Fluid activity detection in geothermal areas using a single seismic station by monitoring horizontal-to-vertical spectral ratios

Abstract Subsurface structure survey based on horizontal-to-vertical (H/V) spectral ratios is widely conducted. The major merit of this survey is its convenience to obtain a stable result using a single station. Spatial variations of H/V spectral ratios are well-known phenomena, and it has been used...

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Autores principales: Kyosuke Okamoto, Hiroshi Asanuma, Hiro Nimiya
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Publicado: Nature Portfolio 2021
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Acceso en línea:https://doaj.org/article/71bf7f2be7a44697b243500a70617fbb
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spelling oai:doaj.org-article:71bf7f2be7a44697b243500a70617fbb2021-12-02T14:30:39ZFluid activity detection in geothermal areas using a single seismic station by monitoring horizontal-to-vertical spectral ratios10.1038/s41598-021-86775-12045-2322https://doaj.org/article/71bf7f2be7a44697b243500a70617fbb2021-04-01T00:00:00Zhttps://doi.org/10.1038/s41598-021-86775-1https://doaj.org/toc/2045-2322Abstract Subsurface structure survey based on horizontal-to-vertical (H/V) spectral ratios is widely conducted. The major merit of this survey is its convenience to obtain a stable result using a single station. Spatial variations of H/V spectral ratios are well-known phenomena, and it has been used to estimate the spatial fluctuation in subsurface structures. It is reasonable to anticipate temporal variations in H/V spectral ratios, especially in areas like geothermal fields, carbon capture and storage fields, etc., where rich fluid flows are expected, although there are few reports about the temporal changes. In Okuaizu Geothermal Field (OGF), Japan, dense seismic monitoring was deployed in 2015, and continuous monitoring has been consistent. We observed the H/V spectral ratios in OGF and found their repeated temporary drops. These drops seemed to be derived from local fluid activities according to a numerical calculation. Based on this finding, we examined a coherency between the H/V spectral ratios and fluid activities in OGF and found a significance. In conclusion, monitoring H/V spectral ratios can enable us to grasp fluid activities that sometimes could lead to a relatively large seismic event.Kyosuke OkamotoHiroshi AsanumaHiro NimiyaNature PortfolioarticleMedicineRScienceQENScientific Reports, Vol 11, Iss 1, Pp 1-9 (2021)
institution DOAJ
collection DOAJ
language EN
topic Medicine
R
Science
Q
spellingShingle Medicine
R
Science
Q
Kyosuke Okamoto
Hiroshi Asanuma
Hiro Nimiya
Fluid activity detection in geothermal areas using a single seismic station by monitoring horizontal-to-vertical spectral ratios
description Abstract Subsurface structure survey based on horizontal-to-vertical (H/V) spectral ratios is widely conducted. The major merit of this survey is its convenience to obtain a stable result using a single station. Spatial variations of H/V spectral ratios are well-known phenomena, and it has been used to estimate the spatial fluctuation in subsurface structures. It is reasonable to anticipate temporal variations in H/V spectral ratios, especially in areas like geothermal fields, carbon capture and storage fields, etc., where rich fluid flows are expected, although there are few reports about the temporal changes. In Okuaizu Geothermal Field (OGF), Japan, dense seismic monitoring was deployed in 2015, and continuous monitoring has been consistent. We observed the H/V spectral ratios in OGF and found their repeated temporary drops. These drops seemed to be derived from local fluid activities according to a numerical calculation. Based on this finding, we examined a coherency between the H/V spectral ratios and fluid activities in OGF and found a significance. In conclusion, monitoring H/V spectral ratios can enable us to grasp fluid activities that sometimes could lead to a relatively large seismic event.
format article
author Kyosuke Okamoto
Hiroshi Asanuma
Hiro Nimiya
author_facet Kyosuke Okamoto
Hiroshi Asanuma
Hiro Nimiya
author_sort Kyosuke Okamoto
title Fluid activity detection in geothermal areas using a single seismic station by monitoring horizontal-to-vertical spectral ratios
title_short Fluid activity detection in geothermal areas using a single seismic station by monitoring horizontal-to-vertical spectral ratios
title_full Fluid activity detection in geothermal areas using a single seismic station by monitoring horizontal-to-vertical spectral ratios
title_fullStr Fluid activity detection in geothermal areas using a single seismic station by monitoring horizontal-to-vertical spectral ratios
title_full_unstemmed Fluid activity detection in geothermal areas using a single seismic station by monitoring horizontal-to-vertical spectral ratios
title_sort fluid activity detection in geothermal areas using a single seismic station by monitoring horizontal-to-vertical spectral ratios
publisher Nature Portfolio
publishDate 2021
url https://doaj.org/article/71bf7f2be7a44697b243500a70617fbb
work_keys_str_mv AT kyosukeokamoto fluidactivitydetectioningeothermalareasusingasingleseismicstationbymonitoringhorizontaltoverticalspectralratios
AT hiroshiasanuma fluidactivitydetectioningeothermalareasusingasingleseismicstationbymonitoringhorizontaltoverticalspectralratios
AT hironimiya fluidactivitydetectioningeothermalareasusingasingleseismicstationbymonitoringhorizontaltoverticalspectralratios
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