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γ能谱法测量铀矿石样品镭-氡平衡系数的初步探索
引用本文:佘冠军,刘宏章,尹旺明,汤彬.γ能谱法测量铀矿石样品镭-氡平衡系数的初步探索[J].国外铀金地质,2009(4):237-240.
作者姓名:佘冠军  刘宏章  尹旺明  汤彬
作者单位:东华理工大学,江西抚州344000
基金项目:[基金项目]国家高技术研究发展计划(863计划)项目(2007AA062111)资助.
摘    要:以测定铀矿石镭-氡平衡系数为目的,提出了对铀矿石样本进行γ能谱测量,根据铀系的衰变平衡规律,利用γ能谱中的特征峰计数计算镭、氡含量。推导了镭-氡平衡系数的计算公式,重点对相关参数进行了探讨。该方法简单、快速,进一步完善后可应用于钻孔岩心样本的现场分析。

关 键 词:镭-氡平衡系数  γ能谱  γ特征峰  质量

Preliminary study on determining radium-radon equilibrium coefficient of uranium ore sample by γ-ray spectroscopy
Authors:SHE Guan-jun  LIU Hong-zhang  YIN Wang-ming  TANG Bin
Institution:(East China Institute of Technology, Fuzhou, Jiangxi 344000, China)
Abstract:In order to determine the equilibrium coefficient of uranium ore sample, this article proposes a method by measuring γ-ray spectroscopy. According to the γ-ray decay and equilibrium law of uranium series, the content of radium and radon is calculated by the count of characteristic peaks in the γ-ray spectroscopy. Calculation formula is deduced for radium-radon equilibrium coefficient and the related parameters are discussed in detail. This method is simple and rapid, and can be used in on-site analysis of drilling core samples after further improved.
Keywords:radium-radon equilibrium coefficient  γ-ray spectroscopy  γ-ray characteristic peak  mass
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