1993
DOI: 10.1111/j.1151-2916.1993.tb06638.x
|View full text |Cite
|
Sign up to set email alerts
|

α‐Dicalcium Silicate Hydrate: Preparation, Decomposed Phase, and Its Hydration

Abstract: ol-C,SH can be synthesized by hydrothermal treatment of lime and silicic acid for 2 h at 200°C. When heated to 390-490"C, a-C,SH dissociates through a two-step process to form an intermediate phase plus some y-C,S. This appears to be a new dicalcium silicate different from known dicalcium silicate-, a'", p, and y phase-and is stable until around 900°C. At 920-96OoC, all the phases are transformed to the atL phase. The intermediate phase has high crystallinity and is stable at room temperature. 29Si MAS NMR mea… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1
1

Citation Types

4
38
0

Year Published

1993
1993
2024
2024

Publication Types

Select...
6
3

Relationship

0
9

Authors

Journals

citations
Cited by 58 publications
(45 citation statements)
references
References 19 publications
4
38
0
Order By: Relevance
“…The most reactive polymorph is indeed an XRD-amorphous phase [52] with the same composition as the crystalline polymorphs. The other very reactive polymorph is x-C 2 S [53]. These polymorphs have the identical chemical composition but a much higher reactivity than polymorphs known from common cement manufacture.…”
Section: Polymorphism and Crystal Structure Of Belitementioning
confidence: 92%
See 1 more Smart Citation
“…The most reactive polymorph is indeed an XRD-amorphous phase [52] with the same composition as the crystalline polymorphs. The other very reactive polymorph is x-C 2 S [53]. These polymorphs have the identical chemical composition but a much higher reactivity than polymorphs known from common cement manufacture.…”
Section: Polymorphism and Crystal Structure Of Belitementioning
confidence: 92%
“…Synthesis of highly reactive belite polymorphs. The production of highly reactive C 2 S polymorphs was pioneered by Ishida [53] and Garbev et al [63]. Supported by the presence of foreign ions it is based on a two-step process that involves the synthesis of α-Ca 2 SiO 4 ⋅ H 2 O in an autoclave at 150-200°C as a first step and its conversion into highly reactive belite polymorphs by tempering at 400-800°C in a second step, see Fig.…”
Section: Synthesis and Stabilization Of Belite Polymorphsmentioning
confidence: 99%
“…On the other hand, XRD analysis illustrates that the crystallographic properties and density of dissociation products of α -C 2 SH depend on the calcination temperature [20]. α -C 2 SH dissociates at 390–490°C forming an intermediate phase plus γ -C 2 S. The intermediate phase then transforms to α L ′ phase at 920–960°C and yields β -C 2 S on cooling while hillebrandite yields β -C 2 S at the lowest temperature [21]. Hillebrandite synthesized by mechanochemical treatment of amorphous precipitated silica/lime decomposed into β -C 2 S below 1000°C [18].…”
Section: Introductionmentioning
confidence: 99%
“…Table 5 lists the weight losses in different temperature ranges for specimens cured in water and carbonate solution and Figure 4 shows the DTG curves for the control samples (cured for 24 h at 270°C) and the samples cured for 10 d. The weight losses up to 400°C can be associated with (sodium, calcium) silica aluminate and CSHs; zeolite decomposition may also contribute to the weight loss in that temperature range (analcime, mordenite and thomsonite (Foldvari, 2011)). Between about 400 and 550°C, calcium-rich CSHs contribute to the weight loss (Ishida et al, 1993), along with calcium hydroxide; the recrystallisation of aragonite to calcite occurs at around 450°C. The weight losses at temperatures above 550°C are, for the most part, due to the decomposition of carbonates such as calcite ($600°C), magnetite ($620-650°C), calcium magnesium carbonates (600-650°C, huntite), magnesium iron calcium carbonate ($700-750°C) and dolomite (750-800°C) (Foldvari, 2011).…”
Section: Resultsmentioning
confidence: 99%