4.6 Article

Entropy change linked to the magnetic field induced Morin transition in Hematite nanoparticles

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APPLIED PHYSICS LETTERS
卷 100, 期 6, 页码 -

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AMER INST PHYSICS
DOI: 10.1063/1.3682084

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cooling; entropy; ferromagnetic materials; iron compounds; magnetic moments; magnetic particles; magnetisation; Morin temperature; nanomagnetics; nanoparticles; spin systems

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The most stable form of iron oxide is Hematite (alpha-Fe2O3), which has interesting electronic, catalytic, and magnetic properties showing size dependent characteristics. At room temperature, Hematite is weakly ferromagnetic with a rhombohedral corundum structure. Upon cooling, the structure undergoes a first order spin reorientation, in which the net magnetic moment is lost. This transition is called the Morin transition. In this work, the first order Morin transition has been analyzed as a function of the temperature and applied magnetic field in Hematite nanoparticles. The magnetization was measured in the temperature range of the transformation at different applied magnetic fields to evaluate the entropy change linked to the Morin transition. The magnetic field promotes a shift of the transformation temperature. The change of entropy has been estimated on the basis of Clausius-Clapeyron type equation. (C) 2012 American Institute of Physics. [doi:10.1063/1.3682084]

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