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地下水开采—地面沉降模型研究
引用本文:陈崇希,裴顺平. 地下水开采—地面沉降模型研究[J]. 水文地质工程地质, 2001, 28(2): 5-8
作者姓名:陈崇希  裴顺平
作者单位:1. 中国地质大学@武汉环境地质研究所,
2. 中国地震局地球物理研究所,
基金项目:国家"九五"重点科技攻关项目(93-913-06-04)
摘    要:本文建立三维流支--一维非线性固结地面沉降模型,在混合井流,降雨滞后补给,初始水头形成,人为边界刻画,水流-固结耦合及软土层固结滞后于地下水开采层水头变化等方面有所改进,所建模型用于苏州市,模拟出若干地面沉降重要特征,地面沉降中心偏离地下水漏斗中心,地面沉降动态滞后于地下水的水头动态,软土层渗透系数随固结过程的变化及头在软土层中的传递特征。

关 键 词:地下水三维流 非线性固结 水流固结耦合 混合井 人为边界 滞后补给 地下水开采 地面沉降模型
文章编号:1000-3665(2001)02-0005-04
修稿时间:2001-01-02

Research on groundwater exploitation-land subsidence model
CHEN Chong|xi et al.. Research on groundwater exploitation-land subsidence model[J]. Hydrogeology and Engineering Geology, 2001, 28(2): 5-8
Authors:CHEN Chong|xi et al.
Abstract:A subsidence model with three dimensional groundwater flow coupled one dimensional nonlinear consolidation is established in the paper. In which some solutions are improved in multilayer well, hysteresis of rainfall recharge, initial head, artificial boundary, the coupling between groundwater flow and consolidation, and the consolidation hysteresis in soft soil. This model is applied to Suzhou city and the most important characters are shown, which include the departure between subsidence center and groundwater funnel center, the variation on land subsidence lagged behind which on water head, the permeation coefficients with consolidation, and the transfer feature of water head in soft soil.
Keywords:groundwater three-dimension flow   nonlinear consolidation   coupling between flow and consolidationl   multiplayer well   artificial boundary   hysteresis of recharge
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