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- Research highlights
- Calcium-Uranyl-Carbonato Species Kinetically Limit U(VI) Reduction by Fe(II) and Result in U(V)-bearing Ferrihydrite
- Diverse Ammonia-Oxidizing Archaea Dominate Subsurface Nitrifying Communities in Semi-Arid Floodplains
- A Simplified Way to Predict the Function of Microbial Communities
- Complexation Organic Matter Controls Uranium Mobility Anoxic Sediments
- FES-Nanoclusters can mobilize Fe and S from sediment to the groundwater
- Hexavalent uranium storage mechanisms in wet-dry cycled sediments at contaminated DOE sites in the Western U.S.
- Redox-Interfaces can Produce Toxic Arsenic Levels Groundwater...
- Sorption to Organic Matter Controls Uranium Mobility
- Thermodynamic preservation of carbon in anoxic environments
- Iron and sulfur cycling in NRZs controlled by sediment textural and hydrology
- A regional model for uranium redox and mobility
- Long-Term in Situ Oxidation of Biogenic Uraninite in an Alluvial Aquifer: Impact of Dissolved Oxygen and Calcium
- U Release from NRZ sediments is inhibited by Transport and Geochemistry
- Team
- Previous research
- Publications
The SLAC SFA scientific program addresses the grand challenge: How do biogeochemical and transport processes in shallow alluvial groundwater systems (bedrock to soil) couple to one-another and control water quality under hydrologically variable conditions? We are identifying hydro-biogeochemical mobilization and retention processes for C, nutrients (P, S, and Fe) and contaminants (U, Mo, Pb, Zn) at molecular to meter scales. Emphasis is placed on understanding the spatio-temporal coupling of biogeochemical and hydrological processes in soil, the capillary fringe, and the upper portion of the saturated zone. Field studies at the mining impacted Coal Creek and Slate River head-watersheds (Gunnison county, CO) and the former ore processing site in semi-arid Riverton, WY are combined with laboratory experiments to understand the impact of timing, duration, and intensity of wet-dry cycling, transport direction, organic carbon content and sediment texture on redox and nutrient and contaminant mobilization. Quantitative process representations that are developed within the SLAC SFA program will be shared with collaborating SFAs and the wider community for incorporation into larger-scale models. Results from this work will advance short- and long-term prediction of water quality by DOE and multi-agency collaborations.
Meet the SLAC SFA scientists videos:
Bradley Tolar's video: Current work being done at Slate River, CO
Zach Perzan's video: Short-term water quality forecasting with continuous-time recurrent neural networks
Tristan Babey's video: Simulation of biogeochemical cycling in an alluvial aquifer
John Bargar's video: How an x-ray microprobe can solve groundwater quality problems
John Bargar at Slate River, CO
Recent Research Highlights
Calcium-Uranyl-Carbonato Species Kinetically Limit U(VI) Reduction by Fe(II) and Result in U(V)-bearing Ferrihydrite
Dewey, C., Sokaras, D., Kroll, T., Bargar, J.R., Fendorf, S. Calcium-Uranyl-Carbonato Species Kinetically Limit U(VI) Reduction by Fe(II) and lead to U(V) - Bearing Ferrihydrite. Environmental Science and Technology (Accepted Manuscript).
The Science: Uranium (U) solubility determines the dissolved concentrations and thus its threat to water quality. It is therefore essential to understand the controls on U solubility to predict and mitigate the impacts of U contamination. Read more >
Microbial Communities in Floodplain Soils Remain Unchanged Throughout Seasonal Redox and Water Table Flux
Tolar, B.B., Boye, K., Bobb, C., Maher, K., Bargar, J.R., Francis, C.A. Stability of floodplain subsurface microbial communities through seasonal hydrological and geochemical cycles. Frontiers in Earth Science – Biogeoscience (in revision).
The Science: Microbial communities play a crucial role in environmental systems, mediating biogeochemical reactions through metabolic processes that can vary depending on environmental conditions. microbial_communities_floodplain_imagerv.jpgmicrobial_communities_floodplain_imagerv.jpg
FeS Nanoclusters Can Mobilize Fe and S from sediment to Groundwater
Noël, V., Kumar, N., Boye, K., Barragan, L., Lezama-Pacheco, J., Chu, R., Tolic, N., Gordon E. Brown Jr., G.E, Bargar, J.R. (2020) FeS Colloids – Formation and Mobilization Pathways in Natural Waters. Environmental Science Nano., Accepted Manuscript.
DOI: 10.1039/C9EN01427F
The Science: Ferrihydrite Sulfidation Promotes FeS Nanocluster Formation. Read more >
For more research highlights read more>
Contacts and Websites
Principal Investigator
John Bargar, bargar@slac.stanford.edu, (650) 926-4949
Support
This program is funded by the Subsurface Biogeochemistry program within the U.S. Department of Energy, Office of Biological and Environmental Research, Climate and Environmental Sciences Division. Funding for SSRL is provided by the Department of Energy, Office of Basic Energy Sciences.
BER Program Managers
David Lesmes, david.lesmes@science.doe.gov, (301) 903-2977
Paul Bayer, paul.bayer@science.doe.gov, (301) 903-5324
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