Proceedings of the International School of Physics "Enrico Fermi.", Volume 70N. Zanichelli, 1978 - Nuclear physics |
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Page 375
We must therefore realize that any measurement of anisotropy or relaxation time
will give an average value , weighed with ... From this it follows that in static
anisotropy measurements the Fe2 + ions next to Sie + will not give any
appreciable ...
We must therefore realize that any measurement of anisotropy or relaxation time
will give an average value , weighed with ... From this it follows that in static
anisotropy measurements the Fe2 + ions next to Sie + will not give any
appreciable ...
Page 428
Extensive measurements on a series of crystals having various concentrations of
tetravalent dopants like silicon would be most useful . For p - type YIG the
situation is even less clear . The Seebeck - coefficient results by VERWEEL and ...
Extensive measurements on a series of crystals having various concentrations of
tetravalent dopants like silicon would be most useful . For p - type YIG the
situation is even less clear . The Seebeck - coefficient results by VERWEEL and ...
Page 442
Hall measurements are in agreement with this supposition . In inhomogeneous ,
n - type , polycrystalline samples also the thermal generation of charge carriers
was shown to be the dominant factor in o . There are only two Seebeck ...
Hall measurements are in agreement with this supposition . In inhomogeneous ,
n - type , polycrystalline samples also the thermal generation of charge carriers
was shown to be the dominant factor in o . There are only two Seebeck ...
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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 |