单孔稳定流抽水试验渗透系数分析
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A tentative study of permeability coefficient on single-hole steady flow pumping tests
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    摘要:

    由于水文地质本身的复杂性和计算的多样性,致使渗透系数计算值往往存在着较大的差异。以台格庙勘查区XJ-7钻孔煤系地层含水层完整井稳定流抽水试验为例,分别利用水位下降资料和水位恢复资料分析计算,通过对比验证,后者计算结果 K=0.058 9 m·d-1更加精确与合理。表明单孔稳定流抽水试验中,利用裘布依公式求得的渗透系数精确度不高,水位恢复期人为和机械因素干扰较小,结果更具可靠性。

    Abstract:

    There is a huge discrepancy between the calculated permeability coefficient and the actual situation of the aquifer being due to some factors such as the complexity of the hydrogeology and the diversity and relative difficulty of counting accurately. With specific illustration,this paper will take the experiment with the steady flow pumping test of the fully penetrating well in the coal-bearing strata aquifer in XJ-7,an exploration area,as an example. In this experiment,we took different methods of analyzing the statistics of groundwater level decrease and water-level recovery respectively. Through the comparison between these two methods,we find out that the result of the latter counting method that K = 0. 058 9 m·d-1is much accurate and reasonable. This experiment thus demonstrates the permeability coefficient is of low accuracy when applying the Dupuit Formula into the practice of single-hole steady flow pumping test. By contrast,the counting result in the water-level recovery period is much more reliable because of the smaller and insignificant influence of both human and mechanical factors.

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汪星晨,关英斌,张立,李金龙,马亚波.单孔稳定流抽水试验渗透系数分析[J].河北工程大学自然版,2014,31(3):78-81

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  • 收稿日期:2014-03-12
  • 在线发布日期: 2015-01-12
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