Numerical Modeling of Quaternary Sediment Amplification. Basin Size, ASCE Site Class and Fault Location

IF 0.5 Q4 ENGINEERING, GEOLOGICAL
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引用次数: 0

Abstract

The main objective of this study is to understand the dependency of basin amplification on-site and source parameters employing high computational numerical simulations. This study mainly addresses the effect of fault dip, size of the basin, site classification, and position of the basin on wave amplification. Two dip angles are considered, 7 and 9 degrees in this study to estimate the factor of amplification. Amplifications observed at the basin center and basin edge station for three different sizes of the basin are analyzed. Simulation results obtained from three different models with the ASCE site class C, D, and E basin sediment specifications are compared. To analyze the effect of basin relative position on amplification, we studied a model with two different basins embedded in bedrock, back and forth of the fault. This study observed multiple peaks at different time periods in response spectra drawn to amplification ratio versus time periods.
第四纪泥沙放大的数值模拟。盆地大小、ASCE站点等级和断层位置
本研究的主要目的是利用高计算数值模拟来了解现场流域放大与源参数的依赖关系。本文主要研究了断层倾角、盆地大小、场地分类、盆地位置等因素对波放大的影响。在本研究中考虑了两个倾角,7度和9度来估计放大因子。分析了三种不同大小的盆地在盆地中心和盆地边缘观测到的放大结果。对ASCE站点C、D、E级流域泥沙指标下3种不同模型的模拟结果进行了比较。为了分析盆地相对位置对放大的影响,我们研究了两个不同的盆地嵌套在基岩上的模型,分别位于断层的前后。本研究在放大比随时间变化的响应谱中观察到不同时间段的多个峰。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
CiteScore
1.90
自引率
25.00%
发文量
11
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