China Geological Environment Monitoring Institute, China Geological Disaster Prevention Engineering Industry AssociationHost
2024 Vol. 35, No. 1
Article Contents

TAO Xiaohu, YE Ming, GONG Jianshi, WANG Hesheng, HU Xiaoyu. Analysis of the formation process of the covered karst ground collapse induced by groundwater changes based on the coupled LBM-DEM numerical simulation at micro scale[J]. The Chinese Journal of Geological Hazard and Control, 2024, 35(1): 124-131. doi: 10.16031/j.cnki.issn.1003-8035.202207027
Citation: TAO Xiaohu, YE Ming, GONG Jianshi, WANG Hesheng, HU Xiaoyu. Analysis of the formation process of the covered karst ground collapse induced by groundwater changes based on the coupled LBM-DEM numerical simulation at micro scale[J]. The Chinese Journal of Geological Hazard and Control, 2024, 35(1): 124-131. doi: 10.16031/j.cnki.issn.1003-8035.202207027

Analysis of the formation process of the covered karst ground collapse induced by groundwater changes based on the coupled LBM-DEM numerical simulation at micro scale

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  • To investigate the hydraulic characteristics and soil behaviors during the formation of covered karst ground collapse induced by the groundwater changes, a 2D fluid-solid coupling model was developed based on discrete element method and lattice Boltzmann method. This model utilizes the linearly interpolated bounce-back scheme of Bouzidi and the momentum exchange method, allowing for the simulation of the formation of covered karst ground collapse from a microscopic perspective. Using the fluid-solid coupling model, an exploratory study was conducted to simulate the formation of covered karst ground collapse induced by a decrease in the hydraulic head of confined aquifers. Simulation results indicate that when the water level of a confined aquifer declines, the groundwater flow mainly affects the particles located above a cave opening and produces a downward force on the surrounding soil. When soil particles spall, the hydraulic heads at the positions of the spalled soil particles drop sharply. This results in a significant increase in the hydraulic gradient, causing the groundwater force on internal particles to sharply increase as well. As a result, the upper particles lose stability due to the combined force of groundwater dragging and gravitational force, which can lead to a gradual acceleration process of collapse. The research results provide valuable insights into the understanding of covered karst ground collapse formation induced by the groundwater changes.

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