Comparison of particulate number concentrations in three Central European capital cities

被引:32
作者
Borsos, T. [1 ]
Rimnacova, D. [2 ]
Zdimal, V. [2 ]
Smolik, J. [2 ]
Wagner, Z. [3 ]
Weidinger, T. [4 ]
Burkart, J. [5 ]
Steiner, G. [5 ]
Reischl, G. [5 ]
Hitzenberger, R. [5 ]
Schwarz, J. [2 ]
Salma, I. [1 ]
机构
[1] Eotvos Lorand Univ, Inst Chem, Budapest, Hungary
[2] Acad Sci Czech Republic, Inst Chem Proc Fundamentals, Dept Aerosols & Laser Studies, CR-16502 Prague, Czech Republic
[3] Acad Sci Czech Republic, Inst Chem Proc Fundamentals, E Hala Lab Thermodynam, CR-16502 Prague, Czech Republic
[4] Eotvos Lorand Univ, Dept Meteorol, Budapest, Hungary
[5] Univ Vienna, Fac Phys, Vienna, Austria
基金
奥地利科学基金会; 匈牙利科学研究基金会;
关键词
Urban environment; Ultrafine aerosol; Diurnal variation; Number size distribution; New particle formation; SIZE DISTRIBUTION; ULTRAFINE PARTICLES; ATMOSPHERIC AEROSOL; PHYSICAL-CHARACTERIZATION; NUCLEATION EVENTS; CCN ACTIVATION; GROWTH-RATES; LONG-TERM; URBAN; DISTRIBUTIONS;
D O I
10.1016/j.scitotenv.2012.06.052
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Number size distributions of atmospheric aerosol particles in the mobility diameter range from 10 to 1000 nm were determined in Budapest. Prague and Vienna for a one-year-long period. Particle number concentrations in various size fractions, their diurnal and seasonal variations, mean size distributions and some properties of new particle formation events were derived and compared. Yearly median particle number concentrations for Budapest, Prague and Vienna were 10.6 x 10(3), 7.3 x 10(3) and 8.0 x 10(3) cm(-3). Differences were linked to the different pollution levels of the cities, and to diverse measurement environments and local conditions. Mean contributions of ultrafine particles (particles with a mobility diameter <100 nm) to the total number concentration were 80%, 84% and 74% for Budapest, Prague and Vienna, thus these particles represent an overwhelming share of all particles in each city. Seasonal variation of particle number concentrations was not obvious. Diurnal variations of particles with a diameter between 100 and 1000 nm (N100-1000) exhibited similar shape for the cities, which was related to the time-activity pattern of inhabitants and regional influences. The structure of the diurnal variation for ultrafine particles was also similar. It contained a huge morning peak in each city which was explained by emissions from vehicular traffic. The second peak was shifted from afternoon rush hours to late evenings as a result of the daily cycling in meteorological parameters. The character of the measurement site also influenced the diurnal variation. Diurnal variation of the mean ratio of ultrafine particles to N100-1000 clearly revealed the presence and importance of new particle formation and subsequent growth in urban environments. Nucleation frequencies in Budapest and Prague were 27% and 23%, respectively on a yearly time scale. They showed a minimum in winter for both places, while the largest nucleation activity was observed in spring for Budapest, and in summer for Prague. (C) 2012 Elsevier B.V. All rights reserved.
引用
收藏
页码:418 / 426
页数:9
相关论文
共 38 条
  • [1] Aerosol particle number concentration measurements in five European cities using TSI-3022 condensation particle counter over a three-year period during health effects pollution on susceptible subpopulations
    Aalto, P
    Hämeri, K
    Paatero, P
    Kulmala, M
    Bellander, T
    Berglind, N
    Bouso, L
    Castano-Vinyals, G
    Sunyer, J
    Cattani, G
    Marconi, A
    Cyrys, J
    von Klot, S
    Peters, A
    Zetzsche, K
    Lanki, T
    Pekkanen, J
    Nyberg, F
    Sjövall, B
    Forastiere, F
    [J]. JOURNAL OF THE AIR & WASTE MANAGEMENT ASSOCIATION, 2005, 55 (08) : 1064 - 1076
  • [2] Physical characterization of aerosol particles during nucleation events
    Aalto, P
    Hämeri, K
    Becker, E
    Weber, R
    Salm, J
    Mäkelä, JM
    Hoell, C
    O'Dowd, CD
    Karlsson, H
    Hansson, HC
    Väkevä, M
    Koponen, IK
    Buzorius, G
    Kulmala, M
    [J]. TELLUS SERIES B-CHEMICAL AND PHYSICAL METEOROLOGY, 2001, 53 (04): : 344 - 358
  • [3] Deep Investigation of Ultrafine Particles in Urban Air
    Avino, Pasquale
    Casciardi, Stefano
    Fanizza, Carla
    Manigrasso, Maurizio
    [J]. AEROSOL AND AIR QUALITY RESEARCH, 2011, 11 (06) : 654 - 663
  • [4] Fine and ultrafine particles in the Zurich (Switzerland) area measured with a mobile laboratory:: an assessment of the seasonal and regional variation throughout a year
    Bukowiecki, N
    Dommen, J
    Prévôt, ASH
    Weingartner, E
    Baltensperger, U
    [J]. ATMOSPHERIC CHEMISTRY AND PHYSICS, 2003, 3 : 1477 - 1494
  • [5] Long-term study of cloud condensation nuclei (CCN) activation of the atmospheric aerosol in Vienna
    Burkart, J.
    Steiner, G.
    Reischl, G.
    Hitzenberger, R.
    [J]. ATMOSPHERIC ENVIRONMENT, 2011, 45 (32) : 5751 - 5759
  • [6] Dal Maso M, 2005, BOREAL ENVIRON RES, V10, P323
  • [7] European Commission Joint Research Centre - European Academies Science Advisory Council, 2011, 24847 JRCEASAC
  • [8] CCN activation of oxalic and malonic acid test aerosols with the University of Vienna cloud condensation nuclei counter
    Giebl, H
    Berner, A
    Reischl, G
    Puxbaum, H
    Kasper-Giebl, A
    Hitzenberger, R
    [J]. JOURNAL OF AEROSOL SCIENCE, 2002, 33 (12) : 1623 - 1634
  • [9] Multisite study of particle number concentrations in urban air
    Harrison, RM
    Jones, AM
    [J]. ENVIRONMENTAL SCIENCE & TECHNOLOGY, 2005, 39 (16) : 6063 - 6070
  • [10] Intercomparison of thermal and optical measurement methods for elemental carbon and black carbon at an urban location
    Hitzenberger, R.
    Petzold, A.
    Bauer, H.
    Ctyroky, P.
    Pouresmaeil, P.
    Laskus, L.
    Puxbaum, H.
    [J]. ENVIRONMENTAL SCIENCE & TECHNOLOGY, 2006, 40 (20) : 6377 - 6383