Pj. Hayward et Im. George, DISSOLUTION OF UO2 IN MOLTEN ZIRCALOY-4 .2. PHASE EVOLUTION DURING DISSOLUTION AND COOLING, Journal of nuclear materials, 208(1-2), 1994, pp. 43-52
Metallography and scanning electron microscopy analyses have been perf
ormed on samples from a previous study of CANDU (CANada Deuterium Uran
ium) UO2 fuel dissolution in molten Zircaloy-4 [1]. Under conditions o
f good convective stirring within the melt, rapid UO2 dissolution occu
rs, leading to melt saturation with respect to U after a few minutes i
n the temperature range 2000 to 2200-degrees-C. Melt saturation is pos
tulated to occur when the melt composition path across the U-Zr-O phas
e diagram intersects the boundary of the two-phase [(U,Zr)O2-x+L] fiel
d. The point of intersection depends significantly on the melt oxygen
content. Contraction of the two-phase field at higher temperatures cau
ses a corresponding increase in fuel solubility.