Proceedings of the International School of Physics "Enrico Fermi.", Volume 70N. Zanichelli, 1978 - Nuclear physics |
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Page 382
The two normal polarizations are the north and south pole of the sphere , and the
appropriate circle between them is the equator . A birefringent medium is one in
which the velocity for one normal mode is greater than that for the other .
The two normal polarizations are the north and south pole of the sphere , and the
appropriate circle between them is the equator . A birefringent medium is one in
which the velocity for one normal mode is greater than that for the other .
Page 385
If there were no MCB and a moderate dichroism , we would move on the
Poincaré sphere toward the normal mode with the lesser absorption . An initial
linear polarization would become elliptical with the same azimuth of its major axis
.
If there were no MCB and a moderate dichroism , we would move on the
Poincaré sphere toward the normal mode with the lesser absorption . An initial
linear polarization would become elliptical with the same azimuth of its major axis
.
Page 387
The separation for k normal to M is the MLB , and the normal modes are linearly
polarized parallel and perpendicular to M. For some intermediate direction the
normal modes are elliptical and we would have to think in terms of a magnetic ...
The separation for k normal to M is the MLB , and the normal modes are linearly
polarized parallel and perpendicular to M. For some intermediate direction the
normal modes are elliptical and we would have to think in terms of a magnetic ...
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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 |