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Relation of gamma dose rate with the intensity of rain showers A. S. Zelinskiy, G. A. Yakovlev, D. E. Fil’trov

By: Zelinskiy, Aleksey SContributor(s): Yakovlev, Grigorii A | Filtrov, D. EMaterial type: ArticleArticleContent type: Текст Media type: электронный Other title: Связь мощности дозы гамма-излучения с интенсивностью ливневых осадков [Parallel title]Subject(s): гамма-излучение | гамма-фон | продукты распада радона | атмосфера | математические моделиGenre/Form: статьи в журналах Online resources: Click here to access online In: Вестник КРАУНЦ. Физико-математические науки Т. 36, № 3. С. 189-199Abstract: Experimental and theoretical studies of the influence of the intensity, amount and duration of liquid atmospheric precipitation on the formation of γ-background in the surface layer of the atmosphere are presented. It was observed that precipitation causes an increase in the γ-radiation dose rate in the form of bursts. In this case, the total amount of precipitation in an event determines the magnitude of the burst of the dose rate, and the intensity of precipitation determines the rate of increase in the dose rate of γ-radiation. A mathematical model, which establishes a quantitative relationship between the dose rate of γ-radiation and the intensity (amount) of liquid atmospheric precipitation has been developed and verified (R2 = 0.93).
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Experimental and theoretical studies of the influence of the intensity, amount and duration of liquid atmospheric precipitation on the formation of γ-background in the surface layer of the atmosphere are presented. It was observed that precipitation causes an increase in the γ-radiation dose rate in the form of bursts. In this case, the total amount of precipitation in an event determines the magnitude of the burst of the dose rate, and the intensity of precipitation determines the rate of increase in the dose rate of γ-radiation. A mathematical model, which establishes a quantitative relationship between the dose rate of γ-radiation and the intensity (amount) of liquid atmospheric precipitation has been developed and verified (R2 = 0.93).

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