Cargando…
Nanoscale mechanism of UO(2) formation through uranium reduction by magnetite
Uranium (U) is a ubiquitous element in the Earth’s crust at ~2 ppm. In anoxic environments, soluble hexavalent uranium (U(VI)) is reduced and immobilized. The underlying reduction mechanism is unknown but likely of critical importance to explain the geochemical behavior of U. Here, we tackle the mec...
Autores principales: | Pan, Zezhen, Bártová, Barbora, LaGrange, Thomas, Butorin, Sergei M., Hyatt, Neil C., Stennett, Martin C., Kvashnina, Kristina O., Bernier-Latmani, Rizlan |
---|---|
Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group UK
2020
|
Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7417540/ https://www.ncbi.nlm.nih.gov/pubmed/32778661 http://dx.doi.org/10.1038/s41467-020-17795-0 |
Ejemplares similares
-
Persistence
of the Isotopic Signature of Pentavalent
Uranium in Magnetite
por: Pan, Zezhen, et al.
Publicado: (2022) -
Cr(2+) solid solution in UO(2) evidenced by advanced spectroscopy
por: Smith, Hannah, et al.
Publicado: (2022) -
Variability in DPA and Calcium Content in the Spores of Clostridium Species
por: Jamroskovic, Jan, et al.
Publicado: (2016) -
Biological
Reduction of a U(V)–Organic Ligand
Complex
por: Molinas, Margaux, et al.
Publicado: (2021) -
Effect of carbon content on electronic structure of uranium carbides
por: Butorin, Sergei M., et al.
Publicado: (2023)