PL EN


Preferencje help
Widoczny [Schowaj] Abstrakt
Liczba wyników
Czasopismo
2015 | 13 | 1 |
Tytuł artykułu

Water-soluble inorganic ions in urban aerosols of the continental part of Balkans (Belgrade) during the summer – autumn (2008)

Treść / Zawartość
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
Size-segregated aerosol samples were collected using six stages High Volume Cascade Impactor. Aerosol mass and water soluble ions concentrations were determined. The Hybrid Single-Particle Lagrangian Integrated Trajectory (HYSPLIT) model was used to study the origin of air masses arriving to Belgrade in the investigated period. The obtained results of aerosol mass and water-soluble ion concentrations have been divided into six sub-data sets based on air mass categories. The highest average mass concentration of the fine mode (Dp ≤ 0.49 μm) was found for air masses coming to Belgrade from the southeast and northwest directions, and of the coarse mode (3.0 < Dp ≤7.2 μm) for air masses arriving from the northwest direction. The highest concentrations of SO42– were found in the fine particles transported to the investigated area by air masses from southeast direction. The analysis of contribution of marine aerosol components (Na+ and Cl-), the Correlation and Cluster Analysis indicated the influence of marine aerosol on urban aerosol of the central Balkans coming from the Western Mediterranean and northern direction. NH4+ and SO42- and K+ dominated in the fine mode for all air mass categories. PCA demonstrated the dominant impact of secondary aerosol formation processes on urban aerosols.
EN
Wydawca
Czasopismo
Rocznik
Tom
13
Numer
1
Opis fizyczny
Daty
otrzymano
2013-10-16
zaakceptowano
2014-04-23
online
2014-11-01
Twórcy
  • Institute of Chemistry, Technology and Metallurgy – Centre of Chemistry, University of Belgrade ,11158 Belgrade, Serbia
  • Institute of Chemistry, Technology and Metallurgy – Centre of Chemistry, University of Belgrade ,11158 Belgrade, Serbia
  • Faculty of Chemistry, University of Belgrade, 11158 Belgrade, Serbia
  • Department of Meteorology, University of Belgrade, 11158 Belgrade, Serbia
  • Faculty of Physical Chemistry, University of Belgrade, 11158 Belgrade, Serbia
  • Institute for the Dynamics of Environmental Processes (CNR-IDPA), 30123 Venice, Italy
  • Environmental Sciences, Informatics, Statistic Department, Ca‘ Foscari University of Venice, 30123 Venice, Italy
Bibliografia
  • [1] Seinfeld J.H., Pandis S.N., Atmospheric Chemistry and Physics: From Air Pollution to Climate Change, John Wiley & Sons, Inc, New York, 1998
  • [2] Glavas S., Moschonas N., Atmos. Environ., 2002, 36, 3089
  • [3] Seinfeld J.H., Atmospheric Chemistry and Physics of Air Pollution, Wiley, New York, 1986
  • [4] Putaud J.P., Van Dingenen R., Dell’ Acqua A., Raes F., Matta E., Decesari S. et al., Atmos. Chem. Phys., 2004, 4, 889
  • [5] Đorđević D., Mihajlidi-Zelić A., Relić D., Ignjatović Lj., Huremović J., Stortini A.M., Gambaro A., Atmos. Environ., 2012, 46, 309
  • [6] Querol X., Alastuey A., Viana M.M., Rodriguez S., Artińano B., Salvador P. et al., Aerosol. Sci., 2004, 35, 1151
  • [7] Delalieux F., Van Grieken R., Potgieter J.H., Mar. Pollut. Bull., 2006, 52, 606[Crossref]
  • [8] Kishcha P., Ničković S., Starobinetes B., di Sarra A., Udisti R., Becagli S. et al., Atmos. Res., 2011, 100, 28
  • [9] Draxler R.R., Hess G.D., Description of the Hysplit_4 modeling system, NOAA Tech. Memo. ERL ARL-224, NOAA Air Resources Laboratory, Silver Spring, MD, 1997, 24
  • [10] Draxler R.R., Hess G.D., Aust. Met. Mag., 1998, 47, 295
  • [11] Draxler R.R., Rolph G.D., HYSPLIT (HYbrid Single-Particle Lagrangian Integrated Trajectory) Model access via NOAA ARL, NOAA Air Resources Laboratory, Silver Spring, MD, 2011, http://ready.arl.noaa.gov/HYSPLIT.php
  • [12] Rolph G.D., Real-time Environmental Applications and Display sYstem (READY), NOAA Air Resources Laboratory, Silver Spring, MD, 2011, http://ready.arl.noaa.gov
  • [13] Poissant L., Atmos. Environ., 1999, 33, 2537
  • [14] Perkauskas D., Proceedings of Millennium (24th) NATO/CCMS International Technical Meeting on Air Pollution Modelling and its Application, 15-19 May 2000, Boulder, Colorado, USA, 212
  • [15] Đorđević D., Tošić I., Unkašević M., Đurašković P., Environ. Sci. Poll. Res., 2010, 17, 1591[Crossref]
  • [16] Stortini A.M., Freda A., Cesari D., Cairns W.R.L., Contini D., Barbante C. et al., Atmos. Environ., 2009, 43, 6296
  • [17] Kalnay E., Kanamitsu M., Kistler R., Collins W. et al., Bull. Amer. Meteor. Soc., 1996, 77, 437[Crossref]
  • [18] Cuccia E., Bernardoni V., Massabò D., Prati P., Valli G., Vecchi R., Atmos. Environ., 2010, 44, 3304
  • [19] Espinosa A.J.F., Rodríguez M.T., de la Rosa F.J.B., Sánchez J.C.J., Atmos. Environ., 2001, 35, 2595
  • [20] Pikridas M., Bougiatioti A., Hildebrandt L., Engelhart G.J., Kostenidou E., Mohr C. et al., Atmos. Chem. Phys., 2010, 10, 6793
  • [21] Wittmaack K., Menzel N., Wehnes H., Heinzmann U., Atmos. Environ., 2002, 36, 5877
  • [22] Tsitouridou R., Papazova P., Simeonova P., Simeonov V., J. Environ. Sci. Health A, 2013, 48(14), 1815[Crossref]
  • [23] Chrysikou L.P., Samara C.A., Atmos. Environ., 2009, 43, 4557
  • [24] Maksimović M., Jovanović M., Nikolić K., Copper, 2007, 32(1), 1
  • [25] Đorđević D., Šolević T., Arsić P., Petrović S., Beograd University, Novi Beograd, 2004, (in Serbian) http://archive.rec.org/REC/Programs/REREP/LawDrafting/status/Serbia_and_Montenegro/Serbian/Srbija/Izvestaji/Konacni%20izvestaj_Pancevo.pdf
  • [26] Marenco F., Bonasoni P., Calzolari F., Ceriani M., Chiari M., Cristofanelli P. et al., J. Geophys. Res., 2006, 111, D24202 (), DOI: 10.1029/2006JD007145[Crossref]
  • [27] Beuck H., Quass U., Klemm O., Kuhlbusch T.A.J., Atmos. Environ., 2011, 45, 5813
  • [28] Astel A., Mazerski J., Polkowska Z., Namiesnik J., Adv. Environ. Res., 2004, 8, 337[Crossref]
  • [29] Huang S., Rahn K.A., Arimoto R., Atmos. Environ., 1999, 33, 2169
Typ dokumentu
Bibliografia
Identyfikatory
Identyfikator YADDA
bwmeta1.element.-psjd-doi-10_1515_chem-2015-0010
JavaScript jest wyłączony w Twojej przeglądarce internetowej. Włącz go, a następnie odśwież stronę, aby móc w pełni z niej korzystać.