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Temperature, magnetic field, and pressure dependence of the crystal and magnetic structures of the magnetocaloric compound Mn1.1 Fe0.9 (P0.8 Ge0.2)

Liu, DM, Huang, QZ, Yue, M, Lynn, JW, Liu, LJ, Chen, Ying (Ian), Wu, ZH and Zhang, JX 2009, Temperature, magnetic field, and pressure dependence of the crystal and magnetic structures of the magnetocaloric compound Mn1.1 Fe0.9 (P0.8 Ge0.2), Physical Review B - Condensed Matter and Materials Physics, vol. 80, no. 17, doi: 10.1103/PhysRevB.80.174415.

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Title Temperature, magnetic field, and pressure dependence of the crystal and magnetic structures of the magnetocaloric compound Mn1.1 Fe0.9 (P0.8 Ge0.2)
Author(s) Liu, DM
Huang, QZ
Yue, M
Lynn, JW
Liu, LJ
Chen, Ying (Ian)ORCID iD for Chen, Ying (Ian) orcid.org/0000-0002-7322-2224
Wu, ZH
Zhang, JX
Journal name Physical Review B - Condensed Matter and Materials Physics
Volume number 80
Issue number 17
Publisher The American Physical Society
Publication date 2009-11-17
ISSN 1098-0121
1550-235X
Summary Neutron powder-diffraction studies of the crystal and magnetic structures of the magnetocaloric compound Mn1.1 Fe0.9 (P0.8 Ge0.2) have been carried out as a function of temperature, applied magnetic field, and pressure. The data reveal that there is only one transition observed over the entire range of variables explored, which is a combined magnetic and structural transformation between the paramagnetic (PM) and ferromagnetic phases (Tc ≈255 K for this composition). The structural part of the transition is associated with an expansion of the hexagonal unit cell in the direction of the a and b axes and a contraction of the c axis as the FM phase is formed, which originates from an increase in the intralayer metal-metal bond distance. The application of pressure is found to have an adverse effect on the formation of the FM phase since pressure opposes the expansion of the lattice and hence decreases Tc. The application of a magnetic field, on the other hand, has the expected effect of enhancing the FM phase and increasing Tc. We find that the substantial range of temperature/field/pressure coexistence of the PM and FM phases observed is due to compositional variations in the sample. In situ high-temperature diffraction measurements were carried out to explore this issue, and reveal a coexisting liquid phase at high temperatures that is the origin of this variation. We show that this range of coexisting phases can be substantially reduced by appropriate heat treatment to improve the sample homogeneity. © 2009 The American Physical Society.
DOI 10.1103/PhysRevB.80.174415
Field of Research 02 Physical Sciences
03 Chemical Sciences
HERDC Research category CN.1 Other journal article
Persistent URL http://hdl.handle.net/10536/DRO/DU:30101966

Document type: Journal Article
Collection: Institute for Frontier Materials
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