生态系统
氮气循环
硝化作用
陆地生态系统
浸出(土壤学)
氮气
环境化学
自行车
反硝化
垃圾箱
环境科学
一氧化二氮
生物量(生态学)
化学
农学
土壤有机质
生态学
土壤水分
土壤科学
生物
林业
有机化学
地理
作者
Lei Meng,Yuanhe Yang,Yiqi Luo,Changming Fang,Xuhui Zhou,Jiakuan Chen,Xin Yang,Bo Li
标识
DOI:10.1111/j.1469-8137.2010.03563.x
摘要
• Anthropogenic nitrogen (N) addition may substantially alter the terrestrial N cycle. However, a comprehensive understanding of how the ecosystem N cycle responds to external N input remains elusive. • Here, we evaluated the central tendencies of the responses of 15 variables associated with the ecosystem N cycle to N addition, using data extracted from 206 peer-reviewed papers. • Our results showed that the largest changes in the ecosystem N cycle caused by N addition were increases in soil inorganic N leaching (461%), soil NO3− concentration (429%), nitrification (154%), nitrous oxide emission (134%), and denitrification (84%). N addition also substantially increased soil NH4+ concentration (47%), and the N content in belowground (53%) and aboveground (44%) plant pools, leaves (24%), litter (24%) and dissolved organic N (21%). Total N content in the organic horizon (6.1%) and mineral soil (6.2%) slightly increased in response to N addition. However, N addition induced a decrease in microbial biomass N by 5.8%. • The increases in N effluxes caused by N addition were much greater than those in plant and soil pools except soil NO3−, suggesting a leaky terrestrial N system.
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