Abstract
The adsorption and possible mechanisms for
the surface transport of stearic acid and some of its derivatives on solids
have been investigated using radioactive tracers.� mono- and multimolecular layers of these
compounds were deposited on quartz glass, mica, and metal specimens, which were
then held at various temperatures for a short period. The resulting changes in
amount and distribution of activity were determined by autoradiography or an
appropriately designed Geiger tube.
On unreactive surfaces such as platinum or
quartz glass the pure acid is only weakly adsorbed and thermal desorption, in
general, readily occurs, especially of layers deposited on an initial
monolayer. Layers of copper or calcium soaps on all surfaces, either deposited
as such or formed in situ, are very much more stable. There is also some
evidence that desorption is favoured by the presence of water vapour. Both pure
acid and soap layers have some resistance to mechanical abrasion, but none to
dissolution by hot benzene unless the adsorption involves a chemical bond.
Part B of the present paper describes an
experimental search for a long-range surface diffusion, using the same surfaces
and adsorbates. It is shown that, under favourable conditions, material
desorbed from one part of a surface will readsorb elsewhere after movement over
considerable distances in the vapour phase. This mechanism may account for some
examples of apparent surface diffusion reported by earlier workers. If,
however, this vapour phase transport is suppressed, then no evidence can be
detected of a true surface diffusion over macroscopic distances.
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