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Oxidative release of U(IV) from NRZs is slow because of low diffusivity, rapid consumption of oxidants by the sediments, and rapid U(VI) re-reduction ...
![Redox cycling in NRZs](/sfagroup/sites/default/files/styles/card/public/2023-06/redox_cycling.png?h=a9359686&itok=DpBZJ561)
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Thermodynamically controlled preservation of organic carbon in floodplains | Nature Geoscience A new study combining X-ray absorption spectroscopy (XAS) at SSRL with...
![A chart of the Anaerobic C degradation in sulfidic and non-sulfidic zones](/sfagroup/sites/default/files/styles/card/public/2023-06/sulfidic_zone.png?h=26a4e6c8&itok=82S0E8vq)
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http://www.pnas.org/content/114/4/711.abstract A new multi-technique study using X-ray absorption spectroscopy at SSRL, nanoscale secondary Ion mass spectroscopy at EMSL, and scanning transmission X-ray microscopy...
![Organics and cells in water](/sfagroup/sites/default/files/styles/card/public/2023-06/smaller_organic_cells.png?h=0693a9c3&itok=MzUsBNQm)
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The Science. Oxidative dissolution of U(IV) to U(VI) controls the release of uranium from reduced sediments to groundwater. In this study, uraninite (UO...
![Dissolved oxygen concentrations in the Rifle aquifer](/sfagroup/sites/default/files/styles/card/public/2023-06/river_discharge.png?h=9612a368&itok=Ou4UvVvk)