Abstract
Abstract The exchange of phosphate ions on a strongly basic anionite, Zeroilite FF‐like in certain soils, has a complex character and does not proceed according to simple stechiometric calculations. It was found that in the description of the exchange mechanism, along with stechiometric ratios between phosphate ions and the anionite, the presence of cations and anions associated with that exchange should be also taken into account.
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.