A new method to measure carbon isotope composition of CO2 respired by trees: stem CO2 equilibration
Article first published online: 1 JUL 2009
DOI: 10.1111/j.1365-2435.2009.01593.x
© 2009 The Authors. Journal compilation © 2009 British Ecological Society
Additional Information
How to Cite
Ubierna, N., Marshall, J. D. and Cernusak, L. A. (2009), A new method to measure carbon isotope composition of CO2 respired by trees: stem CO2 equilibration. Functional Ecology, 23: 1050–1058. doi: 10.1111/j.1365-2435.2009.01593.x
Publication History
- Issue published online: 9 NOV 2009
- Article first published online: 1 JUL 2009
- Received 10 October 2008; accepted 14 May 2009 Handling Editor: Mark Tjoelker
Keywords:
- closed chamber;
- diffusion;
- flux;
- fractionation;
- Keeling plot;
- pool;
- soil respiration;
- stem respiration
Summary
1. Applying Keeling plot techniques to derive δ13C of respiratory input in a closed non-equilibrated chamber can lead to large errors because steady-state diffusion rules are violated in a non-steady-state environment. To avoid these errors, respiratory δ13C can be derived using equilibrated closed chambers.
2. We introduce a new method to obtain stem respired CO2δ13C (δst-r) with closed equilibrated stem chambers (E-SC). We present a theoretical model describing the equilibration process, test the model against field data and find excellent agreement. The method is further tested by comparing it with closed non-equilibrated stem chambers (NE-SC); we found no difference between these methods.
3. Our theoretical model to describe CO2 diffusion from the respiratory pool into the chamber and the equation to derive the δ13C of the efflux are general. They could be applied to other ecosystem components (e.g. soils).
4. Our method is easy to implement, cost effective, minimizes sources of error and allows for rigorous leak detection. One major limitation is its inability to detect rapid change; the equilibration process requires 15 ± 2 h. A second limitation is that it cannot be used for species that produce abundant pitch at sites of stem wounding (e.g. Pseudotsuga menziesii).
5. Investigating δ13C of CO2 respired by different ecosystem components is necessary to interpret δ13C of ecosystem respiration. This parameter has major implications with respect to global carbon cycle science.

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