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   <dc:title>Effect of calcium sulfate source on the hydration of calcium sulfoaluminate eco-cement</dc:title>
   <dc:creator>García-Maté, Marta</dc:creator>
   <dc:creator>Gómez-de-la-Torre, María de los  Ángeles</dc:creator>
   <dc:creator>León-Reina, Laura</dc:creator>
   <dc:creator>Ramírez-Losilla, Enrique</dc:creator>
   <dc:creator>García-Aranda, Miguel Ángel</dc:creator>
   <dc:creator>Santacruz-Cruz, María Isabel</dc:creator>
   <dc:subject>Cemento</dc:subject>
   <dcterms:abstract>The availability of cements, including eco-cements, with tailored mechanical properties is very important&#xd;
for special applications in the building industry. Here we report a full study of the hydration of calcium&#xd;
sulfoaluminate eco-cements with different sulfate sources (gypsum, bassanite and anhydrite) and two&#xd;
water/cement ratios (0.50 and 0.65). These parameters have been chosen because they are known to&#xd;
strongly modify the mechanical properties of the resulting mortars and concretes. The applied multitechnique&#xd;
characterization includes: phase assemblage by Rietveld method, evolved heat, conductivity,&#xd;
rheology, compressive strength and expansion/retraction measurements. The dissolution rate of the sulfate&#xd;
sources is key to control the hydration reactions. Bassanite dissolves very fast and hence the initial&#xd;
setting time of the pastes and mortars is too short (20 min) to produce homogeneous samples. Anhydrite&#xd;
dissolves slowly so, at 1 hydration-day, the amount of ettringite formed (20 wt%) is lower than that in&#xd;
gypsum pastes (26 wt%) (w/c = 0.50), producing mortars with lower compressive strengths. After 3&#xd;
hydration-days, anhydrite pastes showed slightly larger ettringite contents and hence, mortars with&#xd;
slightly higher compressive strengths. Ettringite content is the chief parameter to explain the strength&#xd;
development in these eco-cements.</dcterms:abstract>
   <dcterms:dateAccepted>2017-05-16T12:09:06Z</dcterms:dateAccepted>
   <dcterms:available>2017-05-16T12:09:06Z</dcterms:available>
   <dcterms:created>2017-05-16T12:09:06Z</dcterms:created>
   <dcterms:issued>2014</dcterms:issued>
   <dc:type>journal article</dc:type>
   <dc:identifier>http://hdl.handle.net/10630/13656</dc:identifier>
   <dc:language>eng</dc:language>
   <dc:rights>open access</dc:rights>
   <dc:rights>by-nc-nd</dc:rights>
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