M F Billett
Biographic Data
| ID | 5601715 |
|---|---|
| NAME | M F Billett |
| GIVEN NAMES | M F |
| FAMILY NAME | Billett |
| SIGNATURE | BILLETT M F |
| AFFILIATIONS | University of Stirling |
| VERIFIED | No |
| TOTAL WORKS | 3 |
| TOTAL CITATIONS | 3 |
| AUTHOR COUNT | 3 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 2006 |
| LATEST PUBLICATION YEAR | 2017 |
| H-INDEX | 1 |
Abundant pre-industrial carbon detected in Canadian Arctic headwaters
Mobilization of soil/sediment organic carbon into inland waters constitutes a substantial, but poorly-constrained, component of the global carbon cycle. Radiocarbon (14C) analysis has proven a valuable tool in tracing the sources and fate of mobilized carbon, but aquatic 14C studies in permafrost regions rarely detect 'old' carbon (assimilated from the atmosphere into plants and soil prior to AD1950). The emission of greenhouse gases derived from…
Do Riparian Plants Fix CO 2 Lost by Evasion from Surface Waters? An Investigation Using Carbon Isotopes
Rivers and streams in many parts of the world contain high concentrations of dissolved carbon dioxide, which is lost to the atmosphere by evasion (outgassing). Recent methodological advances now enable the carbon isotopic composition of this evaded CO 2 to be measured directly, with early results from peatland streams showing it to be depleted in 13 C relative to the atmosphere. The first direct measurements of the radiocarbon age of evaded CO 2 …
A Direct Method to Measure 14 CO 2 Lost by Evasion from Surface Waters
Recent methodological advances in the use of zeolite molecular sieves for measuring the isotopic signature of CO 2 have provided the opportunity to make direct measurements of 14 CO2 in various field situations. We linked a portable molecular sieve/pump/IRGA system to a floating chamber to demonstrate the potential of the method to quantify the isotopic signature (δ 13 C and 14 C) of CO 2 lost by evasion (outgassing) from surface waters. The syst…
A Direct Method to Measure 14 CO 2 Lost by Evasion from Surface Waters
Recent methodological advances in the use of zeolite molecular sieves for measuring the isotopic signature of CO 2 have provided the opportunity to make direct measurements of 14 CO2 in various field situations. We linked a portable molecular sieve/pump/IRGA system to a floating chamber to demonstrate the potential of the method to quantify the isotopic signature (δ 13 C and 14 C) of CO 2 lost by evasion (outgassing) from surface waters. The syst…
Do Riparian Plants Fix CO 2 Lost by Evasion from Surface Waters? An Investigation Using Carbon Isotopes
Rivers and streams in many parts of the world contain high concentrations of dissolved carbon dioxide, which is lost to the atmosphere by evasion (outgassing). Recent methodological advances now enable the carbon isotopic composition of this evaded CO 2 to be measured directly, with early results from peatland streams showing it to be depleted in 13 C relative to the atmosphere. The first direct measurements of the radiocarbon age of evaded CO 2 …
A Direct Method to Measure 14 CO 2 Lost by Evasion from Surface Waters
Recent methodological advances in the use of zeolite molecular sieves for measuring the isotopic signature of CO 2 have provided the opportunity to make direct measurements of 14 CO2 in various field situations. We linked a portable molecular sieve/pump/IRGA system to a floating chamber to demonstrate the potential of the method to quantify the isotopic signature (δ 13 C and 14 C) of CO 2 lost by evasion (outgassing) from surface waters. The syst…
Do Riparian Plants Fix CO 2 Lost by Evasion from Surface Waters? An Investigation Using Carbon Isotopes
Rivers and streams in many parts of the world contain high concentrations of dissolved carbon dioxide, which is lost to the atmosphere by evasion (outgassing). Recent methodological advances now enable the carbon isotopic composition of this evaded CO 2 to be measured directly, with early results from peatland streams showing it to be depleted in 13 C relative to the atmosphere. The first direct measurements of the radiocarbon age of evaded CO 2 …
Abundant pre-industrial carbon detected in Canadian Arctic headwaters
Mobilization of soil/sediment organic carbon into inland waters constitutes a substantial, but poorly-constrained, component of the global carbon cycle. Radiocarbon (14C) analysis has proven a valuable tool in tracing the sources and fate of mobilized carbon, but aquatic 14C studies in permafrost regions rarely detect 'old' carbon (assimilated from the atmosphere into plants and soil prior to AD1950). The emission of greenhouse gases derived from…
Biology (3 works) · Chemistry (3 works) · Ecology (3 works) · Environmental Chemistry (3 works) · Environmental Science (3 works) · Carbon cycle (2 works) · Carbon fibers (2 works) · Ecosystem (2 works) · Geology (2 works) · Geology and Paleoclimatology Research (2 works)