Determination of lithium,beryllium,rubidium,cesium,niobium and tantalum in geochemical samples by inductively coupled plasma mass spectrometry and inductively coupled plasma atomic emission spectrometry
ZHU Zhigang, LI Meili, FANG Xiaohong, PENG Liping, XIE Xinkan
Inner Mongolia Minerals Experiment Research Institute,Hohhot 010031,China
Abstract:In view of the characteristics of some geochemical samples, such as large variation range of the associated rare Li, Be, Rb, Cs, Nb and Ta, the high content of Nb and Ta which are easily hydrolyzed, the complicated process of traditional analysis method, and the difficulty to realize simultaneous determination, the sample was decomposed by heating at normal pressure with acid solution system of HF-HNO3-H2SO4 at 10∶5∶1 (volume ratio). The sample solution was extracted with 80 g/L tartaric acid solution to fully complex Nb and Ta. Then the aqua regia was added to fully extract the Li, Be, Rb and Cs into solution by heating. Li, Be, Rb, Nb, Cs and Ta were determined by inductively coupled plasma mass spectrometry (ICP-MS) using 7Li, 9Be, 85Rb, 93Nb, 133Cs and 181Ta as the isotopes for analysis. Li 670.784 nm {Ⅰ}, Be 234.861 nm {Ⅰ}, Rb 780.023 nm {Ⅰ}, Nb 316.340 nm {Ⅱ} and Ta 268.517 nm {Ⅱ} were used as analytical lines for the determination of Li, Be, Rb, Nb and Ta by inductively coupled plasma atomic emission spectrometry (ICP-AES). The method for the determination of Li, Be, Rb, Cs, Nb and Ta in geochemical samples by ICP-MS and ICP-AES was established. The linear correlation coefficients of the calibration curves of Li, Be, Rb, Cs, Nb, and Ta ranged from 0.999 4 to 0.999 9. The limit of detection and limit of quantification (based on ICP-MS) was 0.01-0.15 μg/g and 0.012-0.807 μg/g, respectively. The contents of Li, Be, Rb, Cs, Nb and Ta in certified reference materials of soil, stream sediment and tantalum ore as well as actual sample of a pegmatite mine in Namibia were determined according to the experimental method. The relative standard deviations (RSDs, n=7) of determination results were between 0.78% and 9.6%. The absolute values of the logarithmic difference between the measured and the certified values (|ΔlgC|, n=7) ranged from 0.000 2 to 0.020. The measured values of certified reference materials were basically consistent with the certified values. The spiked recoveries of actual samples were between 93% and 104%.
[1] 汪泰,李沛伦,李汉文,等.新疆某伟晶岩型锂多金属矿石中伴生元素的回收试验[J].金属矿山,2021(11):81-85. WANG Tai,LI Peilun,LI Hanwen,et al.Experimental study on comprehensive recovery of associated elements in pegmatite lithium polymetallic ore in Xinjiang[J].Metal Mine,2021(11):81-85. [2] 岩石矿物分析编委会.岩石矿物分析:第3分册[M].4版.北京:地质出版社,2011:291-292,294-295,378-379. [3] 郭晓瑞,王甜甜,张宏丽,等.电感耦合等离子体质谱法测定地球化学样品中铌钽钨锡[J].冶金分析,2021,41(3):44-50. GUO Xiaorui,WANG Tiantian,ZHANG Hongli,et al.Determination of niobium,tantalum,tungsten and tin in geochemistry samples by inductively coupled plasma mass spectrometer[J].Metallurgical Analysis,2021,41(3):44-50. [4] 胡明,万兵,任志海,等.高压消解-电感耦合等离子体质谱(ICP-MS)法测定地质样品中的铌和钽[J].中国无机分析化学,2016,6(3):35-38. HU Ming,WAN Bing,REN Zhihai,et al.Determination of niobium and tantalum in mineral by high pressure dissolution-inductively coupled plasma mass spectrometer[J]. Chinese Journal of Inorganic Analytical Chemistry,2016,6(3):35-38. [5] 杨秀丽,吕晓惠,陈小迪,等.ICP-MS连续测定地质样品中的锂、铷、铯、铌和钽[J].现代科学仪器,2012(2):94-95. YANG Xiuli,LÜ Xiaohui,CHEN Xiaodi,et al.Determination of lithium,rubidium,cesium,niobium and tantalum in mineral by inductively coupled plasma mass spectrometer[J].Modern Scientific Instruments,2012(2):94-95. [6] 张晨芳,李墨,杨颖,等.密闭压力酸溶-电感耦合等离子体质谱法测定岩浆岩中稀有元素[J].分析科学学报,2018,34(6):801-805. ZHANG Chenfang,LI Mo,YANG Ying,et al.Quantification of rare elements in magmatic rocks by inductively coupled plasma-mass spectrometer after pressurized acid digestion[J].Journal of Analytical Science,2018,34(6):801-805. [7] 姚玉玲,吴丽琨,刘卫,等.乙醇增敏-电感耦合等离子体发射光谱法测定矿石及选冶样品中的铌钽[J].岩矿测试,2015,34(2):224-228. YAO Yuling,WU Likun,LIU Wei,et al.Determination of Nb and Ta in ores and metallurgical samples by inductively coupled plasma-atomic emission spectrometer with ethanol as a sensitizer[J].Rock and Mineral Analysis,2015,34(2):224-228. [8] 潘钢,易建春.恒温电热板湿法消解ICP-AES对地质样品中铌和钽的连续测定[J].光谱实验室,2012,29(3):1597-1600. PAN Gang,YI Jianchun.Continuous determination of niobium and tantalum in geological samples by ICP-AES with constant temperature electric heating plate wet digestion[J].Chinese Journal of Spectroscopy Laboratory,2012,29(3):1597-1600. [9] 郝冬梅,张翼明,许涛,等.ICP-MS法测定稀土铌钽矿中铍、铀、铌、钽、锆、铪量[J].稀土,2010,31(5):67-69. HAO Dongmei,ZHANG Yiming,XU Tao,et al.Determination of beryllium, uranium, niobium, tantalum, zirconium and hafnium in rare earth,niobium,tantalum mineral by ICP-MS[J].Chinese Rare Earths,2010,31(5):67-69. [10] 高会艳.ICP-MS和ICP-AES测定地球化学勘查样品及稀土矿石中铌钽方法体系的建立[J].岩矿测试,2014,33(3):312-320. GAO Huiyan.Determination systems of Nb and Ta in geochemistry samples and rare earth ores by ICP-MS and ICP-AES[J].Rock and Mineral Analysis,2014,33(3):312-320. [11] 胡家祯,于亚辉,吴娣,等.电感耦合等离子体质谱法(ICP-MS)测定水系沉积物中的铌钽锆铪[J].矿产与地质,2016,30(4):699-702. HU Jiazhen,YU Yahui,WU Di,et al.Determination of Nb,Ta,Zr and Hf in stream sediment by inductively coupled plasma mass spectrometer(ICP-MS)[J].Mineral Resources and Geology,2016,30(4):699-702. [12] 孙孟华,李晓敬,王文娟,等.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. SUN Menghua,LI Xiaojing,WANG Wenjuan,et al.Determination of zirconium,niobium,hafnium,tantalum,lithium,beryllium,vanadium,phosphorus,uranium and manganese in geological samples by inductively coupled plasma mass spectrometer with sodium peroxide alkali fusion[J].Metallurgical Analysis,2022,42(1):78-84. [13] 岩石矿物分析编委会.岩石矿物分析:第1分册[M].4版.北京:地质出版社,2011:203-204,750-751.