Dissolution of Uranium-Bearing Minerals and Mobilization of Uranium by Organic Ligands in a Biologically Reduced Sediment

• Published in: Environmental science & technology 2011-04, Vol.45 (7), p.2994-2999
• Main Authors: Luo, Wensui, Gu, Baohua
• Format: Article
• Language: English
• Subjects: ALUMINIUM; Aluminum - chemistry; ANAEROBIC CONDITIONS; Applied sciences; Biological and physicochemical properties of pollutants. Interaction in the soil; Bioreduced sediment; BIOREMEDIATION; CITRATES; Citric Acid - chemistry; Correlation analysis; DISSOLUTION; Earth sciences; Earth, ocean, space; Edetic Acid - chemistry; EDTA; Engineering and environment geology. Geothermics; Environmental Restoration and Remediation - methods; ENVIRONMENTAL SCIENCES; Exact sciences and technology; Geologic Sediments - chemistry; IRON; Iron - chemistry; Kinetics; LEACHING; Ligands; Mineral dissolution; Minerals; Molecules; organic ligands; Oxidation-Reduction; Pollution; Pollution, environment geology; PRECIPITATION; Remediation and Control Technologies; REMOVAL; SEDIMENTS; Soil and sediments pollution; STABILITY; Studies; U(IV) and U(VI) mobilization; URANIUM; Uranium - chemistry; Water Pollutants, Radioactive - chemistry
• ISSN: 0013-936X; 1520-5851
• DOI: 10.1021/es103073u

The stability and mobility of uranium (U) is a concern following its reductive precipitation or immobilization by techniques such as bioremediation at contaminated sites. In this study, the influences of complexing organic ligands such as citrate and ethylenediaminetetraacetate (EDTA) on the mobilization of U were investigated in both batch and column flow systems using a contaminated and bioreduced sediment. Results indicate that both reduced U(IV) and oxidized U(VI) in the sediment can be effectively mobilized with the addition of EDTA or citrate under anaerobic conditions. The dissolution and mobilization of U appear to be correlated to the dissolution of iron (Fe)- or aluminum (Al)-bearing minerals, with EDTA being more effective (with R 2 ≥ 0.89) than citrate (R 2 < 0.60) in dissolving these minerals. The column flow experiments confirm that U, Fe, and Al can be mobilized by these ligands under anoxic conditions, although the cumulative amounts of U removal constituted ∼0.1% of total U present in this sediment following a limited period of leaching. This study concludes that the presence of complexing organic ligands may pose a long-term concern by slowly dissolving U-bearing minerals and mobilizing U even under a strict anaerobic environment.