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
@σ
xx
@
x
1
@τ
y
1
@τ
zx
dm
@
u
@
u
@
u
v
@
u
@
w
@
u
yx
ρ
g
x
5
t
1
x
1
y
1
@
@
z
@
@
z
dxdydz
1
@τ
x
1
@σ
y
1
@τ
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
@τ
yz
1
@τ
y
1
@σ
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
@σ
x
1
@τ
yx
y
1
@τ
@
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
@τ
xy
@
x
1
@σ
yy
y
1
@τ
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
@τ
xz
@
x
1
@τ
y
1
@σ
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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