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Warianty tytułu
Konferencja
International Conference „Radon in the Environment” (2nd ; 25-29.05.2015 ; Kraków, Poland)
Języki publikacji
Abstrakty
Radon activity concentration (RAC) in the outdoor atmosphere was monitored in four localities of Slovakia. The distance between the localities were up to 130 km. The localities had a diverse orography, ranging from flatland to hilly terrain. A significant infl uence of orography and 226Ra and 222Rn content in soil on diurnal time series of RAC was found. A simple approach of determining radon exhalation rate from soil based on the increase of RAC from daily minima to maxima and removal characteristic of radon is presented. A linear dependency between radon exhalation rate from the soil and RAC in the soil gas at a depth of 0.8 m was found for sandy soils.
Słowa kluczowe
Czasopismo
Rocznik
Tom
Strony
281--288
Opis fizyczny
Bibliogr. 24 poz., rys.
Twórcy
autor
- Department of Nuclear Physics and Biophysics, Faculty of Mathematics, Physics and Informatics, Comenius University, Mlynská dolina F-1, 841 04 Bratislava, Slovak Republic, Tel.: +421 2 602 95 526, Fax: +421 2 654 12 305
autor
- Department of Nuclear Physics and Biophysics, Faculty of Mathematics, Physics and Informatics, Comenius University, Mlynská dolina F-1, 841 04 Bratislava, Slovak Republic, Tel.: +421 2 602 95 526, Fax: +421 2 654 12 305
autor
- Department of Nuclear Physics and Biophysics, Faculty of Mathematics, Physics and Informatics, Comenius University, Mlynská dolina F-1, 841 04 Bratislava, Slovak Republic, Tel.: +421 2 602 95 526, Fax: +421 2 654 12 305
autor
- Faculty of Chemical and Food Technology, Slovak University of Technology, Radlinského 9, 812 37 Bratislava, Slovak Republic
autor
- Slovak Hydrometeorological Institute, Jeséniova 17, 833 15 Bratislava, Slovak Republic
Bibliografia
- 1. Gessel, T. F. (1983). Background atmospheric 222Rn concentrations outdoors and indoors: a review. Health Phys., 45(2), 289–302.
- 2. Garzon, L., Juanco, J. M., Perez, J. M., Fernandez, M. C., & Arganza, B. (1986). The universal Rn wave. An approach. Health Phys., 2, 185–195.
- 3. Chambers, S. D., Williams, A. G., Crawford, J., & Griffiths, A. D. (2015). On the use of radon for quantifying the effects of atmospheric stability on urban emissions. Atmos. Chem. Phys., 15, 1175–1190. DOI: 10.5194/acp-15-1175-2015.
- 4. Schmidt, M., Graul, R., Sartorius, H., & Levin, I. (2003). The Schauinsland CO2 record: 30 years of continental observations and their implications for the variability of the European CO2 budget. J. Geophys. Res., 108(D19), 1–7. DOI: 10.1029/2002JD003085.
- 5. Schmidt, M., Glatzel-Mattheier, H., Sartorius, H., Worthy, D. E., & Levin, I. (2001). Western European N2O emissions: A top-down approach based on atmospheric observations. J. Geophys. Res., 106(D6), 5507–5516. DOI: 10.1029/2000JD900701.
- 6. Sobíšek, B. (Ed.). (1993). Meteorological monolingual and terminological dictionary. Praha, Czech Republic: Academia Praha.
- 7. Podstawczyńska, A., Kozak, K., Pawlak, W., & Mazur, J. (2010). Seasonal and diurnal variation of outdoor radon (222Rn) concentrations in urban and rural area with reference to meteorological conditions. Nukleonika, 55(4), 543–547.
- 8. Zimnoch, M., Wach, P., Chmura, L., Gorczyca, Z., Rozanski, K., Godlowska, J., Mazur, J., Kozak, K., & Jeričević, A. (2014). Factors controlling temporal variability of near-ground atmospheric 222Rn concentration over Central Europe. Atmos. Chem. Phys., 14,9567–9581. DOI: 10.5194/acp-14-9567-2014.
- 9. Foundation Soils. (1987). Czechoslovak technical norm. ČSN 73 1001.
- 10. Beláň, T., Chudý, M., Ďurana, L., Grgula, M., Holý, K., Levaiová, D., Povinec, P., Richtáriková, M., & Šivo, A. (1992). Investigation of radionuclide variations in the Bratislava air. In Rare nuclear processes. Proceedings of 14th Europhysics Conference on Nuclear Physics. 22–26 October 1990 (pp. 345–366). Singapore: World Scientific Publishing.
- 11. Ward, D. C., & Borak, T. B. (1991). Determination of time varying 222Rn concentrations using flow-through scintillation flasks. Health Phys., 61, 799–807.
- 12. BITT Technology. (2007). AMS02 manual v.2.0. Description of the “AMS-02” continuous air monitoring system. BITT Technology-A GmbH, Germany.
- 13. Holý, K., Bulko, M., Polášková, A., Holá, O.,Műllerová, M., & Böhm, R. (2010). Fifteen years of continual monitoring of 222Rn activity concentration in the Bratislava atmosphere. In Proceedings of Environmental Radioactivity Conference. Vienna: IAEA. (IAEA-CN-145/153P).
- 14. Bulko, M., Holý, K., Melicherová, T., Polášková, A., Šimon, J., Műllerová, M., & Holá, O. (2006). Radon in the atmosphere in two different localities of Slovakia. Acta Facultaties Ecologiae, 14, 7–13.
- 15. Műllerová, M., Holý, K., & Bulko, M. (2011). Results of outdoor radon monitoring in Bratislava and Nováky. Radiat. Prot. Dosim., 145(2/3), 325–328.
- 16. Bulko, M., Holý, K., Polášková, A., Holá, O., & Šimon, J. (2006). Volume activity of 222Rn in the atmosphere of the nearby localities with the different orography. In 7th Banská Štiavnica Days 2005, 5–7 October 2005 (pp. 1–8). Senec, Slovakia: ISK.
- 17. UNSCEAR. (2000). Report of the United Nations Scientific Committee on the Effects of Atomic Radiation to the General Assembly. Vol. I: Sources, Annex B: Exposures from natural radiation sources. New York: UN.
- 18. Minato, S. (1988). Seasonal variations in radon concentrations in the lower atmosphere at Nagoya. Nagoya: Government Industrial Research Institute. (Report no. 37(9/10)).
- 19. Fontan, J., Druilhet, A., Lopez, A., Bernis, N. J., & Cautenet, G. (1976). Surveillance de la stabilité vertical dans un site urbain. Pollution Atmospherique, 71, 231–240.
- 20. Sesana, L., Barbieri, L., Facchini, U., & Marcazzan, G. (1998). 222Radon as a tracer of atmospheric motions: A study in Milan. Radiat. Prot. Dosim., 78(1), 65–71.
- 21. Guedalia, D., Ntsila, A., Druilhet, A., & Fontan, J. (1980). Monitoring of the atmospheric stability above an urban and suburban site using sodar and radon measurements. J. Appl. Meteor., 19, 839–848. http://dx.doi.org/10.1175/1520-0450.
- 22. State Geological Institute of Dionýz Štúr. (2014). Map server. Retrieved December 15, 2015, from http://mapserver.geology.sk/radio/.
- 23. Mazur, J., & Kozak, K. (2014). Complementary system for long term measurements of radon exhalation rate from soil. Rev. Sci. Instrum., 85(2). DOI:10.1063/1.4865156.
- 24. Szegvary, T., Leuenberger, M. C., & Conen, F. (2007).Predicting terrestrial 222Rn flux using gamma dose rate as a proxy. Atmos. Chem. Phys., 7, 2789–2795
Uwagi
PL
Opracowanie ze środków MNiSW w ramach umowy 812/P-DUN/2016 na działalność upowszechniającą naukę.
Typ dokumentu
Bibliografia
Identyfikator YADDA
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