Uranium as a contaminant and a paleoredox proxy
|Starts:||13:00 27 Mar 2019|
|Ends:||14:00 27 Mar 2019|
|What is it:||Seminar|
|Organiser:||School of Earth and Environmental Sciences|
|Who is it for:||University staff, External researchers, Adults, Alumni, Current University students, General public|
|Speaker:||Rizlan Bernier-Latmani, Ecole Polytechnique Fédérale de Lausanne|
Uranium (U), present in the tetravalent form (relatively insoluble as U(IV)) in igneous rocks, undergoes oxidation and mobilization as part of weathering. As a result, oxidized uranium (hexavalent, U(VI)) is present in surface waters, particularly in areas with an underlying granitic bedrock. In anoxic soils and sediments, uranium can accumulate through reductive processes, forming natural hotspots. Looking through the sedimentary rock record, one can consider the accumulation of U as an indication of local anoxic conditions and the associated isotopic fractionation may reveal more detail about the depositional environment. Additionally, uranium can be a contaminant in the subsurface as a result of anthropogenic activities such as mining and processing of nuclear fuel. Arresting the transport of uranium in the subsurface by reducing uranium in contaminated environments, through harnessing microbial and chemical reductive mechanisms, has been proposed as a engineered remediation strategy.
A thorough understanding of the mechanism of U(VI) reduction and the attendant isotopic fractionation is necessary in order to interpret the geological record and to optimize U remediation strategies.
Here, I will present recent development in laboratory-based investigations of the reduction of U(VI) by microorganisms as well as by minerals along with advances in constraining the associated isotopic fractionation. The work presented will span mechanistic understanding of microbial and abiotic U reduction as well as investigations of the stability of sediment-trapped tetravalent U. Overall, I hope to provide an overview of the exiting new developments in U biogeochemistry.
Rizlan Bernier-Latmani, Ecole Polytechnique Fédérale de Lausanne
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