The density of UO2 pellets decreases with sintering time during the si
ntering at 1500-degrees-C for 0.1 to 40 h in CO2 and H-2-CO2 atmospher
es. The density decrease is caused by pore growth. The microstructure
developed in CO2 atmosphere has many intragranular pores, which are mo
stly annihilated for further sintering, while intergranular pores grow
significantly. The coalescence of intergranular pores occurs consider
ably even under negligible grain growth. In the uniform grain structur
e developed in H-2-CO2 atmosphere, the average pore size is proportion
al to the grain size as long as grain growth proceeds. The mechanisms
of pore growth are discussed on the basis of the pore coalescence due
to grain growth and the interlinkage of pores.