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    碘化铵挥发与分离制样技术在原子荧光光谱法测定地质样品中痕量锗、锡、锑的运用

    Application of Volatilization of Iodides of Ge, Sn and Sb by NH4I as Techniques of Sample Pretreatment and Separation to AFS Determination of the 3 Elements in Geological Samples

    • 摘要: 提出利用锗、锡、锑与磺化铵熔化形成挥发性碘化物的特性行为原子荧光光谱法测定地质样品中上述3种元素含量时的样品前处理和分离方法。试验表明:当将适量样品(0.5 g)与碘化铵(1 g)置于双球玻璃管中混匀,用喷灯直接加热至350 ℃以上,并保持10 min后,试样中的锗、锡及锑将分别形成四碘化锗、四碘化锡及三碘化锑挥发逸出并凝聚于玻璃管壁,从而达到此3种元素与基体的分离。用盐酸将管壁上的凝聚物洗入烧杯中,再先后用硝酸蒸发除碘和用盐酸及过氧化氢溶解残渣制成溶液后即可进行原子荧光光谱测定。上述3种元素的检出限(3s/k)分别为0.08,0.06,0.08 μg·L-1。

       

      Abstract: Based on the fusion of Ge, Sn and Sb with NH4I to form volatile iodides, it was proposed to apply this phenomenon as techniques of sample pretreatment and separation to determination of the 3 elements in geological samples by AFS. It was shown that when the sample (0.5 g) was mixed and fused with NH4I (1 g) in a bi-bulb glass tube at 350 ℃ for 10 min, iodides of the 3 elements were formed, volatilized and condensed on the inner wall of glass tube. Hence, Ge, Sn and Sb were separated from the sample matrix. The condensate was dissolved with HCl into a beaker, and the solution was evaporated to dryness with HNO3 to expel iodine. The residue was dissolved with HCl and H2O2 and the solution was used for AFS determinations. Detection limits (3s/k) found for the 3 elements were 0.08, 0.06, 0.08 μg·L-1 respectively.

       

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