S L Schiff
Biographic Data
| ID | 5600599 |
|---|---|
| NAME | S L Schiff |
| GIVEN NAMES | S L |
| FAMILY NAME | Schiff |
| SIGNATURE | SCHIFF S L |
| VERIFIED | No |
| TOTAL WORKS | 2 |
| TOTAL CITATIONS | 2 |
| AUTHOR COUNT | 2 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 1992 |
| LATEST PUBLICATION YEAR | 1992 |
| H-INDEX | 1 |
Sources and Transformation of Dissolved Organic Carbon in the Harp Lake Forested Catchment: The Role of Soils
The 14 C content of dissolved organic carbon (DOC) in streams, soil water and groundwaters in the Harp Lake catchment in Ontario, Canada, reflect a mixture of DOC sources, including both contemporary plant material and 14 C-depleted soil organic matter. The concentration and isotopic content of DOC in streams is highly variable, reflecting the complex flow path of the source water entering the streams. The characteristics of groundwater DOC are s…
Evaluating Dissolved Inorganic Carbon Cycling in a Forested Lake Watershed Using Carbon Isotopes
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…
Sources and Transformation of Dissolved Organic Carbon in the Harp Lake Forested Catchment: The Role of Soils
The 14 C content of dissolved organic carbon (DOC) in streams, soil water and groundwaters in the Harp Lake catchment in Ontario, Canada, reflect a mixture of DOC sources, including both contemporary plant material and 14 C-depleted soil organic matter. The concentration and isotopic content of DOC in streams is highly variable, reflecting the complex flow path of the source water entering the streams. The characteristics of groundwater DOC are s…
Evaluating Dissolved Inorganic Carbon Cycling in a Forested Lake Watershed Using Carbon Isotopes
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…
Sources and Transformation of Dissolved Organic Carbon in the Harp Lake Forested Catchment: The Role of Soils
The 14 C content of dissolved organic carbon (DOC) in streams, soil water and groundwaters in the Harp Lake catchment in Ontario, Canada, reflect a mixture of DOC sources, including both contemporary plant material and 14 C-depleted soil organic matter. The concentration and isotopic content of DOC in streams is highly variable, reflecting the complex flow path of the source water entering the streams. The characteristics of groundwater DOC are s…
Evaluating Dissolved Inorganic Carbon Cycling in a Forested Lake Watershed Using Carbon Isotopes
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…
Chemistry (2 works) · Dissolved organic carbon (2 works) · Environmental Chemistry (2 works) · Environmental Science (2 works) · Geology (2 works) · Groundwater (2 works) · Groundwater and Isotope Geochemistry (2 works) · Marine and coastal ecosystems (2 works) · Total organic carbon (2 works) · Bedrock (1 works)