Proceedings of the International School of Physics "Enrico Fermi.", Volume 70N. Zanichelli, 1978 - Nuclear physics |
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Page 25
Specimens . Except for the single crystals used in our studies of the rare - earth
iron garnets ( see part II ) , all the garnet specimens on which our magnetization
measurements were made were polycrystalline . Specimens used in the early ...
Specimens . Except for the single crystals used in our studies of the rare - earth
iron garnets ( see part II ) , all the garnet specimens on which our magnetization
measurements were made were polycrystalline . Specimens used in the early ...
Page 37
... plotted in fig . 18 . The specimens were furnace - cooled and so the results
should be expected to be different . The scatter about the line through these data
is worse than for our data , but the results do show that , for most of their
specimens ...
... plotted in fig . 18 . The specimens were furnace - cooled and so the results
should be expected to be different . The scatter about the line through these data
is worse than for our data , but the results do show that , for most of their
specimens ...
Page 39
Because it was found that the incorporation of Bi3 + in yttrium iron garnet
substantially reduced the preparation temperature [ 117 ] , successful attempts
were made to reduce the preparation temperatures of specimens in the A13 + ion
...
Because it was found that the incorporation of Bi3 + in yttrium iron garnet
substantially reduced the preparation temperature [ 117 ] , successful attempts
were made to reduce the preparation temperatures of specimens in the A13 + ion
...
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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 |