The aperture (or opening) of a fracture indicates the energy available
for fracture growth and controls fracture permeability. The relations
hip between aperture and fracture length can therefore be used to infe
r the factors affecting fracture formation at different length scales
and is of practical importance to hydrogeologists and petroleum engine
ers. A recent study(1) of the scaling properties of tensile fractures
in the Krafla fissure swarm, Iceland, revealed a distinct break in slo
pe in the aperture-length scaling relationship, corresponding to fract
ures a few metres in length: this break in slope was interpreted quali
tatively as indicative of non-universal, scale-dependent growth mechan
isms(1), Here we show, using quantitative fracture simulations, that t
he observed non-universal scaling of fracture apertures can be reprodu
ced without recourse to multiple growth mechanisms. We argue that the
break in slope is instead intrinsic to the fracturing process and repr
esents the maximum length scale at which the apertures of smaller frac
tures are affected by stress perturbations induced by larger fractures
.