Structural and Magnetic Phase Transitions in Minerals |
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Page v
Model compounds provide the elements needed to build up a realistic understanding of the thermodynamic behavior of natural inorganic materials in all their complexity . In the first part of the book , a number of papers are devoted to ...
Model compounds provide the elements needed to build up a realistic understanding of the thermodynamic behavior of natural inorganic materials in all their complexity . In the first part of the book , a number of papers are devoted to ...
Page 3
These order parameters are thermodynamic quantities and are not directly related to structural properties . It can be shown , however , that some structural aspects reflect the variation of the order parameter ( with temperature ...
These order parameters are thermodynamic quantities and are not directly related to structural properties . It can be shown , however , that some structural aspects reflect the variation of the order parameter ( with temperature ...
Page 13
Order parameter vector space diagram of albite representing the values of Q and Qod at various temperatures ( thermodynamic equilibrium ) . form and the fully ordered triclinic form ( Q = lod = 1 ) . The contribution of the Al ...
Order parameter vector space diagram of albite representing the values of Q and Qod at various temperatures ( thermodynamic equilibrium ) . form and the fully ordered triclinic form ( Q = lod = 1 ) . The contribution of the Al ...
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Contents
Incommensurate Phase Transitions in Quartz and Berlinite | 17 |
Phase Separation in Quadrilateral Pyroxenes and Olivines | 39 |
Multicritical Phase Relations in Minerals | 60 |
Copyright | |
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Structural and Magnetic Phase Transitions in Minerals S. Ghose,J.M.D. Coey,E. Salje Limited preview - 2012 |
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+ 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 structure symmetry Table temperature theory thermodynamic tion transformation unit variation