Počet záznamů: 1  

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

  1. 1.
    SYSNO ASEP0542525
    Druh ASEPJ - Článek v odborném periodiku
    Zařazení RIVJ - Článek v odborném periodiku
    Poddruh JČlánek ve WOS
    NázevAn Infrared Thermography Approach to Evaluate the Strength of a Rock Cliff
    Tvůrce(i) 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)
    Celkový počet autorů10
    Číslo článku1265
    Zdroj.dok.Remote Sensing. - : MDPI
    Roč. 13, č. 7 (2021)
    Poč.str.13 s.
    Forma vydáníOnline - E
    Jazyk dok.eng - angličtina
    Země vyd.CH - Švýcarsko
    Klíč. slovacompressive strength ; infrared thermography ; rebound hammer ; cooling rate index
    Vědní obor RIVDB - Geologie a mineralogie
    Obor OECDGeology
    Způsob publikováníOpen access
    Institucionální podporaUSMH-B - RVO:67985891
    UT WOS000638803000001
    DOI10.3390/rs13071265
    AnotaceThe 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.
    PracovištěÚstav struktury a mechaniky hornin
    KontaktIva Švihálková, svihalkova@irsm.cas.cz, Tel.: 266 009 216
    Rok sběru2022
    Elektronická adresahttps://www.mdpi.com/2072-4292/13/7/1265
Počet záznamů: 1  

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