Title: 13.42 Lecture: Vortex Induced Vibrations
113.42 LectureVortex Induced Vibrations
- Prof. A. H. Techet
- 18 March 2004
2Classic VIV Catastrophe
If ignored, these vibrations can prove
catastrophic to structures, as they did in the
case of the Tacoma Narrows Bridge in 1940.
3Potential Flow
U(q) 2U? sinq
P(q) 1/2 r U(q)2 P? 1/2 r U?2
Cp P(q) - P ?/1/2 r U?2 1 - 4sin2q
4Axial Pressure Force
(i)
(ii)
Base pressure
i) Potential flow -p/w lt q lt p/2 ii) P
PB p/2 ? q ? 3p/2 (for LAMINAR flow)
5Reynolds Number Dependency
Rd lt 5
5-15 lt Rd lt 40
40 lt Rd lt 150
150 lt Rd lt 300
Transition to turbulence
300 lt Rd lt 3105
3105 lt Rd lt 3.5106
3.5106 lt Rd
6Shear layer instability causes vortex roll-up
- Flow speed outside wake is much higher than
inside - Vorticity gathers at downcrossing points in upper
layer - Vorticity gathers at upcrossings in lower layer
- Induced velocities (due to vortices) causes this
perturbation to amplify
7Wake Instability
8Classical Vortex Shedding
l
h
Von Karman Vortex Street
Alternately shed opposite signed vortices
9Vortex shedding dictated by the Strouhal number
Stfsd/U
fs is the shedding frequency, d is diameter and U
inflow speed
10Additional VIV Parameters
- Reynolds Number
- subcritical (Relt105) (laminar boundary)
- Reduced Velocity
- Vortex Shedding Frequency
- S?0.2 for subcritical flow
11Strouhal Number vs. Reynolds Number
St 0.2
12Vortex Shedding Generates forces on Cylinder
Uo
Both Lift and Drag forces persist on a cylinder
in cross flow. Lift is perpendicular to the
inflow velocity and drag is parallel.
FL(t)
FD(t)
Due to the alternating vortex wake (Karman
street) the oscillations in lift force occur at
the vortex shedding frequency and oscillations in
drag force occur at twice the vortex shedding
frequency.
13Vortex Induced Forces
Due to unsteady flow, forces, X(t) and Y(t), vary
with time.
Force coefficients
Cx
Cy
14Force Time Trace
DRAG
Cx
Avg. Drag ? 0
LIFT
Cy
Avg. Lift 0
15Alternate Vortex shedding causes oscillatory
forces which induce structural vibrations
Heave Motion z(t)
LIFT L(t) Lo cos (wst?)
DRAG D(t) Do cos (2wst ?)
Rigid cylinder is now similar to a spring-mass
system with a harmonic forcing term.
ws 2p fs
16Lock-in
A cylinder is said to be locked in when the
frequency of oscillation is equal to the
frequency of vortex shedding. In this region the
largest amplitude oscillations occur.
wv 2p fv 2p St (U/d)
Shedding frequency
Natural frequency of oscillation
17Equation of Cylinder Heave due to Vortex shedding
z(t)
m
b
k
Added mass term
Restoring force
If Lv gt b system is UNSTABLE
Damping
18Lift Force on a Cylinder
Lift force is sinusoidal component and residual
force. Filtering the recorded lift data will give
the sinusoidal term which can be subtracted from
the total force.
LIFT FORCE
where wv is the frequency of vortex shedding
19Lift Force Components
Two components of lift can be analyzed
Lift in phase with acceleration (added mass)
Lift in-phase with velocity
Total lift
(a zo is cylinder heave amplitude)
20Total Force
- If CLv gt 0 then the fluid force amplifies the
motion instead of opposing it. This is
self-excited oscillation. - Cma, CLv are dependent on w and a.
21Coefficient of Lift in Phase with Velocity
Vortex Induced Vibrations are SELF LIMITED
In air rair small, zmax 0.2 diameter In
water rwater large, zmax 1 diameter
22Lift in phase with velocity
Gopalkrishnan (1993)
23Amplitude Estimation
Blevins (1990)
_
_
2m (2pz) r d2
fn fn/fs m m ma
SG2 p fn2
24Drag Amplification
VIV tends to increase the effective drag
coefficient. This increase has been investigated
experimentally.
Gopalkrishnan (1993)
Fluctuating Drag
Mean drag
Cd 1.2 1.1(a/d)
Cd occurs at twice the shedding frequency.
25 Single Rigid Cylinder Results
1.0
- One-tenth highest transverse oscillation
amplitude ratio - Mean drag coefficient
- Fluctuating drag coefficient
- Ratio of transverse oscillation frequency to
natural frequency of cylinder
1.0
26Flexible Cylinders
Mooring lines and towing cables act in similar
fashion to rigid cylinders except that their
motion is not spanwise uniform.
t
Tension in the cable must be considered when
determining equations of motion
27Flexible Cylinder Motion Trajectories
Long flexible cylinders can move in two
directions and tend to trace a figure-8 motion.
The motion is dictated by the tension in the
cable and the speed of towing.
28Wake Patterns Behind Heaving Cylinders
- Shedding patterns in the wake of oscillating
cylinders are distinct and exist for a certain
range of heave frequencies and amplitudes. - The different modes have a great impact on
structural loading.
29Transition in Shedding Patterns
A/d
Williamson and Roshko (1988)
f fd/U
Vr U/fd
30Formation of 2P shedding pattern
31End Force Correlation
Uniform Cylinder
Hover, Techet, Triantafyllou (JFM 1998)
Tapered Cylinder
32VIV in the Ocean
- Non-uniform currents effect the spanwise vortex
shedding on a cable or riser. - The frequency of shedding can be different along
length. - This leads to cells of vortex shedding with
some length, lc.
33Oscillating Tapered Cylinder
- Strouhal Number for the tapered cylinder
- St fd / U
- where d is the average
- cylinder diameter.
U(x) Uo
34Spanwise Vortex Shedding from 401 Tapered
Cylinder
Rd 400 St 0.198 A/d 0.5
Rd 1500 St 0.198 A/d 0.5
Rd 1500 St 0.198 A/d 1.0
dmax
Techet, et al (JFM 1998)
No Split 2P
dmin
35Flow Visualization Reveals A Hybrid Shedding
Mode
- 2P pattern results at the smaller end
- 2S pattern at the larger end
- This mode is seen to be repeatable over multiple
cycles
Techet, et al (JFM 1998)
36DPIV of Tapered Cylinder Wake
Digital particle image velocimetry (DPIV) in the
horizontal plane leads to a clear picture of two
distinct shedding modes along the cylinder.
2S
z/d 22.9
2P
z/d 7.9
Rd 1500 St 0.198 A/d 0.5
37Vortex Dislocations, Vortex Splits Force
Distribution in Flows past Bluff BodiesD. Lucor
G. E. Karniadakis
- Objectives
- Confirm numerically the existence of a stable,
periodic hybrid shedding mode 2S2P in the wake
of a straight, rigid, oscillating cylinder
- Approach
- DNS - Similar conditions as the MIT experiment
(Triantafyllou et al.) - Harmonically forced oscillating straight rigid
cylinder in linear shear inflow - Average Reynolds number is 400
VORTEX SPLIT
- Methodology
- Parallel simulations using spectral/hp methods
implemented in the incompressible Navier- Stokes
solver NEKTAR
NEKTAR-ALE Simulations
- Results
- Existence and periodicity of hybrid mode
confirmed by near wake visualizations and
spectral analysis of flow velocity in the
cylinder wake and of hydrodynamic forces
- Principal Investigator
- Prof. George Em Karniadakis, Division of Applied
Mathematics, Brown University
38VIV Suppression
- Helical strake
- Shroud
- Axial slats
- Streamlined fairing
- Splitter plate
- Ribboned cable
- Pivoted guiding vane
- Spoiler plates
39VIV Suppression by Helical Strakes
Helical strakes are a common VIV
suppresion device.
40Oscillating Cylinders
Parameters
y(t)
Re Vm d / n
Reynolds
d
b d2 / nT
Reduced frequency
y(t) a cos wt
Keulegan- Carpenter
KC Vm T / d
Vm a w
St fv d / Vm
Strouhal
n m/ r T 2p/w
41Reynolds vs. KC
KC Vm T / d 2p a/d
Re KC b
b d2 / nT
Also effected by roughness and ambient turbulence
42Forced Oscillation in a Current
y(t) a cos wt
q
w 2 p f 2p / T
U
Reduced velocity Ur U/fd
Max. Velocity Vm U aw cos q
Reynolds Re Vm d / n
Roughness and ambient turbulence
43Wall Proximity
e d/2
At e/d gt 1 the wall effects are reduced. Cd, Cm
increase as e/d lt 0.5 Vortex shedding is
significantly effected by the wall presence. In
the absence of viscosity these effects are
effectively non-existent.
44Galloping
Galloping is a result of a wake instability.
Resultant velocity is a combination of the heave
velocity and horizontal inflow.
If wn ltlt 2p fv then the wake is quasi-static.
45Lift Force, Y(a)
Y(t)
V
a
Cy
Stable
Cy
a
Unstable
46Galloping motion
a
b
k
Cl(a) Cl(0)
...
Assuming small angles, a
V U
47Instability Criterion
..
.
(mma)z (b 1/2 r U2 a )z kz 0
b 1/2 r U2 a
lt 0
If
Then the motion is unstable! This is the
criterion for galloping.
48b is shape dependent
Shape
-2.7
0
U
-3.0
-10
-0.66
49Instability
lt
b
Critical speed for galloping
b 1/2 r a
U gt
( )
50Torsional Galloping
Both torsional and lateral galloping are
possible. FLUTTER occurs when the frequency of
the torsional and lateral vibrations are very
close.
51Galloping vs. VIV
- Galloping is low frequency
- Galloping is NOT self-limiting
- Once U gt Ucritical then the instability occurs
irregardless of frequencies.
52References
- Blevins, (1990) Flow Induced Vibrations, Krieger
Publishing Co., Florida.