Abstract
A comprehensive study of the state of alkaline-earth metal uranoarsenates in saturated aqueous solutions in a wide range of solution acidity was made. A physicochemical model based on the experimental solubility data and on principles of equilibrium thermodynamics was suggested for quantitative description of the state of the heterogeneous system crystalline uranoarsenate MII(AsUO6)2·nH2O-aqueous solution. The model was applied to calculation of the solubility products and Gibbs energies of formation of alkaline-earth metal uranoarsenates, and also of distribution diagrams of equilibrium aqueous solutions and bottom phases.
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.
