Impact of radon and thoron levels on technosphere objects in the total urban environment / Mac-Donald Prince, B. Adams, S. V. Smirnov, K. Abdullina ; sci. adv. V. S. Yakovleva
Уровень набора: (RuTPU)RU\TPU\conf\34751, Научная инициатива иностранных студентов и аспирантов, сборник докладовI Международной научно-практической конференции, Томск, 27-29 апреля 2021 г., в 2 т. / Национальный исследовательский Томский политехнический университет, Школа базовой инженерной подготовки = 2021Язык: английский.Страна: Россия.Серия: Science as a vocation and careerРезюме или реферат: Thoron and radon exhalation from earth's crust is the most important source of atmospheric radioactive gases, along with its daughter products present in the soil is one of the major contributors to the external gamma dose in the atmosphere, since its distribution in the earth's crust is important for controlling the production of 220Rn and 222Rn. In this study trace amount of 232Th, 238U permeate almost all soils and rocks, in part due to the influence of buildings from which radioactive gas can emanate over geological time scales. Results obtained from this study indicate that the region has background radioactivity levels within the natural limits and a detailed discussion of the results is presented in the work..Примечания о наличии в документе библиографии/указателя: [Библиогр.: с. 410 (4 назв.)].Тематика: труды учёных ТПУ | электронный ресурс | радон | торон | техносфера | городская среда | радиоактивные газы | радиоактивность Ресурсы он-лайн:Щелкните здесь для доступа в онлайнЗаглавие с титульного экрана
[Библиогр.: с. 410 (4 назв.)]
Thoron and radon exhalation from earth's crust is the most important source of atmospheric radioactive gases, along with its daughter products present in the soil is one of the major contributors to the external gamma dose in the atmosphere, since its distribution in the earth's crust is important for controlling the production of 220Rn and 222Rn. In this study trace amount of 232Th, 238U permeate almost all soils and rocks, in part due to the influence of buildings from which radioactive gas can emanate over geological time scales. Results obtained from this study indicate that the region has background radioactivity levels within the natural limits and a detailed discussion of the results is presented in the work.
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