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镍为基体改进剂—石墨炉原子吸收法连续测定岩石矿物中痕量铊和镓 被引量:1

CONTINUOUSLY DETERMINING TRACE TI GA IN ROCKS AND MINERALS BY USING ATOMIC ABSORPTION METHOD WITH GRAPHITE FURNACE—TAKING NI AS A MATRIX IMPROVER
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摘要 本法采用镍为基体改进剂,消除较复杂试样的基体干扰,直接用石墨炉原子吸收法测定岩石矿物中痕量铊和镓。该法简便、快速、准确。国家一级标样测定值与推荐值吻合。对于镓的测定经过100多个实际样品考查分析质量符合要求。 By taking Ni as a matrix improver, remove matrix disturbance of relatively complcated sampies and determine directly trace Ti, Ga in rocks and minerals by using atomic absorption method with graphite furnace. This method is simple, high—speed, and accurate. The determed value and recommended value reach the state standard A. Morn than one hundred samples of Ga were determed and all the analytical results accord with requirements for quality.
出处 《吉林地质》 1993年第2期66-70,共5页 Jilin Geology
关键词 连续测定 原子吸收光谱 矿物 Continuously determining Ti and Ga Speetrum of atomic absorption with the graphite furnace bench Ni matrix improver
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