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Stable isotope natural abundance of nitrous oxide emitted from Antarctic tundra soils: effects of sea animal excrement depositions

机译:从南极冻原土壤中释放出来的一氧化二氮的稳定同位素自然丰度:海洋动物排泄物沉积物的影响

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Nitrous oxide (N2O), a greenhouse gas, is mainly emitted from soils during the nitrification and denitrification processes. N2O stable isotope investigations can help to characterize the N2O sources and N2O production mechanisms. N2O isotope measurements have been conducted for different types of global terrestrial ecosystems. However, no isotopic data of N2O emitted from Antarctic tundra ecosystems have been reported although the coastal ice-free tundra around Antarctic continent is the largest sea animal colony on the global scale. Here, we report for the first time stable isotope composition of N2O emitted from Antarctic sea animal colonies (including penguin, seal and skua colonies) and normal tundra soils using in situ field observations and laboratory incubations, and we have analyzed the effects of sea animal excrement depositions on stable isotope natural abundance of N2O. For all the field sites, the soil-emitted N2O was N-15- and O-18-depleted compared with N2O in local ambient air. The mean delta values of the soil-emitted N2O were delta N-15 -13.5 +/- 3.2 parts per thousand and delta O-18 = 26.2 +/- 1.4 parts per thousand for the penguin colony, delta N-15 = -11.5 +/- 5.1 parts per thousand and delta O-18 = 26.4 +/- 3.5 parts per thousand for the skua colony and delta N-15 = -18.9 +/- 0.7 parts per thousand and delta O-18 = 28.8 +/- 1.3 parts per thousand for the seal colony. In the soil incubations, the isotopic composition of N2O was measured under N-2 and under ambient air conditions. The soils incubated under the ambient air emitted very little N2O (2.93 mu g N2O-N kg(-1)). Under N-2 conditions, much more N2O was formed (9.74 mu g N2O-N kg(-1)), and the mean delta N-15 and delta O-18 values of N2O were -19.1 +/- 8.0 parts per thousand and 21.3 +/- 4.3 parts per thousand, respectively, from penguin colony soils, and -17.0 +/- 4.2 parts per thousand and 20.6 +/- 3.5 parts per thousand, respectively, from seal colony soils. The data from in situ field observations and laboratory experiments point to denitrification as the predominant N2O source from Antarctic sea animal colonies. Copyright (c) 2008 John Wiley & Sons, Ltd.
机译:一氧化二氮(N2O)是一种温室气体,主要在硝化和反硝化过程中从土壤中排放。 N2O稳定同位素研究可以帮助表征N2O来源和N2O产生机制。已针对不同类型的全球陆地生态系统进行了N2O同位素测量。然而,尽管南极大陆周围的沿海无冰冻苔原是全球规模最大的海洋动物群落,但尚未报道南极冻原生态系统排放的N2O同位素数据。在这里,我们首次使用现场观察和实验室培养报告了南极海洋动物群落(包括企鹅,海豹和贼鸥群落)和正常冻原土壤中排放的N2O的稳定同位素组成,并分析了海洋动物的影响稳定的N2O同位素自然排泄物上的排泄物沉积。在所有野外场所,与本地环境空气中的N2O相比,土壤排放的N2O减少了N-15和O-18。土壤排放的N2O的平均增量值是企鹅种群的增量N-15 -13.5 +/- 3.2千分之一和增量O-18 = 26.2 +/- 1.4千分之千的企鹅殖民地,增量N-15 = -11.5贼鸥的+/- 5.1千分之一和O-18 = 26.4 +/- 3.5千分之一,δN-15 = -18.9 +/- 0.7千分之一和十O-18 = 28.8 +/-密封殖民地千分之1.3。在土壤培养中,在N-2和环境空气条件下测量N2O的同位素组成。在环境空气下孵育的土壤几乎不排放N2O(2.93μgN2O-N kg(-1))。在N-2条件下,形成了更多的N2O(9.74μgN2O-N kg(-1)),N2O的平均增量N-15和增量O-18值为-19.1 +/- 8.0千分之一企鹅殖民地土壤分别为每千分之一和21.3 +/- 4.3份,海豹殖民地土壤分别为每千分之-17.0 +/- 4.2份和千分之20.6 +/- 3.5份。来自现场观察和实验室实验的数据表明,反硝化是南极海洋动物群落中主要的N2O来源。版权所有(c)2008 John Wiley&Sons,Ltd.

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