Published January 8, 2018 | Version v1
Journal article Open

Comparison of performance of tile drainage routines in SWAT 2009 and 2012 in an extensively tile-drained watershed in the Midwest

  • 1. National Center for Water Quality Research
  • 2. Purdue University
  • 3. Grassland Soil and Water Research Laboratory
  • 4. Texas A&M University
  • 5. University of Illinois Urbana-Champaign

Description

ABSTRACT

Subsurface tile drainage systems are widely used in agricultural watersheds in the Midwestern US and enable the Midwest area to become highly productive agricultural lands, but can also create environmental problems, for example nitrate-N contamination associated with drainage waters. The Soil and Water Assessment Tool (SWAT) has been used to model watersheds with tile drainage. SWAT2012 revisions 615 and 645 provide new tile drainage routines. However, few studies have used these revisions to study tile drainage impacts at both field and watershed scales. Moreover, SWAT2012 revision 645 improved the soil moisture based curve number calculation method, which has not been fully tested. This study used long-term (1991–2003) field site and river station data from the Little Vermilion River (LVR) watershed to evaluate performance of tile drainage routines in SWAT2009 revision 528 (the old routine) and SWAT2012 revisions 615 and 645 (the new routine). Both the old and new routines provided reasonable but unsatisfactory (NSE <0.5) uncalibrated flow and nitrate loss results for a mildly sloped watershed with low runoff. The calibrated monthly tile flow, surface flow, nitrate-N in tile and surface flow, sediment and annual corn and soybean yield results from SWAT with the old and new tile drainage routines were compared with observed values. Generally, the new routine provided acceptable simulated tile flow (NSE = 0.48–0.65) and nitrate in tile flow (NSE = 0.48–0.68) for field sites with random pattern tile and constant tile spacing, while the old routine simulated tile flow and nitrate in tile flow results for the field site with constant tile spacing were unacceptable (NSE = 0.00–0.32 and -0.29–0.06, respectively). The new modified curve number calculation method in revision 645
(NSE = 0.50–0.81) better simulated surface runoff than revision 615 (NSE = -0.11–0.49). The calibration provided reasonable parameter sets for the old and new routines in the LVR watershed, and the validation results showed that the new routine has the potential to accurately simulate hydrologic processes in mildly sloped watersheds.

Notes

The data used in this publication from the Little Vermilion River Watershed were a contribution of the Illinois Agricultural Experiment Station, University of Illinois at Urbana-Champaign as a part of Projects 10-309 and 10-301 and Southern Regional Research Project S-1004 (formerly S-249 and S-273). Supported in part with funds from USDA-CSREES under special projects 91-EHUA-1-0040 and 95-EHUA-1-0123, NRI project 9501781, and Special Project 95-34214-2266 (Purdue subcontract 590-1145-2417-01). In addition, this work was supported with funds from the Illinois Council on Food and Agricultural Research and with the assistance of the Champaign County Soil and Water Conservation District which sponsored the installation of the County Line gaging station. Faculty from the Department of Agricultural Engineering supervising the collection and reduction of these data were J. Kent Mitchell, Michael C. Hirschi, Prasanta Kalita, and Richard A. C. Cooke.

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