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Mass Spectrometry A Textbook - Department of Mathematics and ...

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82 3 Isotopes<br />

The isotopic patterns <strong>of</strong> sulfur <strong>and</strong> silicon are by far not as prominent as those<br />

<strong>of</strong> chlorine <strong>and</strong> bromine, but as pointed out, their contributions are sufficiently<br />

important (Fig. 3.5).<br />

The relevance <strong>of</strong> oxygen <strong>and</strong> sulfur isotopic patterns is nicely demonstrated by<br />

the cluster ion series in fast atom bombardment (FAB) spectra <strong>of</strong> concentrated sulfuric<br />

acid, where the comparatively large number <strong>of</strong> sulfur <strong>and</strong> oxygen atoms<br />

gives rise to distinct isotopic patterns in the mass spectrum (Chap. 9).<br />

Fig. 3.5. Calculated isotopic patterns for combinations <strong>of</strong> elemental silicon <strong>and</strong> sulfur. The<br />

peak shown at zero position corresponds to the monoisotopic ion at m/z X. The isotopic<br />

peaks are then located at m/z = X+1, 2, 3, ...<br />

Note: The preferred procedure to reveal the presence <strong>of</strong> S <strong>and</strong> Si in a mass<br />

spectrum is to examine the X+2 intensity carefully: this signal's intensity will<br />

be too high to be caused by the contribution <strong>of</strong> 13 C2 alone, even if the number<br />

<strong>of</strong> carbons has been obtained from X+1 without prior subtraction <strong>of</strong> the S or Si<br />

contribution.<br />

Example: The isotopic pattern related to the elemental composition <strong>of</strong> ethyl<br />

propyl thioether, C5H12S, (Chap. 6.12) is shown below. The contributions <strong>of</strong> 33 S<br />

<strong>and</strong> 13 C to the M+1 <strong>and</strong> <strong>of</strong> 34 S <strong>and</strong> 13 C2 to the M+2 signal are indicated (Fig. 3.6).<br />

If the M+1 peak resulted from 13 C alone, it would indicate rather the presence <strong>of</strong> 6<br />

carbon atoms, which in turn would require an M+2 intensity <strong>of</strong> only 0.1 % instead<br />

<strong>of</strong> the observed 4.6 %. The introduction <strong>of</strong> Si to explain the isotopic pattern would<br />

still fit the M+2 intensity with comparatively low accuracy. For M+1, the situation<br />

would be quite different. As 29 Si alone dem<strong>and</strong>s 5.1 % at M+1, there would be no<br />

or 1 carbon maximum allowed to explain the observed M+1 intensity.

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