2009
DOI: 10.1016/j.gca.2009.08.026
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Denitrification coupled to pyrite oxidation and changes in groundwater quality in a shallow sandy aquifer

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Cited by 118 publications
(95 citation statements)
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References 26 publications
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“…The importance of DOC as an electron donor in aquifers depends on the subsurface setting [35]. Where solid phase components, such as organic matter and pyrite in the aquifer matrix are dominant [36], the electron donors are not replenished and can gradually be depleted with time [7]. Recent studies confirm the important role of pyrite for NO 3 2 removal in groundwater [35].…”
Section: Discussionmentioning
confidence: 99%
See 1 more Smart Citation
“…The importance of DOC as an electron donor in aquifers depends on the subsurface setting [35]. Where solid phase components, such as organic matter and pyrite in the aquifer matrix are dominant [36], the electron donors are not replenished and can gradually be depleted with time [7]. Recent studies confirm the important role of pyrite for NO 3 2 removal in groundwater [35].…”
Section: Discussionmentioning
confidence: 99%
“…As O 2 becomes limiting in the saturated zone, heterotrophic microorganisms increasingly switch to NO 3 2 as an electron acceptor for the oxidation of organic C. This organic C may be present in either dissolved form or as part of the sediment matrix. If pyrite is present in subsurface sediments, denitrification coupled to pyrite oxidation may become the dominant removal process [7]. Pyrite is a common iron disulfide mineral, and is often found in association with unconsolidated marine deposits in the terrestrial subsurface and in association with coal and shale deposits.…”
mentioning
confidence: 99%
“…However, a growing body of research suggests that denitrification in most aquifers depends on matrix-derived, solid-phase electron donors (e.g. Fe 2+ , H 2 S) rather than surface-derived solutes (Green et al, 2008;Schwientek et al, 2008;Zhang et al, 2009;Torrento et al, 2010Torrento et al, , 2011. As a result, concentrations of dissolved organic matter and other electron donors may be a poor indicator of denitrification rates across aquifers, and spatial patterns within aquifers may reflect the distribution of these reactants within the aquifer matrix rather than substrate depletion along advective flowpaths.…”
Section: Introductionmentioning
confidence: 99%
“…A potential source of carbon that may have helped support continued denitrification is dead biomass produced from die-off of bacterial populations that increased during the initial period when ethanol was present in high concentrations. Additionally, given the observed reduction of resident sulfate to sulfide during the tests, the reoxidation of sulfide back to sulfate (and attendant use of nitrate as an electron acceptor) as redox conditions reverted to natural conditions may have helped sustain the low nitrate concentrations (e.g., Robertson et al 1996;Pauwels et al 1998;Tesoriero et al 2000;Schwientek et al 2008;Zhang et al 2009). …”
Section: Resultsmentioning
confidence: 99%