生物炭
矿化(土壤科学)
表土
酸杆菌
修正案
土壤碳
微生物种群生物学
土壤水分
总有机碳
环境科学
环境化学
化学
农学
土壤科学
蛋白质细菌
地质学
生物
热解
生物化学
16S核糖体RNA
政治学
细菌
法学
古生物学
有机化学
基因
作者
Ruiling Ma,Xiulan Wu,Zhiwei Liu,Qi Yi,Man Xu,Jufeng Zheng,Rongjun Bian,Shouxin Zhang,Genxing Pan
标识
DOI:10.1016/j.crsust.2023.100214
摘要
Soil organic carbon (SOC), mineralization and microbial community structures were investigated at different depths of farmland soils 4 years after a single biochar amendment. Biochar increased SOC at 0-20cm (10.7%) and 20-40cm (24.9%). Mineralization decreased with depth and further decreased 12.3% (0-20cm), 8.5% (20-40cm) and 30.5% (40-60cm) with biochar amendment. Subsoils selected for oligotrophs (e.g., Chloroflexi, Acidobacteria) associated with lower mineralization rates and limited copiotrophs (e.g., Proteobacteria, Ascomycota) which exhibit higher respiration rates. Biochar enhanced oligotrophs in topsoil and restricted copiotrophs at all depths. This demonstrates how biochar increases SOC stability by changing microbial community structures at different depths.
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