Published online 7 May 2007
Published in J Environ Qual 36:846-854 (2007)
DOI: 10.2134/jeq2005.0359
© 2007 American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
Nitrogen and Phosphorus Runoff Losses from Variable and Constant Intensity Rainfall Simulations on Loamy Sand under Conventional and Strip Tillage Systems
D. Franklina,*,
C. Trumanb,
T. Potterb,
D. Boschb,
T. Stricklandb and
C. Bednarzc
a USDA-ARS, J. Phil Campbell, Sr. Natural Resource Conservation Center, Watkinsville, GA 30677
b USDA-ARS, Southeast Watershed Research Lab., Tifton, GA 31793
c Univ. of Georgia, Coastal Plain Experiment Station, Tifton, GA 31793

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Fig. 2. Soil-extractable Mechlich I P (STP), water-soluble P (WSP), and NO3N before rainfall simulations, with depth and between tillage treatments: strip tillage (ST) and conventional tillage (CT). Errors bars are standard deviations.
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Fig. 3. (A) Cumulative flow-weighted concentrations of NH4N for 70 min of runoff, and (B) cumulative NH4N losses. The symbol at each 5-min period represents a composite sample for that time period and treatment. Gray shading indicates a significant difference (p < 0.05) between tillage treatments strip tillage (ST) and conventional tillage (CT). Black shading indicates a significant difference (p < 0.05) between rainfall intensity patterns, constant rate (Ic) and variable rate (Iv). The symbol ¤ indicates interaction was significant (p < 0.05) between tillage and intensity pattern for runoff periods (5 min) above which are labeled. In graph A, the inserted graph depicts runoff rates for each treatment studied.
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Fig. 4. Soil KCl-extractable NH4N with depth. Errors bars are standard deviations. (A) Soil concentrations determined from soil samples taken immediately before rain; (B) soil concentrations determined from soil samples taken 1 h after end of simulation.
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Fig. 5. (A) Cumulative flow-weighted concentrations of NO3N for 70 min of runoff, and (B) cumulative NO3N losses. Gray shading indicates a significant difference (p < 0.05) between tillage treatments, strip tillage (ST) and conventional tillage (CT). Black shading indicates a significant difference (p < 0.05) between rainfall intensity patterns, constant rate (Ic) and variable rate (Iv). The symbol ¤ indicates interaction was significant (p < 0.05) between tillage and intensity pattern for runoff periods above which are labeled.
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Fig. 6. (A) Cumulative flow-weighted concentrations of total N (TKN) for 70 min of runoff, and (B) cumulative total N (TKN) losses. Gray shading indicates a significant difference (p < 0.05) between tillage treatments strip tillage (ST) and conventional tillage (CT). Black shading indicates a significant difference (p < 0.05) between rainfall intensity patterns, constant rate (Ic) and variable rate (Iv). The symbol ¤ indicates interaction was significant (p < 0.05) between tillage and intensity pattern for runoff periods (5 min) above which are labeled.
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Fig. 7. (A) Cumulative flow-weighted concentrations of PO4P for 70 min of runoff, and (B) cumulative PO4P losses. Gray shading indicates a significant difference (p < 0.05) between tillage treatments, strip tillage (ST) and conventional tillage (CT). Black shading indicates a significant difference (p < 0.05) between rainfall intensity patterns, constant rate (Ic) and variable rate (Iv). The symbol ¤ indicates interaction was significant (p < 0.05) between tillage and intensity pattern for runoff periods above which are labeled.
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Fig. 8. (A) Cumulative flow-weighted concentrations of total P (TKP) for 70 min of runoff, and (B) total P losses. Gray shading indicates a significant difference (p < 0.05) between tillage treatments, strip tillage (ST) and conventional tillage (CT). Black shading indicates a significant difference (p < 0.05) between rainfall intensity patterns, constant rate (Ic) and variable rate (Iv). The symbol ¤ indicates interaction was significant (p < 0.05) between tillage and intensity pattern for runoff periods above which are labeled.
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Copyright © 2007 by the American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America.