The formation of highly coloured iodide salts of methylviologen MV2+ or diquat DQ2+ within zeolites and clay served as an effective visual probe to delineate the phenomenon that Nal salt migration readily occurs between zeolite crystals and between zeolite and clay upon mere physical contact at ambient temperature.
K. B. Yoon and Y. S. Park, J. Chem. Soc., Chem. Commun., 1993, 522 DOI: 10.1039/C39930000522
To request permission to reproduce material from this article, please go to the Copyright Clearance Center request page.
If you are an author contributing to an RSC publication, you do not need to request permission provided correct acknowledgement is given.
If you are the author of this article, you do not need to request permission to reproduce figures and diagrams provided correct acknowledgement is given. If you want to reproduce the whole article in a third-party publication (excluding your thesis/dissertation for which permission is not required) please go to the Copyright Clearance Center request page.
Read more about how to correctly acknowledge RSC content.
Please wait while we load your content...