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Primary Research Article
Net ecosystem exchange modifies the relationship between the autotrophic and heterotrophic components of soil respiration with abiotic factors in prairie grasslands
Article first published online: 16 MAY 2012
DOI: 10.1111/j.1365-2486.2012.02721.x
© 2012 Blackwell Publishing Ltd
Additional Information
How to Cite
Gomez-Casanovas, N., Matamala, R., Cook, D. R. and Gonzalez-Meler, M. A. (2012), Net ecosystem exchange modifies the relationship between the autotrophic and heterotrophic components of soil respiration with abiotic factors in prairie grasslands. Global Change Biology, 18: 2532–2545. doi: 10.1111/j.1365-2486.2012.02721.x
Publication History
- Issue published online: 10 JUL 2012
- Article first published online: 16 MAY 2012
- Accepted manuscript online: 18 APR 2012 05:24AM EST
- Manuscript Accepted: 28 MAR 2012
- Manuscript Revised: 16 MAR 2012
- Manuscript Received: 24 AUG 2011
- Abstract
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| Filename | Format | Size | Description |
|---|---|---|---|
| gcb2721-sup-0001-FigureS1.JPG | image/JPG | 619K | Figure S1. Data for daytime 10 June 2008 sampling, are shown below as an example of a typical Keeling plot constructed to determine the δ13C of soil-respired CO₂ during this study at any given time. Data points show the relationship between the inverse of the concentration of CO₂ in the headspace of the soil respiration chamber (x-axis) vs. the δ13C of the air collected from the headspace chamber (y-axis) at a given CO₂ concentration. Each headspace air sample was collected from a different PVC collar, when the CO₂ concentration inside the soil respiration chamber was 400-700 µL L-1 and the CO2 concentration differed by at least 50 µL L-1 from that for the previous sample. The data points were fitted to a linear regression Model I. The extrapolated y-intercept represents the δ13C of soil-respired CO₂ (δ13CRsoil). For this linear regression, the slope was 7194 ± 308, the y-intercept was −28.25 ± 0.1 and the r2 = 0.9950. |
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