Abstract
In this study, the rate of dissolution of Turkish trona was measured as a function of the trona brine concentration and temperature. The results were compared with a theoretical model of the rate of dissolution from a vertical wall under conditions of natural convection driven by the density gradient in the boundary layer caused by salt concentration differences. The average rate of dissolution in water was measured to be 2.8 g/m 2 s. It was found that the temperature is apparently a more important factor at low solution concentrations than at high concentrations.
Published Version
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.
