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Seasonal Variation in Nitrate Removal Mechanisms in Coastal Stormwater Ponds
Author(s) -
Gold Adam C.,
Thompson Suzanne P.,
Piehler Michael F.
Publication year - 2021
Publication title -
water resources research
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.863
H-Index - 217
eISSN - 1944-7973
pISSN - 0043-1397
DOI - 10.1029/2021wr029718
Subject(s) - stormwater , environmental science , sediment , denitrification , nitrate , surface runoff , hydrology (agriculture) , nutrient , environmental chemistry , water quality , nitrification , organic matter , nitrogen , ecology , chemistry , geology , biology , paleontology , geotechnical engineering , organic chemistry
Stormwater wet ponds (SWPs) are engineered structures used to collect and retain stormwater runoff from developed areas. SWPs are generally regarded as important nitrogen (N) sinks, but seasonal variation in SWP N cycling that influences pond nitrogen removal has not been characterized. To inform SWP function across seasons, we sampled the sediments and water columns of three stormwater ponds in the southeastern US coastal plain and measured gas and nutrient fluxes from the sediment‐water interface during ambient conditions and nitrate (NO 3 )‐enriched “simulated storm” conditions. Dissolved organic nitrogen (DON) was the dominant form of dissolved N in the water column, while nitrate + nitrite (NO x ) was typically below detection. SWP sediment organic matter properties varied by study site but had minimal impact on sediment N processes or estimated NO 3 fate. SWP sediments generally functioned as TN sinks during NO 3 ‐enriched conditions, but the estimated fate of NO 3 varied based on water temperature, DON concentrations, and sediment O 2 uptake. These results suggest that permanent N removal (denitrification) by SWPs varies seasonally, with retention of NO x becoming more important during hotter conditions when NO x uptake is largest. Low ambient NO x concentrations and rapid NO 3 uptake suggest that coastal stormwater ponds can host reduced conditions that may promote NO 3 retention over denitrification. Additional research is needed to determine the fate of retained NO 3 in SWP sediments and how variation in NO 3 fate might impact downstream water quality.