A numerical simulation study on the evolutionary characteristics of the damage process of karst soil cavity under positive pressure effect

Yongyao Wei , Zongchun Li , Bo Chen , Hong Yin , Jianxun Xiao , Jinqi Kong
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Abstract

Positive pressure effect is the result of rapid urban development in recent years, which leads to over-exploitation of karst groundwater, coupled with the emergence of extreme weather (such as heavy rainfall, the increase in the duration of heavy rainfall), leading to the sharp rise of karst water level, the gas in the karst cavity can not be discharged in time to form a high positive pressure in the soil cavity and promote the destruction of the soil layer, which then induces a series of phenomena, such as karst subsidence. As a new collapse mechanism, the positive pressure effect causes geological disasters that seriously affect the safety of people's lives and properties in karst regions. In order to study the damage characteristics and evolution characteristics of karst soil cavities under positive pressure effect, this study is based on the ASCII text provided by FLAC itself, and the orthotropic simulation computation compilation program, which realizes the finite element analysis in FLAC3D, and focuses on the inhomogeneous change of soil displacement, redistribution of stresses, and plastic damage of karst soil cavities in different evolution stages under the action of positive pressure, and summarizes the characteristics and laws of stress, strain and damage in plastic zone of karst soil cave at different stages of evolution. The results will play a positive role in further investigating the potential mechanical effects, development mechanism and critical warning conditions during the evolution of covered karst soil caves, and also have important scientific research value in deepening the theory of prevention and control of collapse disasters in covered karst soil caves.

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正压力作用下岩溶土洞破坏过程演变特征的数值模拟研究
正压效应是由于近年来城市快速发展,导致岩溶地下水过度开采,加之极端天气的出现(如暴雨、强降雨持续时间的增加),导致岩溶水位急剧上升,岩溶溶腔中的气体不能及时排出,在土腔中形成高正压,促进土层破坏,进而诱发岩溶塌陷等一系列现象。作为一种新的崩塌机制,正压效应引发的地质灾害严重影响着岩溶地区人民的生命财产安全。为了研究正压力效应下岩溶土洞的破坏特征和演化特征,本研究基于 FLAC 本身提供的 ASCII 文本,利用正交模拟计算编译程序,在 FLAC3D 中实现了有限元分析、并重点研究了岩溶土洞在正压力作用下不同演化阶段土体位移的非均质变化、应力的重新分布和塑性破坏,总结了岩溶土洞不同演化阶段塑性区应力、应变和破坏的特点和规律。该成果将对进一步研究覆盖岩溶土洞演化过程中的潜在力学效应、发展机理和临界预警条件起到积极作用,同时对深化覆盖岩溶土洞坍塌灾害防治理论具有重要的科学研究价值。
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