1995•Journal of Geophysical Research AtmospheresRequires access

Simulation of magnetic hysteresis in pseudo‐single‐domain grains of magnetite

Wyn Williams, David J. Dunlop

Open publisher page 84 citations

Abstract

Magnetic hysteresis has been simulated in grains of magnetite for the size range 0.1–0.7 μm. This was achieved using an unconstrained three‐dimensional micromagnetic model of single grains of magnetite with cubic magnetocrystalline anisotropy. Hysteresis loops were obtained for fields applied along both the easy and hard magnetocrystalline axes. Both discrete (Barkhausen) jumps and gradual changes in the magnetic structure are seen, and the reversal of the magnetization can be followed from near saturation in a normal field to a similar state in a reverse field. Predictions of coercivity agree well with published experimental data for unstressed cubic grains of magnetite.

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What this paper is about

Magnetic hysteresis has been simulated in grains of magnetite for the size range 0.1–0.7 μm. This was achieved using an unconstrained three‐dimensional micromagnetic model of single grains of magnetite with cubic magnetocrystalline anisotropy. Hysteresis loops were obtained for fields applied along both the easy and hard magnetocrystalline axes. Both discrete (Barkhausen) jumps and gradual changes in the magnetic structure are seen, and the reversal of the magnetization can be followed from near saturation in a normal field to a similar state in a reverse field. Predictions of coercivity agree well with published experimental data for unstressed cubic grains of magnetite.

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Available abstract

Magnetic hysteresis has been simulated in grains of magnetite for the size range 0.1–0.7 μm. This was achieved using an unconstrained three‐dimensional micromagnetic model of single grains of magnetite with cubic magnetocrystalline anisotropy. Hysteresis loops were obtained for fields applied along both the easy and hard magnetocrystalline axes. Both discrete (Barkhausen) jumps and gradual changes in the magnetic structure are seen, and the reversal of the magnetization can be followed from near saturation in a normal field to a similar state in a reverse field. Predictions of coercivity agree well with published experimental data for unstressed cubic grains of magnetite.

Key concepts: Magnetocrystalline anisotropy, Magnetite, Coercivity, Materials science, Single domain, Condensed matter physics, Magnetic hysteresis, Hysteresis

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