Global patterns and controls of soil greenhouse gas fluxes and crop yield under biochar application

Author:

Jia Xiaoyu1ORCID,Yan Weiming12ORCID,Yang Jingyi3,Chen Weiguang1,Ma Hongze2,Chen Xi1,Liu Jin1,Zhong Yangquanwei4ORCID,Shangguan Zhouping1ORCID

Affiliation:

1. State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau Northwest A&F University Yangling Shaanxi People's Republic of China

2. Institute of Soil and Water Conservation Chinese Academy of Sciences Yangling Shaanxi People's Republic of China

3. Key Laboratory of Mine Geological Hazards Mechanism and Control Ministry of Natural Resources Xi'an Shaanxi People's Republic of China

4. Center for Ecological and Environmental Sciences, Key Laboratory for Space Bioscience & Biotechnology Northwestern Polytechnical University Xi'an Shaanxi People's Republic of China

Abstract

AbstractBiochar application has been proven to be a viable technique in mitigating soil greenhouse gas (GHG) emissions and improving crop yield; however, the global patterns and responses of soil GHG fluxes, global warming potential (GWP), crop yield, and greenhouse gas intensity (GHGI) to biochar application, as well as the key drivers of biochar‐induced changes, are not fully synthesized. Hence, we conducted a meta‐analysis of 3883 paired observations from 220 studies. Overall, biochar application significantly increased carbon dioxide (CO2) emissions (7.4%) and yield (9.4%) and decreased soil methane (CH4, −13.0%) and nitrous oxide (N2O, −26.8%) emissions, as well as GWP (−7.7%) and GHGI (−14.3%). CH4 uptake was, however, not observed to change. The responses of soil GHG fluxes to the biochar application were more sensitive in the incubation and pot experiments compared to the field studies. In addition, increased CO2 emissions were mainly derived from incubation and pot experiments, whereas the biochar application did not significantly change CO2 emissions in the field studies. The climate, soil, and experimental conditions also affected the responses of soil GHG fluxes to biochar application, and the biochar‐induced change in soil pH was the most essential factor associated with the variations in soil GHG fluxes. Globally, biochar application boosted the soil carbon (C) pool (38.1% in upland and 33.4% in paddy) and decreased soil GHGI (−18.7% in upland and −14.5% in paddy). Our study highlights the role of the reduced CH4 and N2O emissions in the biochar‐induced mitigation of soil GHG emissions while exploring the relative importance of the influencing factors and providing crucial insights for the development of individualized biochar management measures.

Funder

Fundamental Research Funds for the Central Universities

National Natural Science Foundation of China

Publisher

Wiley

Subject

Soil Science,General Environmental Science,Development,Environmental Chemistry

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