土壤呼吸
活性氮
环境科学
土壤碳
固碳
氮气
大气碳循环
碳循环
生物地球化学循环
氮气循环
土壤有机质
大气(单位)
生态系统
沉积(地质)
环境化学
土壤科学
化学
土壤水分
生态学
地质学
生物
古生物学
有机化学
沉积物
物理
热力学
作者
Ivan A. Janssens,Wouter Dieleman,Sebastiaan Luyssaert,Jens‐Arne Subke,Markus Reichstein,R. Ceulemans,Philippe Ciais,A. J. Dolman,J. Grace,Gioṙgio Matteucci,Dario Papale,S. L. Piao,Ernst‐Detlef Schulze,Jianwu Tang,B. E. Law
摘要
The use of fossil fuels and fertilizers has increased the amount of biologically reactive nitrogen in the atmosphere over the past century. A meta-analysis suggests that nitrogen deposition typically impedes the decomposition of carbon in forest soils, significantly reducing carbon dioxide emissions to the atmosphere. The use of fossil fuels and fertilizers has increased the amount of biologically reactive nitrogen in the atmosphere over the past century. As a consequence, forests in industrialized regions have experienced greater rates of nitrogen deposition in recent decades. This unintended fertilization has stimulated forest growth, but has also affected soil microbial activity, and thus the recycling of soil carbon and nutrients. A meta-analysis suggests that nitrogen deposition impedes organic matter decomposition, and thus stimulates carbon sequestration, in temperate forest soils where nitrogen is not limiting microbial growth. The concomitant reduction in soil carbon emissions is substantial, and equivalent in magnitude to the amount of carbon taken up by trees owing to nitrogen fertilization. As atmospheric nitrogen levels continue to rise, increased nitrogen deposition could spread to older, more weathered soils, as found in the tropics; however, soil carbon cycling in tropical forests cannot yet be assessed.
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