Monitoring ground water storage at mesoscale using seismic noise: 30 years of continuous observation and thermo-elastic and hydrological modeling

Abstract Groundwater is a vital freshwater resource for both humans and ecosystems. Achieving sustainable management requires a detailed knowledge of the aquifer structure and of its behavior in response to climatic and anthropogenic forcing. Traditional monitoring is carried out using piezometer ne...

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Autores principales: Thomas Lecocq, Laurent Longuevergne, Helle Anette Pedersen, Florent Brenguier, Klaus Stammler
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Lenguaje:EN
Publicado: Nature Portfolio 2017
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Acceso en línea:https://doaj.org/article/21527fcb39334c3285ad01c2f61aff0a
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spelling oai:doaj.org-article:21527fcb39334c3285ad01c2f61aff0a2021-12-02T11:40:53ZMonitoring ground water storage at mesoscale using seismic noise: 30 years of continuous observation and thermo-elastic and hydrological modeling10.1038/s41598-017-14468-92045-2322https://doaj.org/article/21527fcb39334c3285ad01c2f61aff0a2017-10-01T00:00:00Zhttps://doi.org/10.1038/s41598-017-14468-9https://doaj.org/toc/2045-2322Abstract Groundwater is a vital freshwater resource for both humans and ecosystems. Achieving sustainable management requires a detailed knowledge of the aquifer structure and of its behavior in response to climatic and anthropogenic forcing. Traditional monitoring is carried out using piezometer networks, and recently complemented with new geophysical or satellite-based observations. These techniques survey either local (small-scale) water systems or regional areas (large scale) but, to date, adequate observation tools are lacking at the water management scale (i.e. several tens of kms), which is generally explored by modeling. Using 30 years of continuous recording by four seismic stations of the Gräfenberg Array (Germany), we demonstrate that long-term observations of velocity variations (approximately 0.01%) of surface waves can be extracted from such recordings of ocean-generated seismic noise. These small variations can be explained by changes to mechanical properties of the complex aquifer system in the top few hundred meters of the crust. The velocity changes can be interpreted as effects of temperature diffusion and water storage changes. Seismic noise recordings may become a new and valuable tool to monitor heterogeneous groundwater systems at mesoscale, in addition to existing observation methods.Thomas LecocqLaurent LonguevergneHelle Anette PedersenFlorent BrenguierKlaus StammlerNature PortfolioarticleMedicineRScienceQENScientific Reports, Vol 7, Iss 1, Pp 1-16 (2017)
institution DOAJ
collection DOAJ
language EN
topic Medicine
R
Science
Q
spellingShingle Medicine
R
Science
Q
Thomas Lecocq
Laurent Longuevergne
Helle Anette Pedersen
Florent Brenguier
Klaus Stammler
Monitoring ground water storage at mesoscale using seismic noise: 30 years of continuous observation and thermo-elastic and hydrological modeling
description Abstract Groundwater is a vital freshwater resource for both humans and ecosystems. Achieving sustainable management requires a detailed knowledge of the aquifer structure and of its behavior in response to climatic and anthropogenic forcing. Traditional monitoring is carried out using piezometer networks, and recently complemented with new geophysical or satellite-based observations. These techniques survey either local (small-scale) water systems or regional areas (large scale) but, to date, adequate observation tools are lacking at the water management scale (i.e. several tens of kms), which is generally explored by modeling. Using 30 years of continuous recording by four seismic stations of the Gräfenberg Array (Germany), we demonstrate that long-term observations of velocity variations (approximately 0.01%) of surface waves can be extracted from such recordings of ocean-generated seismic noise. These small variations can be explained by changes to mechanical properties of the complex aquifer system in the top few hundred meters of the crust. The velocity changes can be interpreted as effects of temperature diffusion and water storage changes. Seismic noise recordings may become a new and valuable tool to monitor heterogeneous groundwater systems at mesoscale, in addition to existing observation methods.
format article
author Thomas Lecocq
Laurent Longuevergne
Helle Anette Pedersen
Florent Brenguier
Klaus Stammler
author_facet Thomas Lecocq
Laurent Longuevergne
Helle Anette Pedersen
Florent Brenguier
Klaus Stammler
author_sort Thomas Lecocq
title Monitoring ground water storage at mesoscale using seismic noise: 30 years of continuous observation and thermo-elastic and hydrological modeling
title_short Monitoring ground water storage at mesoscale using seismic noise: 30 years of continuous observation and thermo-elastic and hydrological modeling
title_full Monitoring ground water storage at mesoscale using seismic noise: 30 years of continuous observation and thermo-elastic and hydrological modeling
title_fullStr Monitoring ground water storage at mesoscale using seismic noise: 30 years of continuous observation and thermo-elastic and hydrological modeling
title_full_unstemmed Monitoring ground water storage at mesoscale using seismic noise: 30 years of continuous observation and thermo-elastic and hydrological modeling
title_sort monitoring ground water storage at mesoscale using seismic noise: 30 years of continuous observation and thermo-elastic and hydrological modeling
publisher Nature Portfolio
publishDate 2017
url https://doaj.org/article/21527fcb39334c3285ad01c2f61aff0a
work_keys_str_mv AT thomaslecocq monitoringgroundwaterstorageatmesoscaleusingseismicnoise30yearsofcontinuousobservationandthermoelasticandhydrologicalmodeling
AT laurentlonguevergne monitoringgroundwaterstorageatmesoscaleusingseismicnoise30yearsofcontinuousobservationandthermoelasticandhydrologicalmodeling
AT helleanettepedersen monitoringgroundwaterstorageatmesoscaleusingseismicnoise30yearsofcontinuousobservationandthermoelasticandhydrologicalmodeling
AT florentbrenguier monitoringgroundwaterstorageatmesoscaleusingseismicnoise30yearsofcontinuousobservationandthermoelasticandhydrologicalmodeling
AT klausstammler monitoringgroundwaterstorageatmesoscaleusingseismicnoise30yearsofcontinuousobservationandthermoelasticandhydrologicalmodeling
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