NATURAL RADIATION DUE TO RADON. CASE STUDY: RADON CONCENTRATION IN HOUSES FROM APUSENI MOUNTAINS

Authors

  • Nicoleta BICAN-BRIȘAN Babeş-Bolyai University, Faculty of Environmental Science and Engineering, 30 Fântânele Street, 400294 Cluj-Napoca, Romania. https://orcid.org/0000-0003-1264-712X
  • Mircea Claudiu MOLDOVAN Babeş-Bolyai University, Faculty of Environmental Science and Engineering, 30 Fântânele Street, 400294 Cluj-Napoca, Romania. *Corresponding author: mircea.moldovan@ubbcluj.ro https://orcid.org/0000-0002-4727-1321
  • Bety-Denissa BURGHELE Babeş-Bolyai University, Faculty of Environmental Science and Engineering, 30 Fântânele Street, 400294 Cluj-Napoca, Romania. https://orcid.org/0000-0003-2711-8271
  • Petronela DAVID Babeş-Bolyai University, Faculty of Environmental Science and Engineering, 30 Fântânele Street, 400294 Cluj-Napoca, Romania.

DOI:

https://doi.org/10.24193/subbambientum.2017.2.01

Keywords:

radon concentration, soil permeability, dose, radon risk.

Abstract

As a radioactive decay product from rocks, in natural conditions, radon is a source of radiation for the population. Moreover, the awareness regarding the fact that this type of natural radiation is of great radiological health significance for the general population has increased since high concentrations of indoor radon were detected. The first step to prevent the risk of exposure to radon is to identify the sources and find the appropriate mitigation method. Once formed by the disintegration of heavy elements in the Earth’s crust, radon diffuses into the soil and water, and then it is transported to the atmosphere. Being a noble gas, which doesn’t take part in chemical reactions, radon is present in the environmental factors, such as air, water, soil and can accumulates in enclosed spaces with restricted air circulation. The aim of this paper is to determine the total amount of radon to which household members of two houses from Avram Iancu and Câmpeni (Alba County) are being exposed. The radon concentration values were within the national and international proposed limits in the field of radioprotection.

References

Barnet I., Pacherová P., Neznal M., Neznal M., 2008, Radon in geological environment: Czech experience. CGS Special Papers, 19, Czech Geological Survey, Prague.

Cosma C., Cucos (Dinu) A., Papp B., Begy R., Gabor A., Bican-Brișan N., Besutiu L., 2014, Radon implication in life and earth science: Baita-Stei area and Peceneaga-Camena fault (Romania). Carpathian Journal of Earth and Environmental Science, 9(2), pp. 15-21.

Cosma C., Moldovan M., Dicu T., Kovacs T., 2008, Radon in water from Transylvania (Romania). Rad. Meas., 43, pp 1423–1428.

Cosma C., Ristoiu D., 1996, Radon in various environmental samples in the Herculane Spa, Cerna Valley, Romania. Env. Int., 22(1), pp. 383-388.

Cucoş-Dinu A., Cosma C., Dicu T., Begy R., Moldovan M., Papp B., Niţă D.C. Burghele B., Sainz C., 2012, Thorough investigations on indoor radon in Băiţa radon-prone area (Romania). Sci. Tot. Env., 431, pp.78–83.

EU, 2001. European Union Commission Recommendation on the protection of the public against exposure to radon in drinking water supplies (2001/928/Euratom). Office Journal of the European Community, L 344, 28 December, pp. 85–88.

Gunby J.A., Darby S.C., Miles J.C., Green B.M., Cox D.R., 1993, Factors affecting indoor radon concentrations in the United Kingdom. Health Physics, 64(1), pp. 2-12.

ICRP, 2012, Effective dose from inhaled radon and its progeny, by Harrison, J.D., Marsh, J.W., ICRP Publication.

Matolin M., 2010, Protocol on the evaluation of comparison measurement of radon (222Rn) activity concentration in soil gas at reference sites Cetyne, Bohostice and Buk (Czech Republic), Report.

Nazaroff W.W., Moed B.A. Sextro R.G., 1988, Soil as a source of indoor radon: Generation, migration and entry. In: W.W. Nazaroff and A.V. Nero (eds.), Radon and its Decay Products in Indoor Air, John Wiley and Sons Inc., New York, pp. 55-112.

Neznal M., Neznal M., Matolín M. Barnet I., Miksova J., 2004, The new method for assessing the radon risk of building sites. CGS Special Papers, 16, Czech Geological Survey, Prague.

Plch J., Eng M., 2012, Manual for operating LUK 3A, SMM Prague.

Ryan T.P., Sequeira S., McKittrick L., Colgan P.A., 2003, RPII- 03/1 Radon in Drinking Water in Co. Wicklow – a Pilot Study, Radiological protection institute of Ireland, February, pp.12.

Scivyer C., 2007. Radon Guidance on Protective Measures for New Buildings, BR211. BRE, Watford, BRE Press.

UNSCEAR 2000, Sources and effects of ionizing radiation. Report to the General Assembly, Volume I: Sources. United Nations Scientific Committee on the Effects of Atomic Radiation.

Zajzon N., Szentpeteri K., Szakall K., Kristally F., 2015, The origin of the Avram Iancu U–Ni–Co–Bi–As mineralization, Băița (Bihor) metallogenic district, Bihor Mts., Romania. Int J Earth Sci (Geol Rundsch) DOI 10.1007/s00531-015-1175-1.

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Published

2017-12-30

How to Cite

BICAN-BRIȘAN, N., MOLDOVAN, M. C., BURGHELE, B.-D., & DAVID, P. (2017). NATURAL RADIATION DUE TO RADON. CASE STUDY: RADON CONCENTRATION IN HOUSES FROM APUSENI MOUNTAINS. Studia Universitatis Babeș-Bolyai Ambientum, 62(2), 11–18. https://doi.org/10.24193/subbambientum.2017.2.01

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