石墨炉原子吸收测定岩石样品中超痕量铂  

Determination of Ultra-trace Platinum in Rock Samples by GF-AAS Method

作　　者：孙爱琴[1] 姚文生[1] 王烨[2] 陈静[2] 钟莅湘[2] 李艳华[2] 王玉林[3] 

机构地区：[1]河南省地质调查院,河南郑州450007 [2]河南省岩石矿物测试中心,河南郑州450012 [3]河南省地矿局第三地质调查队,河南信阳464000

出　　处：《贵金属》2006年第3期40-44,共5页Precious Metals

基　　金：中国地质科学院基金资助项目(KL05-24)。

摘　　要：样品分解后,用超低灰分活性炭吸附φ为5%～15%HCl溶液中的Pt,活性炭灰化,灰分用王水溶解后,在10%HCl溶液中用GF-AAS方法测定岩石样品中超痕量铂。作者研究了测定酸度、介质及石墨炉灰化温度、原子化温度等因素对吸光度的影响。在选定条件下测定方法的检出限达到0.1×10-9,精密度(SD,n=12)5%～9%,经国家一级标准物质分析验证,结果吻合。After the rock sample was dissolved, the solution was adjusted to the volume fraction of 5%～10% HCl and the Pt in the solution was adsorbed by active carbon. The active carbon was ashed and the ash was re-dissolved by pure aqua regia, and Pt was determinated by GF-AAS using pyrolytically coated electrographite cuvettes produced by Thermo Elemental Corporation. The determination conditions, such as acidity, media and the GF-AAS ashing temperature and graphite furnace atomizing temperature and their effects on the determination were investigated in detail. The detection limit of the method is 0.11×10^-9 for Pt with RSD of 5%～9% for 12 times determination. And the method was used to determine national standard substances with coincidence results.

关 键 词：分析化学 石墨炉原子吸收 岩石样品 超痕量铂 涂层石墨管 

分 类 号：O614.123[理学—无机化学] O657.63[理学—化学]