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13.42 Lecture 2: Vortex Induced Vibrations Prof. A. H. Techet 28 April 2005

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Page 1: 13.42 Lecture 2: Vortex Induced Vibrations - MITweb.mit.edu/13.42/www/handouts/VIV-2.pdf · VIV in the Ocean • Non-uniform currents effect the spanwise vortex shedding on a cable

13.42 Lecture 2:Vortex Induced

Vibrations

Prof. A. H. Techet28 April 2005

Page 2: 13.42 Lecture 2: Vortex Induced Vibrations - MITweb.mit.edu/13.42/www/handouts/VIV-2.pdf · VIV in the Ocean • Non-uniform currents effect the spanwise vortex shedding on a cable

• 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.

Wake Patterns Behind Heaving Cylinders

‘2S’ ‘2P’f , A

f , A

UU

Page 3: 13.42 Lecture 2: Vortex Induced Vibrations - MITweb.mit.edu/13.42/www/handouts/VIV-2.pdf · VIV in the Ocean • Non-uniform currents effect the spanwise vortex shedding on a cable

Transition in Shedding Patterns

Will

iam

son

and

Ros

hko

(198

8)

A/d

f* = fd/UVr = U/fd

Page 4: 13.42 Lecture 2: Vortex Induced Vibrations - MITweb.mit.edu/13.42/www/handouts/VIV-2.pdf · VIV in the Ocean • Non-uniform currents effect the spanwise vortex shedding on a cable

End Force Cross-Correlation

Uniform Cylinder

Tapered Cylinder

Hov

er, T

eche

t, Tr

iant

afyl

lou

(JFM

199

8)

Fc = Force Correlation Coefficient, µ = correlation standard deviation

Page 5: 13.42 Lecture 2: Vortex Induced Vibrations - MITweb.mit.edu/13.42/www/handouts/VIV-2.pdf · VIV in the Ocean • Non-uniform currents effect the spanwise vortex shedding on a cable

VIV 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.

Page 6: 13.42 Lecture 2: Vortex Induced Vibrations - MITweb.mit.edu/13.42/www/handouts/VIV-2.pdf · VIV in the Ocean • Non-uniform currents effect the spanwise vortex shedding on a cable

Three Dimensional Effects

Shear layer instabilities as well as longitudinal (braid) vortices lead to transition from laminar to turbulent flow in cylinder wakes.

Longitudinal vortices appear at Rd = 230.

Page 7: 13.42 Lecture 2: Vortex Induced Vibrations - MITweb.mit.edu/13.42/www/handouts/VIV-2.pdf · VIV in the Ocean • Non-uniform currents effect the spanwise vortex shedding on a cable

Longitudinal Vortices

C.H.K. Williamson (1992)

The presence of longitudinal vortices leads to rapid breakdown of the wake behind a cylinder.

Page 8: 13.42 Lecture 2: Vortex Induced Vibrations - MITweb.mit.edu/13.42/www/handouts/VIV-2.pdf · VIV in the Ocean • Non-uniform currents effect the spanwise vortex shedding on a cable

Strouhal Number for the tapered cylinder:

St = fd / U

where d is the average cylinder diameter.

Oscillating Tapered Cylinder

x

d(x)U(x

) = U

o

Page 9: 13.42 Lecture 2: Vortex Induced Vibrations - MITweb.mit.edu/13.42/www/handouts/VIV-2.pdf · VIV in the Ocean • Non-uniform currents effect the spanwise vortex shedding on a cable

Spanwise Vortex Shedding from 40:1 Tapered Cylinder

Tech

et, e

t al (

JFM

199

8)

dmax

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

dminNo Split: ‘2P’

Page 10: 13.42 Lecture 2: Vortex Induced Vibrations - MITweb.mit.edu/13.42/www/handouts/VIV-2.pdf · VIV in the Ocean • Non-uniform currents effect the spanwise vortex shedding on a cable

Flow 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)

Page 11: 13.42 Lecture 2: Vortex Induced Vibrations - MITweb.mit.edu/13.42/www/handouts/VIV-2.pdf · VIV in the Ocean • Non-uniform currents effect the spanwise vortex shedding on a cable

DPIV of Tapered Cylinder Wake

‘2S’

‘2P’

Digital particle image velocimetry (DPIV) in the horizontal plane leads to a clear picture of two distinct shedding modes along the cylinder.

Rd = 1500; St = 0.198; A/d = 0.5

z/d

= 22

.9z/

d =

7.9

Page 12: 13.42 Lecture 2: Vortex Induced Vibrations - MITweb.mit.edu/13.42/www/handouts/VIV-2.pdf · VIV in the Ocean • Non-uniform currents effect the spanwise vortex shedding on a cable

Evolution of the Hybrid Shedding Mode

‘2P’ ‘2S’

Rd = 1500; St = 0.198; A/d = 0.5

z/d = 22.9z/d = 7.9

Page 13: 13.42 Lecture 2: Vortex Induced Vibrations - MITweb.mit.edu/13.42/www/handouts/VIV-2.pdf · VIV in the Ocean • Non-uniform currents effect the spanwise vortex shedding on a cable

Evolution of the Hybrid Shedding Mode

‘2S’‘2P’

Rd = 1500; St = 0.198; A/d = 0.5

z/d = 22.9z/d = 7.9

Page 14: 13.42 Lecture 2: Vortex Induced Vibrations - MITweb.mit.edu/13.42/www/handouts/VIV-2.pdf · VIV in the Ocean • Non-uniform currents effect the spanwise vortex shedding on a cable

Evolution of the Hybrid Shedding Mode

‘2S’‘2P’

Rd = 1500; St = 0.198; A/d = 0.5

z/d = 22.9z/d = 7.9

Page 15: 13.42 Lecture 2: Vortex Induced Vibrations - MITweb.mit.edu/13.42/www/handouts/VIV-2.pdf · VIV in the Ocean • Non-uniform currents effect the spanwise vortex shedding on a cable

Evolution of the Hybrid Shedding Mode

‘2S’‘2P’

Rd = 1500; St = 0.198; A/d = 0.5

z/d = 22.9z/d = 7.9

Page 16: 13.42 Lecture 2: Vortex Induced Vibrations - MITweb.mit.edu/13.42/www/handouts/VIV-2.pdf · VIV in the Ocean • Non-uniform currents effect the spanwise vortex shedding on a cable

NEKTAR-ALE Simulations

Objectives:• Confirm numerically the existence of a stable,

periodic hybrid shedding mode 2S~2P in the wake of a straight, rigid, oscillating cylinder

Principal Investigator:• Prof. George Em Karniadakis, Division of Applied

Mathematics, Brown University

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 Dislocations, Vortex Splits & Force Distribution in Flows past Bluff Bodies

D. Lucor & G. E. Karniadakis

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

Methodology:• Parallel simulations using spectral/hp methods

implemented in the incompressible Navier- Stokes solver NEKTAR

VORTEX SPLIT

Techet, Hover and Triantafyllou (JFM 1998)

Page 17: 13.42 Lecture 2: Vortex Induced Vibrations - MITweb.mit.edu/13.42/www/handouts/VIV-2.pdf · VIV in the Ocean • Non-uniform currents effect the spanwise vortex shedding on a cable

VIV Suppression•Helical strake

•Shroud

•Axial slats

•Streamlined fairing

•Splitter plate

•Ribboned cable

•Pivoted guiding vane

•Spoiler plates

Page 18: 13.42 Lecture 2: Vortex Induced Vibrations - MITweb.mit.edu/13.42/www/handouts/VIV-2.pdf · VIV in the Ocean • Non-uniform currents effect the spanwise vortex shedding on a cable

VIV Suppression by Helical Strakes

Helical strakes are a common VIV suppressiondevice.

Page 19: 13.42 Lecture 2: Vortex Induced Vibrations - MITweb.mit.edu/13.42/www/handouts/VIV-2.pdf · VIV in the Ocean • Non-uniform currents effect the spanwise vortex shedding on a cable

Flexible 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

Page 20: 13.42 Lecture 2: Vortex Induced Vibrations - MITweb.mit.edu/13.42/www/handouts/VIV-2.pdf · VIV in the Ocean • Non-uniform currents effect the spanwise vortex shedding on a cable

Flexible Cylinder Motion Trajectories

Long flexible cylinders can move in two directions and tend to trace a figure-8 motion. The motion is dictated bythe tension in the cable and the speed of towing.

Page 21: 13.42 Lecture 2: Vortex Induced Vibrations - MITweb.mit.edu/13.42/www/handouts/VIV-2.pdf · VIV in the Ocean • Non-uniform currents effect the spanwise vortex shedding on a cable

Nominal Reduced Velocity, Vrn

Freq

uenc

y R

atio

, fx/f

y

2-DOF Cylinder Motion CYLINDER ORBITAL PLOTS

Rigid cylinder free to move in both transverse (y) and longitudinal (x) directions. High length:diameter ratio.

Page 22: 13.42 Lecture 2: Vortex Induced Vibrations - MITweb.mit.edu/13.42/www/handouts/VIV-2.pdf · VIV in the Ocean • Non-uniform currents effect the spanwise vortex shedding on a cable

FFT Magnitude Contours For Frequency Ratio fx/fy = 1.0

Transverse Position In-Line Position

Page 23: 13.42 Lecture 2: Vortex Induced Vibrations - MITweb.mit.edu/13.42/www/handouts/VIV-2.pdf · VIV in the Ocean • Non-uniform currents effect the spanwise vortex shedding on a cable

FFT Magnitude Contours For Frequency Ratio fx/fy = 2.0

Transverse Position In-Line Position

Page 24: 13.42 Lecture 2: Vortex Induced Vibrations - MITweb.mit.edu/13.42/www/handouts/VIV-2.pdf · VIV in the Ocean • Non-uniform currents effect the spanwise vortex shedding on a cable

Power Balance Along a Riser

Page 25: 13.42 Lecture 2: Vortex Induced Vibrations - MITweb.mit.edu/13.42/www/handouts/VIV-2.pdf · VIV in the Ocean • Non-uniform currents effect the spanwise vortex shedding on a cable

Overview & Aim• Obtain power balance along a riser

– We need power input from the fluid to the riser as a function of z.

– Input:

– Output:

– Power balance is correlated with Clv(z).

212

Cross-flow displacement: Lift force:

Normalized Lift force:

Incoming Velocity Profile: ( )

y(z,t)L(z,t)

L(z,t)f(z,t) dsU

U zρ

=

m( , ) & ( )mlv lvC z C zω

Page 26: 13.42 Lecture 2: Vortex Induced Vibrations - MITweb.mit.edu/13.42/www/handouts/VIV-2.pdf · VIV in the Ocean • Non-uniform currents effect the spanwise vortex shedding on a cable

Fourier Decomposition• Obtain the Fourier decomposition of force and

displacement as:

• Fourier Coefficients

1

1

ˆRe

ˆRe

n

n

Ni t

nn

Ni t

nn

y(z,t) y e

f(z,t) f e

ω

ω

=

=

⎡ ⎤= ⎢ ⎥

⎢ ⎥⎣ ⎦

⎡ ⎤= ⎢ ⎥

⎢ ⎥⎣ ⎦

ˆ ˆˆ ˆ ( , ) & ( , )n n n n n ny y z f f zω ω= =

Page 27: 13.42 Lecture 2: Vortex Induced Vibrations - MITweb.mit.edu/13.42/www/handouts/VIV-2.pdf · VIV in the Ocean • Non-uniform currents effect the spanwise vortex shedding on a cable

Choose a Set of Important Frequencies

• Choose the set of frequencies ωm which represents– peaks in the span-averaged Fourier coefficients:

ˆˆ ( , ) & ( , )m m m my z f zω ω

ˆˆ ,m my f

Page 28: 13.42 Lecture 2: Vortex Induced Vibrations - MITweb.mit.edu/13.42/www/handouts/VIV-2.pdf · VIV in the Ocean • Non-uniform currents effect the spanwise vortex shedding on a cable

Obtaining Global Clv• Obtain the multi-frequency lift coefficients in phase with velocity and acceleration as:

• Global lift coefficient in phase with velocity:

• Clv is very important as it expresses energy balance.

• Clv*U(z)2 is representative of the power input from the fluid to the riser.

( ) ( )( )

( ) ( )( )

m

m m

m

m

Lift coefficient in phase with velocity for :

ˆ ˆ ˆ( , ) ( , ) sin arg arg

Lift coefficient in phase with acclera tion for :

ˆ ˆ ˆ( , ) - ( , ) cos arg arg

m

m

lv m m m

la m m m m

C z f z f y

C z f z f y

ω

ω ω

ω

ω ω

= −

= −

m

2m

ˆ

( )ˆ

mlv mm

lv

mm

C yC z

y

ω

ω

⎛ ⎞⎜ ⎟⎜ ⎟= − ⎜ ⎟⎜ ⎟⎜ ⎟⎝ ⎠

Page 29: 13.42 Lecture 2: Vortex Induced Vibrations - MITweb.mit.edu/13.42/www/handouts/VIV-2.pdf · VIV in the Ocean • Non-uniform currents effect the spanwise vortex shedding on a cable

Input Sheared Velocity Profile

Page 30: 13.42 Lecture 2: Vortex Induced Vibrations - MITweb.mit.edu/13.42/www/handouts/VIV-2.pdf · VIV in the Ocean • Non-uniform currents effect the spanwise vortex shedding on a cable

Selected Frequencies

• Chosen set of frequencies ωm :

ˆˆ ,m my f

( )2 0.1733 0 .1831 0 .1929 0 .2026 0 .2124 0 .2222 0 .2295 0 .2393mω π=

Page 31: 13.42 Lecture 2: Vortex Induced Vibrations - MITweb.mit.edu/13.42/www/handouts/VIV-2.pdf · VIV in the Ocean • Non-uniform currents effect the spanwise vortex shedding on a cable

Global Clv & Cm

• Clv*U(z)2 is representative of the power input from the fluid to the riser.

• One can clearly observe that there is a positive input of power from the fluid where the incoming velocity is high.

• The power is transferred to the low incoming velocity region, as traveling waves in the riser.

Page 32: 13.42 Lecture 2: Vortex Induced Vibrations - MITweb.mit.edu/13.42/www/handouts/VIV-2.pdf · VIV in the Ocean • Non-uniform currents effect the spanwise vortex shedding on a cable

Oscillating Cylinders

d

y(t)

y(t) = a cos ωt

Parameters:Re = Vm d / ν

Vm = a ω

y(t) = -aω sin(ωt).

b = d2 / νT

KC = Vm T / d

St = fv d / Vm

ν = µ/ ρ ; Τ = 2π/ω

Reducedfrequency

Keulegan-Carpenter #

Strouhal #

Reynolds #

Page 33: 13.42 Lecture 2: Vortex Induced Vibrations - MITweb.mit.edu/13.42/www/handouts/VIV-2.pdf · VIV in the Ocean • Non-uniform currents effect the spanwise vortex shedding on a cable

Reynolds # vs. KC #

b = d2 / νT

KC = Vm T / d = 2π a/d

Re = Vm d / ν = ωad/ν = 2π a/d d /νΤ

2)(( )

Re = KC * b

Also effected by roughness and ambient turbulence

Page 34: 13.42 Lecture 2: Vortex Induced Vibrations - MITweb.mit.edu/13.42/www/handouts/VIV-2.pdf · VIV in the Ocean • Non-uniform currents effect the spanwise vortex shedding on a cable

Forced Oscillation in a Current

θ

U

y(t) = a cos ωtω = 2 π f = 2π / T

Parameters: a/d, ρ, ν, θ

Reduced velocity: Ur = U/fd

Max. Velocity: Vm = U + aω cos θ

Reynolds #: Re = Vm d / ν

Roughness and ambient turbulence

Page 35: 13.42 Lecture 2: Vortex Induced Vibrations - MITweb.mit.edu/13.42/www/handouts/VIV-2.pdf · VIV in the Ocean • Non-uniform currents effect the spanwise vortex shedding on a cable

Wall Proximity

e + d/2

At e/d > 1 the wall effects are reduced.

Cd, Cm increase as e/d < 0.5

Vortex shedding is significantly effected by the wall presence.

In the absence of viscosity these effects are effectively non-existent.

Page 36: 13.42 Lecture 2: Vortex Induced Vibrations - MITweb.mit.edu/13.42/www/handouts/VIV-2.pdf · VIV in the Ocean • Non-uniform currents effect the spanwise vortex shedding on a cable

GallopingGalloping is a result of a wake instability.

m

y(t), y(t).Y(t)

U-y(t).

Resultant velocity is a combination of the heave velocity and horizontal inflow.

If ωn << 2π fv then the wake is quasi-static.

Page 37: 13.42 Lecture 2: Vortex Induced Vibrations - MITweb.mit.edu/13.42/www/handouts/VIV-2.pdf · VIV in the Ocean • Non-uniform currents effect the spanwise vortex shedding on a cable

Lift Force, Y(α) Y(t)

Cy = Y(t)

1/2 ρ U2 Ap

α

Cy Stable

Unstable

Page 38: 13.42 Lecture 2: Vortex Induced Vibrations - MITweb.mit.edu/13.42/www/handouts/VIV-2.pdf · VIV in the Ocean • Non-uniform currents effect the spanwise vortex shedding on a cable

Galloping motion

m

z(t), z(t).L(t)

U-z(t).

b k

a mz + bz + kz = L(t).. .

L(t) = 1/2 ρ U2 a Clv - ma y(t)..

Cl(α) = Cl(0) + ∂ Cl (0)∂ α

+ ...

Assuming small angles, α:

α ~ tan α = - zU

.β = ∂ Cl (0)

∂ α V ~ U

Page 39: 13.42 Lecture 2: Vortex Induced Vibrations - MITweb.mit.edu/13.42/www/handouts/VIV-2.pdf · VIV in the Ocean • Non-uniform currents effect the spanwise vortex shedding on a cable

Instability Criterion

(m+ma)z + (b + 1/2 ρ U2 a )z + kz = 0.. .βU

~

b + 1/2 ρ U2 a βU < 0If

Then the motion is unstable!This is the criterion for galloping.

Page 40: 13.42 Lecture 2: Vortex Induced Vibrations - MITweb.mit.edu/13.42/www/handouts/VIV-2.pdf · VIV in the Ocean • Non-uniform currents effect the spanwise vortex shedding on a cable

β is shape dependent

U

1

1

1

2

12

14

Shape ∂ Cl (0)∂ α

-2.7

0

-3.0

-10

-0.66

Page 41: 13.42 Lecture 2: Vortex Induced Vibrations - MITweb.mit.edu/13.42/www/handouts/VIV-2.pdf · VIV in the Ocean • Non-uniform currents effect the spanwise vortex shedding on a cable

b1/2 ρ a ( )

Instability:

β = ∂ Cl (0)∂ α

<b

1/2 ρ U a

Critical speed for galloping:

U > ∂ Cl (0)∂ α

Page 42: 13.42 Lecture 2: Vortex Induced Vibrations - MITweb.mit.edu/13.42/www/handouts/VIV-2.pdf · VIV in the Ocean • Non-uniform currents effect the spanwise vortex shedding on a cable

Torsional Galloping

Both torsional and lateral galloping are possible.FLUTTER occurs when the frequency of the torsional

and lateral vibrations are very close.

Page 43: 13.42 Lecture 2: Vortex Induced Vibrations - MITweb.mit.edu/13.42/www/handouts/VIV-2.pdf · VIV in the Ocean • Non-uniform currents effect the spanwise vortex shedding on a cable

Galloping vs. VIV

• Galloping is low frequency

• Galloping is NOT self-limiting

• Once U > Ucritical then the instability occurs irregardless of frequencies.

Page 44: 13.42 Lecture 2: Vortex Induced Vibrations - MITweb.mit.edu/13.42/www/handouts/VIV-2.pdf · VIV in the Ocean • Non-uniform currents effect the spanwise vortex shedding on a cable

References

• Blevins, (1990) Flow Induced Vibrations, Krieger Publishing Co., Florida.