土壤水分
土壤有机质
优势(遗传学)
土壤碳
启动(农业)
生物
农学
有机质
生态系统
热带和亚热带湿润阔叶林
森林生态学
生态学
菌根
矿化(土壤科学)
氮气循环
负启动
自行车
环境科学
土壤类型
土壤pH值
土壤生物学
碳循环
外生菌根
植物
温带森林
丛枝菌根
微生物种群生物学
营养循环
化学
土壤分类
亚热带
土壤化学
母材
土壤微生物学
作者
Xionghui Liu,Liang Chen,Wenhua Xiang,Shuai Ouyang,Huili Wu,Yanting Hu,Pifeng Lei,Xiangwen Deng,Xiaodong Fang,Biao Zhu,Yakov Kuzyakov
摘要
soil after 28 days of incubation). This is primarily because AM dominated soils have greater availability of mineral-associated organic matter and nitrate content, as well as higher microbial carbon use efficiency. Tree mycorrhizal associations thus regulate priming effects through depth-dependent changes in C stability, nitrogen availability, and microbial functional activity. We conclude that forecasting forest C dynamics in response to mycorrhizal compositional shifts must account for these soil depth-specific mechanisms.
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