摘要
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.
原文 | English |
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頁(從 - 到) | 831-832 |
頁數 | 2 |
期刊 | Science |
卷 | 206 |
發行號 | 4420 |
DOIs | |
出版狀態 | Published - 1979 |
All Science Journal Classification (ASJC) codes
- 多學科