2010
DOI: 10.1016/j.jcrysgro.2010.04.037
|View full text |Cite
|
Sign up to set email alerts
|

The onset of spherulitic growth in crystallization of calcium carbonate

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
3
1
1

Citation Types

2
64
0

Year Published

2011
2011
2022
2022

Publication Types

Select...
6

Relationship

2
4

Authors

Journals

citations
Cited by 80 publications
(66 citation statements)
references
References 41 publications
(57 reference statements)
2
64
0
Order By: Relevance
“…Aragonite crystals produced at 90°C furthermore support the statement that crystal branching increases when supersaturation is raised. Earlier investigations have shown that also the onset of spherulitic growth for the calcite polymorph can be induced by increasing the level of supersaturation [3]. However, in these studies, the effect of supersaturation could not be decoupled from the temperature.…”
Section: Effect Of Supersaturation and Temperaturementioning
confidence: 88%
See 3 more Smart Citations
“…Aragonite crystals produced at 90°C furthermore support the statement that crystal branching increases when supersaturation is raised. Earlier investigations have shown that also the onset of spherulitic growth for the calcite polymorph can be induced by increasing the level of supersaturation [3]. However, in these studies, the effect of supersaturation could not be decoupled from the temperature.…”
Section: Effect Of Supersaturation and Temperaturementioning
confidence: 88%
“…In this case, however, the supersaturation with respect to the amorphous phase is so low (S 0,amorphous = 1.2) that the direct precipitation of crystalline phases is kinetically preferred. Beck et al [3] have earlier reported that aragonite branches to a higher degree in experiments performed at 30°C than at 90°C. This agrees well with the findings of this study.…”
Section: Effect Of Supersaturation and Temperaturementioning
confidence: 94%
See 2 more Smart Citations
“…Despite ongoing debate (Kamhi, 1963;Wang and Becker, 2009;Kabalah-Amitai et al, 2013), the formation of vaterite and its transformation mechanisms among the polymorphs can be explained in terms of sequential dissolution and (re)crystallization processes (Figure 2) (Kralj et al, 1997;Spanos and Koutsoukos, 1998;Katsifaras and Spanos, 1999;Wei et al, 2003): (i) initially formed ACC particles transform to the least stable vaterite and (ii) the most soluble vaterite undergoes dissolution and crystallization finally forming the most stable calcite. The solubility of the CaCO3 polymorphs is in decreasing order of ACC, vaterite, aragonite, and calcite (Beck and Andreassen, 2010). It was revealed that the ACC transformation into vaterite and calcite can be dominantly found below 40°C, while aragonite can be stabilized at elevated temperature above 60°C (Ogino et al, 1987;Chen and Xiang, 2009;Trushina et al, 2014 , the former shows stronger ability to form hydrate.…”
Section: Molecular Mechanism and Polymorph Formation Of Cacomentioning
confidence: 98%