Abstract
The kinetics of the reaction between
manganese dioxide and ferrous ion in acid solution have been investigated by
using the potential of the ferrous-ferric couple as a measure of the extent of
reaction. The experimental conditions were such that the reaction rate was
independent of ferrous, ferric, manganous ions, and acid concentrations and the
agitation was sufficient to prevent bulk diffusion in the solution from being a
rate-determining factor.
The reaction rate of sized samples of
pyrolusite and γ-MnO2 in ferrous
sulphate solution was proportional to the surface area of the solid and was
constant (i.e. " zero-order ") until 50 per cent. of the solid was
consumed. γ-MnO2 reacted about twice
as rapidly as the pyrolusite. The reaction occurred most readily at certain
active sites on the particles and appeared to proceed along crystal boundaries
in such a manner that the active surface area was not significantly changed
during the first half of the reaction. In ferrous perchlorate the reaction rate
of 10 μ diameter pyrolusite was about one-hundredth of that in sulphate
and the reaction appeared to occur at a more even rate over the whole surface
of the particle so that the zero-order law was no longer obeyed. Activation
energies of 7.4 and 5 kcal in sulphate and perchlorate respectively, for the
temperature range 18 to 40 �C, suggest that the difference in rate is a result
of a change in the entropy factor of the Arrhenius equation. It is suggested
that this difference in rate may result from the activation, by sulphate ions,
of a less reactive lower oxide of manganese which is formed on the surface.
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