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Centrifuge modeling of failure patterns in mixed soil layers induced by normal faults

机译:正断层引起混合土层破坏模式的离心模型

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Ground failures and ruptures may be induced by fault movements during an earthquake. Numerous notorious earthquakes including the recent Wenchuan earthquake have revealed that surface fault ruptures cause serious damage to structures located near bedrock fault zones. Physical model tests have been conducted by various researchers to investigate the influence of fault movements at one gravity (1-g) and elevated gravity. Most of these physical model tests have been carried out on clear dry sands even though very complex ground failure patterns have been observed in field case studies. In this study, three centrifuge model tests at 120-g were conducted to observe ground failure patterns in different types of soil. Three different models, a sand model, a silt model and a model with mixed soil layers, were tested in the centrifuge. A newly developed hydraulic setup was used at the bottom of the centrifuge models to simulate normal bedrock fault movement with a dip slip angle of 70° with respect to the horizontal direction. The centrifuge setup, model preparation and testing procedures and experimental results are described, reported and discussed in this paper.
机译:地震期间的断层运动可能会引起地面故障和破裂。包括最近的汶川地震在内的许多臭名昭著的地震表明,地表断层破裂会对位于基岩断层带附近的建筑物造成严重破坏。许多研究人员已经进行了物理模型测试,以研究一个重力(1-g)和重力升高时断层运动的影响。尽管在现场案例研究中发现了非常复杂的地面破坏模式,但大多数物理模型测试都是在干净的干沙上进行的。在这项研究中,进行了三个120 g离心机模型试验,以观察不同类型土壤的地面破坏模式。在离心机中测试了三种不同的模型:沙土模型,淤泥模型和具有混合土壤层的模型。离心机模型的底部使用了新开发的液压装置,以模拟相对于水平方向的倾角为70°的正常基岩断层运动。本文描述,报道和讨论了离心机的设置,模型准备和测试程序以及实验结果。

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