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Transport and Fate of Nitrate in Headwater Agricultural Streams in Illinois

Todd V. Royera,c,*, Jennifer L. Tankb and Mark B. Davida

a Department of Natural Resources and Environmental Sciences, University of Illinois, 1102 South Goodwin Avenue, Urbana, IL 61801
b Department of Biological Sciences, University of Notre Dame, Notre Dame, IN 46556
c Department of Biological Sciences, Kent State University, 256 Cunningham Hall, Kent, OH 44242



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Fig. 1. Conceptual diagram of nutrient spiraling (modified from Newbold, 1992). The stream consists of two compartments, the water column (W) and the benthic sediments (B). In this model, uptake (U) of NO3–N is due to denitrification, making the uptake length denitrification-specific.

 


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Fig. 2. Mean daily water temperature and stream NO3–N concentrations at selected sites from January 2001 through January 2002. All sites showed similar patterns in temperature and NO3–N, and therefore only selected sites are shown. (Site characteristics are given in Table 1.)

 


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Fig. 3. Mean (plus one standard deviation) denitrification rates in August 2001 under ambient and amended conditions at two sites, BLS and BDO. (Site characteristics are given in Table 1.) Within a site, treatments with different letters are significantly different from each other (p < 0.05, Tukey's pairwise comparisons). AFDM, ash-free dry mass; DOC, dissolved organic carbon.

 


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Fig. 4. Calculated denitrification uptake length (Sw,dn) and measured stream water concentrations of NO3–N at sites BDO, LFK, and EMC, 1993–2002. (Site characteristics are given in Table 1.) The term Sw,dn was calculated using stream gaging records and an in-stream denitrification rate of 15 mg N m–2 h–1.

 


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Fig. 5. Relationship between mean daily discharge and stream NO3–N concentration for January 2001 through January 2002 in a headwater agricultural stream in Illinois. (Site characteristics are given in Table 1.)

 


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Fig. 6. (A) Nitrate concentrations at site BLS, January 2001 through January. (B) Mean daily nitrate load and measured rates of nitrate N loss, –k (% d–1), for site BLS. (Site characteristics are given in Table 1.)

 





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