Two-dimensional inversion of wideband spectral data from the capacitively coupled resistivity method – first applications in periglacial environments
The DC resistivity method is a common tool in periglacial research because it can delineate zones of large resistivities, which are often associated with frozen water. The interpretation can be ambiguous, however, because large resistivities may also have other causes, like solid dry rock. One possi...
Published in: | The Cryosphere |
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Format: | Article in Journal/Newspaper |
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Copernicus Publications
2019
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ftnonlinearchiv:oai:noa.gwlb.de:cop_mods_00040419 2023-05-15T18:32:33+02:00 Two-dimensional inversion of wideband spectral data from the capacitively coupled resistivity method – first applications in periglacial environments Mudler, Jan Hördt, Andreas Przyklenk, Anita Fiandaca, Gianluca Maurya, Pradip Kumar Hauck, Christian 2019-09 electronic https://doi.org/10.5194/tc-13-2439-2019 https://noa.gwlb.de/receive/cop_mods_00040419 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00040043/tc-13-2439-2019.pdf https://tc.copernicus.org/articles/13/2439/2019/tc-13-2439-2019.pdf eng eng Copernicus Publications The Cryosphere -- ˜Theœ Cryosphere -- http://www.bibliothek.uni-regensburg.de/ezeit/?2393169 -- http://www.the-cryosphere.net/ -- 1994-0424 https://doi.org/10.5194/tc-13-2439-2019 https://noa.gwlb.de/receive/cop_mods_00040419 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00040043/tc-13-2439-2019.pdf https://tc.copernicus.org/articles/13/2439/2019/tc-13-2439-2019.pdf https://creativecommons.org/licenses/by/4.0/ uneingeschränkt info:eu-repo/semantics/openAccess CC-BY article Verlagsveröffentlichung article Text doc-type:article 2019 ftnonlinearchiv https://doi.org/10.5194/tc-13-2439-2019 2022-02-08T22:42:07Z The DC resistivity method is a common tool in periglacial research because it can delineate zones of large resistivities, which are often associated with frozen water. The interpretation can be ambiguous, however, because large resistivities may also have other causes, like solid dry rock. One possibility to reduce the ambiguity is to measure the frequency-dependent resistivity. At low frequencies (< 100 Hz) the corresponding method is called induced polarization, which has also been used in periglacial environments. For the detection and possibly quantification of water ice, a higher frequency range, between 100 Hz and 100 kHz, may be particularly interesting because in that range, the electrical properties of water ice exhibit a characteristic behaviour. In addition, the large frequencies allow a capacitive coupling of the electrodes, which may have logistical advantages. The capacitively coupled resistivity (CCR) method tries to combine these logistical advantages with the potential scientific benefit of reduced ambiguity. In this paper, we discuss CCR data obtained at two field sites with cryospheric influence: the Schilthorn massif in the Swiss Alps and the frozen Lake Prestvannet in the northern part of Norway. One objective is to add examples to the literature where the method is assessed in different conditions. Our results agree reasonably well with known subsurface structure: at the Prestvannet site, the transition from a frozen lake to the land is clearly visible in the inversion results, whereas at the Schilthorn site, the boundary between a snow cover and the bedrock below can be nicely delineated. In both cases, the electrical parameters are consistent with those expected from literature. The second objective is to discuss useful methodological advancements: first, we investigate the effect of capacitive sensor height above the surface and corroborate the assumption that it is negligible for highly resistive conditions. For the inversion of the data, we modified an existing 2-D inversion code originally developed for low-frequency induced polarization data by including a parametrization of electrical permittivity. The new inversion code allows the extraction of electrical parameters that may be directly compared with literature values, which was previously not possible. Article in Journal/Newspaper The Cryosphere Niedersächsisches Online-Archiv NOA Frozen Lake ENVELOPE(76.108,76.108,-69.415,-69.415) Norway The Cryosphere 13 9 2439 2456 |
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Niedersächsisches Online-Archiv NOA |
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language |
English |
topic |
article Verlagsveröffentlichung |
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article Verlagsveröffentlichung Mudler, Jan Hördt, Andreas Przyklenk, Anita Fiandaca, Gianluca Maurya, Pradip Kumar Hauck, Christian Two-dimensional inversion of wideband spectral data from the capacitively coupled resistivity method – first applications in periglacial environments |
topic_facet |
article Verlagsveröffentlichung |
description |
The DC resistivity method is a common tool in periglacial research because it can delineate zones of large resistivities, which are often associated with frozen water. The interpretation can be ambiguous, however, because large resistivities may also have other causes, like solid dry rock. One possibility to reduce the ambiguity is to measure the frequency-dependent resistivity. At low frequencies (< 100 Hz) the corresponding method is called induced polarization, which has also been used in periglacial environments. For the detection and possibly quantification of water ice, a higher frequency range, between 100 Hz and 100 kHz, may be particularly interesting because in that range, the electrical properties of water ice exhibit a characteristic behaviour. In addition, the large frequencies allow a capacitive coupling of the electrodes, which may have logistical advantages. The capacitively coupled resistivity (CCR) method tries to combine these logistical advantages with the potential scientific benefit of reduced ambiguity. In this paper, we discuss CCR data obtained at two field sites with cryospheric influence: the Schilthorn massif in the Swiss Alps and the frozen Lake Prestvannet in the northern part of Norway. One objective is to add examples to the literature where the method is assessed in different conditions. Our results agree reasonably well with known subsurface structure: at the Prestvannet site, the transition from a frozen lake to the land is clearly visible in the inversion results, whereas at the Schilthorn site, the boundary between a snow cover and the bedrock below can be nicely delineated. In both cases, the electrical parameters are consistent with those expected from literature. The second objective is to discuss useful methodological advancements: first, we investigate the effect of capacitive sensor height above the surface and corroborate the assumption that it is negligible for highly resistive conditions. For the inversion of the data, we modified an existing 2-D inversion code originally developed for low-frequency induced polarization data by including a parametrization of electrical permittivity. The new inversion code allows the extraction of electrical parameters that may be directly compared with literature values, which was previously not possible. |
format |
Article in Journal/Newspaper |
author |
Mudler, Jan Hördt, Andreas Przyklenk, Anita Fiandaca, Gianluca Maurya, Pradip Kumar Hauck, Christian |
author_facet |
Mudler, Jan Hördt, Andreas Przyklenk, Anita Fiandaca, Gianluca Maurya, Pradip Kumar Hauck, Christian |
author_sort |
Mudler, Jan |
title |
Two-dimensional inversion of wideband spectral data from the capacitively coupled resistivity method – first applications in periglacial environments |
title_short |
Two-dimensional inversion of wideband spectral data from the capacitively coupled resistivity method – first applications in periglacial environments |
title_full |
Two-dimensional inversion of wideband spectral data from the capacitively coupled resistivity method – first applications in periglacial environments |
title_fullStr |
Two-dimensional inversion of wideband spectral data from the capacitively coupled resistivity method – first applications in periglacial environments |
title_full_unstemmed |
Two-dimensional inversion of wideband spectral data from the capacitively coupled resistivity method – first applications in periglacial environments |
title_sort |
two-dimensional inversion of wideband spectral data from the capacitively coupled resistivity method – first applications in periglacial environments |
publisher |
Copernicus Publications |
publishDate |
2019 |
url |
https://doi.org/10.5194/tc-13-2439-2019 https://noa.gwlb.de/receive/cop_mods_00040419 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00040043/tc-13-2439-2019.pdf https://tc.copernicus.org/articles/13/2439/2019/tc-13-2439-2019.pdf |
long_lat |
ENVELOPE(76.108,76.108,-69.415,-69.415) |
geographic |
Frozen Lake Norway |
geographic_facet |
Frozen Lake Norway |
genre |
The Cryosphere |
genre_facet |
The Cryosphere |
op_relation |
The Cryosphere -- ˜Theœ Cryosphere -- http://www.bibliothek.uni-regensburg.de/ezeit/?2393169 -- http://www.the-cryosphere.net/ -- 1994-0424 https://doi.org/10.5194/tc-13-2439-2019 https://noa.gwlb.de/receive/cop_mods_00040419 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00040043/tc-13-2439-2019.pdf https://tc.copernicus.org/articles/13/2439/2019/tc-13-2439-2019.pdf |
op_rights |
https://creativecommons.org/licenses/by/4.0/ uneingeschränkt info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.5194/tc-13-2439-2019 |
container_title |
The Cryosphere |
container_volume |
13 |
container_issue |
9 |
container_start_page |
2439 |
op_container_end_page |
2456 |
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1766216755452051456 |