煤炭工程 ›› 2016, Vol. 48 ›› Issue (4): 65-67.doi: 10.11799/ce201604020

• 生产技术 • 上一篇    下一篇

“降深分配法”在反求水文地质参数中的应用

崔思源1,孙亚军2,甄战战1   

  1. 1. 中国矿业大学(徐州)资源与地球科学学院
    2. 中国矿业大学
  • 收稿日期:2015-10-28 修回日期:2015-12-22 出版日期:2016-04-10 发布日期:2016-04-18
  • 通讯作者: 崔思源 E-mail:348306702@qq.com

Application of 'Drwandown Distribution Method' in Reverse-seeking Hydrogeological Parameters

  • Received:2015-10-28 Revised:2015-12-22 Online:2016-04-10 Published:2016-04-18

摘要: 针对我国西部弱胶结砂岩含水介质抽水试验中存在的求参结果偏小问题,根据降深叠加原理和降深分配原则,利用群孔抽水、无专门观测孔抽水资料,采用降深分配系数法对渗透系数进行反求参,并利用FEFLOW模型进行验证。结果表明,与常规方法所求参数对比,采用降深分配系数法所求参数更能反映含水层的性质。

关键词: 降深分配法, 群孔抽水, 弱胶结砂岩, 渗透系数, FEFLOW模型

Abstract: Pumping test is one of the primary means of determining the hydrogeological parameters, and identifying the hydrogeological conditions. For the results that calculated in common pumping test is usually smaller than its truthful data, in weakly cemented sandstone aquifer in western China, this paper aiming at seeking the K parameter by the reverse-seeking method. According to the drawdown superposition principle and drawdown distribution principle, this paper makes use of drawdown-distribution-coefficient to calculate the K factor, in a group pumping wells test and without specially observation hole. Then compare the results with the parameter which is evaluated by the conventional method, and verify the result by the FEFLOW model. The results show that the parameter which is calculated by drawdown-distribution-coefficient can reflect the nature of the aquifer more better.

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