Distribution of Earthquake Peak Ground Accelerations for a Construction Site

IF 0.3 Q4 GEOCHEMISTRY & GEOPHYSICS
O. B. Sabirova
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引用次数: 0

Abstract

To solve the problem of antiseismic strengthening, the integer macroseismic intensity of a building is insufficient, because this intensity cannot describe the seismic hazard of a territory. For this, it is necessary to establish the peak ground accelerations and estimate their statistical parameters. The paper constructs the probability density function of the peak ground acceleration for a building site. The basic data for such construction are the shaking of the territory, the peak ground acceleration values on a seismic scale, and the hypothesis on the distribution of peak ground accelerations according to Weibull’s law for the conditions under which the earthquake has occurred. The peak ground acceleration values are taken in accordance with the new seismic scale developed by F.F. Aptikaev. Shaking of the territory was taken in accordance with the traditional linear dependence of the recurrence macroseismic intensity logarithm. Limiting oneself to integer intensity values leads to a polyextremal distribution of peak ground accelerations with peaks at integer intensity values, since it is assumed that there are no earthquakes with intermediate intensities. A peculiarity of the research is construction of the probability density function of peak ground accelerations without using the discrete macroseismic earthquake intensity, but its continuous calculated value, replacing summation over discrete intensity values with the corresponding integration. As a result, a monotonically decreasing distribution density function is obtained, which, in a first approximation, can be described as exponential distribution.

某建筑工地地震峰值地面加速度分布
为了解决建筑物的抗震加固问题,整宏观地震烈度是不够的,因为这个烈度不能描述一个区域的地震危险性。为此,有必要建立峰值地面加速度并估计其统计参数。本文构造了建筑工地地面加速度峰值的概率密度函数。这种构造的基本资料是土地的震动,地震尺度上的地面加速度峰值值,以及根据威布尔定律对地震发生条件下的地面加速度峰值分布的假设。峰值地加速度值是根据F.F. Aptikaev开发的新地震标度计算的。根据传统的递推大地震烈度对数的线性关系来测量区域的震动。由于假定不存在中等烈度的地震,因此将自己限制在整数烈度值会导致峰值地面加速度的多极值分布,峰值在整数烈度值处。本研究的一个特点是不使用离散大地震地震烈度,而是使用其连续计算值来构建峰值地面加速度的概率密度函数,用相应的积分代替离散烈度值的求和。得到了一个单调递减的分布密度函数,其近似可表示为指数分布。
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来源期刊
Seismic Instruments
Seismic Instruments GEOCHEMISTRY & GEOPHYSICS-
自引率
44.40%
发文量
45
期刊介绍: Seismic Instruments is a journal devoted to the description of geophysical instruments used in seismic research. In addition to covering the actual instruments for registering seismic waves, substantial room is devoted to solving instrumental-methodological problems of geophysical monitoring, applying various methods that are used to search for earthquake precursors, to studying earthquake nucleation processes and to monitoring natural and technogenous processes. The description of the construction, working elements, and technical characteristics of the instruments, as well as some results of implementation of the instruments and interpretation of the results are given. Attention is paid to seismic monitoring data and earthquake catalog quality Analysis.
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