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• W2285338889 abstract "Stream and river restoration activities have recently begun to emphasize the enhancement of biogeochemical processing within river networks through the restoration of river-floodplain connectivity. It is generally accepted that this practice removes pollutants such as nitrogen and phosphorus because the increased contact time of nutrient-rich floodwaters with reactive floodplain sediments. Our study examines this assumption in the floodplain of a recently restored, low-order stream through five seasonal experiments. During each experiment, a floodplain slough was artificially inundated for 3 h. Both the net flux of dissolved nutrients and nitrogen uptake rate were measured during each experiment. The slough was typically a source of dissolved phosphorus and dissolved organic matter, a sink of NO3(-), and variable source/sink of ammonium. NO3(-) uptake rates were relatively high when compared to riverine uptake, especially during the spring and summer experiments. However, when scaled up to the entire 1 km restoration reach with a simple inundation model, less than 0.5-1.5% of the annual NO3(-) load would be removed because of the short duration of river-floodplain connectivity. These results suggest that restoring river-floodplain connectivity is not necessarily an appropriate best management practice for nutrient removal in low-order streams with legacy soil nutrients from past agricultural landuse." @default.
• W2285338889 created "2016-06-24" @default.
• W2285338889 creator A5038339435 @default.
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• W2285338889 date "2015-10-28" @default.
• W2285338889 modified "2023-09-27" @default.
• W2285338889 title "Seasonal Variation in Floodplain Biogeochemical Processing in a Restored Headwater Stream" @default.
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• W2285338889 doi "https://doi.org/10.1021/acs.est.5b02426" @default.
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• W2285338889 hasPublicationYear "2015" @default.
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