Willis-Richards Permeability Model

Overview

In the Willis-Richards permeability model, the stress-aperture relationship is derived based on Barton–Bandis constitutive model. In this model, fracture hydraulic aperture is assumed to be a function of effective normal stress acting on the fracture surface and shear displacement along the fracture surface (Willis-Richards et al., 1996).

a = \frac{ a_{m} + U_{s} \text{tan} \left( \phi_{dil} \right) }{ 1 + 9 \frac{ \sigma_{n} }{ \sigma_{ref} }}

Based on the assumption of parallel plates, the correlation between fracture hydraulic aperture and its corresponding permeability is defined as:

k =  \frac{a^2}{12}

where

a is the fracture hydraulic aperture; a_{m} is the fracture aperture at zero contact stress; U_{s} is the relative shear displacement; \phi_{dil} is the shear dilation angle; \sigma_{n} is the effective normal stress acting on the fracture surface; \sigma_{ref} is the effective normal stress that causes a 90% reduction in the fracture hydraulic aperture.

Parameters

The Willis-Richards permeability model is called in the <Constitutive> block of the input XML file. This permeability model must be assigned a unique name via the name attribute. This name is used to attach the model to regions of the physical domain via a permeabilityModelName attribute in the <CompressibleSolidWillisRichardsPermeability> block.

The following attributes are supported:

Name

Type

Default

Description

dilationCoefficient

real64

required

Dilation coefficient (tan of dilation angle).

maxFracAperture

real64

required

Maximum fracture aperture at zero contact stress.

name

groupName

required

A name is required for any non-unique nodes

refClosureStress

real64

required

Effective normal stress causes 90% reduction in aperture.

Example

<Constitutive>
   ...
   <WillisRichardsPermeability
     name="fracturePerm"
     maxFracAperture="0.005"
     dilationCoefficient="0.01"
     refClosureStress="1.0e7"/>
   ...
</Constitutive>