Synthetic Zn-ferrite (ideally ZnFe2O4; mineral name: franklinite) was studied up to 37 GPa, by X-ray powder diffraction at ESRF (Grenoble, France), on the ID9 beamline; high pressure was achieved by means of a DAC. The P-V equation of state of franklinite was investigated using the Birch-Murnaghan function, and the elastic properties thus inferred [K0 = 166.4(± 3.0) GPa K′0 = 9.3(± 0.6) K″0 = -0.22 GPa-1] are compared with earlier determinations for MgA1-spinel and magnetite. The structural behaviour of Zn-ferrite as a function of pressure was studied by Rietveld refinements, and interpreted in the light of a phase transition from spinel to either CaTi2O4- or MnFe2O4-like structure; this transformation occurs above 24 GPa.
Phase transition of synthetic zinc ferrite spinel (ZnFe2O4) at high pressure, from synchrotron X-ray powder diffraction. / D. Levy, A. Pavese, M. Hanfland. - In: PHYSICS AND CHEMISTRY OF MINERALS. - ISSN 0342-1791. - 27:9(2000 Nov), pp. 638-644.
|Titolo:||Phase transition of synthetic zinc ferrite spinel (ZnFe2O4) at high pressure, from synchrotron X-ray powder diffraction.|
PAVESE, ALESSANDRO (Secondo)
|Settore Scientifico Disciplinare:||Settore GEO/06 - Mineralogia|
|Data di pubblicazione:||nov-2000|
|Digital Object Identifier (DOI):||http://dx.doi.org/10.1007/s002690000117|
|Appare nelle tipologie:||01 - Articolo su periodico|