Model for Reconstruction of gamma-Background during Liquid Atmospheric Precipitation; Mathematics; Vol. 9, iss. 14
| Parent link: | Mathematics Vol. 9, iss. 14.— 2021.— [1636, 10 p.] |
|---|---|
| Autor corporatiu: | |
| Altres autors: | , , , , |
| Sumari: | Title screen With regard to reconstructing the gamma background dose rate, existing models are either empirical with limited applicability or have many unknown input parameters, which complicates their application in practice. Due to this, there is a need to search for a new approach and build a convenient, easily applicable and universal model. The paper proposes a mathematical model for reconstructing the temporal evolution of the ambient equivalent gamma-radiation dose rate during rain episodes, depending on the density of radon flux from the soil surface, as well as the duration and intensity of rain. The efficiency of the model is confirmed by the high coefficient of determination (R2=0.81-0.99) between the measured and reconstructed ambient equivalent ose rate during periods of rain, the simulation of which was performed using Wolfram Mathematica. An algorithm was developed for restoring the dynamics of the ambient equivalent gamma-radiation dose rate during rainfall. Based on the results obtained, assumptions were made where the washout of radionuclides originates. The influence of the radionuclides ratio on the increase in the total gamma-radiation dose rate was investigated. |
| Idioma: | anglès |
| Publicat: |
2021
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| Matèries: | |
| Accés en línia: | http://earchive.tpu.ru/handle/11683/69112 https://doi.org/10.3390/math9141636 |
| Format: | MixedMaterials Electrònic Capítol de llibre |
| KOHA link: | https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=665326 |
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| 200 | 1 | |a Model for Reconstruction of gamma-Background during Liquid Atmospheric Precipitation |f V. S. Yakovleva, A. S. Zelinsky, R. I. Parovik [et al.] | |
| 203 | |a Text |c electronic | ||
| 300 | |a Title screen | ||
| 320 | |a [References: 20 tit.] | ||
| 330 | |a With regard to reconstructing the gamma background dose rate, existing models are either empirical with limited applicability or have many unknown input parameters, which complicates their application in practice. Due to this, there is a need to search for a new approach and build a convenient, easily applicable and universal model. The paper proposes a mathematical model for reconstructing the temporal evolution of the ambient equivalent gamma-radiation dose rate during rain episodes, depending on the density of radon flux from the soil surface, as well as the duration and intensity of rain. The efficiency of the model is confirmed by the high coefficient of determination (R2=0.81-0.99) between the measured and reconstructed ambient equivalent ose rate during periods of rain, the simulation of which was performed using Wolfram Mathematica. An algorithm was developed for restoring the dynamics of the ambient equivalent gamma-radiation dose rate during rainfall. Based on the results obtained, assumptions were made where the washout of radionuclides originates. The influence of the radionuclides ratio on the increase in the total gamma-radiation dose rate was investigated. | ||
| 461 | |t Mathematics | ||
| 463 | |t Vol. 9, iss. 14 |v [1636, 10 p.] |d 2021 | ||
| 610 | 1 | |a электронный ресурс | |
| 610 | 1 | |a труды учёных ТПУ | |
| 610 | 1 | |a radon decay products | |
| 610 | 1 | |a simulation | |
| 610 | 1 | |a model | |
| 610 | 1 | |a gamma background | |
| 610 | 1 | |a dose rate | |
| 610 | 1 | |a atmospheric precipitation | |
| 610 | 1 | |a rain shower | |
| 610 | 1 | |a продукты распада | |
| 610 | 1 | |a радон | |
| 610 | 1 | |a симуляции | |
| 610 | 1 | |a гамма-фон | |
| 610 | 1 | |a мощность | |
| 610 | 1 | |a дозы | |
| 610 | 1 | |a атмосферные осадки | |
| 701 | 1 | |a Yakovleva |b V. S. |c physicist |c Associate Professor of Tomsk Polytechnic University, Candidate of physical and mathematical sciences |f 1970- |g Valentina Stanislavovna |3 (RuTPU)RU\TPU\pers\31214 |9 15410 | |
| 701 | 1 | |a Zelinsky |b A. S. |g Aleksey Sergeevich | |
| 701 | 1 | |a Parovik |b R. I. |g Roman Ivanovich | |
| 701 | 1 | |a Yakovlev |b G. A. |g Grigory Alekseevich | |
| 701 | 1 | |a Kobzev |b A. A. |g Aleksey Anatoljevich | |
| 712 | 0 | 2 | |a Национальный исследовательский Томский политехнический университет |b Инженерная школа ядерных технологий |b Отделение ядерно-топливного цикла |3 (RuTPU)RU\TPU\col\23554 |
| 801 | 2 | |a RU |b 63413507 |c 20211209 |g RCR | |
| 856 | 4 | |u http://earchive.tpu.ru/handle/11683/69112 | |
| 856 | 4 | |u https://doi.org/10.3390/math9141636 | |
| 942 | |c CF | ||