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The effect of flake size on the Mössbauer spectrum of graphite ferrous chloride

✍ Scribed by J.G. Hooley; J.R. Sams; B.V. Liengme


Publisher
Elsevier Science
Year
1970
Tongue
English
Weight
458 KB
Volume
8
Category
Article
ISSN
0008-6223

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✦ Synopsis


The thermal decomposition of graphite ferric chloride produces graphite ferrous chloride with two quadrupole splittings for iron. One of these is the same as the single splitting in bulk FeCl,. The other is larger and has an intensity, relative to the normal splitting, which increases with flake thickness. Both have the same isomer shift as in bulk FeCl,. The extra doublet is believed to be caused by the presence of Cl, trapped in certain spaces in the flake. This modifies the electric field gradient of the FeCl, in those regions. The normal doublet is believed to come from FeCI, in layer spaces containing no trapped Clz. Both the Mossbauer and analytical data show that the thermal stability of FeCl, intercalated between the carbon layers IS less than that of bulk FeCl,.


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