“…They found that by promoting more dispersed slip, or by grain refinement the intergranular fracture mode can be replaced by the conventional ductile rupture in which void formation and shear banding became more pronounced than grain boundary decohesion. Practically, several possible sources of intergranular fracture can be delineated: (i) reduction in the local cohesive stress due to segregation or presence of grain boundary particles, (ii) initiation, growth and coalescence of micro-voids, formed on the grain boundary particles, (iii) localization of the deformation in precipitation free zones (PFZs) adjacent to the grain boundaries, (iv) promotion of coarse slip in the bulk of the grains, and (v) coarsening of the grain size [5,[7][8][9].…”