摘要
地下水微动态形成过程中的水动力学机制是很重要的。笔者利用模拟试验装置,在三种不同的渗透介质与二种不同温度的水的条件下,进行了井孔水位或流量对含水层内各种孔隙压力变化的响应方面的一系列试验研究。本文叙述了这一试验的装置、方法与某些结果。
It is important to know the hydrodynamic mechanism in the formation process of ground-water microbehavior. The authors here carried out a series of experiments to study the water table or flow capacity in a modeling well in response to various changes of pore fluid pressure in the modeling aquifer under conditions of three different permeable media and two different water temperatures. This paper describes the experimental facilities, methods and some of the results.
出处
《地震》
CSCD
北大核心
1989年第5期40-49,共10页
Earthquake
