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Evaluating the source of streamwater nitrate using d15N and d18O in nitrate in two watersheds in New Hampshire, USA
Hydrological Processes. 18: 2699-2712.
The natural abundance of nitrogen and oxygen isotopes in nitrate can be a powerful tool for identifying the source of nitrate in streamwater in forested watersheds, because the two main sources of nitrate, atmospheric deposition and microbial nitrification, have distinct d18O values. Using a simple mixing model, we estimated the relative fractions in streamwater derived from these sources for two forested watersheds with markedly different streamwater nitrate outputs. In this study, we monitored a15N and dl80 of nitrate biweekly in atmospheric deposition and in streamwater for 20 months at the Hubbard Brook Experimental Forest, New Hampshire, USA (moderate nitrogen export), and monthly in streamwater at the Bowl Research Natural Area, New Hampshire, USA (high nitrogen export). For rain, a180 values ranged from +47 to +77% (mean: +58%) and d15N from -5 to +1% (mean: -3%); for snow, d180 values ranged from +52 to +75% (mean: +67%) and d18N from -3 to +2% (mean: -1%). Streamwater nitrate: in contrast to deposition, had d180 values between +12 and +33% (mean: +18%) and d15N between -3 and +6% (mean: 0%). Since nitrate produced by nitrification typically has a180 values ranging from -5 to +15%, our field data suggest that most of the nitrate lost from the watersheds in streamflow was nitrified within the catchment. Our results confirm the importance of microbial nitrogen transformations in regulating nitrogen losses from forested ecosystems and suggest that hydrologic storage may be a factor in controlling catchment nitrate losses.
Pardo, Linda H.; Kendall, Carol; Pett-Ridge, Jennifer; Chang, Cecily C.Y. 2004. Evaluating the source of streamwater nitrate using d15N and d18O in nitrate in two watersheds in New Hampshire, USA. Hydrological Processes. 18: 2699-2712.
Last updated on: October 18, 2007