摘要
本文给出了一种测求水井含水层导水系数的新方法。利用Cooper理论和振动理论,通过简单的试验,可以测求出水井含水层的导水系数。用这种方法计算出珍珠泉井含水层的导水系数为2439m^2/d,用抽水试验法测得该系数为2618m^2/d,两者符合得较好。
A new method of determination of the transmissibility in a well aquifer is described in this paper. By using the Cooper's and the vibration theory and through a simple test, the transmissibility in a well aquifer can be determined. For example, in the well of Pearl Spring, it is calculated as 2439m2/day, which tallies with the one determined by the pumping test, 2618m2/day.
出处
《华南地震》
1990年第3期18-24,共7页
South China Journal of Seismology
基金
地震科学联合基金资助的课题的部分成果
关键词
水井
含水层
导水系数
cooper理论
Transmissibility
The Cooper's theory
Vibration theory
Well aquifer.
