

Author: Shiraishi Yutaka Nagahama Hiroshi Ohta Hiromichi
Publisher: Maney Publishing
ISSN: 0008-4433
Source: Canadian Metallurgical Quarterly, Vol.22, Iss.1, 1983-01, pp. : 37-43
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Abstract
Self-diffusion coefficient of oxygen has been measured by the capillary reservoir method in 56 mol % CaO–44 mol % SiO2 melt and the temperature range between 1550and 1650°C under the atmosphere of high purity argon with 3% H2 or of vacuum. As the tracer, stable isotope 18O was used in the form of SiO2* prepared from 18O enriched water and SiCl4. The diffusion coefficient was derived from the concentration-penetration curve which was determined by the mass analysis of CO2* combined with the carbon arc reduction of the capillary sample sectioned after diffusion run.The results obtained showed the end effect of the capillary which means that the effective length postulated by the theoretical concentration profile differs from the real length of the capillary. With the consideration of this effect, the following expression was obtained by the least squares regression on the theoretical solution of the Fick's second law:
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