Magnetic ordering and spin structure in Ca-bearing clinopyroxenes CaM2+(Si, Ge)2O6, M = Fe, Ni, Co, Mn

被引:38
|
作者
Redhammer, Guenther J. [1 ]
Roth, Georg [2 ]
Treutmann, Werner [3 ]
Paulus, Werner [4 ]
Andre, Gilles [5 ]
Pietzonka, Clemens [6 ]
Amthauer, Georg [1 ]
机构
[1] Salzburg Univ, Div Mineral, Dept Engn Math & Phys, A-5020 Salzburg, Austria
[2] Rhein Westfal TH Aachen, Inst Crystallog, D-52056 Aachen, Germany
[3] Univ Marburg, Inst Mineral, D-35032 Marburg, Germany
[4] Univ Rennes 1, LCSIM UMR6511, F-35042 Rennes, France
[5] CEA Saclay, CNRS, CEA, UMR12,Lab Leon Brillouin, F-91191 Gif Sur Yvette, France
[6] Univ Marburg, Dept Chem, D-35032 Marburg, Germany
关键词
Clinopyroxene; Hedenbergite; Magnetic properties; Spin structure; Neutron diffraction; SQUID magnetometry;
D O I
10.1016/j.jssc.2008.08.014
中图分类号
O61 [无机化学];
学科分类号
070301 ; 081704 ;
摘要
The compounds CaFeSi2O6 (hedenbergite), CaNiGe2O6, CaCoGe2O6 and CaMnGe2O6 have been synthesized by hydrothermal or ceramic sintering techniques and were Subsequently characterized by SQUID magnetometry and powder neutron diffraction in order to determine the magnetic properties and the spin structure at low temperature. All four compounds reveal the well-known clinopyroxene structure-type with monoclinic symmetry, space group C2/c, Z = 4 at all temperatures investigated. Below 35 K hedenbergite shows a ferromagnetic (FM) coupling of spins within the infinite MI chains of edge-sharing octahedra. This FM coupling dominates an antiferromagnetic (AFM) coupling between neighbouring chains. The magnetic moments lie within the a-c plane and form an angle of 43 degrees with the crystallographic a-axis. Magnetic ordering in CaFeSi2O6 causes significant discontinuities in lattice parameters, Fe-O bond lengths and interatomic Fe-Fe distances through the magnetic phase transition, which could be detected from the Rietveld refinements of powder neutron diffraction data. CaCoGe2O6 and CaNiGe2O6 show magnetic ordering below 18 K, the spin structures are similar to the one in hedenbergite with an FM Coupling within and an AFM coupling of spins between the MI chains. The moments lie within the a-c plane. The paramagnetic Curie temperature, however, decreases from CaFeSi2O6, (+40.2 K) to CaCoGe2O6 (+20.1 K) and CaNiGe2O6 (-13.4 K), suggesting an altered interplay between the concurring AFM and FM interaction in and between the MI chains. CaMnGe2O6 finally shows an AFM ordering below 11 K. Here the magnetic moments are mainly oriented along the a-axis with a small tilt out from the a-c plane. (C) 2008 Elsevier Inc. All rights reserved.
引用
收藏
页码:3163 / 3176
页数:14
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