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Abstract
Nitrogen export from small forested watersheds is known to be affected by N deposition but with high regional variability. We studied 10 headwater catchments in the northeastern United States across a gradient of N deposition (5.4 − 9.4 kg ha
−1 yr
−1) to determine if soil nitrification rates could explain differences in stream water NO
3− export. Average annual export of two years (October 2002 through September 2004) varied from 0.1 kg NO
3−-N ha
−1 yr
−1 at Cone Pond watershed in New Hampshire to 5.1 kg ha
−1 yr
−1 at Buck Creek South in the western Adirondack Mountains of New York. Potential net nitrification rates and relative nitrification (fraction of inorganic N as NO
3−) were measured in Oa or A soil horizons at 21–130 sampling points throughout each watershed. Stream NO
3− export was positively related to nitrification rates (
r2 = 0.34,
p = 0.04) and the relative nitrification (
r2 = 0.37,
p = 0.04). These relationships were much improved by restricting consideration to the 6 watersheds with a higher number of rate measurements (59–130) taken in transects parallel to the streams (
r2 of 0.84 and 0.70 for the nitrification rate and relative nitrification, respectively). Potential nitrification rates were also a better predictor of NO
3− export when data were limited to either the 6 sampling points closest to the watershed outlet (
r2 = 0.75) or sampling points <250 m from the watershed outlet (
r2 = 0.68). The basal area of conifer species at the sampling plots was negatively related to NO
3−export. These spatial relationships found here suggest a strong influence of near-stream and near-watershed-outlet soils on measured stream NO
3− export.
Citation
Ross, Donald S.; Shanley, James B.; Campbell, John L.; Lawrence, Gregory B.; Bailey, Scott W.; Likens, Gene E.; Wemple, Beverley C.; Fredriksen, Guinevere; Jamison, Austin E. 2012. Spatial patterns of soil nitrification and nitrate export from forested headwaters in the northeastern United States. Journal of Geophysical Research. 117(G1)