| 000 | 03343nlm1a2200541 4500 | ||
|---|---|---|---|
| 001 | 665326 | ||
| 005 | 20231030041959.0 | ||
| 035 | _a(RuTPU)RU\TPU\network\36525 | ||
| 035 | _aRU\TPU\network\36410 | ||
| 090 | _a665326 | ||
| 100 | _a20210913a2021 k y0engy50 ba | ||
| 101 | 0 | _aeng | |
| 135 | _adrgn ---uucaa | ||
| 181 | 0 | _ai | |
| 182 | 0 | _ab | |
| 200 | 1 |
_aModel for Reconstruction of gamma-Background during Liquid Atmospheric Precipitation _fV. S. Yakovleva, A. S. Zelinsky, R. I. Parovik [et al.] |
|
| 203 |
_aText _celectronic |
||
| 300 | _aTitle screen | ||
| 320 | _a[References: 20 tit.] | ||
| 330 | _aWith 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 | _tMathematics | ||
| 463 |
_tVol. 9, iss. 14 _v[1636, 10 p.] _d2021 |
||
| 610 | 1 | _aэлектронный ресурс | |
| 610 | 1 | _aтруды учёных ТПУ | |
| 610 | 1 | _aradon decay products | |
| 610 | 1 | _asimulation | |
| 610 | 1 | _amodel | |
| 610 | 1 | _agamma background | |
| 610 | 1 | _adose rate | |
| 610 | 1 | _aatmospheric precipitation | |
| 610 | 1 | _arain shower | |
| 610 | 1 | _aпродукты распада | |
| 610 | 1 | _aрадон | |
| 610 | 1 | _aсимуляции | |
| 610 | 1 | _aгамма-фон | |
| 610 | 1 | _aмощность | |
| 610 | 1 | _aдозы | |
| 610 | 1 | _aатмосферные осадки | |
| 701 | 1 |
_aYakovleva _bV. S. _cphysicist _cAssociate Professor of Tomsk Polytechnic University, Candidate of physical and mathematical sciences _f1970- _gValentina Stanislavovna _2stltpush _3(RuTPU)RU\TPU\pers\31214 |
|
| 701 | 1 |
_aZelinsky _bA. S. _gAleksey Sergeevich |
|
| 701 | 1 |
_aParovik _bR. I. _gRoman Ivanovich |
|
| 701 | 1 |
_aYakovlev _bG. A. _gGrigory Alekseevich |
|
| 701 | 1 |
_aKobzev _bA. A. _gAleksey Anatoljevich |
|
| 712 | 0 | 2 |
_aНациональный исследовательский Томский политехнический университет _bИнженерная школа ядерных технологий _bОтделение ядерно-топливного цикла _h7864 _2stltpush _3(RuTPU)RU\TPU\col\23554 |
| 801 | 2 |
_aRU _b63413507 _c20211209 _gRCR |
|
| 856 | 4 | _uhttp://earchive.tpu.ru/handle/11683/69112 | |
| 856 | 4 | _uhttps://doi.org/10.3390/math9141636 | |
| 942 | _cCF | ||