摘要
本文报道ICP-MS直接测定高纯(5N~6N)氧化镱中稀土和非稀土杂质的新方法.对ICP-MS测定中的光谱干扰和基体效应进行了详细考察,结果表明:用镓作内标,可有效地补偿因氧化镱引起的基体效应.方法的检出限在0.0X-0.Xng/mL范围;相对标准偏差(RSD)(n=7)<10%.已应用于高纯氧化镱的工艺流程及其产品分析.
A method for the determination of trace amounts of rare earth and non-rare earth impurities in high purity Yb 2O 3 by ICP-MS has been reported. Experimental parameters which affect analytical results were discussed in detail. Ga as an internal stanard was selected pioneerly to compensate for matrix suppression effect and sensitivity drift. The detection limits are 0.014 ̄0.085ng/mL and 0.05 ̄0.14ng/mL for rare earth and nonrare earth elements, respectively. The recoveries in the range of 88 ̄104% with RSD of 1.2 ̄8.3% were obtained.
出处
《分析科学学报》
CAS
CSCD
1997年第2期97-101,共5页
Journal of Analytical Science
关键词
ICP
MS
氧化镱
稀土
杂质
内标
高纯氧化镱
ICP MS, High purity ytterbium oxide, Rare earth impurities, Non-rare earth impurities, Internal standard