Analysis of Soil Categories on Seismograf Sensor in Java Island Based on Ground Predominant Period and Vs30

The aim of this research is to analyze the categorization of soil at sensor site locations based on predominant period of the ground and Vs30. This study was conducted at nine sites seismograph sensors in Java and Madura. Data processing method is using HVSR (Horizontal to Vertical Ratio) based on t...

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Main Authors: Nugroho Budi Wibowo, Dian Susri Nurhaci
Format: Article
Language:English
Published: Sebelas Maret University 2015-12-01
Series:Indonesian Journal of Applied Physics
Online Access:https://jurnal.uns.ac.id/ijap/article/view/282
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spelling doaj-abae8a816f90450c9952aa77981587f02020-11-24T21:25:11ZengSebelas Maret UniversityIndonesian Journal of Applied Physics2089-01332477-64162015-12-01502344010.13057/ijap.v5i02.282244Analysis of Soil Categories on Seismograf Sensor in Java Island Based on Ground Predominant Period and Vs30Nugroho Budi Wibowo0Dian Susri Nurhaci1BMKG Stasiun Geofisika Yogyakarta Jl.Wates Km8 Jitengan Balecatur Gamping Sleman D.I. YogyakartaBMKG Stasiun Geofisika Yogyakarta Jl.Wates Km8 Jitengan Balecatur Gamping Sleman D.I. YogyakartaThe aim of this research is to analyze the categorization of soil at sensor site locations based on predominant period of the ground and Vs30. This study was conducted at nine sites seismograph sensors in Java and Madura. Data processing method is using HVSR (Horizontal to Vertical Ratio) based on the SESAME European research project. The Java and Madura Vs30’s data were obtained from the USGS. This study utilizes the criteria of JRA 1990 and BSSC 2000 were used to determine the soil categories. It is found that the criteria of JRA 1900 and BSSC 2000 satisfies some sites namely LEM, KMMI, UGM and WOJI. The site of LEM and UGM have a soil that can be categorized in C type (dense soil / sand to soft rock) with dense soil conditions to the rock weathering process. Site KMMI can be categorized in D type (stiff soil) with dense soil conditions. Whereas the site WOJI can be categorized in A + B type (Hard rock and firm to hard rock) with hard rock conditions.https://jurnal.uns.ac.id/ijap/article/view/282
collection DOAJ
language English
format Article
sources DOAJ
author Nugroho Budi Wibowo
Dian Susri Nurhaci
spellingShingle Nugroho Budi Wibowo
Dian Susri Nurhaci
Analysis of Soil Categories on Seismograf Sensor in Java Island Based on Ground Predominant Period and Vs30
Indonesian Journal of Applied Physics
author_facet Nugroho Budi Wibowo
Dian Susri Nurhaci
author_sort Nugroho Budi Wibowo
title Analysis of Soil Categories on Seismograf Sensor in Java Island Based on Ground Predominant Period and Vs30
title_short Analysis of Soil Categories on Seismograf Sensor in Java Island Based on Ground Predominant Period and Vs30
title_full Analysis of Soil Categories on Seismograf Sensor in Java Island Based on Ground Predominant Period and Vs30
title_fullStr Analysis of Soil Categories on Seismograf Sensor in Java Island Based on Ground Predominant Period and Vs30
title_full_unstemmed Analysis of Soil Categories on Seismograf Sensor in Java Island Based on Ground Predominant Period and Vs30
title_sort analysis of soil categories on seismograf sensor in java island based on ground predominant period and vs30
publisher Sebelas Maret University
series Indonesian Journal of Applied Physics
issn 2089-0133
2477-6416
publishDate 2015-12-01
description The aim of this research is to analyze the categorization of soil at sensor site locations based on predominant period of the ground and Vs30. This study was conducted at nine sites seismograph sensors in Java and Madura. Data processing method is using HVSR (Horizontal to Vertical Ratio) based on the SESAME European research project. The Java and Madura Vs30’s data were obtained from the USGS. This study utilizes the criteria of JRA 1990 and BSSC 2000 were used to determine the soil categories. It is found that the criteria of JRA 1900 and BSSC 2000 satisfies some sites namely LEM, KMMI, UGM and WOJI. The site of LEM and UGM have a soil that can be categorized in C type (dense soil / sand to soft rock) with dense soil conditions to the rock weathering process. Site KMMI can be categorized in D type (stiff soil) with dense soil conditions. Whereas the site WOJI can be categorized in A + B type (Hard rock and firm to hard rock) with hard rock conditions.
url https://jurnal.uns.ac.id/ijap/article/view/282
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