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A mathematical description of the diurnal variation of radon progeny
The variation of the alpha ( α) radioactivity in the air near the ground and the ground-level total gamma ( γ) radiation has been monitored in North-eastern Greece over several days. Meteorological information regarding the temperature of the air and humidity has been simultaneously recorded. The α-...
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Published in: | Applied radiation and isotopes 2008, Vol.66 (1), p.75-79 |
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Main Authors: | , , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
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Summary: | The variation of the alpha (
α) radioactivity in the air near the ground and the ground-level total gamma (
γ) radiation has been monitored in North-eastern Greece over several days. Meteorological information regarding the temperature of the air and humidity has been simultaneously recorded. The
α-radioactivity shows a periodic diurnal variation with a peak in the morning followed by a decrease in the afternoon; then, the variation rises again to the peak the next morning. The variation of the ground
γ-radiation follows that of the air
α-radioactivity. Furthermore, their significant dependence on the air temperature and humidity is confirmed, rising with an increase in humidity and a decrease in temperature. Hence, a mathematical function has been developed to describe the diurnal variation of the
α-radioactivity in terms of the ground-level
γ-radiation and the meteorological variables of temperature and humidity. |
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ISSN: | 0969-8043 1872-9800 |
DOI: | 10.1016/j.apradiso.2007.07.006 |