Reoxidation of Biogenic Reduced Uranium: A Challenge Toward Bioremediation

Singh G., Sengoer S. S., Bhalla A., Kumar S., De J., Stewart B., ...Daha Fazla

CRITICAL REVIEWS IN ENVIRONMENTAL SCIENCE AND TECHNOLOGY, cilt.44, sa.4, ss.391-415, 2014 (SCI-Expanded) identifier identifier

  • Yayın Türü: Makale / Derleme
  • Cilt numarası: 44 Sayı: 4
  • Basım Tarihi: 2014
  • Doi Numarası: 10.1080/10643389.2012.728522
  • Dergi Adı: CRITICAL REVIEWS IN ENVIRONMENTAL SCIENCE AND TECHNOLOGY
  • Derginin Tarandığı İndeksler: Science Citation Index Expanded (SCI-EXPANDED), Scopus
  • Sayfa Sayıları: ss.391-415
  • Anahtar Kelimeler: biogenic UO2, Fe(III)-(hydr)oxides, humics, Mn(IV) oxides, siderophores, CONTAMINATED SUBSURFACE SEDIMENTS, U(VI) REDUCTION, DESULFOVIBRIO-DESULFURICANS, IRON(III) (HYDR)OXIDES, COORDINATION CHEMISTRY, BIOLOGICAL REDUCTION, DISSOLVED-OXYGEN, U(IV) OXIDATION, FE(III) OXIDE, SULFATE
  • Orta Doğu Teknik Üniversitesi Adresli: Hayır

Özet

Uraninite (UO2) is the most desirable end product of in situ bioreduction because of its low solubility under reducing conditions. For effective long-term immobilization of uranium (U), there should be no biotic or abiotic reoxidation of the insoluble biogenic U(IV). It is therefore critical to understand the long-term stability of U(IV) under oxic- and nutrient-limited conditions at U-contaminated subsurface sites. It has now been established that following in situ bioremediation of U(VI) via nutrient addition in the subsurface, a range of physical, chemical, and biological factors control the rate and extent of long-term stability of U(IV). Some of these factors are tied to site specific conditions including existence of oxidants such as Fe(III)(hydr)oxides, Mn(IV) oxides, oxygen, and nitrate; the presence of organic carbon and the reduced forms of U (e.g., mononuclear U(IV) or nanometer-sized uraninite particles); and the carbonate concentration and pH of groundwater. This review analyzes the contribution of these factors in controlling U(IV)-reoxidation, and highlights the competition among U(IV) and other electron acceptors and possible mechanisms of reoxidation of various forms of U(IV).