Seismic ground motion study of layered site of saturated frozen soil under P-wave incidence

IF 4.9 2区 工程技术 Q1 ENGINEERING, CIVIL Cold Regions Science and Technology Pub Date : 2025-03-01 Epub Date: 2025-01-18 DOI:10.1016/j.coldregions.2025.104426
Qiang Ma , Hao Jiao , Xusheng Wan
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Abstract

A two-dimensional model of layered saturated frozen soil over bedrock is developed based on porous media theory, focusing on the seismic response to P-wave incidence. The governing equations for saturated frozen soil are formulated and decoupled using the Helmholtz vector decomposition theorem, yielding a general solution for the potential function. Through the application of the transfer matrix method and interface boundary conditions, an analytical solution for surface displacement in saturated frozen soil is derived. This solution is validated against existing literature. The study comprehensively examines the effects of incident frequency, angle, the surface layer's porosity, medium temperature, cementation parameter, contact parameter, soil stiffness, and surface layer thickness on the seismic response. The key findings are as follows: A layered foundation model demonstrates the seismic effects of stratification on ground motion. Compared to uniform foundations, layered models better represent real-world conditions and reveal the amplification and frequency-dependent characteristics of soil stratification under the idealized analytical framework of this study. For constant incident frequency or medium temperature, the peak horizontal displacement amplification factor is higher in an upper-soft and lower-hard foundation compared to an upper-hard and lower-soft foundation. Horizontal and vertical displacement amplification coefficients exhibit periodic fluctuations with variations in soil thickness. High-frequency seismic waves induce pronounced fluctuations in the horizontal displacement amplification coefficient. Under the idealized analytical framework, the vertical displacement amplification coefficient tends to exceed the horizontal one across all frequencies. These findings provide theoretical insights but require validation through field measurements and numerical simulations to assess their applicability to real-world conditions.
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p波入射下饱和冻土层状场地地震动研究
基于多孔介质理论,建立了基岩上层状饱和冻土的二维模型,重点研究了p波入射下的地震响应。利用亥姆霍兹矢量分解定理对饱和冻土的控制方程进行了表述和解耦,得到了势函数的通解。应用传递矩阵法和界面边界条件,导出了饱和冻土表面位移的解析解。根据现有文献验证了该解决方案。综合考察了入射频率、角度、表层孔隙度、介质温度、胶结参数、接触参数、土体刚度、表层厚度等因素对地震响应的影响。主要发现如下:层状地基模型显示了层状对地面运动的地震效应。与均匀基础相比,分层模型更能反映现实条件,揭示了本研究理想化分析框架下土壤分层的放大和频率依赖特征。当入射频率或介质温度不变时,上软下硬地基的峰值水平位移放大系数高于上硬下软地基。水平和垂直位移放大系数随土层厚度的变化呈周期性波动。高频地震波引起水平位移放大系数的显著波动。在理想分析框架下,在所有频率范围内,竖向位移放大系数都趋于大于水平位移放大系数。这些发现提供了理论见解,但需要通过现场测量和数值模拟来验证,以评估其对现实世界条件的适用性。
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来源期刊
Cold Regions Science and Technology
Cold Regions Science and Technology 工程技术-地球科学综合
CiteScore
7.40
自引率
12.20%
发文量
209
审稿时长
4.9 months
期刊介绍: Cold Regions Science and Technology is an international journal dealing with the science and technical problems of cold environments in both the polar regions and more temperate locations. It includes fundamental aspects of cryospheric sciences which have applications for cold regions problems as well as engineering topics which relate to the cryosphere. Emphasis is given to applied science with broad coverage of the physical and mechanical aspects of ice (including glaciers and sea ice), snow and snow avalanches, ice-water systems, ice-bonded soils and permafrost. Relevant aspects of Earth science, materials science, offshore and river ice engineering are also of primary interest. These include icing of ships and structures as well as trafficability in cold environments. Technological advances for cold regions in research, development, and engineering practice are relevant to the journal. Theoretical papers must include a detailed discussion of the potential application of the theory to address cold regions problems. The journal serves a wide range of specialists, providing a medium for interdisciplinary communication and a convenient source of reference.
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