边坡的渗流–应力耦合数学模型与稳定性分析
Mathematical Model of Seepage-Stress Coupling and Stability Analysis of Slope
DOI: 10.12677/pm.2025.1511279, PDF,   
作者: 王琮煜:成都理工大学,数学地质四川省重点实验室,四川 成都;成都理工大学,数学科学学院,四川 成都
关键词: 协同放大边坡耦合稳定性数值模拟Synergistic Amplification Slope Coupling Stability Numerical Simulation
摘要: 针对松散堆积体边坡在降雨与开挖耦合作用下的稳定性问题,本文建立了饱和–非饱和渗流与应力耦合的偏微分方程模型。基于虚功原理与有效应力原理,推导了渗流–应力耦合控制方程,采用FLAC3D平台进行三维数值模拟,并结合强度折减法构建稳定性判据。通过对比单一开挖、单一降雨及耦合工况下的数值试验,揭示了耦合效应对塑性区扩展与安全系数的协同放大效应。结果表明,耦合作用下边坡安全系数显著降低至1.18,揭示了渗流–应力反馈机制在边坡灾变过程中的数学本质。
Abstract: To investigate the stability of loose accumulation slopes under the coupled effects of rainfall and excavation, this study establishes a set of partial differential equations describing the coupled saturated-unsaturated seepage and stress fields. Based on the principles of virtual work and effective stress, the governing equations for seepage-stress coupling are derived. Three-dimensional numerical simulations are performed using the FLAC3D platform, and a stability criterion is developed through the strength-reduction method. By comparing numerical experiments under excavation only, rainfall only, and coupled conditions, the study reveals a synergistic amplification effect of the coupling process on the expansion of the plastic zone and the reduction of the safety factor. The results indicate that the slope safety factor decreases significantly to 1.18 under coupled conditions, highlighting the mathematical essence of the seepage-stress feedback mechanism in slope failure evolution.
文章引用:王琮煜. 边坡的渗流–应力耦合数学模型与稳定性分析[J]. 理论数学, 2025, 15(11): 169-177. https://doi.org/10.12677/pm.2025.1511279

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