We investigated high-precision Pb isotope ratio analysis by multi-collector
-inductively coupled plasma-mass spectrometry (MC-ICP-MS) using added thall
ium as an internal isotopic standard to correct for mass dependent isotopic
fractionation. We compared MC-ICP-MS analysis of both an inter-laboratory
standard, NBS 981, and geological samples to conventional thermal ionizatio
n mass spectrometry (TIMS). As expected, we found that analytical error in
the latter was dominated by mass fractionation, In MC-ICP-MS, we found that
fractionation appears to follow the exponential law, but that the fraction
ation coefficients, f, of Tl and Ph were nor identical. This difference in
fractionation coefficients cannot be compensated for by renormalizing to a
different T1 isotopic composition as done in other studies. We found, howev
er, that the f(Pb)/f(Tl) ratio was constant over the course of an analytica
l session, allowing f(Pb) to be calculated from f(Tl). An exponential law c
orrection was then applied to the Pb isotope measurements which effectively
eliminates enters associated with mass fractionation, Precision for the MC
-ICP-MS analyses ranged from a factor of 2 to a factor of 6 better than for
TIMS analyses for the Pb-206/Pb-204 and Pb-208/Pb-206 ratios respectively.
Residual error in the MC-ICP-MS analyses was dominated by error in the ana
lysis of Pb-204, perhaps in part clue to random errors introduced by correc
ting for a Hg-204 isobaric interference. We also found systematic errors in
the MC-ICP-MS analyses compared to TIMS determinations that may be due to
uneven background and collector biases in the instrument used. We found tha
t these systematic errors were the same for both NBS 981 and the geological
samples, so accurate correction factors could be generated from the standa
rd analyses to correct the sample analyses. MC-ICP-MS has the additional ad
vantages of requiring less preparative chemistry, less instrument time, and
considerably less labor overall. (C) 2000 Elsevier Science B.V. All rights
reserved.