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Published on: January 16, 2014
Interactions between soil and tree roots accelerate long-term soil carbon decomposition.
Feike A Dijkstra1, Weixin Cheng
1Department of Environmental Studies, University of California, Santa Cruz, CA 95064, USA. feike.dijkstra@ars.usda.gov
Tree roots significantly accelerate soil organic carbon (SOC) decomposition, a process known as the rhizosphere priming effect. This effect can lead to a net loss of soil carbon over time.
Area of Science:
- Soil Science
- Ecology
- Biogeochemistry
Background:
- Soil organic carbon (SOC) decomposition releases CO2, impacting atmospheric carbon levels.
- The long-term effects of soil-root interactions on SOC decomposition are not well understood.
Purpose of the Study:
- To investigate the long-term impact of tree roots on SOC decomposition.
- To provide experimental evidence for the rhizosphere priming effect.
Main Methods:
- A 395-day greenhouse study.
- Ponderosa pine and Fremont cottonwood trees grown in three different soils.
- Comparison of SOC decomposition in planted treatments versus soil incubations alone.
Main Results:
- SOC decomposition was significantly higher (up to 225%) in planted treatments compared to unplanted controls.
- The rhizosphere priming effect persisted throughout the experiment.
- The effect increased with greater root-derived carbon input.
Conclusions:
- Tree roots substantially accelerate SOC decomposition via the rhizosphere priming effect.
- Increased carbon inputs from roots may lead to a net loss of soil carbon.
- This highlights the critical role of plant-soil interactions in carbon cycling.
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