This paper presents experimental studies on the kinetics of U release from
near single-phase zirconolite, pyrochlore, brannerite and pyrochlore-rich t
itanate ceramic materials. The dissolution tests were conducted at 20-75 de
greesC with initial pHs from 2 to 12 and flow rates from 10 to 80 mi d(-1)
in the open atmosphere. The U releases from these titanate materials are co
ntrolled by initial fast process and then followed by linear kinetics. The
close-to-stoichiometric U release from zirconolite and pyrochlore-rich mate
rials and preferential U release from brannerite are consistent with the al
terations observed for the natural samples. The rate constants for U releas
es were determined and the effects of pH and temperature were examined. For
each material, the U release vs. pH exhibits a V-shape with a minimum near
pH 8. The measured activation energies suggest surface reaction controlled
dissolution mechanism. Pyrochlore-rich materials and zirconolite demonstra
ted higher chemical durability and more resistance to aqueous attack than b
rannerite. However, impurities and minor brannerite inclusions do not appea
r to have a detrimental effect on U releases from pyrochlor-erich multi-pha
se ceramics. (C) 2001 Elsevier Science B.V. Ail rights reserved.