Strengthening mechanisms and dislocations
As precipitates grow during aging, the strength rises to a maximum and then falls (overaging). Which is the correct explanation in terms of the interaction between precipitates and dislocations? Take the volume fraction of precipitates as constant.
- ASmall precipitates are bypassed by dislocations and larger ones come to be sheared, and the stress needed to shear them increases as the spacing between precipitates widens
- BSmall precipitates are sheared by dislocations with a resistance that grows with their size, but larger ones are passed by dislocations bowing out between them, at a stress that falls as the spacing widens
- CPrecipitates of every size are sheared, and as they grow their coherency with the matrix increases so the shearing resistance keeps rising, while the maximum strength is set by the loss of solid-solution strengthening
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Answer: B. Small precipitates are sheared by dislocations with a resistance that grows with their size, but larger ones are passed by dislocations bowing out between them, at a stress that falls as the spacing widens
The small, coherent precipitates of early aging are sheared and passed through by dislocations. The resistance to shearing comes from the work of creating coherency strain, new interface and, for ordered phases, an antiphase boundary, and at a constant volume fraction it increases as the precipitates grow. Once precipitates become large, it becomes easier for dislocations to bow out between them and pass, leaving loops (the Orowan mechanism), and that stress is inversely proportional to the precipitate spacing, so it falls as the particles coarsen. The strength peaks at the size where the two mechanisms change over, which corresponds to peak aging. The option with the order of bypassing and shearing reversed is wrong. Precipitates tend to lose coherency with the matrix as they grow, so the option in which coherency increases is also wrong.
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