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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
Wß, has been proposed to predict such P desorption, but equations originally proposed to predict values for the constants K,
, 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,
, and ß were calculated and related to soil properties. We found that K,
, and ß values were not well related to clay/OC, but were better related to the ratio of oxalate-extractable Fe/OC content (
) 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
, empirical constant in soil P desorption equation ß, empirical constant in soil P desorption equation
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