Two cumulative ‘size’ effects are responsible for the increased strength of a polycrystalline aggregate above the single crystal strength at low temperatures : a ‘specimen size’ effect and a ‘grain size’ effect. The ‘specimen size’ effect occurs when few grains are present in a specimen cross-section (say less than twenty), and this effect is due mainly to the orientation dependence of crystal plastic flow. The ‘grain size’ effect occurs when many grains are in a specimen cross-section (say more than twenty), and this effect results because, in addition to the orientation dependence of plastic flow within grains, internal concentrations of stress are necessary at grain boundaries to cause bulk yielding and subsequent plastic flow of the polycrystalline aggregate.
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