Abstract
Fracture-mechanism maps are diagrams with tensile stress as one axis and temperature as the other, showing the fields of dominance of a given micromechanism of fracture: cleavage, ductile fracture, rupture, intergranular creep fracture, and so on. Superimposed on the fields are contours of constant time-to-fracture. They can be constructed in either of two ways: empirically, by assembling observations and data for the fracture of a given material; or theoretically, via models for the individual fracture mechanisms. The first approach is developed here.
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