基于压水试验的均质含水层渗透系数计算方法

袁东,张奇华

长江科学院院报 ›› 2014, Vol. 31 ›› Issue (8) : 77-81.

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长江科学院院报 ›› 2014, Vol. 31 ›› Issue (8) : 77-81. DOI: 10.3969/j.issn.1001-5485.2014.08.0152014,31(08):77-81
岩土工程

基于压水试验的均质含水层渗透系数计算方法

  • 袁东,张奇华
作者信息 +

Method of Calculating Permeability Coefficient Using Water PressureTest in Homogeneous Aquifer

  • YUAN Dong,ZHANG Qi-hua
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摘要

从常规吕荣值计算公式出发,分析了用压水试验中的吕荣值作为衡量岩体透水能力定量指标存在的不足,推导出均质条件下压水试验中稳定流和非稳定流状态下的渗透系数计算公式。该公式完善了压水试验数据的分析计算法。选取锦屏一级水电站帷幕灌浆检测孔实测压水数据,采用稳定流及非稳定流方法分别计算其渗透系数,结果表明在短历时压水中采用非稳定流方法计算的渗透系数小于稳定流的计算值。因此,采用非稳定流计算的结果准确性较高。

Abstract

On the basis of the formulae for the Lugeon value, the shortage of Lugeon as a quantitative indicator of rock permeability in water pressure test is analyzed. By deducing the calculation formula of permeability coefficient with steady flow and unsteady flow in homogeneous postulation water pressure test, we believe that the accuracy of calculation result is higher in the presence of unsteady flow. Moreover, with Jinping-I hydropower station as an example, we calculated the permeability coefficient respectively in steady flow and unsteady flow conditions based on the measured water pressure test data of the grouting inspection drilling. The results demonstrate that the permeability coefficient in unsteady flow condition is less than that in steady flow condition in short duration water pressure test.

关键词

压水试验 / 均质含水层 / 稳定流 / 非稳定流 / 渗透系数

Key words

water pressure test / homogeneous aquifer / steady flow / unsteady flow / permeability coefficient

引用本文

导出引用
袁东,张奇华. 基于压水试验的均质含水层渗透系数计算方法[J]. 长江科学院院报. 2014, 31(8): 77-81 https://doi.org/10.3969/j.issn.1001-5485.2014.08.0152014,31(08):77-81
YUAN Dong,ZHANG Qi-hua. Method of Calculating Permeability Coefficient Using Water PressureTest in Homogeneous Aquifer[J]. Journal of Changjiang River Scientific Research Institute. 2014, 31(8): 77-81 https://doi.org/10.3969/j.issn.1001-5485.2014.08.0152014,31(08):77-81
中图分类号: TU45   

参考文献

[1] WAY S C,MCKEE C R. In-situ Determination of Three-dimensional Aquifer Permabilities[J]. Groundwater, 1982, 20(5): 594-603.
[2] BARKER J A. A Generalized Radial-flow Model for Pumping Test in Fractured Rock[J]. Water Resources Research, 1988, 24(4): 1796-1804.
[3] DERSHOWITZ W S,DOE T W. Analysis of Heterogeneously Connected Rock Masses by Forward Modeling of Fractional Dimension Flow Behavior[J]. International Journal of Rock Mechanics and Mining Sciences,1997,34(3/4): 652-663.
[4] 张桢武,李兴成,徐光详. 利用定压力非稳定流压水试验求水文地质参数[J]. 岩石力学与工程学报, 2004,23(15):2543-2546.(ZHANG Zhen-wu, LI Xing-cheng, XU Guang-xiang. Determination of Hydrogeological Parameters by Water Pressure Test of Steady-Pressure and Non-stationary Flow[J]. Chinese Journal of Rock Mechanics and Engineering,2004, 23(15):2543-2546. (in Chinese))
[5] DL/T 5331—2005,水电水利工程钻孔压水试验规程[S]. 北京:中国电力出版社,2005. (DL/T 5331—2005,Code of Water Pressure Test in Borehole for Hydropower and Water Resources Engineering[S]. Beijing:China Electric Power Press, 2005.(in Chinese))

基金

国家青年科学基金项目(41202223);中央级公益性科研院所基本科研业务费项目(CKSF2013043)

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