Complexation by Organic Matter Controls Uranium Mobility in Anoxic Sediments


Complexation by Organic Matter Controls Uranium Mobility in Anoxic Sediments

Bone, S.E.; Cliff, J.; Weaver, K.; Takacs, C.J.; Roycroft, S.; Fendorf, S.; Bargar, J.R. Uranium complexation by organic matter and clay minerals in anoxic contaminated sediments. Environmental Science and Technology 2020, 54, 1493-1502.  

Uranium(IV) adsorbs to organic matter in anoxic alluvial sediment, which may be mobilized through desorption and colloidal release

The Science

In contaminated aquifers, hydrologic and geochemical conditions cause tetravalent uranium – U(IV) – stored in the sediments to be mobilized in the groundwater, elevating the groundwater uranium concentration above the regulatory limit. However, the geochemical mechanisms by which U is released from sediment to solution remain unknown. There is growing belief that sedimentary organic compounds bind U(IV) - a form once considered largely immobile - and mediate its fate in the subsurface. In this work, we combined nano-scale imaging (nano secondary ion mass spectrometry and scanning transmission X-ray microscopy) with a density-based fractionation approach to physically and microscopically isolate organic and mineral matter from anoxic alluvial sediments contaminated with U (collected from the Riverton, WY site). Previously, we applied a combined spectroscopy-microscopy approach to examine U behavior in model systems, which allowed us to unambiguously identify U(IV) adsorption, as opposed to precipitation, as the major mechanism of U(IV) retention in aquifer sediments. Through examination of unaltered sediment from the Riverton site, we have extended and deepened our analysis, leading to the identification of two distinct populations of complexed U control its behavior in anoxic sediments: (i) U adsorbed to organic matter (including particles rich in both carboxylate and phenolic functional groups derived from both plant and microbial material) and (ii) U adsorbed to organic-clay aggregates. This is the first study to demonstrate unambiguously a major role for organic matter as a U(IV) sorbent in unaltered sediments from an alluvial aquifer.

The Impact

Previously, oxidation of U(IV) has been posited as the dominant mechanism by which U is released into groundwater. However, depending on the redox-buffering capacity of the sediment, U(IV) can persist during influxes of oxidants. An additional mechanism of U mobilization from anoxic sediments is therefore needed to explain persistent elevated groundwater concentrations. Our work suggests that adsorbed U(IV), whether complexed by organic matter or clay mineral surfaces, could be mobilized by desorption (e.g. by changing pH or alkalinity). Second, our work provides a mechanistic context for colloidal mobilization of U(IV). We speculate that U associated with POC could be mobilized as that POC is transformed into smaller, more oxidized and more soluble units through hydrolytic degradation reactions. Also, disaggregation of organo-mineral aggregates under changing geochemical conditions (pH, ionic strength, redox) causes the release of organic matter into the dissolved and colloidal phase, along with associated metals. Thus, we conclude that the dominance of organic matter (and clay mineral)-associated U provides a new framework to understand U mobility in the subsurface.        


Uranium contamination threatens the availability of safe and clean drinking water globally. This toxic element occurs both naturally and as a result of mining and ore-processing in alluvial sediments, where it accumulates as tetravalent U [U(IV)], a form once considered largely immobile. Changing hydrologic and geochemical conditions cause U to be released into groundwater. Knowledge of the chemical form(s) of U(IV) is essential to understand the release mechanism, yet the relevant U(IV) species are poorly characterized. There is growing belief that natural organic matter (OM) binds U(IV) and mediates its fate in the subsurface. In this work, we sought to examine the speciation of U in sediment from a contaminated alluvial aquifer to definitively determine whether OM was the dominant U(IV) sorbent. We applied nanoscale chemical imaging and X-ray absorption spectroscopy to density fractionated sediments in which organic matter was separated from minerals, thereby allowing us to assess the U speciation in each pool. We identified two populations of U (dominantly +IV) in anoxic sediments. Uranium was retained on OM and adsorbed to particulate organic carbon, comprising both microbial and plant material. Surprisingly, U was also adsorbed to clay minerals and OM-coated clay minerals. The dominance of OM-associated U provides a framework to understand U mobility in the shallow subsurface, and, in particular, emphasizes roles for desorption and colloid formation in its mobilization.


Contacts (BER PM)

Amy Swain
DOE Office of Biological and Environmental Research, Climate and Environmental Sciences Division

(PI contact)

John Bargar
SLAC National Accelerator Laboratory, Stanford Synchrotron Radiation Lightsource


Funding was provided by the DOE Office of Biological and Environmental Research, Subsurface Biogeochemistry Research (SBR) activity to the SLAC SFA program under contract DE-AC02-76SF00515 to SLAC. Use of SSRL is supported by the U.S. DOE, Office of Basic Energy Sciences.