2004
DOI: 10.4319/lo.2004.49.3.0809
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Stream denitrification and total nitrate uptake rates measured using a field 15N tracer addition approach

Abstract: We measured denitrification and total nitrate uptake rates in a small stream (East Fork of Walker Branch in eastern Tennessee) using a new field 15 N tracer addition and modeling approach that quantifies these rates for entire stream reaches. The field experiment consisted of an 8-h addition of 99 atom% K 15 NO 3 and a conservative solute tracer. Two 15 N tracer addition experiments were performed on consecutive days, the first under ambient NO concentra- (Ͼ99%) and comprised about 16% (Ϯ10%) of total NO uptak… Show more

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Cited by 173 publications
(203 citation statements)
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“…denitrification and DNRA) such as oxygen conditions (water column DO concentrations) and organic carbon (benthic organic matter content) (Tiedje 1988), although U did increase in response to lower DO concentrations. This suggests that much of the demand for NO 3 ( in the Taupo streams during summer was probably assimilatory and is consistent with other studies showing that assimilatory processes tend to dominate instream NO 3 ( uptake (Mulholland et al 2004(Mulholland et al , 2008Arango et al 2008).…”
Section: Discussionsupporting
confidence: 90%
“…denitrification and DNRA) such as oxygen conditions (water column DO concentrations) and organic carbon (benthic organic matter content) (Tiedje 1988), although U did increase in response to lower DO concentrations. This suggests that much of the demand for NO 3 ( in the Taupo streams during summer was probably assimilatory and is consistent with other studies showing that assimilatory processes tend to dominate instream NO 3 ( uptake (Mulholland et al 2004(Mulholland et al , 2008Arango et al 2008).…”
Section: Discussionsupporting
confidence: 90%
“…The rate of denitrification occurring within the stream was determined by using longitudinal flux of tracer 15 N 2 with the model presented by Mulholland et al (2004). Flux of total 15 N 2 was calculated by multiplying the mole fraction of 15 N in the N 2 gas at each station during the 15 NO 3 -experiment by the measured mass of dissolved N 2 in the water, multiplied by the stream discharge.…”
Section: Laboratory Methodsmentioning
confidence: 99%
“…For example, Whitmire and Hamilton [45] using push-pull techniques found that nitrate added to groundwater and re-injected into wetland sediments disappeared rapidly relative to conservative tracers without any lag time, and was depleted to below detection limits (10-15 µg N L −1 ) within 5 to 20 h. In a 15 N denitrification study in a similar natural riparian wetland intercepting shallow groundwater, Burns and Nguyen [46] measured >90% removal of injected 15 NO 3 -N along a 100 cm flow path through the organic wetland soil, with essentially all of the 15 NO 3 -N-removed within 30 cm. Extensive 15 N tracer study performed on small headwater agricultural streams in the USA by Peterson [21] showed that NH 4 -N and NO x -N entering the streams was removed within tens to hundreds of meters and in one of the streams the denitrification rate was 0.045 µg N m −2 s −1 [47]. Denitrification consisted almost entirely of N 2 production (99%), with very little N 2 O production occurring.…”
Section: Discussionmentioning
confidence: 99%
“…To describe the temperature response of denitrification, we used Arrhenius equation, which is most commonly used in this case and where the temperature has a stronger effect on the denitrification at lower temperatures [4,47]. Several authors have reported that denitrification has a "breakpoint" temperature, below which denitrification rates decrease more rapidly [9,48,49].…”
Section: Discussionmentioning
confidence: 99%