A. Danon et A. Amirav, ISOTOPE, MOLECULAR AND SURFACE EFFECTS ON HYPERTHERMAL SURFACE-INDUCED DISSOCIATIVE IONIZATION, International journal of mass spectrometry and ion processes, 125(1), 1993, pp. 63-74
Citations number
38
Categorie Soggetti
Spectroscopy,"Physics, Atomic, Molecular & Chemical
Organic molecules acquired with hyperthermal (1-20eV) kinetic energy u
ndergo efficient surface ionization. This hyperthermal surface ionizat
ion (HSI) may produce both positive and negative fragment ions. The di
ssociative ionization of alkyl halides results in the production of ne
gative ions of the functional group having high electron affinity, and
positive ions of the alkyl radical, which can further dissociate into
smaller fragments. The effect of the alkyl chain length and the bromi
ne isotope effect on the obtained HSI mass spectra were studied in sev
eral alkyl halide molecules. While the negative ion formation yield is
found to be independent of the size of the alkyl radical, the positiv
e ion formation yield strongly increases with the size of the CnH2n 1 radical for n = 1-4 and then a quasi saturation is observed. The obs
erved radical fragmentation increases with the incident molecular kine
tic energy and was affected by the molecular structure and the surface
temperature and cleanliness. A considerable (up to 24%) heavy bromine
isotope increased ionization is observed at intermediate molecular ki
netic energies. Piperidine HSI on a rhenium filament exhibits a single
(M - 1) ion while its HSI from an oxidized rhenium filament having a
much higher work function is characterized by a much richer fragmentat
ion pattern. The dissociative ionization mechanism is rationalized in
terms of a surface-molecule electron transfer followed by an immediate
dissociation into a negative halogen ion and an alkyl radical. This r
adical, which usually has a low ionization potential, can transfer an
electron to the surface and scatter as a positive ion. At high kinetic
energies, the radicals or positive ions can further dissociate near t
he surface, and then scatter away as lower mass ions with ion yield wh
ich depends on their surface reneutralization probabilities. Thus, the
observed fragmentation pattern is governed by surface chemical and el
ectron transfer processes and not by gas phase unimolecular ion dissoc
iation, as found with large polyatomic molecules.