CO2 flux from Acer saccharum logs: sources of variation and the influence of silvicultural treatments

Author:

Read Zoe1ORCID,Fraver Shawn1,D'Amato Anthony W.2ORCID,Evans Daniel M.3,Evans Kevin4,Lutz David A.5,Woodall Christopher W.6ORCID

Affiliation:

1. School of Forest Resources, University of Maine, Orono, ME 04469, USA

2. Rubenstein School of Environment and Natural Resources, University of Vermont, Burlington, VT 05405, USA

3. Judd Gregg Meteorology Institute, Plymouth State University, Plymouth, NH 03264, USA

4. Dartmouth College Woodlands, Milan, NH 03588, USA

5. Environmental Studies Program, Dartmouth College, Hanover, NH 03755, USA

6. USDA Forest Service, Northern Research Station, Durham, NH 03824, USA

Abstract

Several aspects of the forest carbon cycle have not been examined in detail, including sources of variation in carbon dioxide (CO2) emissions from coarse woody material (CWM). To address this knowledge gap, we examined CO2 emissions from Acer saccharum Marshall logs within four harvesting treatments, using closed chambers fitted to the logs. We found that CO2 emissions were highest for logs in small (31.8 ± 20.4 µmol·CO2·m−3·s−1) and large gaps (29.6 ± 24.4 µmol·CO2·m−3·s−1) compared to those in control (13.9 ± 8.3 µmol·CO2·m−3·s−1) and thinned matrix (13.6 ± 8.0 µmol·CO2·m−3·s−1) treatments. CO2 flux rates did not differ between gap sizes, but they increased with temperature, which was higher in the small gap treatment. In addition, two individual logs fitted with multiple closed chambers revealed significant within-log variability in CO2 emissions. On a subset of logs repeatedly sampled throughout the day, we found that log surface temperature generally peaked at midday and was positively correlated with CO2 emissions, although this relationship was weak in one log. This study provides insight into sources of variation in CO2 emissions from CWM while improving our understanding of the forest carbon cycle.

Publisher

Canadian Science Publishing

Subject

Ecology,Forestry,Global and Planetary Change

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