Abstract
The thermal decomposition of precipitated
silver(I) oxide in a vacuum has been studied over the range 100-350 �C. Three
regions are identified : in the fist, 100-200 �C, the activation energy is 30
kcal, 5 per cent. of the total oxygen is evolved, and the lattice parameter
increases to a limiting value ; in the second, 200-300 �C, the activation
energy is 50 kcal, and a further 1-2 per cent. oxygen is evolved; in the third,
above 300 �C, metallic silver crystallizes, the oxide lattice contracts to a constant
value, and the activation energy becomes 36 kcal. The activation energies in
the three regions are interpreted as being associated, respectively, with (i)
the diffusion of silver into the oxide lattice, (ii) the formation of
aggregates of silver " atoms " not conforming to the normal silver
lattice in an oxide lattice saturated with silver, and (iii) the reaction at
the interface between metallic silver and the oxide.
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