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- W4214541552 abstract "Decomposition of soil organic carbon (SOC) is the main process governing the release of CO(2) into the atmosphere from terrestrial systems. Although the importance of soil-root interactions for SOC decomposition has increasingly been recognized, their long-term effect on SOC decomposition remains poorly understood. Here we provide experimental evidence for a rhizosphere priming effect, in which interactions between soil and tree roots substantially accelerate SOC decomposition. In a 395-day greenhouse study with Ponderosa pine and Fremont cottonwood trees grown in three different soils, SOC decomposition in the planted treatments was significantly greater (up to 225%) than in soil incubations alone. This rhizosphere priming effect persisted throughout the experiment, until well after initial soil disturbance, and increased with a greater amount of root-derived SOC formed during the experiment. Loss of old SOC was greater than the formation of new C, suggesting that increased C inputs from roots could result in net soil C loss. PMID: 17910623" @default.
- W4214541552 created "2022-03-02" @default.
- W4214541552 creator A5070725078 @default.
- W4214541552 date "2011-07-28" @default.
- W4214541552 modified "2023-09-27" @default.
- W4214541552 title "Faculty Opinions recommendation of Interactions between soil and tree roots accelerate long-term soil carbon decomposition." @default.
- W4214541552 doi "https://doi.org/10.3410/f.12316956.13493056" @default.
- W4214541552 hasPublicationYear "2011" @default.
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