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天津市汉沽区深层地下水演变研究
引用本文:胡海军,宫爱玺.天津市汉沽区深层地下水演变研究[J].地下水,2014(2):22-24.
作者姓名:胡海军  宫爱玺
作者单位:河北省水利技术试验推广中心,河北石家庄050061
摘    要:根据天津市汉沽区地下水历史资料,分析区域地下水开采量、水位埋深、地面沉降变化及它们之间的联系等。发现汉沽区地下水处于长期超采状态,地下水位也呈逐年下降趋势,地面不断下沉,地下水的过量开采是引起地面沉降和水位持续下降的主要原因。通过建立汉沽区地下水流-地面沉降模型,设定三个水平年地下水开采方案,预测未来地下水位埋深及地面沉降变化。预测表明,随着地下水开采量的消减,地下水位逐步上升,地面下沉趋势可得到遏制。

关 键 词:深层地下水  地面沉降  开采量  水位埋深

Study on Deep Groundwater Evolution in Hangu District of Tianjin
Institution:HU I-Iai- jun, GONG Ai- xi ( HeBei Extenrion and Experiment Center for Water Technology, Shijiazhuang 050061, Hebei)
Abstract:By analyzing past data of groundwater in Hangu District, Tianjing, the paper makes a study on groundwater ex- ploitation quantity, groundwater depth, land subsidence and the relationship between the three. Results show that groundwater in the studied area has been over exploited for a long time, which makes groundwater level dropping and the land sinking con- stantly. To prevent the situation from worsening, the paper puts forward three groundwater exploitation schemes, which are then tested by Hangu groundwater flow - land subsidence model. Results indicate that groundwater level may recover and land subsidence may stop if groundwater exploitation quantity decrease.
Keywords:Deep groundwater  land subsidence  exploitation quantity and groundwater depth
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