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斯瓦尔巴德表层雪中多环芳烃的季节性变化。

The seasonal change of PAHs in Svalbard surface snow.

机构信息

Department of Environmental Sciences, Informatics and Statistics (DAIS), Ca' Foscari University of Venice, Via Torino 155, 30172, Venezia-Mestre, Venice, Italy; Institute of Polar Sciences - National Research Council (ISP-CNR), Via Torino 155, 30172, Venezia-Mestre, Venice, Italy.

Department of Environmental Sciences, Informatics and Statistics (DAIS), Ca' Foscari University of Venice, Via Torino 155, 30172, Venezia-Mestre, Venice, Italy; Institute of Polar Sciences - National Research Council (ISP-CNR), Via Torino 155, 30172, Venezia-Mestre, Venice, Italy.

出版信息

Environ Pollut. 2024 Jan 1;340(Pt 1):122864. doi: 10.1016/j.envpol.2023.122864. Epub 2023 Nov 2.

Abstract

The Arctic region is threatened by contamination deriving from both long-range pollution and local human activities. Polycyclic Aromatic Hydrocarbons (PAHs) are environmental tracers of emission, transport and deposition processes. A first campaign has been conducted at Ny-Ålesund, Svalbard, from October 2018 to May 2019, monitoring weekly concentrations of PAHs in Arctic surface snow. The trend of the 16 high priority PAH compounds showed that long-range inputs occurred mainly in the winter, with concentrations ranging from 0.8 ng L to 37 ng L. In contrast to this, the most abundant analyte retene, showed an opposite seasonal trend with highest values in autumn and late spring (up to 97 ng L), while in winter this compound remained below 3 ng L. This is most likely due to local contributions from outcropping coal deposits and stockpiles. Our results show a general agreement with the atmospheric signal, although significant skews can be attributed to post-depositional processes, wind erosion, melting episodes and redistribution.

摘要

北极地区受到源自远距离污染和当地人类活动的污染的威胁。多环芳烃 (PAHs) 是排放、迁移和沉积过程的环境示踪剂。首次在斯瓦尔巴群岛的新奥尔松进行了一次活动,从 2018 年 10 月至 2019 年 5 月,每周监测北极地表雪中的多环芳烃浓度。16 种高优先级 PAH 化合物的趋势表明,远距离输入主要发生在冬季,浓度范围从 0.8 ng/L 到 37 ng/L。相比之下,最丰富的分析物 retene 表现出相反的季节性趋势,秋季和春末(高达 97 ng/L)的浓度最高,而冬季这种化合物仍低于 3 ng/L。这很可能是由于露头的煤沉积物和库存的本地贡献。尽管可以归因于沉积后过程、风蚀、融雪事件和再分配,但我们的结果与大气信号基本一致。

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