In situ tomographic investigation on the early hydration behaviors of cementing systems

▸ We show in situ evolution of tomographic images of hydrating cements up to 12h. ▸ A linear correlation between tomographic colour and mineral structure is found. ▸ Subsequently, a lecture key for interpretation of tomographic image is proposed. ▸ Peculiar information about the different hydration...

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Veröffentlicht in:Construction & building materials 2012-04, Vol.29 (1), p.284-290
Hauptverfasser: Gastaldi, D., Canonico, F., Capelli, L., Boccaleri, E., Milanesio, M., Palin, L., Croce, G., Marone, F., Mader, K., Stampanoni, M.
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Sprache:eng
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Zusammenfassung:▸ We show in situ evolution of tomographic images of hydrating cements up to 12h. ▸ A linear correlation between tomographic colour and mineral structure is found. ▸ Subsequently, a lecture key for interpretation of tomographic image is proposed. ▸ Peculiar information about the different hydration behavior are extracted. ▸ In situ tomographic investigation allows studying cement microstructure evolution. The early hydration of three cementing materials has been investigated in situ by Synchrotron X-ray Tomographic Microscopy thanks to an automatic sample exchanger recently integrated at the TOMCAT beamline at the Swiss Light Source in Villigen (CH). Hydration has been investigated by following the three dimensional evolution of pastes up to 12h, with particular attention to the consumption of anhydrous phases, the formation of hydrates and to changes in microstructure. A lecture key for the interpretation of the tomographic images is proposed, based on the relationship between the linear attenuation coefficient μ-function of the density and elemental composition of each mineral phase- and the corresponding grey tone experimentally observed. Some examples of application of the technique are proposed, such as: a comparison among the reaction kinetics of the three investigated cements, the study of morphological evolution of mineral phases, the analyses of the three-dimensional evolution of the pore network.
ISSN:0950-0618
1879-0526
DOI:10.1016/j.conbuildmat.2011.10.016