Nitrogen deposition suppresses soil respiration by reducing global belowground activity

被引:4
作者
Xiao, Wenya [1 ]
Chen, Chen [2 ]
Chen, Han Y. H. [2 ]
机构
[1] Jiangsu Univ, Sch Emergency Management, Sch Environm & Safety Engn, Zhenjiang 212013, Jiangsu, Peoples R China
[2] Lakehead Univ, Fac Nat Resources Management, 955 Oliver Rd, Thunder Bay, ON P7B 5E1, Canada
基金
加拿大自然科学与工程研究理事会;
关键词
Microbial biomass; N deposition; Root biomass; Soil pH; Soil respiration; Structure equation model; FINE-ROOT; MICROBIAL ACTIVITY; 1/5; H2O; FOREST; BIOMASS; PH; TEMPERATURE; LIMITATION; DIVERSITY; INCREASES;
D O I
10.1016/j.scitotenv.2024.171246
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Soil respiration (Rs) indicates below-ground biological activities. Previous studies have suggested that higher nitrogen (N) deposition due to human activities exerts an increasingly negative effect on Rs. However, the mechanisms underlying this negative effect remain highly uncertain on a global scale. Using a global dataset of 262 N addition experiments, here we show the overall N addition effects on Rs changed from positive to negative with increasing N addition rate and duration. By constructing a structural equation model (SEM) that explained 41 % variation in the responses of Rs to N addition, we revealed that Rs under increasing N addition was simultaneously associated with decreases in soil pH, root biomass and microbial biomass, with the strongest influence by root biomass. Decreasing soil pH had cascading effects on root and microbial biomass, while Naddition-induced root biomass reduction further manifested a decrease in microbial biomass. Across global variations in the environment, lower background soil pH amplified the negative impacts of N addition on root and microbial biomass, which consequently exhilarated the negative impact of high N on Rs. Our results highlight that predicting the response of belowground biological activities to global changes is complex with the essence of integrative understanding for the multivariate pathways through soil physical properties, plants and microorganisms.
引用
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页数:8
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