Quantifying the platinum group elements (PGEs) and gold in geological samples using cation exchange pretreatment and ultrasonic nebulization inductively coupled plasma mass spectrometry (USN-ICP-MS)

被引:83
作者
Ely, JC [1 ]
Neal, CR [1 ]
O'Neill, JA [1 ]
Jain, JC [1 ]
机构
[1] Univ Notre Dame, Dept Civil Engn & Geol Sci, Notre Dame, IN 46556 USA
基金
美国国家科学基金会;
关键词
platinum group elements; cation exchange; ICP-MS; ultrasonic nebulization; standard addition;
D O I
10.1016/S0009-2541(98)00204-6
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
A method for analyzing low abundances of the platinum group elements (PGEs) and gold has been developed using cation exchange chromatography and ultrasonic nebulization inductively coupled plasma mass spectrometry (USN-ICP-MS). Ultrasonic nebulization increases sensitivity over regular pneumatic nebulization so that resolvable signals above background are possible in the fg/g range. Small sample sizes (less than or equal to 250 mg) and law volumes of reagents produce procedural blank levels below the detection limit for Ru, Pd and Ir, in the fg/g range for Ph and in the low pg/g range for Pt and Au. Heterogeneous PGE and Au distributions in geological samples are avoided by a rigorous homogenization/rehomogenization procedure. The reference material UMT-1, which contains rock concentrations of the PGEs and Au at the low ng/g levels, monitored recoverability. Interferences of HfO+ and TaO+ on Ir, Pt and Au were not seen in the analyses of UMT-1 because Hf and Ta have low abundances in this reference material. However, these interferences are acute for silicate rocks, even after cation exchange chromatography. Isotope dilution cannot be adapted to this method for Ir and Pt because two interference-free isotopes are not available. An external calibration method has been developed for the accurate and precise determination of the PGEs and Au in rocks with low abundances of Hf and Ta (< 1 mu g/g and < 0.2 mu g/g, respectively); a standard addition method for rocks containing higher concentrations of these elements. The work presented here demonstrates the strengths and weaknesses of cation exchange for PGE and Au analyses in geological materials. It can be a useful tool in solving fundamental geological problems that depend on precise and accurate determination of these elements by taking full advantage of current technology and the sensitivity it provides. (C) 1999 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:219 / 234
页数:16
相关论文
共 58 条
[1]   PLATINUM METALS SOLUTION CHEMISTRY AND SEPARATION METHODS (ION-EXCHANGE AND SOLVENT-EXTRACTION) [J].
ALBAZI, SJ ;
CHOW, A .
TALANTA, 1984, 31 (10A) :815-836
[2]   OSMIUM ISOTOPES AS PETROGENETIC AND GEOLOGICAL TRACERS [J].
ALLEGRE, CJ ;
LUCK, JM .
EARTH AND PLANETARY SCIENCE LETTERS, 1980, 48 (01) :148-154
[3]   PLATINUM TRACES IN AIRBORNE PARTICULATE MATTER - DETERMINATION OF WHOLE CONTENT, PARTICLE-SIZE DISTRIBUTION AND SOLUBLE PLATINUM [J].
ALT, F ;
BAMBAUER, A ;
HOPPSTOCK, K ;
MERGLER, B ;
TOLG, G .
FRESENIUS JOURNAL OF ANALYTICAL CHEMISTRY, 1993, 346 (6-9) :693-696
[4]   EXTRATERRESTRIAL CAUSE FOR THE CRETACEOUS-TERTIARY EXTINCTION - EXPERIMENTAL RESULTS AND THEORETICAL INTERPRETATION [J].
ALVAREZ, LW ;
ALVAREZ, W ;
ASARO, F ;
MICHEL, HV .
SCIENCE, 1980, 208 (4448) :1095-1108
[5]  
[Anonymous], 1980, ANAL CHEM, V52, P2242
[6]   ELIMINATION OF REAGENT BLANK PROBLEMS IN THE FIRE-ASSAY PRE-CONCENTRATION OF THE PLATINUM GROUP ELEMENTS AND GOLD WITH A NICKEL SULFIDE BEAD OF LESS THAN ONE GRAM MASS [J].
ASIF, M ;
PARRY, SJ .
ANALYST, 1989, 114 (09) :1057-1059
[7]  
Baes C.F., 1976, HYDROLYSIS CATIONS
[8]  
Beamish F.E., 1966, ANAL CHEM NOBLE META
[9]   Separation of Hf and Lu for high-precision isotope analysis of rock samples by magnetic sector multiple collector ICP-MS [J].
BlichertToft, J ;
Chauvel, C ;
Albarede, F .
CONTRIBUTIONS TO MINERALOGY AND PETROLOGY, 1997, 127 (03) :248-260
[10]  
Cabri L. J, 1981, PLATINUM GROUP ELEME, V23, P83