生物炭
固碳
纤维素酶
化学
土壤碳
环境化学
农学
土壤水分
土壤科学
环境科学
酶
热解
生物
生物化学
有机化学
二氧化碳
作者
Jiao Feng,Dailin Yu,Robert L. Sinsabaugh,Daryl Moorhead,Mathias Neumann Andersen,Pete Smith,Yanting Song,Xinqi Li,Qiaoyun Huang,Yu‐Rong Liu,Ji Chen
摘要
ABSTRACT Biochar amendment is one of the most promising agricultural approaches to tackle climate change by enhancing soil carbon (C) sequestration. Microbial‐mediated decomposition processes are fundamental for the fate and persistence of sequestered C in soil, but the underlying mechanisms are uncertain. Here, we synthesise 923 observations regarding the effects of biochar addition (over periods ranging from several weeks to several years) on soil C‐degrading enzyme activities from 130 articles across five continents worldwide. Our results showed that biochar addition increased soil ligninase activity targeting complex phenolic macromolecules by 7.1%, but suppressed cellulase activity degrading simpler polysaccharides by 8.3%. These shifts in enzyme activities explained the most variation of changes in soil C sequestration across a wide range of climatic, edaphic and experimental conditions, with biochar‐induced shift in ligninase:cellulase ratio correlating negatively with soil C sequestration. Specifically, short‐term (<1 year) biochar addition significantly reduced cellulase activity by 4.6% and enhanced soil organic C sequestration by 87.5%, whereas no significant responses were observed for ligninase activity and ligninase:cellulase ratio. However, long‐term (≥1 year) biochar addition significantly enhanced ligninase activity by 5.2% and ligninase:cellulase ratio by 36.1%, leading to a smaller increase in soil organic C sequestration (25.1%). These results suggest that shifts in enzyme activities increased ligninase:cellulase ratio with time after biochar addition, limiting long‐term soil C sequestration with biochar addition. Our work provides novel evidence to explain the diminished soil C sequestration with long‐term biochar addition and suggests that earlier studies may have overestimated soil C sequestration with biochar addition by failing to consider the physiological acclimation of soil microorganisms over time.
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