期刊
ESTUARIES AND COASTS
卷 45, 期 5, 页码 1287-1304出版社
SPRINGER
DOI: 10.1007/s12237-021-01029-7
关键词
Stable isotopes; Ulva; Atmospheric deposition; Stormwater; Wastewater treatment; Eutrophication
资金
- Institute at Brown for Environment and Society (Voss Undergraduate Research Fellowship)
- National Science Foundation [AGS-1351932]
- National Science Foundation Research Experiences for Undergraduates Site Award [EAR-1852273]
Anthropogenic impacts on nitrogen cycling have changed ecosystems globally, particularly in coastal estuaries. The study in the Narragansett Bay, RI, showed the direct impact of precipitation-derived nitrogen on nutrient dynamics, especially in summer phytoplankton blooms. Further research is needed to understand the magnitude and spatial heterogeneity of precipitation-derived nitrogen in a future wetter climate.
Anthropogenic changes to nitrogen cycling have dramatically altered ecosystems across the globe, particularly in coastal estuaries where nitrogen limits primary production. The impacts of nitrogen pollution are especially evident in Narragansett Bay, RI, where eutrophication in the urbanized Providence River Estuary persists despite a > 50% decrease in wastewater nitrogen loading over the past two decades. Precipitation-derived nitrogen tends to be understudied and may be underestimated in contemporary budgets. Here, the magnitude and ecological impacts of precipitation-derived nitrogen in the Providence River Estuary were assessed by the following: relationships between precipitation, river discharge, and chlorophyll abundance; inorganic nitrogen concentration and isotopic composition of precipitation, surface runoff, and stormwater; and changes in stable nitrogen (delta N-15) and carbon (delta C-13) isotopes of macroalgae (Ulva spp.) after large precipitation events. Precipitation and chlorophyll concentration measured 5 days after the rain event exhibited a linear relationship. Furthermore, Ulva spp. experienced decreases in delta N-15 of 0.3-1 parts per thousand and increases in delta C-13 of 1-3 parts per thousand that peaked 5 days after precipitation events. These results are indicative of a direct impact of precipitation-derived nitrogen on nutrient dynamics, including summer phytoplankton blooms. However, the inorganic nitrogen concentrations of stormwater were approximately 240% higher than surface runoff, and the isotopic composition of stormwater discharge indicates that most precipitation-derived nitrate stems from terrestrial nitrogen and sewage rather than direct atmospheric deposition. The magnitude and spatial heterogeneity of precipitation-derived nitrogen remains uncertain, and further work is needed to understand how this nitrogen source will change in a wetter climate of the future.
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