• journal_title：American Mineralogist
• Contributor：Fabienne Méducin ; Simon A.T. Redfern ; Yann Le Godec ; Howard J. Stone ; Matt G. Tucker ; Martin T. Dove ; William G. Marshall
• Publisher：Mineralogical Society of America
• Date：2004-
• Format：text/html
• Language：en
• journal_abbrev：American Mineralogist
• issn：0003-004X
• volume：89
• issue：7
• firstpage：981
• section：Articles

The 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 O’Neill-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.