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Article Abstract

Rationale: Secondary electrospray ionization (SESI) in a water spray environment at atmospheric pressure involves the reactions of hydrated hydronium reagent ions, H O (H O) , with trace analyte compounds in air samples. Understanding the formation and dehydration of reagent and analyte ions is the foundation for meaningful quantification of trace compounds by SESI-mass spectrometry (MS).

Methods: A numerical model based on gas-phase ion thermochemistry is developed that describes equilibria in H O (H O) reagent cluster ion distributions and ligand switching reactions with polar NH molecules leading to equilibrated hydrated ammonium ions NH (H O) . The model predictions are compared with experimental results obtained using a cylindrical SESI source coupled to an ion-trap mass spectrometer via a heated ion transfer capillary. Non-polar isoprene, C H , was used to further probe the nature of the reagent ions.

Results: Equilibrium distributions of H O (H O) ions and their reactions with NH molecules have been characterized by the model in the near-atmospheric pressure SESI source. NH analyte molecules displace H O ligands from the H O (H O) ions at the collisional rate forming NH (H O) ions, which travel through the heated ion transfer capillary losing H O molecules. The data for variable NH concentrations match the model predictions and the C H test substantiates the notion of dehydration in the heated capillary.

Conclusions: Large cluster ions formed in the SESI region are dehydrated to H O (H O) and NH (H O) while passing through the heated capillary, and considerable diffusion losses also occur. This phenomenon is also predicted for other polar analyte molecules, A, that can undergo similar switching reactions, thus forming AH and AH (H O) analyte ions.

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http://dx.doi.org/10.1002/rcm.9047DOI Listing

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