Abstract
A naturally fractured reservoir is characterized as a system of matrix blocks
with each matrix block surrounded by fractures. The fluid drains from the
matrix block into the fracture system which is interconnected and leads to the
well. Warren and Root(1) introduced a mathematical model for this
dual porosity matrix-fracture behaviour.
Their model has been widely used for many types of reservoirs, including tight
gas and coalbed methane reservoirs. A key part of their model is a geometrical
parameter (shape factor) which controls the drainage rate from the matrix to
the fractures. Although Warren and Root gave formulas for calculating shape
factors, many other authors have presented alternate formulas, leading to
considerable confusion.
In addition to the size and shape of a matrix element, two cases are considered
by the authors: constant drainage rate from a matrix block and constant
pressure in the adjacent fractures.
The current work confirmed the correct formulas for shape factors by using
numerical simulation for the various cases. It was found that some of the most
popular formulas do not seem to be correct. A summary of the correct shape
factor formulas is presented.
Introduction
Naturally fractured reservoirs can be characterized as a system of fractures in
very low conductivity rock. The mathematical formulation of this 'dual
porosity' or 'double porosity' system of matrix blocks and fractures was
presented by Barenblatt et al.(2) The first system is a fracture
system with low storage capacity and high fluid transmissibility and the second
system is the matrix system with high storage capacity and low fluid
transmissibility. The matrix rock stores almost all of the fluid, but has such
low conductivity, that fluid just drains from the matrix 'block' into adjacent
fractures, as is shown in Figure 1. The fractures have relatively high
conductivity, but very little storage.
The drainage from the matrix to the fractures for dual porosity reservoirs was
idealized by Warren and Root(1) according toEquation (1).
Equation 1 (available in full paper)
Equation (1) is in the form of pseudosteady-state flow which means that early
transient effects have been ignored. Pseudosteady-state also means that the
drainage rate is constant. The units of Equation (1) are volume rate of fluid
drainage per volume of reservoir. The units of the shape factor, s, are
1/L2.
For dual porosity reservoirs, when pressure test analyses are available, the
product σ - km can be determined using Equation (2), but cannot be
separated.
Equation 2 (available in full paper)
The interporosity flow coefficient, λ, determines the interrelation between
matrix blocks and the fracture system. When km is available from
core or log analysis, then shape factor, σ, can be estimated. For cases where
pressure test analyses are not available, formulas can be used to estimate
shape factor. However, there are conflicting equations and values for σ in the
literature.
Many authors have interpreted Equation (1) to be the equivalent long-term
reservoir drainage equation with pf held constant and drainage rate
changing with time.
© 2009. Petroleum Society of Canada (now Society of Petroleum Engineers)
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History
- Original manuscript received:
29 March 2006
- Meeting paper published:
13 June 2006
- Revised manuscript received:
10 June 2008
- Manuscript approved:
19 December 2008
- Version of record:
1 February 2009