Microbial communities associated with uranium in-situ recovery mining process are related to acid mine drainage assemblages

• Published in: The Science of the total environment Vol. 628-629; pp. 26 - 35
• Main Authors: Coral, Thomas, Descostes, Michaël, De Boissezon, Hélène, Bernier-Latmani, Rizlan, de Alencastro, Luiz Felippe, Rossi, Pierre
• Format: Journal Article
• Language: English
• Published: Netherlands Elsevier B.V 01-07-2018
• Subjects: Acid mine drainage; Acidophilic bacteria; Acids; Bacteria; Groundwater - chemistry; Groundwater - microbiology; In-situ recovery; Kazakhstan; Mining; Multivariate statistics; Natural attenuation; Next-generation sequencing; Uranium; Uranium - metabolism; Water Pollutants, Radioactive - metabolism; Uranium; Next-generation sequencing; Natural attenuation; Multivariate statistics; In-situ recovery; Acidophilic bacteria; Kazakhstan; Acid mine drainage
• ISSN: 0048-9697; 1879-1026
• DOI: 10.1016/j.scitotenv.2018.01.321

A large fraction (47%) of the world's uranium is mined by a technique called “In Situ Recovery” (ISR). This mining technique involves the injection of a leaching fluid (acidic or alkaline) into a uranium-bearing aquifer and the pumping of the resulting solution through cation exchange columns for the recovery of dissolved uranium. The present study reports the in-depth alterations brought to autochthonous microbial communities during acidic ISR activities. Water samples were collected from a uranium roll-front deposit that is part of an ISR mine in operation (Tortkuduk, Kazakhstan). Water samples were obtained at a depth of ca 500 m below ground level from several zones of the Uyuk aquifer following the natural redox zonation inherited from the roll front deposit, including the native mineralized orebody and both upstream and downstream adjacent locations. Samples were collected equally from both the entrance and the exit of the uranium concentration plant. Next-generation sequencing data showed that the redox gradient shaped the community structures, within the anaerobic, reduced, and oligotrophic habitats of the native aquifer zones. Acid injection induced drastic changes in the structures of these communities, with a large decrease in both cell numbers and diversity. Communities present in the acidified (pH values < 2) mining areas exhibited similarities to those present in acid mine drainage, with the dominance of Sulfobacillus sp., Leptospirillum sp. and Acidithiobacillus sp., as well as the archaean Ferroplasma sp. Communities located up- and downstream of the mineralized zone under ISR and affected by acidic fluids were blended with additional facultative anaerobic and acidophilic microorganisms. These mixed biomes may be suitable communities for the natural attenuation of ISR mining-affected subsurface through the reduction of metals and sulfate. Assessing the effect of acidification on the microbial community is critical to evaluating the potential for natural attenuation or active bioremediation strategies.
[Display omitted]
•Redox gradient shaped community structures within the native aquifer zones.•Acid injection favors acidophilic chemolithoautotrophic Bacteria and Archaea.•This acidophilic community shared strong similarities with AMD-related communities.•Up- and down-stream affected zones showed signs of resilience to ISR fluids.•Assessing community structures is necessary for the setup of remediation strategies.