soil capillary water

Above the interface of air-soil waer distribution profile in entire soil column is similar to the capillary rising blet above ground water table.

在邻近空气-土质界面之上，水分处于饱和，整个土柱剖面水分分布类似地下水位之上的毛管上升带一样。

The results showed that the maximum height of the capillary water rise of layered soil was mainly determined by the sand soil texture, position, thickness and their mutual relationship, and they also were closer connected with other soil texture in the profile.

结果表明：层状土壤毛管水的最大上升高度取决于夹层土壤的质地、厚度、层位及其相互关系，同时也与土壤剖面中其它土壤的质地密切相关。

And the soil saturation water capacity increased from 5.7% to 118.8%, the non-capillary water capacity was over 2.58~ 19.13 times to sloping field;

退耕还林后土壤饱和蓄水量增加5·7%~118·8%，非毛管蓄水量为坡耕地的2·58~19·13倍；