A model for nickel-iron electrodeposition from a sulfate bath onto a relating disk electrode based on an alternate description of electrode kinetics from that most commonly used has been presented and analyzed. The reaction mechanism in this model differs in that Ni2+ and Fe2+ are the electroactive species and NiOH+ and FeOH+ are not involved whatsoever. Transport of each dissolved species is considered to occur via diffusion, convection, and migration. Comparison of simulations with experimental data shows that our model can predict characteristic features of the nickel-iron system, such as anomalous codeposition and the occurrence of a maximum in iron content in the deposit at intermediate currents, at least as well as the earlier models. Furthermore, the computed changes in surface pH are in good agreement with experimental near-surface pH measurements reported in the literature and much too low for NiOH+ and FeOH+ to be present in significant amounts. Some approaches for future work for elucidating the reaction mechanism and distinguish between the various alternatives are discussed.