Abstract
It is shown that layer-by-layer measurements of the electron-transfer activation energy in polycrystalline ferrites allow the profiles of depth distribution of oxygen introduced from the atmosphere into a ferrite at the stage of sintering or thermal treatment to be studied using a simple experimental technique. The analytical equations proposed here make it possible to determine the volume and grain-boundary diffusion coefficients of oxygen using a minimum number of adjustable parameters.
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Tomsk Polytechnic University. Translated from Izvestiya Vysshikh Uchebnykh Zavedenii, Fizika, No. 5, pp. 64–69, May, 1999.
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Surzhikov, A.P., Peshev, V.V., Pritulov, A.M. et al. Grain-boundary diffusion of oxygen in polycrystalline ferrites. Russ Phys J 42, 490–495 (1999). https://doi.org/10.1007/BF02508222
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DOI: https://doi.org/10.1007/BF02508222