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Published online 25 January 2007
Published in J Environ Qual 36:343-353 (2007)
DOI: 10.2134/jeq2006.0019
© 2007 American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America
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Nitrate Retention in Riparian Ground Water at Natural and Elevated Nitrate Levels in North Central Minnesota

John H. Duffa,*, Alan P. Jackmanb, Frank J. Triskaa, Richard W. Sheibleyb and Ronald J. Avanzinoa

a U.S. Geological Survey, Water Resources Division, 345 Middlefield Road, MS 439, Menlo Park, CA 94025
b Dep. of Chemical Engineering and Materials Science, Univ. of California, Davis, CA 95616


Figure 1
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Fig. 1. (a) Map of the study area consisting of the Upper Shingobee River watershed, (b) the location of well Transects 1 and 2 in relation to the relict beaver dam, and (c) a close up of the Experimental Well Array on the alluvial deposit.

 

Figure 2
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Fig. 2. Contour interpolation of the piezometric water levels in the alluvial wells averaged over six dates between 1996 and 1998. Elevations are in cm measured with respect to well SHW 12.

 

Figure 3
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Fig. 3. Chloride concentration in Experimental Array Wells 1 through 4 during Injection 4, September 1998.

 

Figure 4
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Fig. 4. Nitrate–N/halide ratios for Experimental Array Wells 1 through 3 during (a) Injection 1, January 1998, and (b) Injection 2, January 1998. (c) Dissolved oxygen (DO) concentration during Injection 2, January 1998. Injection 1 consisted of bromide and nitrate (NO3). Injection 2 consisted of chloride, NO3, glucose, and acetylene.

 

Figure 5
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Fig. 5. Nitrogen/chloride ratios for nitrate (NO3), nitrite (NO2), and nitrous oxide (N2O) in Experimental Array Wells 1 through 3 (a, b, and c, respectively) during Injection 2 in January 1998. Injection 2 consisted of chloride, NO3, glucose, and acetylene.

 

Figure 6
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Fig. 6. Bromide (Br), nitrate (NO3), and dissolved oxygen (DO) concentration in Experimental Array Well 1 during Injection 3 in September 1998. Injection 3 consisted of Br and glucose.

 

Figure 7
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Fig. 7. Nitrate (NO3) predicted by chloride if NO3 was transported conservatively, and observed NO3, nitrite (NO2), and nitrous oxide (N2O) in Experimental Array Wells (a) 1, (b) 2, and (c) 3 in September 1998. Injection 4 consisted of chloride, NO3, glucose, and acetylene.

 





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