首页> 外文会议>World conference on earthquake engineering >IDENTIFICATION OF SURFACE GROUND CHARACTERISTICS USING HORIZONTAL ARREY EARTHQUAKE OBSERVATION RECORDS AND ITS APPLICATION
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IDENTIFICATION OF SURFACE GROUND CHARACTERISTICS USING HORIZONTAL ARREY EARTHQUAKE OBSERVATION RECORDS AND ITS APPLICATION

机译:使用水平宫际地震观察记录识别表面地面特征及其应用

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In order to clarify the surface ground motion characteristics at Zushi site which has irregular ground condition, horizontal and vertical array earthquake observations were performed at the five stations(K1,K2,K3,K4,and K5) on the ground surface and one bedrock (-30m depth k6) in Zushi City, in 1994. Approximately 100 earthquakes were recorded between July 1994 to December 2003, including the Chibaken-nanbu earthquake (M=5.2), for which Zushi recorded a maximum acceleration of 75 gal (horizontal component). Microtremor measurements were also performed at about 60 points on the surface and seismic explorations were conducted at two sites (K1 and K2) to examine the resonant frequency and the structure of surface ground. From these data, the soil structure and seismic characteristics of the surface ground in Zushi were clarified._A new identification analysis method to estimate the surface ground characteristics using horizontal array observation records, were developed. It is based on assumption that each incident wave of neighboring observation points in the common basement deconvoluted by the multiple reflection theory almost agrees. The soil structure and the seismic response characteristics of the surface ground were verified through the comparison of the identified results and the observed ones The identification method and the results are useful for seismic disaster mitigation and seismic design of structure in Zushi.
机译:为了澄清具有不规则地下条件的Zushi位点的表面地面运动特性,在地面上的五个站(K1,K2,K3,K4和K5)上进行水平和垂直阵列地震观察,并在一个基岩( 1994年Zushi City的-30M深度K6)。1994年7月至2003年7月至2003年12月之间纪录了大约100次地震,包括Zushi录制了75个GAL的最大加速度(水平组分)的最大加速度。在两个位点(K1和K2)下,在表面上的表面和地震勘探中也进行微反射测量,以检查谐振频率和表面接地的结构。从这些数据中,澄清了Zushi的地面地面的土壤结构和地震特性。阐明了使用水平阵列观察记录来估计表面地面特征的新识别分析方法。它基于假设常见的地下室中的相邻观察点的每个入射波被多重反射理论解构的常见地下室分解几乎同意。通过比较鉴定的结果和观察方法的鉴定方法和鉴定方法的比较来验证表面接地的土壤结构和地震反应特征,可用于Zushi的结构灾害缓解和地震设计。

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