Please use this identifier to cite or link to this item: https://hdl.handle.net/11499/5872
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dc.contributor.authorKoralay, Tamer-
dc.contributor.authorÖzkul, Mehmet-
dc.contributor.authorKumsar, Halil-
dc.contributor.authorÇelik, Sefer B.-
dc.contributor.authorPektaş, Kadir-
dc.date.accessioned2019-08-16T12:03:04Z-
dc.date.available2019-08-16T12:03:04Z-
dc.date.issued2011-
dc.identifier.issn1866-6280-
dc.identifier.urihttps://hdl.handle.net/11499/5872-
dc.identifier.urihttps://doi.org/10.1007/s12665-011-0931-1-
dc.description.abstractIgnimbrites are associated with nearly most of the world's volcanoes and are defined as a deposit from pyroclastic density currents. They consist predominantly of pumiceous lapilli and blocks, and glass shards, which shows evidence of having been emplaced as a concentrated hot and dry particulate flow. These rocks are widely used as building stone especially in ancient buildings. Bitlis valley is covered by ignimbritic products, derived from Nemrut stratovolcano, one of the significant volcanic centers in Eastern Anatolia. The Bitlis ignimbrite is separated into lower level (LL), middle level (ML) and upper level (UL) according to color, welding degree and structural features. All three levels were used extensively in many parts of the Bitlis castle as masonry materials. Studies were carried out on mineralogical and geochemical composition and on physical and mechanical properties of the ignimbrites. In addition, a freeze-thaw cycle test was executed. There are no considerable differences in mineralogical composition among the levels of ignimbrite. All levels contain plagioclase, sanidine, pyroxene, and opaque mineral. In addition, anorthoclase and quartz are seen. In general, the LL of ignimbrite shows relic perlitic and eutaxitic texture, whereas eutaxitic and vesicular texture are commonly developed in the ML and UL, respectively. Lower, middle, and upper level ignimbrite samples display similar and limited compositional spread in terms of major oxide elements. They have trachyte composition. Building stones can be classified according to mineralogy, mechanical and physical properties and processing types. Mechanical and physical properties are very important with respect to stone quality/durability. The mechanical and physical properties of the ignimbrites are controlled by the welding degree. It was found that increasing welding degree from UL to LL correlates with increasing density, compressive strength and slake durability index and with decreasing porosity. The Bitlis ignimbrites have turned out as susceptible to freeze-thaw cycles. © 2011 Springer-Verlag.en_US
dc.language.isoenen_US
dc.relation.ispartofEnvironmental Earth Sciencesen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectBitlis castleen_US
dc.subjectBuilding materialen_US
dc.subjectGeotechnical propertiesen_US
dc.subjectIgnimbriteen_US
dc.subjectWeldingen_US
dc.subjectAncient buildingsen_US
dc.subjectBuilding stoneen_US
dc.subjectEastern Anatoliaen_US
dc.subjectEastern Turkeyen_US
dc.subjectEutaxitic texturesen_US
dc.subjectFlow uniten_US
dc.subjectFreeze-thaw cyclesen_US
dc.subjectGeochemical compositionen_US
dc.subjectGlass shardsen_US
dc.subjectIgnimbritesen_US
dc.subjectMajor oxidesen_US
dc.subjectMechanical and physical propertiesen_US
dc.subjectMineralogical compositionsen_US
dc.subjectParticulate flowsen_US
dc.subjectPhysical and mechanical propertiesen_US
dc.subjectPyroclastic density currentsen_US
dc.subjectSanidinesen_US
dc.subjectSlake durabilityen_US
dc.subjectStratovolcanoesen_US
dc.subjectStructural featureen_US
dc.subjectVolcanic centersen_US
dc.subjectBuilding materialsen_US
dc.subjectCompressive strengthen_US
dc.subjectCrystallographyen_US
dc.subjectMasonry materialsen_US
dc.subjectMineralogyen_US
dc.subjectPhysical propertiesen_US
dc.subjectQuartzen_US
dc.subjectSilicate mineralsen_US
dc.subjectTexturesen_US
dc.subjectThawingen_US
dc.subjectVolcanoesen_US
dc.subjectMechanical propertiesen_US
dc.subjectbuilding stoneen_US
dc.subjectchemical compositionen_US
dc.subjectcompressive strengthen_US
dc.subjectdurabilityen_US
dc.subjectflow fielden_US
dc.subjectfreeze-thaw cycleen_US
dc.subjectgeochemistryen_US
dc.subjectgeotechnical propertyen_US
dc.subjecthistoric buildingen_US
dc.subjectignimbriteen_US
dc.subjectmasonryen_US
dc.subjectplagioclaseen_US
dc.subjectporosityen_US
dc.subjectpumiceen_US
dc.subjectpyroxeneen_US
dc.subjectquartzen_US
dc.subjectsanidineen_US
dc.subjectstratovolcanoen_US
dc.subjecttrachyteen_US
dc.subjectvesicleen_US
dc.subjectvolcanismen_US
dc.subjectweldingen_US
dc.subjectAnatoliaen_US
dc.subjectBitlisen_US
dc.subjectNemruten_US
dc.subjectTurkeyen_US
dc.titleThe effect of welding degree on geotechnical properties of an ignimbrite flow unit: The Bitlis castle case (eastern Turkey)en_US
dc.typeArticleen_US
dc.identifier.volume64en_US
dc.identifier.issue3en_US
dc.identifier.startpage869-
dc.identifier.startpage869en_US
dc.identifier.endpage881en_US
dc.authorid0000-0002-8353-3501-
dc.authorid0000-0002-0949-4225-
dc.authorid0000-0001-8051-2150-
dc.authorid0000-0003-1850-5229-
dc.identifier.doi10.1007/s12665-011-0931-1-
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.identifier.scopus2-s2.0-80052832831en_US
dc.identifier.wosWOS:000295845300025en_US
dc.identifier.scopusqualityQ2-
dc.ownerPamukkale University-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.languageiso639-1en-
item.openairetypeArticle-
item.cerifentitytypePublications-
item.grantfulltextnone-
item.fulltextNo Fulltext-
crisitem.author.dept10.08. Geological Engineering-
crisitem.author.dept10.08. Geological Engineering-
crisitem.author.dept10.08. Geological Engineering-
crisitem.author.dept10.08. Geological Engineering-
crisitem.author.dept12.07. Art History-
Appears in Collections:Fen-Edebiyat Fakültesi Koleksiyonu
Mühendislik Fakültesi Koleksiyonu
Scopus İndeksli Yayınlar Koleksiyonu / Scopus Indexed Publications Collection
WoS İndeksli Yayınlar Koleksiyonu / WoS Indexed Publications Collection
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