资源环境科技发展态势分析平台

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 (NO₃)-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 NO₃ fate. SWP sediments generally functioned as TN sinks during NO₃-enriched conditions, but the estimated fate of NO₃ varied based on water temperature, DON concentrations, and sediment O₂ 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 NO₃ uptake suggest that coastal stormwater ponds can host reduced conditions that may promote NO₃ retention over denitrification. Additional research is needed to determine the fate of retained NO₃ in SWP sediments and how variation in NO₃ fate might impact downstream water quality.

This article is protected by copyright. All rights reserved.