冻土边坡融化过程稳定性研究

Pub Date : 2022-10-01 DOI:10.1016/j.rcar.2022.12.004
Heng Zhang , XiaoDong Liu , Cheng Cao , XiaoWu Ma , XiaoLiang Yao , WenLi Wang , RuoXing Zhou , LiPing Wang
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引用次数: 1

摘要

基于热传导理论,建立了一个瞬时分析边坡安全系数随时间变化的数值模拟平台,研究多年冻土边坡在融化过程中的稳定性发展规律。该平台考虑了冻土融化过程中的冰-水相变、弹塑性本构行为和强度折减,能够对不同坡角和含水量的冻土边坡进行安全系数评价。结果表明:在不同坡角和含水量条件下,边坡安全系数随时间的演化表现为先非线性减小后基本保持不变的两个阶段;在减小阶段,塑性滑移线与融化锋重叠。冻融界面抗剪强度保持不变的同时,冻融后冻土层自重不断增大。这是导致安全系数下降的主要原因。在第二阶段,融化深度持续增加,而塑性滑移线位置保持不变,进入安全系数不变阶段。
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Study on stability of permafrost slopes during thawing

A numerical simulation platform that analyzes the variation of the slope factor of safety with time instantaneously is proposed based on heat conduction theory to study the law of stability development of permafrost slopes during thawing. This platform considers ice-water phase change, elastoplastic constitutive behavior and strength reduction in thawing permafrost and can evaluate the factor of safety of permafrost slopes with different slope angles and water contents. Results indicate that under different slope angles and water contents, the evolution of the factor of safety with time displays two stages: nonlinearly decreasing at first and then essentially remaining constant. During the decreasing stage, the plastic slip line overlaps with the thawing front. In this stage, the self-weight of the post-thawed permafrost layer increases continuously while the shear strength of the frozen-thaw interface keeps unchanged. This is the main reason leading to the decrease in the factor of safety. In the second stage, the thawing depth increases continuously while the position of the plastic slip line remains unchanged, resulting in a constant safety factor stage.

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