Monitoring and failure mechanism interpretation of an unstable slope in Southern Switzerland based on terrestrial laser scanner
Details
Serval ID
serval:BIB_D42A01670A3B
Type
Inproceedings: an article in a conference proceedings.
Collection
Publications
Institution
Title
Monitoring and failure mechanism interpretation of an unstable slope in Southern Switzerland based on terrestrial laser scanner
Title of the conference
Proceedings of the 14th Pan-American Conference on Soil Mechanics and Geotechnical Engineering
Publisher
Canadian Geotechnical Society
Publication state
Published
Issued date
2011
Language
english
Notes
Pedrazzini2011
Abstract
We present the application of terrestrial laser scanning (TLS) for
the monitoring and characterization of an active landslide area in
Val Canaria (Ticino, Southern Swiss Alps). At catchment scale, the
study area is affected by a large Deep Seated Gravitational Slope
Deformation (DSGSD) area presenting, in the lower boundary, several
retrogressive landslides active since the 1990s. Due to its frequent
landslide events this area was periodically monitored by TLS since
2006. Periodic acquisitions provided new information on 3D displacements
at the bottom of slope and the detection of centimetre to decimetre
level scale changes (e.g. rockfall and pre-failure deformations).
In October 2009, a major slope collapse occured at the bottom of
the most unstable area. Based on the comparison between TLS data
before and after the collapse, we carried out a detailed failure
mechanism analysis and volume calculation.
the monitoring and characterization of an active landslide area in
Val Canaria (Ticino, Southern Swiss Alps). At catchment scale, the
study area is affected by a large Deep Seated Gravitational Slope
Deformation (DSGSD) area presenting, in the lower boundary, several
retrogressive landslides active since the 1990s. Due to its frequent
landslide events this area was periodically monitored by TLS since
2006. Periodic acquisitions provided new information on 3D displacements
at the bottom of slope and the detection of centimetre to decimetre
level scale changes (e.g. rockfall and pre-failure deformations).
In October 2009, a major slope collapse occured at the bottom of
the most unstable area. Based on the comparison between TLS data
before and after the collapse, we carried out a detailed failure
mechanism analysis and volume calculation.
Create date
25/11/2013 16:26
Last modification date
20/08/2019 15:54
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