Abstract
A method is described for using radioactive tracer for the direct determination of ionic mobility in a molten electrolyte. The ionic mobility of Fe++ in silica-saturated iron silicate is found to be 0.0009 (±0.0002) cm2 sec”1 volt”1 at 1250°C.
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M. T. Simnad and G. Derge: Journal of Chemical Physics (1953) 21, p. 933.
M. T. Simnad, G. Derge and I. George: Trans. AIME (1954) 200, p. 1386; Journal of Metals (December 1954).
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J. W. Tomlinson: Symposium on the Nature of Molten Slags and Salts, Nuffield Research Group in Extraction Metallurgy. (1953) p. 22. London. Institution of Mining and Metallurgy.
F. Korber and W. Oelsen: Mitteilungen Kaiser Wilhelm Institut für Eisenforschung (1933) 15, pp. 271–309.
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TP 4197CD. Manuscript, Oct. 15, 1954
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Simnad, M.T., Yang, L. & Derge, G. Direct Measurement of Ferrous Ion Mobility in Liquid Iron Silicate by a Radioactive Tracer Technique. JOM 8, 691–692 (1956). https://doi.org/10.1007/BF03377756
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DOI: https://doi.org/10.1007/BF03377756