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The equicohesive temperature is an antiquated term for the temperature at which the cohesion (the strength) of the grain boundaries in a crystal (usually a metal) becomes equal to that of the crystalline interior. In practice, it is the temperature at which a transition from an intergranular to transgranular (cleavage)-type fracture is observed. Over time, the concept of the equicohesive temperature has been replace be a more nuanced understanding of the various possible deformation mechanisms possible in polycrystals, with low-temperature, intergranular fracture and transgranular cleavage being only two such examples.

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Q: What is meant by equi-cohesive temperature?
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