
APPENDIX E
Equations of Motion for Porous Media
E.1 RECTANGULAR COORDINATES
The following forms of the x-, y-, and z-components of the equations of motion
in rectangular coordinates for flow through porous media are based on Brinkman’s
empirical modification of Darcy’s law and assume a body force due to a grav-
itational field, and an incompressible fluid having constant viscosity μ and per-
meability k
p
;theu
i
denote the components of the superficial velocity based on
considering a porous medium to be homogeneous
1
:
0 =−
∂P
∂x
−
μ
k
p
u
x
+ μ
∂
2
u
x
∂x
2
+ μ
∂
2
u
x
∂y
2
+ μ
∂
2
u
x
∂z
2
+ ρg
x
(E.1-1)
0 =−
∂P
∂y
−
μ
k
p
u
y
+ μ
∂
2
u
y
∂x
2
+ μ
∂
2
u
y
∂y
2
+ μ
∂
2
u
y
∂z
2
+ ρg
y
(E.1-2)
0 =−
∂P
∂z
−
μ
k
p
u
z
+ μ
∂
2
u
z
∂x
2
+ μ
∂
2
u
z
∂y
2
+ μ
∂
2
u
z
∂z
2
+ ρg
z
(E.1-3)
E.2 CYLINDRICAL COORDINATES
The following forms of the r-, θ-, and z-components of the equations of motion
in cylindrical coordinates for flow through porous media are based on Brinkman’s
empirical modification of Darcy’s law and assume a body force due to a grav-
itational field, and an incompressible fluid having constant viscosity μ and per-
meability k
p
;theu
i
denote the components of the superficial velocity based on
considering a porous medium to be homogeneous
2
:
0 =−
∂P
∂r
−
μ
k
p
u
r
+ μ
∂
∂r
1
r
∂
∂r
(ru
r
)
+ μ
1
r
2
∂
2
u
r
∂θ
2
− μ
2
r
2
∂u
θ
∂θ
+ μ
∂
2
u
r
∂z
2
+ ρg
r
(E.2-1)
1
H. C. Brinkman, Appl.Sci.Res., A1, 27–34, 81–86 (1947).
2
Ibid.
Scaling Analysis in Modeling Transport and Reaction Processes: A Systematic Approach
to Model Building and the Art of Approximation, By William B. Krantz
Copyright © 2007 John Wiley & Sons, Inc.
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