| 石菉铜矿岩溶区地下水运动特性与地面初探塌陷 |
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| 引用本文： | 曾邦锐.石菉铜矿岩溶区地下水运动特性与地面初探塌陷[J].华南师范大学学报(自然科学版),1992(2). |
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| 作者姓名： | 曾邦锐 |
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| 作者单位： | 华南师范大学地理系 |
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| 摘 要： | 岩溶地区地面塌陷是一种环境灾害,明显发生在疏干排水采矿的(厂)矿区,它的产生与多种环境因素有关,本文以石菉铜矿岩溶区为例,从地下水运动角度,探讨其产生原因及其初步防治的办法.
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| 关 键 词： | 覆盖岩溶 地面塌陷 含水层 渗透系数 地下水位 地下水比降 地下径流 断裂 构造 |
A STUDY ON MOVEMENT CHARACTERISTICS OF UNDERGROUND WATER AND COLLAPSE OF LAND SURFACE IN SHILU COPPER MINE, GUANGDONG |
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| Zeng Bangrui.A STUDY ON MOVEMENT CHARACTERISTICS OF UNDERGROUND WATER AND COLLAPSE OF LAND SURFACE IN SHILU COPPER MINE, GUANGDONG[J].Journal of South China Normal University(Natural Science Edition),1992(2). |
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| Authors: | Zeng Bangrui |
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| Institution: | Dept. of Geog. |
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| Abstract: | Surface collapse of karst terrain is an environmental disaster and occurs obviously during draining periods in mining. Its development is affected by a lot of environmental elements.Based on investigations in Shilu Copper Mine, geneses of collapses are discussed rnd methods of prevention and threatment are proposed front the view-point of underground water movement. |
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| Keywords: | covered kafst surface collapse aquiferspermeabslity coefficient water table water-table gradient ground water flow fracture |
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