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连续流动氢化物发生—原子吸收光谱法测定地质样品中痕量硒 被引量:14

Determination of Selenium in Geological Samples by Continuous flow Hydride Generation Atomic Absorption Spectrometry
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摘要 经试验研究,选定了分析地质样品中痕量硒的测定体系,建立了切实可行的分析方法,该方法不需分离,直接测定,灵敏度高,干扰少,方法测定下限可达0.02μg/g,进行了部分标样分析,结果令人满意。 After detailed study ,an optimum system for the determination of selenium in geological samples was developed and a reliable analytical method was established.No separation was needed and the method was highly sensitive with few interferences.The determining limit of the method was 0.02μg/g.Some standard reference materials were analysed and satisfactory results were obtained.
出处 《分析试验室》 CAS CSCD 1997年第2期51-54,共4页 Chinese Journal of Analysis Laboratory
关键词 氢化物发生 原子吸收光谱法 地质样品 Hydride generation atomic absorption spectrometry geological samples selenium determination
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