“…Following Jaeger [3], McDowell [4] measured the tensile strength of sand grains by diametral compression between flat platens as σ = F / d 2 , and showed that the stresses at failure for a given particle size satisfied a Weibull distribution of strengths. These distributions were described by a characteristic value of strength, σ0 and a Weibull modulus, m. In PFC3D, the value of octahedral shear stress, q induced in a particle compressed diametrically between two walls is proportional to F / d 2 [2]; hence, McDowell and de Bono [1] assumed that for a particle under multiple contacts, the particle would break if the octahedral shear stress was greater than or equal to its strength, where the strengths of the particles satisfy a Weibull distribution of q values.…”