Thermal decomposition of tricalcium silicate hydrate

Yoshihiko Okada; Hideki Ishida; Takeshi Mitsuda

Thermal decomposition of tricalcium silicate hydrate

Yoshihiko Okada, Hideki Ishida, Takeshi Mitsuda

Environmental Studies

Research output: Contribution to journal › Article › peer-review

3 Citations (Scopus)

Abstract

Nuclear magnetic resonance examination confirms the existence of dimer silicate anions in C₃SH_1.5, suggesting the possible composition Ca₆(Si₂O₇)(OH)₄. Upon being heated, C₃SH_1.5 dehydrates at 520-550 °C with a sharp endothermy and decomposes to CaO plus a calciochondrodite-like phase, which on further heating dissociates, with a gradual weight loss, to α′_L-C₂S with CaO at 800 °C.

Original language	English
Pages (from-to)	2277-2282
Number of pages	6
Journal	Journal of the American Ceramic Society
Volume	77
Issue number	9
Publication status	Published - 1994 Sep

ASJC Scopus subject areas

Ceramics and Composites

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title = "Thermal decomposition of tricalcium silicate hydrate",

abstract = "Nuclear magnetic resonance examination confirms the existence of dimer silicate anions in C3SH1.5, suggesting the possible composition Ca6(Si2O7)(OH)4. Upon being heated, C3SH1.5 dehydrates at 520-550 °C with a sharp endothermy and decomposes to CaO plus a calciochondrodite-like phase, which on further heating dissociates, with a gradual weight loss, to α′L-C2S with CaO at 800 °C.",

author = "Yoshihiko Okada and Hideki Ishida and Takeshi Mitsuda",

year = "1994",

month = sep,

language = "English",

volume = "77",

pages = "2277--2282",

journal = "Journal of the American Ceramic Society",

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T1 - Thermal decomposition of tricalcium silicate hydrate

AU - Okada, Yoshihiko

AU - Ishida, Hideki

AU - Mitsuda, Takeshi

PY - 1994/9

Y1 - 1994/9

N2 - Nuclear magnetic resonance examination confirms the existence of dimer silicate anions in C3SH1.5, suggesting the possible composition Ca6(Si2O7)(OH)4. Upon being heated, C3SH1.5 dehydrates at 520-550 °C with a sharp endothermy and decomposes to CaO plus a calciochondrodite-like phase, which on further heating dissociates, with a gradual weight loss, to α′L-C2S with CaO at 800 °C.

AB - Nuclear magnetic resonance examination confirms the existence of dimer silicate anions in C3SH1.5, suggesting the possible composition Ca6(Si2O7)(OH)4. Upon being heated, C3SH1.5 dehydrates at 520-550 °C with a sharp endothermy and decomposes to CaO plus a calciochondrodite-like phase, which on further heating dissociates, with a gradual weight loss, to α′L-C2S with CaO at 800 °C.

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M3 - Article

AN - SCOPUS:0028515504

VL - 77

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EP - 2282

JO - Journal of the American Ceramic Society

JF - Journal of the American Ceramic Society

SN - 0002-7820

IS - 9

ER -

Thermal decomposition of tricalcium silicate hydrate

Abstract

ASJC Scopus subject areas

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