Optimal double and triple spiking for high precision lead isotopic measurement

被引:188
作者
Galer, SJG [1 ]
机构
[1] Max Planck Inst Chem, Abt Geochem, D-55020 Mainz, Germany
关键词
lead isotopes; mass discrimination; double spike; triple spike; optimization;
D O I
10.1016/S0009-2541(98)00203-4
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
Conventional lead isotope ratio measurements by thermal ionization mass spectrometry (TIMS) are currently limited to external precisions of similar to 0.1% (2 sigma) due to variations in instrumental mass discrimination, the magnitude of which can only be assessed using external standard or duplicate measurements. The goal of the double-spike technique, by contrast, is to circumvent this fractionation problem entirely by determining the mass discrimination factor epsilon directly for each sample. The unknown factor can be obtained after performing a second measurement on a sample aliquot to which a double spike of known, calibrated composition has been added. Practical applications of the double-spike technique up until now have used a mixed Pb-207-Pb-204 tracer with considerable success, but there appears to have been little or no attempt to optimize the composition of the tracer used. An optimal tracer composition must fulfil two criteria: (1) the ratio of the internal, measured errors to a posteriori errors-the error magnification factors-should be as small as possible; (2) the propagated errors should not be strongly influenced by the spike/sample ratio of the second, mixture run-the latter is important since sample size cannot, in general, be rigorously controlled in advance. Of equal importance to the tracer composition itself is the choice of the three mass-balance equation set used to solve for epsilon; geometrically, this is equivalent to defining a mixing line in a particular 3D isotope space. Potential spike compositions were examined in four such 3D isotope spaces, corresponding to cases where Pb-208,Pb-207,Pb-206 and Pb-204 in turn are common, denominator isotopes of the ratios on the three orthogonal axes. Within each isotope space there exist three possible double-spike families. Tracers composed of three stable isotopes of lead-so-called 'triple spikes'-are also considered, of which there are three families per isotope space. These spike compositions were evaluated for a typical common lead composition, at first using geometric methods, and then refined by determining error magnification factors using an ion statistical error model. It is shown that the Pb-207-Pb-204 double spike used in previous studies, where epsilon is determined in Pb-208,Pb-207,Pb-206/Pb-204 isotope space, is one of the least suitable to use. Optimal tracer compositions for determining epsilon appear to be restricted to two families: The first is a family of Pb-207-Pb-204-Pb-206 triple spikes with Pb-207/Pb-204 of around unity and the isotope space has Pb-206 as the denominator isotope; the second family consists of Pb-204-Pb-207 double spikes, solved in Pb-208,Pb-206,Pb-204/Pb-207 isotope space. Both of these families yield error magnification factors on a posteriori, corrected Pb-206/Pb-204 ratios as low as similar to 1.2, and are less than 2 for all but highly underspiked and overspiked mixture compositions. (C) 1999 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:255 / 274
页数:20
相关论文
共 34 条
[1]   Secular changes of lead and neodymium in central Pacific seawater recorded by a Fe-Mn crust [J].
Abouchami, W ;
Goldstein, SL ;
Galer, SJG ;
Eisenhauer, A ;
Mangini, A .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1997, 61 (18) :3957-3974
[2]  
ABOUCHAMI W, 1998, IN PRESS GEOCHIM COS
[3]  
albarede f, 1995, INTRO GEOCHEMICAL MO, V1st, DOI DOI 10.1017/CBO9780511622960
[4]   LEAD ISOTOPIC ANALYSIS USING A DOUBLE SPIKE [J].
COMPSTON, W ;
OVERSBY, VM .
JOURNAL OF GEOPHYSICAL RESEARCH, 1969, 74 (17) :4338-&
[5]   DOUBLE-SPIKE CALIBRATION OF BROKEN HILL STANDARD LEAD [J].
COOPER, JA ;
REYNOLDS, PH ;
RICHARDS, JR .
EARTH AND PLANETARY SCIENCE LETTERS, 1969, 6 (06) :467-&
[6]   PROPAGATION OF EXPERIMENTAL ERRORS IN LEAD ISOTOPE RATIO MEASUREMENTS USING DOUBLE SPIKE METHOD [J].
CUMMING, GL .
CHEMICAL GEOLOGY, 1973, 11 (03) :157-165
[7]  
DALLWITZ MJ, 1970, CHEM GEOL, V6, P311, DOI DOI 10.1016/0009-2541(70)90032-X
[8]   URANIUM AND THORIUM IN ALKALIC ROCKS FROM ACTIVE CARBONATITE VOLCANO OLDOINYO-LENGAI (TANZANIA) [J].
DAWSON, JB ;
GALE, NH .
CHEMICAL GEOLOGY, 1970, 6 (03) :221-&
[9]   INTERNAL STANDARD TECHNIQUE FOR PRECISE ISOTOPIC ABUNDANCE MEASUREMENTS IN THERMAL IONIZATION MASS SPECTROMETRY [J].
DIETZ, LA ;
LAND, GA ;
PACHUCKI, CF .
ANALYTICAL CHEMISTRY, 1962, 34 (06) :709-&
[10]   A THEORETICAL STUDY OF USE OF INTERNAL STANDARDS FOR PRECISE ISOTOPIC ANALYSIS BY SURFACE IONIZATION TECHNIQUE .1. GENERAL FIRST-ORDER ALGEBRAIC SOLUTIONS [J].
DODSON, MH .
JOURNAL OF SCIENTIFIC INSTRUMENTS, 1963, 40 (06) :289-&