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The chlorine-containing reaction layer acts as a transmitter
between the pure underlying silicide phase and the gas phase
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The level of chlorine intake adjusts the electronic properties of
the reaction layer and determines what silylenoide surface
species are stabilized.
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Primarily, the reactivity of the silicon atoms in the silicide
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dynamic parameters such as enthalpies of mixing or formation
are found to be more useful to explain metal-silicon interactions
rather than band structures of silicide phases. As a second
parameter, the acid-base strength of the reaction gas phase
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distributions between reactions with methyl chloride or hydrogen
chloride can be explained in this manner. Furthermore, the
change in reactivity from metal-rich to silicon-rich silicide
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sites (related to the silicon content) is assumed. The essential
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Yet unclear is how hydrogen is involved in the reaction
mechanism of chlorosilane formation.
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Acknowledgment. We gratefully acknowledge Dr. Kenrick
M. Lewis, Osi Specialties, Crompton Corporation, Tarrytown,
NY, and Professor Gerhard Roewer, Freiberg University, for
fruitful discussions. We thank Dr. S. Roosendaal and Dr. A. J.
Vredenberg, Department of Atomic and Interface Physics, State
University Utrecht, The Netherlands, for RBS investigations and
Dr. N. Mora-Diez, Department of Chemistry, Dalhousie Uni-
versity, Halifax, Nova Scotia, Canada, for manuscripts of
submitted papers. J.A. thanks the Alexander von Humboldt
Foundation for funding provided by a Feodor Lynen Fellowship.
625, 297.
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