Electrical and Electromagnetic Geophysical Prospecting for the Monitoring of Rock Glaciers in the Dolomites, Northeast Italy

The monitoring of rock glaciers plays a relevant role in relation to natural hazards in high mountain environments. Due to the climate warming, mountain permafrost is thawing, and its degradation is influencing the triggering and the evolvement of processes such as rockfalls, landslides, debris flow...

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Bibliographic Details
Main Authors: Mirko Pavoni, Fabio Sirch, Jacopo Boaga
Format: Article
Language:English
Published: MDPI AG 2021-02-01
Series:Sensors
Subjects:
ERT
EMI
Online Access:https://www.mdpi.com/1424-8220/21/4/1294
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spelling doaj-b150ff11c9a5411cb9eca1289ec064b92021-02-12T00:03:33ZengMDPI AGSensors1424-82202021-02-01211294129410.3390/s21041294Electrical and Electromagnetic Geophysical Prospecting for the Monitoring of Rock Glaciers in the Dolomites, Northeast ItalyMirko Pavoni0Fabio Sirch1Jacopo Boaga2Department of Geosciences, University of Padova, via Gradenigo 6, 35131 Padova, ItalyDepartment of Geosciences, University of Padova, via Gradenigo 6, 35131 Padova, ItalyDepartment of Geosciences, University of Padova, via Gradenigo 6, 35131 Padova, ItalyThe monitoring of rock glaciers plays a relevant role in relation to natural hazards in high mountain environments. Due to the climate warming, mountain permafrost is thawing, and its degradation is influencing the triggering and the evolvement of processes such as rockfalls, landslides, debris flows and floods. Therefore, the study and monitoring of these periglacial forms have both a scientific and economic importance. We tested electrical and electromagnetic measurements along the same investigation lines, in two different sites of the Dolomites area (Northeast Italy). Electrical prospecting exploits the high resistivity contrast between frozen and non-frozen debris. However, these measurements have high logistic demands, considering the complex rock glaciers surface and the need of ground galvanic contact. For this reason, we tried to compare electrical measurements with electromagnetic contactless ones, that theoretically can be used to define the distribution of electrical resistivity in the first subsoil in a quicker and easier way. The obtained results show that the joint use of the two methods allows us to characterize a rock glacier subsoil with good confidence. Finally, the advantages and disadvantages of both the techniques are discussed.https://www.mdpi.com/1424-8220/21/4/1294ERTFDEMEMIfrequency domain electro-magnetometrymountain permafrostrock glacier
collection DOAJ
language English
format Article
sources DOAJ
author Mirko Pavoni
Fabio Sirch
Jacopo Boaga
spellingShingle Mirko Pavoni
Fabio Sirch
Jacopo Boaga
Electrical and Electromagnetic Geophysical Prospecting for the Monitoring of Rock Glaciers in the Dolomites, Northeast Italy
Sensors
ERT
FDEM
EMI
frequency domain electro-magnetometry
mountain permafrost
rock glacier
author_facet Mirko Pavoni
Fabio Sirch
Jacopo Boaga
author_sort Mirko Pavoni
title Electrical and Electromagnetic Geophysical Prospecting for the Monitoring of Rock Glaciers in the Dolomites, Northeast Italy
title_short Electrical and Electromagnetic Geophysical Prospecting for the Monitoring of Rock Glaciers in the Dolomites, Northeast Italy
title_full Electrical and Electromagnetic Geophysical Prospecting for the Monitoring of Rock Glaciers in the Dolomites, Northeast Italy
title_fullStr Electrical and Electromagnetic Geophysical Prospecting for the Monitoring of Rock Glaciers in the Dolomites, Northeast Italy
title_full_unstemmed Electrical and Electromagnetic Geophysical Prospecting for the Monitoring of Rock Glaciers in the Dolomites, Northeast Italy
title_sort electrical and electromagnetic geophysical prospecting for the monitoring of rock glaciers in the dolomites, northeast italy
publisher MDPI AG
series Sensors
issn 1424-8220
publishDate 2021-02-01
description The monitoring of rock glaciers plays a relevant role in relation to natural hazards in high mountain environments. Due to the climate warming, mountain permafrost is thawing, and its degradation is influencing the triggering and the evolvement of processes such as rockfalls, landslides, debris flows and floods. Therefore, the study and monitoring of these periglacial forms have both a scientific and economic importance. We tested electrical and electromagnetic measurements along the same investigation lines, in two different sites of the Dolomites area (Northeast Italy). Electrical prospecting exploits the high resistivity contrast between frozen and non-frozen debris. However, these measurements have high logistic demands, considering the complex rock glaciers surface and the need of ground galvanic contact. For this reason, we tried to compare electrical measurements with electromagnetic contactless ones, that theoretically can be used to define the distribution of electrical resistivity in the first subsoil in a quicker and easier way. The obtained results show that the joint use of the two methods allows us to characterize a rock glacier subsoil with good confidence. Finally, the advantages and disadvantages of both the techniques are discussed.
topic ERT
FDEM
EMI
frequency domain electro-magnetometry
mountain permafrost
rock glacier
url https://www.mdpi.com/1424-8220/21/4/1294
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AT fabiosirch electricalandelectromagneticgeophysicalprospectingforthemonitoringofrockglaciersinthedolomitesnortheastitaly
AT jacopoboaga electricalandelectromagneticgeophysicalprospectingforthemonitoringofrockglaciersinthedolomitesnortheastitaly
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