Quantitative understanding of uranium transport by high temperature fluids is crucial for
confident assessment of its migration in a number of natural and artificially induced contexts,
such as hydrothermal uranium ore deposits and nuclear waste stored in geological
repositories. An additional recent and atypical context would be the seawater inundated fuel
of the Fukushima Daiichi Nuclear Power Plant. Given its wide applicability, understanding
uranium transport will be useful regardless of whether nuclear power finds increased or …