CHARACTERIZATION OF FLAME-GENERATED C-10 TO C-160 POLYCYCLIC AROMATIC-HYDROCARBONS BY ATMOSPHERIC-PRESSURE CHEMICAL-IONIZATION MASS-SPECTROMETRY WITH LIQUID INTRODUCTION VIA HEATED NEBULIZER INTERFACE

Citation
Al. Lafleur et al., CHARACTERIZATION OF FLAME-GENERATED C-10 TO C-160 POLYCYCLIC AROMATIC-HYDROCARBONS BY ATMOSPHERIC-PRESSURE CHEMICAL-IONIZATION MASS-SPECTROMETRY WITH LIQUID INTRODUCTION VIA HEATED NEBULIZER INTERFACE, Journal of the American Society for Mass Spectrometry, 7(3), 1996, pp. 276-286
Citations number
40
Categorie Soggetti
Chemistry Physical","Chemistry Analytical",Spectroscopy
ISSN journal
10440305
Volume
7
Issue
3
Year of publication
1996
Pages
276 - 286
Database
ISI
SICI code
1044-0305(1996)7:3<276:COFCTC>2.0.ZU;2-#
Abstract
Complex mixtures of polycyclic aromatic hydrocarbons (PAHs) generated from fuel-rich combustion of ethylene-naphthalene mixtures in a jet-st irred-plug-flow reactor were chemically characterized by combined mass spectrometric techniques to yield product composition data that cover the molecular mass region from simple PAHs (naphthalene, 128 u) to la rge molecules comparable in molecular size (1792 u) to nanoparticles o f soot. Two techniques based on atmospheric-pressure chemical ionizati on mass spectrometry (APCI-MS) were investigated: (1) APCI-MS combined with high-performance Liquid chromatography through a heated nebulize r interface was found suitable for PAHs up to C-36 (448 u). (2) For th e characterization of larger PAHs beyond C-36, direct liquid introduct ion (DLI) of sample into an atmospheric-pressure chemical ionization m ass spectrometer through a heated nebulizer gave protonated molecular ions for PAHs over the m/z 400-2000 range. Although unequivocal elemen tal composition information is unattainable from the unit-resolution D LI/APCI-MS data, by starting with structural data from identified C-16 to C-32 PAHs, and applying PAH molecular growth principles, it was po ssible to generate PAH molecular maps from the DLI/APCI-MS data from w hich values for the elemental composition could be derived for all maj or peaks.