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Published online 9 August 2006
Published in J Environ Qual 35:1742-1755 (2006)
DOI: 10.2134/jeq2005.0373
© 2006 American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America
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TECHNICAL REPORTS

Landscape and Watershed Processes

Nitrogen Loads through Baseflow, Stormflow, and Underflow to Rehoboth Bay, Delaware

J. A. Volka, K. B. Savidgeb, J. R. Scudlarkb, A. S. Andresc and W. J. Ullmanb,*

a Watershed Assessment Section, Delaware Department of Natural Resources and Environmental Control, 820 Silver Lake Boulevard, Suite 220, Dover, DE 19904
b College of Marine Studies, University of Delaware, 700 Pilottown Road, Lewes, DE 19958-1298
c Delaware Geological Survey, University of Delaware, Newark, DE 19716-7501

* Corresponding author (ullman{at}udel.edu)

Received for publication September 26, 2005. A detailed study of water and nitrogen (N) discharge from a small, representative subwatershed of Rehoboth Bay, Delaware, was conducted to determine total N loads to the bay. The concentrations of ammonium (NH4+), nitrate + nitrite (NO3 + NO2), and dissolved and particulate organic N were determined in baseflow and storm waters discharging from Bundicks Branch from October 1998 to April 2002. A novel hydrographic separation model that accounts for significant decreases in baseflow during storm events was developed to estimate N loads during unsampled storms. Nitrogen loads based on gauged flows alone (7100–19 100 kg/yr) significantly underestimated those based on land use–land cover (LULC) and estimated N export factors from different classes of LULC (32 000–40 600 kg/yr). However, when ungauged underflow and associated N loads were included in the total loads (25500–33800 kg/yr), there was much better agreement with LULC export models. This suggests that in permeable coastal plain sediments, underflow contributes significantly to N fluxes to estuarine receiving waters, particularly in drier years. Based on the similarity in LULC, N loads from the Bundicks Branch subwatershed were used to estimate upland loads to the entire Rehoboth Bay Watershed (259 000–316000 kg/yr). These N loads from the watershed were much greater than those from direct atmospheric deposition (49000–64 500 kg/yr) and from a local wastewater treatment plant (9700–13700 kg/yr). While the watershed was the principal source of N at all times during the year, the relative contributions from the watershed, wastewater, and direct atmospheric deposition varied predictably with season.

Abbreviations: LULC, land use–land cover • PON, particulate organic nitrogen • RBWTP, Rehoboth Beach Wastewater Treatment Plant • TDN, total dissolved nitrogen • TN, total nitrogen




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