The fracture of alpha iron and C-Mn submerged arc weld metal at temper
atures below the brittle-ductile transition temperature is examined. T
he probability of intergranular fracture occurring in a regime where c
leavage fracture is observed is considered with respect to simple theo
retical arguments that take into account the geometry of grains and th
e relative energy of the two fracture processes. The experimental obse
rvations are examined in relation to the predictions of these argument
s. Simple geometrical arguments demonstrate that a small proportion of
intergranular fracture is expected to accompany cleavage fracture in
most specimens of polycrystalline alpha iron and ferritic steels fract
ured at temperatures below the brittle-ductile transition temperature.