Struktur Bawah Permukaan Pantai Semarang berdasarkan Metode HVSR

M. I. Nurwidyanto, M. Zainuri, Anindya Wirasatrya, Gatot Yuliyanto
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Abstract

The aim of this study was to obtain a profile for each depth of the subsurface structure of the Semarang coast based on microtremor data. The acquisition of 109 data points in this study was taken using a single-station microtremor tool in the coastal area of Semarang. This study uses the HVSR method to produce the HV curve, amplification factor (A0) and dominant frequency (f0) which can later be used to find the values of vp, vs and vp/vs at each depth. The results obtained in this study include A0 of 0.13 - 5.96, f0 of 0.13 - 7.47 Hz, vs of 154.42 - 1444.404 m/s, vp of 266.40 - 4758.37 m/s and vp/vs of 1,421 – 28,674. Based on the vs analysis, bedrock begins to appear at a depth of 100 m in the eastern and southern parts of West Semarang District and the southern part of North Semarang District. Classification of hard soil, very dense and soft rock from a depth of 100 m shows that it has covered most of the area of Semarang City. However, there are still several areas that still have a medium soil classification, namely most of the areas of Gayamsari District, Genuk District and Pedurungan District, as well as a small part of the area of North Semarang District, West Semarang District and Central Semarang District. Analysis of vp/vs at a depth of 150 m showed a vp/vs classification with a range of 1.4 - 2 in the study area. However, there are still several areas that still have vp/vs values with a value range of 3 – 3.2, namely in the northern part of West Semarang District, eastern Central Semarang District, eastern South Semarang District, northern East Semarang District, northern Gayamsari District, and the central part of Genuk District.

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基于HVSR方法的当前海岸面下结构
本研究的目的是根据微地震数据获得三宝垄海岸地下结构各深度的剖面图。本研究中使用单站微型遥测工具在三宝垄沿海地区采集了109个数据点。本研究使用HVSR方法生成HV曲线、放大因子(A0)和主频(f0),这些曲线稍后可用于找到每个深度的vp、vs和vp/vs值。本研究中获得的结果包括A0为0.13-5.96,f0为0.13–7.47 Hz,vs为154.42–1444.404 m/s,vp为266.40–4758.37 m/s,vp/vs为1421–28674。根据vs分析,基岩开始出现在西三宝垄区东部和南部以及北三宝垄地区南部100 m深处。从100米深处对硬土、非常密实和软岩的分类表明,它已经覆盖了三宝垄市的大部分地区。然而,仍有几个地区仍有中等土壤分类,即加亚姆萨里区、吉努克区和佩杜伦甘区的大部分地区,以及北三宝垄区、西三宝垄和中三宝垄的一小部分地区。对150米深度的vp/vs的分析显示,研究区域的vp/v分类范围为1.4-2。然而,仍有几个地区的vp/vs值范围在3–3.2之间,即西三宝垄区北部、中三宝垄地区东部、南三宝垄区域东部、东三宝垄北部、加亚姆萨里地区北部和杰努克地区中部。
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