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Single-station microtremor surveys for site characterization:A case study in Erzurum city,eastern Turkey

作     者:Fatih Karsli Erdem Bayrak Fatih Karsli;Erdem Bayrak

作者机构:The Higher Education Credit and Hostels InstitutionMinistry of Youth and SportsErzurum 25240Turkey Earthquake Research CentreAtaturk UniversityErzurum 25240Turkey Department of Civil EngineeringAtaturk UniversityErzurum 25240Turkey 

出 版 物:《Earthquake Engineering and Engineering Vibration》 (地震工程与工程振动(英文刊))

年 卷 期:2024年第23卷第3期

页      面:563-576页

核心收录:

学科分类:070801[理学-固体地球物理学] 07[理学] 0708[理学-地球物理学] 0818[工学-地质资源与地质工程] 0903[农学-农业资源与环境] 

基  金:Graduate Institute of Natural and Applied Sciences in Ataturk University Ataturk University Earthquake Research Centre 

主  题:Nakamura horizontal/vertical spectral ratio single-station microtremor predominant frequency vulnerability index Erzurum 

摘      要:The single-station microtremor method is one of the fastest,most reliable,and cheapest methods used to identify dynamic soil *** study utilizes 49 single-station microtremor measurements to identify the dynamic soil properties of the Hilalkent quarter of the Yakutiye district in *** dominant frequency and the amplification factor were calculated by using the Nakamura horizontal/vertical spectral ratio(H/V)*** the soil dominant frequency values varied between 0.4 Hz and 10 Hz,the soil amplification factor changed between 1 and *** H/V values were acquired with lower frequency *** vulnerability index(K_(g))and shear strain parameters that are utilized to estimate the damage that may be caused by an earthquake were *** in the west side of the study area,higher K_(g) values were *** shear strain map was created with 0.25 g,0.50 g and 0.75 g bedrock accelerations,and soil types that lost elasticity during an earthquake were *** average shear wave velocity for the first 30 m(V_(s30))was ***,it was observed that the western part of the study area,which resulted in a higher period and higher H/V,higher K_(g) and lower V_(s30) values,presents a higher risk of damage during an earthquake.

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