Christensen Søren, Rousk Kathrin
Copenhagen University, Department of Biology, VOLT, Center for Volatile Interactions, Universitetsparken 15, 2100 Copenhagen, Denmark.
iScience. 2024 Jan 26;27(2):109042. doi: 10.1016/j.isci.2024.109042. eCollection 2024 Feb 16.
In some places, NO emissions have doubled during the last 2-3 decades. Therefore, it is crucial to identify NO emission hotspots from terrestrial and aquatic systems. Large variation in NO emissions occur in managed as well as in natural areas. Natural unmanaged tropical and subtropical wet forests are important NO sources globally. Emission hotspots, often coupled to human activities, vary across climate zones, whereas NO emissions are most often a few kg N ha year from arable soils, drained organic soils in the boreal and temperate zones often release 20-30 kg N ha year. Similar high NO emissions occur from some tropical crops like tea, palm oil and bamboo. This strong link between increased NO emissions and human activities highlight the potential to mitigate large emissions. In contrast, water where oxic and anoxic conditions meet are NO emission hotspots as well, but not possible to reduce.
在一些地方,一氧化氮排放量在过去二三十年里增加了一倍。因此,识别陆地和水生系统中的一氧化氮排放热点至关重要。一氧化氮排放在人工管理区域和自然区域都存在很大差异。天然的未受管理的热带和亚热带湿润森林是全球重要的一氧化氮排放源。排放热点往往与人类活动相关,在不同气候区有所不同,而耕地土壤的一氧化氮排放量通常为每年每公顷几千克氮,北方和温带地区排水后的有机土壤通常每年释放20 - 30千克氮。一些热带作物如茶叶、棕榈油和竹子也会有类似的高一氧化氮排放。一氧化氮排放增加与人类活动之间的这种紧密联系凸显了减少大量排放的潜力。相比之下,有氧和无氧条件交汇的水域也是一氧化氮排放热点,但无法减少。