Canted antiferromagnetism : Hematite

Hematite ( -F2O3), 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 de...

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Bibliografski detalji
Glavni autor: Morrish, Allan Henry
Format: Knjiga
Jezik:Undetermined
Izdano: Singapore World Scientific 1994
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Thư viện lưu trữ: Trung tâm Học liệu Trường Đại học Cần Thơ
Opis
Sažetak:Hematite ( -F2O3), 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; Mossbauer spectroscopy; and thermal, optical, electrical and elastic measurements