Published online by Cambridge University Press: 25 February 2011
In cooperation with the Ministry of Research and Technology we investigated the influence of hydroxylapatite (HAP) added to the backfill material of a radioactive waste disposal located in a salt dome. The time dependence of the sorption and precipitation of radionuclides has been studied in three different praxisrelevant salt brines under variation of temperature and pH-value.
Performing batch experiments uranium and thorium phosphates were precipitated from UO 2(NO 3)2 and Th(NO 3)4 solutions at 75°C, the amounts of the relevant actinide compounds also exceeding that of HAP. The isolated precipitates were investigated by use of X-ray-powder-diffractometry and SEM. For the various uranium systems two mineral phases were obtained. From solution II and also from Q-brine the mineral saléeite Mg(UO 2)2 (PO 4)2 · 9 H 2 O was formed. From solution III meta-autunite Ca(UO 2)2(PO 4)2 · 6 H 2 O, a dehydration product of autunite, was precipitated.