JEQ
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Published online 2 February 2006
Published in J Environ Qual 35:495-504 (2006)
DOI: 10.2134/jeq2005.0012
© 2006 American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
This Article
Right arrow Abstract Freely available
Right arrow Full Text Free
Right arrow Full Text (PDF) Free
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Similar articles in this journal
Right arrow Similar articles in Web of Science
Right arrow Similar articles in PubMed
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Web of Science (8)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Panno, S. V.
Right arrow Articles by Hwang, H.-H.
Right arrow Search for Related Content
PubMed
Right arrow PubMed Citation
Right arrow Articles by Panno, S. V.
Right arrow Articles by Hwang, H.-H.
Agricola
Right arrow Articles by Panno, S. V.
Right arrow Articles by Hwang, H.-H.
Related Collections
Right arrow Surface Water Quality
Right arrow Nitrogen
Right arrow Nutrients
Right arrow Nutrient Cycling
Right arrow Water Pollution

Isotopic Evidence of Nitrate Sources and Denitrification in the Mississippi River, Illinois

Samuel V. Pannoa,*, Keith C. Hackleya, Walton R. Kellyb and Hue-Hwa Hwanga

a Illinois State Geological Survey, Natural Resources Building, 615 E. Peabody Street, Champaign, IL 61820
b Illinois State Water Survey, 2204 Griffith Drive, Champaign, IL 61820-7495


Figure 1
View larger version (31K):

[in a new window]
 
Fig. 1. Sampling locations. The light gray area on the U.S. map shows the extent of the Mississippi River watershed.

 

Figure 2
View larger version (25K):

[in a new window]
 
Fig. 2. Ranges of {delta}18O and {delta}15N values for potential NO3 sources and values measured in Mississippi River and tile drain samples. The domain of soil organic matter is shaded to show the range of greatest (darkest) to lowest (lightest) frequency. The domain of soil organic matter partially overlaps that of reduced N fertilizer, manure, and sewage with respect to {delta}15N. The {delta}18O of NO3 from these reduced N sources was calculated as described in the discussion. The large arrow represents a denitrification vector; as denitrification proceeds, the {delta}15N and {delta}18O values of the remaining NO3 progressively increase in the direction of the vector. The size of circles represents NO3–N concentration; shaded circles indicate tile drain samples. In all cases, analytical errors are smaller than the circle size. Synthetic NO3 Fertilizer refers to synthetic fertilizer applied as NO3 (e.g., the NO3 in NH4NO3) and Reduced N Fertilizer refers to NO3 produced by nitrification of applied NH3 (as NH3 or the NH4+ in NH4NO3) and urea.

 

Figure 3
View larger version (16K):

[in a new window]
 
Fig. 3. Nitrate-N concentrations vs. (a) {delta}15N and (b) {delta}18O of NO3 for Mississippi River and tile drain samples. Letters indicate sample locations (D = Davenport, Q = Quincy, C = Chester). The gray hexagon represents the average composition of the four river samples collected in April 2004 at Quincy. The month of sample collection is shown for tile samples. Lines are linear regressions for river samples (r2 = 0.64 for {delta}15N and 0.61 {delta}18O).

 

Figure 4
View larger version (23K):

[in a new window]
 
Fig. 4. Detailed portion from Fig. 2, showing the two denitrification lines calculated from the two estimated initial {delta}15N and {delta}18O values (gray hexagons). Open symbols represent river samples, closed symbols represent tile drain samples. Letters indicate river sample locations (D = Davenport, Q = Quincy, C = Chester). Tick marks on the vectors indicate an estimation of the extent of denitrification (percentage of original NO3 lost, using {varepsilon} values of –15.9 for {delta}15N and –8 for {delta}18O in Eq. [3] for NO3 having initial values of 4.4{per thousand} for {delta}15N and 6.4{per thousand} for {delta}18O [solid lines] and for NO3 having initial values of 6.1{per thousand} for {delta}15N and 7.2{per thousand} for {delta}18O [dashed lines]).

 





HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
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 © 2006 by the American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America.