Mossbauer Studies of Ferrous-A Zeolite: Part 1.—Adsorption/Desorption of Water

Dickson, Bruce L.; Rees, Lovat V. C.

dc.contributor.author	Dickson, Bruce L.
dc.contributor.author	Rees, Lovat V. C.
dc.date.accessioned	2025-02-18T11:52:28Z
dc.date.available	2025-02-18T11:52:28Z
dc.date.issued	1974
dc.identifier.uri	http://dspace.bits-pilani.ac.in:8080/jspui/handle/123456789/17873
dc.description.abstract	Ferrous ions have been ion exchanged into A zeolite. The ferrous ions in the dehydrated form of the zeolite give an isomer shift of 1.08 mm s~l and a temperature independent quadrupole splitting of 0.46 mm s~l. The ferrous ions are shown to be located in the sodalite window site with 3-fold coordination to lattice oxygens. In the partially hydrated zeolite two species of iron are seen in the Mossbauer spectra. Temperature studies show these two sites to be related by an equilibrium process, which is interpreted as the dissociation of a water molecule attached to a ferrous ion to give a hydroxyl group.	en_US
dc.language.iso	en	en_US
dc.publisher	Journal of the Chemical Society : Faraday Transaction - I. The Chemical Society, London. 1974, 70 (11)	en_US
dc.subject	Chemistry	en_US
dc.subject	Mossbauer Studies	en_US
dc.subject	Ferrous-A Zeolite	en_US
dc.subject	Journal of the Chemical Society : Faraday Transaction - I	en_US
dc.title	Mossbauer Studies of Ferrous-A Zeolite: Part 1.—Adsorption/Desorption of Water	en_US
dc.type	Article	en_US