适用隧道周边冻土层的地震波传播数值模拟方法及系统

By using adaptive mesh generation and the finite difference method to simulate the propagation of seismic waves in permafrost, the problem of traditional models failing to reflect the complexity of high-ice permafrost layers is solved. This achieves high-precision simulation of seismic wave propagation in permafrost around tunnels, thus improving the seismic safety of tunnel construction.

CN120429931BActive Publication Date: 2026-07-17CHONGQING UNIV

Patent Information

Authority / Receiving Office
CN · China
Patent Type
Patents(China)
Current Assignee / Owner
CHONGQING UNIV
Filing Date
2025-05-27
Publication Date
2026-07-17

AI Technical Summary

Technical Problem

Traditional wave propagation models are insufficient to fully reflect the complexity of high-permafrost layers, especially under the coupled effects of temperature changes, ice-water phase transitions, and changes in water content. Existing methods have limited research on their dynamic response, leading to deviations in seismic wave simulation results.

Method used

An adaptive mesh generation method is adopted to construct a layered model by acquiring geological and environmental parameters of the permafrost layer. The layer range is adjusted by combining the geothermal field and freezing depth, wave velocity gradient zones are identified, and updated mesh shape and density distribution are generated. Numerical calculations are then performed using the finite difference method to simulate seismic wave propagation.

Benefits of technology

It improves the accuracy of seismic wave propagation simulation, effectively addresses the heterogeneity and temperature coupling effects of permafrost, and provides precise dynamic response simulation support for tunnel construction.

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Abstract

本发明公开了适用隧道周边冻土层的地震波传播数值模拟方法及系统,涉及地震波模拟传播领域,方法通过构建分层模型以描述冻土层在不同深度的物性分布,结合黏弹性模型将其整合为隧道周边冻土层的有限元模型,并采用初始化的均匀网格对所述有限元模型划分后初步模拟地震波传播过程,通过比较波速的空间变化率,识别出波速梯度显著变化的区域提取其波速变化幅度和方向性数据来确定其边界和形状,结合梯度变化区域的地质参数规划所述更新网格的密度分布。本发明本通过识别波速梯度区的边界及内部特性,根据梯度的空间变化率和分布特性规划网格形状和密度,确保计算区域既能够反映冻土层的多尺度特性,又能优化地震波传播路径及能量分布的数值计算。
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