Abstract
Our paper, published in Biogeochemistry (Vol. 132, 2017, pp. 87-102), contains a calculation error in the determination of the C-gas flux rates. To correct this error all CO2 flux rates should be multiplied by 3.66, and all CH4 flux rates multiplied by 1.34. As a result, the sustained global warming potentials of mean daily water-air CH4 contributions to total C-gas emissions from the S1 study segment were 39% the sustained global warming potentials of mean soil CO2emissions over the 20-year time frame and 29% the measured background water-air emissions over the 100-year time frame. The revised Table 2 below reports correct values for the paper. This does not alter any of the statistical analyses, other interpretations, or general conclusions of the manuscript. (The original article can be accessed via http://handle.westernsydney.edu.au:8081/1959.7/uws:38371)
| Original language | English |
|---|---|
| Pages (from-to) | 237-238 |
| Number of pages | 2 |
| Journal | Biogeochemistry |
| Volume | 134 |
| Issue number | 1-2 |
| DOIs | |
| Publication status | Published - 2017 |
UN SDGs
This output contributes to the following UN Sustainable Development Goals (SDGs)
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SDG 13 Climate Action
Keywords
- carbon dioxide
- greenhouse gases
- methane
- wetlands
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