A Stormflow/Baseflow Comparison of Dissolved Organic Matter Concentrations and Bioavailability in an Appalachian Stream

Patterns of dissolved organic carbon (DOC) and nitrogen (DON) delivery were compared between times of stormflow and baseflow in Paine Run, an Appalachian stream draining a 12.4 km2 forested catchment in the Shenandoah National Park (SNP), Virginia. The potential in-stream ecological impact of altere...

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Vydáno v:Biogeochemistry Ročník 53; číslo 3; s. 269 - 306
Hlavní autoři: Buffam, Ishi, Galloway, James N., Blum, Linda K., McGlathery, Karen J.
Médium: Journal Article
Jazyk:angličtina
Vydáno: Heidelberg Kluwer Academic Publishers 01.05.2001
Springer
Springer Nature B.V
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ISSN:0168-2563, 1573-515X
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Abstract Patterns of dissolved organic carbon (DOC) and nitrogen (DON) delivery were compared between times of stormflow and baseflow in Paine Run, an Appalachian stream draining a 12.4 km2 forested catchment in the Shenandoah National Park (SNP), Virginia. The potential in-stream ecological impact of altered concentrations and/or chemical composition of DOM during storms also was examined, using standardized bacterial bioassays. DOC and DON concentrations in Paine Run were consistently low during baseflow and did not show a seasonal pattern. During storms however, mean DOC and DON concentrations approximately doubled, with maximum concentrations occurring on the rising limb of storm hydrographs. The rapid response of DOM concentration to changes in flow suggests a near-stream or in-stream source of DOM during storms. Stormflow (4% of the time, 36% of the annual discharge) contributed >50% of DOC, DON and NO3- flux in Paine Run during 1997. In laboratory bacterial bioassays, growth rate constants were higher on Paine Run stormflow water than on baseflow water, but the fraction of total DOM which was bioavailable was not significantly different. The fraction of the total stream DOC pool taken up by water column bacteria was estimated to increase from 0.03 ± 0.02% h-1 during baseflow, to 0.15 ± 0.04% h-1 during storms. This uptake rate would have a minimal effect on bulk DOM concentrations in Paine Run, but storms may still have considerable impact on the bacterial stream communities by mobilizing them into the water column and by supplying a pulse of DOM.
AbstractList Patterns of dissolved organic carbon (DOC) and nitrogen (DON) delivery were compared between times of stormflow and baseflow in Paine Run, an Appalachian stream draining a 12.4 km2 forested catchment in the Shenandoah National Park (SNP), Virginia. The potential in-stream ecological impact of altered concentrations and/or chemical composition of DOM during storms also was examined, using standardized bacterial bioassays. DOC and DON concentrations in Paine Run were consistently low during baseflow and did not show a seasonal pattern. During storms however, mean DOC and DON concentrations approximately doubled, with maximum concentrations occurring on the rising limb of storm hydrographs. The rapid response of DOM concentration to changes in flow suggests a near-stream or in-stream source of DOM during storms. Stormflow (4% of the time, 36% of the annual discharge) contributed >50% of DOC, DON and NO3- flux in Paine Run during 1997. In laboratory bacterial bioassays, growth rate constants were higher on Paine Run stormflow water than on baseflow water, but the fraction of total DOM which was bioavailable was not significantly different. The fraction of the total stream DOC pool taken up by water column bacteria was estimated to increase from 0.03 ± 0.02% h-1 during baseflow, to 0.15 ± 0.04% h-1 during storms. This uptake rate would have a minimal effect on bulk DOM concentrations in Paine Run, but storms may still have considerable impact on the bacterial stream communities by mobilizing them into the water column and by supplying a pulse of DOM.
Patterns of dissolved organic carbon (DOC) and nitrogen (DON) delivery were compared between times of stormflow and baseflow in Paine Run, an Appalachian stream draining a 12.4 km2 forested catchment in the Shenandoah National Park (SNP), Virginia. The potential in-stream ecological impact of altered concentrations and/or chemical composition of DOM during storms also was examined, using standardized bacterial bioassays. DOC and DON concentrations in Paine Run were consistently low during baseflow and did not show a seasonal pattern. During storms however, mean DOC and DON concentrations approximately doubled, with maximum concentrations occurring on the rising limb of storm hydrographs. The rapid response of DOM concentration to changes in flow suggests a near-stream or in-stream source of DOM during storms. Stormflow (4% of the time, 36% of the annual discharge) contributed >50% of DOC, DON and NO3− flux in Paine Run during 1997. In laboratory bacterial bioassays, growth rate constants were higher on Paine Run stormflow water than on baseflow water, but the fraction of total DOM which was bioavailable was not significantly different. The fraction of the total stream DOC pool taken up by water column bacteria was estimated to increase from 0.03 ± 0.02% h−1 during baseflow, to 0.15 ± 0.04% h−1 during storms. This uptake rate would have a minimal effect on bulk DOM concentrations in Paine Run, but storms may still have considerable impact on the bacterial stream communities by mobilizing them into the water column and by supplying a pulse of DOM.
Patterns of dissolved organic carbon (DOC) and nitrogen (DON) delivery were compared between times of stormflow and baseflow in Paine Run, an Appalachian stream draining a 12.4 km super(2) forested catchment in the Shenandoah National Park (SNP), Virginia. The potential in-stream ecological impact of altered concentrations and/or chemical composition of DOM during storms also was examined, using standardized bacterial bioassays. DOC and DON concentrations in Paine Run were consistently low during baseflow and did not show a seasonal pattern. During storms however, mean DOC and DON concentrations approximately doubled, with maximum concentrations occurring on the rising limb of storm hydrographs. The rapid response of DOM concentration to changes in flow suggests a near-stream or in-stream source of DOM during storms. Stormflow (4% of the time, 36% of the annual discharge) contributed >50% of DOC, DON and NO sub(3) super(-) flux in Paine Run during 1997. In laboratory bacterial bioassays, growth rate constants were higher on Paine Run stormflow water than on baseflow water, but the fraction of total DOM which was bioavailable was not significantly different. The fraction of the total stream DOC pool taken up by water column bacteria was estimated to increase from 0.03 plus or minus 0.02% h super(-1) during baseflow, to 0.15 plus or minus 0.04% h super(-1) during storms. This uptake rate would have a minimal effect on bulk DOM concentrations in Paine Run, but storms may still have considerable impact on the bacterial stream communities by mobilizing them into the water column and by supplying a pulse of DOM.
Author McGlathery, Karen J.
Buffam, Ishi
Galloway, James N.
Blum, Linda K.
Author_xml – sequence: 1
  givenname: Ishi
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  givenname: James N.
  surname: Galloway
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  givenname: Linda K.
  surname: Blum
  fullname: Blum, Linda K.
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  givenname: Karen J.
  surname: McGlathery
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ISSN 0168-2563
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IsPeerReviewed true
IsScholarly true
Issue 3
Keywords bacteria
nitrogen
river discharge
streams
runoff
concentration
drainage patterns
nitrates
North America
prokaryotes
hydrochemistry
discharge
organic materials
dissolved materials
chemical composition
organic carbon
hydrographs
storms
national parks
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PublicationTitle Biogeochemistry
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Publisher Kluwer Academic Publishers
Springer
Springer Nature B.V
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Snippet Patterns of dissolved organic carbon (DOC) and nitrogen (DON) delivery were compared between times of stormflow and baseflow in Paine Run, an Appalachian...
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SubjectTerms Bacteria
Base flow
Bio-assays
Bioassay
Bioassays
Bioavailability
Catchment area
Chemical composition
Dissolved organic carbon
Dissolved organic matter
Earth sciences
Earth, ocean, space
Exact sciences and technology
Forested watersheds
Geochemistry
Growth rate
Hydrology
Hydrology. Hydrogeology
Mineralogy
National parks
Nitrogen
Rate constants
Rivers
Seasonal variations
Silicates
Soil organic matter
Storms
Stormwater
Streams
USA, Blue Ridge Mts., Shenandoah Natl. Park
USA, Virginia
USA, Virginia, Blue Ridge Mts., Paine Run
Water circulation
Water column
Water geochemistry
Watersheds
Title A Stormflow/Baseflow Comparison of Dissolved Organic Matter Concentrations and Bioavailability in an Appalachian Stream
URI https://www.jstor.org/stable/1469580
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