Abstract
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.
Original language | English |
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Pages (from-to) | 831-832 |
Number of pages | 2 |
Journal | Science |
Volume | 206 |
Issue number | 4420 |
DOIs | |
Publication status | Published - 1979 |
All Science Journal Classification (ASJC) codes
- General