Basic rules for the interpretation of atmospheric pressure ionization mass spectra of small molecules

This review summarizes the basic rules for the interpretation of atmospheric pressure ionization (API) mass spectra of small molecules written with the style primarily intended for beginners and low-experienced researchers with the mass spectra interpretation. The first and basic step in any interpretation of mass spectra is always the determination of molecular weight, which is relatively easy in case of soft ionization techniques due to the limited extend of fragmentation and the prevailing presence of (de)protonated molecules in the full scan mass spectra. These [M+H]+ and [M−H]− ions are often accompanied by low abundant molecular adducts, which can be used as the supplementary information for the unambiguous determination of molecular weights. In certain cases, adduct ions may dominate the spectra. The subsequent interpretation of full scan and tandem mass spectra is more complicated due to a high number of possible functional groups, structural subunits and their combinations resulting in numerous competitive fragmentation pathways. Typical neutral losses and the effect of individual functional groups on the fragmentation are discussed in detail and illustrated with selected examples. Modern mass analyzers have powerful features for the structural elucidation, for example high resolving power, high mass accuracy, multistage tandem mass spectrometry, dedicated softwares for the interpretation of mass spectra and prediction of their fragmentation. Background information on differences among individual ionization techniques suitable for the HPLC–MS coupling and basic types of mass analyzers with consequences for the data interpretation is briefly discussed as well. Selected examples illustrate that the right optimization of chromatographic separation and the use of other than mass spectrometric detectors can bring valuable complementary information.