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石墨炉原子吸收光谱法测定地质样品中微量镓
引用本文:黄碧燕.石墨炉原子吸收光谱法测定地质样品中微量镓[J].光谱实验室,2010,27(5):2042-2044.
作者姓名:黄碧燕
作者单位:福建省闽西地质大队实验室,福建省三明市富兴路50号,365000
摘    要:用硝酸、硫酸、氢氟酸分解处理样品,4%(V/V)硝酸提取,以硫酸铵(1%)+(0.5mg/mL)钒作为基体改进剂,塞曼效应扣除背景,石墨炉原子吸收光谱测定。该方法快速简便,相对标准偏差(RSD)为2.1%—2.9%,回收率在98.0%—106.0%之间。

关 键 词:石墨炉原子吸收光谱法  地质样品    基体改进剂

Determination of Trace Ga in Geological Samples by GFAAS
HUANG Bi-Yan.Determination of Trace Ga in Geological Samples by GFAAS[J].Chinese Journal of Spectroscopy Laboratory,2010,27(5):2042-2044.
Authors:HUANG Bi-Yan
Institution:HUANG Bi-Yan(Western Geological Lab.of Fujian Province,Sanming,Fujian 36500,P.R.China)
Abstract:The geological samples were digested by HNO3,H2SO4 and HF and extracted by 4% HNO3(V/V).The 1%(NH4)2SO4+V5+ was used as modification.The graphite furnace atomic absorption spectrometry with Zeeman background correction was applied to determinate trace Ga in the samples.This method was convenient.The RSD ranged from 2.1% to 2.9% and recoveries were between 98.0% and 106.0%.
Keywords:GFAAS  Geological Samples  Ga  Modification
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