Abstract
It has been shown that a number of
sulphides and oxides of multivalent metals can be intercalated in graphite. The
results of this investigation support the conclusion, reached in Part II of
this series (Croft 1956a), that the electronic configuration of the cation of a
compound determines the possibility of its intercalation, and that the nature
of the anion has little significance. As in the case of chlorides reported in
Part I of this series (Croft 1956b), the cations of intercalated sulphides and
oxides are in higher valence states.
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