Biogenic non-crystalline U(IV) revealed as major component in uranium ore deposits
Crystalline uraninite is believed to be the dominant form in uranium deposits. Here, the authors find that non-crystalline U(IV) generated through biologically mediated U(VI) reduction is the predominant U(IV)species in ore deposits, implying that biogenic processes are more important than previousl...
Guardado en:
Autores principales: | Amrita Bhattacharyya, Kate M. Campbell, Shelly D. Kelly, Yvonne Roebbert, Stefan Weyer, Rizlan Bernier-Latmani, Thomas Borch |
---|---|
Formato: | article |
Lenguaje: | EN |
Publicado: |
Nature Portfolio
2017
|
Materias: | |
Acceso en línea: | https://doaj.org/article/aa0740f1ce9e468e8e593c6fb490381a |
Etiquetas: |
Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
|
Ejemplares similares
-
Nanoscale mechanism of UO2 formation through uranium reduction by magnetite
por: Zezhen Pan, et al.
Publicado: (2020) -
Evidence for ligand- and solvent-induced disproportionation of uranium(IV)
por: Jingzhen Du, et al.
Publicado: (2021) -
Immiscible hydrous Fe–Ca–P melt and the origin of iron oxide-apatite ore deposits
por: Tong Hou, et al.
Publicado: (2018) -
Origin of the Pd-Rich Pentlandite in the Massive Sulfide Ores of the Talnakh Deposit, Norilsk Region, Russia
por: Valery Kalugin, et al.
Publicado: (2021) -
Application of hyperspectral remote sensing for supplementary investigation of polymetallic deposits in Huaniushan ore region, northwestern China
por: Yu-qing Wan, et al.
Publicado: (2021)