Published online 5 January 2006
Published in J Environ Qual 35:303-311 (2006)
DOI: 10.2134/jeq2005.0093
© 2006 American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
Diuron in Surface Runoff and Tile Drainage from Two Grass-Seed Fields
David E. Ruppa,*,
R. Edward Peacheyb,
Kristina L. Warrena,c and
John S. Selkera
a Department of Bioengineering, Oregon State University, Corvallis, OR 97331
b Department of Horticulture, Oregon State University, Corvallis, OR 97331
c present address: Camp, Dresser & McKee, 11811 NE 1st Street, Suite 201, Bellevue, WA 98005.

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Fig. 1. Map of Field 1 with inset showing the location of the Willamette Basin, OR. Fields 1-W and 1-E are separated by a low berm running northsouth to just south of the diversion pipe inlet. Sheet metal walls inserted 5 cm into the soil extend southwestward from the inlet of the diversion pipe to divert surface flow into the pipe. The heavy solid line bounds the surface area in Field 1-W monitored above the diversion pipe inlet. The gray rectangles show the approximate areas monitored by the flow meters inserted in the tile drain systems in Fields 1-W and 1-E.
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Fig. 2. Map of Field 2. A low berm on the west side of the field directs runoff toward the flumes. A ditch separates the field from the road to the east. The heavy solid line bounds the surface area monitored above the flumes.
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Fig. 3. Field 1 (a) rainfall and surface runoff intensity and (b) diuron concentrations in surface runoff and tile drainage for the 20012002 wet season. Diuron was applied on 15 Sept. 2001. Runoff monitoring began on 6 Nov. 2001 (dashed vertical line) and was stopped in June 2002. The detection limit is 0.02 µg L1.
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Fig. 4. Field 2 (a) rainfall and surface runoff intensity and (b) diuron concentrations in surface runoff and tile drainage for the 20022003 wet season. Diuron was applied on 18 Oct. 2002. The dashed vertical lines in (a) bound the period of surface runoff monitoring. The detection limit is 0.02 µg L1.
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Fig. 5. Diuron concentration (Cl) in surface runoff against dimensionless time (t*) and dimensionless cumulative rainfall (R*) for Field 1-W.
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Fig. 6. Diuron concentration (Cl) in surface runoff against dimensionless time (t*) and dimensionless cumulative rainfall (R*) for Field 2-S.
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Fig. 7. Diuron concentration (Cl) in tile drainage against dimensionless time (t*) and dimensionless cumulative rainfall (R*) for Field 2-N.
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Copyright © 2006 by the American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America.