Biostimulation of indigenous microbes for uranium bioremediation in former U mine water: multidisciplinary approach assessment
Metadatos
Mostrar el registro completo del ítemAutor
Newman Portela, Antonio Martín; Krawczyk Bärsch, Evelyn; López Fernández, Margarita; Bok, Frank; Kassahun, Andrea; Drobot, Björn; Steudtner, Robin; Stumpf, Thorsten; Raff, Johannes; Merroun, Mohamed LarbiEditorial
Springer Nature
Materia
Mine water Uranium Bacterial communities
Fecha
2023-12-29Referencia bibliográfica
Newman-Portela, A.M., Krawczyk-Bärsch, E., Lopez-Fernandez, M. et al. Biostimulation of indigenous microbes for uranium bioremediation in former U mine water: multidisciplinary approach assessment. Environ Sci Pollut Res 31, 7227–7245 (2024). https://doi.org/10.1007/s11356-023-31530-4
Patrocinador
Open Access funding enabled and organized by Projekt DEAL; Rado-Norm project of the Euratom research and training programme 2019–2020 under grant agreement No900009; European Radioecology Alliance (ALLIANCE); “Plan Propio” of the University of Granada and the ERASMUS+ programmeResumen
Characterizing uranium (U) mine water is necessary to understand and design an effective bioremediation strategy. In this study, water samples from two former U-mines in East Germany were analysed. The U and sulphate (SO42−) concentrations of Schlema-Alberoda mine water (U: 1 mg/L; SO42−: 335 mg/L) were 2 and 3 order of magnitude higher than those of the Pöhla sample (U: 0.01 mg/L; SO42−: 0.5 mg/L). U and SO42− seemed to influence the microbial diversity of the two water samples. Microbial diversity analysis identified U(VI)-reducing bacteria (e.g. Desulfurivibrio) and wood-degrading fungi (e.g. Cadophora) providing as electron donors for the growth of U-reducers. U-bioreduction experiments were performed to screen electron donors (glycerol, vanillic acid, and gluconic acid) for Schlema-Alberoda U-mine water bioremediation purpose. Thermodynamic speciation calculations show that under experimental conditions, U(VI) is not coordinated to the amended electron donors. Glycerol was the best-studied electron donor as it effectively removed 99% of soluble U, 95% of Fe, and 58% of SO4 2− from the mine water, probably by biostimulation of indigenous microbes. Vanillic acid removed 90% of U, and no U removal occurred using gluconic acid.