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Investigating the Potential of Infrared Thermography to Inform on Physical and Mechanical Properties of Soils for Geotechnical Engineering

Identifikátory výsledku

  • Kód výsledku v IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985891%3A_____%2F22%3A00564750" target="_blank" >RIV/67985891:_____/22:00564750 - isvavai.cz</a>

  • Nalezeny alternativní kódy

    RIV/00216208:11310/22:10448874

  • Výsledek na webu

    <a href="https://www.mdpi.com/2072-4292/14/16/4067" target="_blank" >https://www.mdpi.com/2072-4292/14/16/4067</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.3390/rs14164067" target="_blank" >10.3390/rs14164067</a>

Alternativní jazyky

  • Jazyk výsledku

    angličtina

  • Název v původním jazyce

    Investigating the Potential of Infrared Thermography to Inform on Physical and Mechanical Properties of Soils for Geotechnical Engineering

  • Popis výsledku v původním jazyce

    Knowledge of physical and mechanical properties of geomaterials is fundamental toncharacterise their response to external forcings (mechanical, climatic) at various scales. This is true, forninstance, in slope stability assessments, civil engineering works, and agriculture. The direct evaluationnof these properties in situ can be difficult, especially in inaccessible or vast areas, and so can be thensampling and subsequent testing in the laboratory—where ensuring the representativeness of thenacquired data at the scale of analysis poses an additional challenge. Thus, empirical correlations withnmore readily determinable quantities remain a powerful and practical tool. Recently, several sensors,nable to inform on various geomaterial properties, have been developed. However, applications haventypically targeted rocks, while studies on uncemented geomaterials (soils, geotechnically speaking)nare lacking. Here, we propose a simple method to evaluate the porosity and critical state frictionnangle of soils via infrared thermography, consisting of periodic acquisitions of images in infrarednwavelengths. To demonstrate the method’s capability, we analysed the cooling behaviour of samplesnof bentonite, kaolin, and sand (for which an extensive characterisation exists in the literature), afterncompaction to different porosities and pre-heating in an oven. We interpreted the results by seekingnthe optimal time interval for which a cooling rate index (CRI) could be defined, which is best linkednwith the target property. We found that the CRI correlates very well with the critical state frictionnangle (R2 > 0.85) and that different materials show unique and strong (R2 = 0.86–0.99) relationshipsnbetween their porosity and the CRI, which also varies in a material-specific fashion according tonthe explored time interval. Although a systematic investigation on a wide range of natural soilsnis warranted, we argue that our method can be highly informative and could be used to calibratenremote sensing-based full-scale implementations in situ for various purposes.n

  • Název v anglickém jazyce

    Investigating the Potential of Infrared Thermography to Inform on Physical and Mechanical Properties of Soils for Geotechnical Engineering

  • Popis výsledku anglicky

    Knowledge of physical and mechanical properties of geomaterials is fundamental toncharacterise their response to external forcings (mechanical, climatic) at various scales. This is true, forninstance, in slope stability assessments, civil engineering works, and agriculture. The direct evaluationnof these properties in situ can be difficult, especially in inaccessible or vast areas, and so can be thensampling and subsequent testing in the laboratory—where ensuring the representativeness of thenacquired data at the scale of analysis poses an additional challenge. Thus, empirical correlations withnmore readily determinable quantities remain a powerful and practical tool. Recently, several sensors,nable to inform on various geomaterial properties, have been developed. However, applications haventypically targeted rocks, while studies on uncemented geomaterials (soils, geotechnically speaking)nare lacking. Here, we propose a simple method to evaluate the porosity and critical state frictionnangle of soils via infrared thermography, consisting of periodic acquisitions of images in infrarednwavelengths. To demonstrate the method’s capability, we analysed the cooling behaviour of samplesnof bentonite, kaolin, and sand (for which an extensive characterisation exists in the literature), afterncompaction to different porosities and pre-heating in an oven. We interpreted the results by seekingnthe optimal time interval for which a cooling rate index (CRI) could be defined, which is best linkednwith the target property. We found that the CRI correlates very well with the critical state frictionnangle (R2 > 0.85) and that different materials show unique and strong (R2 = 0.86–0.99) relationshipsnbetween their porosity and the CRI, which also varies in a material-specific fashion according tonthe explored time interval. Although a systematic investigation on a wide range of natural soilsnis warranted, we argue that our method can be highly informative and could be used to calibratenremote sensing-based full-scale implementations in situ for various purposes.n

Klasifikace

  • Druh

    J<sub>imp</sub> - Článek v periodiku v databázi Web of Science

  • CEP obor

  • OECD FORD obor

    10505 - Geology

Návaznosti výsledku

  • Projekt

    Výsledek vznikl pri realizaci vícero projektů. Více informací v záložce Projekty.

  • Návaznosti

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Ostatní

  • Rok uplatnění

    2022

  • Kód důvěrnosti údajů

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Údaje specifické pro druh výsledku

  • Název periodika

    Remote Sensing

  • ISSN

    2072-4292

  • e-ISSN

    2072-4292

  • Svazek periodika

    14

  • Číslo periodika v rámci svazku

    16

  • Stát vydavatele periodika

    CH - Švýcarská konfederace

  • Počet stran výsledku

    12

  • Strana od-do

    4067

  • Kód UT WoS článku

    000845783500001

  • EID výsledku v databázi Scopus

    2-s2.0-85137784071