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 coefficients or aqueous solubilities.
Chiou
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CT
Peters
L J
LJ
Freed
V H
VH