cee 262a h ydrodynamics lecture 5 conservation laws part i 1
TRANSCRIPT
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CEE 262A
HYDRODYNAMICS
Lecture 5
Conservation Laws Part I
1
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Conservation laws
VA
The ultimate goal is to use Newton's 2nd law (F=ma) to relateforces on fluid parcels to their acceleration. A natural way to do this is to compute the equations of motion following a volume of fluid; We first begin with the governing equations for a solid, non-deformable object with volumeV, surface area A, and density
Mass of object:
Momentum of object: V
dVuP~~
V
dVm
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Newton's 2nd law for the object is given by:
bodysurface
V
FFdVudt
dtP
dt
dF
~~~~~)(
Surface forcese.g. Friction
Body forcese.g. Gravity
Example: Block of mass m pushed with force F along surface with friction coefficient b
0
3
~
3
~
1
~
1
~
~
3
~
3
~
1
~
1
~~
~~~
mgNdt
dwm
Fbudt
dum
amgaNaFabudt
udm
dVagaNaFabudVudt
d
FFdVudt
d
Body
VSurface
V
bodysurface
V
F
m
N
g
u
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),(),(),()(
)(
taFdt
datbF
dt
dbdx
t
FdxtxF
dt
d b
a
tbx
tax
Which in 3D becomes:
~ ~ ~( ) ( ) ( )
( , )A
V t V t A t
d FF x t dV dV F u n dA
dt t
velocity of boundary
The problem for fluids is that the volume is generally not fixed in time, and so mass and momentum may leave the volume unless a material volume is employed.
The key to understanding what to do is Leibniz's Theorem:
Consider a volume V(t) for which the bounding surface moves (but not necessarily at the fluid velocity)
u
n
dA
( )A t( )V t
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Fixed volume–VF : Flow of fluid through system boundary (control surface) is non zero, but velocity of boundary is zero. For this case we get
Material Volume–VM : Consists of same fluid particles and thus the bounding surface moves with the fluid velocity. Thus, the second term from the Leibnitz rule is now non-zero, so
Using Gauss' theorem:
~( , )
F FV V
d FF x t dV dV
dt t
~ ~ ~( , )
M MV V A
D FF x t dV dV F u n dA
Dt t
~ ~ ~
MA V
F u n dA F u dV
~ ~
( , )M MV V
D FF x t dV F u dV
Dt t
This is Reynolds transport theorem, where D/Dt is the same as d/dt but implies a material volume.
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~~
Note that the Reynolds transport theorem is often written in themore general form which does not assume that the control volumeis bounded by a material surface. Instead, the control volume isassumed to move at some velocity and that of the fluid is
defined as relative to the control volume, such that
In this case, V is not necessarily a material surface. If ur=0, thenub=u and we revert to the form on the previous page.
A
rA
bVV
dAnuFdAnuFdVt
FdVtxF
Dt
D~~~~~
),(
bu~
bruuu~~~
~
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n
dA
( )A t( )V t
The general form of all conservation laws that we will use is:
Rate of change of F = effects of volume sources + effects of surface sources
M MV V A
DF dV D dV C n dA
Dt
Quantity (F) Volume sources (D) Surface sources (C)
Momentum1 Gravity Stresses (pressure/viscous)
Heat Dissipation Diffusion/radiation
Salt (scalar) None Diffusion
Algae (e.g.) Growth Diffusion
1 Note: momentum is a vector quantity
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Conservation of Mass
~
0M MV V
DdV u dV
Dt t
Mass is conserved (non-relativistic fluid mechanics)
For any arbitrary material volume
Since integral is zero for any volume, the integrand must be zero
~
0ut
Process: We have taken an integral conservation law and used it to produce a differential balance for mass at any point
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0
~
ii
i
i
ii
i
ii
i
xu
x
u
t
xu
x
uu
xu
However,
andi
i
Du
Dt t x
~
1 Du
Dt
Thus if the density of fluid particles changes, the velocity field must be divergent. Conversely, if fluid densities remain constant,
~0u
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Let where is an intensive property (amount/mass)F f f
dVx
fuu
xf
t
f
tf
dVfux
ft
dVfDt
D
M
MM
V iii
i
V
iiV
)(
)()(
dVDt
Df
dVx
fu
t
fu
xt
M
M
V
V iii
i
0)(But
dVDt
DfdVf
Dt
D
MM VV
Any other fluid property (scalar, vector,.. also drop triple integral)
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Why is this important/useful?
Because Newton’s 2nd law:
dVDt
uDdVu
Dt
D
MM VV ~
~
dVFdVuDt
D
MM VV
~~
Dt
uDF ~
~
But from above:
Rate of Change of Momentum = Net Applied Force
Net Applied Force = Mass AccelerationIndependent of volume type!
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Some Observations
1. Incompressible
~
1u
Dt
D
01
Dt
D
[ No volumetric dilatation, fluid particle density conserved]
0~
i
i
x
uu
Differential form of “Continuity”
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2. Slightly Compressible
• Typically found in stratified conditions where
0( , , , ) ( ) '( , , , )x y z t z x y z t
• Boussinesq Approximation
- Vertical scale of mean motion << scale height
- or0
'1
Allows us to treat fluid as if it were slightly incompressible
Note: Sound and shock waves are not included !
Reference density (1000 kg/m3 for water)
Background variation (typ. 1-10 kg/m3 for water)
Perturbation density due to motion (typ.
0.1-10 kg/m3 for water)
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Informal “Proof”
2dPc dP c d
d
If a fluid is slightly compressible then a small disturbance caused by a change in pressure, , will cause a change in density . This disturbance will propagate at celerity, c.d
dP
• If pressure in fluid is “hydrostatic”
2
dP d gg
dz dz c
Now
and
d d dz
dt dz dt
wdt
dz [ Streamline curvature small]
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2c
gw
dt
d
2
1
c
gw
dt
d
Typically: g ≈10 m/s2 ; c ≈ 1500 m/s ; w ~ 0.1m/s
0~ u
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Conservation of Momentum – Navier-Stokes
We have:
~ ~
~ ~
Du uF u u
Dt t
Two kinds of forces:
• Body forces
• Surface forces
Two kinds of acceleration:
• Unsteady
• Advective (convective/nonlinear)
Two kinds of surface forces:
• Those due to pressure
• Those due to viscous stressesDivergence of Stress Tensor
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Plan for derivation of the Navier Stokes equation
1. Determine fluid accelerations from velocities etc. (done)
2. Decide on forces (done)
3. Determine how surface forces work : stress tensor
4. Split stress tensor into pressure part and viscous part
5. Convert surface forces to volume effect (Gauss' theorem)
6. Use integral theorem to get pointwise variable p.d.e.
7. Use constitutive relation to connect viscous stress tensor to strain rate tensor
8. Compute divergence of viscous stress tensor (incompressible fluid)
9. Result = Incompressible Navier Stokes equation
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Forces acting on a fluid
a) Body Forces: - distributed throughout the mass of the fluid and are expressed either per unit mass or per unit volume
- can be conservative & non-conservative
~g
Force potential
Examples:
(1) force due to gravity (acts only in negative z direction)
(2) force due to magnetic fields
gz
We only care about gravity
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b) Surface forces: - are those that are exerted on an area element by the surroundings through direct contact
- expressed per unit of area
- normal and tangential components
dA
ndF
sdF
~dF
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c) Interfacial forces:
- act at fluid interfaces, esp. phase discontinuities (air/water)
- do not appear directly in equations of motion (appear as boundary conditions only)
- e.g. surface tension – surfactants important
- very important for multiphase flows (bubbles, droplets,. free surfaces!)
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Very important deviation from text!!!
CEE262a (and most others)
Deviatoric (viscous) stress
Full stress
Kundu and Cohen
Full stress
Deviatoric (viscous) stress
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Stress at a point(From K&C – remember difference in nomenclature,i.e. ij ←ij)
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What is the force vector I need to apply at a face defined by theunit normal vector to equal that of the internal stresses?
~n
Consider a small (differential) 2-D element
1
2
11
12
1112
21
21
22
22
11
12
2122
n
1n
2n
1dx
2dx ds
dF
cut away
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1 11 2 21 1 F dx dx force component in x1 direction
1 2 11 11 21
11 1 21 2
11 1 21 2~
cos cos
dF dx dxf
ds ds ds
n n n[ has magnitude of 1]
Defining the stress tensor to be ij
11 12 13
21 22 23
31 32 33
And in general
jjjj nfandnf 2211
jjii nf
d
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But [see Kundu p90]ijji
or
or (3D)
ii ij j
total
CS
dFf n
ds
dFf n
ds
dFf n F n dA
dA
“ Surface force per unit area”(note this is a 2D area)
Total, or net, force due to surface stresses
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Conservation of momentum
2),( 1
1
112111
dx
xxx
2),( 1
1
112111
dx
xxx
2),( 2
2
212121
dx
xxx
2),( 2
2
212121
dx
xxx
1x
2x
3x
2),( 3
3
312131
dx
xxx
2),( 3
3
312131
dx
xxx
Dimensions:dx1 . dx2 . dx3
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Sum of surface forces in x1 direction:
11 1 11 111 11 2 3
1 1
21 2 21 221 21 1 3
2 2
31 3 31 331 31 1 2
3 3
3111 211 2 3
1 2 3
2 2
2 2
2 2
ji
j
dx dxdx dx
x x
dx dxdx dx
x x
dx dxdx dx
x x
dx dx dxx x x
dVx
Defining i component of surface force per unit volume
to be iVF
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~For body forces we use gravity = ig g
~gF
Dt
DuV
i
In general :
iV ij
j
Fx
j
iji
i
xg
Dt
Du
“Cauchy’s equation of motion”
Force = divergence of stress tensor
3
Note that usually
-g g e
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Important Note: This can also be derived from the Integral From of Newton’s 2nd Law for a Material Volume VM
A jijV iV i dAdVgdVu
Dt
DMM
MM V
i
V i dVDt
DudVu
Dt
D But
and [Gauss' Theorem]M
ijij jA V
j
dA dVx
0M
ijiiV
j
Dug dV
Dt x
ijii
j
Dug
Dt x
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Constitutive relation for a Newtonian fluid“Equation that linearly relates the stress to the rate of
strain in a Newtonian Fluid Medium”
(i) Static Fluid: - By definition cannot support a shear stress
- still feels thermodynamic pressure
(in compression)
ij ijp
(ii) Moving Fluid: - develops additional components of stress
(due to viscosity)ij ij ijp Hypothesis
Note difference from Kundu !
Deviatoric stress tensor [Viscous stress tensor]ij
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If medium is isotropic and stress tensor is symmetric
only 2 non-zero elements of
ij ij mm ij2 e e
Assume mnijmnij eK
ijmnK 4th order tensor (81 components!) that depend on thermodynamic state of medium
K
which gives
or
ijijij eup 2)ˆ3
2(
See derivation of in Kundu, p 100
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Special cases
(i) Incompressible 0ˆ u
ijijij ep 2
(ii) Static 0 ije
ijij p
In summary
Cauchy's equation
Constitutive relation fora compressible, Newtonian fluid.
ijijij eupii 2)ˆ3
2()(
( ) ijii
j
Dui g
Dt x
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Navier-Stokes equation
2
2
ii ij ij
j
i iji j
Dug p e
Dt x
pg e
x x
The general form of the Navier-Stokes equation is given by substitutionof the constitutive equation for a Newtonian fluid into the Cauchy equation of motion:
ijijkki
ii eep
xg
Dt
Du 23
2
Incompressible form (ekk=0):
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22
2
2
12
2
ijii
i j
jii
i j j i
jii
i j j i j
i ii
eDu pg
Dt x x
uupg
x x x x
uupg
x x x x x
pg u
x
),,,( tzyxfAssuming
23
2
22
2
21
222
x
u
x
u
x
u
xx
uu iii
jj
ii
where
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~
2
~
~ ugpDt
uD
If “Inviscid” 0
~
~ gpDt
uD Euler Equation
Or in vector notation
Inertia Pressure gradient
Gravity (buoyancy)
Divergence of viscous stress
(friction)