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陈耀惠, 韩绍荣. 火焰原子吸收法测定岩石中痕量钡[J]. 岩矿测试, 1990, (3): 201-203.
引用本文: 陈耀惠, 韩绍荣. 火焰原子吸收法测定岩石中痕量钡[J]. 岩矿测试, 1990, (3): 201-203.
Determination of Trace Barium in Rocks by Flame AAS[J]. Rock and Mineral Analysis, 1990, (3): 201-203.
Citation: Determination of Trace Barium in Rocks by Flame AAS[J]. Rock and Mineral Analysis, 1990, (3): 201-203.

火焰原子吸收法测定岩石中痕量钡

Determination of Trace Barium in Rocks by Flame AAS

  • 摘要: 本文在pH为6.0的HAc-NaAc缓冲溶液中,以Pb为共沉淀剂用K_2CrO_4使Ba成BaCrO_4沉淀进行富集,再应用N_2O-C_2H_2火焰原子吸收光谱法测定Ba。方法的特征浓度为0.18μg/ml/1%吸收,标准加入回收率为96—102%。对于含Ba 3.86PPm的岩石样品进行10次测定,其相对标准偏差为0.96%。测定了GSD水系沉积物标样中的Ba,结果与推荐值吻合。

     

    Abstract: Barium is preconcentrated and separated by coprecipitation with lead as chromate in sodium acetate buffer(pH 6)and determined by AAS in a nitrous oxide-acetylene flame. The interference of aluminum can be eliminated by adding salicylic acid as spectrochem

     

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