Journal
SCIENCE OF THE TOTAL ENVIRONMENT
Volume 838, Issue -, Pages -Publisher
ELSEVIER
DOI: 10.1016/j.scitotenv.2022.156439
Keywords
Managed aquifer recharge (MAR); Trace metals; Nitrogen cycling; Water quality; Soil microbiology; Groundwater supply
Categories
Funding
- Gordon and Betty Moore Foundation [5595, 9964]
- UC Water Security and Sustainability Research Initiative (UCOP) [13941]
- USDA/NIFA [2017-6702626315, 2021-67019-33595]
- USDA/NRCS Resource Conservation Partnership Program [2019-CSA-03]
- Recharge Initiative
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This study presents the effects of adding a carbon-rich, permeable reactive barrier (PRB) on nitrogen cycling and trace metal mobilization during rapid infiltration. The results show that the addition of a carbon-rich PRB can improve water quality, reduce nitrogen load, and enhance the removal of dissolved nitrogen species.
We present results from a series of plot-scale field experiments to quantify physical infiltration dynamics and the influence of adding a carbon-rich, permeable reactive barrier (PRB) for the cycling of nitrogen and associated trace metals during rapid infiltration for managed aquifer recharge (MAR). Recent studies suggest that adding a bio-available carbon source to soils can enhance denitrification rates and associated N load reduction during moderate-to-rapid infiltration (<= 1 m/day). We examined the potential for N removal during faster infiltration (>1 m/day), through coarse and carbon-poor soils, and how adding a carbon-rich PRB (wood chips) affects subsurface redox conditions and trace metal mobilization. During rapid infiltration, plots amended with a carbon-rich PRB generally demonstrated modest increases in subsurface loads of dissolved organic carbon, nitrite, manganese and iron, decreases in loads of nitrate and ammonium, and variable changes in arsenic. These trends differed considerably from those seen during infiltration through native soil without a carbon-rich PRB. Use of a carbon-rich soil amendment increased the fraction of dissolved N species that was removed at equivalent inflowing N loads. There is evidence that N removal took place primarily via denitrification. Shifts in microbial ecology following infiltration in all of the plots included increases in the relative abundances of microbes in the families Comamonadaceae, Pseudomonadaceae, Methylophilaceae, Rhodocyclaceae and Sphingomonadaceae, all of which contain genera capable of carrying out denitrification. These results, in combination with studies that have tested other soil types, flow rates, and system scales, show how water quality can be improved during infiltration for managed recharge, even during rapid infiltration, with a carbon-rich soil amendment.
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