Article citationsMore >>

Sylwester E.R., Hudson, E.A., Allen, P.G. The structure of uranium (VI) sorption complexes on silica, alumina, and montmorillonite. Geochim. Cosmochim. Acta 64, 2431-2438. 2000a.

has been cited by the following article:

Article

Migration and Retention of Uranium in the Weathering Blanket Developed on Uraniferous Syenite in Ngombas Southern Cameroon

1The University Institute of Technology, University of Douala, P.O Box 8698, Douala, Cameroon

2University of Douala, Faculty of Sciences, P.O Box 24157, Douala, Cameroon

3Sorbonne Universités CNRS UMR 7590, MNHN, IRD, Institut de Minéralogie, de Physique des Matériaux, et de Cosmochimie (IMPMC), 4 Place Jussieu, Paris F-75005, France


Journal of Geosciences and Geomatics. 2022, Vol. 10 No. 2, 99-111
DOI: 10.12691/jgg-10-2-4
Copyright © 2022 Science and Education Publishing

Cite this paper:
Joel Simon Mbai, Akumbom Vishiti, Bravo Martin Mbang Bonda, Gilbert François NGON NGON, Elie Constantin Bayiga, Martine Gérard, Jacques Etamè. Migration and Retention of Uranium in the Weathering Blanket Developed on Uraniferous Syenite in Ngombas Southern Cameroon. Journal of Geosciences and Geomatics. 2022; 10(2):99-111. doi: 10.12691/jgg-10-2-4.

Correspondence to: Joel  Simon Mbai, The University Institute of Technology, University of Douala, P.O Box 8698, Douala, Cameroon. Email: mbai_s@yahoo.fr

Abstract

The lolodorf syenite axis is known for its radiometric indices. In the Ngombas area the migration and retention of uranium in the regolith developed on syenite is studied using a combination of mineralogy and geochemistry in a bid to understand the processes involved in the dissolution and redistribution of uranium in the secondary environment. A trench dug in the area shows three horizons from the bottom to the top. They include the saprolite, B and Ah horizons. Petrographic and XRD investigations of the syenites reveals minerals such as plagioclase, potassic feldspar, amphibole, pyroxene, biotite, quartz, hematite, zircon coupled with uraninite, U-monazite. The regolith developed on the syenite shows relics of plagioclase, amphibole, quartz, hematite, goethite, chlorite, vermiculite, kaolinite. This is associated with U-bearing minerals such as uranothorite, U-monazite, U-zircon, U-florencite and U-rhadophane. The chemical alteration index (CIA), and gain and loss diagrams indicate that the horizons are more weathered from the top to the bottom. The presence of uranium bearing phases such as uranothorite indicates that U-minerals were dissolved, migrated and sorbed on thorite. The occurrences of U-florencite and U-rhabdophane in the weathering blanket indicate that uranyl is stabilized by phosphate minerals. Under oxidizing conditions the stability of hexavalent uranium is favored by the presence of clay minerals and Fe/Mn-oxyhydroxides. Thus, the migration of uranium in Ngombas is sequestrated by clay blended on Fe-oxides through the process of sorption. The U-bearing phases in the regolith that survived weathering include monazite and zircon. The presence of accessories minerals (U-zircon, U-monazite), sorption of uranium by phosphates, by Fe/Mn-oxyhydroxides, and clays minerals play important roles to reduce the U migration in environmental impact of Ngombas region.

Keywords