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 inJournal of environmental quality Vol. 30; no. 3; pp. 1059 - 1063
Main Authors Lu, Peng, O'Connor, George A.
Format Journal Article
LanguageEnglish
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
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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.
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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Issue 3
Keywords Aluminium oxide
Iron oxide
Pollutant behavior
Adsorption capacity
Property of soil
Mobility
Phosphorus
Sandy soil
Sewage sludge
Amendment
Lixiviation
Nutrient
Soil interaction
Language English
License CC BY 4.0
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Notes Contribution of the Florida Agric. Exp. Stn. Journal Series no. R‐07430.
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PublicationTitle Journal of environmental quality
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Crop Science Society of America
American Society of Agronomy
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Snippet 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...
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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StartPage 1059
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
Volume 30
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