2007
DOI: 10.1016/j.ab.2007.03.037
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Inaccuracies in selected ion monitoring determination of isotope ratios obviated by profile acquisition: nucleotide 18O/16O measurements

Abstract: Precise and accurate measurements of isotopologue distributions (IDs) in biological molecules are needed for the determination of isotope effects, quantitation by isotope dilution and quantifying isotope tracers employed in both metabolic and biophysical studies. While single ion monitoring (SIM) yields significantly greater sensitivity and signal/noise than profile mode acquisitions, we show that small changes in the SIM window width and/or center can alter experimentally determined isotope ratios by up to 5%… Show more

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Cited by 17 publications
(29 citation statements)
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References 47 publications
(135 reference statements)
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“…In these results, to our surprise, the ion trap instrument performed better than the SIM quadrupole determination which had greater precision than the MALDI-TOF analyses. The performance of the quadrupole analysis contributed to our more thorough evaluation of the potential effects of mass granularity reported in the accompanying paper [15]. Based on the results reported there, the accuracy of the quadrupole could have been improved if the data had been acquired and analyzed in profile scan rather than SIM mode.…”
mentioning
confidence: 90%
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“…In these results, to our surprise, the ion trap instrument performed better than the SIM quadrupole determination which had greater precision than the MALDI-TOF analyses. The performance of the quadrupole analysis contributed to our more thorough evaluation of the potential effects of mass granularity reported in the accompanying paper [15]. Based on the results reported there, the accuracy of the quadrupole could have been improved if the data had been acquired and analyzed in profile scan rather than SIM mode.…”
mentioning
confidence: 90%
“…The areas of the successive ions in the IIC comprise the ID and are denoted M n . The isotopologues contributing to the intensity of the M 1 peak will have a single heavy atom substitution, exactly one 2 H, 13 C, 15 N or 17 O atom substituted for the more common isotope (with the higher resolution of ion cyclotron resonance mass spectrometry it is possible to separate the different isotopologues, but not with the typical resolution of commercial TOF instruments).…”
Section: Theorymentioning
confidence: 99%
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