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天津平原地面沉降条件下的深层地下水资源组成

Composition of groundwater resources in deep-seated aquifers under the condition of land subsidence in Tianjin Plain

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【作者】 王家兵李平

【Author】 WANG Jia-bing~(1,2), LI Ping~(1,3) (1.School of Water Resources and Environment, China University of Geosciences, Beijing100083, China; 2.Tianjin Geological Survey Institute, Tianjin300191, China; 3.Tianjin Geological and Mining Exploitation Bureau, Tianjin300191, China)

【机构】 中国地质大学水资源与环境学院中国地质大学水资源与环境学院 北京 100083天津市地质调查研究院天津 300191北京 100083天津市地质矿产勘查开发局天津 300191

【摘要】 根据天津平原地面沉降监测结果,采用水量均衡法,计算出深层地下水开采量中,浅层地下水越流补给量占38 2%,粘土性压密释水量占41 3%,弹性释水量占5 6%,侧向流入量占14 9%。在控制地面沉降的条件下,深层地下水持续利用的对策是调整开采三维布局,适度开发利用浅层地下水对深层地下水的越流补给。

【Abstract】 On the basis of the monitoring results of land subsidence and calculation of deep groundwater resources by using water balance method, it is shown that the leakage recharge from its upper shallow groundwater account for approximately 38.2%, drainage of the clay layers, about 41.3%, water release from the aquifers, around 5.6%, and lateral inflow, some 14.9%, of the total groundwater resources. In order to control the land subsidence, adjusting three dimensional exploitive positions and moderately utilizing the leakage recharge from its upper shallow groundwater play a key role in realizing the sustainable development of deep groundwater resources in this area.

【基金】 国土资源大调查项目中华北平原(天津部分)地下水资源调查评价(200110400005)
  • 【文献出处】 水文地质工程地质 ,Hydrogeology and Engineering Geology , 编辑部邮箱 ,2004年05期
  • 【分类号】P642.26
  • 【被引频次】45
  • 【下载频次】484
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