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过氧化钠碱熔-电感耦合等离子体质谱法测定地质样品中锆铌铪钽锂铍钒磷铀锰
引用本文:孙孟华,李晓敬,王文娟,王昕,于聪灵.过氧化钠碱熔-电感耦合等离子体质谱法测定地质样品中锆铌铪钽锂铍钒磷铀锰[J].冶金分析,2022,42(1):78-84.
作者姓名:孙孟华  李晓敬  王文娟  王昕  于聪灵
作者单位:1.河北省地质实验测试中心,河北保定 071051; 2.河北省矿产资源与生态环境监测重点实验室,河北保定 071051
基金项目:河北省地矿局科技发展项目(201829)
摘    要:地质样品中Zr、Nb、Hf、Ta、Li、Be、V、P、U、Mn的准确测定有利于地球化学、岩石成因等地质环境的研究。采用过氧化钠碱熔、盐酸酸化的方法处理样品,选择6Li校正Li、Be,103Rh校正V、P、Zr、Nb、Mn,185Re校正Ta、Hf、U,建立了电感耦合等离子体质谱法(ICP-MS)测定地质样品中这些元素的方法。熔样试验表明,对于0.100 0 g地质样品,以1.0 g 过氧化钠为熔剂于750 ℃马弗炉中熔融8 min,样品可熔解完全。基体干扰试验表明:将溶液稀释10倍,待测液中Na+的质量浓度小于1.0 mg/mL,其产生的干扰可忽略;样品中主量元素K、Ca、Fe、Mg、Al对测定的干扰可忽略。对待测溶液的放置时间进行了优化,选择放置时间为1 d以内。在优化的实验条件下,所测10种元素校准曲线的线性相关系数均在0.999以上,检出限为0.10~2.64 μg/g,定量限为0.33~8.80 μg/g。按照实验方法对土壤、水系沉积物和岩石的标准物质及实际样品中的Zr、Nb、Hf、Ta、Li、Be、V、P、U、Mn进行测定。结果表明,标准物质的测定结果与认定值基本一致,相对标准偏差(RSD)不大于4.8%,相对误差(RE)不大于5.1%;实际样品的相对标准偏差均不大于4.9%。

关 键 词:碱熔  电感耦合等离子体质谱法(ICP-MS)  地质样品                      
收稿时间:2021-03-15

Determination of zirconium,niobium,hafnium,tantalum,lithium,beryllium,vanadium,phosphorus,uranium and manganese in geological samples by inductively coupled plasma mass spectrometry with sodium peroxide alkali fusion
SUN Menghua,LI Xiaojing,WANG Wenjuan,WANG Xin,YU Congling.Determination of zirconium,niobium,hafnium,tantalum,lithium,beryllium,vanadium,phosphorus,uranium and manganese in geological samples by inductively coupled plasma mass spectrometry with sodium peroxide alkali fusion[J].Metallurgical Analysis,2022,42(1):78-84.
Authors:SUN Menghua  LI Xiaojing  WANG Wenjuan  WANG Xin  YU Congling
Affiliation:1. Hebei Research Center for Geoanalysis, Baoding 071051, China; 2. Hebei Provincial Key Laboratory of Mineral Resources and Ecological Environment Monitoring, Baoding 071051, China
Abstract:The accurate determination of Zr, Nb, Hf, Ta, Li, Be, V, P, U and Mn in geological sample is beneficial to the study of geological environments such as geochemistry and petrogenesis. The sample was treated by alkali fusion with sodium peroxide and acidification with hydrochloric acid. 6Li was selected to correct Li and Be. 103Rh was selected to correct V, P, Zr, Nb and Mn. 185Re was selected to correct Ta, Hf and U. The method for determination of these elements in geological sample by inductively coupled plasma mass spectrometry (ICP-MS) was established. The sample fusion experiments showed that 0.100 0 g of geological sample could be fully fused by 1.0 g of sodium peroxide in muffle furnace at 750 ℃ for 8 min. The matrix interference tests showed that the mass concentration of Na+ in testing solution was less than 1.0 mg/mL after dilution for 10 times, and the interference caused could be ignored. The interference of major elements in sample including K, Ca, Fe, Mg and Al could be also ignored. The standing time of testing solution was optimized, which should be within 1 d. Under the optimized experimental conditions, the linear correlation coefficients of calibration curves for ten testing elements were all higher than 0.999. The limits of detection were between 0.10 μg/g and 2.64 μg/g. The limits of quantification were between 0.33 μg/g and 8.80 μg/g. The contents of Zr, Nb, Hf, Ta, Li, Be, V, P, U and Mn in certified reference materials of soil, stream sediments and rocks as well as actual samples were determined according to the experimental methods. The results showed that the determination results of certified reference materials were basically consistent with the certified values. The relative standard deviations (RSD) were not more than 4.8%, and the relative errors (RE) were not more than 5.1%. The RSDs of actual samples were all not more than 4.9%.
Keywords:alkali fusion  inductively coupled plasma mass spectrometry(ICP-MS)  geological sample  zirconium  niobium  hafnium  tantalum  lithium  beryllium  vanadium  phosphorus  uranium  manganese  
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