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Published online 27 October 2006
Published in J Environ Qual 35:2026-2042 (2006)
DOI: 10.2134/jeq2005.0249
© 2006 American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
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Field Evaluation of a Model for Predicting Nitrogen Losses from Drained Lands

Mohamed A. Youssefa,*, R. Wayne Skaggsa, George M. Chescheira and J. Wendell Gilliamb

a Department of Biological and Agricultural Engineering., North Carolina State University, Raleigh, NC 27695
b Department of Soil Science, North Carolina State University, Raleigh, NC 27695


Figure 1
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Fig. 1. The N cycle as modeled in DRAINMOD-N II.

 

Figure 2
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Fig. 2. The carbon cycle as modeled in DRAINMOD-N II (MET = metabolic; STR = structural; LGN = lignin; CEL = cellulose; MCR = microbe; SURF = surface; ACT = active; SLO = slow; PAS = passive).

 

Figure 3
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Fig. 3. General layout of the research site at the Tidewater Experiment Stn., Plymouth, NC.

 

Figure 4
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Fig. 4. Nitrogen uptake functions for crops grown on the TES site from 1992 through 1997.

 

Figure 5
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Fig. 5. Observed and simulated water table depths for plot 3 from 1992 through 1994.

 

Figure 6
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Fig. 6. Observed and simulated water table depths for plot 4 from 1992 through 1994.

 

Figure 7
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Fig. 7. Observed and simulated subsurface drainage for plot 3 from 1992 through 1994.

 

Figure 8
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Fig. 8. Observed and simulated subsurface drainage for plot 4 from 1992 through 1994.

 

Figure 9
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Fig. 9. Scatter diagram comparing observed and predicted monthly NO3–N losses with drain flow for plots 2 through 5 from 1992 through 1997.

 

Figure 10
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Fig. 10. Observed and predicted NO3–N loss via subsurface drainage for plot 3 from 1992 through 1994.

 

Figure 11
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Fig. 11. Observed and predicted NO3–N loss via subsurface drainage for plot 4 from 1992 through 1994.

 

Figure 12
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Fig. 12. Observed and predicted cumulative rates of subsurface drainage and NO3–N leaching loss for experimental plots 2 through 5 from 1992 through 1997.

 





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