Standard Potential of the Ferric–Ferrous Couple

E(Fe3+/Fe2+)=0.771 VE^{\circ}(\mathrm{Fe^{3+}}/\mathrm{Fe^{2+}}) = 0.771\ \text{V}
Value0.771 V
StatusMeasured: ± 0.001 V (0.0013 relative)
SourceCRC Handbook
CategoriesChemistryelectrochemistry
E°(Fe³⁺/Fe²⁺) in every voltage unit
microvolt771,000 μV
millivolt771 mV
volt0.771 V
kilovolt0.000771 kV

Learning zone

The ferric–ferrous couple is the redox equivalent of a pH indicator for natural systems. At +0.771 V it sits in the middle of the range that groundwater, sediments and soils actually occupy, so whether iron is present as soluble Fe²⁺ or insoluble Fe(OH)₃ tells you immediately whether an environment is oxidising or reducing. Anoxic well water carries clear Fe²⁺ that oxidises and turns orange within minutes of reaching the tap.

The couple is also fast and reversible, which makes it a favourite in analytical chemistry: the ceric–ferrous titration and the ferroin indicator both depend on it, and iron is a common mediator in electrochemical and biological electron transport chains. Note the potential shifts strongly with complexation — bind the iron with EDTA or cyanide and the ferricyanide/ferrocyanide couple drops to +0.358 V, a reminder that a standard potential describes a specific chemical species and not simply an element.