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- W2554732336 abstract "In a continuous monitoring of the natural radioactive background held in Tien-Shan mountains at a height of 3340 m above the sea level, and in Almaty city at 850 m a.s.l. with inorganic NaI scintillation gamma-detectors it was found, that after beginning of a precipitation period the intensity of scintillation signals in the range of gamma-radiation energies Eγ ≥ 30 keV starts to grow, its maximum (up to 20 − 40% above the usual background level) being achieved 30 − 40 minutes later. Such behavior of scintillation signals is characteristic for a large bulk of observed events, and repeats regularly each time by precipitations. After the maximum (though precipitations may be continuing) the counting rates of gamma-radiation for the rain water, hail, or melted snow exponentially return to their initial level with one and the same lifetime duration, typically about 30 − 50 minutes, which is an evidence about the common radioactivity nature of different precipitation species. Comparison of relative magnitude of the precipitation-caused gamma-intensity enhancements observed at different elevation heights, so as the revealed difference in gamma-radioactivity detected for collected rain water and melted hail gives an evidence that the source of additional radioactivity is connected with the region of precipitation formation, i.e. with the upper, but not with near-earth, atmosphere." @default.
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- W2554732336 date "2011-01-01" @default.
- W2554732336 modified "2023-09-24" @default.
- W2554732336 title "An increase of the soft gamma-radiation background by precipitations" @default.
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