Articles | Volume 16, issue 5
https://doi.org/10.5194/tc-16-1903-2022
© Author(s) 2022. 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-16-1903-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
20 May 2022
Research article |
| 20 May 2022
| 20 May 2022
Spectral induced polarization imaging to investigate an ice-rich mountain permafrost site in Switzerland
Theresa Maierhofer
CORRESPONDING AUTHOR
Geophysics Research Division, Department of Geodesy and Geoinformation, TU Wien, Vienna, 1040,
Austria
Department of Geosciences, University of Fribourg, Fribourg, 1700,
Switzerland
Christian Hauck
Department of Geosciences, University of Fribourg, Fribourg, 1700,
Switzerland
Christin Hilbich
Department of Geosciences, University of Fribourg, Fribourg, 1700,
Switzerland
Andreas Kemna
Geophysics Section, Institute of Geosciences, University of Bonn, Bonn, 53121, Germany
Adrián Flores-Orozco
Geophysics Research Division, Department of Geodesy and Geoinformation, TU Wien, Vienna, 1040,
Austria
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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
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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
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Jan Mudler, Andreas Hördt, Anita Przyklenk, Gianluca Fiandaca, Pradip Kumar Maurya, and Christian Hauck
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Matthias Steiner, Florian M. Wagner, and Adrian Flores Orozco
The Cryosphere Discuss., https://doi.org/10.5194/tc-2019-52, https://doi.org/10.5194/tc-2019-52, 2019
Revised manuscript not accepted
Sathyanarayan Rao, Félicien Meunier, Solomon Ehosioke, Nolwenn Lesparre, Andreas Kemna, Frédéric Nguyen, Sarah Garré, and Mathieu Javaux
Biogeosciences Discuss., https://doi.org/10.5194/bg-2018-280, https://doi.org/10.5194/bg-2018-280, 2018
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Klaus Haaken, Gian Piero Deidda, Giorgio Cassiani, Rita Deiana, Mario Putti, Claudio Paniconi, Carlotta Scudeler, and Andreas Kemna
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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
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G. Blöschl, A. P. Blaschke, M. Broer, C. Bucher, G. Carr, X. Chen, A. Eder, M. Exner-Kittridge, A. Farnleitner, A. Flores-Orozco, P. Haas, P. Hogan, A. Kazemi Amiri, M. Oismüller, J. Parajka, R. Silasari, P. Stadler, P. Strauss, M. Vreugdenhil, W. Wagner, and M. Zessner
Hydrol. Earth Syst. Sci., 20, 227–255, https://doi.org/10.5194/hess-20-227-2016, https://doi.org/10.5194/hess-20-227-2016, 2016
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This paper illustrates the experimental and monitoring set-up of the 66 ha Hydrological Open Air Laboratory (HOAL) in Petzenkirchen, Lower Austria, which allows meaningful hypothesis testing. The HOAL catchment features a range of different runoff generation processes (surface runoff, springs, tile drains, wetlands), and is convenient from a logistic point of view as all instruments can be connected to the power grid and a high-speed glassfibre local area network.
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
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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
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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
Related subject area
Discipline: Frozen ground | Subject: Field Studies
Spring-water temperature suggests widespread occurrence of Alpine permafrost in pseudo-relict rock glaciers
Spectral induced polarization imaging to monitor seasonal and annual dynamics of frozen ground at a mountain permafrost site in the Italian Alps
Mapping subsea permafrost around Tuktoyaktuk Island (NWT, Canada) using electrical resistivity tomography
Brief communication: Alternation of thaw zones and deep permafrost in the cold climate conditions of the East Siberian Mountains, Suntar-Khayata Range
Brief communication: Combining borehole temperature, borehole piezometer and cross-borehole electrical resistivity tomography measurements to investigate seasonal changes in ice-rich mountain permafrost
Contrasting geophysical signatures of a relict and an intact Andean rock glacier
First investigation of perennial ice in Winter Wonderland Cave, Uinta Mountains, Utah, USA
Soil respiration of alpine meadow is controlled by freeze–thaw processes of active layer in the permafrost region of the Qinghai–Tibet Plateau
Luca Carturan, Giulia Zuecco, Angela Andreotti, Jacopo Boaga, Costanza Morino, Mirko Pavoni, Roberto Seppi, Monica Tolotti, Thomas Zanoner, and Matteo Zumiani
The Cryosphere, 18, 5713–5733, https://doi.org/10.5194/tc-18-5713-2024, https://doi.org/10.5194/tc-18-5713-2024, 2024
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Pseudo-relict rock glaciers look relict but contain patches of permafrost. They are poorly known in terms of permafrost content, spatial distribution and frequency. Here we use spring-water temperature for a preliminary estimate of the permafrost presence in rock glaciers of a 795 km2 catchment in the Italian Alps. The results show that ~50 % of rock glaciers classified as relict might be pseudo-relict and might contain ~20 % of the ice stored in the rock glaciers in the study area.
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
The Cryosphere, 18, 3383–3414, https://doi.org/10.5194/tc-18-3383-2024, https://doi.org/10.5194/tc-18-3383-2024, 2024
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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 a 3-year 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.
Ephraim Erkens, Michael Angelopoulos, Jens Tronicke, Scott R. Dallimore, Dustin Whalen, Julia Boike, and Pier Paul Overduin
EGUsphere, https://doi.org/10.5194/egusphere-2024-1044, https://doi.org/10.5194/egusphere-2024-1044, 2024
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We investigate the depth of subsea permafrost formed by inundation of terrestrial permafrost due to marine transgression around the rapidly disappearing, permafrost-cored Tuktoyaktuk Island (Beaufort Sea, NWT, Canada). We use geoelectrical surveys with floating electrodes to identify the boundary between unfrozen and frozen sediment. Our findings indicate that permafrost thaw depths beneath the seabed can be explained by coastal erosion rates and landscape features before inundation.
Robert Sysolyatin, Sergei Serikov, Anatoly Kirillin, Andrey Litovko, and Maxim Sivtsev
The Cryosphere, 17, 4601–4608, https://doi.org/10.5194/tc-17-4601-2023, https://doi.org/10.5194/tc-17-4601-2023, 2023
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Permafrost conditions of the East Siberian Mountains are poorly known because of the severe climate, extreme terrain, and farness and scarcity of data. The ground temperature regime plays a key role in mountainous regions, influencing the environment, slope stability, geomorphological processes and hydrological processes. We present the results of recent examinations of the permafrost thickness variations, temperature regime of thaw zones (taliks) and permafrost of the Suntar-Khayata Range.
Marcia Phillips, Chasper Buchli, Samuel Weber, Jacopo Boaga, Mirko Pavoni, and Alexander Bast
The Cryosphere, 17, 753–760, https://doi.org/10.5194/tc-17-753-2023, https://doi.org/10.5194/tc-17-753-2023, 2023
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A new combination of temperature, water pressure and cross-borehole electrical resistivity data is used to investigate ice/water contents in an ice-rich rock glacier. The landform is close to 0°C and has locally heterogeneous characteristics, ice/water contents and temperatures. The techniques presented continuously monitor temporal and spatial phase changes to a depth of 12 m and provide the basis for a better understanding of accelerating rock glacier movements and future water availability.
Giulia de Pasquale, Rémi Valois, Nicole Schaffer, and Shelley MacDonell
The Cryosphere, 16, 1579–1596, https://doi.org/10.5194/tc-16-1579-2022, https://doi.org/10.5194/tc-16-1579-2022, 2022
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We presented a geophysical study of one intact and one relict rock glacier in semi-arid Chile. The interpretation of the collected data through different methods identifies geophysical signature differences between the two rock glaciers and characterizes their subsurface structure and composition. This is of great importance because of rock glaciers' relevant role in freshwater production, transfer and storage, especially in this area of increasing human pressure and high rainfall variability.
Jeffrey S. Munroe
The Cryosphere, 15, 863–881, https://doi.org/10.5194/tc-15-863-2021, https://doi.org/10.5194/tc-15-863-2021, 2021
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This study investigated a cave in Utah (USA) that contains a deposit of perennial ice. Such ice caves are important sources of information about past climate and are currently threatened by rising temperatures. The origin (precipitation), thickness (3 m), and age (several centuries) of the ice were constrained by a variety of methods. Liquid water recently entered the cave for the first time in many years, suggesting a destabilization of the cave environment.
Junfeng Wang, Qingbai Wu, Ziqiang Yuan, and Hojeong Kang
The Cryosphere, 14, 2835–2848, https://doi.org/10.5194/tc-14-2835-2020, https://doi.org/10.5194/tc-14-2835-2020, 2020
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The active layer, a buffer between permafrost and the atmosphere, is more sensitive and responds more quickly to climate change. How the freeze–thaw action at different stages regulates carbon emissions is still unclear. We conducted 2-year continuous in situ measurements in an alpine meadow permafrost ecosystem in the Qinghai–Tibet Plateau and found the freeze–thaw process modified the Rs dynamics differently in different stages. Results suggest great changes in freeze–thaw process patterns.
Cited articles
Abdulsamad, F., Revil, A., Ghorbani, A., Toy, V., Kirilova, M., Coperey, A., Duvillard, P. A., Ménard, G., and Ravanel, L.: Complex conductivity of graphitic schists and sandstones, J. Geophys. Res.-Sol. Ea., 124, 8223–8249, https://doi.org/10.1029/2019JB017628, 2019.
Arenson, L. U. and Jakob, M.: The significance of rock glaciers in the dry
Andes – A discussion of Azócar and Brenning (2010) and Brenning and
Azócar (2010), Permafr. Periglac. Process., 21, 282–285,
https://doi.org/10.1002/ppp.693, 2010.
Auty, R. P. and Cole, R. H.: Dielectric properties of ice and solid D2O, J.
Chem. Phys., 20, 1309–1314, https://doi.org/10.1063/1.1700726, 1952.
Bazin, S., Lysdahl, A., Olaus Harstad, A., and Frauenfelder, R.: Resistivity
and Induced Polarization (ERT/IP) survey for bedrock mapping in Permafrost,
Svalbard, 25th Eur. Meet. Environ. Eng. Geophys. Held Near Surf. Geosci.
Conf. Exhib. 2019, NSG 2019, The Hague, The Netherlands, 8–12 September 2019, 1–5,
https://doi.org/10.3997/2214-4609.201902362, 2019.
Bing, Z. and Greenhalgh, S. A.: Cross-hole resistivity tomography using different electrode configurations, Geophys. Prospect., 48, 887–912, https://doi.org/10.1046/j.1365-2478.2000.00220.x, 2000.
Binley, A. and Kemna, A.: DC Resistivity and Induced Polarization Methods,
in: Hydrogeophysics, Water Science and Technology Library book series, volume 50, edited by: Rubin, Y. and Hubbard, S. S., pp. 129–156, https://doi.org/10.1007/1-4020-3102-5_5,
2005.
Binley, A. and Slater, L.: Resistivity and Induced Polarization: theory and
Applications to the Near-Surface Earth, Cambridge, United Kingdom, New York,
USA, New Delhi, India, ISBN 9781108685955, https://doi.org/10.1017/9781108685955, 2020.
Binley, A., Ramirez, A., and Daily, W.: Regularised Image Reconstruction of
Noisy Electrical Resistance Tomography Data, in: Proceedings of the 4th
Workshop of the European Concerted Action on process Tomography, Bergen, 6–8 April 1995, pp.
401–410, http://www.es.lancs.ac.uk/people/amb/Publications/pdfs/Binley_et_al_1995.pdf (last access: 17 May 2022), 1995.
Binley, A., Slater, L. D., Fukes, M., and Cassiani, G.: Relationship between
spectral induced polarization and hydraulic properties of saturated and
unsaturated sandstone, Water Resour. Res., 41, W12417,
https://doi.org/10.1029/2005WR004202, 2005.
Binley, A., Kruschwitz, S., Lesmes, D., and Kettridge, N.: Exploiting the
temperature effects on low frequency electrical spectra of sandstone: A
comparison of effective diffusion path lengths, Geophysics, 75, 10–13,
https://doi.org/10.1190/1.3483815, 2010.
Binley, A., Hubbard, S. S., Huisman, J. A., Revil, A., Robinson, D. A., Singha, K., and Slater, L. D.: The emergence of hydrogeophysics for improved understanding of subsurface processes over multiple scales, Water Resour. Res., 51, 3837–3866, https://doi.org/10.1002/2015WR017016, 2015.
Biskaborn, B. K., Smith, S. L., Noetzli, J., Matthes, H., Vieira, G., Streletskiy, D. A., Schoeneich, P., Romanovsky, V. E., Lewkowicz, A. G., Abramov, A., Allard, M., Boike, J., Cable, W. L., Christiansen, H. H., Delaloye, R., Diekmann, B., Drozdov, D., Etzelmüller, B., Grosse, G., Guglielmin, M., Ingeman-Nielsen, T., Isaksen, K., Ishikawa, M., Johansson, M., Johannsson, H., Joo, A., Kaverin, D., Kholodov, A., Konstantinov, P., Kröger, T., Lambiel, C., Lanckman, J. P., Luo, D., Malkova, G., Meiklejohn, I., Moskalenko, N., Oliva, M., Phillips, M., Ramos, M., Sannel, A. B. K., Sergeev, D., Seybold, C., Skryabin, P., Vasiliev, A., Wu, Q., Yoshikawa, K., Zheleznyak, M., and Lantuit, H.: Permafrost is warming at a global scale, Nat. Commun., 10, 264, https://doi.org/10.1038/s41467-018-08240-4, 2019.
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.
Bücker, M., Flores Orozco, A., Undorf, S., and Kemna, A.: On the Role of
Stern- and Diffuse-Layer Polarization Mechanisms in Porous Media, J.
Geophys. Res.-Sol. Ea., 124, 5656–5677, https://doi.org/10.1029/2019JB017679,
2019.
Coperey, A., Revil, A., Abdulsamad, F., Stutz, B., Duvillard, P. A., and
Ravanel, L.: Low-Frequency Induced Polarization of Porous Media Undergoing
Freezing: Preliminary Observations and Modeling, J. Geophys. Res.-Sol.
Ea., 124, 4523–4544, https://doi.org/10.1029/2018JB017015, 2019.
Dahlin, T., Leroux, V., and Nissen, J.: Measuring techniques in induced
polarisation imaging, J. Appl. Geophys., 50, 279–298,
https://doi.org/10.1016/S0926-9851(02)00148-9, 2002.
Dash, J. G., Rempel, A. W., and Wettlaufer, J. S.: The physics of premelted
ice and its geophysical consequences, Rev. Mod. Phys., 78, 695–741,
https://doi.org/10.1103/RevModPhys.78.695, 2006.
Delaloye, R.: Contribution à l'étude du pergélisol de montagne en zone marginale, PhD Thesis, Department of Geosciences–Geography, University of Fribourg, https://folia.unifr.ch/unifr/documents/299916 (last access: 17 May 2022), 2004.
Delaloye, R. and Lambiel, C.: Evidence of winter ascending air circulation
throughout talus slopes and rock glaciers situated in the lower belt of
alpine discontinuous permafrost (Swiss Alps), Nor. Geogr. Tidsskr., 59,
194–203, https://doi.org/10.1080/00291950510020673, 2005.
Delaloye, R., Reynard, E., and Lambiel, C.: Pergélisol et construction
de remontées mécaniques: l'exemple des Lapires (Mont-Gelé,
Valais), Le gel en géotechnique, Publications de la Société
Suisse de Mécanique des Sols et des Roches, 141, 103–113, 2001.
Doetsch, J., Ingeman-Nielsen, T., Christiansen, A. V., Fiandaca, G., Auken,
E., and Elberling, B.: Direct current (DC) resistivity and induced
polarization (IP) monitoring of active layer dynamics at high temporal
resolution, Cold Reg. Sci. Technol., 119, 16–28,
https://doi.org/10.1016/j.coldregions.2015.07.002, 2015.
Dukhin, S. S., Shilov, V. N., and Bikerman, J. J.: Dielectric Phenomena and
Double Layer in Disperse Systems and Polyelectrolytes, J. Electrochem. Soc.,
121, 154C, https://doi.org/10.1149/1.2402374, 1974.
Duvillard, P., Magnin, F., Revil, A., Legay, A., Ravanel, L., Abdulsamad, F.,
and Coperey, A.: Temperature distribution in a permafrost-affected rock
ridge from conductivity and induced polarization tomography, Geophys. J.
Int., 225, 1207–1221, https://doi.org/10.1093/gji/ggaa597, 2021.
Duvillard, P. A., 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.
Flores Orozco, A., Williams, K. H., Long, P. E., Hubbard, S. S., and Kemna,
A.: Using complex resistivity imaging to infer biogeochemical processes
associated with bioremediation of an uranium-contaminated aquifer, J.
Geophys. Res.-Biogeo., 116, G03001, https://doi.org/10.1029/2010JG001591, 2011.
Flores Orozco, A., Kemna, A., and Zimmermann, E.: Data error quantification
in spectral induced polarization imaging, Geophysics, 77,
E227–E237, https://doi.org/10.1190/geo2010-0194.1, 2012.
Flores Orozco, A., Williams, K. H., and Kemna, A.: Time-lapse spectral
induced polarization imaging of stimulated uranium bioremediation, Near
Surf. Geophys., 11, 531–544, https://doi.org/10.3997/1873-0604.2013020, 2013.
Flores Orozco, A., Bücker, M., Steiner, M., and Malet, J.-P.:
Complex-conductivity imaging for the understanding of landslide
architecture, Eng. Geol., 243, 241–252,
https://doi.org/10.1016/j.enggeo.2018.07.009, 2018.
Flores Orozco, A., Kemna, A., Binley, A., and Cassiani, G.: Analysis of
time-lapse data error in complex conductivity imaging to alleviate
anthropogenic noise for site characterization, Geophysics, 84,
B181–B193, https://doi.org/10.1190/GEO2017-0755.1, 2019.
Flores Orozco, A., Aigner, L., and Gallistl, J.: Investigation of cable
effects in spectral induced polarization imaging at the field scale using
multicore and coaxial cables, Geophysics, 86, E59–E75,
https://doi.org/10.1190/geo2019-0552.1, 2021.
Grimm, R. E. and Stillman, D. E.: Field test of detection and
characterisation of subsurface ice using broadband spectral-induced
polarisation, Permafr. Periglac. Process., 26, 28–38,
https://doi.org/10.1002/ppp.1833, 2015.
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.
Haeberli, W., Huder, J., Keusen, H.-R., Pika, J., and Röthlisberger, H.:
Core drilling through rock glacier-permafrost, in: Proceedings of the Fifth
International Conference on Permafrost, 2–5th August 1988, Trondheim, Norway, pp. 937–942, https://www.researchgate.net/profile/Wilfried-Haeberli/publication/245800726_Core_drilling_through_rock_glacier_permafrost/links/5a535051458515e7b72ea12c/Core-drilling-through-rock-glacier-permafrost.pdf (last access: 17 May 2022), 1988.
Halla, C., Blöthe, J. H., Tapia Baldis, C., Trombotto Liaudat, D., Hilbich, C., Hauck, C., and Schrott, L.: Ice content and interannual water storage changes of an active rock glacier in the dry Andes of Argentina, The Cryosphere, 15, 1187–1213, https://doi.org/10.5194/tc-15-1187-2021, 2021.
Harrington, J. S., Mozil, A., Hayashi, M., and Bentley, L. R.: Groundwater
flow and storage processes in an inactive rock glacier, Hydrol. Process.,
32, 3070–3088, https://doi.org/10.1002/hyp.13248, 2018.
Harris, S., French, H., Heginbottom, J. A., Johnston, G. H., Ladanyi, B.,
Sego, D., and Van Everdingen, R. O.: Glossary of Permafrost and Related
Ground-Ice Terms, National Research Council of Canada, Technical Report, 159
pp., https://doi.org/10.4224/20386561, 1988.
Hauck, C.: Frozen ground monitoring using DC resistivity tomography,
Geophys. Res. Lett., 29, 10–13, https://doi.org/10.1029/2002GL014995, 2002.
Hauck, C.: New Concepts in Geophysical Surveying and Data Interpretation for
Permafrost Terrain, Permafr. Periglac. Process., 137, 131–137,
https://doi.org/10.1002/ppp.1774, 2013.
Hauck, C. and Kneisel, C.: Applied geophysics in periglacial
environments, Cambridge University Press, 256 pp., ISBN 9780511535628, https://doi.org/10.1017/CBO9780511535628, 2008.
Hauck, C., Böttcher, M., and Maurer, H.: A new model for estimating subsurface ice content based on combined electrical and seismic data sets, The Cryosphere, 5, 453–468, https://doi.org/10.5194/tc-5-453-2011, 2011.
Hausmann, H., Krainer, K., Brückl, E., and Mostler, W.: Internal structure and ice content of Reichenkar rock glacier (Stubai Alps, Austria) assessed by geophysical investigations, Permafr. Periglac. Process.,
18, 351–367, https://doi.org/10.1002/ppp.601, 2007.
Hilbich, C.: Time-lapse refraction seismic tomography for the detection of ground ice degradation, The Cryosphere, 4, 243–259, https://doi.org/10.5194/tc-4-243-2010, 2010.
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.-Earth, 113, F01S90, https://doi.org/10.1029/2007JF000799, 2008.
Hilbich, C., Marescot, L., Hauck, C., Loke, M. H., and Mäusbacher, R.:
Applicability of Electrical Resistivity Tomography Monitoring to Coarse
Blocky and Ice-rich Permafrost Landforms, Permafr. Periglac. Process., 20,
269–284, https://doi.org/10.1002/ppp.652, 2009.
Hobbs, P. V.: Ice Physics, Clarendon, Oxford, 837 pp., ISBN 978-0-19-958771-1,
1974.
Hördt, A., Bücker, M., Bairlein, K., Bielefeld, A., Kuhn, E.,
Nordsiek, S., and Stebner, H.: The dependence of induced polarization on
fluid salinity and pH, studied with an extended model of membrane
polarization, J. Appl. Geophys., 135, 408–417,
https://doi.org/10.1016/j.jappgeo.2016.02.007, 2016.
Huisman, J. A., Zimmermann, E., Esser, O., Haegel, F.-H., Treichel, A., and
Vereecken, H.: Evaluation of a novel correction procedure to remove
electrode impedance effects from broadband SIP measurements, J. Appl.
Geophys., 135, 466–473, https://doi.org/10.1016/j.jappgeo.2015.11.008, 2016.
Kemna, A.: Tomographic inversion of complex resistivity: Theory and
application, PhD thesis, Ruhr-University of Bochum, ISBN 3-934366-92-9, 2000.
Kemna, A., Binley, A., Cassiani, G., Niederleithinger, E., Revil, A.,
Slater, L., Williams, K. H., Orozco, A. F., 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, https://doi.org/10.3997/1873-0604.2012027, 2012.
Kemna, A., Weigand, M., and Zimmermann, E.: Resistivity and SIP response of
rocks during freezing and thawing, in: Proceedings of the 3rd International Workshop on Induced Polarization, Ile d’Oléron, France, 6–9 April 2014, https://ip.geosciences.mines-paristech.fr/s1_kemna (last access: 17 May 2022), 2014a.
Kemna, A., Huisman, J. A., Zimmermann, E., Martin, R., Zhao, Y., Treichel,
A., Flores-Orozco, A., and Fechner, T.: Broadband Electrical Impedance
Tomography for Subsurface Characterization Using Improved Corrections of
Electromagnetic Coupling and Spectral Regularization, in: Tomography of the Earth’s Crust: From
Geophysical Sounding to Real-Time Monitoring, Springer, pp. 1–20
https://doi.org/10.1007/978-3-319-04205-3_1,
2014b.
Kenner, R., Noetzli, J., Hoelzle, M., Raetzo, H., and Phillips, M.: Distinguishing ice-rich and ice-poor permafrost to map ground temperatures and ground ice occurrence in the Swiss Alps, The Cryosphere, 13, 1925–1941, https://doi.org/10.5194/tc-13-1925-2019, 2019.
Keuschnig, M., Krautblatter, M., Hartmeyer, I., Fuss, C., and Schrott, L.:
Automated Electrical Resistivity Tomography Testing for Early Warning in
Unstable Permafrost Rock Walls Around Alpine Infrastructure, Permafr.
Periglac. Process., 28, 158–171, https://doi.org/10.1002/ppp.1916, 2017.
Krainer, K., Bressan, D., Dietre, B., Haas, J. N., Hajdas, I., Lang, K.,
Mair, V., Nickus, U., Reidl, D., Thies, H., and Tonidandel, D.: A
10,300-year-old permafrost core from the active rock glacier Lazaun,
southern Ötztal Alps (South Tyrol, northern Italy), Quaternary Res., 83,
324–335, https://doi.org/10.1016/j.yqres.2014.12.005, 2014.
Krautblatter, M., Verleysdonk, S., Flores Orozco, A., and Kemna, A.:
Temperature – calibrated imaging of seasonal changes in permafrost rock
walls by quantitative electrical resistivity tomography (Zugspitze, German/Austrian Alps), J. Geophys. Res., 115, F02003,
https://doi.org/10.1029/2008JF001209, 2010.
LaBrecque, D. J. and Ward, S. H.: Two-Dimensional Cross-Borehole Resistivity
Model Fitting, Geotech. Environ. Geophys., 3, 51–74, 1990.
LaBrecque, D. J., Miletto, M., Daily, W., Ramirez, A., and Owen, E.: The
effects of noise on Occam's inversion of resistivity tomography data,
Geophysics, 61, 538–548, https://doi.org/10.1190/1.1443980, 1996.
Lambiel, C.: Le pergélisol dans les terrains sédimentaires à
forte déclivité: distribution, régime thermique et
instabilités, Travaux et recherches, Vol. 33, Institut de Géographie, University of Lausanne, 260 pp., https://www.researchgate.net/profile/Christophe-Lambiel/publication/33683076
(last access: 17 May 2022), 2006.
Langston, G., Bentley, L. R., Hayashi, M., Mcclymont, A., and Pidlisecky, A.:
Internal structure and hydrological functions of an alpine proglacial
moraine, Hydrol. Process., 25, 2967–2982, https://doi.org/10.1002/hyp.8144, 2011.
Leroy, P., Revil, A., Kemna, A., Cosenza, P., and Ghorbani, A.: Complex
conductivity of water-saturated packs of glass beads, J. Colloid Interface
Sci., 321, 103–117, https://doi.org/10.1016/j.jcis.2007.12.031, 2008.
Lesparre, N., Nguyen, F., Kemna, A., Robert, T., Hermans, T., Daoudi, M., and
Flores Orozco, A.: A new approach for time-lapse data weighting in
electrical resistivity tomography, Geophysics, 82, E325–E333,
https://doi.org/10.1190/GEO2017-0024.1, 2017.
Limbrock, J. K., Weigand, M., and Kemna, A.: Textural and mineralogical
controls on temperature dependent SIP behavior during freezing and thawing,
EGU General Assembly 2021, online, 19–30 Apr 2021, EGU21-14273,
https://doi.org/10.5194/egusphere-egu21-14273, 2021.
Loke, M. and Barker, R.: Rapid least-squares inversion of apparent resistivity pseudosections by a quasi-Newton method, Geophys. Prospect., 44, 131–152, https://doi.org/10.1111/j.1365-2478.1996.tb00142.x, 1996 (code available at: https://www.aarhusgeosoftware.dk/download-resxdinv, last access: 18 May 2022).
Maierhofer, T., Hauck, C., Hilbich, C., and Flores-Orozco, A.: Spectral Induced Polarization Applied at Different Mountain Permafrost Sites in the European Alps, NSG2021 1st Conference on Hydrogeophysics, European Association of Geoscientists & Engineers, Bordeaux, France, 29 August–2 September 2021, vol. 2021, pp. 1–5, https://doi.org/10.3997/2214-4609.202120172, 2021.
Marmy, A., Rajczak, J., Delaloye, R., Hilbich, C., Hoelzle, M., Kotlarski, S., Lambiel, C., Noetzli, J., Phillips, M., Salzmann, N., Staub, B., and Hauck, C.: Semi-automated calibration method for modelling of mountain permafrost evolution in Switzerland, The Cryosphere, 10, 2693–2719, https://doi.org/10.5194/tc-10-2693-2016, 2016.
Marshall, D. J. and Madden, T. R.: Induced Polarization, a study of its
causes, Geophysics, 24, 790–816, https://doi.org/10.1190/1.1438659, 1959.
Martin, T., Günther, T., Flores Orozco, A., and Dahlin, T.: Evaluation of
spectral induced polarization fi eld measurements in time and frequency
domain, J. Appl. Geophys., 180, 104141, https://doi.org/10.1016/j.jappgeo.2020.104141,
2020.
McKenzie, J. M., Voss, C. I., and Siegel, D. I.: Groundwater flow with energy
transport and water-ice phase change: Numerical simulations, benchmarks, and
application to freezing in peat bogs, Adv. Water Resour., 30, 966–983,
https://doi.org/10.1016/j.advwatres.2006.08.008, 2007.
Menke, W.: Geophysical data analysis: Discrete inverse theory, 4th edn., Academic Press, Inc., Orlando, 260 pp., ISBN 978-0-12-813555-6, 1984.
Mollaret, C., Hilbich, C., Pellet, C., Flores-Orozco, A., Delaloye, R., and Hauck, C.: Mountain permafrost degradation documented through a network of permanent electrical resistivity tomography sites, The Cryosphere, 13, 2557–2578, https://doi.org/10.5194/tc-13-2557-2019, 2019.
Mollaret, C., Wagner, F. M., Hilbich, C., Scapozza, C., and Hauck, C.:
Petrophysical Joint Inversion Applied to Alpine Permafrost Field Sites to
Image Subsurface Ice, Water, Air, and Rock Contents, Front. Earth Sci.,
8, 1–25, https://doi.org/10.3389/feart.2020.00085, 2020.
Morelli, G. and LaBrecque, D. J.: Robust scheme for ERT inverse modelling, 9th EEGS Symposium on the Application of Geophysics to Engineering and Environmental Problems Conference, Keystone, Colorado, USA, 28 April–2 May 1996, SEG, 629–638, https://doi.org/10.4133/1.2922327, 1996.
Mudler, J., Hördt, A., Przyklenk, A., Fiandaca, G., Maurya, P. K., and Hauck, C.: Two-dimensional inversion of wideband spectral data from the capacitively coupled resistivity method – first applications in periglacial environments, The Cryosphere, 13, 2439–2456, https://doi.org/10.5194/tc-13-2439-2019, 2019.
Oldenborger, G. A. and LeBlanc, A. M.: Monitoring changes in unfrozen water
content with electrical resistivity surveys in cold continuous permafrost,
Geophys. J. Int., 215, 965–977, https://doi.org/10.1093/GJI/GGY321, 2018.
Oldenburg, D. W. and Li, Y.: Inversion of induced polarization data, Geophysics, 59, 1327–1341, https://doi.org/10.1190/1.1443692, 1994.
Olhoeft, G. R.: Electrical properties of natural clay permafrost, Can. J.
Earth Sci., 14, 16–24, 1977.
Parkhomenko, E. I.: Electrical Resistivity of Minerals and Rocks at High
Temperature and Pressure, Rev. Geophys. Sp. Phys., 20, 193–218, 1982.
Pelton, W., Ward, S., Hallof, P., Sill, W., and Nelson, P.: Mineral
discrimination and removal of inductive coupling with multifrequency IP,
Geophysics, 43, 497–638, https://doi.org/10.1190/1.1440839, 1978.
PERMOS: PERMOS Database, Swiss Permafrost Monitoring Network, Fribourg
and Davos, Switzerland [data set], https://doi.org/10.13093/permos-2019-01, 2019.
PERMOS: PERMOS Database, Swiss Permafrost Monitoring Network, Fribourg
and Davos, Switzerland [data set], http://www.permos.ch/doi/permos-2021-01.html (last access: 17 May 2022), 2021.
Rangecroft, S., Suggitt, A. J., Anderson, K., and Harrison, S.: Future
climate warming and changes to mountain permafrost in the Bolivian Andes,
Climatic Change, 137, 231–243, https://doi.org/10.1007/s10584-016-1655-8, 2016.
Revil, A.: Spectral induced polarization of shaly sands: Influence of the
electrical double layer, Water Resour. Res., 48, W02517,
https://doi.org/10.1029/2011WR011260, 2012.
Revil, A.: Effective conductivity and permittivity of unsaturated porous
materials in the frequency range 1 mHz–1 GHz, Water Resour. Res., 49, 306–327, https://doi.org/10.1029/2012WR012700, 2013a.
Revil, A.: On charge accumulation in heterogeneous porous rocks under the
influence of an external electric field, Geophysics, 78, 1JA-Z103,
https://doi.org/10.1190/geo2012-0503.1, 2013b.
Revil, A. and Florsch, N.: Determination of permeability from spectral
induced polarization in granular media, Geophys. J. Int., 181,
1480–1498, https://doi.org/10.1111/j.1365-246X.2010.04573.x, 2010.
Revil, A. and Glover, P. W. J.: Nature of surface electrical conductivity in
natural sands, sandstones, and clays, Geophys. Res. Lett., 25, 691–694,
1998.
Revil, A. and Skold, M.: Salinity dependence of spectral induced
polarization in sands and sandstones, Geophys. J. Int., 187, 813–824,
https://doi.org/10.1111/j.1365-246X.2011.05181.x, 2011.
Revil, A., Koch, K., and Holliger, K.: Is it the grain size or the
characteristic pore size that controls the induced polarization relaxation
time of clean sands and sandstones?, Water Resour. Res., 48, W05602,
https://doi.org/10.1029/2011WR011561, 2012.
Revil, A., Razdan, M., Julien, S., Coperey, A., Abdulsamad, F., Ghorbani,
A., Gasquet, D., Sharma, R., and Rossi, M.: Induced polarization response of
porous media with metallic particles – Part 9: Influence of permafrost,
Geophysics, 84, E337–E355, https://doi.org/10.1190/geo2019-0013.1, 2019.
Scapozza, C.: Stratigraphie, morphodynamique, paléoenviron-nements des
terrains sédimentaires meubles à forte déclivité dudomaine
périglaciaire alpin (Géovisions no. 40), PhD Thesis, University of
Lausanne, 580 pp., ISBN 978-2-940368-16-7,
http://www.unil.ch/igul/page96426.html (last access: 17 May 2022), 2013.
Scapozza, C., Baron, L., and Lambiel, C.: Borehole logging in alpine
periglacial talus slopes (Valais, Swiss Alps), Permafr. Periglac. Process.,
26, 67–83, https://doi.org/10.1002/ppp.1832, 2015.
Scapozza, C., Lambiel, C., Abbet, D., Delaloye, R., and Hilbich, C.: Internal
structure and permafrost characteristics of the Lapires talus slope (Nendaz,
Valais), 8th Swiss Geoscience Meeting 2010, Fribourg, Switzerland,
19–20 November 2010, Extended Abstract 7.16, 166–167, https://www.researchgate.net/publication/313192421_Internal_structure_and_permafrost_characteristics_of_the_Lapires_talus_slope_Nendaz_Valais_8th_Swiss_Geoscience_Meeting_2010_Fribourg_Switzerland_19-20_November_2010 (last access: 17 May 2022), 2010.
Schneider, S., Hoelzle, M., and Hauck, C.: Influence of surface and subsurface heterogeneity on observed borehole temperatures at a mountain permafrost site in the Upper Engadine, Swiss Alps, The Cryosphere, 6, 517–531, https://doi.org/10.5194/tc-6-517-2012, 2012.
Schrott, L.: The hydrological significance of high mountain permafrost and
its relation to solar radiation. A case study in the high andes of San Juan,
Argentina, Bamberger Geogr. Schriften, Bd. 15, 71–84, https://www.researchgate.net/profile/Lothar-Schrott/publication/284339606 (last access: 17 May 2022), 1998.
Schwarz, G.: A theory of the low-frequency dielectric dispersion of
colloidal particles in electrolyte solution, J. Phys. Chem., 66,
2636–2642, https://doi.org/10.1021/j100818a067, 1962.
Scott, W. J., Sellmann, P. V., and Hunter, J. A.: 13. Geophysics in
the study of permafrost, in: Geotechnical and Environmental Geophysics, edited by:
Ward, S. H., Society of Exploration Geophysicists, Tulsa, OK, 355–384, https://doi.org/10.1190/1.9781560802785.ch13, 1990.
Slater, L. and Binley, A.: Synthetic and field-based electrical imaging of a
zerovalent iron barrier: Implications for monitoring long-term barrier
performance, Geophysics, 71, B129–B137, https://doi.org/10.1190/1.2235931, 2006.
Slater, L., Binley, A. M., Daily, W., and Johnson, R.: Cross-hole electrical
imaging of a controlled saline tracer injection, J. Appl. Geophys., 44,
85–102, 2000.
Son, J.-S., Kim, J.-H., and Yi, M.: A new algorithm for SIP parameter
estimation from multi-frequency IP data: preliminary results A new
algorithm for SIP parameter estimation from multi-frequency IP data:
preliminary results, Explor. Geophys., 38, 60–68, https://doi.org/10.1071/EG07009,
2007.
Staub, B., Marmy, A., Hauck, C., Hilbich, C., and Delaloye, R.: The evolution
of mountain permafrost in the context of climate change: towards a
comprehensive analysis of permafrost monitoring data from the Swiss Alps,
University of Fribourg, https://doc.rero.ch/record/261348/files/StaubB.pdf (last access: 17 May 2022), 2015.
Steiner, M., Wagner, F. M., Maierhofer, T., Schöner, W., and Flores Orozco, A.: Improved estimation of ice and water contents in alpine
permafrost through constrained petrophysical joint inversion: The Hoher
Sonnblick case study, Geophysics, 86, WB119–WB133,
https://doi.org/10.1190/geo2020-0592.1, 2021.
Stillman, D. E., Grimm, R. E., and Dec, S. F.: Low-Frequency Electrical
Properties of Ice – Silicate Mixtures, J. Phys. Chem., 114, 6065–6073,
https://doi.org/10.1021/jp9070778, 2010.
Stummer, P., Maurer, H., and Green, A. G.: Experimental design: Electrical resistivity data sets that provide optimum subsurface information, Geophysics, 69, 120–139, https://doi.org/10.1190/1.1649381, 2004.
Sumner, J. S.: Principles of Induced Polarisation for geophysical
exploration, in: Developments in Economic Geology, 5, Elsevier, Amsterdam, ISBN 0-444-41 481-9, 1976.
Supper, R., Ottowitz, D., Jochum, B., Kim, J.-H., Römer, A., Baron, I.,
Pfeiler, S., Lovisolo, M., Gruber, S., and Vecchiotti, F.: Geoelectrical
monitoring: an innovative method to supplement landslide surveillance and
early warning, Near Surf. Geophys., 12, 133–150,
https://doi.org/10.3997/1873-0604.2013060, 2014.
Vinegar, H. J. and Waxman, M. H.: Induced polarization of shaly sands – the
effect of clay counterion type, Geophysics,49, 1267, https://doi.org/10.1190/1.1441755, 1984.
Vonder Mühll, D. S. and Holub, P.: Borehole logging in alpine
permafrost, upper Engadin, Swiss Alps, Permafrost and Periglac., 3, 125–132, 1992.
Wagner, F. M., Mollaret, C., Kemna, A., and Hauck, C.: Quantitative imaging
of water, ice and air in permafrost systems through petrophysical joint
inversion of seismic refraction and electrical resistivity data, Geophys. J.
Int., 219, 1866–1875, https://doi.org/10.1093/gji/ggz402, 2019.
Wait, J. R.: Relaxation phenomena and induced polarization, Geoexploration,
22, 107–127, 1984.
Wang, S., Sheng, Y., Li, J., Wu, J., Cao, W., and Ma, S.: An Estimation of Ground Ice Volumes in Permafrost Layers in Northeastern Qinghai-Tibet Plateau, China, Chinese Geogr. Sci., 28, 61–73, https://doi.org/10.1007/s11769-018-0932-z, 2018.
Ward, S.: The Resistivity And Induced Polarization Methods, in: Conference Proceedings, 1st EEGS Symposium on the Application of Geophysics to Engineering and Environmental Problems Conference, Golden, Colorado, USA, 28–31 March 1988, cp-214-00002, European Association of Geoscientists & Engineers, https://doi.org/10.3997/2214-4609-pdb.214.1988_002, 1990.
Waxman, M. H. and Smits, L. J. M.: Electrical conductivities in oil-bearing
shaly sands, Soc. Pet. Eng. J., 243, 107–122, 1968.
Weigand, M., Flores Orozco, A., and Kemna, A.: Reconstruction quality of SIP
parameters in multi-frequency complex resistivity imaging, Near Surf.
Geophys., 15, 187–199, https://doi.org/10.3997/1873-0604.2016050, 2017.
Weller, A., Slater, L., and Nordsiek, S.: On the relationship between induced
polarization and surface conductivity: Implications for petrophysical
interpretation of electrical measurements, Geophysics, 78, D315–D325,
https://doi.org/10.1190/GEO2013-0076.1, 2013.
Wicky, J. and Hauck, C.: Numerical modelling of convective heat transport by air flow in permafrost talus slopes, The Cryosphere, 11, 1311–1325, https://doi.org/10.5194/tc-11-1311-2017, 2017.
Wicky, J. and Hauck, C.: Air Convection in the Active Layer of Rock
Glaciers, Front. Earth Sci., 8, 335, https://doi.org/10.3389/feart.2020.00335,
2020.
Wu, Y., Nakagawa, S., Kneafsey, T. J., Dafflon, B., and Hubbard, S.:
Electrical and seismic response of saline permafrost soil during freeze –
Thaw transition, J. Appl. Geophys., 146, 16–26,
https://doi.org/10.1016/j.jappgeo.2017.08.008, 2017.
Zhao, Y., Zimmermann, E., Huisman, J. A., Treichel, A., Wolters, B., Van
Waasen, S., and Kemna, A.: Broadband EIT borehole measurements with high
phase accuracy using numerical corrections of electromagnetic coupling
effects, Meas. Sci. Technol., 24, 085005, https://doi.org/10.1088/0957-0233/24/8/085005,
2013.
Zimmermann, E., Kemna, A., Berwix, J., Glaas, W., and Vereecken, H.: EIT
measurement system with high phase accuracy for the imaging of spectral
induced polarization properties of soils and sediments, Meas. Sci. Technol.,
19, 094010, https://doi.org/10.1088/0957-0233/19/9/094010, 2008.
Zimmermann, E., Huisman, J. A., Mester, A., and Van Waasen, S.: Correction of
phase errors due to leakage currents in wideband EIT field measurements on
soil and sediments, Meas. Sci. Technol., 30, 084002,
https://doi.org/10.1088/1361-6501/ab1b09, 2019.
Zisser, N., Kemna, A., and Nover, G.: Dependence of spectral – induced
polarization response of sandstone on temperature and its relevance to
permeability estimation, J. Geophys. Res., 115, B09214,
https://doi.org/10.1029/2010JB007526, 2010.
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.
We extend the application of electrical methods to characterize alpine permafrost using the...
