GSTDTAP  > 地球科学
DOI10.1016/j.atmosres.2018.06.004
Sources and physicochemical characteristics of submicron aerosols during three intensive campaigns in Granada (Spain)
del Aguila, A.1; Sorribas, M.1; Lyamani, H.2,3; Titos, G.2,4; Olmo, F. J.2,3; Arruda-Moreira, G.2,5; Yela, M.1; Alados-Arboledas, L.2,3
2018-11-15
发表期刊ATMOSPHERIC RESEARCH
ISSN0169-8095
EISSN1873-2895
出版年2018
卷号213页码:398-410
文章类型Article
语种英语
国家Spain; Brazil
英文摘要

Aerosol particles in the submicron range and their physicochemical characteristics were investigated for the first time in Granada, southeastern Iberian Peninsula, during three intensive campaigns. The physical and chemical characteristics were analysed during two spring campaigns and one autumn campaign. New particle formation (NPF) events were found to be more frequent in spring than in autumn. The mean duration, growth rates and maximum diameters had ranges of 5.3-13.2 h, 2.4-4.0 nm h(-1) and 35-47 nm, respectively. In addition, one shrinkage event occurred and had a duration of 2.2 h and a shrinkage rate of -2.5 nm h(-1). During a period of atmospheric stagnation conditions under the influence of mountain breezes, three consecutive NPF events occurred. The high frequency of the NPF events was attributed to higher temperature and radiation levels and lower relative humidity than during a previous day with similar stagnant conditions but no nucleation occurrence. According to correlation analysis, mineral components correlated with particle number in the Aitken mode, while metals and secondary inorganic aerosols correlated with particle number in the finer and larger fractions, respectively. Pollutants such as CO, NO2, NO and black carbon showed moderate and high correlations with particle number in the submicron fraction. To assess the impact of the particle number contribution according to sources, a new approach was introduced using black carbon concentrations, resulting in four major contributors: urban background, traffic, NPF and biomass burning. The proposed approach was validated by means of different models based on the aerosol spectral dependencies and chemical compositions that classify aerosol populations. Both the models and the proposed approach identified biomass burning and fossil fuel particles during the same periods, and the results showed good agreement. The proposed approach can guide future studies attempting to account for submicron particle contributions in other urban environments.


英文关键词Submicron size distribution Chemical composition Source apportionment New particle formation Biomass burning Traffic contribution
领域地球科学
收录类别SCI-E
WOS记录号WOS:000442169800034
WOS关键词ULTRAFINE ATMOSPHERIC PARTICLES ; PARTICULATE AIR-POLLUTION ; OPTICAL-PROPERTIES ; NUMBER CONCENTRATIONS ; NUCLEATION EVENTS ; SIZE DISTRIBUTION ; CARBON AEROSOLS ; BOUNDARY-LAYER ; SAHARAN DUST ; LONG-TERM
WOS类目Meteorology & Atmospheric Sciences
WOS研究方向Meteorology & Atmospheric Sciences
引用统计
被引频次:12[WOS]   [WOS记录]     [WOS相关记录]
文献类型期刊论文
条目标识符http://119.78.100.173/C666/handle/2XK7JSWQ/38509
专题地球科学
作者单位1.Natl Inst Aerosp Technol INTA, Atmospher Res & Instrumentat Branch, Mazagon 21130, Huelva, Spain;
2.Univ Granada, Andalusian Inst Earth Syst Res, IISTA CEAMA, Granada 18006, Spain;
3.Univ Granada, Dept Appl Phys, E-18071 Granada, Spain;
4.Inst Environm Assessment & Water Res IDAEA, CSIC, Dept Geosci, Barcelona, Spain;
5.Inst Energet & Nucl Res IPEN, Sao Paulo, Brazil
推荐引用方式
GB/T 7714
del Aguila, A.,Sorribas, M.,Lyamani, H.,et al. Sources and physicochemical characteristics of submicron aerosols during three intensive campaigns in Granada (Spain)[J]. ATMOSPHERIC RESEARCH,2018,213:398-410.
APA del Aguila, A..,Sorribas, M..,Lyamani, H..,Titos, G..,Olmo, F. J..,...&Alados-Arboledas, L..(2018).Sources and physicochemical characteristics of submicron aerosols during three intensive campaigns in Granada (Spain).ATMOSPHERIC RESEARCH,213,398-410.
MLA del Aguila, A.,et al."Sources and physicochemical characteristics of submicron aerosols during three intensive campaigns in Granada (Spain)".ATMOSPHERIC RESEARCH 213(2018):398-410.
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