Utilizing distributed acoustic sensing and ocean bottom fiber optic cables for submarine structural characterization

Abstract The sparsity of permanent seismic instrumentation in marine environments often limits the availability of subsea information on geohazards, including active fault systems, in both time and space. One sensing resource that provides observational access to the seafloor environment are existin...

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Autores principales: Feng Cheng, Benxin Chi, Nathaniel J. Lindsey, T. Craig Dawe, Jonathan B. Ajo-Franklin
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Lenguaje:EN
Publicado: Nature Portfolio 2021
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Acceso en línea:https://doaj.org/article/a9c8fb556b2341f9a24e146d488d271b
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spelling oai:doaj.org-article:a9c8fb556b2341f9a24e146d488d271b2021-12-02T15:53:42ZUtilizing distributed acoustic sensing and ocean bottom fiber optic cables for submarine structural characterization10.1038/s41598-021-84845-y2045-2322https://doaj.org/article/a9c8fb556b2341f9a24e146d488d271b2021-03-01T00:00:00Zhttps://doi.org/10.1038/s41598-021-84845-yhttps://doaj.org/toc/2045-2322Abstract The sparsity of permanent seismic instrumentation in marine environments often limits the availability of subsea information on geohazards, including active fault systems, in both time and space. One sensing resource that provides observational access to the seafloor environment are existing networks of ocean bottom fiber optic cables; these cables, coupled to modern distributed acoustic sensing (DAS) systems, can provide dense arrays of broadband seismic observations capable of recording both seismic events and the ambient noise wavefield. Here, we report a marine DAS application which demonstrates the strength and limitation of this new technique on submarine structural characterization. Based on ambient noise DAS records on a 20 km section of a fiber optic cable offshore of Moss Landing, CA, in Monterey Bay, we extract Scholte waves from DAS ambient noise records using interferometry techniques and invert the resulting multimodal dispersion curves to recover a high resolution 2D shear-wave velocity image of the near seafloor sediments. We show for the first time that the migration of coherently scattered Scholte waves observed on DAS records can provide an approach for resolving sharp lateral contrasts in subsurface properties, particularly shallow faults and depositional features near the seafloor. Our results provide improved constraints on shallow submarine features in Monterey Bay, including fault zones and paleo-channel deposits, thus highlighting one of many possible geophysical uses of the marine cable network.Feng ChengBenxin ChiNathaniel J. LindseyT. Craig DaweJonathan B. Ajo-FranklinNature PortfolioarticleMedicineRScienceQENScientific Reports, Vol 11, Iss 1, Pp 1-14 (2021)
institution DOAJ
collection DOAJ
language EN
topic Medicine
R
Science
Q
spellingShingle Medicine
R
Science
Q
Feng Cheng
Benxin Chi
Nathaniel J. Lindsey
T. Craig Dawe
Jonathan B. Ajo-Franklin
Utilizing distributed acoustic sensing and ocean bottom fiber optic cables for submarine structural characterization
description Abstract The sparsity of permanent seismic instrumentation in marine environments often limits the availability of subsea information on geohazards, including active fault systems, in both time and space. One sensing resource that provides observational access to the seafloor environment are existing networks of ocean bottom fiber optic cables; these cables, coupled to modern distributed acoustic sensing (DAS) systems, can provide dense arrays of broadband seismic observations capable of recording both seismic events and the ambient noise wavefield. Here, we report a marine DAS application which demonstrates the strength and limitation of this new technique on submarine structural characterization. Based on ambient noise DAS records on a 20 km section of a fiber optic cable offshore of Moss Landing, CA, in Monterey Bay, we extract Scholte waves from DAS ambient noise records using interferometry techniques and invert the resulting multimodal dispersion curves to recover a high resolution 2D shear-wave velocity image of the near seafloor sediments. We show for the first time that the migration of coherently scattered Scholte waves observed on DAS records can provide an approach for resolving sharp lateral contrasts in subsurface properties, particularly shallow faults and depositional features near the seafloor. Our results provide improved constraints on shallow submarine features in Monterey Bay, including fault zones and paleo-channel deposits, thus highlighting one of many possible geophysical uses of the marine cable network.
format article
author Feng Cheng
Benxin Chi
Nathaniel J. Lindsey
T. Craig Dawe
Jonathan B. Ajo-Franklin
author_facet Feng Cheng
Benxin Chi
Nathaniel J. Lindsey
T. Craig Dawe
Jonathan B. Ajo-Franklin
author_sort Feng Cheng
title Utilizing distributed acoustic sensing and ocean bottom fiber optic cables for submarine structural characterization
title_short Utilizing distributed acoustic sensing and ocean bottom fiber optic cables for submarine structural characterization
title_full Utilizing distributed acoustic sensing and ocean bottom fiber optic cables for submarine structural characterization
title_fullStr Utilizing distributed acoustic sensing and ocean bottom fiber optic cables for submarine structural characterization
title_full_unstemmed Utilizing distributed acoustic sensing and ocean bottom fiber optic cables for submarine structural characterization
title_sort utilizing distributed acoustic sensing and ocean bottom fiber optic cables for submarine structural characterization
publisher Nature Portfolio
publishDate 2021
url https://doaj.org/article/a9c8fb556b2341f9a24e146d488d271b
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AT benxinchi utilizingdistributedacousticsensingandoceanbottomfiberopticcablesforsubmarinestructuralcharacterization
AT nathanieljlindsey utilizingdistributedacousticsensingandoceanbottomfiberopticcablesforsubmarinestructuralcharacterization
AT tcraigdawe utilizingdistributedacousticsensingandoceanbottomfiberopticcablesforsubmarinestructuralcharacterization
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