Fixation et reduction de l'uranium par les matieres organiques naturelles: mecanismes et aspects cinetiques.

11Citations
Citations of this article
2Readers
Mendeley users who have this article in their library.
Get full text

Abstract

The reactivity of lignite towards soluble uranyl species in an aqueous medium has been investigated experimentally as a function of T (20-400oC). The fixation process starts near 45oC, with reduction beginning at approx 120oC, and leads to the formation of chemically and thermally stable organo-uranyl species. The reduction of free uranyl species is accompanied by a stoichiometric (2:1) liberation of protons into the medium; these protons originate from the organic matter which thus undergoes dehydrogenation, explaining the low hydrogen content of natural organic materials associated with U deposits. Alcoholic and aliphatic hydrocarbon groups are responsible for the reduction; the kinetics have been studied at 180, 190 and 200oC and, when extrapolated to 20oC, show that reduction can be a crucial process in the geochemical behaviour of U especially in the thermal conditions in which sedimentary basins evolve. -R.A.H.

Cite

CITATION STYLE

APA

Nakashima, S., Disnar, J. R., Perruchot, A., & Trichet, J. (1987). Fixation et reduction de l’uranium par les matieres organiques naturelles: mecanismes et aspects cinetiques. Bulletin de Mineralogie, 110(2–3), 227–234. https://doi.org/10.3406/bulmi.1987.7982

Register to see more suggestions

Mendeley helps you to discover research relevant for your work.

Already have an account?

Save time finding and organizing research with Mendeley

Sign up for free