Erratum to “Simulation of metastable zone width and induction time for a seeded aqueous solution of potassium sulfate” [J. Cryst. Growth 312 (2010) 2734–2739]

2011 ◽  
Vol 316 (1) ◽  
pp. 201
Author(s):  
M. Kobari ◽  
N. Kubota ◽  
I. Hirasawa
1984 ◽  
Vol 49 (3) ◽  
pp. 559-569 ◽  
Author(s):  
Jaroslav Nývlt

The metastable zone width of an aqueous solution of KCI was measured as a function of the time and temperature of overheating above the equilibrium solubility temperature. It has been found that when the experiments follow close upon one another, the parameters of the preceding experiment affect the results of the experiment to follow.The results are interpreted in terms of hypotheses advanced in the literature to account for the effect of thermal history of solution. The plausibility and applicability of these hypotheses are assessed for the given cause of aqueous solution of a well soluble electrolyte.


CrystEngComm ◽  
2014 ◽  
Vol 16 (41) ◽  
pp. 9743-9752 ◽  
Author(s):  
Lie-Ding Shiau ◽  
Tsan-Sheng Lu

A model is developed to recover the interfacial energy from the induction time and the metastable zone width data.


CrystEngComm ◽  
2015 ◽  
Vol 17 (23) ◽  
pp. 4402-4404 ◽  
Author(s):  
Lie-Ding Shiau

An integral equation is developed to predict MSZW from the induction time results based on the classical nucleation theory.


CrystEngComm ◽  
2015 ◽  
Vol 17 (3) ◽  
pp. 577-586 ◽  
Author(s):  
Huaiyu Yang

A relation between induction time and metastable zone width has been developed based on Classical Nucleation Theory, by which relation metastable zone width has been extrapolated from the induction time results and compared with experimental values. Influences of several thermodynamic and kinetic parameters on metastable zone width have been estimated.


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