Proceedings of the International School of Physics "Enrico Fermi.", Volume 70N. Zanichelli, 1978 - Nuclear physics |
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Page 104
The degree of anisotropy of these lowest levels thus is a clear indication for the
magnitude of anisotropic phenomena such as magnetic anisotropy ,
magnetostriction , or relaxation mechanisms . If we apply the Hamiltonians given
in sect .
The degree of anisotropy of these lowest levels thus is a clear indication for the
magnitude of anisotropic phenomena such as magnetic anisotropy ,
magnetostriction , or relaxation mechanisms . If we apply the Hamiltonians given
in sect .
Page 107
The two lowest levels behave like a magnetic doublet , which , in addition , is well
separated from the higher levels . In contrast to the Co2 + ions , near crossings of
the lowest levels , which induce sharp peaks in the field for ferromagnetic ...
The two lowest levels behave like a magnetic doublet , which , in addition , is well
separated from the higher levels . In contrast to the Co2 + ions , near crossings of
the lowest levels , which induce sharp peaks in the field for ferromagnetic ...
Page 108
The rare - earth ions give rise to the highest anisotropies in garnets , which is
reflected by their energy level diagram . A very typical example is the terbium ion
. The angular variation of its energy levels shows a pronounced structure , as can
...
The rare - earth ions give rise to the highest anisotropies in garnets , which is
reflected by their energy level diagram . A very typical example is the terbium ion
. The angular variation of its energy levels shows a pronounced structure , as can
...
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Contents
Magnetooptical rotation | 2 |
Rareearth iron garnets | 5 |
Bubble translation | 8 |
Copyright | |
35 other sections not shown
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Common terms and phrases
absorption angle anisotropy Appl applied assumed axis Bloch lines bubble calculated causes centres composition consider constants contribution corresponding coupling crystal cubic curve dependence determined direction discussed distribution domain effects electron energy equation exchange experiment experimental expression Fe2+ Fe3+ ions ferrimagnetic field film function GELLER give given ground increases interaction iron garnets Journ lattice levels light magnetic field magnitude material measurements mode moments motion normal observed obtained occur octahedral orientation parallel parameter photoinduced Phys plane polarization position properties rare-earth ions region relation relaxation represents resonance respectively rotation sample shown in fig shows space group specimens spin wave spontaneous spontaneous magnetization structure sublattice substitution surface symmetry temperature tetrahedral theory tion torque transition uniaxial unit values variation wall yttrium iron garnet
References to this book
 |
Structural and Magnetic Phase Transitions in Minerals S. Ghose,J.M.D. Coey,E. Salje Snippet view - 1988 |
Bibliographic information
| Title | Proceedings of the International School of Physics "Enrico Fermi.", Volume 70 Proceedings of the International School of Physics "Enrico Fermi.", Società italiana di fisica Rivista del nuovo cimento |
| Contributor | Società italiana di fisica |
| Publisher | N. Zanichelli, 1978 |
| Original from | the University of California |
| Digitized | 13 Aug 2008 |
| ISBN | 044485200X, 9780444852007 |
| Export Citation | BiBTeX EndNote RefMan |