Abstract
The settling velocities of aqueous slurries of praseodymium oxalate are well represented by the Maude–Whitmore equation in both the fairly dilute and very concentrated cases. Extensive channeling occurs in some slurries with intermediate concentrations, but not in other slurries at the same concentration. Thus, there is a duplicity of values rather than a transition. Aqueous slurries of calcium carbonate also follow the Maude–Whitmore equation at low and high concentrations. Extensive channeling occurs at intermediate values, but there is a region of instability rather than a duplicity of values.
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.
