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<rdf:RDF xmlns:rdf="http://www.w3.org/1999/02/22-rdf-syntax-ns#" xmlns:dc="http://purl.org/dc/elements/1.1/"><rdf:Description rdf:about="https://repozitorij.uni-lj.si/IzpisGradiva.php?id=125411"><dc:title>Detailed investigation of ACR in concrete with silica-free dolomite aggregate</dc:title><dc:creator>Štukovnik,	Petra	(Avtor)
	</dc:creator><dc:creator>Bokan-Bosiljkov,	Violeta	(Avtor)
	</dc:creator><dc:creator>Marinšek,	Marjan	(Avtor)
	</dc:creator><dc:subject>alkali carbonate reaction - ACR in concrete</dc:subject><dc:subject>silica-free dolomite aggregate</dc:subject><dc:subject>microstructure investigation</dc:subject><dc:subject>reaction mechanism</dc:subject><dc:description>The progress of the alkali-carbonate reaction (ACR) in NaOH or an aqueous environment at elevated tem-perature (60°C) was investigated in concrete prepared with silica-free dolomite aggregate. The resultsobtained show that chemical reactions characteristic for the ACR progressed in all aged concrete systems.In NaOH aged samples, dolomite grains smaller than 2 mm in diameter went through a completededolomitisation process. Additionally, new Mg-Al, Mg-Si and Mg-Al-Si phases were recognized at theaggregate-cement paste interface. The less alkaline environment in the case of H2O-aged samplesresulted in substantially decelerated ACR reaction. Based on observed long-term microstructural andphase changes, a detailed scheme of the ACR in concretes with silica-free dolomite aggregates was pro-posed. It turned out that the soluble Si-source does not necessarily originate from the aggregate itself butrather through the Pozzolanic reaction of cement binder decomposition/regeneration cycle.</dc:description><dc:date>2019</dc:date><dc:date>2021-03-15 09:12:21</dc:date><dc:type>Članek v reviji</dc:type><dc:identifier>125411</dc:identifier><dc:language>sl</dc:language></rdf:Description></rdf:RDF>
