari juncea L. is a well-known nutrient indicator fodder and green manure crop with a high yield potential. The complexity of the desertification phenomenon has drawn our attention to categorize, inventory, monitor and repair the condition of the land (Arnalds and Archer 1999). Therefore, farmers are constantly being subjected to soil fertility changes that are beyond their control on account of factors that affect the viability and profitability their farming enterprise. They must acquire the capacity to respond to these changing situations and opportunities in order to maximise production. Grower need to be helped to develop this capability by encouraging their innovations and by involving them in a learning process in which they are exposed to new knowledge and technologies. The functioning of soils and their ability to supply nutrients, store water, release greenhouse gases, modify pollutants, resist physical degradation and produce crops within a sustainable management system. Mineral fertilization is determined in the first place by the needs of plants for nutrients but due attention must also by given to soil process. Nitrogen is essential to the growth and reproduction of crops. It plays a major role in the development and functions of protoplasm, being an essential constituent of all proteins. Crotalaria has a high demand for nitrogen. The problem of the nitrogen nutrition in case of this plant is much more difficult than those of phosphatic or potassic nutrition because production is limited by nitrogen deficiency more often than by that of any other nutrient. The omission of no other element causes such a drastic decline in yield and growth. Nitrogen is therefore without question the most important fertilizer nutrient for this crop. The essential micronutrients -also called trace or minor elements- or elements taken up by plants in very much smaller amounts, are iron, boron, zinc, copper, manganese, molybdenum and chlorine. Deficiencies in the supply of these elements to crops may be due to their absence or scarcity in the soil or to their being present in the soil but unavailable because of certain soil conditions -in very calcareous or in overlimed soils, in very old acidic, leached soils etc. Each of these nutrient elements has a definite key function also within the plant. Some of these functions are still imperfectly understood. In many early studies on plant utilization of microelement chelated (for example Fe chelated) with a high stability constant in solution by various synthetic or natural chelates were assumed to be more efficient as micronutrient suppliers to plants than the uncelated micronutriens. Primary criterion for microelement complexes is a high complex stability. Various siderophores and synthetic chelates stability constants are well documented in many papers (Shenker at al. 1996). Desferal -chelating agent deferoxamin-methansulfonic- is a well know chelator with a high stability constant and micronutrient supplier potential to plant nutrition. Sunn hemp (Crotalaria juncea L.) is one of the earliest, important and most distinctly named animal fodder and green manure plant. There is one of the most widely grown crop throughout the tropics, subtropics and temperate climate conditions. It is grown in rotation with rice, maize, tobacco, cotton, sugar cane, pineapples, coffee, orchard and in other crops. It is characterized by its rapid growth and high biomass production potential of green (60 t ha-1) and dry (20 t ha-1) material (Kiyoko 1996). As a green manure for example has been the key element in the maintenance of soil organic matter content, of soil fertility (Márton 2001). Crop is ploughed in after 2 months when the plants begin to flower as it decomposes more rapidly at this stage. The mentioned above yields wich on decomposition may add 80-100 kg ha-1 of N to the soil. Materials and Methods Field experiment was carried out on a chernozem meadow soil (Kunság- region of Hungary, Kunmadaras) in partly of experiment series (6 years) in 2001. The ploughed layer of region soils contained with about 2.6-3.4% humus and 40-42% clay, had a humus stability index of 0.9-2.5 by Márton (1997), pH (H2O) of 6.5-7.7, pH (KCl) of 5.3-6.8, y1 of 6.7-13.3. The topsoil was poorly supplied with all five macronutrients (N-NO3 1 mg 100 g-1, AL-soluble P2O5 14 mg 100 g-1, AL-K2O 36 mg 100 g-1, Ca 330 mg 100 g-1, Mg 43 mg 100 g-1) and with all four micronutrients (0.5m HNO3 soluble Cu 1 mg kg-1, Zn 1 mg kg-1, Mn 9 mg kg-1, Fe 80 mg kg-1) according to soil analysis. The groundwater depth was 2-3 m. Nitrogen x Desferal (Novartis Pharma AG Basie, Switzerland, Suiza 500mg) x Genotype (Brazíl-EMBRAPA/CNPH, Brazilia-DF, India-University of Agricultural Sciences, Bangalore) x Time experiment involved 4Nx2Dx2Gx3T=48 treatments in 3 replications, giving a total of 144 plots. The N levels were 0, 100, 200 and 300 kg ha-1 year-1, and desferal levels 0 and 20 kg ha-1 year-1 with a 100 kg ha-1 year-1 P2O5 and 120 kg ha-1 year-1 K2O basic fertilisation (Table 1.) in the form of 34% NH4NO3, 18% superphosphate and 60% potassium chloride. The plot size had an area of 4x2=8 m2 with 920-920 individual plants. Forecrop over 2 years was crotalaria. Plant samples were taken and measured (green and air dry matter weight) during the vegetation grown period at least 3 times (07.07.2001., 23.08.2001. and 20.10.2001.), using 5-5 plants plot-1 randomly. Experimental datas were estimated by MANOVA of SPSS. The main goal of the whole research programme was described earlier by Márton (1999). This paper reports results of Nitrogen x Desferal x Indian genotype experimental combinations at stage the start of flowering of 23.08.2001. Results and Discussion Improving soil fertility in all the world over farming systems has become a major issue of concern on the development plant nutrition and plant production agendas. A number of international initiatives and programmes have been established which aim to address the problem of soil fertility decline, and would imply major investment of soil researches. This research reports on the nitrogen x desferal nutrition and potential use of Crotalaria juncea L. as a nonwood source of animal fodder and green manure under temperate climate conditions to soil fertility maintenance. The most important results can be summarised as follows. As the N supplies improved the root length (cm), plant height (cm), mean scores (1-5), fresh root weight (t ha-1), green straw+leaf weight (t ha-1), total green biomass weight (t ha-1), air dry root weight (t ha-1), air dry straw+leaf weight (t ha-1), and total air dry biomass weight (t ha-1) increased 1.4, 1.3, 4.3, 1.3, 1.8, 1.6, 2.1, 1.9 and 2.0 times compared to the control (Table 2.) by the start of flowering. As the N doses rised the root length, plant height, mean scores, fresh root weight, green straw+leaf weight, total green biomass weight, air dry root weight, air dry straw+leaf weight and total air dry biomass weight reaching 34.3 cm, 168.0 cm, 4.3, 14.8 t ha-1, 51.7 t ha-1, 66.5 t ha-1, 7.4 t ha-1, 16.5 t ha-1 and 23.9 t ha-1. About three-fourth of the total green biomass and total air dry biomass production at harvest was given by the straw+leaf yield, which ranged between 29.0-51.7 t ha-1 and 8.7-16.5 t ha-1, depending on the N-treatment applied. The root length, plant height, mean scores, fresh root weight, green straw+leaf weight, total green biomass weight, air dry root weight, air dry straw+leaf weight and total air dry biomass weight was increased in average with an 14, 15, 21, 157, 30, 63, 102, 28 and 51% by N+Desferal treatments compared to mean of N doses effects. By N+Desferal treatments the root length, plant height, mean scores, fresh root weight, green straw+leaf weight, total green biomass weight, air dry root weight, air dry straw+leaf weight and total air dry biomass weight achieved 37.0 cm, 173.3 cm, 4.3, 37.8 t ha-1, 64.4 t ha-1, 102.2 t ha-1, 13.8 t ha-1, 19.3 t ha-1 and 33.1 t ha-1. Approximately two-third of the total green biomass and total air dry biomass production at harvest was given by the straw+leaf yield, which ranged between 44.7-64.4 t ha-1 and 24.1-33.1 t ha-1, depending on the N+Desferal treatment rates. On the given soil the highest quantity of 300 kg ha-1 year-1 N mineral fertilizer + 20 kg ha-1 year-1 Desferal chelating agent seemed to give already over fertilization and lowered in its tendency mainly the total green biomass yield and verifiable the total air dry biomass yield. By experimental results can be summarised that we was able to increase with a great rate Crotalaria juncea L. total green biomass yield and total air dry biomass yield by N and Desferal treatments. As well as so we can show and offer different nutrition systems -with input of low, mean, high level- to different sustainable farming managements next future. Acknowledgements This research was supported by Research Institute for Soil Science and Agricultural Chemistry of the Hungarian Academy of Sciences, Budapest Hungary, National Vegetable Crops Research Centre, Brazília-DF Brazíl and University of Agricultural Sciences, Bangalore India References Arnalds, O. and Archer, S. 1999. Case studies of Rangeland desertification. Rala report 200. Agricultural Research Institute. Reykjavik Kiyoko, H. 1996. Study of the utilization of sunn hemp, Crotalaria juncea, in different sowing dates, 1995 and 1996, Okinawa-II, Santa Cruz, Bolivia. CETABOL. Santa Cruz. Bolivia Márton, L. 1997. Soil conservation research in a long term field experiment. Work paper. UAD. Karcag Márton, L. 1999. Diseases information of an alternative -Crotalaria juncea L.- crop. Plant Protection. 35:529-531. Márton, L. 2001. Effects of Crotalaria juncea L. and Crotalaria spectabilis ROTH on soil fertility and soil conservation in Hungary. Acta Agronomica Óváriensis. 43:1-8. Shenker, M., Hadar, Y. and Chen, Y. 1996. Stability Constants of the Fungal Siderophore Rhizoferrin with Various Microelements and Calcium. Soil Sci. Soc. Am. J. 60:1140-1144.

Climate Change: Natural Water and Fertilization Effects on Winter Rye (Secale cereale L.) Yield in Monoculture

NASA Astrophysics Data System (ADS)

László Phd, M., ,, Dr.

2009-04-01

Interaction of rainfall on crop fertilization factors, such as macronutrients and yield, were studied during a long-term field experiment on a calcareous sandy soil with a low humus content in north Hungary at Örbottyán Experimental Station of RISSAC-HAS from 1961 to 2004. When the experiment was commenced (1959) the plowed portion of experimental soil (top soil) had a pH (H2O) 7.5-7.8, pH(KCl) 6.9-7.1, humus content of 0.6-1.0%, clay content about 5%, CaCO3 content 3-7%, AL (ammonium-lactate) soluble P2O5 content 40-60 mg . kg-1 and AL soluble K2O content 50-100 mg . kg-1. The experiment consisted of ten treatments in five replications, giving a total of 50 plots arranged in a Latin square design. The gross plot size was 35 m2. From the 1st to the 25th year the fertilization rates were 0, 50, 100 kg . ha-1 . year-1 nitrogen, 0, 54 kg . ha-1 . year-1 P2O5 and 0, 80 kg . ha-1 . year-1 K2O and their combinations. From the 26th year onwards these rates were 0, 120 kg . ha-1 . year-1 nitrogen, 0, 60, 120 kg . ha-1 . year-1 P2O5 and 0, 60, 120 kg . ha-1 . year-1 K2O. The major results were as follows: i., In average years the yield in the control plots stabilised at around 0.8 t . ha-1. The yield doubled (1.8-1.9 t . ha-1) in the N, NP and NK treatments, while the full NPK doses gave the maximum yield of 2.1 t . ha-1. ii., In dry years yields of 0.7 t . ha-1 could be harvested in the control plots. These was a yield reduction of 13% compared with the many years' mean. Yield depressions of 33, 16, 21 and 20% were caused by drought in the N, NP, NK and NPK treatments. iii., In wet years the yield was little more than 0.5 t . ha-1 (0.6 t . ha-1) in the control plots, representing a yield loss of 25% compared with average years. The N, NP, NK and NPK treatments led to yield depressions of 28, 26, 26 and 26%. Rye grown in a monoculture has approx. 5% less tolerance of wet years than of drought. iv., Depending on the nutrient supplies, significant quadratic correlations were observed between the rainfall quantity and the yield (0: R=0.7489***, N: R=0.8974***, NP: R=0.8020***, NK: R=0.7370***, NPK: R=0.9047***, mean R2=0.8180; 66.9%) during the vegetation period. v., The increase in grain yield per mm rainfall ranged from 3.0 to 6.4 kg . ha-1 in the case of optimum rainfall supplies, while the quantity of rainfall during the vegetation period required for the production of 1 kg air-dry yield ranged from 1529 to 3360 liters in the case of maximum yield. vi., Based on the meteorological database for the 44 years of the long-term experiment (1961-2004) the frequency of years in which the rainfall was optimum for various levels of nutrient supply was as follows: control: 2%, N: 7%, NP: 7%, NK: 9%, NPK: 7%, giving an average of 6% over the treatments. This suggests that the occurrence of optimum rainfall supplies and the possibility of achieving optimum yields in a rye monoculture will be decline in the future. vii., The yield average of rye grown in a monoculture on calcareous sandy soil (Őrbottyán) was 86% less than that achieved in a biculture on acidic sandy soil (Nyírlugos) under the similar fertilization and rainfall conditions. viii., The results show rye production is totally (66.9%) dependent on rainfall and fertilization changes. Key words: rye, monoculture, rainfall, artificial fertilization, yield Introduction: Climate change is recognized as a serious environmental issue (Easterling et al., 1999; Johnston, 2000; Harnos, 2005). It has repeatedly affected much or all of the earth (Láng, 2005). Available evidence suggests that such changes are not only possible but likely in the future, potentially with large impacts on ecosystems and societies (Barrow et al., 2000; NRC, 2002; Hulme et al., 2002; Rajendra, 2004; Márton, 2004; 2005ab). During the 20th Century green house gases, especially CO2, in the atmosphere increased markedly (Szász, 2005). Nearly concurrently with this, relative global temperatures of the 19th Century increased 0.6 0C (Hulme et al., 2002; Láng et al., 2004; Jolánkai, 2005; Várallyay, 2005). In the coming decades, global plant production faces the prospect of a changing climate and environment, too the known challenge of continuing to feed the world's population, predicted to double its present level of six billion by about the year 2050. The prospective climate change is global warming with associated changes in hydrological regimes and other climatic variables induced by the increasing concentration of radiatively active greenhouse gases. Climate change could have far-reaching effects on patterns of trade among nations, development, and food security (Rosenzweig et al., 1993). These changes (largely caused by human activities) are likely to affect crop yields differently form region to region across the globe (Márton, 2004., 2005ab., Seth & Jeffrey 2005). Significant issue that becomes apparent from even a cursory summary of existing knowledge is that from the crop's perspective the important point is the net effect of all the environmental changes that occur, or might occur, at any given place and time. Today, plenty of agricultural investigations focused on understanding the relation between mean climate change and crop production (Várallyay, 1992; Rajendra, 2004; JolánkaI, 2005). Few investigations, however, studied the effects of climate variability on agriculture crop yields (Németh, 2004). The response of agricultural crop yield to changes in climate variability were attributed primrily to changes in the frequency of extreme climatic events (EU, 2003). Recent studies demonstrated a greater effect on the frequency of extreme climatic events than changes in the mean climatic response (EM, 2004). Hence, in studying the effects of climatic change on crop production, the changes in the climatic variability and associated weather patterns should be included (Barrow et al., 2000). Changes in weather patterns were observed thoughout Europe (including Hungary) as early as 1850. Among the natural consequences of changing weather patterns, years of drought (rainfall deficit) and wet (rainfall excess) conditions, resulted in problems among plant nutrition and field crop production (EU, 2003). Whereas rye (Secale cereale L.) is a crop of worldwide importance, limited research exists about the effects of climate change on these crop (Kádár et al., 1984; Kádár, 2005; Márton, 2002). These crop has sensitive reactions to the prevailing weather conditions (such as rainfall) and, for this reason, understanding the effects of anthropogenic climate change on it's production has a great importance. In addition to rainfall, the crop require an optimal level of soil macronutrients: nitrogen, phosphorus and potassium (Várallyay, 1939; Kádár, 1992; Kárár et al., 1982; Kádár et al., 1984; Kádár & Szemes, 1994). Most environmental research focuses on only one, or a very few changes instead of the concomitant multiple changes occurring in our world. Unfortunately, however, the bulk of past research has focused on one factor at a time. As a result for example, much is known about the effects of a change in a geochemical element (macro, meso, micro or trace) loading on yield of some crops, but much less is known about the effects of a change in a geochemical element in combination with a change in rainfall quantity and distribution on the yield of those same crops. It is obviously the effects of all the environmental changes occurring, rather than just a geochemical element (or just other geochemical elements, or just raifall quantity and distribution, etc.), that is of importance to any crop. Although much of this paper focuses on single factors (rainfall quantity, rainfall distribution, N-, P-, K-fertilization), it was our intent to emphasize that the net effect of multiple environmental changes on rye is far more important than the effect of a single factor on that crop. So, we show interaction findings related to rainfall quantity, rainfall distribution changes and N, P, K fertilization effects on rye yield formation on a calcareous sandy soil with a low humus content in an ecologically fragile experimental site at Örbottyán in Hungary from 1961 to 2004 for 44 years. Materials and Methods: The effect of rainfall (quantity and distribution) on crop fertilization factors, such as macronutrients and yield, were studied during a long-term (1961 to 2004) field experiment on a calcareous sandy soil with a low humus content in north Hungary at Örbottyán Experimental Station of RISSAC-HAS. When the experiment was commenced (1959; in LÁNG, 1973) the plowed portion of experimental soil (top soil) had a pH (H2O) 7.5-7.8, pH(KCl) 6.9-7.1, humus content of 0.6-1.0%, clay content about 5%, CaCO3 content 3-7%, AL (ammonium-lactate) soluble P2O5 content 40-60 mg . kg-1 and AL soluble K2O content 50-100 mg . kg-1. The experiment consisted of ten treatments in five replications, giving a total of 50 plots arranged in a Latin square design. The gross plot size was 35 m2. From the 1st to the 25th year the fertilization rates were 0, 50, 100 kg . ha-1 . year-1 nitrogen, 0, 54 kg . ha-1 . year-1 P2O5 and 0, 80 kg . ha-1 . year-1 K2O and their combinations. From the 26th year onwards these rates were 0, 120 kg . ha-1 . year-1 nitrogen, 0, 60, 120 kg . ha-1 . year-1 P2O5 and 0, 60, 120 kg . ha-1 . year-1 K2O and their combinations in the form of 25 % calcium ammonium nitrate, 18 % superphosphate, 40 % potassium chloride. The groundwater table was at a depth of 2-3 m below the surface. Rainfall amounts, deviation in rainfall from the average over many years (dry year -10 - -20%, drought year -20% over, wet year +10 - +20%, year with excess rainfall +20% over) and other related data were determined based on traditional Hungarian (Harnos, 1993) and Research Institute for Soil Science and Agricultural Chemistry of the Hungarian Academy of Sciences (Márton, 2004) standards, and MANOVA (Multivariate Analysis of Variance) by SPSS test (SPSS Inc., 1988). Results and Discussion: In average years the yield in the control plots stabilised at around 0.8 t . ha-1 (Table 5). The yield doubled (1.8-1.9 t . ha-1) in the N, NP and NK treatments, while the full NPK doses gave the maximum yield of 2.1 t . ha-1. In dry years yields of 0.7 t . ha-1 could be harvested in the control plots. These was a yield reduction of 13% compared with the many years' mean. Yield depressions of 33, 16, 21 and 20% were caused by drought in the N, NP, NK and NPK treatments. In wet years the yield was little more than 0.5 t . ha-1 (0.6 t . ha-1) in the control plots, representing a yield loss of 25% compared with average years. The N, NP, NK and NPK treatments led to yield depressions of 28, 26, 26 and 26%. Rye grown in a monoculture has approx. 5% less tolerance of wet years than of drought. Depending on the nutrient supplies, significant quadratic correlations were observed between the rainfall quantity and the yield (0: R=0.7489***, N: R=0.8974***, NP: R=0.8020***, NK: R=0.7370***, NPK: R=0.9047***, mean R2=0.8180; 66.9%) during the vegetation period (Figure 1). The increase in grain yield per mm rainfall ranged from 3.0 to 6.4 kg . ha-1 in the case of optimum rainfall supplies, while the quantity of rainfall during the vegetation period required for the production of 1 kg air-dry yield ranged from 1529 to 3360 liters in the case of maximum yield. Based on the meteorological database for the 44 years of the long-term experiment (1961-2004) the frequency of years in which the rainfall was optimum for various levels of nutrient supply was as follows: control: 2%, N: 7%, NP: 7%, NK: 9%, NPK: 7%, giving an average of 6% over the treatments. This suggests that the occurrence of optimum rainfall supplies and the possibility of achieving optimum yields in a rye monoculture will be decline in the future. The yield average of rye grown in a monoculture on calcareous sandy soil (Őrbottyán) was 86% less than that achieved in a biculture on acidic sandy soil (Nyírlugos) under the similar fertilization and rainfall conditions. These results show rye production is totally (66.9%) dependent on rainfall and fertilization changes. Acknowledgement: We are grateful to Hungarian Academy of Sciences who supplied experiment, data and Internet URLs, as well as helping on other ways with this paper. Most of all, I would like to thank National Office for Research and Technology, Hungary and Hungarian Science and Technology Foundation, Hungary (Project No.: OMFB-00112/2005-E-2/04) for their support during the course of this research and my presentation. References Barrow, E. M., Hulme, M., Semenov, M. A. & Brooks, R. J., 2000. Climate change scenarios. In: Climate Change, Climatic Variability and Agriculture in Europe (ed's.: Downing, T. E., Harrison, P. A., Butterfield, R. E. and Londsdale, K. G.). European Commision, Brussel Easterling, D. R., Evans, J. L., Groisman, YA. P., Karl, T. R., Kunkel, K. E. & Ambenje, P., 1999. Observed variability and trends in extreme climate events. A brief review. 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