Hysteresis and coercivity of hematite

Abstract

In room-temperature hysteresis, 14 submicron hematites (0.12-0.45 μm) had large coercive forces Hc (150-350 mT), while 22 natural 1-5.5 mm hematite crystals had Hc = 0.8-23 mT (basal-plane measurements). Single-domain (SD) and multidomain (MD) hematites owe their high Hc mainly to magnetoelastic anisotropy, caused in fine particles by internal strains and in large crystals by defects like dislocations, with a smaller contribution by triaxial magnetocrystalline anisotropy. A strong correlation between Hc and the defect moment Md measured below hematite's Morin transition also favors magnetoelastic control. Saturation remanence/saturation magnetization ratios Mrs/Ms and coercivity ratios Hcr/Hc (Hcr is remanent coercive force) are distinctive: Mrs/Ms = 0.5-0.9, H cr/Hc = 1.02-1.17 for MD hematites; Mrs/M s = 0.5-0.7, Hcr/Hc = 1.45-1.62 for SD hematites. In high-temperature (20-690C) hysteresis, Hc(T) ~ M s(T) to a power 1.8-2.4 above 385C. Magnetoelastic wall pinning by crystal defects is thus more likely than control by domain nucleation which depends on magnetocrystalline anisotropy. Our results compare well with existing Hc vs. crystal size d data. A suggested peak in Hc around 15 μm and a proposed slope change around 100 μm are both questionable. Using only near-saturation data, Hc varies continuously as d -0.61 from ≈0.1 μm to 2 mm. The SD threshold size d0 may be >15 μm but there is no strong evidence that d0 ≈100 μm. Direct domain observations are needed to settle the question. Augmented data sets for Hc and Mrs vs. d show that SD hematite is increasingly affected by thermal fluctuations below ≈0.3 μm and generally confirm a superparamagnetic threshold size ds of 0.025-0.03 μm. ©2014. American Geophysical Union. All Rights Reserved.