摘要
抽水引起地裂缝活动的现象目前已经引起了人们的关注。抽水改变了土体中承压含水层的孔隙水压力分布,引起了土体的变形,地裂缝错断了地层使得地裂缝左右两侧发生差异沉降,进一步诱发地裂缝的活动,这是一个复杂的物理力学过程。充分考虑了抽水引起地裂缝活动的机理,基于理想地层模型,采用流固耦合的计算方法,基于FLAC3D6.0软件平台编译程序,建立地裂缝活动量计算模型,计算和模拟不同抽水流量条件下完整井和非完整井抽水引起的地裂缝活动量。结果表明,随着抽水流量增大,地裂缝的活动量增大,完整井比非完整井引起的地裂缝活动量大。
The phenomenon of ground fissure activity caused by pumping has attracted people's attention.Pumping changes the pore water pressure distribution of the confined aquifer in the soil,causes the deformation of the soil,and the ground fissure breaks the stratum,resulting in differential settlement on the left and right sides of the ground fissure,which further induces the activity of the ground fissure,which is a complex physical and mechanical process.In this paper,the mechanism of ground fracture activity caused by pumping is fully considered.Based on the ideal formation model,the fluid structure coupling calculation method is adopted,based on FLAC3D6.0 software platform to compile the program,establish the calculation model of ground fracture activity,calculate and simulate the ground fracture activity caused by pumping from complete wells and incomplete wells under different pumping flow conditions.The results show that with the increase of pumping flow,the activity of ground fractures increases,and the activity of ground fractures caused by complete wells is larger than that caused by incomplete wells.
作者
郭乐凡
刘雪弟
刘超
成盛林
韩冰
韩宁博
GUO Le-fan;LIU Xue-di;LIU Chao;CHENG Sheng-lin;HAN Bing;HAN Ning-bo(Hebei GEO University,Shijiazhuang 050031,China;Hebei Center for Ecological and Environmental Geology Research,Shijiazhuang 050031,China;Hebei Technology Innovation Center for Intelligent Development and Control of Underground Built Environment,Shijiazhuang 050031,China)
出处
《河北地质大学学报》
2022年第6期54-61,共8页
Journal of Hebei Geo University
基金
河北省自然科学基金项目(D2019403182)
河北地质大学博士科研启动基金(BQ2017022)
河北地质大学青年科技基金项目(QN202110)
河北地质大学科技创新团队项目(KJCXTD-2021-08)
河北省大中学生科技创新能力培育专项(22E50153D)。
关键词
地裂缝
FLAC3D
流固耦合
孔隙水压力
抽水
ground fissures
FLAC3D
fluid-solid coupling
pore water pressure
pumping