STUDY OF CATION ORDER-DISORDER IN MGAL2O4 SPINEL BY IN SITU NEUTRON DIFFRACTION UP TO 1600 K AND 3.2 GPA

dc.contributor.authorMéducin F.
dc.contributor.authorRedfern S.A.T.
dc.contributor.authorStone H.J.
dc.contributor.authorTucker M.G.
dc.contributor.authorDove M.T.
dc.contributor.authorLe Godec Y.
dc.contributor.authorMarshall W.G.
dc.date.accessioned2022-04-18T05:17:17Z
dc.date.available2022-04-18T05:17:17Z
dc.date.issued2004
dc.description.abstractThe temperature-dependence of the cation distribution in synthetic spinel (MgAl2O4) was investigated using in situ time-of-flight neutron powder diffraction at ISIS, the pulsed-neutron source at the Rutherford Appleton Laboratory. Neutron diffraction patterns of stoichiometric MgAl2O4 were collected on heating from room temperature to ∼1600 K at pressures of ∼2.6 GPa. The cation distribution was determined directly from site occupancies obtained by Rietveld refinement. The equilibrium non-convergent ordering was analyzed using the OʼNeill-Navrotsky (1983) thermodynamic model, which fits the observed behavior well over the temperature range of the measurements. Fitting the data between 790 and 1600 K yields α = 31(6) kJ/mol and β = -20(13) kJ/mol in the expression for the free energy of ordering. The high-pressure temperature-dependent behavior, as compared to equivalent ambient-pressure behavior, demonstrates that disordering occurs to a much greater extent in MgAl2O4 at high pressure and that pressure favors disordering toward the inverse structure.
dc.identifierhttps://www.elibrary.ru/item.asp?id=14537005
dc.identifier.citationAmerican Mineralogist, 2004, 89, 7, 981-986
dc.identifier.issn0003-004X
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/37248
dc.subjectspinel
dc.titleSTUDY OF CATION ORDER-DISORDER IN MGAL2O4 SPINEL BY IN SITU NEUTRON DIFFRACTION UP TO 1600 K AND 3.2 GPA
dc.typeСтатья

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