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在斯瓦尔巴群岛的新奥尔松对低级羰基化合物和碳氢化合物进行测量。

Measurements of lower carbonyls and hydrocarbons at Ny-Alesund, Svalbard.

作者信息

Mabilia Rosanna, Di Palo Vincenzo, Cassardo Claudio, Ciuchini Carla, Pasini Antonello, Possanzini Massimiliano

机构信息

CNR Institute for Atmospheric Pollution, CP 10, 00016-Monterotondo Scalo, Rome, Italy.

出版信息

Ann Chim. 2007 Oct;97(10):1027-37. doi: 10.1002/adic.200790087.

Abstract

Measurements of gaseous organic compounds were carried out near Ny-Alesund, in the Norwegian Arctic, during September 2004. Twenty alkanes, alkenes and aromatic hydrocarbons from ethane to toluene and six aldehydes and ketones from formaldehyde to butanal, were identified and quantified in air samples. Hydrocarbons showed a quite uniform distribution, with ethane being by far the most abundant component (> 1 ppb), followed by propane (> 0.4 ppb) and butanes (> 0.3 ppb), while for unsaturated homologues, except ethene, concentrations never exceeding 0.05 ppb were observed. This distribution confirmed that hydrocarbon depletion during the transport time from Europe into the Arctic was depending upon their atmospheric lifetimes, calculated relatively to the OH reactivity scale. The presence of short lived hydrocarbons could be associated to local sources of anthropogenic and/or biogenic origin. Although the local air photochemistry played a primary role in the production of lower aldehydes in late summer, the observed mixing ratios of formaldehyde (in the 0.25 - 0.50 ppb range) could not be fully explained by known gas-phase chemistry. In this case additional sources, such as fluxes of formaldehyde from snow pack to the atmosphere and/or local anthropogenic activities, were to be taken into consideration. The possible influences of these sources on HCHO mixing ratios were analysed by means of a backward-trajectory circulation model.

摘要

2004年9月,在挪威北极地区的新奥尔松附近对气态有机化合物进行了测量。在空气样本中鉴定并定量了从乙烷到甲苯的20种烷烃、烯烃和芳烃,以及从甲醛到丁醛的6种醛和酮。碳氢化合物呈现出相当均匀的分布,乙烷是迄今为止含量最高的成分(>1 ppb),其次是丙烷(>0.4 ppb)和丁烷(>0.3 ppb),而对于不饱和同系物,除乙烯外,观察到其浓度从未超过0.05 ppb。这种分布证实,从欧洲输送到北极期间碳氢化合物的消耗取决于它们相对于OH反应性尺度计算的大气寿命。短寿命碳氢化合物的存在可能与人为和/或生物源的本地来源有关。尽管当地的空气光化学在夏末低级醛的产生中起主要作用,但观测到的甲醛混合比(在0.25 - 0.50 ppb范围内)无法用已知的气相化学完全解释。在这种情况下,需要考虑其他来源,如雪堆向大气的甲醛通量和/或当地的人为活动。通过反向轨迹环流模型分析了这些来源对HCHO混合比的可能影响。

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