Thermal behaviour of pyrope at 1000 and 1100 degrees C: mechanism of Fe2+ oxidation and decomposition model
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61989592%3A15410%2F03%3A00001545" target="_blank" >RIV/61989592:15410/03:00001545 - isvavai.cz</a>
Alternative codes found
RIV/68145535:_____/03:15033061
Result on the web
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DOI - Digital Object Identifier
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Alternative languages
Result language
angličtina
Original language name
Thermal behaviour of pyrope at 1000 and 1100 degrees C: mechanism of Fe2+ oxidation and decomposition model
Original language description
The mechanism of thermally induced oxidation of Fe2+ from natural pyrope has been studied at 1000 and 1100 degreesC using Fe-57 Mossbauer spectroscopy in conjunction with XRD, XRF, AFM, QELS, TG, DTA and electron microprobe analyses. At 1000 degreesC, the non-destructive oxidation of Fe2+ in air includes the partial stabilization of Fe3+ in the dodecahedral 24c position of the garnet structure and the simultaneous formation of hematite particles (15-20 nm). The incorporation of the magnesium ions to thehematite structure results in the suppression of the Morin transition temperature to below 20 K. The general garnet structure is preserved during the redox process at 1000 degreesC, in accordance with XRD and DTA data. At 1100 degreesC, however, oxidative conversion of pyrope to the mixed magnesium aluminium iron oxide, Fe-orthoenstatite and cristoballite was observed. During this destructive decomposition, Fe2+ is predominantly oxidized and incorporated into the spinel structure of Mg(
Czech name
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Czech description
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Classification
Type
J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)
CEP classification
BM - Solid-state physics and magnetism
OECD FORD branch
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Result continuities
Project
<a href="/en/project/GA202%2F00%2F0982" target="_blank" >GA202/00/0982: The study of the formation and transformations of the different iron(III)oxide forms during the thermal decom-position of iron salts</a><br>
Continuities
Z - Vyzkumny zamer (s odkazem do CEZ)
Others
Publication year
2003
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
PHYSICS AND CHEMISTRY OF MINERALS
ISSN
0342-1791
e-ISSN
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Volume of the periodical
30
Issue of the periodical within the volume
10
Country of publishing house
DE - GERMANY
Number of pages
8
Pages from-to
620-627
UT code for WoS article
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EID of the result in the Scopus database
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