Effects of solution pH and complexing reagents on uranium and thorium desorption under saturated equilibrium conditions

摘要

Three contaminated bulk surface soils were used for investigating the effect of solution pH and complexing reagents on uranium and thorium desorption. At a low solution pH, the major chemical species of uranium and thorium, uranyl UO(sub 2)(sup +2), thorium dihydroxide Th(OH)(sub 2)(sup +2), and thorium hydroxide Th(OH)(sup +3), tend to form complexes with acetates in the solution phase, which increases the fractions of uranium and thorium desorbed into this phase. At a high solution pH, important uranium and thorium species such as uranyl tricarbonate complex UO(sub 2)(CO)(sub 3)(sub 3)(sup (minus)4) and thorium tetrahydroxide complex Th(OH)(sub 4) tend to resist complexation with acetates. The presence of complexing reagents in solution can release radionuclides such as uranium and/or thorium from the soil to the solution by forming soluble complexes. Sodium bicarbonate (NaHCO(sub 3)) and diethylenetriaminepentaacetic acid (DTPA) are strong complex formers that released 38% to 62% of total uranium activity and 78% to 86% of total thorium activity, respectively, from the soil samples investigated. Solutions of 0.1 molar sodium nitrate (NaNO(sub 3)) and 0.1 molar sodium sulfate (Na(sub 2)SO(sub 4)) were not effective complex formers with uranium and thorium under the experimental conditions. Fractions of uranium and thorium desorbed by 0.15g/200ml humic acid ranged from 4.62% to 6.17% and 1.59% to 7.09%, respectively. This work demonstrates the importance of a knowledge of solution chemistry in investigating the desorption of radionuclides. (ERA citation 17:029432)