| 直角正交电网络模型上对裂隙和岩溶含水层的模拟 |
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| 引用本文： | 陈明征.直角正交电网络模型上对裂隙和岩溶含水层的模拟[J].地球科学,1985(1). |
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| 作者姓名： | 陈明征 |
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| 作者单位： | Wuhan College of Geology，Wuhan 430074 |
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| 摘 要： | 笔者对×水电站库区左岸的渗漏进行了直角正交电网络模拟。圈定了裂隙发育强带及岩溶通道的位置,并用不同比例(对全区1:2000,对裂隙带1:500,对岩溶通道1:125)进行模拟,得出了渗漏量。其结果与实际资料基本吻合。
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| 关 键 词： | 裂隙水 岩溶水 直角正交电模拟 渗透率 |
THE USE OF SQUARE MASH ELECTRIC ANALOG OF MODELLING OF FRACTURE AND KARST AQUIFERS |
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| Chen Ming-zheng.THE USE OF SQUARE MASH ELECTRIC ANALOG OF MODELLING OF FRACTURE AND KARST AQUIFERS[J].Earth Science-Journal of China University of Geosciences,1985(1). |
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| Authors: | Chen Ming-zheng |
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| Abstract: | The author has used square mesh electrie analog to measure the left side seepage of some hydropowers tation reservoirs. Have been found out the location of fracture zone and karst channels and applied different scales (for the whole regime 1:2000, for fracture zone 1:500, for karst channels 1:125). Obtained seepage flux agrees with field data pretty well. |
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| Keywords: | fracture water karst water square mesh electric analog permeability |
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