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Storm NO₃⁻ and NH₄⁺ Exports in Stream, Overland Flow, and Tile Drains of the US Midwest

Philippe Vidon, The State University of New York College of Environmental Science and Forestry
Hilary Hubbard, Indiana University - Purdue University, Indianapolis
Pilar Cuadra, Indiana University - Purdue University, Indianapolis
Matthew Hennessy, Indiana University - Purdue University, Indianapolis

Keywords

subsurface drainage, nitrogen, export rates, precipitation, runoff, overland flow

Publication Date

9-19-2012

Subject Areas

Environmental Hydrology, Agriculture, Environmental Science, Environmental Analysis, Pollution, Fertilizers

Abstract

A better understanding of the dynamics of nitrogen (N) losses to streams during storms in agro-ecosystems of the US Midwest is critical to better understand how to mitigate N pollution in the Mississippi River Basin. This study investigates storm NO3- and NH4+ concentrations and fluxes in tile drains, overland flow and stream water in relation to bulk precipitation and antecedent moisture conditions. For moderate size spring storms (1.0 - 4.5 cm bulk precipitation), the occurrence of overland flow was primarily associated with high antecedent moisture conditions, but had no direct effect on stream NO3- and NH4+ concentrations. Mean storm NO3- and NH4+ concentrations in the stream and tile drains were also not significantly correlated (p>0.05) to either bulk precipitation or antecedent moisture conditions. Nevertheless, mean stream NO3- concentrations (7.50 mg N/L) were on average 28% lower than in tile drains (10.38 mg N/L). No significant difference in NH4+ concentrations were observed between the stream (0.06 mg N/L) and tile drains (0.05 mg N/L). NO3- and NH4+ fluxes were positively correlated with bulk precipitation (p < 0.05) and high fluxes were typically associated with wet antecedent moisture conditions. Specific NO3- fluxes in tile drains (750 g N/ha/storm) were approximately 2 times larger than in the stream (398 g N/ha/storm). Such differences were not observed for NH4+ fluxes. Considering the positive correlation between storm NO3- fluxes and stream NO3- baseflow concentrations (r = 0.87, p < 0.05), it is likely that one of the most efficient strategies for reducing N losses at the watershed scale may simply lie in reducing N inputs to cropland, as opposed to trying to manage N after it is applied to fields.

Permanent URL

http://hdl.handle.net/2047/d20002606

Recommended Citation

Vidon, Philippe; Hubbard, Hilary; Cuadra, Pilar; and Hennessy, Matthew (2012) "Storm NO₃⁻ and NH₄⁺ Exports in Stream, Overland Flow, and Tile Drains of the US Midwest," Annals of Environmental Science: Vol. 6, Article 5.
Available at: http://hdl.handle.net/2047/d20002606

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