Please use this identifier to cite or link to this item: https://hdl.handle.net/11499/5872
Title: The effect of welding degree on geotechnical properties of an ignimbrite flow unit: The Bitlis castle case (eastern Turkey)
Authors: Koralay, Tamer
Özkul, Mehmet
Kumsar, Halil
Çelik, Sefer B.
Pektaş, Kadir
Keywords: Bitlis castle
Building material
Geotechnical properties
Ignimbrite
Welding
Ancient buildings
Building stone
Eastern Anatolia
Eastern Turkey
Eutaxitic textures
Flow unit
Freeze-thaw cycles
Geochemical composition
Glass shards
Ignimbrites
Major oxides
Mechanical and physical properties
Mineralogical compositions
Particulate flows
Physical and mechanical properties
Pyroclastic density currents
Sanidines
Slake durability
Stratovolcanoes
Structural feature
Volcanic centers
Building materials
Compressive strength
Crystallography
Masonry materials
Mineralogy
Physical properties
Quartz
Silicate minerals
Textures
Thawing
Volcanoes
Mechanical properties
building stone
chemical composition
compressive strength
durability
flow field
freeze-thaw cycle
geochemistry
geotechnical property
historic building
ignimbrite
masonry
plagioclase
porosity
pumice
pyroxene
quartz
sanidine
stratovolcano
trachyte
vesicle
volcanism
welding
Anatolia
Bitlis
Nemrut
Turkey
Abstract: Ignimbrites 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.
URI: https://hdl.handle.net/11499/5872
https://doi.org/10.1007/s12665-011-0931-1
ISSN: 1866-6280
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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