
Canted Antiferromagnetism: Hematite
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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 obtain...
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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 obtain...
Read more
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