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Updated: Jun 27, 2026

Simulating Temperature in a Soil Incubation Experiment
Published on: October 28, 2022
Adjustment of forest ecosystem root respiration as temperature warms
Andrew J Burton1, Jerry M Melillo, Serita D Frey
1Ecosystem Science Center, Michigan Technological University, Houghton, Michigan 49931, USA. ajburton@mtu.edu
Forest root respiration increases with temperature but at a slower rate than previously thought. This suggests models may overestimate carbon release and underestimate carbon for plant growth in warmer climates.
Area of Science:
- Ecology
- Climate Change Biology
- Forest Science
Background:
- Soil respiration is a major component of ecosystem carbon cycling.
- Root respiration's response to warming is crucial for predicting future carbon availability.
- Previous models often assume a high temperature sensitivity (Q10) for root respiration.
Purpose of the Study:
- To investigate the relationship between forest root respiration and mean annual temperature across ecosystems.
- To compare cross-ecosystem temperature sensitivity of root respiration with short-term within-ecosystem responses.
- To assess the impact of soil warming experiments on root metabolic capacity.
Main Methods:
- Meta-analysis of 44 published annual forest root respiration values.
- Examination of specific root respiration rates and root biomass.
- Analysis of root respiration data from three soil warming experiments at Harvard Forest.
Main Results:
- Ecosystem root respiration increased with mean annual temperature, but with a lower Q10 (1.6) than short-term responses (Q10=2-3).
- Root metabolic capacity decreased with increasing mean annual temperature, showing a tradeoff with root biomass.
- Roots from heated plots in soil warming experiments exhibited reduced metabolic capacity.
Conclusions:
- Current models may overestimate root respiration's contribution to CO2 efflux under future warming.
- Underestimation of carbon availability for net primary productivity is a potential consequence.
- Root physiological acclimation or soil moisture effects may explain reduced metabolic capacity in warmer conditions.
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