Although it is recognized that the opening of fractures changes with changi
ng fracture spacing, it is a common practice to consider only the effects o
f loading and rock properties, and to assume that opening of all fractures
is independent of fracture spacing. Thus, one would expect that the more fr
actures contained in a rock mass, the greater the fluid flow tate. Using th
e cubic law and the Finite Element Method, we have investigated the volumet
ric flow rate through a number of equally-spaced fractures in a fractured r
ock layer as a function of the ratio of fracture spacing to layer thickness
, under a remote extension. Results show that there is an optimum value for
the ratio of fracture spacing to layer thickness that yields the maximum f
low rate. This value is independent of the fluid properties, the head gradi
ent, the applied extension, the internal fluid pressure and the overburden
stress.