The role of sediment denitrification in reducing groundwater-derived nitrate inputs to Nauset Marsh estuary, Cape Cod, Massachusetts

Nowicki BL, Requintina E, Van D, Portnoy J. 1999. The role of sediment denitrification in reducing groundwater-derived nitrate inputs to Nauset Marsh estuary, Cape Cod, Massachusetts. Estuaries. 22(2A):245-259

The Nauset Marsh estuary is the most extensive (9.45 km(2)) and least disturbed salt marsh/estuarine system within the Cape Cod National Seashore, even though much of the 19 km(2) watershed area of the estuary is developed for residential or commercial purposes, Because all of the Nauset watershed is serviced by on-sire individual sewage disposal systems, there is concern over the potential impact of groundwater-derived nutrients passing from these systems to the shallow receiving waters of the estuary. The purpose of this study was to determine whether denitrification (the bacterial conversion of nitrate to gaseous nitrogen) in estuarine sediments could effectively remove the nitrate from contaminated groundwater before it passed from the watershed to the estuary. Rates of denitrification were measured both in situ and in sediment cores, in areas of active groundwater discharge, in relatively pristine locations, and in areas situated down-gradient of moderate to heavily developed regions of the watershed. Denitrification rates for 47 sediment cores taken over an annual cycle at 5 stations ranged from non-detectable to 47 mu mol N-2 m(-2) h(-1). Mean denitrification rates were positively correlated with sediment organic content, and varied seasonally due to changes in sediment organic content and to the effect of water temperatures on sediment oxygen penetration depths. There was no correlation between observed denitrification rates and corresponding nitrate concentrations in groundwater. A comparison of in situ denitrification rates (supported by groundwater nitrate) with denitrification rates observed in sediment cores (supported by remineralized nitrate) showed that groundwater-driven denitrification rates were small, and not in excess of denitrification rates supported by remineralized nitrate. Most of the denitrification in Nauset sediments was apparently fueled by remineralized nitrate through coupled nitrification/ denitrification. Denitrification did not con

Type
Journal Article
Authors
Nowicki, Barbara; Requintina, Edwin; Van, D; Portnoy, J
Units
BOHA
Keywords
Aarhus Bight, Boston Harbor, Coastal Waters, contaminated Groundwater, Mass Balance, Nearshore Marine Sediments, Norsminde Fjord, North Atlantic Ocean, Nutrient Enrichment, Seasonal variation

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