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Biochar-induced reductions in the rhizosphere priming effect are weaker under elevated CO2
Biochar can store carbon in soils for decades to centuries, and is considered to have some potential to contribute to mitigating climate change. However, both biochar and elevated atmospheric CO2 (eCO2) can influence the rhizosphere priming effect (RPE) on pre-existing soil organic carbon (SOC) deco...
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Published in: | Soil biology & biochemistry 2020-03, Vol.142, p.107700, Article 107700 |
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Main Authors: | , , , , , , , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
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Summary: | Biochar can store carbon in soils for decades to centuries, and is considered to have some potential to contribute to mitigating climate change. However, both biochar and elevated atmospheric CO2 (eCO2) can influence the rhizosphere priming effect (RPE) on pre-existing soil organic carbon (SOC) decomposition, leading to uncertainty in comprehensively evaluating the soil carbon sequestration potential of biochar under future climate change. In the present study, we investigated the RPE on pre-existing SOC decomposition of paddy rice in a soil-plant-biochar system under eCO2 (700 ppm). Plant-derived sources of carbon were separated from soil-derived sources using a continuous 13C-labelling method. We found that the RPEs decreased significantly with increasing biochar addition rates (1%, 2%, 3%, 4%, and 5% by weight) with mean reductions of 12% and 40% on day 31 and 54 after sowing, respectively, suggesting that biochar can enhance the stability of pre-existing SOC by decreasing the RPE. Although compared to ambient CO2 (aCO2, 400 ppm), eCO2 significantly decreased RPEs by 33% and 37% on day 31 and 54 after sowing, respectively, the decline in the RPE in response to biochar was weaker under eCO2. Decreases in soil enzyme activities and microbial biomass carbon could explain the decline in the RPE in response to biochar addition. Our findings highlight that biochar can inhibit the decomposition of pre-existing SOC by reducing the RPE, while this effect will be weakened in the face of atmospheric CO2 increase in the future.
Elevated CO2 (eCO2) weakens the positive effect of biochar on soil carbon stability through the rhizosphere priming effect (RPE) compared to ambient CO2 (aCO2). Our findings suggest that both biochar and eCO2 can protect pre-existing SOC from decomposition in the presence of plants, leading to an increase in soil carbon sequestration, while the effect of biochar may weaken in the face of the continuous rise in atmospheric CO2 concentration in the future. [Display omitted]
•Biochar and elevated CO2 (eCO2) influenced the rhizosphere priming effect (RPE).•Biochar sequestered additional carbon by decreasing the RPE.•eCO2 decreased the RPE.•The negative effect of biochar on the RPE was weaker under eCO2.•Microbial biomass carbon and enzyme activity explained the effect of biochar on RPE. |
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ISSN: | 0038-0717 1879-3428 |
DOI: | 10.1016/j.soilbio.2019.107700 |