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Earthquake-induced settlement of a clay layer

机译:地震引起的粘土层沉降

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摘要

A model for pore water pressure accumulation and settlement of saturated clay layer induced by uniform and irregular cyclic shear strains was developed by concerning the direction of cyclic shear strain. To apply this model to any kinds of clay, the effects of Atterberg's limits of cohesive clay on the cyclic shear-induced pore water pressure and the settlement were observed by using the strain-controlled cyclic simple shear test apparatus which can control the cyclic shear direction. In conclusion, the effects of Atterberg's limits of clay on the cyclic shear-induced pore water pressure accumulation and settlement were clarified by using the cumulative shear strain. Based on the experimental results, estimation methods for the pore water pressure accumulation and post cyclic settlement of clay with a wide range of Atterberg's limits were developed. Furthermore, to apply the proposed methods to the earthquake-induced ground motions, a transformation procedure of irregular cyclic shears to the equivalent uniform ones including the effect of cyclic shear direction was developed and the practical applicability was confirmed.
机译:通过考虑循环剪应变的方向,建立了由均匀和不规则的循环剪应变引起的饱和黏土层孔隙水压力的积累和沉降模型。为了将该模型应用于任何类型的黏土,通过使用可控制循环剪切方向的应变控制循环简单剪切试验装置,观察了阿特伯格黏性黏土极限对循环剪切引起的孔隙水压力和沉降的影响。 。总之,利用累积剪切应变,阐明了阿特伯格极限对循环剪切引起的孔隙水压力积累和沉降的影响。根据实验结果,开发了一种在广泛的阿特伯格极限范围内的孔隙水压力累积和循环后沉降的估算方法。此外,将所提出的方法应用到地震引起的地震动中,开发了将不规则循环剪切转换为等效均匀剪切的程序,包括循环剪切方向的影响,并证实了其实际应用性。

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