HE Jun, YANG Chaowen. Measurement of γ absorption dose rate through measuring the full energy peak of γ spectrum[J]. Nuclear techniques, 2014, 37(7): 070403
HE Jun, YANG Chaowen. Measurement of γ absorption dose rate through measuring the full energy peak of γ spectrum[J]. Nuclear techniques, 2014, 37(7): 070403 DOI: 10.11889/j.0253-3219.2014.hjs.37.070403.
提出了通过γ能谱全能峰测量吸收剂量的方法,定义了全能峰角响应函数。采用蒙特卡罗方法计算了50 mm×50 mm NaI(Tl)探测器的平均角响应随射线能量的变化,用标准点源137Cs、60Co、152Eu、133Ba和参考辐射场137Cs、60Co、226Ra、241Am进行了实验验证。结果证明,在近似各向同性的条件下,对标准点源的测量结果与理论值相比误差小于2%,对参考辐射场的测量结果与电离室测量结果相差小于3%。该方法适合低能到高能的较宽能谱段剂量率测量,不仅能测出某种核素对总剂量率的贡献,且能同时分辨核素种类,无需实验刻度。
Abstract
Background: At present most radiation dose meters have the serious problem of energy response
and they just use the count rate plus relative correction method to measure the dose rate. This method has large error
and cannot distinguish the type of radionuclide
also cannot obtain the contribution of each radionuclide to the dose rate. Purpose: The research of new method is to measure the dose rate and improve the accuracy of measurement. Methods: The method of γ dose rate measurement through measuring full energy peak of γ spectrum was put forward
the angular response function of parallel γ ray injected into detector was defined. The average angular response over full space in the energy range from 0.02 MeV to 3 MeV was calculated by Monte Carlo simulation for ?50mm×50mm NaI(Tl) detector. Measurement tests have been done using standard radioactive sources of 137Cs
60Co
152Eu
133Ba and in reference radioactive field of 137Cs
60Co
226Ra
241Am in a national lab. Results: The test errors are smaller than 2% compared with the theoretical value for standard sources
and smaller than 3% compared with the value of PTW 10 L spherical chamber for reference radiation field. Conclusion: The results show that the method is suitable for the dose rate measurement for a wide range of energy without experimental calibration
can calculate the dose rate of different energy ray
and at the same time identify the radioactive nuclides in the radiation source. Abstract