New Insights Into Uranium Chemistry Can Aid Geological Disposal of Radioactive Waste
The uranium-persulfide complex associated with the transforming mineral surface.
Credit: Diamond Light Source
A new paper to be published on December 16, 2019, provides a significant new insight into our understanding of uranium biogeochemistry and could help with the UK’s nuclear legacy.
Conducted by a team of researchers from the University of Manchester, Diamond Light Source and Radioactive Waste Management, their work shows for the first time how uranium forms a uranium-sulfur complex under conditions generally found in the environment and how this compound can be an important intermediary in uranium immobilization. Published in Environmental Science & Technology, the paper is called “Formation of a U(VI)-persulfide complex during environmentally relevant sulfidation of iron (oxyhydr)oxides.”
Professor Katherine Morris, Associate Dean for Research Facilities in the Faculty of Science and Engineering, University of Manchester and the Research Director for the BNFL Research Centre in Radwaste Disposal explains why recreating and studying these chemical complexes is highly relevant for understanding and dealing with radioactive waste. She explains: “To be able to predict the behavior of the uranium during geological disposal, we need to take into account that it may have interacted with other processes taking place in the ground. These so-called biogeochemical reactions are often a complex set of interactions between dissolved chemical species, mineral surfaces, and microorganisms.”
The recent study is the first time that researchers have shown that a uranium-sulfide complex can form under conditions representative of a deep underground environment. This complex then transforms further into highly immobile uranium oxide nanoparticles.
In the experiment, the researchers studied uranium when it sits at the surface of the mineral ferrihydrite, which is a widespread mineral in the environment. The researchers used an X-ray based method called X-ray Absorption Spectroscopy (XAS) to study the samples at Diamond Light Source, the UK’s national Synchrotron. The XAS data, in combination with computational modeling, showed that during the sulfidation reaction, a short-lived and novel U(VI)-persulfide complex formed during this biogeochemical process.
Professor Sam Shaw, Co-Investigator and Professor of Environmental Mineralogy at the University of Manchester; “Shining the synchrotron beam onto the sample causes the uranium within to emit X-rays. By analyzing the X-ray signal from the samples our team were able to determine the chemical form of uranium, and to which other elements it is bound. To further validate the theory on the formation pathway of the uranium-sulfur complexes, our team also made computer simulations to conclude which type of complex is more likely to form. This is the first observation of this form of uranium under aqueous conditions, and provides new insight into how uranium behaves in environments where sulfide is present. This work
demonstrates the deep understanding we can develop of these complex systems and this knowledge will help underpin efforts to manage radioactive wastes in a geological disposal facility.”
Dr. Luke Townsend, Postdoctoral Fellow in Environmental Radiochemistry at The University of Manchester, who undertook this research as part of his Ph.D. further adds: