基辅境内各场地对地震荷载的地震反应

IF 0.6 Q4 GEOCHEMISTRY & GEOPHYSICS
O. Kendzera, Y. Semenova
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引用次数: 0

摘要

工作中提出的研究旨在评估基辅境内通过工程和地质类比方法确定的三个不同分类点的地震响应,对于不同谱含量和峰值振幅为0.01g至0.06g的地震荷载,评估当地土壤条件对地震烈度的影响是抗震设计和施工的一项重要任务。研究场地底部的土层起到了过滤地震振动的作用。它放大或衰减从基岩传播到自由表面的地震波的振幅。本文考虑了各种土壤复合体可能放大地震运动的机制,以及计算不同强度地震荷载的地震反应的方法。等效线性分析作为分析分类区对地震振动响应(地震响应)的分析工具,在工程地震学中得到了广泛的研究和应用。对于选定的场地,建立了土层模型,并计算了峰值剪切应变和峰值地面加速度(PGA)随深度的变化图,以及上层地震运动的预测(在给定不超过概率的情况下预期)振幅傅立叶谱和对最大振幅为0.01g至0.06g的地震效应具有5%衰减的单个振荡器的响应谱。对基辅个别地区这些参数值的变化进行了比较分析。研究表明,为了评估地震期间地震动的潜在危害,有必要使用最大数量的设计参数来表征特定区域的地震危害,并用于确定建筑物和结构的抗震性。计算物体地震稳定性的最完整的地震危险是由时间上部署的地震运动的全矢量设定的:计算的加速度图、地震图和速度图。所提出的计算结果计划用于解决地震防护的方法和实际问题,这些问题可以在基辅领土的不同地区实现。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Seismic response of various sites of the territory of Kyiv to seismic loads
The research presented in the work aims to assess the seismic response of three different taxonometric sites, identified by the method of engineering and geological analogies within the territory of Kyiv, to seismic loads with different spectral content and peak amplitude from 0.01 g to 0.06 g. Assessment of the influence of local soil conditions on the intensity of earthquakes is an important task of earthquake-resistant design and construction. The soil layer at the base of the study site acts as a filter on seismic vibrations. It amplifies or attenuates the amplitude of the seismic wave propagating from the bedrock to the free surface. The paper considers the mechanisms of the possible amplification of seismic motions by various soil complexes and methods for calculating the seismic response to seismic loads of various intensities. As an analytical tool for analyzing the response of the taxonometric areas to seismic vibrations (seismic response), an equivalent linear analysis was used, which is comprehensively studied and widely used in engineering seismology. For the selected sites, models of soil strata were built, and graphs of changes with depth of peak shear strain and peak ground acceleration (PGA) were calculated, as well as predicted (expected with a given probability of non-exceeding) amplitude Fourier spectra of seismic motions in the upper layer and the response spectra of single oscillators with 5 % attenuation to seismic effects with a maximum amplitude from 0.01 g to 0.06 g. A comparative analysis of the change in the value of these parameters in individual sections of Kyiv is presented. It is shown that to assess the potential hazard from seismic ground motions during earthquakes, it is necessary to use the maximum number of design parameters that characterize the seismic hazard of specific areas and which are used to determine the seismic resistance of buildings and structures. The most complete seismic hazard for calculating the seismic stability of objects is set by the full vector of seismic motions deployed in time: calculated accelerograms, seismograms and velocigrams. The presented calculation results are planned to be used in solving methodological and practical problems of earthquake protection, which can be realized in different parts of the territory of Kyiv.
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来源期刊
Geofizicheskiy Zhurnal-Geophysical Journal
Geofizicheskiy Zhurnal-Geophysical Journal GEOCHEMISTRY & GEOPHYSICS-
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60.00%
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50
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