天津市汉沽区深层地下水演变研究 |
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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. |
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作者姓名: | 胡海军 宫爱玺 |
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作者单位: | 河北省水利技术试验推广中心,河北石家庄050061 |
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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。
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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 |
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Institution: | HU I-Iai- jun, GONG Ai- xi ( HeBei Extenrion and Experiment Center for Water Technology, Shijiazhuang 050061, Hebei) |
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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. |
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Keywords: | Deep groundwater land subsidence exploitation quantity and groundwater depth |
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