Monitoring and failure mechanism interpretation of an unstable slope in Southern Switzerland based on terrestrial laser scanner
Détails
ID Serval
serval:BIB_D42A01670A3B
Type
Actes de conférence (partie): contribution originale à la littérature scientifique, publiée à l'occasion de conférences scientifiques, dans un ouvrage de compte-rendu (proceedings), ou dans l'édition spéciale d'un journal reconnu (conference proceedings).
Collection
Publications
Institution
Titre
Monitoring and failure mechanism interpretation of an unstable slope in Southern Switzerland based on terrestrial laser scanner
Titre de la conférence
Proceedings of the 14th Pan-American Conference on Soil Mechanics and Geotechnical Engineering
Editeur
Canadian Geotechnical Society
Statut éditorial
Publié
Date de publication
2011
Langue
anglais
Notes
Pedrazzini2011
Résumé
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.
Création de la notice
25/11/2013 16:26
Dernière modification de la notice
20/08/2019 15:54
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