1986
DOI: 10.2172/59924
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Effect of gamma radiation on groundwater chemistry and glass leaching as related to the NNWSI repository site

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Cited by 4 publications
(4 citation statements)
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“…Under steady-state conditions, the mass of secondary phases increases with time [9]. In open-system (flow-through) experiments, the rate of release of most elements is approximately constant or slowly decreases with time.…”
Section: Overview Of Glass Dissolution Processesmentioning
confidence: 99%
“…Under steady-state conditions, the mass of secondary phases increases with time [9]. In open-system (flow-through) experiments, the rate of release of most elements is approximately constant or slowly decreases with time.…”
Section: Overview Of Glass Dissolution Processesmentioning
confidence: 99%
“…Steady-state conditions are commonly observed during glass dissolution in which the rates of water diffusion and ion exchange are equal to the rate at which the glass network dissolves. Steady-state conditions are evidenced by the tendency for the glass diffusion layer to remain constant in thickness while the glass dissolves away and the mass of secondary phases increases with time (Abrajano et al, 1986). In open-system experiments, the rate of release of most elements is approximately constant or slowly decreasing with time.…”
Section: Glass-dissolution Mechanismmentioning
confidence: 99%
“…Steady-state conditions are commonly observed during glass dissolution where the rates of water diffusion and ion exchange are equal to the rate at which the glass network dissolves. Steady state conditions are evidenced by the tendency for the glass diffusion layer to remain constant in thickness while the glass dissolves away and the mass of secondary phases increases with time 6 . In open system experiments, the rate of release of most elements is approximately constant or slowly decreasing with time.…”
Section: If/ Diffusion Layermentioning
confidence: 99%