Serrated yielding was observed between 500 and 775°K in alloys of iron which exhibited marked solid-solution hardening. The serrations result from the formation of bands of localized deformation. In a soft machine where the applied load remains constant, the band spreads immediately over the entire gauge length. In a hard machine the burst of strain associated with the formation of the band causes the load to drop, so that the spreading of the band front stops when the applied stress falls below a critical level. During reloading, aging of the dislocations in the band front occurs. At low temperatures where little aging occurs during reloading, the band front propagates along the gauge length with only small undulations in load. At higher temperatures, where aging is more rapid, the band front becomes pinned during reloading and can move only by breaking away. Alternate aging and breakaway recurs as the band front propagates along the gauge length, producing regular serrations on the load-extension curve, and surface markings on the specimen. The serration height Δθ increases with increase in reloading time, t, and temperature, T, according to Δθ = A + B log Z, where A and B are constants and Z = t exp ( −Q RT ) . The apparent activation energy for appearance and growth of serrations, Q, is about half the activation energy for diffusion of a substitutional atom in iron. The negative results of vacancy annealing experiments, and failure of the critical strain criterion indicate that the apparent high diffusivity is not due to deformation-induced vacancies. Rather, the results suggest that pinning of dislocations is due to a redistribution or reorientation of solutes or solute clusters in dislocation cores. At the upper critical temperature, which is dependent on strain rate, the growing serrations abruptly disappear. The critical rate appears to be that which just allows one lattice jump of the solute between serrations. The apparent activation energy associated with disappearance is near that for lattice diffusion of solutes in iron.
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