Open AccessEffects of Transition Zone on Magnetic Properties of Low Temperature Oxidation of Magnetite Particle:Comparison of Experiment and Micromagnetic Modeling
Author(s) -
Kunpeng Ge,
Wyn Williams
Publication year - 2020
Publication title -
iop conference series. materials science and engineering
Language(s) - English
Resource type - Journals
eISSN - 1757-899X
pISSN - 1757-8981
DOI - 10.1088/1757-899x/840/1/012007
Subject(s) - remanence , materials science , magnetite , coercivity , magnetic hysteresis , hysteresis , saturation (graph theory) , micromagnetics , single domain , microstructure , core (optical fiber) , condensed matter physics , magnetization , magnetic domain , nuclear magnetic resonance , composite material , magnetic field , metallurgy , physics , mathematics , quantum mechanics , combinatorics
A relationship of hysteresis parameters and oxidation of ultrafine magnetic particles on both experimental measurements and micromagnetic simulations is obtained through a step-by-step oxidation of magnetite. Numerical simulations of hysteresis loop and microstructure of a core-shell geometry with transition zone using a multi-layer structure show two categories of behaviour for magnetic grains during oxidation. First, the SD (Single Domain, 130 nm) particles remain unchanged ratio of saturation remanence to saturation magnetization ( M rs / M s ), and slightly decreased coercivity ( B c ) during oxidation. Second, the fine SV particles (80 nm to 120 nm), the hysteresis parameters respectively increase and dramatic decrease at the early and late stage of oxidation, and the micromagnetic behaviors vary significantly. Finally the hysteresis parameters of larger SV particles remain nearly unchanged during oxidation. The predicted magnetic properties for the core-shell model exhibit better agreement with experimental data than that of previously used core-shell geometry (a stoichiometric core surrounded by an oxidized shell). It indicates that the magnetic properties of partially oxidized magnetic grains are controlled by the multi-layer coupling effects and can record paleomagnetic signals.