Abstract
New data relevant to calcium silicate hydrate (C-S-H) gels prepared at room temperature have been obtained over a time period of up to 112 weeks. X-ray diffraction (XRD) indicates equilibrium was attained after 64 weeks. Coupled with fourier transform infrared (FT-IR) spectroscopy, a phase change in C-S-H gel at Ca/Si ≈ 1.0 was identified and the occurrence of portlandite as a distinct phase for Ca/Si > 1.64. The incongruent dissolution of C-S-H gel was modeled as a non-ideal solid solution aqueous solution (SSAS) between the end-member components CaH2SiO4 (CSH) and Ca(OH)2 (CH) using equations defining the solidus and solutus curves on a Lippmann phase diagram. Despite being semi-empirical, the model provides a reasonable and consistent fit to the solubility data and can therefore be used to describe the incongruent dissolution of C-S-H gels with compositions Ca/Si ≥ 1.0.
Original language | English |
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Pages (from-to) | 502-511 |
Number of pages | 10 |
Journal | Cement and Concrete Research |
Volume | 37 |
Issue number | 4 |
DOIs | |
Publication status | Published - Apr 2007 |
Bibliographical note
Funding Information:This work was funded by a Natural Environment Research Council (NERC) CASE PhD studentship with contributions from Nirex, Nagra, and Castle Cement. We are indebted to Rory Wilson, Richard Brooker and Poon Cheung Choi who assisted us with the access and use of the PSD-XRD, FT-IR and ICP-AES instruments, respectively. We would also like to thank the anonymous reviewers whose suggestions improved this manuscript.
Other keywords
- A. pH
- B. calcium silicate hydrate (C-S-H)
- C. Ca(OH)
- E. Modeling