R. Kuster et K. Christmann, THE INTERACTION OF METHYL-CHLORIDE WITH A SILICON(111) SURFACE, Berichte der Bunsengesellschaft fur Physikalische Chemie, 101(12), 1997, pp. 1799-1810
Citations number
41
Journal title
Berichte der Bunsengesellschaft fur Physikalische Chemie
In the technical Muller-Rochow synthesis, dimethyl dichlorsilane (DMD)
is fabricated from methyl chloride which interacts with a 'contact ma
ss' consisting of elemental Si and Cu (Cu being a catalyst). In order
to better understand some of the elementary steps of this reaction, we
have followed the adsorption of methyl chloride on a (7x7) reconstruc
ted Si(111) surface in the temperature range between 100 and 1000 K by
means of LEED, Auger electron spectroscopy (AES), temperature-program
med thermal desorption (TPD), vibrational loss spectroscopy (HREELS),
and work function change (Delta Phi) measurements. CH3Cl adsorbs effec
tively in a single weakly chemisorbed state. The adsorption energy is
strongly coverage-dependent and decreases from initially similar to 40
kJ/mol to similar to 30 kJ/mol near the monolayer. During adsorption,
the work function of the Si(111) surface first increases sharply by 0
.36 eV and saturates, after an intermediate maximum of similar to 40 e
V near the monolayer, at similar to 0.61 eV. CH3Cl-derived vibrational
losses appear at 88, 176, 340, and 370 meV and can be associated with
known gas phase vibrations of CH3Cl. An additional band at 260 meV is
tentatively ascribed to the Si-H stretching vibration, pointing to co
mpeting dissociation of adsorbed CH3Cl into hydrogen and methylene chl
oride CH2Cl. Otherwise, CH3Cl does not react with Si(111) under our UH
V conditions (CH3Cl partial pressures less than or equal to 10(-5) mba
r, 100 less than or equal to T less than or equal to 300 K), as the ab
sence of any Cl- and/or Si-containing mass fragments in the TPD spectr
a proves. We deduce from our investigation that the combined chlorinat
ion and methylation of Si in the technical Muller-Rochow process is di
ctated by processes which run only at much larger (atmospheric) pressu
res and/or elevated temperatures.