氢化物发生-原子荧光光谱法测定岩石中砷和锑
HG-AFS Determination of Arsenic and Antimony in Rocks
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摘要: 应用氢化物发生-原子荧光光谱法测定了岩石中砷和锑的含量。样品预先粉碎至通过孔径为0.25~0.42 mm的细筛,称取此粉碎的样品0.100 0~0.300 0 g,先于盐酸-硝酸(3+1)混合酸8 mL中浸泡30 min,然后放入沸水浴中消解2 h,将溶液及不溶物一起移入50 mL容量瓶中,加水定容。移取上清液5.00 mL置于10 mL容量瓶中,加入100 g·L-1硫脲及抗坏血酸混合溶液2.5 mL,用盐酸(5+95)溶液定容,分取此溶液1.0 mL进样按选定的仪器条件进行分析。用20 g·L-1硼氢化钾溶液作为产生砷及锑的氢化物的还原剂,砷(Ⅲ)及锑(Ⅲ)的质量浓度依次在0.50~60 μg·L-1和0.50~80 μg·L-1范围内与其相应的荧光强度呈线性关系。应用此方法测定了两种岩石标准物质(GBW 07106及GBW 07108)中的砷及锑量,其测定值与认定值一致,相对标准偏差(n=5)均小于3.5%。Abstract: AFS with hydride generation was applied to the determination of arsenic and antimony in rocks. Rock sample was crushed to pass sieves with bores of 0.25 mm to 0.42 mm. 0.100 0 to 0.300 0 g of the crushed sample were soaked in 8 mL of an acid mixture of conc. HCl and HNO3 (3+1) for 30 min and then digested in boiling water bath for 2 h. The mixture was transferred to a 50 mL volumetric flask and diluted to mark with water. 5.00 mL of the supernatant were taken and transferred to a 10 mL volumetric flask, 2.5 mL of 100 g·L-1 thiourea-ascorbic acid solution were added and the solution was diluted to 10 mL with HCl (5+95). An aliquot of 1.0 mL was taken for the analysis under prescribed instrumental conditions. 20 g·L-1 KBH4 solution was used as reductant to generate the hydrides of arsenic and antimony. Linear relationships between values of fluorescence intensity and concentrations of As and Sb were obtained in the ranges of 0.50-60 μg·L-1 and 0.50-80 μg·L-1 respectively. The proposed method was used in the analysis of 2 rock CRM′s (GBW 07106 and GBW 07108), contents of As and Sb found were in consistency with the certified values, and values of RSD′s (n=5) found were less than 3.5%.