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Damage to Buildings in Large Slope Rock Instabilities Monitored with the PSInSAR™ Technique
by
Crosta, Giovanni
, Allievi, Jacopo
, Frattini, Paolo
in
buildings
/ damage
/ deep-seated slope deformation
/ Interferometry
/ Landslides
/ PSInSAR™ displacements
/ Remote sensing
/ rock slide
/ Rockslides
2013
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Damage to Buildings in Large Slope Rock Instabilities Monitored with the PSInSAR™ Technique
by
Crosta, Giovanni
, Allievi, Jacopo
, Frattini, Paolo
in
buildings
/ damage
/ deep-seated slope deformation
/ Interferometry
/ Landslides
/ PSInSAR™ displacements
/ Remote sensing
/ rock slide
/ Rockslides
2013
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Do you wish to request the book?
Damage to Buildings in Large Slope Rock Instabilities Monitored with the PSInSAR™ Technique
by
Crosta, Giovanni
, Allievi, Jacopo
, Frattini, Paolo
in
buildings
/ damage
/ deep-seated slope deformation
/ Interferometry
/ Landslides
/ PSInSAR™ displacements
/ Remote sensing
/ rock slide
/ Rockslides
2013
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Damage to Buildings in Large Slope Rock Instabilities Monitored with the PSInSAR™ Technique
Journal Article
Damage to Buildings in Large Slope Rock Instabilities Monitored with the PSInSAR™ Technique
2013
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Overview
The slow movement of active deep-seated slope gravitational deformations (DSGSDs) and deep-seated rockslides can cause damage to structures and infrastructures. We use Permanent Scatterers Synthetic Aperture Radar Interferometry (PSInSAR™) displacement rate data for the analysis of DSGSD/rockslide activity and kinematics and for the analysis of damage to buildings. We surveyed the degree of damage to buildings directly in the field, and we tried to correlate it with the superficial displacement rate obtained by the PSInSAR™ technique at seven sites. Overall, we observe that the degree of damage increases with increasing displacement rate, but this trend shows a large dispersion that can be due to different causes, including: the uncertainty in the attribution of the degree of damage for buildings presenting wall coatings; the complexity of the deformation for large phenomena with different materials and subjected to differential behavior within the displaced mass; the absence of differential superficial movements in buildings, due to the large size of the investigated phenomena; and the different types of buildings and their position along the slope or relative to landslide portions.
Publisher
MDPI AG
Subject
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