Characterizing the impact of urban emissions on regional aerosol particles: airborne measurements during the MEGAPOLI experiment

被引:47
|
作者
Freney, E. J. [1 ]
Sellegri, K. [1 ]
Canonaco, F. [2 ]
Colomb, A. [1 ]
Borbon, A. [3 ]
Michoud, V. [3 ]
Doussin, J. -F. [3 ]
Crumeyrolle, S. [1 ]
Amarouche, N. [4 ]
Pichon, J. -M. [1 ]
Bourianne, T. [5 ]
Gomes, L. [5 ]
Prevot, A. S. H. [2 ]
Beekmann, M. [3 ]
Schwarzenboeeck, A. [1 ]
机构
[1] CNRS Univ Blaise Pascal, Lab Meteorol Phys, UMR6016, Clermont Ferrand, France
[2] Paul Scherrer Inst, Lab Atmospher Chem, CH-5232 Villigen, Switzerland
[3] UPEC, LISA IPSL, Lab Interuniv Syst Atmospher, LISA IPSL,UMR CNRS 7583, Paris, France
[4] CNRS, Div Tech, Inst Natl Sci Univers, UPS 855, F-92195 Meudon, France
[5] Ctr Natl Rech Meteorol, URA1357, Toulouse, France
关键词
POSITIVE MATRIX FACTORIZATION; ORGANIC AEROSOL; SOURCE APPORTIONMENT; MEXICO-CITY; CHEMICAL-COMPOSITION; TIME EVOLUTION; MEGACITY; SIZE; SYSTEM; PARIS;
D O I
10.5194/acp-14-1397-2014
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The MEGAPOLI (Megacities: Emissions, urban, regional and Global Atmospheric POLlution and climate effects, and Integrated tools for assessment and mitigation) experiment took place in July 2009. The aim of this campaign was to study the aging and reactions of aerosol and gas-phase emissions in the city of Paris. Three ground-based measurement sites and several mobile platforms including instrument equipped vehicles and the ATR-42 aircraft were involved. We present here the variations in particle-and gas-phase species over the city of Paris, using a combination of high-time resolution measurements aboard the ATR-42 aircraft. Particle chemical composition was measured using a compact time-of-flight aerosol mass spectrometer (C-ToF-AMS), giving detailed information on the non-refractory submicron aerosol species. The mass concentration of black carbon (BC), measured by a particle absorption soot photometer (PSAP), was used as a marker to identify the urban pollution plume boundaries. Aerosol mass concentrations and composition were affected by air-mass history, with air masses that spent longest time over land having highest fractions of organic aerosol and higher total mass concentrations. The Paris plume is mainly composed of organic aerosol (OA), BC, and nitrate aerosol, as well as high concentrations of anthropogenic gas-phase species such as toluene, benzene, and NOx. Using BC and CO as tracers for air-mass dilution, we observe the ratio of Delta OA/Delta BC and Delta OA/Delta CO increase with increasing photochemical age (-log(NOx/NOy)). Plotting the equivalent ratios of different organic aerosol species (LV-OOA, SV-OOA, and HOA) illustrate that the increase in OA is a result of secondary organic aerosol (SOA) formation. Within Paris the changes in the Delta OA/Delta CO are similar to those observed during other studies in London, Mexico City, and in New England, USA. Using the measured SOA volatile organic compounds (VOCs) species together with organic aerosol formation yields, we were able to predict similar to 50% of the measured organics. These airborne measurements during the MEGAPOLI experiment show that urban emissions contribute to the formation of OA and have an impact on aerosol composition on a regional scale.
引用
收藏
页码:1397 / 1412
页数:16
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