Jm. Rosenbaum et al., Chlorine stable isotopes: A comparison of dual inlet and thermal ionization mass spectrometric measurements, ANALYT CHEM, 72(10), 2000, pp. 2261-2264
Chlorine stable isotope ratios, Cl-37/Cl-35, currently are measured using d
ual-inlet and thermal-ionization mass spectrometry, These two different ana
lytical techniques, however, have never been cross calibrated. A set of sam
ples with chlorine stable isotope delta values ranging from -4.4 to +0.3 pa
rts per thousand relative to standard mean ocean water chloride has been an
alyzed using both of these techniques. Our data show that both techniques c
an yield similar results within analytical uncertainty. CsCl thermal ioniza
tion data are extremely sensitive to the amount of chlorine being measured
and cannot be used to determine absolute ratios without an independent mean
s of correcting for machine-induced mass fractionation, As long as standard
s and samples are of equivalent size, however, the differences between samp
les measured by thermal ionization remain constant. Dual inlet stable isoto
pe mass spectrometry is suited best for samples of >10 mu mol Cl, yielding
chlorine stable isotope data with less than or equal to 0.1 parts per thous
and reproducibilities (2 sigma), Thermal ionization mass spectrometry easil
y accommodates samples of similar to 0.1-0.3 mu mol Cl, with achievable unc
ertainties of less than or equal to 0.2 parts per thousand (2 sigma).