Abstract
The rate of intercalation of graphite by bromine has been measured for natural crystals over a range of 500 fold in area and 10 fold in thickness. The results have been interpreted in terms of Fick's Law for radial diffusion in a cylinder and a mechanism in which all layers are open to intercalation as soon as bromine is admitted at high relative pressure.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Disclaimer: 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.