Biomedical Engineering Reference
In-Depth Information
For this formulation, gravity does not need to align with a particular Cartesian direc-
tion. Substituting Equation 3.57 into Equation 3.55 and writing it in terms of vector compo-
nents gives us
dxdydz
1 xx
@
x 1
y 1 zx
dm @
u
@
u @
u
v @
u
@
w @
u
yx
ρ
g x
5
t 1
x 1
y 1
@
@
z
@
@
z
dxdydz
1
x 1
y 1
dm @
v
@
u @
v
@
v @
v
w @
v
xy
yy
zy
ρ
g y
5
t 1
x 1
y 1
@
@
@
z
@
@
z
dxdydz
x 1 yz
1
y 1
dm @
w
@
u @
w
@
v @
w
@
w @
w
@
xz
zz
ρ
g z
5
t 1
x 1
y 1
@
@
@
z
z
Using the relationship that dm
5 ρ
dV
5 ρ
dxdydz , the equations of motion become
g x 1
x 1 yx
y 1
@
u
@
u @
u
v @
u
w @
u
@
Du
Dt
xx
zx
ρ
5 ρ
5 ρ
t 1
x 1
y 1
@
@
@
z
@
@
z
g y 1 xy
@
x 1 yy
y 1 zy
@
v
@
u @
v
v @
v
w @
v
Dv
Dt
ρ
5 ρ
5 ρ
ð
3
:
58
Þ
t 1
x 1
y 1
@
@
z
@
@
@
z
g z 1 xz
@
x 1
y 1 zz
@
w
@
u @
w
@
v @
w
@
w @
w
@
Dw
Dt
yz
ρ
5 ρ
5 ρ
t 1
x 1
y 1
@
@
z
z
Equation 3.58 is the differential equations of motion, which are valid for any fluid that
is a continuum and for any fluid that has the force of gravity as the only body force. In
Chapter 2, we defined the normal stress as a function of hydrostatic pressure and the
shear stresses as a function of viscosity and shear rate (which is a function of velocity).
The following definitions apply:
2
3 μr U
μ @
u
-
σ
p
2
52
2
1
xx
@
x
2
3 μr U
μ @
v
-
σ
p
2
52
2
1
yy
@
x
2
3 μr U
μ @
w
@
-
σ zz 52
p
2
2
1
x
ð
3
:
59
Þ
@
u
y 1 @
v
τ xy 5 τ yx 5 μ
@
@
x
@
u
@
z 1 @
w
@
τ xz 5 τ zx 5 μ
x
@
v
z 1 @
w
@
τ
5 τ
5 μ
yz
zy
@
y
where
r
is the gradient operator and is defined as
5 @
f
1 @
f
1 @
f
x -
y -
z -
r
f
@
@
@
where f is any function in the Cartesian coordinate system (note that the gradient function
can be calculated in any coordinate system for any function; we are just highlighting the
Cartesian coordinate system for this analysis).
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