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        <identifier>oai:www.ideals.illinois.edu:2142/25794</identifier>
        <datestamp>2023-07-10</datestamp>
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        <thesis xmlns="http://www.ndltd.org/standards/metadata/etdms/1.1/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:dc="http://purl.org/dc/elements/1.1/" xsi:schemaLocation="http://www.ndltd.org/standards/metadata/etdms/1.1/ http://www.ndltd.org/standards/metadata/etdms/1.1/etdms11.xsd http://purl.org/dc/elements/1.1/ http://www.ndltd.org/standards/metadata/etdms/1.1/etdmsdc.xsd">
          <dc:contributor>Drickamer, H.G.</dc:contributor>
          <dc:creator>Christoe, Charles William</dc:creator>
          <dc:date>2011-07-13T15:51:22Z</dc:date>
          <dc:date>2011-07-13T15:51:22Z</dc:date>
          <dc:date>10000-01-01</dc:date>
          <dc:date>1969</dc:date>
          <dc:description>Using the inter-atomic distance as a parameter, Mossbauer
spectra have been observed for the three isomorphic ferric compounds
K3FeF6, Na3
FeF6 and (NH4)3FeF6' In addition, the compressibility and
the pressure dependence of cia were determined by X-ray diffraction for
the ferrous compound FeF2 , In all of these compounds, the local
environment of the iron ion is a slightly distorted octahedron of
fluoride ions. A detailed analysis was made of the quadrupole pplitting
of the Mossbauer spectra for both the ferrous and the ferric salts.
The analysis proceeded along two lines: the usual pointcharge
approximation and a covalent approximation based upon configuration
interaction. Although the quadrupole splitting increased with pressure
in the ferric case--whereas it decreased in the ferrous case--the local
crystalline distortions were shown to decrease in both cases when the
pressure exceeded about fifty kilobars. The covalent contribution was
shown to be a significant portion of the total field gradient at the
iron sites for the ferric compounds; that is, it is of the same order
of magnitude as the gradient produced by the distorted octahedron.
For the ferrous compound, the covalent contribution was shown to be
negligible compared to the gradient produced by the ferrous valence
electron, although it did tend to diminish the latter effect. Both
the point-charge and the covalent models predict zero quadrupole
splitting in the event of a truly regular octahedral (or tetrahedral)
iron environment.</dc:description>
          <dc:description>Submitted by Carolyn Mead (cmead2@illinois.edu) on 2011-07-13T15:51:22Z
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  Previous issue date: 1969</dc:description>
          <dc:description>Restriction data tranferred 2014-07-01T11:32:49-05:00
Original Data
Group with Access UIUC Users [automated]
Release Date: none
Reason: Thesis</dc:description>
          <dc:description>Item marked as restricted to the 'UIUC Users [automated]' Group (id=2) by Carolyn Mead (cmead2@illinois.edu) on 2011-07-13T15:51:22Z
Item is restricted indefinitely.</dc:description>
          <dc:description>Thesis</dc:description>
          <dc:description>U of I Only</dc:description>
          <dc:identifier>6074149</dc:identifier>
          <dc:identifier>http://hdl.handle.net/2142/25794</dc:identifier>
          <dc:language>en</dc:language>
          <dc:rights>1969 Charles William Christoe</dc:rights>
          <dc:subject>quadrupole interaction</dc:subject>
          <dc:subject>iron-fluoride compounds</dc:subject>
          <dc:subject>inter-atomic distance</dc:subject>
          <dc:subject>Mossbauer spectra</dc:subject>
          <dc:subject>compressibility</dc:subject>
          <dc:subject>x-ray diffraction</dc:subject>
          <dc:title>The effect of high pressure on the quadrupole interaction in iron-fluorine compounds</dc:title>
          <dc:type>Dissertation / Thesis</dc:type>
          <dc:type>text</dc:type>
          <degree>
            <department>Physics</department>
            <discipline>Physics</discipline>
            <disciplineCode>University of Illinois at Urbana-Champaign</disciplineCode>
            <level>Dissertation</level>
            <name>Ph.D.</name>
          </degree>
        </thesis>
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