4.7 Article

Phosphorus dynamics in tile-drain flow during storms in the US Midwest

Journal

AGRICULTURAL WATER MANAGEMENT
Volume 98, Issue 4, Pages 532-540

Publisher

ELSEVIER SCIENCE BV
DOI: 10.1016/j.agwat.2010.09.010

Keywords

Non-point source pollution; Macropore flow; Matrix flow; Particulate phosphorus; Soluble reactive phosphorus; Rainfall events; Drainage

Funding

  1. United States Geological Survey (USGS) [06HQGR0084]
  2. Indiana University, Indianapolis
  3. Purdue University, Indianapolis

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Excess phosphorus phosphorus (P) in freshwater systems has been associated with eutrophication in agro-ecosystems of the US Midwest and elsewhere. A better understanding of processes regulating both soluble reactive phosphorus (SRP) and total phosphorus (TP) exports to tile-drains is therefore critical to minimize P losses to streams while maintaining crop yield. This paper investigates SRP and TP dynamics at a high temporal resolution during four spring storms in two tile-drains in the US Midwest. Depending on the storm, median concentrations varied between 0.006-0.025 mg/L for SRP and 0.057-0.176 mg/L for TP. For large storms (>6 cm bulk precipitation), for which macropore flow represented between 43 and 50% of total tile-drain flow, SRP transport to tile-drains was primarily regulated by macropore flow. For smaller tile-flow generating events (<3 cm bulk precipitation), for which macropore flow only accounted for 11-17% of total tile-drain flow, SRP transport was primarily regulated by matrix flow. Total P transport to tile-drains was primarily regulated by macropore flow regardless of the storm. Soluble reactive P (0.01-1.83 mg m(-2)/storm) and TP (0.10-8.64 mg m(-2)/storm) export rates were extremely variable and positively significantly correlated to both mean discharge and bulk precipitation. Soluble reactive P accounted for 9.9-15.5% of TP fluxes for small tile-flow generating events (<3 cm bulk precipitation) and for 16.2-22.0% of TP fluxes for large precipitation events (>6 cm bulk precipitation). Although significant variations in tile-flow response to precipitation were observed, no significant differences in SRP and TP concentrations were observed between adjacent tile-drains. Results stress the dominance of particulate P and the importance of macropore flow in P transport to tile-drains in the US Midwest. Although only spring storms are investigated, this study brings critical insight into P dynamics in tile-drains at a critical time of the year for water quality management. (C) 2010 Elsevier B.V. All rights reserved.

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