Abstract
Experimental results given in Part I of
this series (Croft 1956a) have been examined theoretically with particular
attention given to finding reasons for the specificity shown by graphite
towards various chlorides. This specificity cannot be accounted for in terms of
"molecular sieving" or polar interaction. It is suggested that
intercalation involves transfer of electrons from the conducting band of
graphite to cations of reactive chlorides.
Intercalation of transition metal
chlorides can be correlated with possession of unsaturated penultimate electron
shells by the cations concerned. However, correlation is only complete when the
cations exhibit maximum electron affinities, as in their higher valence states.
Reaction of Group IIIA chlorides appears
due to accommodation of electron pairs from the π band of graphite in n(p)
orbitals (or their hybrids) of the cations. The distinctive hydrolysis of these
chlorides in situ indicates that graphite is a weaker donor than water.
Similar consideration of unreactive
chlorides indicates that they are not intercalated because their cations are
incapable of electronic interaction with graphite.
Several important conclusions, supported
experimentally in Parts III and IV of this series (Croft 1956b, 1956c), have
been drawn from these theoretical considerations. Firstly, since intercalation
depends on electronic configurations of cations, any compound containing a
suitable cation should be capable of intercalation in graphite irrespective of
the anion associated with it. Secondly, provided they satisfy two conditions,
other substances should be capable of intercalating foreign compounds in a
similar manner to graphite. The necessary conditions are that a host substance
is able to interact electronically with an intercalated substance, and that it
must afford physical accommodation for the latter.
The potential value of graphite reactions,
in elucidating fundamental problems, is also discussed.
Cited by
13 articles.
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