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Published online 5 April 2007
Published in J Environ Qual 36:681-693 (2007)
DOI: 10.2134/jeq2006.0161
© 2007 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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Phosphorus Transport through Subsurface Drainage and Surface Runoff from a Flat Watershed in East Central Illinois, USA

A. S. Algoazanya, P. K. Kalitab,*, G. F. Czaparc and J. K. Mitchellb

a King Abdulaziz City for Science and Technology, GDRGP, P. O. Box 6086, Riyadh 11442, Saudi Arabia
b Dep. of Agricultural and Biological Engineering, Univ. of Illinois at Urbana-Champaign, 1304 W. Pennsylvania Avenue, Urbana, IL 61801 USA
c Univ. of Illinois Extension, Springfield Center, P.O. Box 8199, Springfield, IL 62791 USA


Figure 1
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  		Fig. 1. The Little Vermilion River (LVR) watershed and water quality monitoring stations for each site in the LVR watershed, IL.

 

Figure 2
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  		Fig. 2. Rainfall, subsurface flow, and surface runoff for each site in the Little Vermilion River (LVR) watershed, IL.

 

Figure 3
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  		Fig. 3. Monthly average flow volume for both subsurface and surface runoff and rainfall for the study sites at Little Vermilion River (LVR) watershed, IL.

 

Figure 4
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  		Fig. 4. Soluble phosphorus concentrations in subsurface flow and surface runoff for all stations at the Little Vermilion River (LVR) watershed, IL.

 

Figure 5
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  		Fig. 5. Soluble phosphorus concentrations and discharge in subsurface flow and surface runoff for all stations at the Little Vermilion River (LVR) watershed, IL.

 

Figure 6
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  		Fig. 6. Monthly average soluble phosphorus mass loads in subsurface flow and surface runoff in all study sites at Little Vermilion River (LVR) watershed, IL.

 




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