Airborne geophysical mapping as an innovative methodology for landslide investigation: evaluation of results from the Gschliefgraben landslide, Austria

In September 2009, a complex airborne geophysical survey was performed in the large landslide affected area of the Gschliefgraben valley, Upper Austria, in order to evaluate the applicability of this method for landslide detection and mapping. An evaluation of the results, including different remote...

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Main Authors: R. Supper, I. Baroň, D. Ottowitz, K. Motschka, S. Gruber, E. Winkler, B. Jochum, A. Römer
Format: Article
Language:English
Published: Copernicus Publications 2013-12-01
Series:Natural Hazards and Earth System Sciences
Online Access:http://www.nat-hazards-earth-syst-sci.net/13/3313/2013/nhess-13-3313-2013.pdf
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author R. Supper
I. Baroň
D. Ottowitz
K. Motschka
S. Gruber
E. Winkler
B. Jochum
A. Römer
author_facet R. Supper
I. Baroň
D. Ottowitz
K. Motschka
S. Gruber
E. Winkler
B. Jochum
A. Römer
author_sort R. Supper
collection DOAJ
description In September 2009, a complex airborne geophysical survey was performed in the large landslide affected area of the Gschliefgraben valley, Upper Austria, in order to evaluate the applicability of this method for landslide detection and mapping. An evaluation of the results, including different remote-sensing and ground-based methods, proved that airborne geophysics, especially the airborne electromagnetic method, has a high potential for landslide investigation. This is due to its sensitivity to fluid and clay content and porosity, which are parameters showing characteristic values in landslide prone structures. Resistivity distributions in different depth levels as well as depth slices along selected profiles are presented and compared with ground geoelectrical profiles for the test area of Gschliefgraben. <br><br> Further interesting results can be derived from the radiometric survey, whereas the naturally occurring radioisotopes <sup>40</sup>K and <sup>232</sup>Th, as well as the man-made nuclide <sup>137</sup>Cs have been considered. While the content of potassium and thorium in the shallow subsurface layer is expressively related to the lithological composition, the distribution of caesium is mainly determined by mass wasting processes.
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spelling doaj.art-a62fe0c35cf144ed94f8ba46abb706262022-12-22T03:14:57ZengCopernicus PublicationsNatural Hazards and Earth System Sciences1561-86331684-99812013-12-0113123313332810.5194/nhess-13-3313-2013Airborne geophysical mapping as an innovative methodology for landslide investigation: evaluation of results from the Gschliefgraben landslide, AustriaR. Supper0I. Baroň1D. Ottowitz2K. Motschka3S. Gruber4E. Winkler5B. Jochum6A. Römer7Geologische Bundesanstalt, Neulinggasse 38, 1030 Wien, AustriaGeologische Bundesanstalt, Neulinggasse 38, 1030 Wien, AustriaGeologische Bundesanstalt, Neulinggasse 38, 1030 Wien, AustriaGeologische Bundesanstalt, Neulinggasse 38, 1030 Wien, AustriaGeologische Bundesanstalt, Neulinggasse 38, 1030 Wien, AustriaGeologische Bundesanstalt, Neulinggasse 38, 1030 Wien, AustriaGeologische Bundesanstalt, Neulinggasse 38, 1030 Wien, AustriaGeologische Bundesanstalt, Neulinggasse 38, 1030 Wien, AustriaIn September 2009, a complex airborne geophysical survey was performed in the large landslide affected area of the Gschliefgraben valley, Upper Austria, in order to evaluate the applicability of this method for landslide detection and mapping. An evaluation of the results, including different remote-sensing and ground-based methods, proved that airborne geophysics, especially the airborne electromagnetic method, has a high potential for landslide investigation. This is due to its sensitivity to fluid and clay content and porosity, which are parameters showing characteristic values in landslide prone structures. Resistivity distributions in different depth levels as well as depth slices along selected profiles are presented and compared with ground geoelectrical profiles for the test area of Gschliefgraben. <br><br> Further interesting results can be derived from the radiometric survey, whereas the naturally occurring radioisotopes <sup>40</sup>K and <sup>232</sup>Th, as well as the man-made nuclide <sup>137</sup>Cs have been considered. While the content of potassium and thorium in the shallow subsurface layer is expressively related to the lithological composition, the distribution of caesium is mainly determined by mass wasting processes.http://www.nat-hazards-earth-syst-sci.net/13/3313/2013/nhess-13-3313-2013.pdf
spellingShingle R. Supper
I. Baroň
D. Ottowitz
K. Motschka
S. Gruber
E. Winkler
B. Jochum
A. Römer
Airborne geophysical mapping as an innovative methodology for landslide investigation: evaluation of results from the Gschliefgraben landslide, Austria
Natural Hazards and Earth System Sciences
title Airborne geophysical mapping as an innovative methodology for landslide investigation: evaluation of results from the Gschliefgraben landslide, Austria
title_full Airborne geophysical mapping as an innovative methodology for landslide investigation: evaluation of results from the Gschliefgraben landslide, Austria
title_fullStr Airborne geophysical mapping as an innovative methodology for landslide investigation: evaluation of results from the Gschliefgraben landslide, Austria
title_full_unstemmed Airborne geophysical mapping as an innovative methodology for landslide investigation: evaluation of results from the Gschliefgraben landslide, Austria
title_short Airborne geophysical mapping as an innovative methodology for landslide investigation: evaluation of results from the Gschliefgraben landslide, Austria
title_sort airborne geophysical mapping as an innovative methodology for landslide investigation evaluation of results from the gschliefgraben landslide austria
url http://www.nat-hazards-earth-syst-sci.net/13/3313/2013/nhess-13-3313-2013.pdf
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