Simple and cost-effective methods for precise analysis of trace element abundances in geological materials with ICP-MS

被引:85
作者
Chen, Shuo [1 ,2 ,3 ]
Wang, Xiaohong [1 ,2 ]
Niu, Yaoling [1 ,2 ,4 ]
Sun, Pu [1 ,2 ,3 ]
Duan, Meng
Xiao, Yuanyuan [1 ,2 ]
Guo, Pengyuan [1 ,2 ]
Gong, Hongmei [1 ,2 ]
Wang, Guodong [1 ,2 ]
Xue, Qiqi [5 ]
机构
[1] Chinese Acad Sci, Inst Oceanol, Qingdao 266071, Peoples R China
[2] Qingdao Natl Lab Marine Sci & Technol, Lab Marine Geol, Qingdao 266061, Peoples R China
[3] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
[4] Univ Durham, Dept Earth Sci, Durham DH1 3LE, England
[5] China Univ Geosci, Sch Earth Sci & Mineral Resources, Beijing 100083, Peoples R China
基金
中国国家自然科学基金;
关键词
Inductively coupled plasma mass spectrometry; High-pressure digestion; Oxide and hydroxide interferences; Instrumental drift; Correction methods; Trace elements; PLASMA-MASS-SPECTROMETRY; UPPER CONTINENTAL-CRUST; RARE-EARTH-ELEMENTS; INTERNAL STANDARDIZATION; ROCK DISSOLUTION; SAMPLES; DECOMPOSITION; OXIDE; INTERFERENCES; GEOCHEMISTRY;
D O I
10.1016/j.scib.2017.01.004
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Inductively coupled plasma mass spectrometry (ICP-MS) is the most commonly used technique to determine the abundances of trace elements in a wide range of geological materials. However, incomplete sample digestion, isobaric interferences and instrumental drift remain obvious problems that must be overcome in order to obtain precise and accurate results. For this reason, we have done many experiments and developed a set of simple, cost-effective and practical methods widely applicable for precise and rapid determination of trace element abundances in geological materials using ICP-MS. Commonly used high-pressure digestion technique is indeed effective in decomposing refractory phases, but this inevitably produces fluoride complexes that create new problems. We demonstrate that the fluoride complexes formed during high-pressure digestion can be readily re-dissolved using high-pressure vessel at 190 degrees C for only 2 h for 50 mg sample. In the case of isobaric interferences, although oxide (e.g., MO+/M+) and hydroxide (e.g., MOH+/M+) productivity is variable between runs, the (MO+/M+)/(CeO+/Ce+) and (MOH+/M+)/(CeO+/Ce+) ratios remain constant, making isobaric interference correction for all other elements of interest straightforward, for which we provide an easy-to-use off-line procedure. We also show that mass-time-intensity drift curve is smooth as recognized previously, for which the correction can be readily done by analyzing a quality-control (QC) solution and using off-line Excel VBA procedure without internal standards. With these methods, we can produce data in reasonable agreement with recommended values of international rock reference standards with a relative error of <8% and precision generally better than 5%. Importantly, compared to the widely used analytical practice, we can effectively save >60% of time (e.g., < 24 h vs. > 60 h). (C) 2017 Science China Press. Published by Elsevier B.V. and Science China Press. All rights reserved.
引用
收藏
页码:277 / 289
页数:13
相关论文
共 38 条
[1]   Matrix effects in inductively coupled plasma mass spectrometry: A review [J].
Agatemor, Christian ;
Beauchemin, Diane .
ANALYTICA CHIMICA ACTA, 2011, 706 (01) :66-83
[2]   Simultaneous correction for drift and non-spectroscopic matrix effect in the measurement of geological samples by inductively coupled plasma-mass spectrometry using common analyte internal standardization chemometric technique [J].
Al-Ammar, AS .
SPECTROCHIMICA ACTA PART B-ATOMIC SPECTROSCOPY, 2003, 58 (08) :1391-1401
[3]  
[Anonymous], GEOSTAND GEOANAL RES
[4]   A routine method for oxide and hydroxide interference corrections in ICP-MS chemical analysis of environmental and geological samples [J].
Aries, S ;
Valladon, M ;
Polvé, M ;
Dupré, B .
GEOSTANDARDS NEWSLETTER-THE JOURNAL OF GEOSTANDARDS AND GEOANALYSIS, 2000, 24 (01) :19-31
[5]   Large U loss during weathering of upper continental crust: The sedimentary record [J].
Carpentier, Marion ;
Weis, Dominique ;
Chauvel, Catherine .
CHEMICAL GEOLOGY, 2013, 340 :91-104
[6]   DECOMPOSITION TECHNIQUES [J].
CHAO, TT ;
SANZOLONE, RF .
JOURNAL OF GEOCHEMICAL EXPLORATION, 1992, 44 (1-3) :65-106
[7]  
CHEATHAM MM, 1993, SPECTROCHIM ACTA B, V48, pE487
[8]  
Chen S, 2015, MINERAL PETROL, P1
[9]   Classical and New Procedures of Whole Rock Dissolution for Trace Element Determination by ICP-MS [J].
Cotta, Aloisio J. B. ;
Enzweiler, Jacinta .
GEOSTANDARDS AND GEOANALYTICAL RESEARCH, 2012, 36 (01) :27-50
[10]   Reference materials for geochemical studies: New analytical data by ICP-MS and critical discussion of reference values [J].
Dulski, P .
GEOSTANDARDS NEWSLETTER-THE JOURNAL OF GEOSTANDARDS AND GEOANALYSIS, 2001, 25 (01) :87-125