or
A = 1,742,400 / 43,560 = 40 acres
Matthews, Brons, and Hazebroek (1954) pointed out that once the
reservoir is producing under the semisteady-state condition, each well
will drain from within its own no-flow boundary independently of the
other wells. For this condition to prevail, the pressure decline rate dp/dt
must be approximately constant throughout the entire reservoir, other-
wise flow would occur across the boundaries causing a readjustment in
their positions. Because the pressure at every point in the reservoir is
changing at the same rate, it leads to the conclusion that the average
reservoir pressure is changing at the same rate. This average reservoir
pressure is essentially set equal to the volumetric average reservoir pres-
sure p
–
r
. It is the pressure that is used to perform flow calculations during
the semisteady state flowing condition. In the above discussion, p
–
r
indi-
cates that, in principal, Equation 6-128 can be used to estimate by replac-
ing the pressure decline rate dp/dt with (p
i
- p
–
r
)/t, or:
or
where t is approximately the elapsed time since the end of the transient
flow regime to the time of interest.
It should be noted that when performing material balance calculations,
the volumetric average pressure of the entire reservoir is used to calcu-
late the fluid properties. This pressure can be determined from the indi-
vidual well drainage properties as follows:
pp
qt
cAh
ri
t
=-
0 23396.
f
(6 -129)
Fundamentals of Reservoir Fluid Flow 407
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