首页> 外文期刊>Journal of geotechnical and geoenvironmental engineering >Discrete-Element Analysis of Influence of Granular Soil Density on Earthquake Surface Fault Rupture Interaction with Rigid Foundations
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Discrete-Element Analysis of Influence of Granular Soil Density on Earthquake Surface Fault Rupture Interaction with Rigid Foundations

机译:颗粒土密度对地震地表破裂与刚性基础相互作用的影响的离散元分析

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Parametric analysis of the effects of soil relative density on earthquake surface fault rupture interaction with foundations having different contact pressures and positions was performed with the discrete-element method (DEM). DEM simulations provide insights into particle responses not possible with continuum methods. The relative density of soil has a significant impact on the interaction of surface fault rupture with a building foundation. The number of horizontally oriented contacts achieves a peak value before decreasing during reverse fault rupture through a dense particle assemblage due to its strain-softening response, and the number of horizontally oriented contacts tends to monotonically approach a constant value during reverse fault rupture through a loose particle assemblage. The mobilization of stresses reflects the trends seen with the contact forces and shows quantitatively the more brittle response of denser particle assemblages. Heavy foundations consistently alter the path of reverse fault rupture propagation while undergoing less rotation than light foundations. During normal fault rupture, heavy foundations can undergo more rotation when positioned on the footwall side of the free-field surface outcrop location.
机译:使用离散元法(DEM)对土壤相对密度对与具有不同接触压力和位置的地基的地震表面断层破裂相互作用的影响进行了参数分析。 DEM模拟可提供对连续方法无法实现的粒子响应的深入了解。土壤的相对密度对表面断层破裂与建筑物基础的相互作用有重要影响。在水平方向接触的数量达到峰值之前,由于其应变软化响应,在反向断裂过程中由于致密的颗粒组合而减小,水平方向接触的数量趋于单向接近恒定值,在反向断裂过程中由于松散的应变粒子集合。应力的传递反映了接触力的趋势,并定量显示了较密颗粒组合的脆性响应。与轻基础相比,重基础持续旋转反向断层破裂传播的路径,同时旋转较少。在正常的断层破裂过程中,重地基放置在自由场地面露头位置的底壁侧时,可能会经受更大的旋转。

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