Science. 1979 Nov 16;206(4420):831-2. doi: 10.1126/science.206.4420.831.
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.
土壤-水平衡数据表明,非离子化学物质从水中向土壤的转移可以用溶质在土壤有机质中分配的假说来描述。这一概念允许根据溶剂-水分配系数或水溶解度来估算土壤-水分配系数。