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Martensite in Steels - Department of Materials Science and Metallurgy

Martensite in Steels - Department of Materials Science and Metallurgy

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at low temperatures, it need not do so. Therefore, a low transformation temperature is notsufficient evidence for diffusionless transformation.<strong>Martensite</strong> plates can grow at speeds which approach that <strong>of</strong> sound <strong>in</strong> the metal. In steelthis can be as high as 1100 m s −1 , which compares with the fastest recorded solidification frontvelocity <strong>of</strong> about 80 m s −1 <strong>in</strong> pure nickel. Such large speeds are <strong>in</strong>consistent with diffusiondur<strong>in</strong>g transformation. Note that martensite need not grow so rapidly. For example, <strong>in</strong> shape–memory alloys or <strong>in</strong> s<strong>in</strong>gle–<strong>in</strong>terface transformations, the <strong>in</strong>terface velocity is small enough toobserve.The chemical composition <strong>of</strong> martensite can be measured <strong>and</strong> shown to be identical tothat <strong>of</strong> the parent austenite. The totality <strong>of</strong> these observations demonstrate conv<strong>in</strong>c<strong>in</strong>gly thatmartensitic transformations are diffusionless.The Habit PlaneThis is the <strong>in</strong>terface plane between austenite <strong>and</strong> martensite as measured on a macroscopicscale (Fig. 1), for example by us<strong>in</strong>g one or two–surface crystallographic trace analysis onmetallographic samples. For unconstra<strong>in</strong>ed transformations this <strong>in</strong>terface plane is flat, butstra<strong>in</strong> energy m<strong>in</strong>imisation <strong>in</strong>troduces some curvature when the transformation is constra<strong>in</strong>edby its surround<strong>in</strong>gs. Nevertheless, the macroscopic habit plane is identical for both cases, asillustrated <strong>in</strong> Figure 1.Figure 1: An illustration <strong>of</strong> the habit plane between austenite (γ) <strong>and</strong> martensite(α ′ )2

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