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- W2023652444 abstract "Abstract The kinetics of phosphorus (P) desorption by six Greek soils, four Alfisols and two Entisols, have been studied. By the addition of several amounts of P fertilizers at different water/soil rations and different contact times, that amount of P fertilizer required for the two major categories for Greek soils in order to avoid enviromental pollution from overdoses was determined. The experimental data lead to the same desorption model as given by Sharpley (1981): Pd = kPot∂wb; where, Pd is the amount of P desorption from the soil in μg P/g soil, Po the amount of P fertilizers in grams added into the soil, t the contact time of P fertilizers with the soil, w the water/soil rations, and k, ∂, and b constants. The values of the ∂, k, and b constants for each soil are nearly the same for all the experimental conditions. For the Entisols, the ∂ values are lower than for the Alfisols. Calcium carbonate (CaCO3) and exchangeable Ca of the Entisols influenced negatively the desorption‐time relationship, while exchangeable Fe and Mn, and the low CEC of the Alfisols had a positive influence. For the Entisols, the b values are higher than for the Alfisols, except for the Agrinio B soil. The clay silty soils with high CECs and low exchangeable Fe and Mn had a positive influence on the the desoption water‐soil relationship. Since the values for the ∂, K, and b constants for each soil are almost the same, the average of these values can be used in the Shapley model for the determination of desorbed P for each agricultural use for the two major categories of Greek soils." @default.
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- W2023652444 date "1993-06-01" @default.
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- W2023652444 title "Kinetic study of phosphorus desorption by Alfisols and Entisols" @default.
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- W2023652444 doi "https://doi.org/10.1080/00103629309368855" @default.
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