Seismic Amplification by Deep Subsurface and Proposal of a New Proxy

Codes of practice and ground motion prediction equations involve ground structure proxies to account for seismic amplification. Although the ground consists of both shallow and deep subsurface, proxies are mainly related to the shallow subsurface as it is shallow subsurface information that is mostl...

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Main Author: T. Nagao
Format: Article
Language:English
Published: D. G. Pylarinos 2020-02-01
Series:Engineering, Technology & Applied Science Research
Subjects:
Online Access:https://etasr.com/index.php/ETASR/article/view/3276
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spelling doaj-55a051cd374e4e0994fbdc5dc969bd1b2020-12-02T17:32:34ZengD. G. PylarinosEngineering, Technology & Applied Science Research2241-44871792-80362020-02-01101945Seismic Amplification by Deep Subsurface and Proposal of a New ProxyT. Nagao0Research Center for Urban Security and Safety, Kobe University, JapanCodes of practice and ground motion prediction equations involve ground structure proxies to account for seismic amplification. Although the ground consists of both shallow and deep subsurface, proxies are mainly related to the shallow subsurface as it is shallow subsurface information that is mostly available. However, as deep subsurface seismic amplification is not negligible, it may not be appropriate to use shallow subsurface proxies. In this study, the relationship between shallow and deep subsurface seismic amplification factors is discussed on the basis of S-wave velocity profile data from Japanese KiK-net strong-motion observation system stations. The correlation between typical proxies such as the average S-wave velocity of the top 30m of the ground surface and the seismic amplification factor was examined. Although there was a negative correlation between the two, the degree of the correlation was weak. A new proxy showing stronger correlations with the seismic amplification factor is proposed and its effectiveness is demonstrated. https://etasr.com/index.php/ETASR/article/view/3276seismic amplificationVs30S-wave velocitydeep subsurface
collection DOAJ
language English
format Article
sources DOAJ
author T. Nagao
spellingShingle T. Nagao
Seismic Amplification by Deep Subsurface and Proposal of a New Proxy
Engineering, Technology & Applied Science Research
seismic amplification
Vs30
S-wave velocity
deep subsurface
author_facet T. Nagao
author_sort T. Nagao
title Seismic Amplification by Deep Subsurface and Proposal of a New Proxy
title_short Seismic Amplification by Deep Subsurface and Proposal of a New Proxy
title_full Seismic Amplification by Deep Subsurface and Proposal of a New Proxy
title_fullStr Seismic Amplification by Deep Subsurface and Proposal of a New Proxy
title_full_unstemmed Seismic Amplification by Deep Subsurface and Proposal of a New Proxy
title_sort seismic amplification by deep subsurface and proposal of a new proxy
publisher D. G. Pylarinos
series Engineering, Technology & Applied Science Research
issn 2241-4487
1792-8036
publishDate 2020-02-01
description Codes of practice and ground motion prediction equations involve ground structure proxies to account for seismic amplification. Although the ground consists of both shallow and deep subsurface, proxies are mainly related to the shallow subsurface as it is shallow subsurface information that is mostly available. However, as deep subsurface seismic amplification is not negligible, it may not be appropriate to use shallow subsurface proxies. In this study, the relationship between shallow and deep subsurface seismic amplification factors is discussed on the basis of S-wave velocity profile data from Japanese KiK-net strong-motion observation system stations. The correlation between typical proxies such as the average S-wave velocity of the top 30m of the ground surface and the seismic amplification factor was examined. Although there was a negative correlation between the two, the degree of the correlation was weak. A new proxy showing stronger correlations with the seismic amplification factor is proposed and its effectiveness is demonstrated.
topic seismic amplification
Vs30
S-wave velocity
deep subsurface
url https://etasr.com/index.php/ETASR/article/view/3276
work_keys_str_mv AT tnagao seismicamplificationbydeepsubsurfaceandproposalofanewproxy
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