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溴化镧探测器空气吸收剂量率G(E)函数法研究

Study of the G(E) Function Method for the Air Absorbed Dose Rate of LaBr3: Ce3+ Detectors

  • 摘要: 利用溴化镧探测器测量了标准γ放射源(137Cs、60Co)的γ能谱,并使用蒙特卡罗程序Geant4对实验过程进行了理论模拟,生成了40 keV~3 MeV能量范围内γ能谱响应矩阵。采用Tikhonov正则化矩阵方法,得到了Geant4模拟γ能谱与对应吸收剂量值之间的转换关系,即能谱-剂量转换G(E)函数。基于该G(E)函数,将标准γ源137Cs,60Co和土壤源测量的实验能谱转换得到了相应空气吸收剂量率值,并与理论计算值进行了比较。结果表明,G(E)函数法得到的实验结果与理论计算值的偏差在7.2%以内,验证了该方法的准确性。

     

    Abstract: In this paper, the γ ray spectrum of the standard γ radioactive source (137Cs, 60Co) was measured by using a lanthanum bromide detector, and the experimental process was theoretically simulated by using the Monte Carlo program Geant4, and the response matrix of the γ ray spectrum in the energy range of 40 keV~3 MeV was generated. Using the Tikhonov regularization matrix method, the conversion relationship between the Geant4 simulated γ ray spectrum and the corresponding absorbed dose value is obtained, that is, the energy spectrum-dose conversion G(E) function. Based on the G(E) function, the corresponding air absorbed dose rate values were obtained by converting the experimental energy spectrum of the standard γ source 137Cs, 60Co and soil source measurements, and compared with the theoretical calculated values. The results show that the experimental results obtained by the G(E) function method are in good agreement with the theoretical calculated values, and the deviation is within 7.2%, which verifies the accuracy of the method.

     

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