H. Gnaser, ISOTOPE EFFECTS IN THE FORMATION OF MCS(+) MOLECULAR SECONDARY IONS, Nuclear instruments & methods in physics research. Section B, Beam interactions with materials and atoms, 100(2-3), 1995, pp. 347-351
Bombardment of solid surfaces by Cs+ ions results in the emission of m
olecular secondary ions of the type MCs(+), where M stands for an elem
ent contained in the sample. Generally, these molecular species exhibi
t emission characteristics distinctly different from those of the atom
ic ions. Previous experiments ascribed this observation to the possibl
e formation mechanism of MCs(+) ions: the association of a neutral M a
tom with a Cs+ ion in the sputtering event. To further elucidate these
formation processes, the possible influence of isotopic mass differen
ces was investigated: the yields of MCs(+) ions sputtered from various
elements (M = B, Si, Ge, and Mo) under 5.5 keV Cs+ bombardment were m
easured as a function of the emission energy for two (or more) isotope
s of any of those elements. While the atomic ions Mf exhibit a pronoun
ced (up to similar to 10%) light-isotope enrichment in the flux which
decreases with increasing energy, for MCs(+) species the isotope effec
ts are much smaller and show a different emission-energy dependence. A
bove similar to 10 eV the light/heavy ratio of the MCs(+) nux tends to
increase with increasing emission energy; with MCs(+) ions probing th
e emission of neutral M atoms, this finding agrees with the prediction
s of computer simulations which indicate a pronounced enrichment of th
e lighter isotope in the flux of sputtered neutral atoms at higher ene
rgies. At very low energies (< 5 eV), MCs(+) ions from Si, Ge, and Mo
show an isotope fractionation similar to that of atomic ions, while th
e flux of BCs+ is enriched in the heavier B isotope.