水分渗入含钾离子均质黄土的试验研究

Experiments study on water infiltrating into homogeneous loess with K^+

通过室内试验研究结果表明 ,在入渗过程中 ,单位土壤对钾离子的吸附量相等 ;吸附量与参与吸附的土壤总量成正比。当土壤钾离子含量不同时 ,对入渗过程有明显影响。入渗时间相同 。

It is shown by experiments in the laboratory that during water infiltrating into homogeneous loess with KCl, the amount of K + aborbed by loess is proportional to the volume of the soil, and that the total infiltration amount and wetting front position are decreasing with the K + content increasing.