Opening-mode fractures developed from a free surface in a layered material
often terminate at the interface that divides the fractured layer and the u
nderlying layer. They also display regular spacing that is of the same orde
r of magnitude as the thickness of the fractured layer. We have investigate
d the stress distribution between two adjacent edge fractures as a function
of the ratio of fracture spacing to thickness of the fractured layer using
a two-layer elastic model with a fractured top layer. The results show tha
t when the ratio of fracture spacing to the layer thickness changes from gr
eater than to less than a critical value the normal stress acting perpendic
ular to the fractures near the free surface changes from tensile to compres
sive. This stress state transition precludes further infilling of fractures
unless they are driven by mechanisms other than a pure extension, or there
are flaws that significantly perturb the local stress field between the fr
actures. Hence, the critical fracture spacing to layer thickness ratio defi
nes a lower limit for fractures driven by extension, which also defines the
condition of fracture saturation. The critical value of the fracture spaci
ng to layer thickness ratio is independent of the average strain of the fra
ctured layer, and it increases with increasing ratio of Young's modulus of
the fractured layer to that of the underlying layer. The critical value inc
reases with increasing Poisson's ratio of the fractured layer, but it decre
ases with increasing Poisson's ratio of the underlying layer. For the case
with the same elastic constants for the fractured layer and the underlying
layer, the critical spacing to layer thickness ratio is about 3.1. Delamina
tion between the fractured layer and the underlying layer makes the critica
l spacing to layer thickness ratio much greater. Infilling fractures grow m
ore easily from flaws located near the bottom of the fractured layer than f
rom those located near the free surface when the spacing to layer thickness
ratio is less than the critical value. The propagation of an edge flaw bet
ween adjacent edge fractures is unstable, but for the flaw to propagate to
the interface, its height has to be greater than a critical size, that decr
eases with increasing fracture spacing to layer thickness ratio. The propag
ation behavior of an internal flaw with its lower tip at the interface depe
nds on the edge fracture spacing to layer thickness ratio. The propagation
is unstable, when the fracture spacing to layer thickness ratio is greater
than a critical value; stable, when the fracture spacing to layer thickness
ratio is less than another critical value; and first unstable, then stable
, and/or unstable again, when the fracture spacing to layer thickness ratio
is between these two critical values.