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Hydrologie and biotic influences on nitrate removal in a subtropical spring-fed river

dc.contributor.author Heffernan, JB
dc.contributor.author Cohen, MJ
dc.contributor.author Frazer, TK
dc.contributor.author Thomas, RG
dc.contributor.author Rayfield, TJ
dc.contributor.author Gulley, J
dc.contributor.author Martin, JB
dc.contributor.author Delfmo, JJ
dc.contributor.author Graham, WD
dc.date.accessioned 2014-02-06T18:38:50Z
dc.date.issued 2010-01-01
dc.identifier.issn 0024-3590
dc.identifier.uri https://hdl.handle.net/10161/8364
dc.description.abstract We use a long-term chemical and hydrologic record in combination with longitudinal sampling and highfrequency nitrate (NO3-) measurements from in situ sensors to describe temporal and spatial patterns of nitrogen (N) inputs and removal in the spring-fed Ichetucknee River (Columbia County, Florida) and to determine the hydrological, geomorphic, and biological factors that influence those dynamics. Over a 20-yr period of record, NO 3-N removal averaged 118 kg N d-1 (0.77 g N m-2 d-1 ) over the upper 5 km of the Ichetucknee River. Three independent estimates of gross autotrophic N assimilation (from gross primary production, diel NO3- variation, and standing biomass) agreed closely but accounted for less than 20% of observed N removal. Longitudinal surveys indicate negligible or negative dissolved organic nitrogen and ammonium (NH4+) production, suggesting that denitrification is the predominant mechanism of N removal in this river. A positive relationship between discharge and the magnitude of NO3-N removal shows that interactions with the surrounding floodplain exert considerable influence at high flows, and longitudinal NO3- patterns indicate that N removal may be influenced by channel morphology. These results suggest a greater role for dissimilatory processes and hydrologic connectivity with hyporheic and floodplain sediments than has been previously recognized in highly productive spring-fed rivers of north Florida. While hydrologic variation is the primary determinant of variation in NO 3- removal within the Ichetucknee River, comparison across systems indicates that biotic characteristics can cause significant deviation from predictions based on purely physical models of relationships between river size and N removal. © 2010 by the American Society of Limnology and Oceanography, Inc.
dc.publisher Wiley
dc.relation.ispartof Limnology and Oceanography
dc.title Hydrologie and biotic influences on nitrate removal in a subtropical spring-fed river
dc.type Journal article
duke.contributor.id Heffernan, JB|0574664
pubs.begin-page 249
pubs.end-page 263
pubs.issue 1
pubs.organisational-group Duke
pubs.organisational-group Environmental Sciences and Policy
pubs.organisational-group Nicholas School of the Environment
pubs.publication-status Published
pubs.volume 55
duke.contributor.orcid Heffernan, JB|0000-0001-7641-9949


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