Determination of trace elements in granites by inductively coupled plasma mass spectrometry

被引:1396
作者
Liang, Q [1 ]
Jing, H
Gregoire, DC
机构
[1] Chinese Acad Sci, Open Lab Ore Deposit, Inst Geochem, Guiyang 350002, Peoples R China
[2] Geol Survey Canada, Ottawa, ON K1A 0E8, Canada
关键词
trace elements; granites; ICP mass spectrometry;
D O I
10.1016/S0039-9140(99)00318-5
中图分类号
O65 [分析化学];
学科分类号
070302 ; 081704 ;
摘要
Proposed is a simple and reliable method for the dissolution of granite and the determination of 38 elements by inductively coupled plasma mass spectrometry. One hundred milligrams of sample are digested with 1 mi of HF and 0.5 mi of HNO3 in screw top PTFE-lined stainless steel bombs at 190 degrees C for 12 h. Insoluble residues are dissolved using 8 mi of 40% HNO3 (v/v) heated to 110 degrees C for 3 h. Six granite standard reference materials (GSR-1, JG-2, G-2, NIM-G, SG-3, SG-La) were studied. Analytical calibration was accomplished using aqueous standard solutions. Rhodium was used as an internal standard to correct for matrix effects and instrument drift. We report data for: Li, Be, Sc, V, Cr, Co, Ni, Cu, Zn, Ga, Rb, Sr, Y, Zr, Nb, Mo, Cs, Ba, Hf, Ta, W, Pb, Th, U and 14 of the rare earth elements. The recoveries for most of these elements in granite ranged from 90 to 110%. (C) 2000 Elsevier Science B.V. All rights reserved.
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页码:507 / 513
页数:7
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