1991
DOI: 10.1557/proc-257-513
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Obsidians and Tektites: Natural Analogues for Water Diffusion in Nuclear Waste Glasses

Abstract: Molecular water diffusion in natural obsidians and tektite was investigated in vapor hydration tests performed between 75 and 230°C for up to 400 days. Reaction progress was monitored using measurements of the birefringent hydration layer, an alteration feature associated with strain caused by molecular water diffusion in obsidians. The hydration rate constants and temperature dependence of the reaction are strongly correlated with the logarithm of the initial total water content of the glass. These values hav… Show more

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Cited by 18 publications
(15 citation statements)
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“…Nevertheless, defects in the silicate structure may provide diffusion channels large enough to permit molecular water diffusion. For example, water diffusion is known to occur without affecting the silicate network of obsidian [20][21][22][23]. In most instances, tests of alkali silicate glasses in silicate solutions also show dealkalization to occur without affecting the silicate network [24].…”
Section: Water Diffusionmentioning
confidence: 99%
“…Nevertheless, defects in the silicate structure may provide diffusion channels large enough to permit molecular water diffusion. For example, water diffusion is known to occur without affecting the silicate network of obsidian [20][21][22][23]. In most instances, tests of alkali silicate glasses in silicate solutions also show dealkalization to occur without affecting the silicate network [24].…”
Section: Water Diffusionmentioning
confidence: 99%
“…The method has also been used to simulate the long-term weathering of tektite (Mazer et al 1992) and basaltic glasses (Byers et al 1986). Because the test method produces the same alteration phases that form during the weathering of natural glasses over long periods, the test has also been used to accelerate the corrosion of waste glasses.…”
Section: Vapor Hydration Test Methodsmentioning
confidence: 99%
“…obsidian artifacts recovered from terrestrial sites (Friedman and Long 1976). The method has also been used to simulate the long-term weathering of tektite (Mazer et al 1992) and basaltic glasses ). Because the test method produces the same alteration phases that form during the weathering of natural glasses over long periods, the test has also been used to accelerate the corrosion of waste glasses.…”
Section: Vapor Hydration Testmentioning
confidence: 99%