Magnetic Domain State and Anisotropy in Hematite (<i>α</i>‐Fe<sub>2</sub>O<sub>3</sub>) From First‐Order Reversal Curve Diagrams
Andrew P. Roberts, Xiang Zhao, Pengxiang Hu, Alexandra Abrajevitch, Yen‐Hua Chen, R. J. Harrison, David Heslop, Zhaoxia Jiang, Jinhua Li, Qingsong Liu, Adrian R. Muxworthy, Hirokuni Oda, Hugh O’Neill, Brad Pillans, Tetsuro Sato
Abstract
Abstract Hematite carries magnetic signals of interest in tectonic, paleoclimatic, paleomagnetic, and planetary studies. First‐order reversal curve (FORC) diagrams have become an important tool for assessing the domain state of, and magnetostatic interactions among, magnetic particles in such studies. We present here FORC diagrams for diverse hematite samples, which provide a catalog for comparison with other studies and explain key features observed for hematite. Ridge‐type signatures typical of uniaxial single‐domain particle assemblages and “kidney‐shaped” FORC signatures, and combinations of these responses, occur commonly in natural and synthetic hematite. Asymmetric features that arise from the triaxial basal plane anisotropy of hematite contribute to vertical spreading in kidney‐shaped FORC distributions and are intrinsic responses even for magnetostatically noninteracting particles. The dominant FORC distribution type in a sample (ridge, kidney‐shaped, or mixture) depends on the balance between uniaxial/triaxial switching. The identified signals explain magnetization switching and anisotropy features that are intrinsic to the magnetic properties of hematite and other materials with multiaxial magnetic anisotropy.