Radon decay products and 10–1100 nm aerosol particles in Postojna Cave

At the lowest point along the tourist route in Postojna Cave, the activity concentration of radon (<sup>222</sup>Rn) decay products and the number concentration and size distribution of aerosol particles in the size range of 10–1100 nm were monitored, with the focus on the unattached fra...

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Main Authors: M. Bezek, A. Gregorič, J. Vaupotič
Format: Article
Language:English
Published: Copernicus Publications 2013-03-01
Series:Natural Hazards and Earth System Sciences
Online Access:http://www.nat-hazards-earth-syst-sci.net/13/823/2013/nhess-13-823-2013.pdf
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spelling doaj-a236cdaf12ed46cb99ae424e8b5072ff2020-11-24T21:06:40ZengCopernicus PublicationsNatural Hazards and Earth System Sciences1561-86331684-99812013-03-0113382383110.5194/nhess-13-823-2013Radon decay products and 10&ndash;1100 nm aerosol particles in Postojna CaveM. BezekA. GregoričJ. VaupotičAt the lowest point along the tourist route in Postojna Cave, the activity concentration of radon (<sup>222</sup>Rn) decay products and the number concentration and size distribution of aerosol particles in the size range of 10–1100 nm were monitored, with the focus on the unattached fraction (<i>f</i><sup>un</sup>) of radon decay products (RnDPs), a key parameter in radon dosimetry. The total number concentration of aerosols during visits in summer was lower (700 cm<sup>−3</sup>) than in winter (2800 cm<sup>−3</sup>), and was dominated by <50 nm particles (related to unattached RnDPs) in summer and by >50 nm particles (related to the attached RnDPs) in winter. This explains the higher <i>f</i><sup>un</sup> values in summer (0.75) and the lower winter measurement (0.04) and, consequently, DCF<sub>D</sub> values of 43.6 and 13.1 mSv WLM<sup>−1</sup> respectively for the calculated dose conversion factors. The difference is caused by an enhanced inflow of fresh outside air, driven in winter by the higher air temperature in the cave compared to outside, resulting in the introduction of outside aerosol particles into the cave.http://www.nat-hazards-earth-syst-sci.net/13/823/2013/nhess-13-823-2013.pdf
collection DOAJ
language English
format Article
sources DOAJ
author M. Bezek
A. Gregorič
J. Vaupotič
spellingShingle M. Bezek
A. Gregorič
J. Vaupotič
Radon decay products and 10&ndash;1100 nm aerosol particles in Postojna Cave
Natural Hazards and Earth System Sciences
author_facet M. Bezek
A. Gregorič
J. Vaupotič
author_sort M. Bezek
title Radon decay products and 10&ndash;1100 nm aerosol particles in Postojna Cave
title_short Radon decay products and 10&ndash;1100 nm aerosol particles in Postojna Cave
title_full Radon decay products and 10&ndash;1100 nm aerosol particles in Postojna Cave
title_fullStr Radon decay products and 10&ndash;1100 nm aerosol particles in Postojna Cave
title_full_unstemmed Radon decay products and 10&ndash;1100 nm aerosol particles in Postojna Cave
title_sort radon decay products and 10&ndash;1100 nm aerosol particles in postojna cave
publisher Copernicus Publications
series Natural Hazards and Earth System Sciences
issn 1561-8633
1684-9981
publishDate 2013-03-01
description At the lowest point along the tourist route in Postojna Cave, the activity concentration of radon (<sup>222</sup>Rn) decay products and the number concentration and size distribution of aerosol particles in the size range of 10–1100 nm were monitored, with the focus on the unattached fraction (<i>f</i><sup>un</sup>) of radon decay products (RnDPs), a key parameter in radon dosimetry. The total number concentration of aerosols during visits in summer was lower (700 cm<sup>−3</sup>) than in winter (2800 cm<sup>−3</sup>), and was dominated by <50 nm particles (related to unattached RnDPs) in summer and by >50 nm particles (related to the attached RnDPs) in winter. This explains the higher <i>f</i><sup>un</sup> values in summer (0.75) and the lower winter measurement (0.04) and, consequently, DCF<sub>D</sub> values of 43.6 and 13.1 mSv WLM<sup>−1</sup> respectively for the calculated dose conversion factors. The difference is caused by an enhanced inflow of fresh outside air, driven in winter by the higher air temperature in the cave compared to outside, resulting in the introduction of outside aerosol particles into the cave.
url http://www.nat-hazards-earth-syst-sci.net/13/823/2013/nhess-13-823-2013.pdf
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