Global distribution of N2O emissions from aquatic systems: natural emissions and anthropogenic effects

Sybil P Seitzinger , Carolien Kroeze , Renée V Styles
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引用次数: 214

Abstract

Context Abstract: Atmospheric concentrations of nitrous oxide, a greenhouse gas, are increasing due to human activities. Our analysis suggests that a third of global anthropogenic N2O emission is from aquatic sources (rivers, estuaries, continental shelves) and the terrestrial sources comprise the remainder. Over 80% of aquatic anthropogenic N2O emissions are from the Northern Hemisphere mid-latitudes consistent with the geographic distribution of N fertilizer use, human population and atmospheric N deposition. These N inputs to land have increased aquatic as well as terrestrial anthropogenic N2O emissions because a substantial portion enters aquatic systems and results in increased N2O production. Thus, wise management of N in the terrestrial environment could help reduce/control both aquatic and terrestrial N2O emissions.

Main Abstract: The global distribution of N2O emissions from rivers, estuaries, continental shelves, and oceans are compared to each other, and to terrestrial emissions, using existing gridded inventories. Rivers, estuaries and continental shelves (1.9 Tg N y−1) account for about 35% of total aquatic N2O emissions; oceanic emissions comprise the remainder. Oceanic N2O emissions are approximately equally distributed between the Northern and Southern Hemispheres; however, over 90% of emissions from estuaries and rivers are in the Northern Hemisphere. N2O emissions from rivers, estuaries, and continental shelves combined equal oceanic emissions in both the 20°–45°N and 45°–66°N latitudinal zones. Over 90% of river and estuary emissions are considered anthropogenic (1.2 Tg N y−1); only 25% of continental shelf emissions are considered anthropogenic (0.1 Tg N y−1); oceanic emissions are considered natural. Overall, approximately one third of both aquatic and of terrestrial emissions are anthropogenic.

Natural terrestrial emissions are highest in tropical latitudes while natural aquatic emissions are relatively evenly distributed among latitudinal zones. Over half of both the anthropogenic terrestrial and aquatic emissions occur between 20° and 66°N. Anthropogenic N inputs to the terrestrial environment drive anthropogenic N2O emissions from both land and aquatic ecosystems, because a substantial portion of the anthropogenic N applied to watersheds enters rivers, estuaries and continental shelves.

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水生系统N2O排放的全球分布:自然排放和人为影响
摘要:由于人类活动,大气中一氧化二氮(一种温室气体)的浓度正在增加。我们的分析表明,全球人为N2O排放的三分之一来自水生来源(河流、河口、大陆架),其余部分由陆地来源构成。超过80%的水生人为N2O排放来自北半球中纬度地区,这与氮肥使用、人口和大气氮沉降的地理分布一致。这些向陆地输入的氮增加了水生和陆地人为的N2O排放,因为很大一部分进入水生系统并导致N2O产量增加。因此,明智地管理陆地环境中的氮可以帮助减少/控制水生和陆地的N2O排放。摘要/ Abstract摘要:利用现有的网格化清单,比较了全球河流、河口、大陆架和海洋的N2O排放分布,并与陆地的N2O排放进行了比较。河流、河口和大陆架(1.9 Tg N y−1)约占水生N2O总排放量的35%;剩下的是海洋排放。海洋N2O排放在北半球和南半球之间的分布大致相等;然而,超过90%的河口和河流排放在北半球。在20°-45°N和45°-66°N纬向带,河流、河口和大陆架的N2O排放总和相等。超过90%的河流和河口排放被认为是人为的(1.2 Tg N y−1);只有25%的大陆架排放被认为是人为的(0.1 Tg N y−1);海洋排放被认为是自然的。总的来说,大约三分之一的水生和陆地排放是人为的。自然陆地排放在热带纬度地区最高,而自然水生排放在纬向带之间分布相对均匀。超过一半的人为陆地和水生排放发生在北纬20°至66°之间。陆地环境的人为N输入驱动陆地和水生生态系统的人为N2O排放,因为施加于流域的大量人为N进入河流、河口和大陆架。
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