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- W807731414 abstract "Radon concentrations in the natural environment in stable weather conditions have more or less diurnal periodical behaviour, with clear minima during the day and maxima during the night [7]. When boundary layer stabilizes during late afternoon, night and early morning, radon is trapped within the inversion layer and its level increases. During the day, a vertical mixing is the major process for restoring low concentrations of radon and its short-lived progeny, due to a dilution with clean air from above the mixing layer. In unstable and windy weather, the near-ground radon concentrations are quite low due to efficient mixing, and the differences between minimum and maximum daily levels are rather small. Within the area where several radon sources are present (e.g. U-mine area with tailings piles, mine ventilation shafts, etc.), an industrial radon diurnal behaviour is, in principle, the same as for natural radon, but in some meteorological conditions it might be modified. Namely, a carefully designed network of active radon monitors enabled to detect sharp and high peaks in time series of radon concentrations that were superimposed on normal periodical curves [3, 5]. These radon peaks are an indication of a sudden appearance of radon with enhanced concentration and they have never been reported in relation to the uranium mine and to radiation exposure. They are termed here as Radon events in the U-mine environment and related radiation exposure Milko J. Križman, Jože Rojc, Josef E. Peter" @default.
- W807731414 created "2016-06-24" @default.
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- W807731414 date "2010-01-01" @default.
- W807731414 modified "2023-09-28" @default.
- W807731414 title "Radon events in the U-mine environment and related radiation exposure" @default.
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