Publication | Open Access
Stormwater biofilter response to high nitrogen loading under transient flow conditions: Ammonium and nitrate fates, and nitrous oxide emissions
10
Citations
39
References
2022
Year
Nitrogen (N) in urban runoff is often treated with green infrastructure including biofilters. However, N fates across biofilters are insufficiently understood because prior studies emphasize low N loading under laboratory conditions, or use "steady-state" flow regimes over short time scales. Here, we tested field scale biofilter N fates during simulated storms delivering realistic transient flows with high N loading. Biofilter outflow ammonium (NH<sub>4</sub><sup>+</sup>-N) was 60.7 to 92.3% lower than that of the inflow. Yet the characteristic times for nitrification (days to weeks) and denitrification (days) relative to N residence times (7 to 30 h) suggested low N transformation across the biofilters. Still, across 7 successive storms, total outflow nitrate (NO<sub>3</sub><sup>-</sup>-N) greatly exceeded (3100 to 3900%) inflow nitrate, a result only explainable by biofilter soil N nitrification occurring between storms. Archaeal, and bacterial amoA gene copies (2.1 × 10<sup>5</sup> to 1.2 × 10<sup>6</sup> gc g soil<sup>-1</sup>), nitrifier presence by16S rRNA gene sequencing, and outflow δ<sup>18</sup>O-NO<sub>3</sub><sup>-</sup> values (-3.0 to 17.1 ‰) reinforced that nitrification was occurring. A ratio of δ<sup>18</sup>O-NO<sup>3-</sup> to δ<sup>15</sup>N-NO<sub>3</sub><sup>-</sup> of 1.83 for soil eluates indicated additional processes: N assimilation, and N mineralization. Denitrification potential was suggested by enzyme activities and soil denitrifying gene copies (nirK + nirS: 3.0 × 10<sup>6</sup> to 1.8 × 10<sup>7</sup>; nosZ: 5.0 × 10<sup>5</sup> to 2.2 × 10<sup>6</sup> gc g soil<sup>-1</sup>). However, nitrous oxide (N<sub>2</sub>O-N) emissions (13.5 to 84.3 μg N m <sup>-</sup> <sup>2</sup> h <sup>-</sup> <sup>1</sup>) and N<sub>2</sub>O export (0.014 g N) were low, and soil nitrification enzyme activities (0.45 to 1.63 mg N kg soil<sup>-1</sup>day<sup>-1</sup>) exceeded those for denitrification (0.17 to 0.49 mg N kg soil<sup>-1</sup> day<sup>-1</sup>). Taken together, chemical, bacterial, and isotopic metrics evidenced that storm inflow NH<sub>4</sub><sup>+</sup>sorbs and, along with mineralized soil N, nitrifies during biofilter dry-down; little denitrification and associated N<sub>2</sub>O emissions ensue, and thus subsequent storms export copious NO<sub>3</sub><sup>-</sup>-N. As such, pulsed pass-through biofilters require redesign to promote plant assimilation and/or denitrification of mineralized and nitrified N, to minimize NO<sub>3</sub><sup>-</sup>-N generation and export.
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