Canted Antiferromagnetism

Hematite

By: Allan H Morrish

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Hardcover | 1 January 1995

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208 Pages

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22.86 x 17.15 x 1.91

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Hematite (α-Fe2O3), the stable oxide of iron, is a major constituent of soils, rocks and the earth's crust. It has unique magnetic properties that make it the prototype for the class of materials known as canted antiferromagnets.This book has no equivalent. The mean-field theory is treated in detail, and thus the book is a useful text for students mastering this general method. Information obtained by a wide variety of experimental methods is provided. These techniques include x-ray and neutron diffraction; electron magnetic resonance; Mössbauer spectroscopy; and thermal, optical, electrical and elastic measurements.

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Preface
Introduction	p. 1
Crystal Growth and Characterization of Hematite	p. 3
Material Preparation	p. 3
X-ray Diffraction Studies, Crystal Structure	p. 15
Neutron Diffraction; Magnetic Structure	p. 20
Theory	p. 25
The Terms of the Thermodynamic Free Energy	p. 25
Stability Relations and the Equations of Motion	p. 28
The Phase Transitions for Hematite	p. 32
Magnetization and Susceptibility; Phase Transitions	p. 51
Temperature-driven Phase Transitions	p. 51
Field-driven Phase Transitions	p. 63
Pressure-driven Phase Transitions	p. 71
Heat Capacity and Other Thermodynamic Quantities	p. 76
Electrical Transport and Optical Properties	p. 81
Elastic and Magnetoelastic Interactions	p. 86
Electron Magnetic Resonance	p. 92
WFS Electron Resonance	p. 92
AFS Electron Resonance	p. 107
Hyperfine Interactions	p. 125
Small Particles and Thin Films; Surface and Rock Magnetism	p. 129
Domains; Magnetization Processes	p. 134
Doped [alpha]-Fe[subscript 2]O[subscript 3]	p. 148
References	p. 157
Author Index	p. 174
Subject Index	p. 187
Table of Contents provided by Blackwell. All Rights Reserved.

Canted Antiferromagnetism

Hematite

At a Glance

Hardcover

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How to return your order

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