Effects of freeze-thawing cycles on the physical and mechanical properties of basaltic and dolomitic rocks evaluated with a decay function model

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dc.authorscopusid57212405947
dc.authorscopusid56218275200
dc.authorscopusid7004045635
dc.contributor.authorAral, İbrahim Feda
dc.contributor.authorBoy, Ramiz
dc.contributor.authorDinçer, Ali Rıza
dc.date.accessioned2022-05-11T14:01:34Z
dc.date.available2022-05-11T14:01:34Z
dc.date.issued2021
dc.departmentFakülteler, Çorlu Mühendislik Fakültesi, İnşaat Mühendisliği Bölümü
dc.departmentFakülteler, Çorlu Mühendislik Fakültesi, Tekstil Mühendisliği Bölümü
dc.departmentFakülteler, Çorlu Mühendislik Fakültesi, Çevre Mühendisliği Bölümü
dc.description.abstractBasalts from Çorlu Karatepe and dolomite from Kırklareli subjected to freeze-thawing (F-T) cycles were studied, and the resulting changes were analyzed. The unweathered rocks and those subjected to 50 F-T cycles after every 10 cycles were tested for the water absorption by weight and volume, P-wave velocity, uniaxial compression strength, point load strength index, and Schmidt hardness values under laboratory conditions. In addition, the relationship between physical and mechanical properties was examined after every 10 cycles, and an exponential model was proposed for the mechanical properties. Two model-generated parameters, i.e., the decay constant and half-life value for each mechanical property, were used to evaluate the disintegration rate of the rocks under the cyclical action of F-T. The evaluation suggests that disintegration behavior was not comparable between the two types of rocks. However, the basalt samples had similar mechanical properties, which indicated a high degree of correlation. © 2021, Springer-Verlag GmbH Germany, part of Springer Nature.
dc.identifier.doi10.1007/s10064-021-02132-6
dc.identifier.endpage2962
dc.identifier.issn1435-9529
dc.identifier.issue4en_US
dc.identifier.scopus2-s2.0-85100905596
dc.identifier.scopusqualityQ1
dc.identifier.startpage2955
dc.identifier.urihttps://doi.org/10.1007/s10064-021-02132-6
dc.identifier.urihttps://hdl.handle.net/20.500.11776/4440
dc.identifier.volume80
dc.identifier.wosWOS:000618611100002
dc.identifier.wosqualityQ2
dc.indekslendigikaynakWeb of Science
dc.indekslendigikaynakScopus
dc.institutionauthorAral, İbrahim Feda
dc.institutionauthorBoy, Ramiz
dc.institutionauthorDinçer, Ali Rıza
dc.language.isoen
dc.publisherSpringer Science and Business Media Deutschland GmbH
dc.relation.ispartofBulletin of Engineering Geology and the Environment
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/closedAccess
dc.subjectBasalt
dc.subjectDecay constant
dc.subjectDolomite
dc.subjectFreeze-thawing
dc.subjectHalf-life
dc.subjectMechanical property
dc.subjectBasalt
dc.subjectDisintegration
dc.subjectSeismic waves
dc.subjectThawing
dc.subjectWater absorption
dc.subjectWave propagation
dc.subjectDegree of correlations
dc.subjectDisintegration rate
dc.subjectExponential models
dc.subjectFreeze-thawing cycles
dc.subjectLaboratory conditions
dc.subjectPhysical and mechanical properties
dc.subjectPoint load strength indices
dc.subjectUni-axial compression
dc.subjectMechanical properties
dc.subjectabsorption
dc.subjectbasalt
dc.subjectcomparative study
dc.subjectcompressive strength
dc.subjectcorrelation
dc.subjectdolomite
dc.subjectfreeze-thaw cycle
dc.subjectmechanical property
dc.subjectP-wave
dc.subjectrock mechanics
dc.subjectuniaxial strength
dc.titleEffects of freeze-thawing cycles on the physical and mechanical properties of basaltic and dolomitic rocks evaluated with a decay function model
dc.typeArticle

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