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笔者基本上赞同原文的观点.另外,根据我们的调查及试验所得,提几点意见供商榷. (一)地下水上升运动的土壤剖面上,毛管破裂含水率出现的高度和毛管上升最大高度相当.笔者认为,地下水在土壤剖面上的上升运动,第一步是水压支持的上升运动;第二步是毛管运动;第三步是薄膜运动;第四步是水汽扩散运动.总之,在土壤中普温存在不同机制的土壤水分运动,在地下水上升运动的整个运动过程中,也是毫不例外的存在着。在室內用足够长的玻璃管装取干燥土样测定地下水上
In addition, based on our investigation and experimental findings, I would like to make a few comments for discussion. (1) In the soil profile of groundwater rising movement, the height of capillary rupture moisture content is the same as the maximum height of capillary rise. The author believes that the groundwater in the soil profile of the rising movement, the first step is the water pressure to support the rising movement; the second step is the capillary movement; the third step is the film movement; the fourth step is the diffusion of water vapor movement.In short, in the soil The existence of different mechanisms of soil moisture movement in Prawen exists, without exception, throughout the movement of groundwater ascending movement. Indoors, use a long enough glass tube to collect dry soil samples for determination of groundwater