Fluid flow in rock fractures: From the Navier-Stokes equations to the cubic law

The mathematical analysis of the flow of a single-phase Newtonian fluid through a rough-walled rock fracture is reviewed, starting with the Navier-Stokes equations. By a combination of order-of-magnitude analysis, appeal to available analytical solutions, and reanalysis of some data from the literature, it is shown that the Navier-Stokes equations can be linearized if the Reynolds number is less than about 10. Further analysis shows that the linear Stokes equations can be replaced by the simpler Reynolds lubrication equation if the wavelength of the dominant aperture variations is about three times greater than the mean aperture. However, this criterion does not seem to be strongly obeyed by all fractures. The Reynolds equation (i.e., the local cubic law) may therefore suffice in estimating fracture permeabilities to within a factor of about 2, but more accurate estimates will require solution of the Stokes equations. Similarly, estimates of mean aperture based on inverting transmissivity data may have errors of a factor of two if any version of the local cubic law is used to relate transmissivity to mean aperture.

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