Abstract
The conductivity of MgAl2O4 has been measured at 1273, 1473 and 1673 K as a function of the partial pressure of oxygen ranging from 105 to 10-14 Pa. The MgAl2O4 pellet, sandwiched between two platinum electrodes, was equilibrated with a flowing stream of either Ar + O2, CO + CO2 or Ar + H2 + H2O mixture of known composition. The gas mixture established a known oxygen partial pressure. All measurements were made at a frequency of 1 kHz. These measurements indicate pressure independent ionic conductivity in the range 1 to 10-14 Pa at 1273 K, 10-1 to 10-12 Pa at 1473 K and 10-1 to 10-4 Pa at 1673 K. The activation energy for ionic conduction is 1·48 eV, close to that for self-diffusion of Mg2+ ion in MgAl2O4 calculated from the theoretical relation of Glyde. Using the model, the energy for cation vacancy formation and activation energy for migration are estimated. © 1990 The Indian Academy of Sciences.
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Mathews, T., Jacob, K. T., & Hajra, J. P. (1990). Electrical transport in magnesium aluminate. Bulletin of Materials Science, 13(4), 293–300. https://doi.org/10.1007/BF02744986
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