Variation of thermal conductivity of rocks with pressure

Basit Öğe Kaydı
dc.contributor.authorDurutürk, YS
dc.contributor.authorDemirci, A
dc.contributor.authorKeçeciler, A
dc.date.accessioned2024-09-18T20:32:52Z
dc.date.available2024-09-18T20:32:52Z
dc.date.issued2002
dc.departmentHatay Mustafa Kemal Üniversitesien_US
dc.description.abstractThis paper deals with the results of the variation of thermal conductivity of rocks with pressure on a laboratory scale. For this purpose, the authors have added a pressure-supplying unit to the apparatus developed by Mousset-Jones and McPherson (7986), Onder (1995), Ashworth and Ashworth (1979), and Innaurato and Occella (1989) in order to measure the thermal conductivity under pressure. The values obtained from the tests performed by this new apparatus have been stated using a regression analysis and the related graphs have been drawn. Results have shown that the thermal conductivity of rock varies digressively with pressure. The same results have been obtained in different rocks types.en_US
dc.identifier.endpage71en_US
dc.identifier.issn0317-0926
dc.identifier.issue1061en_US
dc.identifier.startpage67en_US
dc.identifier.urihttps://hdl.handle.net/20.500.12483/11185
dc.identifier.volume95en_US
dc.identifier.wosWOS:000176753100017en_US
dc.identifier.wosqualityQ4en_US
dc.indekslendigikaynakWeb of Scienceen_US
dc.language.isoenen_US
dc.publisherCanadian Inst Mining Metallurgy Petroleumen_US
dc.relation.ispartofCim Bulletinen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectmine heaten_US
dc.subjectgeothermal gradientsen_US
dc.subjectheat transferen_US
dc.subjectthermal conductivityen_US
dc.titleVariation of thermal conductivity of rocks with pressureen_US
dc.typeArticleen_US

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