A monitoring system for spatiotemporal electrical self-potential measurements in cryospheric environments

Climate-induced warming increasingly leads to degradation of high-alpine permafrost. In order to develop early warning systems for imminent slope destabilization, knowledge about hydrological flow processes in the subsurface is urgently needed. Due to the fast dynamics associated with slope failures...

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Main Authors: Weigand, Maximilian, Wagner, Florian M., Limbrock, Jonas K., Hilbich, Christin, Hauck, Christian, Kemna, Andreas
Format: Text
Language:English
Published: 2020
Subjects:
Ice
Online Access:https://doi.org/10.5194/gi-2020-5
https://gi.copernicus.org/preprints/gi-2020-5/
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spelling ftcopernicus:oai:publications.copernicus.org:gid84333 2023-05-15T16:37:46+02:00 A monitoring system for spatiotemporal electrical self-potential measurements in cryospheric environments Weigand, Maximilian Wagner, Florian M. Limbrock, Jonas K. Hilbich, Christin Hauck, Christian Kemna, Andreas 2020-03-16 application/pdf https://doi.org/10.5194/gi-2020-5 https://gi.copernicus.org/preprints/gi-2020-5/ eng eng doi:10.5194/gi-2020-5 https://gi.copernicus.org/preprints/gi-2020-5/ eISSN: 2193-0864 Text 2020 ftcopernicus https://doi.org/10.5194/gi-2020-5 2020-07-20T16:22:21Z Climate-induced warming increasingly leads to degradation of high-alpine permafrost. In order to develop early warning systems for imminent slope destabilization, knowledge about hydrological flow processes in the subsurface is urgently needed. Due to the fast dynamics associated with slope failures, non- or minimally invasive methods are required for cheap and timely characterization and monitoring of potential failure sites to allow in-time responses. These requirements can potentially be met by geophysical methods usually applied in near-surface geophysical settings, such as electrical resistivity tomography (ERT), ground penetrating radar (GPR), various seismic methods, and self-potential (SP) measurements. While ERT and GPR have their primary uses in detecting lithological subsurface structure and liquid water/ice content variations, SP measurements are sensitive to active water flow in the subsurface. Combined, these methods provide huge potential to monitor the dynamic hydrological evolution of permafrost systems. However, while conceptually simple, the technical application of the SP method in high-alpine mountain regions is challenging, especially if spatially resolved information is required. We here report on the design, construction, and testing phase of a multi-electrode SP measurement system aimed at characterizing surface runoff and melt-water flow at the Schilthorn, Bernese Alps, Switzerland. Design requirements for a year-round measurement system are discussed, the hardware and software of the constructed system, as well as test measurements are presented, including detailed quality assessment studies. On-site noise measurements and one laboratory experiment on freezing and thawing characteristics of the SP electrodes provide supporting information. It was found that a detailed quality assessment of the measured data is important for such challenging field site operations, requiring adapted measurement schemes to allow for the extraction of robust data in light of an environment highly contaminated by anthropogenic and natural noise components. Finally, possible short- and long-term improvements to the system are discussed and recommendations for future installations are developed. Text Ice permafrost Copernicus Publications: E-Journals
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description Climate-induced warming increasingly leads to degradation of high-alpine permafrost. In order to develop early warning systems for imminent slope destabilization, knowledge about hydrological flow processes in the subsurface is urgently needed. Due to the fast dynamics associated with slope failures, non- or minimally invasive methods are required for cheap and timely characterization and monitoring of potential failure sites to allow in-time responses. These requirements can potentially be met by geophysical methods usually applied in near-surface geophysical settings, such as electrical resistivity tomography (ERT), ground penetrating radar (GPR), various seismic methods, and self-potential (SP) measurements. While ERT and GPR have their primary uses in detecting lithological subsurface structure and liquid water/ice content variations, SP measurements are sensitive to active water flow in the subsurface. Combined, these methods provide huge potential to monitor the dynamic hydrological evolution of permafrost systems. However, while conceptually simple, the technical application of the SP method in high-alpine mountain regions is challenging, especially if spatially resolved information is required. We here report on the design, construction, and testing phase of a multi-electrode SP measurement system aimed at characterizing surface runoff and melt-water flow at the Schilthorn, Bernese Alps, Switzerland. Design requirements for a year-round measurement system are discussed, the hardware and software of the constructed system, as well as test measurements are presented, including detailed quality assessment studies. On-site noise measurements and one laboratory experiment on freezing and thawing characteristics of the SP electrodes provide supporting information. It was found that a detailed quality assessment of the measured data is important for such challenging field site operations, requiring adapted measurement schemes to allow for the extraction of robust data in light of an environment highly contaminated by anthropogenic and natural noise components. Finally, possible short- and long-term improvements to the system are discussed and recommendations for future installations are developed.
format Text
author Weigand, Maximilian
Wagner, Florian M.
Limbrock, Jonas K.
Hilbich, Christin
Hauck, Christian
Kemna, Andreas
spellingShingle Weigand, Maximilian
Wagner, Florian M.
Limbrock, Jonas K.
Hilbich, Christin
Hauck, Christian
Kemna, Andreas
A monitoring system for spatiotemporal electrical self-potential measurements in cryospheric environments
author_facet Weigand, Maximilian
Wagner, Florian M.
Limbrock, Jonas K.
Hilbich, Christin
Hauck, Christian
Kemna, Andreas
author_sort Weigand, Maximilian
title A monitoring system for spatiotemporal electrical self-potential measurements in cryospheric environments
title_short A monitoring system for spatiotemporal electrical self-potential measurements in cryospheric environments
title_full A monitoring system for spatiotemporal electrical self-potential measurements in cryospheric environments
title_fullStr A monitoring system for spatiotemporal electrical self-potential measurements in cryospheric environments
title_full_unstemmed A monitoring system for spatiotemporal electrical self-potential measurements in cryospheric environments
title_sort monitoring system for spatiotemporal electrical self-potential measurements in cryospheric environments
publishDate 2020
url https://doi.org/10.5194/gi-2020-5
https://gi.copernicus.org/preprints/gi-2020-5/
genre Ice
permafrost
genre_facet Ice
permafrost
op_source eISSN: 2193-0864
op_relation doi:10.5194/gi-2020-5
https://gi.copernicus.org/preprints/gi-2020-5/
op_doi https://doi.org/10.5194/gi-2020-5
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