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An Infrared Thermography Approach to Evaluate the Strength of a Rock Cliff

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    SYSNO ASEP0542525
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleAn Infrared Thermography Approach to Evaluate the Strength of a Rock Cliff
    Author(s) Loche, M. (CZ)
    Scaringi, G. (CZ)
    Blahůt, Jan (USMH-B) RID, ORCID, SAI
    Melis, M.T. (IT)
    Funedda, A. (IT)
    Da Pelo, S. (IT)
    Erbi, I. (IT)
    Deiana, G. (IT)
    Meloni, M.A. (IT)
    Cocco, F. (IT)
    Number of authors10
    Article number1265
    Source TitleRemote Sensing. - : MDPI
    Roč. 13, č. 7 (2021)
    Number of pages13 s.
    Publication formOnline - E
    Languageeng - English
    CountryCH - Switzerland
    Keywordscompressive strength ; infrared thermography ; rebound hammer ; cooling rate index
    Subject RIVDB - Geology ; Mineralogy
    OECD categoryGeology
    Method of publishingOpen access
    Institutional supportUSMH-B - RVO:67985891
    UT WOS000638803000001
    DOI10.3390/rs13071265
    AnnotationThe mechanical strength is a fundamental characteristic of rock masses that can be empirically related to a number of properties and to the likelihood of instability phenomena. Direct field acquisition of mechanical information on tall cliffs, however, is challenging, particularly in coastal and alpine environments. Here, we propose a method to evaluate the compressive strength of rock blocks by monitoring their thermal behaviour over a 24-h period by infrared thermography. Using a drone-mounted thermal camera and a Schmidt (rebound) hammer, we surveyed granitoid and aphanitic blocks in a coastal cliff in south-east Sardinia, Italy. We observed a strong correlation between a simple cooling index, evaluated in the hours succeeding the temperature peak, and strength values estimated from rebound hammer test results. We also noticed different heating-cooling patterns in relation to the nature and structure of the rock blocks and to the size of the fractures. Although further validation is warranted in different morpho-lithological settings, we believe the proposed method may prove a valid tool for the characterisation of non-directly accessible rock faces, and may serve as a basis for the formulation, calibration, and validation of thermo-hydro-mechanical constitutive models.
    WorkplaceInstitute of Rock Structure and Mechanics
    ContactIva Švihálková, svihalkova@irsm.cas.cz, Tel.: 266 009 216
    Year of Publishing2022
    Electronic addresshttps://www.mdpi.com/2072-4292/13/7/1265
Number of the records: 1  

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