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Tillage and Nutrient Source Effects on Surface and Subsurface Water Quality at Corn Planting

Suling L. Zhaoa, Satish C. Guptab, David R. Hugginsc and John F. Moncriefb

a Resource 21, 7257 S. Tucson Way, Suite 200, Englewood, CO 80112
b Dep. of Soil Water, and Climate, 1991 Upper Buford Circle, Univ. of Minnesota, St. Paul, MN 55108
c USDA-ARS, Dep. of Crop and Soil Sciences, Washington State Univ., Pullman, WA 99164



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Fig. 1. Plot layout of the experiment on tillage and nutrient source effect on water quality of surface runoff and subsurface tile flow at the Southwest Research and Outreach Center, Lamberton, MN.

 


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Fig. 2. An example of the variation in cumulative flow and flow rate through tile lines as a function of time for moldboard plow with manure (MP*M), moldboard plow with urea (MP*U), ridge tillage with manure (RT*M), and ridge tillage with urea (RT*U) treatments on a Webster clay loam soil.

 


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Fig. 3. An example of the variation in sediment concentration in tile line flow as a function of time for moldboard plow with manure (MP*M), moldboard plow with urea (MP*U), ridge tillage with manure (RT*M), and ridge tillage with urea (RT*U) treatments on a Webster clay loam soil.

 


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Fig. 4. An example of the variation in NH+4–N and NO-3–N concentration in tile line flow as a function of time for moldboard plow with manure (MP*M), moldboard plow with urea (MP*U), ridge tillage with manure (RT*M), and ridge tillage with urea (RT*U) treatments on a Webster clay loam soil.

 





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The SCI Journals Agronomy Journal Crop Science
Journal of Natural Resources
and Life Sciences Education
Vadose Zone Journal
Soil Science Society of America Journal Journal of Plant Registrations The Plant Genome
Copyright © 2001 by the American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America.