Penyusunan Peta Koefisien Amplifikasi Berdasarkan Rasio Spektra Percepatan

Elvis Saputra
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Abstract

One of the most important parameters in the building structure design process is an amplification coefficient. The amplification coefficient is needed to propagate a spectra acceleration at bedrock to soil surface. The amplification coefficient can be determined by several methods such as MASW Method, HVSR Method and other methods. One alternative method that can be used in determining the amplification coefficient is to determine the ratio between the ground acceleration at the surface and at the bedrock. Therefore, the purpose of this study was to identify the amplification coefficient in the Province of the Special Region of Yogyakarta with the PSHA method analysis approach by utilizing the shear wave velocity data (Vs30). This research method was carried out in 3 stages, namely data collection, acceleration analysis using the PSHA method, and determination of the amplification coefficient based on the acceleration ratio. The results of the study obtained a distribution of the amplification coefficient of the acceleration spectra of 0.2 and 1 second in the DIY province with a maximum value of Fa amplification coefficient was 1.414 on hard soil conditions and 1.653 on medium soil conditions. The maximum Fv amplification coefficient was 1.508 on hard soil conditions and 1,923 on medium soil conditions.
基于加速度摄谱比的系数放大地图
放大系数是建筑结构设计过程中最重要的参数之一。将基岩处的光谱加速度传播到土壤表面需要放大系数。放大系数的测定方法有MASW法、HVSR法等。确定放大系数的另一种方法是确定地表加速度与基岩加速度之比。因此,本研究的目的是利用横波速度数据(Vs30),采用PSHA方法分析方法确定日惹特区省的放大系数。本研究方法分数据采集、PSHA法加速度分析、基于加速度比确定放大系数3个阶段进行。研究结果得到了0.2和1 s加速度谱放大系数在DIY省的分布,其中硬土条件下Fa放大系数最大值为1.414,中土条件下Fa放大系数最大值为1.653。在硬土条件下Fv放大系数最大为1.508,在中土条件下最大为1923。
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