Abstract
When a glass comes into contact with water, an electric double layer forms at the glass-water interface. An analytical model that calculates the electric field and the resulting velocity of univalent alkali ions migrating in the glass matrix is developed. The ion migration velocity is calculated for an 85% SiO 2–15% Na 2O glass and for more complex glasses. The calculations indicate that the process of ion migration leads to normalized leach rates which are small compared to glass network dissolution rates.
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.
