Abstract
Precipitation and dehydration has produced a series of cobalt–iron oxides CoxFe3–xO4(0 ⩽x⩽ 3) whose surfaces at intermediate x show only marginal iron enrichment and which are useful precursors to ammonia synthesis catalysts. With increasing x activation energies for electrical conduction increase but surface areas estimated by adsorption of N2, H2O and n-hexane decrease (and are significantly different for three adsorbates, SHC < SN2 < SH2O , reflecting increasing surface–adsorbate specific interactions). Even for n-hexane enthalpies of adsorption are stronger than expected from mere physical adsorption.

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