生物炭
修正案
表土
底土
环境科学
农学
土壤水分
土壤碳
全溶胶
总有机碳
环境化学
Ultisol公司
碳纤维
营养物
生物固体
土壤改良剂
土壤分类
固碳
营养循环
土壤肥力
土壤生物学
化学
土壤有机质
浸出(土壤学)
微生物种群生物学
土壤科学
土壤质量
氮气循环
氮气
作者
Kaiyue Song,Zhiwei Liu,Ruiling Ma,Qi Yi,Jufeng Zheng,Rongjun Bian,Kun Cheng,Shaopan Xia,Xiaoyu Liu,Xuhui Zhang,Lianqing Li
出处
期刊:Biochar
[Springer Nature]
日期:2026-03-16
卷期号:8 (1)
标识
DOI:10.1007/s42773-026-00577-0
摘要
Abstract Soil microbial necromass carbon (MNC), a major contributor to stable soil organic C (SOC), is increasingly recognized as a crucial indicator of long-term C sequestration. However, the depth-dependent responses of MNC to long-term biochar amendment remain poorly understood. Here, we conducted a 12-year field experiment in two contrasting cropland soils—a C-rich Entisol and a C-poor Ultisol—to assess the effects of biochar on MNC accumulation and composition in both topsoil (0–20 cm) and subsoil (20–40 cm). In the topsoil, biochar increased MNC by 23.3% in the Entisol and 39.0% in the Ultisol, with a stronger response in fungal necromass than in bacterial necromass. Conversely, subsoil MNC decreased by 17.9–30.4% across both soils. These contrasting patterns were associated with biochar-induced changes in nutrient availability and microbial traits, including nitrogen availability, enzyme activity, metabolic quotient, and microbial biomass. To complement our findings, a meta-analysis of 85 pairs of observations from 23 peer-reviewed studies confirmed that biochar increased topsoil MNC in 83.5% of cases, with an average increase of 10.2%. The magnitude of the effect was greater in soils with low initial SOC and high sand content, and it intensified over time, peaking 10 years after application. In summary, 12-year biochar amendment enhanced MNC accumulation in the topsoil but reduced it in the subsoil, highlighting the importance of long-term and depth-specific evaluations to fully understand biochar’s role in microbially mediated SOC sequestration.
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