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Quantitative X-ray pair distribution function analysis of nanocrystalline calcium silicate hydrates: a contribution to the understanding of cement chemistry.


ABSTRACT: The structural evolution of nanocrystalline calcium silicate hydrate (C-S-H) as a function of its calcium to silicon (Ca/Si) ratio has been probed using qualitative and quantitative X-ray atomic pair distribution function analysis of synchrotron X-ray scattering data. Whatever the Ca/Si ratio, the C-S-H structure is similar to that of tobermorite. When the Ca/Si ratio increases from ?0.6 to ?1.2, Si wollastonite-like chains progressively depolymerize through preferential omission of Si bridging tetrahedra. When the Ca/Si ratio approaches ?1.5, nanosheets of portlandite are detected in samples aged for 1?d, while microcrystalline portlandite is detected in samples aged for 1?year. High-resolution transmission electron microscopy imaging shows that the tobermorite-like structure is maintained to Ca/Si > 3.

SUBMITTER: Grangeon S 

PROVIDER: S-EPMC5294392 | biostudies-other | 2017 Feb

REPOSITORIES: biostudies-other

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Quantitative X-ray pair distribution function analysis of nanocrystalline calcium silicate hydrates: a contribution to the understanding of cement chemistry.

Grangeon Sylvain S   Fernandez-Martinez Alejandro A   Baronnet Alain A   Marty Nicolas N   Poulain Agnieszka A   Elkaïm Erik E   Roosz Cédric C   Gaboreau Stéphane S   Henocq Pierre P   Claret Francis F  

Journal of applied crystallography 20170201 Pt 1


The structural evolution of nanocrystalline calcium silicate hydrate (C-S-H) as a function of its calcium to silicon (Ca/Si) ratio has been probed using qualitative and quantitative X-ray atomic pair distribution function analysis of synchrotron X-ray scattering data. Whatever the Ca/Si ratio, the C-S-H structure is similar to that of tobermorite. When the Ca/Si ratio increases from ∼0.6 to ∼1.2, Si wollastonite-like chains progressively depolymerize through preferential omission of Si bridging  ...[more]

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