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1 July 2016 Sediment-Water Nitrogen Exchange along the Potomac River Estuarine Salinity Gradient
Jeffrey C. Cornwell, Michael S. Owens, Walter R. Boynton, Lora A. Harris
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Cornwell, J.C.; Owens, M.S.; Boynton, W.R., and Harris, L.A., 2016. Sediment-water nitrogen exchange along the Potomac River estuarine salinity gradient.

Observations of N2 efflux in estuarine sediments across the salinity gradient of the tidal Potomac River, a eutrophic subestuary of the Chesapeake Bay, were used to evaluate environmental controls of microbial denitrification. Rates of denitrification were measured using N2:Ar ratios in core incubations and were similar to other nitrogen-enriched estuaries, with summer and spring N2-N efflux rates averaging 54 ± 47 and 153 ± 97 μmol m−2 h−1, respectively. The paradigm of higher denitrification rates at lower salinities was not supported by observations during summer and spring conditions along this estuarine salinity gradient. Low bottom water oxygen concentrations in the lower, more saline part of the estuary resulted in low rates of coupled nitrification/denitrification. The most favorable region for denitrification in the tidal Potomac River occurred where changes in salinity were most rapid and oxygen concentrations were not depleted, with high rates observed within the estuarine turbidity maximum (ETM) zone. Overall, the key role of salinity in the tidal Potomac River in controlling denitrification appears to be in the focusing of materials into ETM and providing stratification in the lower estuary that restricts the vertical exchange of oxygen necessary for coupled nitrification/denitrification.

Jeffrey C. Cornwell, Michael S. Owens, Walter R. Boynton, and Lora A. Harris "Sediment-Water Nitrogen Exchange along the Potomac River Estuarine Salinity Gradient," Journal of Coastal Research 32(4), 776-787, (1 July 2016).
Received: 25 August 2015; Accepted: 16 September 2015; Published: 1 July 2016
Chesapeake Bay
estuarine biogeochemistry
estuarine turbidity maximum zone
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