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Evaluating Dissolved Inorganic Carbon Cycling in a Forested Lake Watershed Using Carbon Isotopes

Bibliographic Data

ID9244382
AuthorsRamon Aravena (0000-0003-2582-3639), S L Schiff, S E Trumbore, P J Dillon, Richard Elgood
Year1992
Volume34
Issue3
Pages636-645
Publication date1992-01-01
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueRadiocarbon (JOURNAL)
Journal identifiersISSN: 0033-8222 • E-ISSN: 1945-5755
PublisherCambridge University Press (CUP) (PUBLISHER)
DOI10.1017/s003382220006392x
OpenAlexW255634124
LanguageEN
Citations received1
References cited24

Dissolved inorganic carbon (DIC) is the main acid buffer in forested lake watersheds in Canada. We used carbon isotopes ( 13 C, 14 C) to evaluate the production and cycling of DIC in an acid-sensitive lake watershed of the Precambrian Shield. Soil CO 2 , groundwater and stream DIC were characterized chemically and isotopically. Soil CO 2 concentration profiles reflect both changes in production and in losses due to diffusion. δ 13 C soil CO 2 profiles (δ 13 C values of −23‰ in summer, slightly enriched during the fall and −25%‰ during the winter) are a reflection of the isotopic composition of the sources and changes in isotopic fractionation due to diffusion. Carbon isotopic composition ( 13 C, 14 C) of the groundwater and stream DIC clearly indicate that weathering of silicates by soil CO 2 is the main source of DIC in these watersheds. 14 C data show that, in addition to recent groundwater, an older groundwater component with depleted 14 C activity is also present in the bedrock. The carbon isotope pattern in the groundwater also implies that, besides the main springtime recharge events, contributions to the groundwater may also occur during late winter/early spring

Bedrock · Carbon cycle · Carbon fibers · Dissolved organic carbon · Geochemistry · Geomorphology · Groundwater · Isotopes of carbon · Total organic carbon · Weathering · Chemistry · Environmental Science · Geology and Paleoclimatology Research · Groundwater and Isotope Geochemistry · Marine and coastal ecosystems · Ecology · Environmental Chemistry · Geology

  • Sources and Transformation of Dissolved Organic Carbon in the Harp Lake Forested Catchment

    Open Access•S E Trumbore, S L Schiff et al.•Radiocarbon•1992

  • Carbon isotopes in soils and palaeosols as ecology and palaeoecology indicators

    Open Access•Thure E Cerling, Jay Quade et al.•Nature•1989

  • The geochemistry of C14 in fresh-water systems

    Open Access•Wallace S Broecker, A Walton•Geochimica et Cosmochimica Acta•1959

  • The stable isotopic composition of modern soil carbonate and its relationship to climate

    Open Access•Thure E Cerling•Earth and Planetary Science Letters•1984

  • Sources and Transformation of Dissolved Organic Carbon in the Harp Lake Forested Catchment

    Open Access•S E Trumbore, S L Schiff et al.•Radiocarbon•1992

  • Annual Variations of the 14 C Content of Soil CO 2

    Open Access•Helmut Dörr, K O Münnich•Radiocarbon•1986

  • Carbon-14 and Carbon-13 in Soil Co 2

    Open Access•Helmut Dörr, Karl Otto Münnich•Radiocarbon•1980

  • Discussion Reporting of 14 C Data

    Open Access•Minze Stuiver, Henry A Polach•Radiocarbon•1977

Unique citing works1
Citations per year0,03
Citation span1992 - 1992 (1)
Citation velocityhistorical
Highly citedNo
Citation typesNeutral: 1

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