硝化作用
矿化(土壤科学)
生态系统
氮气循环
环境科学
陆地生态系统
土壤有机质
有机质
亚热带
生态学
生物量(生态学)
农学
氮气
环境化学
土壤科学
土壤水分
生物
化学
有机化学
作者
Zihong Zhu,Hu Du,Kun Gao,Yuantian Fang,Kelin Wang,Tongbin Zhu,Jing Zhu,Yi Cheng,Dejun Li
标识
DOI:10.1111/1365-2664.14407
摘要
Abstract Plant species diversity (PSD) regulates ecosystem structure and functions, and is a key issue we need to consider when design vegetation restoration projects. Increasing PSD has been shown to promote or decrease soil nitrogen (N) availability, but the underlying mechanisms have not been well explored. Here, 45 plots with the Shannon–Weiner indices ranging from 0.15 to 3.57 were selected in a subtropical forest to explore the effect of PSD on soil N transformations. Higher PSD significantly enhanced the rates of gross N mineralization, gross nitrification, microbial N immobilization, net N mineralization, net nitrification and the contents of soil total N and inorganic N. Structural equation modelling showed that PSD indirectly impacted gross N transformations via its roles in regulating soil organic matter, mineral and microbial traits. Higher PSD stimulated gross N mineralization and nitrification mainly via its positive effects on microbial biomass content and gene abundances of chiA , archaeal or bacterial amoA , while increased microbial N immobilization mainly due to its stimulation of soil organic matter. Synthesis and applications . Our findings highlight the crucial role of PSD in stimulating soil N availability and provide a mechanistic understanding which can be integrated into Earth system models to better predict soil N availability and C sequestration in response to PSD.
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