毛乌素沙地降雨入渗和蒸发特征
Characteristics of rainwater infiltration and evaporation in Mu Us Sandland
-
摘要: 通过室内和野外模拟降雨的入渗和蒸发实验,研究不同降雨量条件下,沙地的最大入渗深度、入渗速率以及每天的蒸发量。结果表明:降雨量大小对沙地的入渗深度、入渗速率影响显著,并且不同下渗深度的水分在沙土中保存时间不同,1、2、5和10mm降雨分别在4、6、11和15 d左右全部蒸发,而15mm以上的降雨由于稳定干沙层的抑制作用,除了一部分蒸发以外,还有部分水分保存在沙土中。同时由于沙区不同植被根系的垂直分布差异较大,所以,降雨量越大,入渗越深,越能被深根性植被所利用,且利用时间越长。Abstract: By indoor and field simulated experiments of infiltration and evaporation of the rainwater,the paper studies the depth and velocity of infiltration and the daily evaporation.The result indicates that the effects of different rainfall amount on depth and velocity of infiltration are significant.The preserved time of rainwater in the sand soil is different.It spends 4,6,11,15 d to evaporate rainwater of 1,2,5,10 mm.Apart from some evaporated,a part of the 15 mm rainwater is kept in the sand soil because of a dry layer of sandland.Due to the great difference of vertical distribution of the various plant roots,the more rainfall and the deeper the infiltration,the more rainwater can be used by deep-rooted plants in a longer period.
下载: