| 上海地下水开采格局与渗流场变化 |
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| 引用本文： | 吴继红.上海地下水开采格局与渗流场变化[J].地下水,2008,30(6):25-26. |
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| 作者姓名： | 吴继红 |
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| 作者单位： | 上海市地质调查研究院,上海,200072 |
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| 摘 要： | 含水层地下水位变化是上海地面沉降的关键因素。深部含水层开采日趋集中、浅部含水层大规模工程降水以及邻省开采等地下水开采格局的新特点，使渗流场发生显著变化。进一步加强地下水系统管理，是深化地面沉降防治的重要环节。
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| 关 键 词： | 地下水开采 渗流场 资源管理 地面沉降 |
Groundwater exploitation setup and seepage field changesin Shanghai |
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| WU Ji-hong.Groundwater exploitation setup and seepage field changesin Shanghai[J].Groundwater,2008,30(6):25-26. |
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| Authors: | WU Ji-hong |
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| Institution: | WU Ji-hong (Shanghai Institute of Geological Survey,Shanghai 200072,China) |
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| Abstract: | The groundwater level change is the key factor for land subsidence in Shanghai.At present,the groundwater exploitation setup have many new changes,such as daily concentrating in the deep aquifer and engineering precipitation in the large scale of the shallow aquifer and some effects of exploitation in the neighbor provinces,so the seepage field have advisable changes.It is the key procedure that the systematic management of groundwater is to be strengthened furthermore for controlling the deep ground level ... |
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| Keywords: | Groundwater exploitation seepage field resources management land sedimentation |
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