Abstract
The transitions from vaterite to calcite and from vaterite to aragonite, were found with the anionic surfactant sodium dodecyl benzene sulfonate and β-cyclodextrin as a template, respectively, when the experimental temperature was controlled at 90 °C. The transition from calcite to aragonite was found when the experimental temperature was controlled at 120 °C. The molar ratio of 1:1 and 1:2 supermolecules composed of sodium dodecyl benzene sulfonate ion and β-cyclodextrin molecule may be formed at 90 and 120 °C, respectively. The possible formation mechanisms of different CaCO 3 polymorphs are proposed based on the “structural correspondence”.
Sign-in/Register to access full text options 
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.
