Abstract
Estimation of the metastable zone width has been explored by using models based on the fact that metastable zone width is determined by the nucleation mechanisms acting within a crystallizer. Calculations were carried out for three organic systems and 28 aqueous inorganic systems at the various cooling rates and compositions. Both seeded and unseeded systems have also been applied to the calculations. The models developed were verified with published experimental data. About 150-data points of metastable zone widths measured from bench-scale crystallizer were compared to those obtained by the model. Theoretical model could be used for the prediction of metastable zone width for various nucleation processes.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
