Journal of Physics C Solid State Physics · 1983 · 11 citations · 15 references
Natural SciencesChemistryPhysicsCondensed Matter PhysicsInorganic ChemistrySolid State PhysicsIron OxidesMagnetic OxidesMagnetic Properties Of SolidsMagnetism In SolidsMagnetism Of Inorganic CompoundsTransition Metal ChemistryCrystal Field Effects In Solid-state MaterialsCrystal Field Effects On Spin-orbit CouplingHigh-pressure Phase TransitionsHigh-spin StatesMagnetic Properties Of Transition Metal ComplexesPressure-induced Phase TransitionsSpin State TransitionsVolume Change
Several transition-metal compounds change their volume abruptly under high pressure through their electronic spin-state transition. The pressure-induced spin-state transitions in transition-metal compounds are studied on the basis of the ligand-field theory by using the model in which the coupling of transition-metal ions with crystal distortions is taken into account. The various types of transitions occur due to the crystal distortion induced by pressure, that is, the continuous and discontinuous high-spin (HS) to low-spin (LS) transitions with increasing pressure in the weak-crystal-field compounds, the continuous and discontinuous LS to HS transitions and the multiple LS to HS to LS to HS transition in the strong-crystal-field compounds. The pressure against volume curve shows various features of changes due to the crystal distortion associated with the spin-state transitions. The observed pressure against volume curve of haematite Fe2O3 is well explained by the discontinuous HS to LS transition of Fe3+ ions.
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Some elastic constant data on minerals relevant to geophysics
Orson L. Anderson, Edward Schreiber, Robert C. Liebermann et al. · Reviews of Geophysics · 1968 · 534 citations
Mitsuo Kataoka, Junjiro Kanamori · Journal of the Physical Society of Japan · 1972 · 157 citations