Abstract

In hydrated MnNa Y, the MnII ion is present as a fully hydrated complex in the zeolite large cavities while NaI is located in site I′ as an octahedral complex composed of three lattice oxide ions and three H2O molecules located in site II′. Upon dehydration, manganese is found in all of the sites I, I′ and II. The exposure of this dehydrated sample to long periods of Cu X-radiation induces a significant redistribution of the exchangeable cations as well as increasing the amount of an oxygen species found at site II′. The presence of this oxygen necessitates the participation of lattice oxide ions in the formation of extra lattice complexes in the sodalite cage.

Full Text
Paper version not known

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 call

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.