Abstract

The electrical conductivity of a series of iron-cobalt molybdates has been measured at 370°C, as a function of the iron content. An important increase of the electrical conductivity occurred when small amounts of iron were substituted for cobalt. This takes place because iron is partially in the 3+ oxidation state. This species, which is stabilized into the CoMoO 4 structure, creates a valence induction effect which is responsible for the drastic variation of the electrical conductivity with compounds whose iron content ranges from 0 to 20%. UV spectroscopy allows us to propose that the ferric species involved in this valence induction phenomenon are those giving rise to the intervalence charge transfer between iron cations (Fe 2+-O-Fe 3+). By contrast, ESR spectroscopy is silent for such a phenomenon (too short relaxation time) and shows two typical Fe 3+ ( d 5 ion) spectra for Fe 3+ engaged either in a different manner in the solid solution (strongly distorted octahedral site) or a given compound such as Fe 2(MoO 4) 3 observed at high iron content.

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