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氮素在地球生物中的分布及循环
张 驰1, 李生秀2, 王长春3
1.陕西省政府农业办公室;2.西北农业大学 农化系;3.陕西省铜川市效区农技站
摘要:
地球上98%的氮素存在于原生岩(火成岩)中,但其对氮素循环贡献甚微;大气圈中的气态氮仅是地球中总氮素质量的1.9%,但实际上是供应所有生命需要的唯一氮源;生物圈中的氮量很小,然而全球植物初级净产物中90%~97%的氮在生物圈内循环。氮素在生物圈中的循环主要包括增加、损失和转化3个途径,这种循环因生态系统而不同。
关键词:  氮素,循环,氮素分布,地圈,气圈,生物圈
DOI:
分类号:S154
基金项目:
Geobiological Distribution of N and Its Cycle
Zhang Chi Li Shengxiu Wang Changcun,Zhang Chi Li Shengxiu Wang Changcun,Zhang Chi Li Shengxiu Wang Changcun
Abstract:
The primary (igneous) rocks of the earth's crust hold approximately 97.8% of the global N.However,these rocks contribute very little to the cycling of N.Although gaseous N in the atmosphere represents only 19% of the earth's total N mass,it has apparently contributed virtually the sole source of N for nutrition of all forms of 1ife.In comparison with N contained in the atmosphere and lithosphere,the quantities present in the biosphere are very small.However,on a global scale,90一97% N content of the net primary production of plant is derived from recyeling of N within the biosphere.The N cycling in the biosphere include 3 ways in the main;additions,losses and transformations,and the cycling varies with different ecosystems.
Key words:  N eycling ,N distribution ,lithosphere ,atmosphere, biosphere