Articles | Volume 13, issue 9
https://doi.org/10.5194/tc-13-2439-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-13-2439-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
20 Sep 2019
Research article |
| 20 Sep 2019
| 20 Sep 2019
Two-dimensional inversion of wideband spectral data from the capacitively coupled resistivity method – first applications in periglacial environments
Jan Mudler
CORRESPONDING AUTHOR
Institut für Geophysik und extraterrestrische Physik, Technische Universität Braunschweig, Braunschweig, Germany
Andreas Hördt
Institut für Geophysik und extraterrestrische Physik, Technische Universität Braunschweig, Braunschweig, Germany
Anita Przyklenk
Institut für Geophysik und extraterrestrische Physik, Technische Universität Braunschweig, Braunschweig, Germany
Gianluca Fiandaca
Department of Geoscience, Hydrogeophysics Group, Aarhus University, Aarhus, Denmark
Pradip Kumar Maurya
Department of Geoscience, Hydrogeophysics Group, Aarhus University, Aarhus, Denmark
Christian Hauck
Department of Geosciences, University of Fribourg, Fribourg, Switzerland
Related authors
Jan Mudler, Andreas Hördt, Dennis Kreith, Madhuri Sugand, Kirill Bazhin, Lyudmila Lebedeva, and Tino Radić
The Cryosphere, 16, 4727–4744, https://doi.org/10.5194/tc-16-4727-2022, https://doi.org/10.5194/tc-16-4727-2022, 2022
Short summary
Short summary
The spectral electrical signal of ice exhibits a strong characteristic behaviour in the frequency range from 100 Hz to 100 kHz, due to polarization effects. With our geophysical method, we can analyse this characteristic to detect subsurface ice. Moreover, we use a model to quantify 2-D ground ice content based on our data. The potential of our new measurement device is showed up. Data were taken on a permafrost site in Yakutia, and the results are in agreement with other existing field data.
Wilfried Haeberli, Lukas U. Arenson, Julie Wee, Christian Hauck, and Nico Mölg
The Cryosphere, 18, 1669–1683, https://doi.org/10.5194/tc-18-1669-2024, https://doi.org/10.5194/tc-18-1669-2024, 2024
Short summary
Short summary
Rock glaciers in ice-rich permafrost can be discriminated from debris-covered glaciers. The key physical phenomenon relates to the tight mechanical coupling between the moving frozen body at depth and the surface layer of debris in the case of rock glaciers, as opposed to the virtually inexistent coupling in the case of surface ice with a debris cover. Contact zones of surface ice with subsurface ice in permafrost constitute diffuse landforms beyond either–or-type landform classification.
Mohammad Farzamian, Teddi Herring, Goncalo Vieira, Miguel Angel de Pablo, Borhan Yaghoobi Tabar, and Christian Hauck
EGUsphere, https://doi.org/10.5194/egusphere-2023-2908, https://doi.org/10.5194/egusphere-2023-2908, 2024
Short summary
Short summary
An Automated Electrical Resistivity Tomography (A-ERT) system was developed and deployed in Antarctica to monitor permafrost and active layer dynamics. The A-ERT, coupled with an efficient processing workflow, demonstrated its capability to monitor real-time thaw depth progression, detect seasonal and surficial freezing/thawing events, and assess permafrost stability. Our study showcased the potential of A-ERT for contributing to global permafrost monitoring networks.
Bernd Etzelmüller, Ketil Isaksen, Justyna Czekirda, Sebastian Westermann, Christin Hilbich, and Christian Hauck
The Cryosphere, 17, 5477–5497, https://doi.org/10.5194/tc-17-5477-2023, https://doi.org/10.5194/tc-17-5477-2023, 2023
Short summary
Short summary
Permafrost (permanently frozen ground) is widespread in the mountains of Norway and Iceland. Several boreholes were drilled after 1999 for long-term permafrost monitoring. We document a strong warming of permafrost, including the development of unfrozen bodies in the permafrost. Warming and degradation of mountain permafrost may lead to more natural hazards.
Johannes Buckel, Jan Mudler, Rainer Gardeweg, Christian Hauck, Christin Hilbich, Regula Frauenfelder, Christof Kneisel, Sebastian Buchelt, Jan Henrik Blöthe, Andreas Hördt, and Matthias Bücker
The Cryosphere, 17, 2919–2940, https://doi.org/10.5194/tc-17-2919-2023, https://doi.org/10.5194/tc-17-2919-2023, 2023
Short summary
Short summary
This study reveals permafrost degradation by repeating old geophysical measurements at three Alpine sites. The compared data indicate that ice-poor permafrost is highly affected by temperature warming. The melting of ice-rich permafrost could not be identified. However, complex geomorphic processes are responsible for this rather than external temperature change. We suspect permafrost degradation here as well. In addition, we introduce a new current injection method for data acquisition.
Theresa Maierhofer, Adrian Flores Orozco, Nathalie Roser, Jonas K. Limbrock, Christin Hilbich, Clemens Moser, Andreas Kemna, Elisabetta Drigo, Umberto Morra di Cella, and Christian Hauck
EGUsphere, https://doi.org/10.5194/egusphere-2023-671, https://doi.org/10.5194/egusphere-2023-671, 2023
Short summary
Short summary
In this study, we apply an electrical method in a high mountain permafrost terrain in the Italian Alps, where long-term borehole temperature data are available for validation. In particular, we investigate the frequency dependence of the electrical properties for seasonal and annual variations along three years monitoring period. We demonstrate that our method is capable of resolving temporal changes in the thermal state and the ice/water ratio associated with seasonal freeze-thaw processes.
Adrian Wicki, Peter Lehmann, Christian Hauck, and Manfred Stähli
Nat. Hazards Earth Syst. Sci., 23, 1059–1077, https://doi.org/10.5194/nhess-23-1059-2023, https://doi.org/10.5194/nhess-23-1059-2023, 2023
Short summary
Short summary
Soil wetness measurements are used for shallow landslide prediction; however, existing sites are often located in flat terrain. Here, we assessed the ability of monitoring sites at flat locations to detect critically saturated conditions compared to if they were situated at a landslide-prone location. We found that differences exist but that both sites could equally well distinguish critical from non-critical conditions for shallow landslide triggering if relative changes are considered.
Jan Mudler, Andreas Hördt, Dennis Kreith, Madhuri Sugand, Kirill Bazhin, Lyudmila Lebedeva, and Tino Radić
The Cryosphere, 16, 4727–4744, https://doi.org/10.5194/tc-16-4727-2022, https://doi.org/10.5194/tc-16-4727-2022, 2022
Short summary
Short summary
The spectral electrical signal of ice exhibits a strong characteristic behaviour in the frequency range from 100 Hz to 100 kHz, due to polarization effects. With our geophysical method, we can analyse this characteristic to detect subsurface ice. Moreover, we use a model to quantify 2-D ground ice content based on our data. The potential of our new measurement device is showed up. Data were taken on a permafrost site in Yakutia, and the results are in agreement with other existing field data.
Tamara Mathys, Christin Hilbich, Lukas U. Arenson, Pablo A. Wainstein, and Christian Hauck
The Cryosphere, 16, 2595–2615, https://doi.org/10.5194/tc-16-2595-2022, https://doi.org/10.5194/tc-16-2595-2022, 2022
Short summary
Short summary
With ongoing climate change, there is a pressing need to understand how much water is stored as ground ice in permafrost. Still, field-based data on permafrost in the Andes are scarce, resulting in large uncertainties regarding ground ice volumes and their hydrological role. We introduce an upscaling methodology of geophysical-based ground ice quantifications at the catchment scale. Our results indicate that substantial ground ice volumes may also be present in areas without rock glaciers.
Pradip Kumar Maurya, Frederik Ersted Christensen, Masson Andy Kass, Jesper B. Pedersen, Rasmus R. Frederiksen, Nikolaj Foged, Anders Vest Christiansen, and Esben Auken
Hydrol. Earth Syst. Sci., 26, 2813–2827, https://doi.org/10.5194/hess-26-2813-2022, https://doi.org/10.5194/hess-26-2813-2022, 2022
Short summary
Short summary
In this paper, we present an application of the electromagnetic method to image the subsurface below rivers, lakes, or any surface water body. The scanning of the subsurface is carried out by sailing an electromagnetic sensor called FloaTEM. Imaging results show a 3D distribution of different sediment types below the freshwater lakes. In the case of saline water, the system is capable of identifying the probable location of groundwater discharge into seawater.
Theresa Maierhofer, Christian Hauck, Christin Hilbich, Andreas Kemna, and Adrián Flores-Orozco
The Cryosphere, 16, 1903–1925, https://doi.org/10.5194/tc-16-1903-2022, https://doi.org/10.5194/tc-16-1903-2022, 2022
Short summary
Short summary
We extend the application of electrical methods to characterize alpine permafrost using the so-called induced polarization (IP) effect associated with the storage of charges at the interface between liquid and solid phases. We investigate different field protocols to enhance data quality and conclude that with appropriate measurement and processing procedures, the characteristic dependence of the IP response of frozen rocks improves the assessment of thermal state and ice content in permafrost.
Christin Hilbich, Christian Hauck, Coline Mollaret, Pablo Wainstein, and Lukas U. Arenson
The Cryosphere, 16, 1845–1872, https://doi.org/10.5194/tc-16-1845-2022, https://doi.org/10.5194/tc-16-1845-2022, 2022
Short summary
Short summary
In view of water scarcity in the Andes, the significance of permafrost as a future water resource is often debated focusing on satellite-detected features such as rock glaciers. We present data from > 50 geophysical surveys in Chile and Argentina to quantify the ground ice volume stored in various permafrost landforms, showing that not only rock glacier but also non-rock-glacier permafrost contains significant ground ice volumes and is relevant when assessing the hydrological role of permafrost.
Martin Hoelzle, Christian Hauck, Tamara Mathys, Jeannette Noetzli, Cécile Pellet, and Martin Scherler
Earth Syst. Sci. Data, 14, 1531–1547, https://doi.org/10.5194/essd-14-1531-2022, https://doi.org/10.5194/essd-14-1531-2022, 2022
Short summary
Short summary
With ongoing climate change, it is crucial to understand the interactions of the individual heat fluxes at the surface and within the subsurface layers, as well as their impacts on the permafrost thermal regime. A unique set of high-altitude meteorological measurements has been analysed to determine the energy balance at three mountain permafrost sites in the Swiss Alps, where data have been collected since the late 1990s in collaboration with the Swiss Permafrost Monitoring Network (PERMOS).
Bernd Etzelmüller, Justyna Czekirda, Florence Magnin, Pierre-Allain Duvillard, Ludovic Ravanel, Emanuelle Malet, Andreas Aspaas, Lene Kristensen, Ingrid Skrede, Gudrun D. Majala, Benjamin Jacobs, Johannes Leinauer, Christian Hauck, Christin Hilbich, Martina Böhme, Reginald Hermanns, Harald Ø. Eriksen, Tom Rune Lauknes, Michael Krautblatter, and Sebastian Westermann
Earth Surf. Dynam., 10, 97–129, https://doi.org/10.5194/esurf-10-97-2022, https://doi.org/10.5194/esurf-10-97-2022, 2022
Short summary
Short summary
This paper is a multi-authored study documenting the possible existence of permafrost in permanently monitored rockslides in Norway for the first time by combining a multitude of field data, including geophysical surveys in rock walls. The paper discusses the possible role of thermal regime and rockslide movement, and it evaluates the possible impact of atmospheric warming on rockslide dynamics in Norwegian mountains.
Adrian Wicki, Per-Erik Jansson, Peter Lehmann, Christian Hauck, and Manfred Stähli
Hydrol. Earth Syst. Sci., 25, 4585–4610, https://doi.org/10.5194/hess-25-4585-2021, https://doi.org/10.5194/hess-25-4585-2021, 2021
Short summary
Short summary
Soil moisture information was shown to be valuable for landslide prediction. Soil moisture was simulated at 133 sites in Switzerland, and the temporal variability was compared to the regional occurrence of landslides. We found that simulated soil moisture is a good predictor for landslides, and that the forecast goodness is similar to using in situ measurements. This encourages the use of models for complementing existing soil moisture monitoring networks for regional landslide early warning.
Alexis Neven, Pradip Kumar Maurya, Anders Vest Christiansen, and Philippe Renard
Earth Syst. Sci. Data, 13, 2743–2752, https://doi.org/10.5194/essd-13-2743-2021, https://doi.org/10.5194/essd-13-2743-2021, 2021
Short summary
Short summary
The shallow underground is constituted of sediments that present high spatial variability. This upper layer is the most extensively used for resource exploitation (groundwater, geothermal heat, construction materials, etc.). Understanding and modeling the spatial variability of these deposits is crucial. We present a high-resolution electrical resistivity dataset that covers the upper Aare Valley in Switzerland. These data can help develop methods to characterize these geological formations.
Christian Halla, Jan Henrik Blöthe, Carla Tapia Baldis, Dario Trombotto Liaudat, Christin Hilbich, Christian Hauck, and Lothar Schrott
The Cryosphere, 15, 1187–1213, https://doi.org/10.5194/tc-15-1187-2021, https://doi.org/10.5194/tc-15-1187-2021, 2021
Short summary
Short summary
In the semi-arid to arid Andes of Argentina, rock glaciers contain invisible and unknown amounts of ground ice that could become more important in future for the water availability during the dry season. The study shows that the investigated rock glacier represents an important long-term ice reservoir in the dry mountain catchment and that interannual changes of ground ice can store and release significant amounts of annual precipitation.
Maximilian Weigand, Florian M. Wagner, Jonas K. Limbrock, Christin Hilbich, Christian Hauck, and Andreas Kemna
Geosci. Instrum. Method. Data Syst., 9, 317–336, https://doi.org/10.5194/gi-9-317-2020, https://doi.org/10.5194/gi-9-317-2020, 2020
Short summary
Short summary
In times of global warming, permafrost is starting to degrade at alarming rates, requiring new and improved characterization approaches. We describe the design and test installation, as well as detailed data quality assessment, of a monitoring system used to capture natural electrical potentials in the subsurface. These self-potential signals are of great interest for the noninvasive investigation of water flow in the non-frozen or partially frozen subsurface.
Mohammad Farzamian, Gonçalo Vieira, Fernando A. Monteiro Santos, Borhan Yaghoobi Tabar, Christian Hauck, Maria Catarina Paz, Ivo Bernardo, Miguel Ramos, and Miguel Angel de Pablo
The Cryosphere, 14, 1105–1120, https://doi.org/10.5194/tc-14-1105-2020, https://doi.org/10.5194/tc-14-1105-2020, 2020
Short summary
Short summary
A 2-D automated electrical resistivity tomography (A-ERT) system was installed for the first time in Antarctica at Deception Island to (i) monitor subsurface freezing and thawing processes on a daily and seasonal basis and map the spatial and temporal variability of thaw depth and to (ii) study the impact of short-lived extreme meteorological events on active layer dynamics.
Coline Mollaret, Christin Hilbich, Cécile Pellet, Adrian Flores-Orozco, Reynald Delaloye, and Christian Hauck
The Cryosphere, 13, 2557–2578, https://doi.org/10.5194/tc-13-2557-2019, https://doi.org/10.5194/tc-13-2557-2019, 2019
Short summary
Short summary
We present a long-term multisite electrical resistivity tomography monitoring network (more than 1000 datasets recorded from six mountain permafrost sites). Despite harsh and remote measurement conditions, the datasets are of good quality and show consistent spatio-temporal variations yielding significant added value to point-scale borehole information. Observed long-term trends are similar for all permafrost sites, showing ongoing permafrost thaw and ground ice loss due to climatic conditions.
Martin Beniston, Daniel Farinotti, Markus Stoffel, Liss M. Andreassen, Erika Coppola, Nicolas Eckert, Adriano Fantini, Florie Giacona, Christian Hauck, Matthias Huss, Hendrik Huwald, Michael Lehning, Juan-Ignacio López-Moreno, Jan Magnusson, Christoph Marty, Enrique Morán-Tejéda, Samuel Morin, Mohamed Naaim, Antonello Provenzale, Antoine Rabatel, Delphine Six, Johann Stötter, Ulrich Strasser, Silvia Terzago, and Christian Vincent
The Cryosphere, 12, 759–794, https://doi.org/10.5194/tc-12-759-2018, https://doi.org/10.5194/tc-12-759-2018, 2018
Short summary
Short summary
This paper makes a rather exhaustive overview of current knowledge of past, current, and future aspects of cryospheric issues in continental Europe and makes a number of reflections of areas of uncertainty requiring more attention in both scientific and policy terms. The review paper is completed by a bibliography containing 350 recent references that will certainly be of value to scholars engaged in the fields of glacier, snow, and permafrost research.
Benjamin Mewes, Christin Hilbich, Reynald Delaloye, and Christian Hauck
The Cryosphere, 11, 2957–2974, https://doi.org/10.5194/tc-11-2957-2017, https://doi.org/10.5194/tc-11-2957-2017, 2017
Cécile Pellet and Christian Hauck
Hydrol. Earth Syst. Sci., 21, 3199–3220, https://doi.org/10.5194/hess-21-3199-2017, https://doi.org/10.5194/hess-21-3199-2017, 2017
Short summary
Short summary
This paper presents a detailed description of the new Swiss soil moisture monitoring network SOMOMOUNT, which comprises six stations distributed along an elevation gradient ranging from 1205 to 3410 m. The liquid soil moisture (LSM) data collected during the first 3 years are discussed with regard to their soil type and climate dependency as well as their altitudinal distribution. The elevation dependency of the LSM was found to be non-linear with distinct dynamics at high and low elevation.
Jonas Wicky and Christian Hauck
The Cryosphere, 11, 1311–1325, https://doi.org/10.5194/tc-11-1311-2017, https://doi.org/10.5194/tc-11-1311-2017, 2017
Short summary
Short summary
Talus slopes are a widespread geomorphic feature, which may show permafrost conditions even at low elevation due to cold microclimates induced by a gravity-driven internal air circulation. We show for the first time a numerical simulation of this internal air circulation of a field-scale talus slope. Results indicate that convective heat transfer leads to a pronounced ground cooling in the lower part of the talus slope favoring the persistence of permafrost.
Antoine Marmy, Jan Rajczak, Reynald Delaloye, Christin Hilbich, Martin Hoelzle, Sven Kotlarski, Christophe Lambiel, Jeannette Noetzli, Marcia Phillips, Nadine Salzmann, Benno Staub, and Christian Hauck
The Cryosphere, 10, 2693–2719, https://doi.org/10.5194/tc-10-2693-2016, https://doi.org/10.5194/tc-10-2693-2016, 2016
Short summary
Short summary
This paper presents a new semi-automated method to calibrate the 1-D soil model COUP. It is the first time (as far as we know) that this approach is developed for mountain permafrost. It is applied at six test sites in the Swiss Alps. In a second step, the calibrated model is used for RCM-based simulations with specific downscaling of RCM data to the borehole scale. We show projections of the permafrost evolution at the six sites until the end of the century and according to the A1B scenario.
A. Ekici, S. Chadburn, N. Chaudhary, L. H. Hajdu, A. Marmy, S. Peng, J. Boike, E. Burke, A. D. Friend, C. Hauck, G. Krinner, M. Langer, P. A. Miller, and C. Beer
The Cryosphere, 9, 1343–1361, https://doi.org/10.5194/tc-9-1343-2015, https://doi.org/10.5194/tc-9-1343-2015, 2015
Short summary
Short summary
This paper compares the performance of different land models in estimating soil thermal regimes at distinct cold region landscape types. Comparing models with different processes reveal the importance of surface insulation (snow/moss layer) and soil internal processes (heat/water transfer). The importance of model processes also depend on site conditions such as high/low snow cover, dry/wet soil types.
P. Pogliotti, M. Guglielmin, E. Cremonese, U. Morra di Cella, G. Filippa, C. Pellet, and C. Hauck
The Cryosphere, 9, 647–661, https://doi.org/10.5194/tc-9-647-2015, https://doi.org/10.5194/tc-9-647-2015, 2015
Short summary
Short summary
This study presents the thermal state and recent evolution of permafrost at Cime Bianche.
The analysis reveals that (i) spatial variability of MAGST is greater than its interannual variability and is controlled by snow duration and air temperature during the snow-free period, (ii) the ALT has a pronounced spatial variability caused by a different subsurface ice and water content, and (iii) permafrost is warming at significant rates below 8m of depth.
B. Staub, A. Marmy, C. Hauck, C. Hilbich, and R. Delaloye
Geogr. Helv., 70, 45–62, https://doi.org/10.5194/gh-70-45-2015, https://doi.org/10.5194/gh-70-45-2015, 2015
A. Ekici, C. Beer, S. Hagemann, J. Boike, M. Langer, and C. Hauck
Geosci. Model Dev., 7, 631–647, https://doi.org/10.5194/gmd-7-631-2014, https://doi.org/10.5194/gmd-7-631-2014, 2014
M. Scherler, S. Schneider, M. Hoelzle, and C. Hauck
Earth Surf. Dynam., 2, 141–154, https://doi.org/10.5194/esurf-2-141-2014, https://doi.org/10.5194/esurf-2-141-2014, 2014
S. Schneider, S. Daengeli, C. Hauck, and M. Hoelzle
Geogr. Helv., 68, 265–280, https://doi.org/10.5194/gh-68-265-2013, https://doi.org/10.5194/gh-68-265-2013, 2013
D. Herckenrath, G. Fiandaca, E. Auken, and P. Bauer-Gottwein
Hydrol. Earth Syst. Sci., 17, 4043–4060, https://doi.org/10.5194/hess-17-4043-2013, https://doi.org/10.5194/hess-17-4043-2013, 2013
Cited articles
Achammer, T. and Denoth, A.: Snow dielectric properties: from DC to
microwave X-band, Ann Glaciol, 19, 92–96,
https://doi.org/10.3189/S0260305500011034, 1994. a
Arenson, L., Colgan, W., and Marshall, H.: Physical, Thermal, and
Mechanical Properties of Snow, Ice, and Permafrost, in: Snow and Ice-Related
Hazards, Risks and Disasters, https://doi.org/10.1016/B978-0-12-394849-6.00002-0, 2015. a, b, c, d
Artemov, V. and Volkov, A.: Water and Ice Dielectric Spectra Scaling at
0 ∘C, Ferroelectrics, 466, 158–165,
https://doi.org/10.1080/00150193.2014.895216, 2014. a, b
Auken, E., Christiansen, A., Kirkegaard, C., Fiandaca, G., Schamper,
C., Behroozmand, A., Binley, A., Nielsen, E., Effersø, F.,
Christensen, N., Sørensen, K., Foged, N., and Vignoli, G.: An
overview of a highly versatile forward and stable inverse algorithm for
airborne, ground-based and borehole electromagnetic and electric data,
Explor. Geophys., 46, 223–235, https://doi.org/10.1071/EG13097, 2014. a, b
Auty, R. and Cole, R.: Dielectric Properties of Ice and Solid D2O, J. Chem.
Phys., 20, 1309, https://doi.org/10.1063/1.1700726, 1952. a, b
Bittelli, M., Flury, M., and Roth, K.: Use of dielectric spectroscopy to
estimate ice content in frozen porous media, Water Resour. Res., 40, W04212,
https://doi.org/10.1029/2003WR002343, 2004. a, b
Cole, K. and Cole, R.: Dispersion and Absorption in Dielectrics:
1.Alternating Current Characteristics, J. Chem. Phys., 9, 341–351,
https://doi.org/10.1063/1.1750906, 1941. a
Dashevsky, Y., Dashevsky, O., Filkovsky, M., and Synakh, V.:
Capacitance Sounding: a New Geophysical Method for Asphalt Pavement Quality
Evaluation, J. Appl. Geophys., 57, 95–106,
https://doi.org/10.1016/j.jappgeo.2004.10.001, 2005. a
Duvillard, P., Revil, A., Qi, Y., Soueid Ahmed, A., Coperey, A., and
Ravanel, L.: Three-Dimensional Electrical Conductivity and Induced
Polarization Tomography of a Rock Glacier, J. Geophys. Res.-Sol. Ea., 123, 9528–9554, https://doi.org/10.1029/2018JB015965, 2018. a
Evans, S.: Dielectric Properties of Ice and Snow – a Review, J. Glaciol.,
5, 773–792, https://doi.org/10.3189/S0022143000018840, 1965. a, b, c, d
Fiandaca, G.: Induction-free acquisition range in spectral time- and
frequency-domain induced polarization at field scale, Geophys. J. Int.,
https://doi.org/10.1093/gji/ggy409, in press, 2018. a
Fiandaca, G., Ramm, J., Binley, A., Gazoty, A., Christiansen, A., and
Auken, E.: Resolving spectral information from time domain induced
polarization data through 2-D inversion, Geophys. J. Int., 192, 631–646,
https://doi.org/10.1093/gji/ggs060, 2013. a, b
Fiandaca, G., Christiansen, A., and Auken, E.: Depth of Investigation
for Multi-parameters Inversions, European Association of Geoscientists and
Engineers, Near Surface Geoscience 2015, Conference Paper, 631–646,
https://doi.org/10.3997/2214-4609.201413797, 2015. a
Flageul, S., Dabas, M., Thiesson, J., Reijiba, F., and Tabbagh, A.:
First in situ test of a new electrostatic resistivity meter, Near Surf.
Geophys., 11, 265–273, https://doi.org/10.3997/1873-0604.2012063, 2013. a
Grard, R.: A quadrupolar array for measuring the complex permittivity of the
ground: application to Earth prospection and planetary exploration, Meas. Sci.
Technol., 1, 295–301, 1990. a
Grard, R. and Tabbagh, A.: A mobile four-electrode array and its
application to the electrical survey of planetary grounds at shallow depth, J.
Geophys. Res., 96, 4117–4123, https://doi.org/10.1029/90JB02329, 1991. a
Grimm, R., Stillman, D., and MacGregor, J.: Dielectric signatures and
evolution of glacier ice, J. Glaciol., 61, 1159–1170,
https://doi.org/10.3189/2015JoG15J113, 2015. a, b
Günther, T. and Martin, T.: Spectral two-dimensional inversion of
frequency-domain induced polarization data from a mining slag heap, J. Appl.
Geophys., 135, 436–448, https://doi.org/10.1016/j.jappgeo.2016.01.008, 2016. a, b
Hauck, C. and Kneisel, C.: Application of Capacitively-coupled and DC
Electrical Resistivity Imaging for Mountain Permafrost Studies, Permafrost
Periglac., 17, 169–177, https://doi.org/10.1002/ppp.555, 2006. a
Hauck, C. and Kneisel, C.: Applied Geophysics in Periglacial
Environments, Cambridge Univ. Press, https://doi.org/10.1017/CBO9780511535628, 2008. a, b, c
Hauck, C., Böttcher, M., and Maurer, H.: A new model for estimating
subsurface ice content based on combined electrical and seismic data sets,
Cryosphere, 5, 453–468, https://doi.org/10.5194/tc-5-453-2011, 2011. a
Hilbich, C., Hauck, C., Hoelzle, M., Scherler, M., Schudel, L.,
Völksch, I., Vonder Mühll, D., and Mäusbacher, R.: Monitoring
mountain permafrost evolution using electrical resistivity tomography: A
7-year study of seasonal, annual, and long-term variations at Schilthorn,
Swiss Alps, J. Geophys. Res., 113, F01S90, https://doi.org/10.1029/2007JF000799,
2008. a
Hördt, A., Weidelt, P., and Przyklenk, A.: Contact impedance of
grounded and capacitive electrodes, Geophys. J. Int., 193, 187–196,
https://doi.org/10.1093/gji/ggs091, 2013. a
Kemna, A., Binley, A., Ramirez, A., and Daily, W.: Complex resistivity
tomography for environmental applications, Chem. Eng. J., 77, 11–18,
https://doi.org/10.1016/S1385-8947(99)00135-7, 2000. a
Kemna, A., Binley, A., Cassiani, G., Niederleithinger, E., Revil, A.,
Slater, L., Williams, K., Flores Orozco, A., Haegel, F.-H., Hördt,
A., Kruschwitz, S., Leroux, V., Titov, K., and Zimmermann, E.: An
overview of the spectral induced polarization method for near-surface
applications, Near Surf. Geophys., 10, 453–468, 2012. a, b
Kuras, O., Beamish, D., Meldrum, P., and Ogilvy, R.: Fundamentals of
the capacitive resistivity technique, Geophysics, 71, 135–152,
https://doi.org/10.1190/1.2194892, 2006. a, b, c, d
Kuras, O., Beamish, D., Meldrum, P., Ogilvy, R., and Lala, D.:
Capacitive Resistivity Imaging with Towed Arrays, J. Environ. Eng. Geoph., 12,
267–279, https://doi.org/10.2113/JEEG12.3.267, 2007. a
Loewer, M., Günther, T., Igel, J., Kruschwitz, S., Martin, T., and
Wagner, N.: Ultra-broad-band electrical spectroscopy of soils and
sediments – a combined permittivity and conductivity model, Geophys. J. Int.,
210, 1360–1373, 2017. a
Madsen, L., Fiandaca, G., Auken, E., and Christiansen, A.: Time-domain
induced polarization – an analysis of Cole-Cole parameter resolution and
correlation using Markov Chain Monte Carlo inversion, Geophys. J. Int., 211, 1341–1353, https://doi.org/10.1093/gji/ggx355, 2017. a, b
Maurya, P., Fiandaca, G., Christiansen, A., and Auken, E.: Field-scale
comparison of frequency- and time-domain spectral induced polarization,
Geophys. J. Int., 214, 1441–1466, https://doi.org/10.1093/gji/ggy218, 2018. a, b, c, d
McNeill, J.: Electromagnetic terrain conductivity measurement at low
induction numbers, Technical note TN-6, Geonics Ltd., 1980. a
Militzer, H. and Weber, F.: Angewandte Geophysik, 2,
Geoelektrik-Geothermik-Radiometrie-Aerogeophysik, Springer Wien,
Akademie-Verlag Berlin, 1985. a
Murton, J. B., Kuras, O., Krautblatter, M., Cane, T., Tschofen, D., Uhlemann,
S., Schober, S., and Watson, P.: Monitoring rock frezing and thawing by
novel geoelectrical and acoustic techniques, J. Geophys. Res.-Earth, 121, 2309–2332, https://doi.org/10.1002/2016JF003948, 2016. a, b, c
Olatinsu, O. B., Olorode, D. O., and Oyedele, K. F.: Radio frequency
dielectric properties of limestone and sandstone from Ewekoro, Earstern
Dahomey Basin, Advances in Applied Science Research, 4, 150–158, 2013. a
Olhoeft, G. R.: Electrical properties of natural clay permafrost, Can. J.
Earth Sci., 14, 16–24, https://doi.org/10.1139/e77-002, 1977. a
Palacky, G. J.: Resistivity characteristics of geologic targets, in:
Electromagnetic methods in applied geophysics, 52–129,
https://doi.org/10.1190/1.9781560802631.ch3, 1988. a
Pelton, W., Ward, S., Hallof, P., Sill, W., and Nelson, P.: Mineral
discrimination and removal of inductive coupling with multifrequency IP,
Geophysics, 43, 588–609, https://doi.org/10.1190/1.1440839, 1978. a
Przyklenk, A., Hördt, A., and Radić, T.: Capacitively-Coupled
Resistivity measurements to determine frequency-dependent electrical
parameters in periglacial environments – theoretical considerations and first
field tests, Geophys. J. Int., 206, 1352–1365, https://doi.org/10.1093/gji/ggw178,
2016. a, b, c, d, e, f, g, h, i, j, k, l, m, n
Radić, T.: First Results from the New Multi-purpose Instrument CapGeo,
19th European Meeting of Environmental and Engeneering Geophysics, Near
Surface Geoscience 2013, Extended abstract, https://doi.org/10.3997/2214-4609.20131364, 2013. a
Routh, P., Oldenburg, D., and Li, Y.: Regularized inversion of spectral
IP parameters from complex resistivity data, Expanded Abstracts of the 68th
Annual International Meeting, Society of Exploration Geophysicists, 810–813, 1998. a
Rowan, M.: Structural geometry of the Wildhorn Nappe between the Aar massif
and the Brienzer See, Eclogae Geol. Helv., 86, 87–119, 1993. a
Scherler, M., Hauck, C., Hoelzle, M., Stähli, M., and Völksch, I.:
Meltwater infiltration into the frozen active layer at an alpine permafrost
site, Permafrost Periglac., 21, 325–334, https://doi.org/10.1002/ppp.694, 2010. a, b, c
Seidensticker, K., Möhlmann, D., Apathy, I., Schmidt, W., Thiel, K.,
Arnold, W., Fischer, H., Kretschmer, M., Madlener, D., Peter, A.,
Trautner, R., and Schieke, S.: Sesame – An Experiment of the Rosetta
Lander Philae: Objectives and General Design, Space Sci. Rev., 128, 301–337, https://doi.org/10.1007/s11214-006-9118-6, 2007. a
Seshadri, S., Chin, K., Buehler, M., and Anderson, R.: Using
Electrical Impedance Spectroscopy to Detect Water in Planetary Regoliths,
Astrobiology, 8, 781–792, https://doi.org/10.1089/ast.2007.0180, 2008. a, b, c, d
Souffaché, B., Cosenza, P., Flageul, S., Pencolé, J.-P., Seladji,
S., and Tabbagh, A.: Electrostatic multipole for electrical resistivity
measurements at the decimetric scale, J. Appl. Geophys., 71, 6–12,
https://doi.org/10.1016/j.jappgeo.2010.01.009, 2010. a
Stabbel, B.: Development of the diatom flora in Prestvannet, Tromsø,
northern Norway, Norsk Geol Tidsskr, 65, 179–186, 1985. a
Stillman, D., Grimm, R., and Dec, F.: Low-Frequency Electrical
Properties of Ice-Silicate Mixtures Regoliths, J. Phys. Chem.-US, 114, 6065–6073, https://doi.org/10.1021/jp9070778, 2010. a, b, c
Tabbagh, A., Hesse, A., and Grard, R.: Determination of electrical properties
of the ground at shallow depth with an electrostatic quadrupole: Field trials
on archaelogical sites, Geophys. Prospect, 41, 579–597,
https://doi.org/10.1111/j.1365-2478.1993.tb00872.x, 1993. a
Tarasov, A. and Titov, K.: On the use of the Cole–Cole equations in spectral
induced polarization, Geophys. J. Int., 195, 352–356,
https://doi.org/10.1093/gji/ggt251, 2013. a
Telford, W. M., Geldart, L. P., and Sheriff, R. E.: Applied Geophysics,
Cambridge Univ. Press, 2. edn., textbook gravity seismics
electrical-properties magnetics MT resistivity DC IP tellurics WL, 1990. a
Wang, Z., Wang, S., Fang, G., and Zhang, Q.: Investigation on a Novel
Capacitive Electrode for Geophysical Surveys, J. Sensors, 2016, 9 pp.,
https://doi.org/10.1155/2016/4209850, 2016. a
Weigand, M. and Kemna, A.: Relationship between Cole-Cole model parametes and
spectral decomposition parameters derived from SIP data, Geophys. J. Int., 205,
1414–1419, https://doi.org/10.1093/gji/ggw099, 2016. a, b
Yuval, D. and Oldenburg, W.: Computation of Cole-Cole parametes from IP data,
Geophysics, 62, 436–448, https://doi.org/10.1190/1.1444154, 1997. a
Short summary
The capacitively coupled resistivity (CCR) method enables the determination of frequency-dependent electrical parameters of the subsurface. CCR is well suited for application in cryospheric areas because it provides logistical advantages regarding coupling on hard surfaces and highly resistive grounds. With our new spectral two-dimensional inversion, we can identify subsurface structures based on full spectral information. We show the first results of the inversion method on the field scale.
The capacitively coupled resistivity (CCR) method enables the determination of...
