Cation distribution in synthetic zinc ferrite (Zn0.97Fe2.02O4) from in situ high-temperature neutron powder diffraction

被引:39
|
作者
Pavese, A
Levy, D
Hoser, A
机构
[1] Univ Milan, Dipartimento Sci Terra, I-20133 Milan, Italy
[2] Natl Res Council, Ctr Studio Geodinam Alpina & Quaternaria, I-20133 Milan, Italy
[3] European Synchrotron Radiat Facil, F-38043 Grenoble, France
[4] Hahn Meitner Inst Kernforsch Berlin GmbH, BENSC, Berlin Neutron Scattering Ctr, D-43100 Berlin, Germany
关键词
D O I
10.2138/am-2000-1020
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Neutron powder diffraction experiments at high temperature (300-1600 K) were performed at BENSC (Berlin, D), on synthetic Zn0.97Fe2.02O4, to investigate the cation partitioning of Zn and Fe over the tetrahedral and octahedral sites as a function of T. The data analysis combined Rietveld structure refinements with minimization techniques. The thermodynamic behavior of the thermally activated order-disorder transformation occurring in Zn-ferrite was interpreted by the O'Neill-Navrotsky model (alpha = 49.3 +/- 0.4 and beta = -31.6 +/- 2.0 kJ/mol) and by the equilibrium Landau theory. We obtain lambda(2) = 2.813 +/- 0.002/K, T-c = 1022 +/- 37 K using a "pure" Landau approach, and h = -1.164 +/- 0.002 kJ/mol, c = 9.868 +/- 0.06 kJ/mol, T-c = -742 +/- 10 K, if the configurational contribution to entropy is explicitly accounted. The results are in agreement with the earlier powder XRD work of O'Neill (1992) on quenched specimens, but extend the temperature over which measurements were obtained to 1600 K.
引用
收藏
页码:1497 / 1502
页数:6
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