Abstract
The simultaneous dehydration and decomposition of zinc and cadmium fiuorosilicates leads to the release of gaseous H2O and SiF4, which form amorphous SiO2. The difference of the weight loss measured by thermogravimetry from the calculated value can be accounted for on the basis of the reaction mechanism given. The reaction of H2O with SiF4 affects the thermal dehydration and decomposition of the fluorosilicates studied, and complicated energy effects also occur.
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.
