Visible to the public Modeling the Role of the Buildup of Magnetic Charges in Low Anisotropy Polycrystalline Materials

TitleModeling the Role of the Buildup of Magnetic Charges in Low Anisotropy Polycrystalline Materials
Publication TypeJournal Article
Year of Publication2018
AuthorsElbidweihy, H., Arrott, A. S., Provenzano, V.
JournalIEEE Transactions on Magnetics
Volume54
Pagination1–5
Date Publishednov
ISSN0018-9464
KeywordsAnisotropic magnetoresistance, anisotropy field, composability, compositionality, cyber physical systems, demagnetisation, gadolinium, grain boundaries, Internet of Things, low anisotropy polycrystalline materials, Magnetic anisotropy, magnetic charges, Magnetic Remanence, magnetic susceptibility, Magnetization, magneto-thermal characteristics, magnetocaloric effects, Magnetometers, negative-field cooling, Perpendicular magnetic anisotropy, phenomenological energy barriers, polycrystalline gadolinium, polymer structure, positive-field warming, pubcrawl, remanence, remnant magnetization, Resiliency, Soft magnetic materials, soft-magnetic materials, Stoner-Wohlfarth-type model, Stoner–Wohlfarth model, susceptibility, Temperature measurement, thermal relaxation
Abstract

A Stoner-Wohlfarth-type model is used to demonstrate the effect of the buildup of magnetic charges near the grain boundaries of low anisotropy polycrystalline materials, revealed by measuring the magnetization during positive-field warming after negative-field cooling. The remnant magnetization after negative-field cooling has two different contributions. The temperature-dependent component is modeled as an assembly of particles with thermal relaxation. The temperature-independent component is modeled as an assembly of particles overcoming variable phenomenological energy barriers corresponding to the change in susceptibility when the anisotropy constant changes its sign. The model is applicable to soft-magnetic materials where the buildup of the magnetic charges near the grain boundaries creates demagnetizing fields opposing, and comparable in magnitude to, the anisotropy field. The results of the model are in qualitative agreement with published data revealing the magneto-thermal characteristics of polycrystalline gadolinium.

URLhttps://ieeexplore.ieee.org/document/8383699
DOI10.1109/TMAG.2018.2832294
Citation Keyelbidweihy_modeling_2018