Structural and Magnetic Phase Transitions in MineralsThis volume in Advances in Physical Geochemistry presents the latest synthesis of theory and experimental data pertaining to structural and magnetic phase transitions in a variety of geochemically important minerals. The book is the first to cover the impact of this rapidly progressing area of solid state physics in earth sciences and reflects its growing significance for mineralogy and petrology. |
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Page 114
Hund's rule can break down , however , if the exchange energy can be overcome
by a nonspherical crystal field ( e.g. , an octahedral coordination site in a silicate
or oxide ) that removes the degeneracy of the Fe2 + 3d orbitals . Under an ...
Hund's rule can break down , however , if the exchange energy can be overcome
by a nonspherical crystal field ( e.g. , an octahedral coordination site in a silicate
or oxide ) that removes the degeneracy of the Fe2 + 3d orbitals . Under an ...
Page 152
Magnetic Phase Transitions The Nature of the Fe2 + -Fe3 + Interaction The
molecular orbital description of the chemical bonding in a double ... In such a
cluster , Fe - Fe bonding occurs through an overlap of the Fea ( t2gFeb ( t2g )
orbitals .
Magnetic Phase Transitions The Nature of the Fe2 + -Fe3 + Interaction The
molecular orbital description of the chemical bonding in a double ... In such a
cluster , Fe - Fe bonding occurs through an overlap of the Fea ( t2gFeb ( t2g )
orbitals .
Page 162
... magnetic properties . Ferric iron , Fe3 + , ( like Mn2 + ) has a half - filled 3d
shell , giving a 3ds configuration . The spin quantum number S is y , and there is
no orbital angular momentum so the magnetic moment of the free ion ( “ S5 / 2 ) ...
... magnetic properties . Ferric iron , Fe3 + , ( like Mn2 + ) has a half - filled 3d
shell , giving a 3ds configuration . The spin quantum number S is y , and there is
no orbital angular momentum so the magnetic moment of the free ion ( “ S5 / 2 ) ...
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Contents
Preface | 1 |
Incommensurate Phase Transitions in Quartz and Berlinite | 17 |
Phase Separation in Quadrilateral Pyroxenes and Olivines | 39 |
Copyright | |
8 other sections not shown
Other editions - View all
Structural and Magnetic Phase Transitions in Minerals S. Ghose,J.M.D. Coey,E. Salje Limited preview - 2012 |
Structural and Magnetic Phase Transitions in Minerals S. Ghose,J.M.D. Coey,E. Salje Snippet view - 1988 |
Common terms and phrases
antiferromagnetic appears applied approximation atoms axis Ballet behavior bond calculated cation Chem chemical cluster Coey components composition constant corresponding coupling critical crystal decreases density dependence described determined diffraction direction disordered Dolino effect electron energy equilibrium estimated et al exchange experimental experiments Fe2+ Fe3+ ferromagnetic field function Ghose give given heat ilvaite inc phase increases indicate interactions ions iron lattice layers Lindsley lower mantle magnetic magnetic order materials measurements Mineral mode Mössbauer natural neutron observed obtained occur octahedral olivines order parameter pairs perovskite phase diagrams phase transition Phys physical pigeonite polytypes positions possible potential predicted pressure properties pyroxenes quartz range respectively Salje sample shown shows silicates solid solution space group spin stability strain structure symmetry Table temperature theory thermodynamic tion transformation unit variation