ANALISIS TINGKAT RESIKO DAMPAK GEMPABUMI DI KABUPATEN CILACAP MENGGUNAKAN METODE DSHA DAN DATA MIKROTREMOR

JGE Pub Date : 2020-01-17 DOI:10.23960/JGE.V4I3.1075
Kukuh Dialosa, R. Rustadi, B. Mulyatno, C. Sulaeman
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Abstract

Soil mechanical research has been done in Cilacap Regency using DSHA method and microtremor data. This study aims to analyze the local land response to earthquakes based on the dominant frequency parameters (f0), amplification factor (A0), wave velocity VS30 and seismic hazard analysis through deterministic approach. This research uses 193 microtremor measurement points using a short period TDS-303 type (3 component) seismometer. Microtremor data were analyzed using the Horizontal to Vertical Spectral Ratio (HVSR) method in geopsy software. DSHA analysis refers to the source of the Lembang Fault earthquake and Java Subduction zone for deterministic calculations. Based on the analysis of HVSR method, Cilacap Regency is located on land type 1 (frequency 0-1.33 Hz) and soil type 2 (frequency 1,33-5 Hz) according to Kanai Classification (1983), dominated amplification value 1,104 to 8,171 times, then Dominated by soil class E (VS30 value 183 m / s) and soil class D (183 m / s VS30 366 m / s) according to NEHRP Classification (2000). This indicates that Cilacap Regency has high vulnerability to earthquake disaster. Based on the estimated value of PGA calculation method of DSHA, from the calculation of earthquake source Subduction obtained Java PGA bedrock 0,045 g - 0,0671 g and PGA surface rock 0,1926 g - 0,4855 g and calculation of Lembang Fault obtained PGA bedrock 0, 09 g - 0.025 g and PGA surface rocks 0.017 g - 0.089 g. Based on risk map analysis (combination of dominant frequency analysis, amplification, susceptibility factor and ability factor), the highest risk areas are Kec. Adipala, Kasugihan, Binangun, Nusawungun, Cil. Middle, Cil. South, Cil. North, allegedly the soil layer constituent area is a layer of thick and soft sediments. While the low risk of Kec. Majenang and Dayeuh Luhur.
CILACAP船长实施DSHA方法和微观数据改进风险分析
Cilacap Regency利用DSHA方法和微地震数据进行了土壤力学研究。本研究旨在通过确定性方法,基于主频参数(f0)、放大因子(A0)、波速VS30和地震危险性分析,分析当地土地对地震的反应。本研究采用TDS-303型(三分量)短周期地震仪对193个微动测点进行了测量。使用地球物理软件中的水平与垂直频谱比(HVSR)方法分析微地震数据。DSHA分析参考了Lembang断层地震的震源和Java俯冲带进行确定性计算。根据HVSR方法的分析,根据Kanai分类(1983),Cilacap Regency位于1类土地(频率0-1.33 Hz)和2类土壤(频率1,33-5 Hz)上,以1104至8171倍的放大值为主,然后根据NEHRP分类(2000),以E类土壤(VS30值183 m/s)和D类土壤(183 m/s VS30 366 m/s)为主。这表明Cilacap Regency对地震灾害具有很高的脆弱性。根据DSHA PGA计算方法的估算值,从震源俯冲计算得到Java PGA基岩0045 g-00671 g和PGA表层岩石01926 g-04855 g,从Lembang断层计算得到PGA基岩0.09 g-0.025 g和PGA地表岩石0.017 g-0.089 g。根据风险图分析(主频分析、放大、易感性因素和能力因素相结合),风险最高的地区是Kec。阿迪帕拉、卡苏吉汉、比南贡、努萨云贡、Cil。中,Cil。南部,Cil。北部,据称土层组成区是一层厚而软的沉积物。而Kec。Majenang和Dayeuh Luhur。
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JGE
JGE
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