CATION ORDERING IN MgTi2O5 (KARROOITE): PROBING TEMPERATURE DEPENDENT EFFECTS WITH NEUTRONS

dc.contributor.authorLennie A.R.
dc.contributor.authorHenderson M.B.
dc.contributor.authorKnight K.S.
dc.date.accessioned2026-04-04T05:19:13Z
dc.date.issued2007
dc.description.abstractMgTi2O5 (karrooite) exhibits cation exchange between the two non-equivalent octahedral M1 and M2 sites. The temperature dependence of Ti-Mg disorder has been determined using in situ time-of-flight powder neutron diffraction to establish the cation population of each site. The equilibrium Ti-Mg exchange commences above 700-800 °C, and continues up to 1300 °C. At ~1350 °C MgTi2O5 appears to undergo a reversible, displacive phase transition, although the structure can still be refined in space group 63. This transition shows discontinuities in the degree of order, the c cell parameter, and in the M-O bond lengths, quadratic elongation, and bond angle variance for the M1 octahedron, which becomes pseudo-tetrahedral. By contrast, the M2 octahedron shows no significant change. An Arrhenius plot exhibits linear behavior from 750-1300 °C, gives an exchange enthalpy of ordering of 33.6 kJ/mol, and a value of 10.7 kJ/mol for the entropy of disordering. A value of 5.92 cm3/mol is deduced for the ΔV of the high-temperature reaction of geikielite (MgTiO3) + rutile (TiO2) to form fully disordered MgTi2O5 at an extrapolated temperature of 1860 °C.
dc.identifierhttps://elibrary.ru/item.asp?id=14662857
dc.identifier.citationAmerican Mineralogist, 2007, 92, 7, 1165-1180
dc.identifier.doi10.2138/am.2007.2322
dc.identifier.issn0003-004X
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/52195
dc.subjectCRYSTAL STRUCTURE
dc.subjectGEIKIELITE
dc.subjectHIGH-TEMPERATURE
dc.subjectKARROOITE
dc.subjectNEUTRON DIFFRACTION
dc.subjectORDER-DISORDER
dc.subjectOXIDES
dc.subjectRUTILE
dc.titleCATION ORDERING IN MgTi2O5 (KARROOITE): PROBING TEMPERATURE DEPENDENT EFFECTS WITH NEUTRONS
dc.typeСтатья

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