An investigation of Calcium Silicate Hydrate (C-S-H) topological distribution and modes of precipitation is performed by combining X-ray powder diffraction tomography, performed on an ordinary Portland cement sample, with a numerical scheme that simulates C-S-H precipitation. C-S-H distribution maps obtained both experimentally and numerically are analyzed by means of a quantitative method based on the principles of multifractal systems. The combination of these methods allows C-S-H spatial distribution and modes of precipitation and aggregation to be assessed quantitatively. In particular, the multifractal spectra obtained from the digital images of the cement paste microstructure, act as a structural probe, which is able to quantify the tendency of C-S-H to form clusters. The results of this combined approach suggest that a multifractal network forms by aggregation of C-S-H clusters heterogeneously nucleated on clinker grains and preexisting clusters that are partly homogeneously nucleated in the porous space.

Multifractal analysis of calcium silicate hydrate (C-S-H) mapped by X-ray diffraction microtomography / L. Valentini, G. Artioli, M. Voltolini, M.C. Dalconi. - In: JOURNAL OF THE AMERICAN CERAMIC SOCIETY. - ISSN 0002-7820. - 95:8(2012 Aug), pp. 2647-2652. [10.1111/j.1551-2916.2012.05255.x]

Multifractal analysis of calcium silicate hydrate (C-S-H) mapped by X-ray diffraction microtomography

G. Artioli
Secondo
;
M. Voltolini;
2012

Abstract

An investigation of Calcium Silicate Hydrate (C-S-H) topological distribution and modes of precipitation is performed by combining X-ray powder diffraction tomography, performed on an ordinary Portland cement sample, with a numerical scheme that simulates C-S-H precipitation. C-S-H distribution maps obtained both experimentally and numerically are analyzed by means of a quantitative method based on the principles of multifractal systems. The combination of these methods allows C-S-H spatial distribution and modes of precipitation and aggregation to be assessed quantitatively. In particular, the multifractal spectra obtained from the digital images of the cement paste microstructure, act as a structural probe, which is able to quantify the tendency of C-S-H to form clusters. The results of this combined approach suggest that a multifractal network forms by aggregation of C-S-H clusters heterogeneously nucleated on clinker grains and preexisting clusters that are partly homogeneously nucleated in the porous space.
Settore GEO/06 - Mineralogia
Settore GEO/09 - Georisorse Miner.Appl.Mineral.-Petrogr.per l'amb.e i Beni Cul
ago-2012
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/2434/908530
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