Proceedings of the International School of Physics "Enrico Fermi.", Volume 70N. Zanichelli, 1978 - Nuclear physics |
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Page 24
Strictly speaking , at compensation the materials are ferrimagnets with zero
spontaneous magnetization . From a group - theoretical point of view , which is
the fundamental way to look at magnetically ordered magnetic materials , each ...
Strictly speaking , at compensation the materials are ferrimagnets with zero
spontaneous magnetization . From a group - theoretical point of view , which is
the fundamental way to look at magnetically ordered magnetic materials , each ...
Page 44
012 was found [ 150 ] to be ferrimagnetic with T. = 8 K ; the analogous Ni2 + and
Co2 + garnets were found [ 148 ] to remain para magnetic down to 1.3 K. The
garnet { MnGd , } [ Mn , ] ( Ge , ) 0,2 was also found [ 150 ] to be ferrimagnetic , but
it ...
012 was found [ 150 ] to be ferrimagnetic with T. = 8 K ; the analogous Ni2 + and
Co2 + garnets were found [ 148 ] to remain para magnetic down to 1.3 K. The
garnet { MnGd , } [ Mn , ] ( Ge , ) 0,2 was also found [ 150 ] to be ferrimagnetic , but
it ...
Page 276
... the motion of the magnetization which has been given in this section provides
a useful way to visualize and compare the various ways in which the
magnetization of a ferrimagnetic sample may respond to a change in the
magnetizing field .
... the motion of the magnetization which has been given in this section provides
a useful way to visualize and compare the various ways in which the
magnetization of a ferrimagnetic sample may respond to a change in the
magnetizing field .
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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 |