Abstract

The kinetics of dissociation of several iron(II) diimine complexes by aqueous hydroxide ions have been studied spectrophotometrically at atmospheric pressure and elevated pressures, at 298.2 K. Values of Δ V * are between + 10 and + 16 cm 3 mol −1, and are interpreted as arising from a significant loss of electrostricted water from the hydroxide ion as it reacts with the iron(II) complex associatively. Dissociation of the [Fe(5NO 2phen) 3] 2+ and [Fe(5Brphen) 3] 2+ complexes in the presence of aqueous EDTA is reported. For both, Δ V * is + 22 cm 3 mol −1. These values can be understood by considering the reaction as a process comparable to aquation in acidic medium, a dissociative process. Activation enthalpy data support this idea.

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