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Seasonal and diurnal variation of outdoor radon (222Rn) concentrations in urban and rural area with reference to meteorological conditions

Treść / Zawartość
Identyfikatory
Warianty tytułu
Konferencja
Proceedings of the International Conference "Radon in Environment" 10-14 May 2009, Zakopane Poland
Języki publikacji
EN
Abstrakty
EN
The objective of the study was to investigate temporal variability of outdoor radon (222Rn) concentration registered in the center of Łódź (urban station), at Ciosny (rural station) and Kraków (suburban station) in relation to meteorological parameters (i.e. air temperature, temperature vertical gradient, wind speed, soil heat flux, volumetric water content in soil) with special consideration of urban-rural differences. Continuous measurements of 222Rn concentration (at 60 min intervals) were performed at a height of 2 m above the ground using AlphaGUARDŽ PQ2000PRO (ionization chamber) from January 2008 to May 2009. 222Rn levels were characterized by a diurnal cycle with an early morning maximum and a minimum in the afternoon. The well-marked 24 h pattern of radon concentration occurred in summer at anticyclonic weather with cloudless sky, light wind and large diurnal temperature ranges. The urban measurement site was characterized by the lowest atmospheric 222Rn concentration and an urban-rural differences of radon levels increased from winter to summer and during the nighttime periods. The maximum contrasts of 222Rn levels between Łódź and Ciosny, reaching – 30 Bqźm–3, were registered in June and July during the urban heat island (UHI) phenomenon (a positive thermal anomaly of a city if compared to rural area) and strong thermal inversion near the ground in the rural area.
Czasopismo
Rocznik
Strony
543--547
Opis fizyczny
Bibliogr.15 poz., rys.
Twórcy
autor
autor
autor
  • Department of Meteorology and Climatology, University of Łódź, 88 Narutowicza Str., 90-139 Łódź, Poland, Tel.: +48 42 665 5959, Fax: +48 42 665 5951, apodstaw@uni.lodz.pl
Bibliografia
  • 1. Arnold D, Vargas A, Ortega X (2009) Analysis of radon progeny concentration measured at the Spanish radioactive aerosol automatic monitoring network. Appl Radiat Isot 67:833–838
  • 2. Baciu AC (2005) Radon and thoron progeny concentration variability in relation to meteorological conditions at Bucharest (Romania). J Environ Radioactiv 83:171–189
  • 3. Biernacka M, Isajenko K, Lipiński P, Pietrzak-Flis Z (2006) Radiation atlas of Poland 2005. Biblioteka Monitoringu Środowiska, Główny Inspektorat Ochrony Środowiska, Warszawa (in Polish/English)
  • 4. Duenas C, Perez M, Fernandez MC, Carretero J (1996) Radon concentration in the surface air and vertical atmosphericstability in the lower atmosphere. J Environ Radioactiv 31:87–102
  • 5. Fortuniak K (2005) Urban climate research in Poland. Global Change 12:35–47
  • 6. Kataoka T, Tsukamoto O (1992) Variation of 222Rn concentration in outdoor air due to variation of the atmospheric boundary layer. Radiat Prot Dosim 45;1/4:403–406
  • 7. Kłysik K (1996) Spatial and seasonal distribution of antropogenic heat emission in Lodz, Poland. Atmos Environ 33:3885–3895
  • 8. Krajny E, Ośródka L, Skowronek J, Skubacz K, Wojtylak M (2005) Diurnal variation of the mixing-layer height and polonium concentration in the air. Int J Environ Pollut 25:95–104
  • 9. Landsberg HE (1981) The urban climate. Academic Press, New York
  • 10. Mazur J (2008) Dynamics of the process of radon exhalation from ground in connection with meteorological parameters and soil properties. IFJ PAN Report no.2014/AP (Ph.D. thesis). IFJ, Kraków, http://www.ifj.edu.pl/publ/reports/2008/2014.pdf (in Polish)
  • 11. Oke TR (1987) Boundary layer climate. Metheun, London
  • 12. Perrino C, Pietrodangelo A, Febo A (2001) An atmospheric stability index based on radon progeny measurements for the evaluation of primary urban pollution. Atmos Environ 35:5235–5244
  • 13. Porstendörfer J, Butterweck G, Reineking A (1991) Diurnal variation of concentration of radon and its short-lived daughters in the atmosphere near the ground. Atmos Environ 25:709–713
  • 14. Sesana L, Barbieri L, Facchini U, Marcazzan G (1998) 222Rn as a tracer of atmospheric motions: a study in Milan. Radiat Prot Dosim 78:65–71
  • 15.Winkler R, Ruckerbauer F, Trautmannsheimer M, Tschiersch J, Karg E (2001) Diurnal and seasonal variation of the equlibrium state between short-lived radon decay products and radon gas in the ground-level air. Radiat Environ Biophys 40:115–123
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BUJ7-0014-0087
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