Biosolids Effects on Phosphorus Retention and Release in Some Sandy Florida Soils
ABSTRACT The soil solid phase components most responsible for P sorption in Florida soils are Fe and Al oxides. Thus, we hypothesized that land application of biosolids would significantly increase a soil's P retention by increasing its content of P‐sorbing solids, especially when biosolids wit...
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Published in | Journal of environmental quality Vol. 30; no. 3; pp. 1059 - 1063 |
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Main Authors | , |
Format | Journal Article |
Language | English |
Published |
Madison
American Society of Agronomy, Crop Science Society of America, Soil Science Society
01.05.2001
Crop Science Society of America American Society of Agronomy |
Subjects | |
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Abstract | ABSTRACT
The soil solid phase components most responsible for P sorption in Florida soils are Fe and Al oxides. Thus, we hypothesized that land application of biosolids would significantly increase a soil's P retention by increasing its content of P‐sorbing solids, especially when biosolids with high Fe and Al concentrations are applied to soils that sorb P poorly. Biosolids effects were quantified by a series of single‐point isotherms on soils from two field studies sampled for up to 4 yr after initial biosolids application. Biosolids additions had little effect on P retention in a soil with abundant oxalate‐extractable Fe and Al and a correspondingly large native P‐sorbing capacity. However, biosolids significantly increased P retention in a soil with low oxalate‐extractable Fe and Al content and low native P‐sorbing capacity. Biosolids effects on P retention lasted 1 to 3 yr after application, depending on biosolids source and rate of application, and generally mimicked persistence of increased extractable Fe and Al concentrations in the poorly P‐sorbing soil. Disappearance of added Fe and Al (and, hence, P retention capacity) from the surface horizons over time was relatively rapid, perhaps due to abundant organic acid production associated with biosolids degradation. Phosphorus in biosolids containing (or tailored to contain) abundant Fe and/or Al can be expected to behave as a slowly available P source, and to be less subject to leaching losses than completely soluble P sources. |
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AbstractList | The soil solid phase components most responsible for P sorption in Florida soils are Fe and Al oxides. Thus, we hypothesized that land application of biosolids would significantly increase a soil's P retention by increasing its content of P‐sorbing solids, especially when biosolids with high Fe and Al concentrations are applied to soils that sorb P poorly. Biosolids effects were quantified by a series of single‐point isotherms on soils from two field studies sampled for up to 4 yr after initial biosolids application. Biosolids additions had little effect on P retention in a soil with abundant oxalate‐extractable Fe and Al and a correspondingly large native P‐sorbing capacity. However, biosolids significantly increased P retention in a soil with low oxalate‐extractable Fe and Al content and low native P‐sorbing capacity. Biosolids effects on P retention lasted 1 to 3 yr after application, depending on biosolids source and rate of application, and generally mimicked persistence of increased extractable Fe and Al concentrations in the poorly P‐sorbing soil. Disappearance of added Fe and Al (and, hence, P retention capacity) from the surface horizons over time was relatively rapid, perhaps due to abundant organic acid production associated with biosolids degradation. Phosphorus in biosolids containing (or tailored to contain) abundant Fe and/or Al can be expected to behave as a slowly available P source, and to be less subject to leaching losses than completely soluble P sources. Surface-soil samples were collected from two field studies in Florida of bahiagrass Paspalum notatum response to biosolids applications, and the effects of biosolids on phosphorus retention and release for up to 4 yr were determined. Phosphorus sorption appeared to be unaffected by additions of biosolids to the Millhopper soil, due to its large native iron and aluminum contents and associated large P sorption capacity. At the other site, however, the Immokalee soil sorbed much less P and contained much less native Fe and Al. The increase in P sorption at the site was proportional roughly to the biosolids application rate. Phosphorus retention remained significantly greater than in the control samples well into the third year, but the biosolids rate effects disappeared by the end of the year, and there were only minor effects of biosolids application on P retention in the fourth year. The greater P retention was attributed to increases in oxalate-extractable Fe and Al contents from biosolids application. ABSTRACT The soil solid phase components most responsible for P sorption in Florida soils are Fe and Al oxides. Thus, we hypothesized that land application of biosolids would significantly increase a soil's P retention by increasing its content of P‐sorbing solids, especially when biosolids with high Fe and Al concentrations are applied to soils that sorb P poorly. Biosolids effects were quantified by a series of single‐point isotherms on soils from two field studies sampled for up to 4 yr after initial biosolids application. Biosolids additions had little effect on P retention in a soil with abundant oxalate‐extractable Fe and Al and a correspondingly large native P‐sorbing capacity. However, biosolids significantly increased P retention in a soil with low oxalate‐extractable Fe and Al content and low native P‐sorbing capacity. Biosolids effects on P retention lasted 1 to 3 yr after application, depending on biosolids source and rate of application, and generally mimicked persistence of increased extractable Fe and Al concentrations in the poorly P‐sorbing soil. Disappearance of added Fe and Al (and, hence, P retention capacity) from the surface horizons over time was relatively rapid, perhaps due to abundant organic acid production associated with biosolids degradation. Phosphorus in biosolids containing (or tailored to contain) abundant Fe and/or Al can be expected to behave as a slowly available P source, and to be less subject to leaching losses than completely soluble P sources. The soil solid phase components most responsible for P sorption in Florida soils are Fe and Al oxides. Thus, we hypothesized that land application of biosolids would significantly increase a soil's P retention by increasing its content of P-sorbing solids, especially when biosolids with high Fe and Al concentrations are applied to soils that sorb P poorly. Biosolids effects were quantified by a series of single-point isotherms on soils from two field studies sampled for up to 4 yr after initial biosolids application. Biosolids additions had little effect on P retention in a soil with abundant oxalate-extractable Fe and Al and a correspondingly large native P-sorbing capacity. However, biosolids significantly increased P retention in a soil with low oxalate-extractable Fe and Al content and low native P-sorbing capacity. Biosolids effects on P retention lasted 1 to 3 yr after application, depending on biosolids source and rate of application, and generally mimicked persistence of increased extractable Fe and Al concentrations in the poorly P-sorbing soil. Disappearance of added Fe and Al (and, hence, P retention capacity) from the surface horizons over time was relatively rapid, perhaps due to abundant organic acid production associated with biosolids degradation. Phosphorus in biosolids containing (or tailored to contain) abundant Fe and/or Al can be expected to behave as a slowly available P source, and to be less subject to leaching losses than completely soluble P sources.The soil solid phase components most responsible for P sorption in Florida soils are Fe and Al oxides. Thus, we hypothesized that land application of biosolids would significantly increase a soil's P retention by increasing its content of P-sorbing solids, especially when biosolids with high Fe and Al concentrations are applied to soils that sorb P poorly. Biosolids effects were quantified by a series of single-point isotherms on soils from two field studies sampled for up to 4 yr after initial biosolids application. Biosolids additions had little effect on P retention in a soil with abundant oxalate-extractable Fe and Al and a correspondingly large native P-sorbing capacity. However, biosolids significantly increased P retention in a soil with low oxalate-extractable Fe and Al content and low native P-sorbing capacity. Biosolids effects on P retention lasted 1 to 3 yr after application, depending on biosolids source and rate of application, and generally mimicked persistence of increased extractable Fe and Al concentrations in the poorly P-sorbing soil. Disappearance of added Fe and Al (and, hence, P retention capacity) from the surface horizons over time was relatively rapid, perhaps due to abundant organic acid production associated with biosolids degradation. Phosphorus in biosolids containing (or tailored to contain) abundant Fe and/or Al can be expected to behave as a slowly available P source, and to be less subject to leaching losses than completely soluble P sources. |
Author | O'Connor, George A. Lu, Peng |
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Copyright | Published in J. Environ. Qual.30:1059–1063. 2001 INIST-CNRS Copyright American Society of Agronomy, Inc. May/Jun 2001 |
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Keywords | Aluminium oxide Iron oxide Pollutant behavior Adsorption capacity Property of soil Mobility Phosphorus Sandy soil Sewage sludge Amendment Lixiviation Nutrient Soil interaction |
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The soil solid phase components most responsible for P sorption in Florida soils are Fe and Al oxides. Thus, we hypothesized that land application of... The soil solid phase components most responsible for P sorption in Florida soils are Fe and Al oxides. Thus, we hypothesized that land application of biosolids... Surface-soil samples were collected from two field studies in Florida of bahiagrass Paspalum notatum response to biosolids applications, and the effects of... |
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SubjectTerms | Absorption Acid production Agronomy. Soil science and plant productions aluminum Aluminum Oxide Aluminum Oxide - chemistry analysis Applied sciences Biological and medical sciences Biological and physicochemical properties of pollutants. Interaction in the soil Biosolids chemistry Earth sciences Earth, ocean, space Engineering and environment geology. Geothermics Exact sciences and technology Ferric Compounds Ferric Compounds - chemistry Florida Fundamental and applied biological sciences. Psychology General agronomy. Plant production Hydrogen-Ion Concentration iron iron oxides land application Leaching Ligands measurement Organic acids Organic Chemicals Organic phosphorus Other nutrients. Amendments. Solid and liquid wastes. Sludges and slurries Paspalum notatum phosphorus Phosphorus - chemistry Pollution Pollution, environment geology Retention Retention capacity sandy soils soil soil amendments Soil and sediments pollution Soil and water pollution Soil Pollutants Soil Pollutants - analysis soil pollution Soil science Soil-plant relationships. Soil fertility. Fertilization. Amendments Soils soluble phosphorus sorption sorption isotherms waste utilization |
Title | Biosolids Effects on Phosphorus Retention and Release in Some Sandy Florida Soils |
URI | https://onlinelibrary.wiley.com/doi/abs/10.2134%2Fjeq2001.3031059x https://www.ncbi.nlm.nih.gov/pubmed/11401253 https://www.proquest.com/docview/197395668 https://www.proquest.com/docview/14578821 https://www.proquest.com/docview/2352451480 https://www.proquest.com/docview/49102775 https://www.proquest.com/docview/70919311 |
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