Investigation of seasonal dynamics of [beta]- and [gamma]-radiation Helds vertical profile in the surface atmospheric layer; IOP Conference Series: Materials Science and Engineering; Vol. 135 : Issues of Physics and Technology in Science, Industry and Medicine

Detalles Bibliográficos
Parent link:IOP Conference Series: Materials Science and Engineering
Vol. 135 : Issues of Physics and Technology in Science, Industry and Medicine.— 2016.— [012036, 6 p.]
Autor Corporativo: Национальный исследовательский Томский политехнический университет (ТПУ) Физико-технический институт (ФТИ) Кафедра прикладной физики (№ 12) (ПФ)
Outros autores: Ryabkina K. S., Kondrateva (Kondratieva) A. G. Alla Georgievna, Nagorskiy P. M., Yakovleva V. S. Valentina Stanislavovna
Summary:Title screen
This paper is devoted to the seasonal dynamics of [beta]- and [gamma]-radiation field vertical profile in the surface atmospheric layer study. The findings revealed the following: a) significant seasonal variation in vertical distribution characteristics fields [beta]- and [gamma]-radiation; b) reduced [beta]-radiation flux density and [gamma]-radiation dose with increasing height is maintained in the range of spring and fall, namely, starting with snow melt and finishing its setting; c) distortion vertical profile in the winter season, an inverse relationship [beta]-flux density and dose rate of [gamma]-radiation from the heights above the earth's surface was registered.
Idioma:inglés
Publicado: 2016
Subjects:
Acceso en liña:http://dx.doi.org/10.1088/1757-899X/135/1/012036
http://earchive.tpu.ru/handle/11683/34825
Formato: Electrónico Capítulo de libro
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=650314

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330 |a This paper is devoted to the seasonal dynamics of [beta]- and [gamma]-radiation field vertical profile in the surface atmospheric layer study. The findings revealed the following: a) significant seasonal variation in vertical distribution characteristics fields [beta]- and [gamma]-radiation; b) reduced [beta]-radiation flux density and [gamma]-radiation dose with increasing height is maintained in the range of spring and fall, namely, starting with snow melt and finishing its setting; c) distortion vertical profile in the winter season, an inverse relationship [beta]-flux density and dose rate of [gamma]-radiation from the heights above the earth's surface was registered. 
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