Effects of Water Composition on the Dissolution Rate of UO2 Under Oxidizing Conditionsby C. N. Wilson, Pacific Northwest Lab, United States,
W. J. Gray, Pacific Northwest Lab, United States,
Document Type: Proceeding Paper
Part of: High Level Radioactive Waste Management 1990
Abstract: Dissolution rates were measured on crushed unirradiated UO2 fuel pellet samples under oxidizing conditions using a flow-through testing method. Water compositions included Nevada Test Site J-13 well water, deionized distilled water (DIW), and variations on the J-13 water composition selected to measure the effects of various J-13 water components on UO2 dissolution rates. Lower apparent UO2 dissolution rates were measured in waters containing Si and Ca than in DIW or in dilute NaHCO3 solution. A thin (approx. 5 nm) U-Si-O surface alteration layer was identified by Auger microprobe examination of UO2 particles tested at 25°C in Ca-Si containing waters, and a thin layer containing Ca + Si was identified on the surface of particles tested at 85°C. Limited data suggest that the alteration layers act as kinetic barriers to UO2 dissolution rather than as solubility limiting phases. These experiments and their preliminary results are discussed as they apply to the potential disposal of spent nuclear fuel at the candidate Yucca Mountain repository site.
Subject Headings: Fuels | Water management | Waste sites | Site investigation | Uranium | Radioactive wastes | Particles | Chemical wastes | Nuclear power | Nevada | North America | United States
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