Impact of environmental moisture on C3A polymorphs in the absence and presence of CaSO4 · 0·5 H2O
Source abstract
Abstract
The phenomenon of water vapour sorption by anhydrous C3A polymorphs both in the absence and in the presence of CaSO4·0·5 H2O was studied utilising dynamic and static sorption methods. It was found that orthorhombic C3A starts to sorb water at 55% relative humidity (RH) and cubic C3A at 80% RH. Also, C3Ao sorbs a higher amount of water which is predominantly physically bound, whereas C3Ac preferentially interacts with water by chemical reaction. In the presence of calcium sulfate hemihydrate, ettringite was observed as the predominant pre-hydration product for both C3A modifications: that is, ion transport had occurred between C3A and sulfate. Environmental scanning electron microscopic imaging revealed that in a moist atmosphere, a liquid water film condenses on the surface of the phases as a consequence of capillary condensation between the particles. C3A and sulfate can then dissolve and react with each other. Seemingly, pre-hydration is mainly facilitated through capillary condensation and less through surface interaction with gaseous water molecules.
Source: crossref · Quality: baseline
Research context
OpenAlex topics: Clay minerals and soil interactions · Calcium Carbonate Crystallization and Inhibition · Soil and Unsaturated Flow
SciVX discovery tags are terminology-based. OpenAlex topics are source-provided classifications.
Affiliations
PhD student, Technische Universität München, Lehrstuhl für Bauchemie, Munich, Germany
Professor and Chair for Construction Chemistry, Technische Universität München, Lehrstuhl für Bauchemie, Munich, Germany
Senior Lecturer in Civil Engineering Materials, Institute for Resilient Infrastructure, School of Civil Engineering, University of Leeds, Leeds, UK
Professor, Department of Building Materials, University of Lund, Lund, Sweden
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