东南欧某地水溶性棕碳的来源

Charalampia Baliaka, Christos Kaltsonoudis, K. Florou, Spiro D. Jorga, Christina N. Vasilakopoulou, J. Kodros, Andreas Aktypis, Angeliki Matrali, D. Paraskevopoulou, M. Masiol, S. Pandis, A. Nenes
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引用次数: 1

摘要

大气棕色碳(BrC)是一个高度不确定的,但对大气中光吸收的潜在重要贡献者。实验室和实地研究表明,BrC可以从多种来源产生,包括化石燃料燃烧和生物质燃烧(BB)的一次排放,以及通过许多反应途径的二次形成。目前认为大气中BrC的主要来源是BB的一次排放,但相对较少的研究在具有复杂源剖面的环境中证实了这一点。2020年,在为期一个月的冬季期间,在希腊帕特雷西南部的伯罗奔尼撒大学校园内进行了一项实地活动,该校园代表了一个城市遗址。在此期间,收集了环境过滤器样品(共35个过滤器),其中使用类似于Hecobian等人(2010)的半自动系统测定水溶性BrC,其中在1 m路径长度上测量吸收。为了测量BrC,将紫外可见分光光度计与液体波导毛细管电池耦合,在365和700 nm处记录光吸收强度。后者被用作参考波长。我们发现Patras在365 nm波长处的BrC平均吸收率为8.5 ±3.9 Mm-1表明这一时期有机气溶胶中存在显著的BrC。同时使用化学成分数据观察(主要是有机碳、黑碳和硝酸盐)结合正矩阵分解分析来确定BrC的来源。该分析表明,除了生物质燃烧(贡献约20%)和其他燃烧排放(也接近20%)的重要作用外,氧化有机气溶胶(约40%)也是研究区域BrC的重要贡献者。ReferenceHecobian,张,X。,郑,M,弗兰克,N。,好的,大肠,韦伯,R.J。2010。美国东南部测量的水溶性有机气溶胶物质和水萃取物的光吸收特性。大气压。化学。物理10,5965 –5977。https://doi.org/10.5194/acp - 10 - 5965 - 2010 - & # 160;
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Sources of water-soluble Brown Carbon at a South-Eastern European Site

Atmospheric brown carbon (BrC) is a highly uncertain, but potentially important contributor to light absorption in the atmosphere. Laboratory and field studies have shown that BrC can be produced from multiple sources, including primary emissions from fossil fuel combustion and biomass burning (BB), as well as secondary formation through a number of reaction pathways. It is currently thought that the dominant source of atmospheric BrC is primary emissions from BB, but relatively few studies demonstrate this in environments with complex source profiles.

A field campaign was conducted during a month-long wintertime period in 2020 on the campus of the University of Peloponnese in the southwest of Patras, Greece which represents an urban site. During this time, ambient filter samples (a total of 35 filters) were collected from which the water-soluble BrC was determined using a semi-automated system similar to Hecobian et al. (2010),  where absorption was measured over a 1 m path length. To measure the BrC, a UV-Vis Spectrophotometer was coupled to a Liquid Waveguide Capillary Cell and the light absorption intensity was recorded at 365 and 700 nm. The latter was used as a reference wavelength. We found that the average BrC absorption in Patras at a wavelength of 365 nm was 8.5 ± 3.9 Mm-1 suggesting that there was significant BrC in the organic aerosol during this period. Attribution of sources of BrC was done using simultaneous chemical composition data observations (primarily organic carbon, black carbon, and nitrate) combined with Positive Matrix Factorization analysis. This analysis showed that in addition to the important role of biomass burning (a contribution of about 20%) and other combustion emissions (also close to 20%), oxidized organic aerosol (approximately 40%) is also a significant contributor to BrC in the study area.

Reference

Hecobian, A., Zhang, X., Zheng, M., Frank, N., Edgerton, E.S., Weber, R.J., 2010. Water-soluble organic aerosol material and the light-absorption characteristics of aqueous extracts measured over the Southeastern United States. Atmos. Chem. Phys. 10, 5965–5977. https://doi.org/10.5194/acp-10-5965-2010

 

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