节点文献

求解黄土含水层水文地质参数的流量-时间配线法

Discharge-time curve fitting method for calculating hydrogeological parameters in loess aquifer

  • 推荐 CAJ下载
  • PDF下载
  • 不支持迅雷等下载工具,请取消加速工具后下载。

【作者】 张学真常安定

【Author】 ZHANG Xue-zhen,CHANG An-ding (Faculty of Environmental Science and Engineering,Chang’an University, Xi’an 710054,China)

【机构】 长安大学环境科学与工程学院

【摘要】 利用基于割离井法的流量-时间配线法反求抽水过程黄土含水层水文地质参数,并与裘布依公式法、割离井公式法的求解结果进行对比。计算结果表明,黄土含水层水文地质参数的求解选用流量-时间配线法求解精度高,可以减少繁琐的计算,结果是可靠的。根据稳定流井流理论,抽水过程观测孔的水位降深值S和观测孔到主井的距离的对数lgr存在一定的关系。利用Dpp软件包的图像处理功能,对实测点据在平面内进行拟合,确定了抽水井影响半径为172 m,确定了抽水过程Q-S、q-S关系曲线方程。

【Abstract】 The discharge-time curve fitting method based on the isolated well method was used to calculate the hydrogeological parameters in the process of pumping.Compared with the Dupuit Equation and isolated well method,the results of the new method are more accurate and reliable,and its solution process is simpler.According to steady well flow theories,the water table decline at the observation well,S,has a certain relationship with the logarithm of the distance between the observation well and the main well,lgr,in the pumping process.By plane fitting of the measured data using an image processing function of the software Dpp,it is found that the influence radius of the pumping well is 172 m.The Q-S and q-S curves in the pumping process are also presented.

【基金】 陕西省科技厅资助项目(2002K09-GB)
  • 【文献出处】 水资源保护 ,Water Resources Protection , 编辑部邮箱 ,2009年01期
  • 【分类号】P641.2
  • 【被引频次】4
  • 【下载频次】150
节点文献中: 

本文链接的文献网络图示:

本文的引文网络