环境科学
地球大气中的二氧化碳
氮气
一氧化二氮
二氧化碳
海洋学
大气科学
辐射压力
水位下降(水文)
气候变化
生态学
化学
地质学
地下水
岩土工程
有机化学
含水层
生物
作者
Robert A. Duce,Julie LaRoche,Katye E. Altieri,Kevin R. Arrigo,Alex R. Baker,Douglas G. Capone,Sarah Cornell,Frank Dentener,James N. Galloway,Raja S. Ganeshram,Richard J. Geider,T. D. Jickells,M. M. Kuypers,Rebecca Langlois,Peter S. Liss,S. M. Liu,Jack J. Middelburg,C. Mark Moore,Slobodan Ničković,Andreas Oschlies
出处
期刊:Science
[American Association for the Advancement of Science]
日期:2008-05-16
卷期号:320 (5878): 893-897
被引量:1138
标识
DOI:10.1126/science.1150369
摘要
Increasing quantities of atmospheric anthropogenic fixed nitrogen entering the open ocean could account for up to about a third of the ocean's external (nonrecycled) nitrogen supply and up to â¼3% of the annual new marine biological production, â¼0.3 petagram of carbon per year. This input could account for the production of up to â¼1.6 teragrams of nitrous oxide (N 2 O) per year. Although â¼10% of the ocean's drawdown of atmospheric anthropogenic carbon dioxide may result from this atmospheric nitrogen fertilization, leading to a decrease in radiative forcing, up to about two-thirds of this amount may be offset by the increase in N 2 O emissions. The effects of increasing atmospheric nitrogen deposition are expected to continue to grow in the future.
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