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P J Dillon

Biographic Data

ID5600600
NAMEP J Dillon
GIVEN NAMESP J
FAMILY NAMEDillon
SIGNATUREDILLON P J
VERIFIEDNo
TOTAL WORKS1
TOTAL CITATIONS1
AUTHOR COUNT1
EDITOR COUNT0
FIRST PUBLICATION YEAR1992
LATEST PUBLICATION YEAR1992
H-INDEX1
  • Evaluating Dissolved Inorganic Carbon Cycling in a Forested Lake Watershed Using Carbon Isotopes

    Open Access•Ramon Aravena, S L Schiff et al.•ARTICLE•Radiocarbon•1992•Cited by: 1•References: 24

    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 pro…

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

    Open Access•Ramon Aravena, S L Schiff et al.•ARTICLE•Radiocarbon•1992•Cited by: 1•References: 24

    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 pro…

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

    Open Access•Ramon Aravena, S L Schiff et al.•ARTICLE•Radiocarbon•1992•Cited by: 1•References: 24

    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 pro…

Bedrock (1 works) · Carbon cycle (1 works) · Carbon fibers (1 works) · Chemistry (1 works) · Dissolved organic carbon (1 works) · Ecology (1 works) · Environmental Chemistry (1 works) · Environmental Science (1 works) · Geochemistry (1 works) · Geology (1 works)

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