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Application of γ spectra measurement in the research of lake sediment and palaeoenvironment

机译:γ光谱测量在湖泊沉积物与古环境研究中的应用

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Xigeda Formation layer, which is widely distributed in Panzhihua area, is researched by the method of γ spectrum measurement. Qinglongshan Xigeda Formation profile is measured by the low-background multi-channelγenergy spectrometer in Panzhihua, the change rules of radioactive elements, including URa, Th, K, Ir and Ira on the profile are analyzed in detail. The characteristics and palaeoenvironmental significance of the sediment layer on the profile is researched by combining the geological features. The results show that the contents of radioactive elements in Xigeda Formation profile reduce obviously from the old to the new layer and change regularly and the radioactive characteristics are consistent to the sediment geological features. All these show that the γ spectrum method is a good one for the study of lake sediment and palaeoenvironment.
机译:通过γ光谱测量方法研究了广泛分布的Xigeda形成层,研究了γ光谱测量方法。清香川庆龙山Xigeda形成型材是通过攀枝花的低背景多通道γenergy光谱仪测量的,详细分析了轮廓上的放射性元素的变化规则,包括URA,Th,K,IR和IRA。通过组合地质特征,研究了沉积物层对曲线上的特征和古环境意义。结果表明,XIGEA形成型材中的放射性元素内容显然从旧的层减少到新层并定期变化,放射性特性与沉积物地质特征一致。所有这些都表明,γ谱法对于湖泊沉积物和古环境研究是一个很好的方法。

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