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Cation Diffusion in Single Crystal MgO up to 2500 °C
Author(s) -
Harding B. C.
Publication year - 1973
Publication title -
physica status solidi (b)
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.51
H-Index - 109
eISSN - 1521-3951
pISSN - 0370-1972
DOI - 10.1002/pssb.2220560228
Subject(s) - ion , divalent , ionic radius , diffusion , activation energy , chemistry , valence (chemistry) , halide , enthalpy , ionic bonding , ionic potential , crystal (programming language) , alkali metal , atmospheric temperature range , analytical chemistry (journal) , thermodynamics , inorganic chemistry , physics , organic chemistry , chromatography , computer science , programming language
The diffusion of Ca 2+ and Ge 4+ in single crystal MgO has been studied over the temperature range 1850 to 2400 °C using a sectioning technique. The activation energy for the diffusion of Ca 2+ (3.2 eV) is similar to the values obtained for other divalent cations at the same temperatures, but the value for Ge 4+ (4.0 eV) is significantly greater. For ions of a given valence, it is concluded that the activation energy for diffusion in MgO is independent of the “hard‐sphere” ionic radius of the diffusing ion, while the pre‐exponential factor, Do, appears to depend on its mass and electronic polarisability. If results for aliovalent ion diffusion are interpreted in terms of the association theory developed for the alkali halides, an empirical relation between the charge of the diffusing ion and its enthalpy of migration emerges.