Elemental Composition and Size Distribution of Atmospheric Aerosols During Long Range Transport

1984 ◽  
pp. 339-347 ◽  
Author(s):  
Petra Metternich ◽  
H.-W. Georgii ◽  
K. O. Groeneveld
Keyword(s):  
Elemental Composition ◽  
Size Distribution ◽  
Long Range ◽  
Atmospheric Aerosols ◽  
Long Range Transport ◽  
Range Transport

Observation of difference in the size distribution of carbon and major inorganic compounds of atmospheric aerosols after the long-range transport between the selected days of winter and summer

2008 ◽  
Vol 42 (5) ◽  
pp. 1057-1063 ◽  
Author(s):  
Kyu-Won Hwang ◽  
Joo-Ho Lee ◽  
Dae-Young Jeong ◽  
Chi-Hun Lee ◽  
Amit Bhatnagar ◽  
...  
Keyword(s):  
Size Distribution ◽  
Long Range ◽  
Atmospheric Aerosols ◽  
Inorganic Compounds ◽  
Long Range Transport ◽  
Range Transport

Regional and Transported A erosols in Ambient A tmosphere of Raipur,India, during W inter

2021 ◽  
Vol 30 (1) ◽  
pp. 7-17
Author(s):  
Manas Kanti Deb ◽  
Mithlesh Mahilang ◽  
Jayant Nirmalkar
Keyword(s):  
Size Distribution ◽  
Long Range ◽  
Fine Particles ◽  
Characteristic Size ◽  
Long Range Transport ◽  
Bimodal Size Distribution ◽  
Entire Study ◽  
Coarse Mode ◽  
Range Transport ◽  
Air Trajectory

Size fractionated atmospheric aerosols were collected using cascade impactor sampler on quartz flter substrate during October 2015 to February 2016 in campus of Pt Ravishankar Shukla University of Raipur Chhattisgarh. The size of aerosol particles is of crucial importance to several processes in the atmosphere. The relative concentrations in both modes are responsible for the variability observed in the shape of the size distribution. Characteristic size distributions of measured aerosol over central India showed identifcation of three main behaviour types during entire study period: (i) month in which bimodal size distribution dominated in coarse mode (October 2015, 5 December 2015 and January, 2016), (ii) those months in which bimodal distribution equally intense in both one, and coarse modes (November, 2015) and (iii) those which were mainly dominated within fine (February, 2016, December, 2015). The two-subsequent month namely November 2015 and December 2015 shows bimodal size distribution with dominance in fine size range in comparison to coarse mode, possibly these high loading of one particles is due to long range transport. The peculiar observation of air trajectory shows that there is increase in fine particles concentration during December 2015, although there in increase in temperature and wind speed. The reason for this high concentration is long range transport of air masses. However, January has normal trend in particular matter concentration. The important finding of the present study based on characteristic size distribution and air trajectory plots accomplishes that fine particles are obtained through long range transport whereas coarse particles are mainly from local origin.

Monitoring Aerosol Elemental Composition in Particle Size Fractions in Case of Long-Range Transport

1983 ◽  
Vol 30 (2) ◽  
pp. 1282-1284 ◽  
Author(s):  
Petra Metternich ◽  
H.-W. Georgii ◽  
K. O. Groeneveld
Keyword(s):  
Particle Size ◽  
Elemental Composition ◽  
Long Range ◽  
Long Range Transport ◽  
Size Fractions ◽  
Particle Size Fractions ◽  
Range Transport

Aerosol ionic components at Mt. Heng in central southern China: Abundances, size distribution, and impacts of long-range transport

2012 ◽  
Vol 433 ◽  
pp. 498-506 ◽  
Author(s):  
Xiaomei Gao ◽  
Likun Xue ◽  
Xinfeng Wang ◽  
Tao Wang ◽  
Chao Yuan ◽  
...  
Keyword(s):  
Size Distribution ◽  
Long Range ◽  
Southern China ◽  
Long Range Transport ◽  
Range Transport ◽  
Ionic Components

scholarly journals Chemically speciated mass size distribution, particle effective density and origin of non-refractory PM<sub>1 </sub>measured at a rural background site in Central Europe

2021 ◽  
Author(s):  
Petra Pokorná ◽  
Naděžda Zíková ◽  
Radek Lhotka ◽  
Petr Vodička ◽  
Saliou Mbengue ◽  
...  
Keyword(s):  
Size Distribution ◽  
Long Range ◽  
Central Europe ◽  
Effective Density ◽  
Long Range Transport ◽  
Air Masses ◽  
Mass Size Distribution ◽  
Background Site ◽  
Range Transport ◽  
Mass Size

Abstract. The seasonal variability of non-refractory PM1 (NR-PM1) was studied at a rural background site (National Atmospheric Observatory Košetice – NAOK) in the Czech Republic to examine the impact of atmospheric regional and long-range transport in Central Europe. NR-PM1 measurements were performed by compact time-of-flight aerosol mass spectrometry (C-ToF-AMS), and the chemically speciated mass size distributions, effective density, and origin were discussed. The average PM1 concentrations, calculated as the sum of the NR-PM1 (after collection efficiency corrections – CE corrections of 0.4 and 0.33 in summer and winter, respectively) and the equivalent black carbon (eBC) concentrations measured by an aethalometer (AE), were 8.58 ± 3.70 μg m−3 in summer and 10.08 ± 8.04 μg m−3 in winter. Organics dominated during both campaigns (summer/winter: 4.97 ± 2.92/4.55 ± 4.40 μg m−3), followed by sulphate in summer (1.68 ± 0.81/1.36± 1.38 μg m−3) and nitrate in winter (0.67 ± 0.38/2.03 ± 1.71 μg m−3). The accumulation mode dominated the average mass size distribution during both seasons, with larger particles of all species measured in winter (mode diameters: Org: 334/413 nm, NO3−: 377/501 nm, SO42−: 400/547 nm, and NH4+: 489/515 nm) pointing to regional and long-range transport. However, since the winter aerosols were less oxidized than the summer aerosols (comparing fragments f44 and f43), the importance of local sources in the cold part of the year was not negligible. The average PM1 particle effective density, defined as the ratio of the mass to the volume of a particle, corresponded to higher inorganic contents during both seasons (summer: ∼ 1.30 g cm−3 and winter: ∼ 1.40 g cm−3). However, the effective densities during episodes of higher mass concentrations calculated based on the particle number (mobility diameter) and mass size distribution (vacuum aerodynamic diameter) were even higher, ranging from 1.40–1.60 g cm−3 in summer and from 1.40–1.75 g cm−3 in winter. Although aged continental air masses from the SE were rare in summer (7 %), they were connected with the highest concentrations of all NR-PM1 species, especially sulphate and ammonium. In winter, slow continental air masses from the SW (44 %) were linked to inversion conditions over Central Europe and were associated with the highest concentrations among all NR-PM1 measurements.

Effect of local and long-range transport emissions on the elemental composition of PM10–2.5 and PM2.5 in Beirut

2007 ◽  
Vol 41 (31) ◽  
pp. 6497-6509 ◽  
Author(s):  
Najat A. Saliba ◽  
Hovig Kouyoumdjian ◽  
Mohamad Roumié
Keyword(s):  
Elemental Composition ◽  
Long Range ◽  
Long Range Transport ◽  
Range Transport ◽  
Transport Emissions
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