Carbon and nitrogen isotope studies in an arctic aquatic ecosystem

The Phase II studies of the R4D Program on stream and watershed ecology reflect the accomplishments and accumulation of baseline information obtained during the past studies. Although our rough estimates indicate that nitrogen inputs to the watershed ba lance losses, the carbon fluxes suggest that t...

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Main Author: Schell, D.M.
Language:unknown
Published: 2008
Subjects:
Online Access:http://www.osti.gov/servlets/purl/10137210
https://www.osti.gov/biblio/10137210
https://doi.org/10.2172/10137210
id ftosti:oai:osti.gov:10137210
record_format openpolar
spelling ftosti:oai:osti.gov:10137210 2023-07-30T04:01:24+02:00 Carbon and nitrogen isotope studies in an arctic aquatic ecosystem Schell, D.M. 2008-06-19 application/pdf http://www.osti.gov/servlets/purl/10137210 https://www.osti.gov/biblio/10137210 https://doi.org/10.2172/10137210 unknown http://www.osti.gov/servlets/purl/10137210 https://www.osti.gov/biblio/10137210 https://doi.org/10.2172/10137210 doi:10.2172/10137210 54 ENVIRONMENTAL SCIENCES TUNDRA CARBON CYCLE NITROGEN CYCLE NITROGEN ISOTOPES ECOLOGICAL CONCENTRATION CARBON ISOTOPES ARCTIC REGIONS AQUATIC ECOSYSTEMS BASELINE ECOLOGY CARBON DIOXIDE ALASKA CARBON 14 2008 ftosti https://doi.org/10.2172/10137210 2023-07-11T10:58:43Z The Phase II studies of the R4D Program on stream and watershed ecology reflect the accomplishments and accumulation of baseline information obtained during the past studies. Although our rough estimates indicate that nitrogen inputs to the watershed ba lance losses, the carbon fluxes suggest that they are not in equilibrium and that there is a net loss of carbon from the tundra ecosystem through respiration and transport out of the watershed via the stream system. Radiocarbon profiles of soil sections coupled with mass transport calculations revealed that peat accumulation has essentially ceased in the R4D watershed and appears to be in ablative loss. Thus the carbon flux measurements provide validation tests for the PLANTGRO and GAS-HYDRO models of the PHASE II studies. These findings are also important in the context of global CO{sub 2} increases from positive feedback mechanisms in peatlands associated with climatic warming in the subarctic regions. Other/Unknown Material Arctic Subarctic Tundra Alaska SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy) Arctic
institution Open Polar
collection SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy)
op_collection_id ftosti
language unknown
topic 54 ENVIRONMENTAL SCIENCES
TUNDRA
CARBON CYCLE
NITROGEN CYCLE
NITROGEN ISOTOPES
ECOLOGICAL CONCENTRATION
CARBON ISOTOPES
ARCTIC REGIONS
AQUATIC ECOSYSTEMS
BASELINE ECOLOGY
CARBON DIOXIDE
ALASKA
CARBON 14
spellingShingle 54 ENVIRONMENTAL SCIENCES
TUNDRA
CARBON CYCLE
NITROGEN CYCLE
NITROGEN ISOTOPES
ECOLOGICAL CONCENTRATION
CARBON ISOTOPES
ARCTIC REGIONS
AQUATIC ECOSYSTEMS
BASELINE ECOLOGY
CARBON DIOXIDE
ALASKA
CARBON 14
Schell, D.M.
Carbon and nitrogen isotope studies in an arctic aquatic ecosystem
topic_facet 54 ENVIRONMENTAL SCIENCES
TUNDRA
CARBON CYCLE
NITROGEN CYCLE
NITROGEN ISOTOPES
ECOLOGICAL CONCENTRATION
CARBON ISOTOPES
ARCTIC REGIONS
AQUATIC ECOSYSTEMS
BASELINE ECOLOGY
CARBON DIOXIDE
ALASKA
CARBON 14
description The Phase II studies of the R4D Program on stream and watershed ecology reflect the accomplishments and accumulation of baseline information obtained during the past studies. Although our rough estimates indicate that nitrogen inputs to the watershed ba lance losses, the carbon fluxes suggest that they are not in equilibrium and that there is a net loss of carbon from the tundra ecosystem through respiration and transport out of the watershed via the stream system. Radiocarbon profiles of soil sections coupled with mass transport calculations revealed that peat accumulation has essentially ceased in the R4D watershed and appears to be in ablative loss. Thus the carbon flux measurements provide validation tests for the PLANTGRO and GAS-HYDRO models of the PHASE II studies. These findings are also important in the context of global CO{sub 2} increases from positive feedback mechanisms in peatlands associated with climatic warming in the subarctic regions.
author Schell, D.M.
author_facet Schell, D.M.
author_sort Schell, D.M.
title Carbon and nitrogen isotope studies in an arctic aquatic ecosystem
title_short Carbon and nitrogen isotope studies in an arctic aquatic ecosystem
title_full Carbon and nitrogen isotope studies in an arctic aquatic ecosystem
title_fullStr Carbon and nitrogen isotope studies in an arctic aquatic ecosystem
title_full_unstemmed Carbon and nitrogen isotope studies in an arctic aquatic ecosystem
title_sort carbon and nitrogen isotope studies in an arctic aquatic ecosystem
publishDate 2008
url http://www.osti.gov/servlets/purl/10137210
https://www.osti.gov/biblio/10137210
https://doi.org/10.2172/10137210
geographic Arctic
geographic_facet Arctic
genre Arctic
Subarctic
Tundra
Alaska
genre_facet Arctic
Subarctic
Tundra
Alaska
op_relation http://www.osti.gov/servlets/purl/10137210
https://www.osti.gov/biblio/10137210
https://doi.org/10.2172/10137210
doi:10.2172/10137210
op_doi https://doi.org/10.2172/10137210
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