Abstract
The Monte Carlo method is used to calculate the coefficients used to convert from the measured (using retrospective luminescence dosimetry) γ-ray dose inside the wall of a building to the dose in air. The γ-ray dose distributions in the wall and in air were calculated simultaneously. The calculations were performed for a γ-ray sources located in air, on the surface of soil, and in a 0–5 cm thick top layer of soil. The γ-ray spectra in air and inside a wall are calculated and it is shown that the spectrum depends strongly on the type of source – the average energy of the spectrum is 0.25 MeV for a source located on a soil surface, 0.39 MeV for a source located inside the soil, and 0.53 MeV for a source located in air.
Similar content being viewed by others
REFERENCES
H. Goksu and P. Schwenk, “Thermoluminescence dating of terrazzo from monastery church of Tegernsee (Bavaria, Germany) using 210°C TL peak of quartz,” Rad.-Environ. Biophys., 39, 301–308 (2000).
T. Maruyama, Yo. Kumamoto, and Yu. Noda, “Reassessment of gamma-ray doses in Hiroshima and Nagasaki,” Rad. Res., 113, 1–14 (1988).
M. Hoshi, Sh. Sawada, Yo. Ichikawa, et al., “Thermoluminescence dosimetry of γ-rays from the Hiroshima atomic bomb at distances 1.91–2.05 km from the hypocenter,” Health Phys., 57, No.6, 1003–1008 (1989).
E. Haskel, I. Bailiff, G. Kenner, et al., “Thermoluminescence measurements of gamma-ray doses attributable to fallout from the Nevada test site using building bricks as natural dosimeters,” ibid., 66, No.4, 380–391 (1994).
J. Takada, M. Hoshi, Tsu. Nagamoto, et al., “External doses of residents near the Semipalatinsk nuclear test site,” J. Rad. Res., 40, 337–344 (1999).
N. G. Bugrov, H. Goksu, E. Haskell, et al., “Issues in the reconstruction of environmental doses on the basis of thermoluminescence measurements in the Techa riverside,” Health Phys., 75, No.6, 574–583 (1998).
Yo. Ichikawa, Tsu. Nagamoto, M. Hoshi, and S. Kondo, “Thermoluminescence dosimetry of γ-rays from the Hiroshima atomic bomb at distances 1.27–1.46 km from the hypocenter,” ibid., 52, No.4, 443–451 (1987).
H. Goksu, “Luminescence methods in restrospective dosimetry using porcelain,” in: Proceedings of the 2nd Hiroshima International Symposium “Effects of Low-Level Radiation for Residents Near the Semipalatinsk Nuclear Test Site,” RIRBM, Hiroshima (1996), pp. 251–260.
I. Bailiff, “Aspects of retrospective dosimetry using luminescence techniques in areas contaminated by Chernobyl fallout,” ibid., pp. 237–249.
Dose Reconstruction for Populations in Areas Contaminated by Chernobyl Fallout, IC15-CT96-0315 Final Report to the European Commission, Durham, UK: Environmental Research Center, University of Durham (2001).
L. R. Kimel' and V. P. Mashkovich, Handbook of Protection from Ionizing Radiation, Atomizdat, Moscow (1966).
T. Ishii, T. Secine, and K. Ono, “A Monte-Carlo calculation of gamma-ray scattering on the JEIDAC computer,” in: Codes for Reactors Computations, IAEA, Vienna (1961), pp. 53–66.
S. M. Ermakov, Monte Carlo Method and Related Questions, Nauka, Moscow (1971).
N. G. Gusev and V. A. Belyaev, Handbook of Radioactive Emissions in the Biosphere, Énergoatomizdat, Moscow (1991).
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Orlov, M.Y., Stepanenko, V.F., Kolyzhenkov, T.V. et al. Monte-Carlo Calculation of the γ-Ray Dose Distribution Inside a Wall of a Building and in Air. Atomic Energy 94, 428–433 (2003). https://doi.org/10.1023/A:1025573331981
Issue Date:
DOI: https://doi.org/10.1023/A:1025573331981