Cargando…

Remote thermal detection of exfoliation sheet deformation

A growing body of research indicates that rock slope failures, particularly from exfoliating cliffs, are promoted by rock deformations induced by daily temperature cycles. Although previous research has described how these deformations occur, full three-dimensional monitoring of both the deformation...

Descripción completa

Detalles Bibliográficos
Autores principales: Guerin, Antoine, Jaboyedoff, Michel, Collins, Brian D., Stock, Greg M., Derron, Marc-Henri, Abellán, Antonio, Matasci, Battista
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Springer Berlin Heidelberg 2020
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7936945/
https://www.ncbi.nlm.nih.gov/pubmed/33746675
http://dx.doi.org/10.1007/s10346-020-01524-1
_version_ 1783661293408878592
author Guerin, Antoine
Jaboyedoff, Michel
Collins, Brian D.
Stock, Greg M.
Derron, Marc-Henri
Abellán, Antonio
Matasci, Battista
author_facet Guerin, Antoine
Jaboyedoff, Michel
Collins, Brian D.
Stock, Greg M.
Derron, Marc-Henri
Abellán, Antonio
Matasci, Battista
author_sort Guerin, Antoine
collection PubMed
description A growing body of research indicates that rock slope failures, particularly from exfoliating cliffs, are promoted by rock deformations induced by daily temperature cycles. Although previous research has described how these deformations occur, full three-dimensional monitoring of both the deformations and the associated temperature changes has not yet been performed. Here we use integrated terrestrial laser scanning (TLS) and infrared thermography (IRT) techniques to monitor daily deformations of two granitic exfoliating cliffs in Yosemite National Park (CA, USA). At one cliff, we employed TLS and IRT in conjunction with in situ instrumentation to confirm previously documented behavior of an exfoliated rock sheet, which experiences daily closing and opening of the exfoliation fracture during rock cooling and heating, respectively, with a few hours delay from the minimum and maximum temperatures. The most deformed portion of the sheet coincides with the area where both the fracture aperture and the temperature variations are greatest. With the general deformation and temperature relations established, we then employed IRT at a second cliff, where we remotely detected and identified 11 exfoliation sheets that displayed those general thermal relations. TLS measurements then subsequently confirmed the deformation patterns of these sheets showing that sheets with larger apertures are more likely to display larger thermal-related deformations. Our high-frequency monitoring shows how coupled TLS and IRT allows for remote detection of thermally induced deformations and, importantly, how IRT could potentially be used on its own to identify partially detached exfoliation sheets capable of large-scale deformation. These results offer a new and efficient approach for investigating potential rockfall sources on exfoliating cliffs. ELECTRONIC SUPPLEMENTARY MATERIAL: The online version of this article (10.1007/s10346-020-01524-1) contains supplementary material, which is available to authorized users.
format Online
Article
Text
id pubmed-7936945
institution National Center for Biotechnology Information
language English
publishDate 2020
publisher Springer Berlin Heidelberg
record_format MEDLINE/PubMed
spelling pubmed-79369452021-03-19 Remote thermal detection of exfoliation sheet deformation Guerin, Antoine Jaboyedoff, Michel Collins, Brian D. Stock, Greg M. Derron, Marc-Henri Abellán, Antonio Matasci, Battista Landslides Original Paper A growing body of research indicates that rock slope failures, particularly from exfoliating cliffs, are promoted by rock deformations induced by daily temperature cycles. Although previous research has described how these deformations occur, full three-dimensional monitoring of both the deformations and the associated temperature changes has not yet been performed. Here we use integrated terrestrial laser scanning (TLS) and infrared thermography (IRT) techniques to monitor daily deformations of two granitic exfoliating cliffs in Yosemite National Park (CA, USA). At one cliff, we employed TLS and IRT in conjunction with in situ instrumentation to confirm previously documented behavior of an exfoliated rock sheet, which experiences daily closing and opening of the exfoliation fracture during rock cooling and heating, respectively, with a few hours delay from the minimum and maximum temperatures. The most deformed portion of the sheet coincides with the area where both the fracture aperture and the temperature variations are greatest. With the general deformation and temperature relations established, we then employed IRT at a second cliff, where we remotely detected and identified 11 exfoliation sheets that displayed those general thermal relations. TLS measurements then subsequently confirmed the deformation patterns of these sheets showing that sheets with larger apertures are more likely to display larger thermal-related deformations. Our high-frequency monitoring shows how coupled TLS and IRT allows for remote detection of thermally induced deformations and, importantly, how IRT could potentially be used on its own to identify partially detached exfoliation sheets capable of large-scale deformation. These results offer a new and efficient approach for investigating potential rockfall sources on exfoliating cliffs. ELECTRONIC SUPPLEMENTARY MATERIAL: The online version of this article (10.1007/s10346-020-01524-1) contains supplementary material, which is available to authorized users. Springer Berlin Heidelberg 2020-10-07 2021 /pmc/articles/PMC7936945/ /pubmed/33746675 http://dx.doi.org/10.1007/s10346-020-01524-1 Text en © The Author(s) 2020 Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/.
spellingShingle Original Paper
Guerin, Antoine
Jaboyedoff, Michel
Collins, Brian D.
Stock, Greg M.
Derron, Marc-Henri
Abellán, Antonio
Matasci, Battista
Remote thermal detection of exfoliation sheet deformation
title Remote thermal detection of exfoliation sheet deformation
title_full Remote thermal detection of exfoliation sheet deformation
title_fullStr Remote thermal detection of exfoliation sheet deformation
title_full_unstemmed Remote thermal detection of exfoliation sheet deformation
title_short Remote thermal detection of exfoliation sheet deformation
title_sort remote thermal detection of exfoliation sheet deformation
topic Original Paper
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7936945/
https://www.ncbi.nlm.nih.gov/pubmed/33746675
http://dx.doi.org/10.1007/s10346-020-01524-1
work_keys_str_mv AT guerinantoine remotethermaldetectionofexfoliationsheetdeformation
AT jaboyedoffmichel remotethermaldetectionofexfoliationsheetdeformation
AT collinsbriand remotethermaldetectionofexfoliationsheetdeformation
AT stockgregm remotethermaldetectionofexfoliationsheetdeformation
AT derronmarchenri remotethermaldetectionofexfoliationsheetdeformation
AT abellanantonio remotethermaldetectionofexfoliationsheetdeformation
AT matascibattista remotethermaldetectionofexfoliationsheetdeformation