Many fields of basic and applied
sciences, including geochronology,
astronomy, metabolism, etc., rely on the ability of mass spectrometry
to obtain isotope ratio measurements having a high degree of certainty.
The inability to resolve difficult isobaric interferences plagues
certain measurements. A combined atomic and molecular (CAM) ionization
source has been interfaced to a high-field Orbitrap mass spectrometer
to alleviate severe atomic, isobaric interferences. This work examines
the geochronologically significant 87Sr and 87Rb isotope pair. The mass difference between 87Sr and 87Rb is approximately 0.3 mDa, requiring a minimum resolving
power (R = m/Δm) of ∼290,000, a value ∼30× higher than available
with sector-field elemental mass spectrometers. Under ultrahigh-resolution
conditions, Sr isotope ratio accuracy and precision were evaluated
using NIST Sr SRM 987, yielding precision values of <0.1% relative
standard deviation (RSD) for the major isotopes and a calculated LOD
of 2 pg mL–1 (120 fg of Sr for a 60 μL injection).
In addition to manipulating the signal transient length, the total
number of ions in the electrostatic trap and the 87Sr/87Rb concentration ratio were found to influence resolution.
Ultimately, the isotopes were baseline-resolved with a calculated
mass resolution of >1.7M. At equal 87Sr and 87Rb intensities, 87Sr/86Sr was measured as 0.71294
(a relative error of only 0.37%) with a precision of 0.097% RSD, clearly
reflecting the alleviation of the isobaric interference.