Abstract
The processing of sediment to accurately characterize the spatially-resolved depth profiles of geophysical and geochemical properties along with signatures of microbial density and activity remains a challenge especially in complex contaminated areas. This study processed cores from two sediment boreholes from background and contaminated core sediments and surrounding groundwater. Fresh core sediments were compared by depth to capture the changes in sediment structure, sediment minerals, biomass, and pore water geochemistry in terms of major and trace elements including pollutants, cations, anions, and organic acids. Soil porewater samples were matched to groundwater level, flow rate, and preferential flows and compared to homogenized groundwater-only samples from neighboring monitoring wells. Groundwater analysis of nearby wells only revealed high sulfate and nitrate concentrations while the same analysis using sediment pore water samples with depth was able to suggest areas high in sulfate- and nitrate-reducing bacteria based on their decreased concentration and production of reduced by-products that could not be seen in the groundwater samples. Positive correlations among porewater content, total organic carbon, trace metals and clay minerals revealed a more complicated relationship among contaminant, sediment texture, groundwater table, and biomass. The fluctuating capillary interface had high concentrations of Fe and Mn-oxides combined with trace elements including U, Th, Sr, Ba, Cu, and Co. This suggests the mobility of potentially hazardous elements, sediment structure, and biogeochemical factors are all linked together to impact microbial communities, emphasizing that solid interfaces play an important role in determining the abundance of bacteria in the sediments.
Original language | English |
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Article number | 126951 |
Journal | Chemosphere |
Volume | 255 |
DOIs | |
State | Published - Sep 2020 |
Funding
We thank Kelley Meinhardt in the Stahl lab for performing the sediment gas measurements and Deanne Brice at ORNL for C&N analysis. We gratefully acknowledge D. Parkinson for assistance with tomography imaging at beamline 8.3.2 of the Advanced Light Source (ALS) at Lawrence Berkeley National Laboratory . The ALS is supported by the Director, Office of Science , Office of Basic Energy Sciences , of the U.S. Department of Energy under Contract DE-AC02-05CH11231 . This material by ENIGMA- Ecosystems and Networks Integrated with Genes and Molecular Assemblies ( http://enigma.lbl.gov ), a Scientific Focus Area Program at Lawrence Berkeley National Laboratory is based upon work supported by the U.S. Department of Energy, Office of Science, Office of Biological & Environmental Research under contract number DE-AC02-05CH11231. Oak Ridge National Laboratory is managed by UT-Battelle, LLC, for the U.S. Department of Energy under contract DE-AC05-00OR22725 . We thank Kelley Meinhardt in the Stahl lab for performing the sediment gas measurements and Deanne Brice at ORNL for C&N analysis. We gratefully acknowledge D. Parkinson for assistance with tomography imaging at beamline 8.3.2 of the Advanced Light Source (ALS) at Lawrence Berkeley National Laboratory. The ALS is supported by the Director, Office of Science, Office of Basic Energy Sciences, of the U.S. Department of Energy under Contract DE-AC02-05CH11231. This material by ENIGMA- Ecosystems and Networks Integrated with Genes and Molecular Assemblies (http://enigma.lbl.gov), a Scientific Focus Area Program at Lawrence Berkeley National Laboratory is based upon work supported by the U.S. Department of Energy, Office of Science, Office of Biological & Environmental Research under contract number DE-AC02-05CH11231. Oak Ridge National Laboratory is managed by UT-Battelle, LLC, for the U.S. Department of Energy under contract DE-AC05-00OR22725.
Keywords
- Bacteria
- Biomass
- Contaminants
- Groundwater
- Sediment
- Uranium