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Please use this identifier to cite or link to this item: http://dspace.bits-pilani.ac.in:8080/jspui/handle/123456789/17873
Title: Mossbauer Studies of Ferrous-A Zeolite: Part 1.—Adsorption/Desorption of Water
Authors: Dickson, Bruce L.
Rees, Lovat V. C.
Keywords: Chemistry
Mossbauer Studies
Ferrous-A Zeolite
Journal of the Chemical Society : Faraday Transaction - I
Issue Date: 1974
Publisher: Journal of the Chemical Society : Faraday Transaction - I. The Chemical Society, London. 1974, 70 (11)
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.
URI: http://dspace.bits-pilani.ac.in:8080/jspui/handle/123456789/17873
Appears in Collections:Journal Articles (before-1995)

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