Predicting of the Seismogram and Accelerogram of Strong Motions of the Soil for an Earthquake Model Considered as an Instantaneous Rupture of the Earth’s Surface

E. Khachiyan
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引用次数: 1

Abstract

Problems of the prediction of displacement and acceleration values for strong soil displacements are considered for the case where an earthquake is regarded as an instantaneous mechanical rupture of the Earth’s surface. We have attempted to develop, based on recent concepts of earthquake generation process, simplified theoretical methods for the quantitative prediction of soil displacement parameters during strong earthquakes. As an illustrative example, we consider an earthquake originating as a consequence of relative displacements of suddenly ruptured blocks in a horizontal direction with a given initial velocity. An empirical relationship between soil particle motion velocity near the rupture and at a certain distance from it, on one hand, and the earthquake magnitude, on the other hand, was established. It is assumed that the impact of inertial motions of a deep soil stratum on the inertial motions of upper subsurface soil stratum at instantaneous break of a medium can be neglected. By solving a wave problem for a multilayer near surface stratum, analytical relations were developed for a soil seismogram and accelerogram on the surface depending on the physical–mechanical and dynamic characteristics of the soil at all layers of the stratum; attenuation coefficients of mechanical soil vibrations; the distance to the rupture; and the magnitude of the predicted earthquake. The results obtained enable us to determine the maximum displacement and acceleration values of the soil, taking into account local soil conditions and their variations over time, as well as the values of the predominant vibration periods in the soil. The method was applied for solid and loose soil basements.
考虑地表瞬时破裂的地震模型的地震记录和土壤强运动加速度的预测
当地震被认为是地球表面的瞬时机械断裂时,考虑了强土壤位移和加速度值的预测问题。我们试图在地震发生过程的最新概念的基础上,发展简化的理论方法来定量预测强震时土壤位移参数。作为一个说明性的例子,我们考虑由于突然破裂的块体以给定的初速度在水平方向上的相对位移而引起的地震。建立了破裂点附近和离破裂点一定距离的土粒运动速度与地震震级之间的经验关系。假定介质瞬时断裂时深层土层的惯性运动对上层地下土层惯性运动的影响可以忽略。通过求解多层近地表地层的波动问题,根据地层各层土壤的物理力学和动力特性,建立了地表土壤地震记录和加速度记录的解析关系;土壤机械振动衰减系数;到破裂的距离;以及预测地震的震级。得到的结果使我们能够确定土壤的最大位移和加速度值,考虑到当地土壤条件及其随时间的变化,以及土壤中主要振动周期的值。该方法适用于固体和疏松地基。
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