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一种测求水井含水层导水系数的新方法
引用本文:张照栋,郑香媛.一种测求水井含水层导水系数的新方法[J].华南地震,1990,10(3):18-24.
作者姓名:张照栋  郑香媛
作者单位:山东省地震局 济南 (张昭栋,张教祥),国家地震局分析预报中心 北京 (郑香媛),国家地震局分析预报中心 北京(殷积涛)
基金项目:地震科学联合基金资助的课题的部分成果
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。

关 键 词:水井  含水层  导水系数  cooper理论

A NEW METHOD OF DETERMINATION OF TRANSMISSIBILITY IN WELL AQUIFER
Zhang Zhaodong Zheng Xiangyuan Yen Jitao Zhang Jiaoxiang Seismological Bureau of Shandong Province,Jinan, Centre for Analysis and Predition,S S B,Beijing.A NEW METHOD OF DETERMINATION OF TRANSMISSIBILITY IN WELL AQUIFER[J].South China Journal of Seismology,1990,10(3):18-24.
Authors:Zhang Zhaodong Zheng Xiangyuan Yen Jitao Zhang Jiaoxiang Seismological Bureau of Shandong Province  Jinan  Centre for Analysis and Predition  S S B  Beijing
Abstract: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.
Keywords:Transmissibility  The Cooper's theory  Vibration theory  Well aquifer  
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