A physical concept of soil-water equilibria for nonionic organic compounds

Soil-water equilibrium data suggest that the transfer of nonionic chemicals from water to soil may be described in terms of a hypothesis of solute partitioning in the soil organic matter. This concept allows estimation of soil-water distribution coefficients either from solvent-water partition coeff...

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Veröffentlicht in:Science (American Association for the Advancement of Science) 1979-11, Vol.206 (4420), p.831-832
Hauptverfasser: Chiou, Cary T., Peters, Louis J., Freed, Virgil H.
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container_title Science (American Association for the Advancement of Science)
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creator Chiou, Cary T.
Peters, Louis J.
Freed, Virgil H.
description Soil-water equilibrium data suggest that the transfer of nonionic chemicals from water to soil may be described in terms of a hypothesis of solute partitioning in the soil organic matter. This concept allows estimation of soil-water distribution coefficients either from solvent-water partition coefficients or aqueous solubilities.
doi_str_mv 10.1126/science.206.4420.831
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identifier ISSN: 0036-8075
ispartof Science (American Association for the Advancement of Science), 1979-11, Vol.206 (4420), p.831-832
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source JSTOR Archive Collection A-Z Listing; American Association for the Advancement of Science
subjects Agricultural soils
Isotherms
Organic soils
Silt loam soils
Soil biochemistry
Soil organic matter
Soil science
Soil water
Solubility
Sorption
title A physical concept of soil-water equilibria for nonionic organic compounds
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