氮循环与气候

H. Dolman
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引用次数: 0

摘要

介绍了氮循环及其反硝化和硝化过程,包括厌氧氨氧化过程。人类通过哈伯-博世过程干预的重要性通过确定农业粮食生产的巨大增长来满足不断增长的世界人口而得到体现。描述了从海洋和陆地排放氧化亚氮的过程。本文还描述了活性氮通过陆地水进入海洋的作用,在沿海地区提供富营养化,以及氮在气溶胶形成中的作用。然后讨论氮循环的地质记录与地球氧合作用的关系。讨论了氮对碳循环的影响。
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The Nitrogen Cycle and Climate
The nitrogen cycle is described, together with its denitrification and nitrification processes, including the Anammox process. The importance of human intervention through the Haber–Bosch process is shown by identifying the tremendous growth of agricultural food production for a growing world population. The processes of emission of nitrous oxide from the ocean and land are described. The role of reactive nitrogen in cascading through land water into the ocean, where it provides eutrophication in coastal areas, is also described, as is the role of nitrogen in aerosol formation. The geological record of nitrogen cycling is then discussed in relation to Earth’s oxygenation. The impact of nitrogen on the carbon cycle is also discussed.
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Reflections on the Anthropocene The Nitrogen Cycle and Climate Aerosols and Climate Methane Cycling and Climate The Hydrological Cycle and Climate
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