We report a detailed study on the magnetic properties of the pyroxene series M 2 M 1Si 2 O 6 , with M 2 = Ca and M 1 = Mg, where magnesium and then calcium are progressively substituted by cobalt. For cobalt site occupancy larger than 0.7 at the M 1 site, a collinear antiferromagnetic phase is detected for T < T N1 = 12 K with a monodimensional character (i.e. M 1 site intra-chain order parallel to c axis). Moreover the magnetization easy axis has been estimated to lie roughly along the [1 0 1] direction. Cobalt content ?0.5 at the M 2 site (overall content 1.5) determines the formation of a new independent antiferromagnetic order with higher N?el temperature, involving only the M 2 site intra-chain interactions. The incoming M 2 site order is accompanied by a lowering of the space symmetry which yields to a weakly ferromagnetic resultant due to spin canted distribution of the magnetic moments either along the M 1 or M 2 chains. Furthermore, metamagnetic transitions are observed for both M 1 and M 2 site intra-chain orders at relatively low critical magnetic fields, around 2 T, suggesting that this series of pyroxenes can be used as a model system for investigating the fundamental aspects of magnetism in the matter.

A comprehensive study of the magnetic properties of the pyroxenes series CaMgSi2O6-Co2S2O6 as a function of Co content

Davide Delmonte;Francesco Mezzadri;Edmondo Gilioli;
2018

Abstract

We report a detailed study on the magnetic properties of the pyroxene series M 2 M 1Si 2 O 6 , with M 2 = Ca and M 1 = Mg, where magnesium and then calcium are progressively substituted by cobalt. For cobalt site occupancy larger than 0.7 at the M 1 site, a collinear antiferromagnetic phase is detected for T < T N1 = 12 K with a monodimensional character (i.e. M 1 site intra-chain order parallel to c axis). Moreover the magnetization easy axis has been estimated to lie roughly along the [1 0 1] direction. Cobalt content ?0.5 at the M 2 site (overall content 1.5) determines the formation of a new independent antiferromagnetic order with higher N?el temperature, involving only the M 2 site intra-chain interactions. The incoming M 2 site order is accompanied by a lowering of the space symmetry which yields to a weakly ferromagnetic resultant due to spin canted distribution of the magnetic moments either along the M 1 or M 2 chains. Furthermore, metamagnetic transitions are observed for both M 1 and M 2 site intra-chain orders at relatively low critical magnetic fields, around 2 T, suggesting that this series of pyroxenes can be used as a model system for investigating the fundamental aspects of magnetism in the matter.
2018
Istituto dei Materiali per l'Elettronica ed il Magnetismo - IMEM
antiferromagnetism
spin canting
metamagnetic transition
weak ferromagnetism
1D magnetic order
pyroxenes
mineralogy
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/20.500.14243/373787
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