Abstract
The article describes a model and method for calculating beta-exposure doses to secretory and basal cells of the tracheobronchial part of the respiratory tract when a point source of 1 Bq activity moves along the inner surface of respiratory formations. The calculations, that used for proposed model, were performed by using a 90Y point source as an example. The dose calculation model takes into account the speed o f movement of the radiation source in each respiratory formation, the size of the respiratory formations, and the depth of the secretory and basal cells. The dose calculation is based on the dose rate attenuation functions published by W. G. Cross et al. (DOI: 10.1097/00004032-199208000-00002). The calculations were performed for a cylindrical model of a respiratory formation. Two kinds of cells were considered for the dose estimation: cells irradiated without beta-particle exit into bronchial lumen (type 1 cells) and cells irradiated due to beta-particle exit into bronchial lumen (type 2 cells). The results of calculations showed, that as far as the generation number increasing, the average irradiation doses of the type 1 cells are 10 or more times greater than those of the type 2 cells. With increasing generation number in the tracheobronchial tree, doses per cells increase by several orders of magnitude. The highest doses are formed in bronchioles of generations 9-15, reaching units and tens of mGy. In spite of the fact that the number of generation increases, the total number of irradiated cells decreases, the collective doses of irradiated cells (sum of doses to all cells of the respiratory formation) in the last generations are 30-50 times higher than the doses of the first generations. Thus, in case of a single point source, there is a significant (by many orders of magnitude) scatter of doses to individual cells in individual respiratory formation, as well as significant differences in average doses of trachea, individual bronchi and bronchioles.
Highlights
В результате аварии на 4 энергоблоке Чернобыльской АЭС в окружающую среду было выброшено большое ко личество радионуклидов, приведшее к интенсивному ра диоактивному загрязнению территории вокруг атомной станции [1,2,3,4,5,6,7,8,9,10]
The radio logical significance o f beta emiting hot partucles released from Chernobyl nuclear power plant / / Radiation Protection Dosimetry. 1988
Analysis of Chernobyl fuel Particles and their migration Characteristics in Water and Soil / / Seminar on Comparative Assessment of Environmental Impact o f Radionuclides Released during Three Major Nuclear Accidents: Kyshtym, Windscale, Chernobyl: Luxemburg, 1-5 October 1990
Summary
Report of a Consultation 6 May 1986 (provisional). World Health Organization. 3. Information on the Chernobyl accident and its consequences, prepared for the IAEA. 4. Izrael YuA, Petrov VN, Severov DA. Effect o f Meteorogical Conditions and Release Compositions on Radionuclide Deposition After Chernobyl Accident. Hot particles from Chernobyl fallout: Proceeding of an international workshop, Theuern, 28-29 Oct. 1987. Seminar on Comparative Assessment of Environmental Impact o f Radionuclides Released during Three Major Nuclear Accidents: Kyshtym, Windscale, Chernobyl: Luxemburg, 1-5 October 1990. Study of Hot Particles co l lected in Sweden one year after Chernobyl Accident. Prevalence of hot par ticles on the territory o f USSR after Chernobyl accident. Human Respiratory Tract Model for Radiological Protection.
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