Articles | Volume 12, issue 16
https://doi.org/10.5194/bg-12-5143-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/bg-12-5143-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
31 Aug 2015
Research article |
| 31 Aug 2015
Environmental forcing does not induce diel or synoptic variation in the carbon isotope content of forest soil respiration
Department of Biology, University of Utah, Salt Lake City, Utah, USA
J. E. Egan
Department of Earth Sciences, Dalhousie University, Halifax, Nova Scotia, Canada
S. J. Hall
Global Change and Sustainability Center, Univ. of Utah, Salt Lake City, Utah, USA
D. A. Risk
Department of Earth Sciences, St. Francis Xavier University, Antigonish, Nova Scotia, Canada
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Saved (final revised paper)
Latest update: 20 Apr 2024
Short summary
Soil respiration and its stable isotopes were studied in a subalpine forest. There was strong diel variability in soil efflux but not in the isotope content of soil efflux or CO2 from biological activity in the soil. Following rain, soil efflux increased, but the isotope content of these fluxes did not change. Temporal variation in the isotope content of soil efflux was unrelated to environmental variables. Results confirmed established theory regarding diffusive soil gas transport.
Soil respiration and its stable isotopes were studied in a subalpine forest. There was strong...
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