نمایش مختصر رکورد

dc.contributor.authorghobadi, mhen_US
dc.contributor.authorKapelehe, men_US
dc.date.accessioned1399-08-23T06:08:46Zfa_IR
dc.date.accessioned2020-11-13T06:08:47Z
dc.date.available1399-08-23T06:08:46Zfa_IR
dc.date.available2020-11-13T06:08:47Z
dc.date.issued2017-05-01en_US
dc.date.issued1396-02-11fa_IR
dc.identifier.citation(1396). نشریه زمین شناسی مهندسی, 10(4), 3699-3718. doi: 10.18869/acadpub.jeg.10.4.3699fa_IR
dc.identifier.issn2228-6837
dc.identifier.issn7386-8222
dc.identifier.urihttps://dx.doi.org/10.18869/acadpub.jeg.10.4.3699
dc.identifier.urihttp://jeg.khu.ac.ir/article-1-2664-en.html
dc.identifier.urihttps://iranjournals.nlai.ir/handle/123456789/580702
dc.description.abstractDurability is a significant parameter in engineering geology and it shows the extent of the degradability of rocks as the result of mechanical and chemical breakdowns. This phenomenon is closely linked to the composition, porosity and texture of rocks. To understand the relationship between the chemical composition of rocks and their durability the mineralogical properties of the rocks along with durability tests under both acidic and alkaline pH environments were determined. Five samples of limestone and three samples of marl were analyzed. The results revealed that rocks containing high levels of CaCo3 were affected in the acidic conditions while rocks containing high levels of SiO2 were not affected by variance in the pH of the environment. These second groups of rocks were more dependent on the texture of their constituent minerals.en_US
dc.format.extent782
dc.format.mimetypeapplication/pdf
dc.languageEnglish
dc.language.isoen_US
dc.publisherدانشگاه خوارزمیfa_IR
dc.relation.ispartofنشریه زمین شناسی مهندسیfa_IR
dc.relation.ispartofJournal of Engineering Geologyen_US
dc.relation.isversionofhttps://dx.doi.org/10.18869/acadpub.jeg.10.4.3699
dc.subjectSlake durability indexen_US
dc.subjectMineralogical propertiesen_US
dc.subjectChemical compositionen_US
dc.subjectTextureen_US
dc.subjectQom formationen_US
dc.subjectGeotecnicen_US
dc.titleThe Influence of pH of Water and Chemical Composition on the Durability of Different Rocks from the Qom Formation, East and Northeast of Hamedan, Iranen_US
dc.typeTexten_US
dc.citation.volume10
dc.citation.issue4
dc.citation.spage3699
dc.citation.epage3718


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