2018
DOI: 10.1007/s12665-018-7485-4
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Ghaleh-khargushi rhyodacite and Gorid andesite from Iran: characterization, uses, and durability

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Cited by 26 publications
(7 citation statements)
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“…5) according to the level of weathering. Similar results were measured on other andesite lithotypes (Zalooli et al 2018); Fener and İnce (2015) detected 24% strength reduction after 30 F-T cycles, and Yavuz 2011detected 8% after 30 and 13% after 50 cycles. The highest uniaxial compressive strength and modulus of elasticity values were measured in the case of andesite-9 ( Figs.…”
Section: Resultssupporting
confidence: 78%
“…5) according to the level of weathering. Similar results were measured on other andesite lithotypes (Zalooli et al 2018); Fener and İnce (2015) detected 24% strength reduction after 30 F-T cycles, and Yavuz 2011detected 8% after 30 and 13% after 50 cycles. The highest uniaxial compressive strength and modulus of elasticity values were measured in the case of andesite-9 ( Figs.…”
Section: Resultssupporting
confidence: 78%
“…Explanations joining mechanical strength and bulk properties of the pore system, such as porosity, water absorption, and capillarity coefficient, with higher values of microporosity have been presented for higher susceptibility to salt crystallization of travertines [81] and pyroclastic rocks, with the variations in this last study being related to welding degree [43]. A comparison of rhyodacite and andesite found the former more susceptible than andesite because of the lower strength, higher porosity, and also higher microporosity [58]. Similar results were obtained in studies of freeze-thaw tests with travertines and limestones [41].…”
Section: Multiple Factorsmentioning
confidence: 75%
“…Weight loss occurs when the stress induced by salt crystallization exceeds the cohesion threshold of the stone. When crystallization pressure is insufficient to reach the cohesion threshold, there is no grain loss, although other deterioration processes such as development and enlargement of microcracks may have occurred (Benavente et al 2007;Zalooli et al 2018a). Uniaxial compression strength and Brazilian tensile strength reflect these cohesive forces at a macroscopic scale.…”
Section: Discussionmentioning
confidence: 99%
“…Different microscopic approaches have been utilized to characterize decay in building stones, including optical, polarized and fluorescence microscopies, scanning electron microscopy (SEM), and confocal scanning laser microscopy (CSLM). These techniques provide clear evidence of the decay processes in the stones and the area where the decay is taking place (Benavente et al 1999;Siedel and Siegesmund 2014;Zalooli et al 2018a).…”
Section: Introductionmentioning
confidence: 99%