SSSAJ Grow Your Career with SSSA
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


This Article
Right arrow Figures Only
Right arrow Full Text Free
Right arrow Full Text (PDF) Free
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Similar articles in this journal
Right arrow Similar articles in ISI Web of Science
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via ISI Web of Science (10)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Vadas, P. A.
Right arrow Articles by Sims, J. T.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Vadas, P. A.
Right arrow Articles by Sims, J. T.
GeoRef
Right arrow GeoRef Citation
Agricola
Right arrow Articles by Vadas, P. A.
Right arrow Articles by Sims, J. T.
Related Collections
Right arrow Surface Water Quality
Right arrow Soil Models
Right arrow Soil Chemistry
Soil Science Society of America Journal 66:623-631 (2002)
© 2002 Soil Science Society of America


DIVISION S-8—NUTRIENT MANAGEMENT & SOIL & PLANT ANALYSIS

Predicting Phosphorus Desorption from Mid-Atlantic Coastal Plain Soils

Peter A. Vadas*,a and J. Thomas Simsb

a USDA, ARS, ANRI, AMBL, B-163F Rm. 5, BARC-East, 10300 Baltimore Ave., Beltsville, MD 20705
b Dep. of Plant and Soil Sciences, 152 Townsend Hall, University of Delaware, Newark, DE 19717

* Corresponding author (pvadas{at}anri.barc.usda.gov)

Pollution of surface waters by P from agricultural areas is a water quality issue in Delaware. The FHANTM 2.0 computer model can help identify areas with a high potential for P loss, but the model's representation of P desorption from soils to runoff waters needs re-evaluation. The equation, Pd = K Po t{alpha} Wß, has been proposed to predict such P desorption, but equations originally proposed to predict values for the constants K, {alpha}, and ß from the ratio of soil clay content/soil organic C content may not be accurate for Delaware soils. Therefore, we measured P desorption for 23 sandy Delaware soils for times of 5 to 180 min, water/soil ratios of 10 to 1000 L kg-1, and three initial levels of soil desorbable P. Values for the constants K, {alpha}, and ß were calculated and related to soil properties. We found that K, {alpha}, and ß values were not well related to clay/OC, but were better related to the ratio of oxalate-extractable Fe/OC content ({alpha}) or the sum of oxalate extractable Fe and Al (ß and K). These results can be used to help refine the FHANTM 2.0 model in predicting P loss from agricultural areas in Delaware and similar landscapes in the Mid-Atlantic Coastal Plain.

Abbreviations: Alox, acid ammonium oxalate-extractable Al • AWS, amount of rainfall needed to saturate the topsoil layer in the FHANTM 2.0 model • B, extraction coefficient used in the FHANTM 2.0 model • (Cav)p, quantity of P in the topsoil available for runoff used in the FHANTM 2.0 model • CPLAB, quantity of desorbable P in the topsoil used in the FHANTM 2.0 model • (Cw)p, concentration of P in runoff used in the FHANTM 2.0 model • Feox, acid ammonium oxalate-extractable Fe • FHANTM, Field Hydrologic and Nutrient Transport Model • OC, organic C • OM, organic matter • UDSTP, University of Delaware Soil Testing Program • K, empirical constant in soil P desorption equation • Kd, partitioning coefficient used in the FHANTM 2.0 model • Pd, amount of P desorbed from the soil • Po, initial concentration of desorbable P in soil • POR, porosity used in the FHANTM 2.0 model • Pr, value for precipitation used in the FHANTM 2.0 model • Q, value for runoff used in the FHANTM 2.0 model • SSG, soil specific gravity used in the FHANTM 2.0 model • t, time of P desorption • TMDL, total maximum daily load • W, water/soil ratio during P desorption • {alpha}, empirical constant in soil P desorption equation • ß, empirical constant in soil P desorption equation




This article has been cited by other articles:


Home page
Soil Sci.Home page
C. J. Penn, G. L. Mullins, L. W. Zelazny, and A. N. Sharpley
Estimating Dissolved Phosphorus Concentrations in Runoff from Three Physiographic Regions of Virginia
Soil Sci. Soc. Am. J., September 20, 2006; 70(6): 1967 - 1974.
[Abstract] [Full Text] [PDF]


Home page
Soil Sci.Home page
P. A. Vadas, T. Krogstad, and A. N. Sharpley
Modeling Phosphorus Transfer between Labile and Nonlabile Soil Pools: Updating the EPIC Model
Soil Sci. Soc. Am. J., March 29, 2006; 70(3): 736 - 743.
[Abstract] [Full Text] [PDF]


Home page
Soil Sci.Home page
Y. Arai, K. J. T. Livi, and D. L. Sparks
Phosphate Reactivity in Long-Term Poultry Litter-Amended Southern Delaware Sandy Soils
Soil Sci. Soc. Am. J., April 11, 2005; 69(3): 616 - 629.
[Abstract] [Full Text] [PDF]


Home page
J. Environ. Qual.Home page
K. E. Staats, Y. Arai, and D. L. Sparks
Alum Amendment Effects on Phosphorus Release and Distribution in Poultry Litter-Amended Sandy Soils
J. Environ. Qual., September 1, 2004; 33(5): 1904 - 1911.
[Abstract] [Full Text] [PDF]


Home page
Soil Sci.Home page
M. T. Siddique and J. S. Robinson
Differences in Phosphorus Retention and Release in Soils Amended with Animal Manures and Sewage Sludge
Soil Sci. Soc. Am. J., July 1, 2004; 68(4): 1421 - 1428.
[Abstract] [Full Text] [PDF]


Home page
Soil Sci.Home page
P. A. Vadas, J. T. Sims, A. B. Leytem, and C. J. Penn
Modifying FHANTM 2.0 to Estimate Phosphorus Concentrations in Runoff from Mid-Atlantic Coastal Plain Soils
Soil Sci. Soc. Am. J., November 1, 2002; 66(6): 1974 - 1980.
[Abstract] [Full Text] [PDF]




HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Agronomy Journal Crop Science
Journal of Natural Resources
and Life Sciences Education
Vadose Zone Journal
Journal of Plant Registrations Journal of
Environmental Quality
The Plant Genome
Copyright © 2002 by the Soil Science Society of America.