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AbstractAbstract
[en] Oxygen self-diffusion coefficients were measured in a 20K2O-20SrO-60SiO2 (wt%) glass above and below the glass transition temperature using the single spectrum proton activation analysis of oxygen-18 using the nuclear reaction 18O(p,α)15N. The α-particle spectrum recorded during proton irradiation is used to determine the 18O concentration profile. The self-diffusion coefficients, D, determined for the three diffusion times of about 22 h, 3 1/2 and 7 1/2 days were in good agreement within experimental error, except for the two lowest temperatures of the short-time run possibly because of the shallow depths of diffusion and surface exchange. Expressions are given for the D values in the temperature range 600 to 1000 K. (author)
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Journal Article
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Journal of Materials Science; ISSN 0022-2461;
; v. 14(6); p. 1425-1432

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ALKALI METAL COMPOUNDS, ALKALINE EARTH METAL COMPOUNDS, BARYON REACTIONS, BARYONS, CATIONS, CHALCOGENIDES, CHARGED PARTICLES, CHEMICAL ANALYSIS, DIFFUSION, ELEMENTARY PARTICLES, ELEMENTS, EVEN-EVEN NUCLEI, FERMIONS, HADRON REACTIONS, HADRONS, HELIUM IONS, HYDROGEN IONS, HYDROGEN IONS 1 PLUS, IONS, ISOTOPES, LIGHT NUCLEI, NITROGEN ISOTOPES, NONMETALS, NUCLEAR REACTIONS, NUCLEI, NUCLEON REACTIONS, NUCLEONS, ODD-EVEN NUCLEI, OXIDES, OXYGEN COMPOUNDS, OXYGEN ISOTOPES, POTASSIUM COMPOUNDS, SILICON COMPOUNDS, SPECTRA, STABLE ISOTOPES, STRONTIUM COMPOUNDS
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