对缓坡地在土壤饱和情形下土壤溶质的流失过程进行了室内模拟实验,研究结果表明,在缓坡地,只考虑坡地上方来水对饱和土壤的作用,土壤溶质、水土的流失过程更适合采用幂函数来描述,而且溶质受土壤吸附的特性也影响其流失速率,但并不影响其流失过程的规律性。 Indoor simulation experiments were carried out on the process of soil solute loss in the gentle slope with the soil saturated. The results show that only the action of the incoming water on the saturated soil is considered in the gentle slope, and the process of soil solute and soil erosion is more suitable Function, and the solute adsorbed by the soil properties also affect the rate of its loss, but does not affect the regularity of its loss process.