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DEPARTMENTAL PUBLICATION NO 37 DYNAMICS Part B (TTB002) by Prof. Victor Krylov Department of Aeronautical and Automotive Engineering, Loughborough University, Loughborough, Leicestershire LE11 3TU September 2007 © Copyright This publication may not be reproduced in whole or in part without the written permission of the author
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Page 1: Dyn Lect Notes 2007

DEPARTMENTAL PUBLICATION NO 37

DYNAMICS Part B

(TTB002)

by

Prof. Victor Krylov

Department of Aeronautical and Automotive Engineering, Loughborough University, Loughborough, Leicestershire LE11 3TU

September 2007 © Copyright This publication may not be reproduced in whole or in part without the written permission of the author

Page 2: Dyn Lect Notes 2007

2

PREFACE The module Dynamics studied by all Part B students in the Department is a continuation of the Part A Module Engineering Mechanics, both Statics and Introduction to Dynamics. The main aim of the present module is to develop and deepen students’ knowledge of Dynamics, so that they would be able to analyse and understand the behaviour of complex dynamic systems. The ability to understand and predict the behaviour of such systems is extremely important for aeronautical and automotive engineers. For that reason, the module Dynamics is one of the basic components of the fundamental engineering education, and the acquired skills can be applied to studying more specific optional modules in Parts C and D. These Lecture Notes reflect the material delivered on lectures, and they are aimed to provide students with the basic information about methods and problems of Dynamics written in a concentrated form. The logical structure of these Notes is the following. Consideration starts with the dynamics of single particles, which mainly discusses the central-force motion and the associated aspects of orbital motion of planets and spacecraft. Then, the dynamics of systems of particles is considered, including the impact phenomena. The next step in the logical development of Dynamics is the dynamics of rigid bodies that are considered as systems of particles with fixed distances between each other. After that, a special consideration is given to a general and efficient approach to solving dynamic problems of complex systems – Analytical Mechanics. The main tool of Analytical Mechanics, Lagrange’s equations, are introduced in detail and are illustrated on several practical examples. The next chapters of these Lecture Notes are devoted to vibration of particles, rigid bodies, and complex systems with two or more degrees of freedom. The analytical technique based on Lagrange’s equations is applied widely to analysing many of the problems considered in these chapters. The last two chapters discuss non-linear vibrations and self-excited oscillations, including a simple theory of wing flutter. I am much grateful to Mrs. Pat Griffin for her careful word-processing of the manuscript and for her computer drawing of numerous figures.

Victor V. Krylov Loughborough, September 2007

Page 3: Dyn Lect Notes 2007

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CONTENTS

I Dynamics of Particles 6 1. Central -force motion 6

2. Orbital motion of planets and spacecraft 13

2.1 Worked example 17

II Dynamics of Systems of Particles 18

1. Generalised Newton’s 2nd law 18

2. Linear momentum of a system 19

3. Angular momentum of a system 20

4. Conservation of energy of a system 22

5. Impact phenomena 23

III Dynamics of Rigid Bodies (2D) 30

1. Basic definitions 30

2. Equations of motion of a rigid body 32

3. Work and energy 35

4. Impulse-momentum equations for rigid bodies 38

IV Introduction to Analytical Mechanics 41

1. Generalised coordinates 41

2. Lagrange’s equations 42

3. Some applications of Lagrange’s equations 47

3.1 Planetary motion 47

3.2 System of two inter-connected bodies 48

3.3 Double pendulum 50

4. Principle of least action (Hamilton’s principle) 52

5. Note on Hamilton’s equations 54

Page 4: Dyn Lect Notes 2007

4

V Vibration of Particles 55

1. Free vibrations 55

2. Effect of damping 63

3. Forced vibrations 67

3.1 Force excitation 67

3.2 Base excitation 71

3.3 Vibrations due to rotating unbalance 74

VI Vibration of Rigid Bodies 76

1. Typical examples 76

1.1 Physical pendulum 76

1.2 Log suspended via two ropes 77

1.3 Log suspended via two rods 78

1.4 Bar with a torsional spring 80

2. Energy method of determining the frequency of vibration 81

2.1 Rocking motion of a semi-disk: comparative

analysis by energy method and by means of

Lagrange’s equations 82

VII Systems with Two or More Degrees of Freedom 85

1. Free vibrations 85

2. Matrix notation 88

3. Some practical examples 89

3.1 2-DOF vehicle model for bounce and pitch 89

3.2. Symmetrical 2-DOF system 92

4. Initial conditions 94

5. Forced harmonic vibrations 97

5.1 Construction of the inverse matrix 98

5.2 Representation in terms of normal mode

summation 101

5.3 Principle of tuned vibration absorber 102

Page 5: Dyn Lect Notes 2007

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VIII Non-linear Vibrations 104

1. Perturbation analysis of a non-linear pendulum 104

IX Self - excited Oscillations 110

1. Systems with ‘negative friction’ 110

1.1. Mass on the moving belt 110

1.2. Froude’s pendulum 113

2. Simple theory of wing flutter: 2-DOF model 114

2.1. Coupled bending and torsional vibrations 114

2.2. Effects of aerodynamic lift and moment 115

2.3. Conditions of instability 116

Recommended Literature 118

Page 6: Dyn Lect Notes 2007

6

I. DYNAMICS OF PARTICLES

1. CENTRAL FORCE MOTION This type of motion is extremely important in nature: movement of planets,

elementary particles (electrons, protons, etc). In engineering, it defines the

movement of rockets, earth satellites and other space vehicles.

Let the central force F(r) be the attraction (pulling) force:

F(r) = - F(r) er = - F (r) rr

Here r is a radius-vector defining the position of a particle, and e r is a unit

vector in the direction of r. Then, Newton’s 2nd law for a particle with the

mass m subject to such a force can be written as:

- F(r) er = m r&& (1)

In particular, for gravity force F(r) = G 2o

rmm , where m0 is the mass of the

attracting (heavy) body, and G is the gravity constant.

M

r

X

v

F r

θ m0

O

m

Page 7: Dyn Lect Notes 2007

7

Particle motion caused by a gravity central force

Consider particle motion caused by a gravity central force. Using polar co-

ordinates r and θ, the following expressions for the first and second time

derivatives of r can be written:

( ) ( )θ

θ

θθ

θ

erdtd

rerrr

ererr

r

r

&&&&&&

&&

22

.

1+−=

+=

(see e.g. Engineering Mechanics: Dynamics. Part A)

Then, it follows from Equation (1) that

( ) ( )

( ) ( )310:

2:

2

22

θ

θ

θ&

&&&

rdtd

rme

rrmr

mmGe o

r

=

−=−

It follows from (3) that ( ) 02 =θ&rdtd

or h const 2 ==θ&r (4)

Note that Equation ( 4) describes conservation of the angular momentum of

the particle of mass m:

θ&2mrvmxr =

Page 8: Dyn Lect Notes 2007

8

Area swept out by the radius vector during the time dt:

( )

θθ

θ

&& 2221

21

21

rdtdr

dtdAA

rdrdA

====>

⎟⎠⎞

⎜⎝⎛=

But, according to Equation (4), const A =& .

This gives the mathematical proof of Kepler’s 2nd law (J. Kepler, 1571 -

1630), which was first established empirically. This law reads: ‘Areas swept

through in equal times are equal’.

Determination of the path of the body:

Let us determine the path of the body from the above equations by excluding

time t. Let us first introduce the useful change of variable:

uu

rThen

ur

&&2

1

1

−=

=

Using Equation (4), we can rewrite this expression as

( )θθ dduhuhr −=⎟

⎠⎞⎜

⎝⎛−= &&&

Continuing differentiation one gets

2

θ&&&

⎟⎟⎠

⎞⎜⎜⎝

⎛−=

dudhr

Using Equation (4) again gives:

Page 9: Dyn Lect Notes 2007

9

⎟⎟⎠

⎞⎜⎜⎝

⎛−=

2

222

θduduhr&&

Now substitute r&& into Equation (2) The result is

422

2222 1 uh

ududuhuGmo −−=−

θ

or 22

2

h

Gmu

dud o=+

θ (5)

This is a non-homogenous linear differential equation.

Its solution is (check by substitution into Equation (5)!):

( )2cos1

h

GmC

ru o++== δθ

Here C and δ are constants of the integration. If to assume r = min at θ =0,

then δ = 0 and

2 cos 1h

GmC

ro+= θ

or eddr1 cos 11

+= θ , (6)

where we have introduced the new notations:

oGmCheCd

2 and 1 ==

Page 10: Dyn Lect Notes 2007

10

Analysis of Equation (6)

Equation (6) describes three different types of curves (particle trajectories),

depending on the value of the parameter e (in polar coordinates) :

hyperbolae

ee

−>−=−<

1parabola1ellipse1

1. Ellipse )1( <e

Obviously,

2maxmin12

112

eed

eed

eedrra

−==

−+

+=+=

Other useful expressions for minr and maxr :

( ) ( )earear +=−= 1:1 maxmin

1e >

1e <

0e =

1e =

Perigee Apogee 2b

2a

om

θ X

1

1

Page 11: Dyn Lect Notes 2007

11

If to express d in terms of a, then Equation (6) can be rewritten as

( )21cos11ea

er −

+=

θ (7)

The value of 2b is determined from the geometrical properties of the ellipse:

2b = 2a 21 e−

Note that Equations (6) and (7) reflect Kepler’s 1st law, which reads:

‘The planets move in elliptical orbits around the sun as a focus’.

The period of a particle motion on the elliptical orbit can be calculated as

hab

r

abAA π

θ

πτ 2

21 2

===&&

.

Using the above-mentioned geometrical expressions for a and b and

applying the well-known relationship Gm0 = gR2 for low altitude orbits, where

g is the gravity acceleration and R is the average radius of the attracting

body (e.g. planet), one can rewrite the above formula as

or gR

a 23

2πτ =

This is the mathematical expression of Kepler’s 3rd law:

‘The square of the period of motion is proportional to the cube of the

semi major axis of the orbit’.

Page 12: Dyn Lect Notes 2007

12

2. Parabola ( )1e =

In this case, Equation (6) takes the form

( )θcos 111+=

dr

One can see that

πθ →

∞→→

when

rorr

01

This means that a particle moves away from the attracting body.

m

r

X

mo

θ

Page 13: Dyn Lect Notes 2007

13

3. Hyperbola ( 1e > )

It follows from equation (6) in this case that

∞→→ rorr

01

when e1cos −=θ

i.e. at ⎟⎠⎞

⎜⎝⎛−±== −

e1cos 1

1θθ

2. ORBITAL MOTION OF PLANETS AND SPACECRAFT Expressions for a Particle’s Velocity

In this section we consider an important case of orbital motion of planets and

spacecraft. It is often necessary to determine the velocity of the orbiting body

in any point of the orbit. The easiest way to do so is to use energy

conservation law:

m

X

1θ− om

Page 14: Dyn Lect Notes 2007

14

constV =+Τ=Ε .

Here E is the total energy of a particle, and T and V are its kinetic and

potential energies respectively.

Note that ( )2222

21

21 θυ && rrmm +==Τ

Considering V, we recall that near the surface of the attracting body (e.g.

near the earth surface)

( ) hmghhmgVV g Δ=−=Δ=Δ 12

As we mentioned already, near the Earth surface

2

2

gRGm

mgR

GmmF

o

og

==>

==

Then, the change in gravitational potential energy for large hΔ = r’ – r will

be:

gg

r

rg

VV

rrmgR

rdrmgRV

−′=

=⎟⎠⎞

⎜⎝⎛ −=−=Δ ∫ '

22

2 11'

2h

For large hΔ one should use a more precise expression for the gravity force:

2r

GmmF o

g = Δh

h1

Page 15: Dyn Lect Notes 2007

15

In space problems it is customary to take Vg’ = 0 at 1r = ∞

Therefore,

Vg = -r

mgR2 (8)

Then, the energy conservation law can be written as

( ) constr

mgRrrm =−+=Ε2

22221 θ&& (9)

or

constr

mgRm =−=Ε2

221 υ

Hence

( )mr

gRr Ε+==

212 222 υυ (10)

It is convenient to express Ε via other parameters of the problem and

substitute such expressions into Equation (10) so that to obtain simple and

useful expressions for v.

In what follows we consider elliptical orbits only.

Take θ = 0 in Equation (7). Then, it follows from Equation (7) that

( ) ( )eaeae

rr −=

+==

11

1111

2min

Note that r& = 0 at θ = 0 and always rhrhr ==>= θθ &&2

Then it follows from Equation (9) that:

Page 16: Dyn Lect Notes 2007

16

=−=Εr

mgRrhm

2

2

2

21

( ) ( )

( )aee

dCand

CeGm

hBut

eamgR

eahm

o2

2

2

22

2

11

1121

−===

−−

−=

Then

( ) ( )

( )( ) ( ) a

mgRea

mgRea

eagRm

eagReaGmh o

2111

21

1122

22

22

222

−=−

−−

−=Ε=>

−=−=

Substituting Ε = -a

mgR2

2 into Equation (10), we obtain the following

expression for v in the arbitrary point r of the orbit:

⎟⎠⎞

⎜⎝⎛ −=

argR

2112 22υ (11)

For some particular positions of the particle, the following useful expressions

can be easily obtained from Equation (11):

1. At r = rmin =a(1-e) (a perigee)

min

max11

rr

agR

ee

agRp =

−+

== υυ

2. At r = rmax = a(1 + e) (an apogee)

max

min11

rr

agR

ee

agRA =

+−

== υυ

Page 17: Dyn Lect Notes 2007

17

2.1 WORKED EXAMPLE

Problem 3/275 (M & K, 5th Ed. )

1. Find υ for a circular orbit (e=0)

For e=0 => a=r=R+H

Then, using Equation (11), one obtains

HR

gRrr

gR+

=⎟⎠⎞

⎜⎝⎛ −=

12112 222υ

Hence )( HRgR +=υ

2. Escape means that a ∞→

Then, from Equation (11):

( )

( )υυυυ

υ

υ

12

2

12112 222

−=−=Δ

+=∴

+=⎟

⎠⎞

⎜⎝⎛

∞−=

esc

esc

esc

HRgR

HRgR

rgR

3. Substituting R = 6371 Km and g = 9.825 m/s2, we obtain:

skmvskmvskm esc /20.3,/92.10,/72.7 =Δ==υ

XH

R

A spacecraft is on a circular orbit around the earth at H = 320 Km. Determine the increase in velocity

υΔ necessary to escape the earth

Page 18: Dyn Lect Notes 2007

18

II. DYNAMICS OF SYSTEMS PARTICLES

1. GENERALISED NEWTON’S SECOND LAW (aka the theorem about the motion of a centre of mass of a system;

see also Engineering Mechanics: Statics )

∑≠

+=ij

jiext

iii FFam

j

i ij

ext

ii

ii iFiFam ∑ ∑∑∑

≠+=

Let us introduce tot

ii

cm m

irmr

∑= (1)

where mtot = ∑i

im

∑∑

=

=

===

i

exticmtot

cmtot

cmtoti

iii

ii

Fam

am

rmrmam &&&&

(2)

Ζ

X

y ir

then

0

Page 19: Dyn Lect Notes 2007

19

2. LINEAR MOMENTUM OF A SYSTEM

By definition,

ii

ii

idef

iidef

i

mGG

vmG

υ∑∑ ==

= - for a single particle and for a system of particles

Using equation (1), one can easily obtain that

cmtotVmG = (3)

If 0=∑ ext

iiF , then it follows from equation (2) that

0=cmtot am

i.e. constVmG cmtot == (4)

If only a projection of ext

iiF∑ is zero, e.g. x – projection, then only

constVm cmxtot =,

Using the above definition of linear momentum of a system, it is often

convenient to use the equivalent form of the Equation (2):

ext

iiFG ∑=& (5)

Page 20: Dyn Lect Notes 2007

20

3. ANGULAR MOMENTUM OF A SYSTEM

1) Angular momentum about a fixed point O. By definition, the angular momentum about a fixed point 0 is:

( )∑∑ ×==i

iiii

oio vmrHH

Let us consider oH&

( ) ( )∑∑ ×+×=i

iiii

iiio vmrvmrH &&&

But ( ) ( )∑∑ ×=×i

iii

iii Frvmr & ,

where ∑≠

+=ij

ijext

ii FFF

As before, only extiF give non-zero contribution.

Hence ( ) ( )∑∑ ×=×i

extii

iiii FrVmr &

Governing equation It follows from the above that:

( )∑ ∑ ×==i i

extii

extoio FrMH& (6)

2) Angular momentum about a mass centre G

)(det ∑ ×=i

iiiG rmH &ρ (7)

0

G

0

ir

Gr

0

ri i

Page 21: Dyn Lect Notes 2007

21

But iGi rr ρ+= &&& ,

Then ( ) ( )∑ ∑ ×+×=i i

iiiGiiG mrmH ρρρ &&

Noticing that ( ) ( )iGiGii rmrm ρρ ×−=× &&

One obtains ( )43421

&&

Gforll

ii

iGi

Gii mrrm

0

ρρ ∑∑ ×−=×

Hence ( )∑ ×=i

iiiG mH ρρ & (8)

Equations (7) and (8) give two different forms of angular momentum of the

system about G – absolute angular momentum (7) and relative angular

momentum (8), and they are identical.

Let us now consider :HG&

Taking, for example, Equation (7), one can express GH& as

( ) ∑∑ ×++×= iiii

iGiiG rmrmH &&

444 3444 21

&&&& ρρρ

0

The equality of the first term to zero in the above expression can be proven

using the definition of the mass centre and some properties of cross products.

The rest can be rewritten using Newton’s 2nd Law:

( ) ( )∑∑ ×=×i

iii

iii Frm ρρ && ,

where ∑≠

+=ij

jiext

ii FFF

Page 22: Dyn Lect Notes 2007

22

As only extiF give non-zero input, one can obtain the following governing

equation:

( )∑∑ ×==i

extii

ext

iGG FMH ρ& (9)

Note that GH in Equation (9) can be written both in ‘absolute’ and ‘relative’

forms.

Conservation of Angular Momentum of a System

If the sum of moments of external forces is zero about O or about G, then it

follows from Equations (6) or (9) that

constHorconstH Go ==

or, which is the same, 0H,0H Go =Δ=Δ

If only certain projections of the external force moments are zero, then only

the corresponding projections of H0 or HG are zero.

4. CONSERVATION OF ENERGY OF A SYSTEM

If no work is done on a conservative system then,

consti

i =Ε=Ε ∑

or, which is the same,

0=ΔΕ (10)

or

finalinitial Ε=Ε

Page 23: Dyn Lect Notes 2007

23

More specifically, one can rewrite Equation (10) as:

0=Δ+Δ+Δ eg VVT

Here T is the kinetic energy of a system, and Vg and Ve are parts of its

potential energy associated with gravity and elasticity respectively.

5. IMPACT PHENOMENA

There are three stages in the impact phenomena:

1-D case (consider this case first for simplicity)

21 υ>υ

Before Impact

Collision and deformation

'1υ < '

After impact

m1 m2

m1 m2

m1 m2

Page 24: Dyn Lect Notes 2007

24

Repulsive normal forces during the collision in the case of central impact

time

2-D case

Fn(t)

to

n

t

1m

1m

2m

2m

'2υ

'1υ 1υ

Page 25: Dyn Lect Notes 2007

25

Conservation of Linear Momentum at the impact

As there are no external forces acting on the system of two colliding particles

its total linear momentum conserves in the normal direction to the contact

surface:

( ) ( ) constvmG nii

in == ∑ .

For example, for a one-dimensional impact:

constvmvmvmvmG =+=+= '22

'112211 (1)

Also, one needs to take into account the physics of the impact.

The simplest way to do so is to use the experimental law of restitution

(I. Newton)

This law states that ‘when two bodies collide their relative parting velocity in

the direction of the common normal at the point of impact is equal to –e times

their relative approach velocity in this direction’

Or

( ) ( )( ) ( )nn

nnvvvv

e12

'1

'2

−−= (2)

Here e≤ 1 is the restitution coefficient

Coefficient of restitution, e, varies from 0 (perfectly plastic impact) to 1

(perfectly elastic impact).

Page 26: Dyn Lect Notes 2007

26

For One-dimensional Problems

12

'1

'2

vvvve

−−

−= (2’)

Then from Equations (1) and (2’) one can find final velocities ν1’ and ν2’ :

( ) ( )[ ]2112221

1 11' emmemmm

−+++

= ννν

(3)

( ) ( )[ ]1221121

2 11' emmemmm

−+++

= ννν

Consider an important particular case of mmm 21 == in Equations (3). Then

( ) ( )[ ]

( ) ( )[ ]ee

ee

−++=

−++=

1121'

1121'

212

121

ννν

ννν

Consider now a perfectly elastic impact (e=1). Then

1221 '' νννν == and ,

i.e. the exchange of velocities takes place.

Energy Losses During Impacts

This always takes place. Therefore, in reality e < 1.

In the idealised case of perfectly elastic impact, e =1, there is no energy

loss, i.e. the total energy conserves:

Page 27: Dyn Lect Notes 2007

27

constm ii

i ==Τ=Ε ∑ 2)2/1( ν

In the above-considered 1-D case this takes the form:

constmmmm=+=+=Τ

2'

2'

22

222

211

222

211 νννν (4)

Assume for simplicity that mmm 21 ==

Then 22

21

22

21 '' νννν +=+ (*)

On the other hand, it follows from Equation (1) that

'' 2121 νννν +=+ (**)

Equations (*) and (**) give an alternative solution to the problem for the ideal case of perfectly elastic impact. This alternative solution does not require the knowledge of the restitution coefficient.

Let us prove that in this idealised case e = 1 indeed.

To do so let’s rewrite Equation (*) in the form

22

22

21

21 '' νννν −=− ,

which can be rewritten also as

( )( ) ( )( )22221111 '''' νννννννν +−=+− . (***)

But, it follows from Equation (**) that

2211 '' νννν −=− (****)

Therefore, using Equation (****) in (***), one obtains

2211 '' νννν +=+ (*****)

Page 28: Dyn Lect Notes 2007

28

On the other hand, if

1''

12

12 =−−

−=ννννe ,

then 22112112 '''' νννννννν +=+−=− or .

Obviously, the latter expression coincides with Equation (*****) following from

the energy conservation law in the case of idealised perfectly elastic impact,

which proves the point!

For e < 1 energy loss takes place. In the case e = 0 corresponding to

perfectly inelastic impact or, which is the same, perfectly plastic impact the loss of energy is a maximum.

2-D case: Oblique Impact

In this case there are four unknowns:

( ) ( ) ( ) ( )tntn and '''' 22,1,1 νννν

n

t

1m 1m

2m2m

'2υ 2υ

'1υ 1υ

θ2

'1θθ1

'2θ

Page 29: Dyn Lect Notes 2007

29

Equations to find the unknowns:

1. Linear momentum of the whole system conserves in the normal

direction: G(n) = const:

or

( ) ( ) ( ) ( )nnnn mmmm '' 22112211 νννν +=+

2. Linear momentum of each particle conserves in the tangential

direction (as there are no impact forces along t):

( ) ( ) ( ) ( )tttt mmmm ',' 22221111 νννν ==

3. Finally, the remaining fourth equation is Equation (2) for the restitution coefficient e:

( ) ( )( ) ( )nn

nnvvvv

e12

'1

'2

−−=

Solving the above-mentioned system of four simultaneous equations gives the

solution of an arbitrary problem of central impact at oblique incidence.

Page 30: Dyn Lect Notes 2007

30

III. DYNAMICS OF RIGID BODIES (2D)

1. BASIC DEFINITIONS We recall that a rigid body is a system of particles with fixed distances

between all of them. Some general expressions useful to describe motion of

a rigid body are reminded below.

We recall (see Engineering Mechanics: Statics) that the arbitrary motion of a

rigid body can be described completely as the translation motion of one of its

points (say point O) and the rotation of the body around that point.

ανω rarra tn === ;22

x

y

ý

R

r

O

( )rVor

V

rRr

×+=

+=

+=

ων

νν

~

~

~

o

r θ

ων

θωωα

θθω

r

dtd

dtd

=

===

==

&&&

&

Page 31: Dyn Lect Notes 2007

31

2D – Case (Plain Motion)

A simple but important case of plain motion of a rigid body is characterised by

three coordinates (degrees of freedom): two coordinates of the mass centre

and the rotation angle θ.

We recall that the angular momentum about the centre of mass G is:

iii

iG mH ρρ &×= ∑

In 2D-case the magnitude of GH is

=

==

iii

iii

iG

m

mH

2

.

ρω

ωρρ

Introduce the notation

ii

i mI ∑= 2ρ - mass moment of inertia about Z-axis.

For a body made of a continuum the summation is replaced by the integration:

∫∑ == dmmI ii

i22 ρρ

Then ωIHG = (3)

y

Page 32: Dyn Lect Notes 2007

32

2. EQUATIONS OF MOTION OF A RIGID BODY

Let us apply the general equations for a system of particles derived earlier.

1. Generalised Newton’s second law:

∑=i

exticmtot Fam (1)

2. Momentum equation about the mass centre:

( )∑∑ ×==i

extii

i

extGiG FMH ρ& (2)

The above equations are valid in the general 3-D case.

In what follows we consider only 2- D case in detail.

The momentum equation (Equation (2)) then takes the form (see previous

section)

∑==i

extGiMII αω& (4)

This should be complemented by the generalised second Newton’s law:

(5)

where m = mtot and cmG aa =

Note that we already derived Equation (4) in ‘Eng. Mechanics: Statics’ by

another (a more direct) method.

∑=i

extiG Fam

Page 33: Dyn Lect Notes 2007

33

Recall the example.

Rotation Around an Arbitrary Fixed Axis

But GGi

iiGiii

G mrmrmr υυυ ×=×=× ∑∑ (using definition of G)

and Giii

i Hm =×∑ υρ (in absolute form)

d

R

F

ϕ

2

2

22 ~

mRFd

FdmR

FdI

mRrmI ii

i

=

=

=

= ∑

ω

ω

ω

&

&

&

ω

G

i

ρ

O

Gr

ir~

iGi rr ρ+=~

Angular momentum about O:

( )

( )

( )iii

iiiG

iiiio

m

mr

vmrH

υρ

υ

×+

+×=

=×=

∑ w

F

Page 34: Dyn Lect Notes 2007

34

Then, GGGo mrHH υ×+= (6)

Consider magnitude of oH :

GGGo rmrHH ω.+= (6’)

If to recall that GH = Iω, where ii

i mI ∑= 2ρ , then Equation (6’) can be

rewritten as

H0 = I0ω,

where

20 GmrII += . (7)

Equation (7) describes the so-called Steiner’s theorem, which is used widely

for calculation of mass moments of inertia versus different axes.

The momentum equation in this case takes the form

ext

ioioo MII ∑== αω& (8)

where all oiM ext are now calculated about point O.

Page 35: Dyn Lect Notes 2007

35

3. WORK AND ENERGY

Reminder

Work done by a force F

( )∫ ∫== dsFUorrdFU αcos

Work done by a couple

∫ θ= MdU

Let us now introduce the expressions for the kinetic energy of a rigid

body for different types of its motion:

1. Translation

Derivation of the corresponding expression for this case is quite obvious:

∑∑ ===Τ 22221

21

21 mvmvvm iii

i (9)

2. Fixed Axis Rotation

This case is easy as well:

Page 36: Dyn Lect Notes 2007

36

222221

21

21 ωω o

Io

ii

iiii

Irmvm ===Τ ∑∑43421

(10)

3. General Plane Motion

In this case the derivation is a bit more complicated:

)cos2(21

21 2222 θωρωρ iGiG

iiii

ivvmvm ++==Τ ∑∑ (*)

Consider the last term in Equation (*):

==

=

θρω

θωρ

cos

cos221

iiG

iGii

mv

vm

0== ∑ ii

iG ymvω

Due to the definition of the centre of masses:

0==∑ Gii

i myym

Then the kinetic energy takes the form

2221

21 ωImvG +=Τ (11)

Here I is the moment of inertia of the body about its mass centre.

Thus, the contributions of translation and rotation into the kinetic energy of the

body are separate.

ω

G υΓ

υΓ

ρ/ υi

ρi

mi

yi

0

Page 37: Dyn Lect Notes 2007

37

Instantaneous Centre of Zero Velocity

Practical Example: A Rolling Wheel.

υυυυω 22

==>== AARR

Useful expression for the kinetic energy in terms of the rotational velocity

about the instantaneous centre C of zero velocity:

221 ωcI=Τ

B

A

C

rA rB

Bυ B

B

A

A

rrυ

A υA

R

C

υ

Page 38: Dyn Lect Notes 2007

38

Energy Relations

Let us start from the earlier mentioned general expression valid for a system

of particles:

eg VVU Δ+Δ+ΔΤ=−21'

Here 21'

−U is the work done by external non-gravitational and non-elastic

forces on the transfer of the system from the situation 1 to the situation 2.

Specifics of Rigid Bodies

In rigid bodies the distances between all particles are constant. Then, ΔVe =

0. In the light of this,

gVU Δ+ΔΤ=−21'

If there is no work done by external forces, i.e. 021' =−U , then

0=Δ+ΔΤ gV

This is the energy conservation law for rigid bodies.

4. IMPULSE MOMENTUM EQUATIONS FOR RIGID BODIES

Consider the generalised Newton’s second law:

Page 39: Dyn Lect Notes 2007

39

dtFVmd

FdtVd

m

Fam

extt

tiG

iv

i

exti

G

i

extiG

∫∫

=

=

=

2

1

or, which is the same,

{ {

1

1

2

2

2

1 GG

t

t

exti mmdtF υυ −=∫

This holds for all projections.

If dtF2

1

t

t

exti∫ = 0, then

12 GG = ,

which describes conservation of linear momentum of a rigid body.

Consider now the angular momentum equation:

∑=i

extGiG MH& (*)

or ∑=i

extGiMIω& (**)

It follows from Equation (*) that

dtMHHt

t i

extGiGG ∫∑=−

2

112

Page 40: Dyn Lect Notes 2007

40

Similarly, it follows from (**) that

( ) dtMIt

t i

extGi∫∑=−

2

112 ωω

if 0dtM2

1

t

t i

extGi =∫∑ , then

1212 ωω IIorHH GG ==

which describes conservation of the angular momentum.

Worked Example. (Problem 6/114, M & K 5 Ed.)

Use energy conservation law:

( )( )0

21

0

22 −=ΔΤ

=Δ + ΔΤ

G

g

vm

V

(there is only translation movement and no rotation)

( )

( )o

g

Hence

g

mgV

2.33

0cos15421

cos55

2

=

=−−∴

−−=Δ

θ

θ

θ

5m 5m θ θ

υ = 4 m/s

The suspended log is used as a battering ram. Find θ providing the final velocity υ = 4 m/s

Page 41: Dyn Lect Notes 2007

41

IV. INTRODUCTION TO ANALYTICAL MECHANICS

This is a generalised theory of mechanics (dynamics) established largely by

works of J.-L. Lagrange (1736 – 1813) and some other scientists. It greatly

facilitates the analysis of complex dynamic systems.

1. Generalised Coordinates

Consider a system of N particles. To describe the positions of all

particles at any instant t one should know 3N coordinates.

The number S of independent co-ordinates (or the number of

degrees of freedom) can be smaller than 3N, i.e.

S ≤ 3N

Thus, a system can be described by any S independent variables qi ,

that are called generalised coordinates

Siqi ..........2,1; =

Page 42: Dyn Lect Notes 2007

42

Example: Spherical Pendulum

Thus, the system has only two degrees of freedom.

On the other hand, the same system is described completely by two

spherical coordinates ( angles ϕ and θ ). The third coordinate , r, is not

needed as always r = l.

In this example, the coordinates ϕ and θ can be considered as generalised

coordinates.

2. Lagrange’s Equations

Lagrange’s equations are differential equations of motion expressed in terms

of generalised coordinates.

Consider first a conservative system, i.e. a system in which the sum of kinetic

and potential energy conserves. Thus,

( ) 0=+Τ Vd (1)

X

Z

y

ϕ l θ

This system can be described traditionally by three Cartesian coordinates: x, y, z. Only two of them are independent due to the obvious constraint 2222 lzyx =++

Page 43: Dyn Lect Notes 2007

43

Let us represent Τ and V as functions of the generalised coordinates qi

and their time derivatives iq& (that are called generalised velocities):

( )( )s

ssqqqVV

qqqqqq...,

...,,...,

21

2121=

Τ=Τ &&& (2)

Consider the differential of Τ:

Differential of Τ

is

i ii

s

i iqd

qdq

qd &

&∑∑== ∂

Τ∂+

∂Τ∂

=Τ11

(3)

Now consider the general expression for the kinetic energy Τ in generalised

coordinates (the so-called quadratic form):

jis

i

s

jij qqm &&∑ ∑

= ==Τ

1 121

(4)

Here ji

m are coefficients. It can be proven (Euler’s theorem) that the following

relationship holds for Τ defined by equation (4):

Τ=∂

Τ∂∑=

21

is

i iq

q&

& (5)

Let us use Equation (5) to exclude iqd & in equation (3)

First consider differential of Equation (5):

is

i ii

i

s

iqd

qq

qdd &

&&

& ∑∑== ∂

Τ∂+⎟⎟

⎞⎜⎜⎝

⎛∂

Τ∂=Τ

112 (6)

Page 44: Dyn Lect Notes 2007

44

Now subtract Equation (3) from Equation (6):

is

i ii

i

s

idq

qq

qdd ∑∑

== ∂Τ∂

−⎟⎟⎠

⎞⎜⎜⎝

⎛∂

Τ∂=Τ

11&

& (7)

But

ii

i

ii

i

dqqdt

d

dtdq

qdq

qd

⎟⎟⎠

⎞⎜⎜⎝

⎛∂

Τ∂=

=⎟⎟⎠

⎞⎜⎜⎝

⎛∂

Τ∂=⎟⎟

⎞⎜⎜⎝

⎛∂

Τ∂

&

&&

&

Then, it follows from Equation (7) that

∑= ⎥

⎥⎦

⎢⎢⎣

∂Τ∂

−⎟⎟⎠

⎞⎜⎜⎝

⎛∂

Τ∂=Τ

s

ii

iidq

qqdtdd

1 & (8)

Using the obvious expression for dV:

is

i idq

qVdV ∑

= ∂∂

=1

, (9)

the expression for energy conservation, d(Τ + V) = 0, can be rewritten as

01

=⎥⎥⎦

⎢⎢⎣

∂∂

+∂

Τ∂−⎟⎟

⎞⎜⎜⎝

⎛∂

Τ∂∑=

is

i iiidq

qV

qqdtd

& (10)

Because the s generalised coordinates iq are independent and, therefore

the idq can take arbitrary values, Equation (10) is satisfied only if

siqV

qqdtd

iii......2,1

0

=

=∂∂

+∂

Τ∂−⎟⎟

⎞⎜⎜⎝

⎛∂

Τ∂& (11)

Equation (11) is Lagrange’s equation (or Lagrange’s equations) for a

conservative system (all forces are potential ones).

Page 45: Dyn Lect Notes 2007

45

It is useful to introduce Lagrange’s function L (or the Lagrangian):

VL −Τ=

Then, because 0/ =∂∂ iqV & , Equation (11) can be rewritten as

si

qL

qL

dtd

ii......2,1

0

=

=∂∂

−⎟⎟⎠

⎞⎜⎜⎝

⎛∂∂& (12)

For Non - conservative Systems

( ) npUVd δ=+Τ (13)

where npUδ is the work done by non-potential forces.

Let us express npUδ in terms of generalised coordinates:

is

iinp qQU δδ ∑

==

1

where iQ are known as generalised forces associated with the

corresponding generalised coordinates iq

Then, with the account of Equation (13), the Lagrange’s equation takes the

form

Ni

QqV

qqdtd

iiii

.......2,1=

=∂∂

+∂

Τ∂−⎟⎟

⎞⎜⎜⎝

⎛∂

Τ∂& (14)

Page 46: Dyn Lect Notes 2007

46

Or, if to use Lagrange’s function,

Ni

QqL

qL

dtd

iii

.......2,1=

=∂∂

−⎟⎟⎠

⎞⎜⎜⎝

⎛∂∂& (15)

Example

Let us illustrate the application of Lagrange’s equation to a one-dimensional

movement of a particle of mass m subjected to the force F.

Then,

( )

0

0

221

21

,

1

1

1

1

2

11

=∂∂

=∂∂

=∂Τ∂

=∂

Τ∂

==⎟⎟⎠

⎞⎜⎜⎝

⎛∂

Τ∂

==∂Τ∂

=∂

Τ∂

==

xV

qV

xq

xmxmdtd

qdtd

xmxmxq

xm

FQxq

&&&&

&&&&

&

Substituting the above expressions into Equations (14) or (15), we obtain:

Fxm =&& ,

which is the familiar Newton’s second law for a particle, as expected.

The advantage of using Lagrange’s equations shows in the case of complex

dynamic systems.

Page 47: Dyn Lect Notes 2007

47

3. Some Examples of Application of Lagrange’s Equations

3.1 Planetary Motion

L.E. : 2,1

0

=

=∂∂

+∂

Τ∂−⎟⎟

⎞⎜⎜⎝

⎛∂

Τ∂

iqV

qqdtd

iii&

( )

rmm

GV

rrmm

qrq

o−=

+==Τ

==

2222

2

1

21

21 θυ

θ

&&

( )

21

2

1

1

1

rmmG

rV

qV

mrrq

rmrmdtd

qdtd

rmrq

o=∂∂

=∂∂

=∂Τ∂

=∂

Τ∂

==⎟⎟⎠

⎞⎜⎜⎝

⎛∂

Τ∂

=∂Τ∂

=∂

Τ∂

θ&

&&&&

&&&

mo

m

x

r θ

r&

θ&rυ

2o gRGm =

Page 48: Dyn Lect Notes 2007

48

( )

0

0

2

2

2

2

2

2

=∂∂

=∂∂

=∂

Τ∂=

∂Τ∂

=⎟⎟⎠

⎞⎜⎜⎝

⎛∂

Τ∂

=∂

Τ∂=

∂Τ∂

θ

θ

θ

θθ

VqVq

mrdtd

qdtd

mrq

&&

&&&

Then, it follows from LE that

( ) 0

0

2

22

=

=+−

θ

θ

&

&&&

rdtdm

r

mmGmrrm o

As expected, these equations are equivalent to the ones derived in Chapter 1.

3.2 System of Two Interconnected Bodies

(Problem 7.3-2 from the book of Thomson)

( )22

22

21

21

21

21

xrkkxV

Ixm

−+=

+=Τ

θ

θ&&

M(t)

k k

m R

r

I

xq1 = 2q=θ

for small x

Page 49: Dyn Lect Notes 2007

49

To define the generalised non-potential force we recall that in this case

δθδδ MqMUnp == 2

Hence, the generalised force is M

Then,

xmqdt

d

xmxq

&&&

&&&

=⎟⎟⎠

⎞⎜⎜⎝

⎛∂

Τ∂

=∂Τ∂

=∂

Τ∂

1

1

( )( )1

0

1

1

−−+=∂∂

=∂∂

=∂Τ∂

=∂

Τ∂

xrkkxxV

qV

xq

θ

( )rxrkVqVq

Iqdt

d

Iq

−=∂∂

=∂∂

=∂

Τ∂=

∂Τ∂

=⎟⎟⎠

⎞⎜⎜⎝

⎛∂

Τ∂

=∂

Τ∂=

∂Τ∂

θθ

θ

θ

θθ

2

2

2

2

0

&&&

&&&

Then, it follows from LE that

( )tMkrkrxI

krkxxm

=+−

=−+

θθ

θ2

02&&

&&

Page 50: Dyn Lect Notes 2007

50

N.B. In engineering practice, the values of mass moment of inertia, I, for

different bodies are often expressed in the form 2gmrI = , where rg is

the so-called radius of gyration. For example, for a thin ring of radius

R obviously rg = R. Generally, the radius of gyration is smaller than

the geometrical dimensions of the body.

3.3 Double Pendulum

(Example from the book of Landau & Lifshits)

Find Τ, V and Lagrange’s function L for the system shown in the

Figure.

11112

12

111 cos21 ϕϕ glmVlm −==Τ &

To find Τ2 and V2 , we express x2 and y2 in terms of ϕ1 and ϕ2 :

22112

22112coscossinsin

ϕϕϕϕ

llyllx

+=+=

x

y 2ϕ

1ϕ 1m

2m

2l

1l

22

11

qq

ϕ=ϕ=

Page 51: Dyn Lect Notes 2007

51

Then,

( )22

22

22 2

yxm

&& +=Τ

( ) ( )( ) ( ) 2221112

2221112sinsin

coscosϕϕϕϕ

ϕϕϕϕ&&&

&&&

llyllx

−−=+=

Hence

( ) ([ ) ( )( ) ) ( ) ]

[ ( ) ]212121212

22

22

12

12

222

222212121

211

221

222

222212121

211

221

22

sinsincoscos22

sinsinsin2sin

coscoscos2cos2

ϕϕϕϕϕϕϕϕ

ϕϕϕϕϕϕϕϕ

ϕϕϕϕϕϕϕϕ

+⋅++=

=+++

++⋅+=Τ

&&&&

&&&&

&&&&

llllmllll

llllm

But

( )212121 cossinsincoscos ϕϕϕϕϕϕ −=+

Then

( )[ ]2121212

22

22

12

12

2 cos22

ϕϕϕϕϕϕ −++=Τ &&&& llllm

( )221122 coscos ϕϕ llgmV +−=

( )

( )

( )

VL

glmglmmVVV

llm

lmlmm

−Τ=

−−+−=+=

−+

+++

=Τ+Τ=Τ

222

112121

2121212

22

22

2211

2121

coscos

cos22

ϕϕ

ϕϕϕϕ

ϕϕ

&&

&&

Substitution of the above expressions for Τ and V (or for L) into Lagrange’s

equations gives the two equations versus ϕ1 and ϕ2 that describe

completely the dynamics of the system under consideration.

Page 52: Dyn Lect Notes 2007

52

4. Principle of Least Action (or Hamilton’s Principle)

Consider two moments of time, t1 and t2, in which the dynamic system is

characterised by the coordinates ( ) ( )2i

1i qandq , where i=1, 2……..s.

Now consider the integral

( ) ,,,2

1

dttqqLS ii

t

t&∫= (1)

where L = Τ - V is the Lagrangian of the system. The integral S is called

action. Its dimension is Energy x Time.

The principle of least action (P. L. Action) states that the dynamic system

moves in such a way that the integral (1) takes the minimum value.

Let us derive the differential equations that solve the problem of finding a

minimum of the integral (1). This is one of the general problems of the

Calculus of Variations.

Consider first a system with one degree of freedom, i.e. with one q(t). Let q(t)

is the function for which the integral in Equation (1) has a minimum. If to

replace q(t) by q(t) +δq(t), where δq(t) is a small function in the interval (t1,

t2) (it is called variation of the function q(t)), then the integral S will increase.

All functions q(t) + )t(qδ to be compared have to take equal values at t = t1

and t = t2 , i.e. it must be that ( ) 0)( 21 == tqtq δδ . Let us express ΔS from (1):

( )

( )dttqqL

dttqqqqLS

tt

tt

,,

,,

21

21

&

&&

∫−

−++=Δ δδ (2)

Page 53: Dyn Lect Notes 2007

53

Let us now expand ΔS in the series of powers of δq and qS& .

The necessary condition of S having a minimum is the equality to zero of the

linear terms of ΔS expansion (these terms are called the first variation or

simply variation δS of the integral (1)).

Thus, the principle of least action can be written in the form:

( ) 0dtt,q,qLS2

1

t

t=δ=δ ∫ & (3)

or

∫ =⎟⎟⎠

⎞⎜⎜⎝

⎛∂∂

+∂∂

= 21

0tt

dtqqLq

qLS &

&δδδ (4)

Note that qdtdq δ=δ& and integrate the second term in Equation (4) by parts:

=∂∂

=∂∂

∫∫ qdtdtd

qLdtq

qL t

ttt

δδ 21

21 &

&&

(5)

qdtqL

dtdq

qL t

t

t

tδδ&& ∂

∂−

∂∂

= ∫ 21

2

1

Now substitute Equation (5) into Equation (4):

∫ =⎟⎟⎠

⎞⎜⎜⎝

⎛∂∂

−∂∂

+∂∂

= 21

2

1

0tt

t

tqdt

qL

dtd

qLq

qLS δδδ

&& (6)

The first term in (6) is zero because ( ) ( ) 021 == tqtq δδ . The remaining integral

in equation (6) can be equal to zero only if

0=∂∂

−∂∂

qL

dtd

qL

& (7)

because δq are arbitrary between t1 and t2.

u dυ

u υ υ

du

0

Page 54: Dyn Lect Notes 2007

54

For a system with s degrees of freedom s different functions qi, where

i=1,2…s, should be considered independently. This gives us s already

familiar Lagrange’s equations:

0=∂∂

−∂∂

ii qL

dtd

qL

&, (8)

which proves the Principle of Least Action.

5. Note on Hamilton’s Equations

Let us introduce a generalised linear momentum pi associated with qi ,

i

i qLp&∂

∂= , (9)

and define Hamilton’s function (or the Hamiltonian):

LqpH iS

ii −= ∑

=&

1

For conservative systems

Ε=+Τ= VH (10)

Hamilton’s equations are:

siqHp

pHq

ii

ii

...2,1

,

=∂∂

−=∂∂

= && (11)

Equations (11) are differential equations of the first order. There are 2s

Hamilton’s equations; they are equivalent to s Lagrange’s equations.

Page 55: Dyn Lect Notes 2007

55

V. VIBRATION OF PARTICLES 1. FREE VIBRATIONS

Consider motion of the following simple system.

Apply Newton’s second law: ∑ = xmFx &&

As Fx = - kx, we obtain

xmkx &&=−

or

0=+ kxxm && (1)

or

02 =+ xx nω&& , (2)

where mkn /=ω is called the natural circular frequency.

kx

k

x

m

Equilibrium position

Simplest 1- DOF System

Page 56: Dyn Lect Notes 2007

56

Solution of Equation (2)

tinBtAx nn ωω s+= cos (3)

or

( )ψω += tCx usin (4)

Constants A, B or C, ψ are determined from the initial conditions, i.e. the

initial displacement xo and initial velocity ox& .

For example, for the solution in the form of Equation (3), it follows from

Equation (3) that at t=0:

noo BxandAx ω== &

Then Equation (3) can be rewritten in terms of oo xandx & as

tx

txx nn

ono ω

ωω sincos

&+= (5)

For the solution in the form of Equation (4) at t=0:

ψωψ cossin noo CxandCx == &

To find out C and ψ let us do the following:

a). 2222 ..sin no Cx ωψ=

ψω 2222 cosno Cx =&

( )22

22222

/ noo

nono

xxCHence

Cxx

ω

ωω

&

&

+=

=+

+

Page 57: Dyn Lect Notes 2007

57

b). ψsinCxo =

ψω cosno Cx =&

( )ono xxHence &/tan 1 ωψ −=

Then, Equation (4) can be rewritten in terms of oo xandx & as

( )[ ]ononnoo xxtxxx && /tansin/ 1222 ωωω −++= (6)

Very often, instead of Equation (4) (with ‘sin’), the ‘cos’ form of equation is

used:

( )ϕω += tCx ncos (7)

In this case ϕ = −tan-1⎟⎟⎠

⎞⎜⎜⎝

no

ox

xω&

and

⎥⎥⎦

⎢⎢⎣

⎡⎟⎟⎠

⎞⎜⎜⎝

⎛−+= −

no

onnoo x

xtxxx

ωωω

&& 1222 tancos/ (8)

One period of vibration τ is obviously defined from the condition.

nn

n

fei 12..

,2

==

=

ωπτ

πτω,

where fn = ωn/2π is the natural frequency [Hz].

In Equations (4) and (7) or (6) and (8), the parameters C or

222 / noo xx ω&+ are called the amplitudes of vibration. The arguments of

‘sin’ or ‘cos’ functions in the same equations are called the phases of

vibration, ψ or ϕ being the initial phases.

:

Page 58: Dyn Lect Notes 2007

58

For illustration:

)cos( ϕω += tCx n

nnf ωπτ 21

==

2π is the period in this plot

22π

ωnt [rad]

X

C

ϕ

(ϕ<0)

π 2

π 3π 2

τ is the period in this plot X

C

t [s.]

nωϕ

Page 59: Dyn Lect Notes 2007

59

A more convenient way of description of vibration processes using complex numbers

Consider Equation (7):

( )ϕω += tx ucos

Using the well-known relationship

( ),'sincos formulasEulerzize iz ±=±

one can rewrite Equation (7) as

( )[ ] [ ]tnitni eCCex ωϕω ~ReRe == +

Here C~ = ϕiCe is the so-called complex amplitude. Operation “Re” can be

made at the very end. Before that, the expression ( )ϕω += tniCex is often

being used, assuming that x is a complex number.

Vibration of a vertically suspended particle.

m

k

x Equilibrium position

Page 60: Dyn Lect Notes 2007

60

In this case

( )

xmxmkxkxmg

xxkmgFxxx

xmF

stst

stx

sttot

totx

&&&&43421

&&

+=−−∴

+−=Σ+=

0

m

kxxor

kxxmHence

nn ==+

=+

ωω ,0

02&&

&&

Thus, the final differential equation is the same as for horizontally vibrating

particle.

Another example: a ‘mathematical’ pendulum.

Pt = mg sinα

For small α

Pt = mgα

For small α the displacement is

lxlx =∴= αα

Then, applying Newton’s 2nd law, one can get

0=+

−=

xlgxor

lxmgxm

&&

&&

(9)

or 02 =+ xx nω&& (10)

α

l

x m

mg

Pn Pt

Page 61: Dyn Lect Notes 2007

61

gl

flgf

lgHere

n

nn

n

πππ

ω

ω

21,21

2==Τ==

=

General case of not small α

For a general case of not small α one should use polar coordinates : r,

α. Note that there is no movement along r. Therefore, r = l.

We recall that αααα &&&&&& lrra =+= 2

Then, Newton’s second law gives:

αα sinmgml −=&&

or 0sin =+ ααlg

&& (11)

Equation (11) is a non-linear equation, which requires a special approach

that will be considered in one of the following chapters. For small angles α:

sin α ~α, and Equation (11) can be ‘linearised’:

0

0

2 =+

=+

αωα

αα

norlg

&&

&&, (12)

with the same lg

n =ω as in the start of this example (see Equations (9)

and (10)). Indeed, multiplying Equation (12) by l and using lα =x, we can

reduce Equation (12) to the initially derived Equation (10).

0

Page 62: Dyn Lect Notes 2007

62

Alternative derivation using Lagrange’s equation.

Let us now use Lagrange’s equation to describe large vibrations of a

mathematical pendulum. In the case under consideration the kinetic and

potential energies are:

0.

cos,21 2.2

=∂∂

+∂

Τ∂−⎟⎟

⎞⎜⎜⎝

⎛∂

Τ∂

−==Τ

iii qV

qqdtdisELThen

mglVml

&

& αα

In our case i = 1 and q1 = α. Continuing in a familiar way, we obtain:

αα

α

αα

αα

sin

0

2

2

mglV

mldtd

ml

=∂∂

=∂

Τ∂

=⎟⎠⎞

⎜⎝⎛

∂Τ∂

=∂

Τ∂

&&&

&&

It follows from L.E. that

0sin2 =+ αα mglml &&

or

0sin =+ ααlg

&& ,

i.e. , we have derived the same Equation (11), as expected.

Page 63: Dyn Lect Notes 2007

63

3. EFFECT OF DAMPING

xmxckx &&& =−−

02

02 =++

=++

xxxor

kxxcxmor

nn ωζω &&&

&&&

Here we have introduced the new parameter (‘zeta’):

kmc

mc

n 22==

ωζ

We recall that

mk

n =ω

Let us use the general rule of solving differential equations with constant

coefficients and seek the solution in the form

tAex λ= (2)

Now substitute Equation (2) into Equation (1)

xc&

k

m

x kx

Let us add a linear viscous dashpot describing damping

xmFx &&=Σ

(1)

c

Page 64: Dyn Lect Notes 2007

64

As a result, we obtain the characteristic equation:

02 22 =++ nn ωλζωλ (3)

The roots of the characteristic equation (3) are:

⎟⎠⎞

⎜⎝⎛ −±−= 12

2,1 ζζωλ n

Then, the general solution of Equation (1) is

tntn

tt

eAeA

eAeAx

ωζζωζζ

λλ

⎟⎠⎞

⎜⎝⎛ −−−⎟

⎠⎞

⎜⎝⎛ −+−

+=

=+=

12

212

1

2211 (4)

Analysis of the Equation (4).

Note that generally∞≤≤ ζ0 . Let us consider the following cases:

1. ζ > 1 - overdamping

λ1 and λ2 are real and negative ( no oscillations)

overdamping (ζ>1)

critical damping (ζ=1)

t,s 0

x xo

( )0x0 =&

Page 65: Dyn Lect Notes 2007

65

2. ζ = 1 - critical damping

nωλλ −== 21 are equal and negative

For this special case

( ) tnetAAx ω−+= 21 (no oscillations)

3. ζ < 1 - underdamping

In this case ζ2 – 1 < 0

22 11 ζζ −=− iand

[ ] tntditdi eeAeAxthen ζωωω −−+= 21 , (5)

where we have introduced 21 ζωω −= nd .

The parameter isnd21 ζωω −= often called the damped natural

frequency.

If one is interested in real values of x, or in physical solution, then, taking a

real part of Equation (5) (i.e. by applying operation “Re”) and keeping in mind

that A1 and A2 are in general complex numbers, one can obtain the following

expression for x, which is also used widely:

( )ϕωζω += − tCex dtn cos , (6)

Here C is the vibration amplitude, and ϕ is the initial phase.

Page 66: Dyn Lect Notes 2007

66

For illustration:

21

221

ζω

πω

πτ−

===ndd

d f

Useful definition – the logarithmic decrement δ

( ) ===∴ dndne τζωδ τζωln

πζζ

πζ

ζω

πζω 21

2

1

222

≈−

=−

=n

n

0

τd

t , s

tnCe ξω−

tnCe ξω−−

envelope

x2

t , s

x1

t1 t2

x

τd

⎟⎟⎠

⎞⎜⎜⎝

⎛=

2

1lnxx

δ

( )

dn

dtn

tn

e

CeCe

xx

τζω

τζω

ζω

=

==+−

1

1

2

1

Page 67: Dyn Lect Notes 2007

67

3. FORCED VIBRATIONS

3.1. Force excitation

xmFx &&=Σ , then

( ) xmxckxtF &&& =−−

or

( )tFxxx nn~2 2 =++ ωζω &&& , (1)

( ) ( ) mtFtFandkmc

mcm

kwhere

n

n

/~22

=

==

=

ωζ

ω

Consider a harmonic force:

( ) [ ] tFeFtF oti

o ωω cos~~Re~ ==

Then, the general solution of Equation (1) is:

+

k

xc&

m

xkx F(t)

c

F(t)

x(t) = General solution of Equation (1) with ( ) 0tF~ =

Particular solution of Equation (1) with

( ) 0tF~ ≠

Page 68: Dyn Lect Notes 2007

68

1. The first term in the right-hand side of the above expression has been

studied by us in the previous section. It decays with time t and is

important only for relatively small t (the so-called transient processes).

2. Consider the second term and choose the following form for it: tioeFH ω~ .

Ignoring transients, i.e. for large t, we can assume that

tioeFHtx ω~)( = (2)

Let us substitute Equation (2) into (1).

Then

( ) ( ) tio

tino

tion

tio eFeFHeHFieFH ωωωω ωωζωω /=/+//+/−/

~~~2~ 22

Hence

( )ωζωωω

ωnn i

H2

122 +−

= (3)

Function H(ω) is called the frequency response function.

Thus, the solution for large t (the steady –state solution) is

( )ωζωωω

ω

nn

ti

i

eFtx

2

~

220

+−= (4)

Strictly speaking, we have to take the real part of the right-hand side of

Equation (4) to obtain the final physical solution.

Let us analyse the function H(ω):

Page 69: Dyn Lect Notes 2007

69

Let us introduce the non-dimensional frequency ratio nω

ωγ = .

Then

( )ζγγω iH

n 21122 +−

= (5)

or

( )( ) =−−+−

−−=

ζγγζγγω

ζγγ

ii

iHn 2121

)21(1222

2

( ) ( )

( ) ( )

( ) ( ) ⎥⎦⎤

⎢⎣⎡ +−

⎥⎦⎤

⎢⎣⎡ +−

=

⎥⎦⎤

⎢⎣⎡ +−

−−=

⎟⎟

⎜⎜

−−−

2222

21

21tan21

222

2222

2

21

21

21

21

ζγγω

ζγγ

ζγγω

ζγγγ

ζγ

n

i

n

ei

Hence

( ) ( )

( )

44 344 21

44444 344444 21

θ

γ

ζγ

γ

ζγγω

⎟⎟

⎜⎜

−−−

⎥⎦⎤

⎢⎣⎡ +−

=

21

21tan

2/12222 21

1i

H

n

eH (6)

or

( ) θγ ieHH =

Page 70: Dyn Lect Notes 2007

70

It is convenient to introduce the parameter |)0(||)(|

HHG γ

=

Then it follows from Equation (6) that ( ) ∞→==>→ 10 γζ Gfor

Some other cases are illustrated in figures below.

1 2 3 4

0.5

0.25

0.15

ξ = 1

uωωγ =

-18

-90

0

θ

0

1 2

ζ=

ωωγ =

2

1

3

Page 71: Dyn Lect Notes 2007

71

3.2. Base excitation.

In addition to a directly applied force considered above, the movement of the

base (to which the mass is connected by springs) is also an important

mechanism of forced vibrations.

Examples: structures shaken by earthquakes:

vehicle vibrations due to road roughness.

xmFx &&=Σ

( ) xmxcxxk B &&& =−−−

or

m

tkbxxx nnωωζω cos2 2 =++ &&& (7)

Equation (7) is the same as Equation (1), but 0F~ is replaced by mkb .

m

Bk

xc &

x

XB = bcosωt

k(x -xB)

B k

x

Page 72: Dyn Lect Notes 2007

72

Another example of base excitation: a vehicle suspension.

Let us discard static forces due to static equilibrium. Then

( ) ( ) xmxxcxxk BB &&&& =−−−− (8)

Let us now make the substitution: z = x – xB. Then

tbmxmkzzczm B ωω cos2=−=++ &&&&& (9)

The solution of Equation (9) is (see Equations (4) – (6))

tieHbtz ωωω )()( 2= (10)

( ) ( ) ( ) ( )ζγγωωωω θ

iHoreHH

n

i

21122 +−

== ,

where γ = nωω

Now let us find x = z + xB .

m m X

XB =bcosωt ( )Bxxc && − ( )Bxxk −

Page 73: Dyn Lect Notes 2007

73

( )

( )

( )( )

ti

ti

titi

ei

ib

eHb

beeHbx

ω

ω

ωω

ζγγ

ζγω

ωω

ωω

2121

1

2

22

2

+−

+=

=⎟⎟⎠

⎞⎜⎜⎝

⎛+=

=+=

(11)

( ) ( )θ

ζγγ

γζ

ζγγ

ζγ

i

B

B

exxor

ii

xx

222

22

2

21

41

2121

+−

+=

+−

+=

, (12)

⎟⎟⎠

⎞⎜⎜⎝

+−

−= −

222

31

412tan

γζγ

ζγθwhere (13)

One can see that

21 >=<nB

ifxx

ωωγ

1

2

2 431 2

0.25

1=ζ

Bxx

nωωγ =

Page 74: Dyn Lect Notes 2007

74

Consider the simplest model of a vehicle on a rough road.

[ ]Hz

Lvfor

Lvwhere

tbL

vtbxB

==

=⎟⎠⎞

⎜⎝⎛=

πω

ωπ

2

cos2cos

For a smooth ride it should be:

mk

Lvor

n222 >> π

ωω

3.3. Vibrations due to rotating imbalance.

The vertical displacement of m is x + e sinωt

m υ

b

k c

y

υt L

m ω e

2k

x

M

C 2k

An eccentric mass m is present, with the eccentricity e M is the whole mass, including m.

Page 75: Dyn Lect Notes 2007

75

Then, applying Newton’s second law, one can get:

( ) ( ) xckxtexdtdmxmM &&& −−=++− ωsin2

2,

or tmekxxcxM ωω sin2=++ &&& , (14)

or tMmexxx nn ωωωζω sin2 22 =++ &&& (15)

Mkwhere n =ω

The solution of Equation (15):

( ) ( )

( )θωζγγ

γ+

+−= tM

me

x sin21 222

2

(16)

⎟⎟⎠

⎞⎜⎜⎝

⎛−

−= −2

1

12tan

γζγθwhere

Note that vibrations are low at low angular velocities ω of rotation. They

achieve maximum value at ω slightly higher than ωn.

1

1 2 3 4

2

0.05

0.25

0.5

1=ζ

nωωγ =

⎟⎠⎞

⎜⎝⎛

Mmex

Page 76: Dyn Lect Notes 2007

76

VI. VIBRATION OF RIGID BODIES.

This is a general situation when consideration of a body as a particle is no

longer valid. This means that both translation and rotation of a body should be

taken into account.

1. TYPICAL EXAMPLES

1.1. Physical pendulum.

Then 0sin2

=+ θθog

cm

r

gr&& . 22

og

cmn

rgr

=∴ ω

If to assume that the whole mass m is concentrated in G, then cmog rr =

and we arrive to the already familiar equation of mathematical pendulum:

ωn2 = g/rcm .

G

0

θ

mg

rcm

0sin

sin

=+

=−∴

θθ

θθ

θ

o

cm

ocm

oo

Imgr

or

Imgr

IM

&&

&&

&&

As was mentioned earlier, it is convenient to represent 2

ogo mrI = , where ogr is the radius of gyration of a body about 0

Page 77: Dyn Lect Notes 2007

77

1.2. Log suspended via two ropes

Let us use Lagrange’s equation:

( )2221

21 ϕ&lmmv ==Τ ϕ=1q

ϕϕϕ

ϕϕ

ϕϕ

ϕ

sin;0

;

cos

22

mglV

mldtdml

mglV

=∂∂

=∂

Τ∂

=⎟⎟⎠

⎞⎜⎜⎝

⎛∂

Τ∂=

∂Τ∂

−=

&&&

&&

0sin

0sin:.. 2

=+∴

=/+/

ϕϕ

ϕϕ

lg

glmlmEL

&&

&&

For small ϕ : sinϕ ~ ϕ

lg

nn ==+∴ ωϕωϕ ,02&&

mg

m

ϕ

Τ Τ

l l

This is the same equation as the equation of Mathematical Pendulum, because there is no rotation in this example.

Page 78: Dyn Lect Notes 2007

78

1.3. Log suspended via two rods (Problem 8/124, M&K, 5ed)

Use Lagrange’s equation again:

( )

ϕϕϕϕ

ϕϕϕ

ϕϕ

ϕϕ

&&&&&&&

&&&

&&

222

22

222

~32~

32

2~31

cos2

~2cos

~31

212

21

lmmlmmldtd

lmml

lgmmglV

lmlm

⎟⎠⎞

⎜⎝⎛ +==+=⎟⎟

⎞⎜⎜⎝

⎛∂

Τ∂

+=∂

Τ∂

−−=

⎟⎠⎞

⎜⎝⎛+=Τ

( )

( ) 0sin~~32

:..

sin~sin~sin

0

2 =++⎟⎠⎞

⎜⎝⎛ +

+=+=∂∂

=∂

Τ∂

ϕϕ

ϕϕϕϕ

ϕ

glmmlmm

EL

glmmglmmglV

&&

or

mg

m

ϕ

m~ l l m~ 2~

31 lmI R =

Page 79: Dyn Lect Notes 2007

79

0sin~

32

~=

+

++ ϕϕ

lg

mm

mm&&

For small ϕ : sinϕ ~ ϕ,

⎟⎟⎟⎟

⎜⎜⎜⎜

+

+=

=+∴

mm

mmlgwhere n

n

~32

~

,02

ω

ϕωϕ&&

If m~ = 0, then ,lg

n =ω as in the previous example.

If m = 0, then lg

n 23

Compare the latter expression with ωn for a single rod.

Indeed, let us recall the Example 1.1: (Physical pendulum).

But for a rod, rcm = 2l and 2~31 lmIr =

Hence lg

lm

mlgn 2

3~

31

~2

.

2=

/

//

=/

ω ,

i.e. the values of ωn are the same, as expected.

m~

ϕ

l cmr

If we assume that I0 = Ir, then it follows from Equation (1) that for small ϕ

r

cmn I

mgr ~=ω G

Page 80: Dyn Lect Notes 2007

80

1.4. Bar with a torsional spring.

( )( ) 2

2

2

312

0

312

~sin:31sin

2

mlmglk

ml

kmglsmallFor

mlmglk

IM

n

o

−=∴

=+−

+∴

=+−

ω

ϕϕ

ϕϕϕ

ϕϕϕ

ϕ

&&

&&

&&

Thus, the minimum k is ( 2l )mg. Let us look at what it means.

Consider the potential energy of the system under consideration:

ϕ+ϕ= cosmg2lk

21V 2

Let us find a minimum of V, which, as we know, corresponds to the condition

of stability of the system:

0,0sin2

=∴=−= ϕϕϕϕ

mglkddV

For 0=ϕϕddV to have a minimum (and not a maximum!) it should be:

k

m ϕ

l

Equilibrium position at ϕ=0. Find natural frequency of small vibrations. Show that there is a minimum k below which the natural frequency is not a real number.

Page 81: Dyn Lect Notes 2007

81

or 02

cos2

Statics): Mech. Eng. (see00

002

2

2

2

>−=−=

>=

==

mglkmglkd

Vd

dVd

ϕϕ

ϕϕ

ϕϕ

Thus, k > mg2l is the condition of stability. As we have seen above, this is

reflected also in the requirement for ωn to be real.

2. ENERGY METHOD OF DETERMINING THE FRQUENCY OF VIBRATION

For conservative systems:

constV =+Τ=Ε

Since Τ changes from 0 to Τmax = Ε, whereas V changes from Vmax = Ε

to 0, it is clear that Ε==Τ maxmax V . The equality Tmax = Vmax can be

used for determining the natural frequency of the system.

Example of a simple harmonic oscillator

( )

( )2maxmax

2maxmax

2121

xkV

xm

=

=Τ &

But for harmonic oscillations

( )ψω += txx ncos.max it follows that maxmax xx nω=& .

Then, using the equality Tmax = Vmax, we obtain:

( ) ( )

mk

xkxm

n

n

=∴

=

ω

ω 2max

2max 2

121

as expected.

Page 82: Dyn Lect Notes 2007

82

2.1. Rocking motion of a semi-disk: comparative analysis by energy method and by means of Lagrange’s equations

Using energy method ( ) ( )[ ]

( )θπ

θ

cos134

cosmax

−⎟⎠⎞

⎜⎝⎛=

=−−−=

rmg

rrrrmgV

( ) ( )

( )3D Table see21

21

2

222

02

max

mrI

rrmrmIrrmII

I

o

Iorc

c

r

=

−+−=−+=

=Τ=

43421

θ

( ) 22maxmax

222

38

23

21cos1

34:

38

232

21

θπ

θπ

π

&rmrgmV

mrrmrmrmrIc

/⎟⎠⎞

⎜⎝⎛ −=−⎟

⎠⎞

⎜⎝⎛

/=Τ

⎟⎠⎞

⎜⎝⎛ −=−+=∴

gr

rgHence

rg

nn

n

n

78.72;807.0

34

43

211

34

: nsoscillatio harmonicFor 21~cos : smallFor

222

max

2

===

⎟⎠⎞

⎜⎝⎛ −=

⎥⎥⎦

⎢⎢⎣

⎡⎟⎟⎠

⎞⎜⎜⎝

⎛−−∴

=

ωπτω

ωθπ

θπ

θωθ

θθθ&

c mg

r

G r

0

θ− cosrr

Find the period τ of small oscillations of the semi-disk shown in the Figure ( )3,&

34 DableKMrr Τ=π

θ

Page 83: Dyn Lect Notes 2007

83

A more general approach to the solution of this problem using Lagrange's equation.

( )θcosrrmgV −= q1 = θ

( ) 2.21 θθ &cI=Τ

Use Taylor’s series expansion for Ic (θ):

1 ( ) ( ) ( ) ...00 ' ++= θθ ccc III

( )

( )[ ] ( ) ( )θθθθθθ

θθθ

θθθ

θθθ

&&&&&&

&&&&&

&&

0 smallfor ~..00)0(~

~.)

)()

''cccc

cc

c

IIII

II

dtdb

Ia

++

∂∂

+=⎟⎠⎞

⎜⎝⎛

∂Τ∂

=∂

Τ∂

( )

θθθ

θθθ

θθ

.~sin)

smallfor 0~.0

21~.

)0(21) 2'2

rmgrmgVd

II

c cc

=∂∂

∂∂

=∂

Τ∂ &&

L. E. :

( )

( )0

0

0.02

cn

n

c

Irmgwhere

or

rmgI

=

=+

=+

ω

θωθ

θθ&&

&&

Now use the expression for r and Ic(0) from the first part of this example:

π3

4rr = and ( ) 238

230 mrII cc ⎟

⎠⎞

⎜⎝⎛ −==

π

0 0

for small θ

Page 84: Dyn Lect Notes 2007

84

Then rg0.807

38

23

34

38

23

34

2=

⎟⎠⎞

⎜⎝⎛ −

=/⎟

⎠⎞

⎜⎝⎛ −

⎟⎠⎞

⎜⎝⎛

/=

π

π

π

πωrg

rm

rgmn

Hence

gr

n78.72

==ω

πτ

As expected, the results for ωn and τ are the same. However, the L. E.

approach provides a more comprehensive insight into the problem.

Page 85: Dyn Lect Notes 2007

85

VII SYSTEMS WITH TWO OR MORE DEGREES OF FREEDOM

1. FREE VIBRATIONS

Consider the following 2 –DOF System:

Use second Newton’s Law for each mass:

( )1221111 xxkxkxm −+−=&& (1)

( ) 2312222 xkxxkxm −−−=&& (2)

Let us seek the solution in the form:

titi eAxeAx ωω2211 ; == (3)

Substitute equations (3) into (1) and (2):

( )[ ] 022112

21 =−−+ AkAmkk ω (4)

( )[ ] 0222

3212 =−++− AmkkAk ω (5)

m2 m1

k2 k1 k3

x1 x2

Page 86: Dyn Lect Notes 2007

86

For the system of homogeneous equations (4), (5) to have a non-trivial

solution ( 0A,0A 21 ≠≠ ), the determinant of the system must be zero:

( )[ ]

( )[ ]22

322

212

21

mkkk

kmkk

ω

ω

−+−

−−+ = 0 (6)

or

( )( ) ( ) ( ) 02221

42

221321

23221 =−++−+−++ kmmmkkkkmkkkk ωωω

(7)

or

021

3231212

2

32

1

214 =++

+

⎥⎥⎥⎥

⎢⎢⎢⎢

⎡+

++

−444 3444 21

444 8444 76

c

b

mmkkkkkk

mkk

mkk

ωω (8)

Introducing the notation λω =2 , we can rewrite Equation (8) as:

cbb

cb

−±=∴

=+−

42

02

2,1

2

λ

λλ

For illustration purposes, let us assume that

m2m,mmandkkkk 21321 ===== (see book of Thomson, Section 5.1)

Then 2

23,3 ⎟

⎠⎞

⎜⎝⎛==

mkc

mkb , and

mk

mk

mk

mk

366.223

23

634.023

23

2

1

=⎟⎟⎠

⎞⎜⎜⎝

⎛+=

=⎟⎟⎠

⎞⎜⎜⎝

⎛−=

λ

λ

Page 87: Dyn Lect Notes 2007

87

Hence

( )mk634.011 == λω (9)

( )mk366.222 == λω (10)

These are the natural frequencies of the system. Now return back to

Equations (4) and (5) and substitute ω1 and then ω2 into any of them,

e.g. into Equation (4):

( ) mk

kmkk

kAA

21

221

2

2

1

2 ωω −=

−+=

Then, for ( )

731.0634.01

2

121 =⎟⎟

⎞⎜⎜⎝

⎛=>=

AA

mkω

for 73.2366.2)2(

2

122 −=⎟⎟

⎞⎜⎜⎝

⎛=>=

AA

mkω

Thus, each of the two natural frequencies of the system, ω1 and ω2,

corresponds to the specific ratio of the amplitudes, ( )( ) ( )( )221

121 A/AandA/A

respectively. Such specific distributions of amplitudes associated with the

corresponding natural frequencies are called the normal modes of the

system. It is convenient to choose 1A2 = . Then, one can show the modes as

follows:

A1 A2

1 0.731

mk634.0w2

1 = -2.73

A2

A1

1

mk366.2w2

2 =

Page 88: Dyn Lect Notes 2007

88

Note that in mathematical terminology, instead of natural frequencies and

normal modes, the more general definitions are used – eigenvalues and

eigenvectors respectively.

2. MATRIX NOTATION

It is convenient to rewrite the initial equations, Equations (1) and (2), in the

form:

( )

( ) ⎭⎬⎫

⎩⎨⎧

=⎭⎬⎫

⎩⎨⎧

⎥⎦

⎤⎢⎣

⎡+−

−++

⎭⎬⎫

⎩⎨⎧

⎥⎦

⎤⎢⎣

⎡00

00

2

1

322

221

2

1

2

1xx

kkkkkk

xx

mm

&&

&& (11)

or

}0{}]{[}]{[ =+ XKXM && (12)

[M] is called the mass matrix, and [K] is called the stiffness matrix. The matrix notation, Equation (12), is especially useful for systems with many

degrees of freedom (more than two)

Using the amplitude vector {A} = ⎭⎬⎫

⎩⎨⎧

2

1AA

, one can rewrite Equation (12):

( ) }0{}{][][2 =+− AKMω (13)

Then the equation for natural frequencies is

0][][2 =+− KMω (14)

Page 89: Dyn Lect Notes 2007

89

3. SOME PRACTICAL EXAMPLES 3.1. 2-DOF vehicle model for bounce and pitch.

Derive Lagrange’s equations:

( ) ( )

0,,

21

21

21

21

222

211

22

=∂Τ∂

=⎟⎠⎞

⎜⎝⎛

∂Τ∂

=∂Τ∂

++−=

+=Τ

zzm

zdtdzm

z

lzklzkV

Izm

&&&

&&

&&

θθ

θ

( ) ( )

0,,

2211

=∂

Τ∂=⎟

⎠⎞

⎜⎝⎛

∂Τ∂

=∂

Τ∂

++−=∂∂

θθ

θθ

θ

θθ

&&&

&&

IdtdI

lzklzkzV

( )( ) ( ) 222111 llzkllzkV θθθ

++−−=∂∂

bounce

pitch G

k1 k2 1l 2l

G

Z

θ k1 k2

θ− 1lz θ+ 2lz equilibrium

mNkmNk

mlml

mr

mrI

kgm

g

g

4000035000

8.1;5.1

2.1

1500

2

1

21

2

==

==

=

=

=

θ==

2

1q

zq

Page 90: Dyn Lect Notes 2007

90

L. E. :

( ) ( )( ) ( ) 0

0

222111

2211

=++−−

=++−+

llzkllzkI

lzklzkzm

θθθ

θθ&&

&&

Let us seek the solution in the form:

tio

tio eeZz ωω θθ == , . Then

( ) ( )( ) ( ) ⎭

⎬⎫

⎩⎨⎧

=⎭⎬⎫

⎩⎨⎧

⎥⎥⎦

⎢⎢⎣

−+−−−−−+

00

2222

2112211

22112

21

o

ozIlklklklk

lklkmkkθω

ω

Equalising the determinant of the matrix to zero, we obtain:

( ) 022211

2222

211

221

2

=−−⎟⎟⎟

⎜⎜⎜

⎛−+

⎟⎟⎟

⎜⎜⎜

⎛−+

44342143421321cba

lklkIlklkmkk ωω

Using the notations a, b and c2, we rewrite this equation in the form

( )( )

0

0

2422

222

=−+−−

=−−−

cmIIambab

orcIbma

ωωω

ωω

Let us solve this equation versus ω.

Simplify it first:

0

~

22

~

4 =−

++

−4342143421

cb

mIcab

mIaImb ωω

Introduce Then.2 λω =

Page 91: Dyn Lect Notes 2007

91

cbb

cbb

cbb

cb

~4

~

2

~

~4

~

2

~

~4

~

2

~0~~

22

21

22,1

2

−+=

−−=

−±=∴

=+−

λ

λ

λ

λλ

and 22

11

λω

λω

=

=

Substitute the numerical values of the parameters. Then the results for the

natural frequencies are:

[ ]

[ ]Hzf

Hzf

582.12

098.12

22

11

==

==

πωπ

ω

The amplitude ratios corresponding to the frequencies 21 and ωω

:are)fandfor( 21

⎥⎦⎤

⎢⎣⎡=

−+

−=⎟⎟

⎞⎜⎜⎝

⎥⎦⎤

⎢⎣⎡−=

−+

−=⎟⎟

⎞⎜⎜⎝

radm

mkk

lklkZ

radm

mkk

lklkZ

o

o

o

o

266.0

412.5

2221

2211

2121

2211

2

1

ωθ

ωθ

ω

ω

Page 92: Dyn Lect Notes 2007

92

Mode shapes:

Mostly translation

Mostly rotation

3.2. Symmetrical 2-DOF system. It is instructive to consider a symmetrical 2-DOF system. For example, let us

consider the system shown in the Figure.

The conditions of symmetry in this case are:

mmmkkk ==== 2131 ,

equilibrium

ω1:

equilibriumω2

m2 m1

k2 k1 k3

x1 x2

Page 93: Dyn Lect Notes 2007

93

The equations of this system for the general case of arbitrary m1, m2 and k1,

k2 , k3 have been derived in the previous section. In the symmetric case

under consideration we have for the coefficients:

2

222 2,2m

kkkcm

kkb +=

+=

mk

mkk

m

kkkkkkkm

kk

cbb

22

222

222

22

22

2,12,1

22

42

±+

=

=/−//−+//+/

±+

=

=−±== ωλ

Thus,

mkk

mk

mk

mk

mk

22

2222

1211

2;2

;

+=+==

===

ωωλ

ωωλ

Now determine :212

1 ωω andforAA

( )( )

( )1

2:2

1:

22

22

2

122

2

21

2

11

22

2

2

1

−=−−+

=⎟⎟⎠

⎞⎜⎜⎝

⎛+=

=/

/−+

=⎟⎟⎠

⎞⎜⎜⎝

⎛=

=>−+

=

mmkm

mkkk

kAA

mkk

mmkkk

kAA

mk

mkk

kAA

ω

ω

ω

Obviously, the first mode (frequency ω1) is anti-symmetric, and the second

mode (frequency ω2) is symmetric. Generally, in all symmetric systems

there are symmetric and anti-symmetric modes.

Page 94: Dyn Lect Notes 2007

94

4. INITIAL CONDITIONS

Let us return to the example considered in Section 1 for the particular case

m2 = 2m1 = 2m, k1 = k2 = k3 = k.

⎩⎨⎧−

=Φ=

⎩⎨⎧

=Φ=

000.1732.2

,366.2

000.1731.0

,634.0

22

11

mk

mk

ω

ω

For general initial conditions a free vibration of the system contains both

modes simultaneously:

( ) ( )2221112

1 cos000.1732.2

cos000.1731.0

ϕωϕω +⎭⎬⎫

⎩⎨⎧−

++⎭⎬⎫

⎩⎨⎧

=⎭⎬⎫

⎩⎨⎧

tctcxx

(1)

Equations (1) are the two equations giving the solutions for x1 and x2.

Parameters 2121 and,c,c ϕϕ are the four necessary constants required

for two differential equations of the second order.

To find all four constants we need another two equations for 21 xandx && ,

which are obtained by differentiating Equations (1).

m2 m1

k2 k1 k3

x1 x2

Page 95: Dyn Lect Notes 2007

95

( ) ( )222211112

1 sin000.1732.2

sin000.1731.0

ϕωωϕωω +⎭⎬⎫

⎩⎨⎧−

−+⎭⎬⎫

⎩⎨⎧

−=⎭⎬⎫

⎩⎨⎧

tctcxx&

& (2)

Specifying the initial conditions at t=0, one can find from Equations (1) and (2)

the values of 2121 and,c,c ϕϕ .

For example, let the initial conditions are

( )( )( ) ⎭

⎬⎫

⎩⎨⎧

=⎭⎬⎫

⎩⎨⎧

⎭⎬⎫

⎩⎨⎧

=⎭⎬⎫

⎩⎨⎧

00

0x0x

and00.1

c0x)0(x

2

11

2

1

&

&

Then, it follows from Equations (1), (2) that

( )( ) 2211 cos

000.1732.2

cos000.1731.0

00.1

III

ϕϕ⎭⎬⎫

⎩⎨⎧−

+⎭⎬⎫

⎩⎨⎧

=⎭⎬⎫

⎩⎨⎧

cc

( )( ) 222211 sin

000.1732.2

sin000.1731.0

00

IVIII

ϕωϕω⎭⎬⎫

⎩⎨⎧−

−⎭⎬⎫

⎩⎨⎧

−=⎭⎬⎫

⎩⎨⎧

cc

These are the four equations to determine 2121 ,,c,c ϕϕ .

( ) ( )( )

( ) ( )( )( )

( )( ) ( )

( ) 222

111

22

11

sin731.0732.20:III731.0(IV)

sin732.2731.00:III732.2(IV)

cos731.0732.20.1:I)(731.0II

cos732.2731.00.1:I732.2II

ϕω

ϕω

ϕ

ϕ

−−−=+−

+−=+

−−=+−

+=+

cx

cx

cx

cx

It follows from the last two resulting equations that

Page 96: Dyn Lect Notes 2007

96

1coscos0

0sinsin

2121

21

====

==

ϕϕϕϕ

ϕϕ

andor

Then from the first two equations:

289.0

463.31

732.2731.00.1

289.0463.31

732.2731.00.1

2

1

−=−=+

−=

==+

=

c

c

Thus

0,0

289.0,289.0

21

21

==−==

ϕϕcc

N.B. Even if only one of the masses (on the left) has been displaced initially,

the resulting free vibration involves movements of both masses.

Typical behaviour of a 2-DOF system

x1,x2

0

t

x1

x2

Page 97: Dyn Lect Notes 2007

97

5. FORCED HARMONIC VIBRATIONS

Consider a 2-DOF system described by the matrix equation.

tF

xx

kkkk

xx

mm

ωcos00

0 1

2

1

2221

1211

2

1

2

1

⎭⎬⎫

⎩⎨⎧

=⎭⎬⎫

⎩⎨⎧

⎥⎦

⎤⎢⎣

⎡+

⎭⎬⎫

⎩⎨⎧

⎥⎦

⎤⎢⎣

⎡&&

&& (3)

As before, for simplicity, we consider a system without damping.

Let us look for a steady-state solution of Equations (3) in the form.

tXX

xx

ωcos2

1

2

1

⎭⎬⎫

⎩⎨⎧

=⎭⎬⎫

⎩⎨⎧ (4)

Substitute Equation (4) into (3):

( )( ) ⎭

⎬⎫

⎩⎨⎧

=⎭⎬⎫

⎩⎨⎧

⎥⎥⎦

⎢⎢⎣

−−

01

2

12

22221

122

111 FXX

mkkkmk

ωω (5)

If to introduce the notation

( )[ ] ( )( )⎥⎥⎦

⎢⎢⎣

−−= 2

22221

122

111ω

ωωmkk

kmkz ,

then we can rewrite Equation (5) as:

( )[ ]⎭⎬⎫

⎩⎨⎧

=⎭⎬⎫

⎩⎨⎧

01

2

1 FXX

z ω (6)

Page 98: Dyn Lect Notes 2007

98

5.1. Construction of the inverse matrix.

Equation (6) can be solved versus X1, X2 using the following formal

operation: multiplying both sides of Equation (6) by the inverse matrix

( )[ ] 1−ωz , so that

( )[ ]⎭⎬⎫

⎩⎨⎧

=⎭⎬⎫

⎩⎨⎧ −

011

2

1 Fz

XX

ω (7)

In deriving Equation (7) we used the property

( )[ ] ( )[ ] [ ] [ ] ⎥⎦

⎤⎢⎣

⎡==−

1001

I,I1 wherezz ωω

How to find ( )[ ] 1wz − ? According to matrix algebra,

( )[ ] ( )[ ][ ])(det

1ωωω

zzadjz =− ,

where ( )[ ]ωzadj is the adjoint matrix of the square matrix ( )[ ]ωz

The adjoint matrix ( )[ ]ωzadj is defined as a transpose of the matrix of

cofactors of ( )[ ]ωz . If

( )[ ] ⎥⎦

⎤⎢⎣

⎡=

2221

1211zzzz

z ω , (8)

then the cofactor ji

c is defined as

( )jj i

jii Mc +−= 1 ,

where ji

M is a minor of the element ji

z .

Page 99: Dyn Lect Notes 2007

99

For the matrix ( )[ ]ωz defined by Equation (8):

( )( )( )( ) 1111

2222

121212

21

212121

12

222211

11

1

1

1

1

zzC

zzC

zzC

zzC

=−=

−=−=

−=−=

=−=

+

+

+

+

Thus [ ]cofactorsof

matrixthezzzz

C ⎥⎦

⎤⎢⎣

⎡−

−=

1112

2122

and [ ]cofactorsofmatrix

transposedthezzzz

C T⎥⎦

⎤⎢⎣

⎡−

−=

1121

1222

Then

( )[ ] [ ] ( )( )⎥⎥⎦

⎢⎢⎣

−−−−=⎥

⎤⎢⎣

⎡−

−== Τ

211121

122

2221121

1222

ωωω

mkkkmk

zzzz

Czadj

It is convenient also to transform det ( )[ ]ωz as a product

( )[ ] ( )( )222

22121det ωωωωω −−= mmz ,

where ω12 and ω2

2 are the solutions of the algebraic equation ( )[ ] 0det =ωz ,

or

( )[ ] ( )( )

0

det

21124

212

211222

12211

21122

2222

111

=−+−−=

=−−−=

kkmmmkkmkk

kkmkmkz

ωωω

ωωω

Solving the above equation, we can find 21 ωω and , i.e. the normal mode

frequencies:

Page 100: Dyn Lect Notes 2007

100

21

221122122

1

11

2

22

1

11

2

2222,1 4

121

mmkkkk

mk

mk

mk

mk −

+⎟⎟⎠

⎞⎜⎜⎝

⎛+±⎟⎟

⎞⎜⎜⎝

⎛+=ω

Finally, using Equation (7), we obtain:

( )[ ]( )

( ) ⎭⎬⎫

⎩⎨⎧

⎥⎥⎦

⎢⎢⎣

−−−−=

⎭⎬⎫

⎩⎨⎧

0det1 1

211121

122

2222

1 F

mkkkmk

zXX

ωω

ω

or

( )

( )222

22121

12

2221

)( ωωωω

ω

−−

−=

mm

FmkX

(9)

( )( )222

22121

1122

ωωωω −−

−=

mm

FkX

1

121

Fkx

1

122

Fkx

1ωω

3 2 1

1

121

Fkx

1

122

Fkx

Page 101: Dyn Lect Notes 2007

101

5.2 Representation in terms of normal mode summation. Let us rewrite Equations (9) for amplitudes of forced vibrations in the form:

( )( )( ) 22

2

222

1

122

222

121

12

2221

ωωωωωωωω

ω

−+

−=

−−

−=

cc

mm

FmkX (10)

( ) 222

422

1

322

222

121

1122

)( ωωωωωωωω −+

−=

−−

−=

cc

mm

FkX (11)

Find 4321 c,c,c,c

(a) Multiply Equation (10) by 221 ωω − and then let 1ωω = :

( )

( ) 121

2221

121222 c

mm

Fmk=

ωω

ω

(b) Multiply Equation (10) by 222 ωω − and then let 2ωω = :

( )

( ) 222

2121

122222 c

mm

Fmk=

ωω

ω

(c) Multiply Equation (11) by 221 ωω − and then let 1ωω = :

( ) 321

2221

112 cmm

Fk=

ωω

(d) Multiply Equation (11) by 222 ωω − and then let 2ωω = :

422

2121

112

)(c

mm

Fk=

ωω

Thus

( )( )

( )( )

( ) ( ) 222

22

2121

11222

121

2221

1122

222

22

2121

122222

221

21

2221

121222

1

1.1.

1.1.

ωωωωωωωω

ωωωω

ω

ωωωω

ω

−−

−+

−−

−=

−−

−+

−−

−=

mm

Fk

mm

FkX

mm

Fmk

mm

FmkX

Page 102: Dyn Lect Notes 2007

102

5.3. Principle of tuned vibration absorber

To understand the principle of tuned vibration absorber we can use the

general matrix equation (Equation (3)) in which we have to specify

22211211 k,k,k,k . To do so, let us derive the equations for the above

system.

( )

( )( ) :

cos~:

222

11212111

111

xmF

xmxxktFxk

xmF

x

x

&&

&&

&&

=−−+−

ω (12)

( ) 22122 xmxxk &&=−−

or

( )0

cos~

221222

12212111=+−

−=−++xkxkxm

tFxkxkkxm&&

&& ω (13)

Compare Equations (13) with Equation (3). Then

11222221

2122111 F~F:kk,kkkk,kkk

−==−=

−=+=

m2 m1

k2 k1

x1 x2 tF ωcos~1

x

Page 103: Dyn Lect Notes 2007

103

Now we can use the general solution (Equation (9) ) for the amplitudes:

( )( )( )

( )( )( )( )22

222

121

12

2222

222

121

12

2221

~

ωωωω

ω

ωωωω

ω

−−

−−=

−−

−=

mm

Fmk

mm

FmkX (14)

( )( )( )

( )( )222

22121

1222

222

121

1122

~

ωωωωωωωω −−

−=

−−

−=

mm

Fk

mm

FkX (15)

It follows from Equation (14) that X1 = 0 if k2 – m1ω2 = 0, i.e. this happens

at frequency 2222 ωω == mk . Note that the frequency 2222 mk=ω is

the partial resonant frequency of the second mass, m2. Of course, 02 ≠X

(see Equation (15)). Thus, by changing k2 and m2, one can change the

resonant frequency of maximum absorption.

Page 104: Dyn Lect Notes 2007

104

VIII NON-LINEAR VIBRATIONS

So far we have considered linear vibrations associated with small amplitudes,

for which the dynamic equations can be linearised.

Here we discuss a more general situation of non-linear dynamic equations.

1. PERTURBATION ANAYLSIS OF NONLINEAR PENDULUM Example: Mathematical pendulum.

The equation of motion of mathematical pendulum has

been derived in one of the previous sections:

0sin20 =+ θωθ&& (1)

where gl /20 =ω

For simplicity, let us introduce the notation x = θ and rewrite Equation (1) as

0sin20 =+ xx ω&& (2)

Now let us expand sin x in Taylor’s series:

...61sin 3 +−= xxx

θ

l

m

Page 105: Dyn Lect Notes 2007

105

Assuming that x<<1, we neglect higher order terms in this expansion (higher

than x3) and rewrite Equation (2) as

06

3202

0 =−+ xxxω

ω&& (3)

In further consideration, it is convenient to deal with a more general equation.

0320

20 =++ xxx αωω&& (4)

where α is a constant. Equation (3) thus corresponds to the particular case

of α = - 61 .

Let us seek the solution of Equation (4) by perturbation method:

...22

10 +++= xxxx αα (5)

and

...122

02 +++= gg ααωω (6)

Here x0 and ω0 correspond to the ‘zero’ approximation

00200 =+ xx ω&& ,

and yet unknown functions ....g,g,...x,x 121 describe higher order

corrections.

Keeping only the first order correction in Equation (6) and substituting it into

Equation (4), we can rewrite the latter in the form:

Page 106: Dyn Lect Notes 2007

106

0322 =+−+ xgxxx αωαω&& (7)

The zero approximation for Equation (7) is

002

0 =+ xx ω&& (8)

For the initial conditions at t=0: 0, == xax & , the solution of Equation (8) is

tax ωcos~0 = (8’)

Let us substitute Equation (5) into Equation (7):

0...30

21

201

20

210 =++−−+++ xgxgxxxxx αωαααωωα &&&&

Obviously, the equation of the first approximation is

30

201

21 xgxxx ωω −=+&& (9)

Substituting Equation (81) for x0 into Equation (9) and using the well known

trigonometrical formula

ttt ωωω cos433cos

41cos3 +=

we can rewrite Equation (9) as

tatatgaxx ωωωωωω cos~433cos~

41cos~ 3232

12

1 −−=+&& (10)

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107

In Equation (10), terms with cosωt would cause a resonant growth of x1

proportional to t, which cannot be. Therefore, the terms with cosωt have to

be eliminated.

We can eliminate the terms with cosωt if we choose g in such a way that

0~43~ 32 =− aga ω (11)

Then Equation (10) becomes

taxx ωωω 3cos~41 32

12

1 −=+&& (12)

It follows from Equation (11) that

22 ~43 ag ω= (13)

Substituting Equation (13) into Equation (6), we obtain

...~43 222

02 aαωωω += ,

from which it follows that

2

202

~431 aα

ωω

−= (14)

The particular solution of Equation (12) is

tax ω3cos32

~3

1 =

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108

Then the general solution of Equation (12), i.e. the first approximation solution

is

tatCtCx ωωω 3cos32

~sincos

3

211 ++=

And the complete solution, x = x0 + x1, is

tatCtCtax ωαωαωαω 3cos32

sincoscos3

21 +++= (15)

Constants C1 and C2 can be found from the same initial conditions at t = 0:

x = a, x& =0

Then

tataax ωαωα 3cos32

~cos

32

~1

32

+⎟⎟⎠

⎞⎜⎜⎝

⎛−= , (16)

where (see Equation (14))

2

202

~431 aα

ωω

−=

Now recall that for our particular case of a pendulum 61

−=α . Then, it

follows from Equations (16) and (14) that

tataax ωω 3cos192

~cos

192

~1

32

−⎟⎟⎠

⎞⎜⎜⎝

⎛+= (17)

and

2

202

~811 a+

ω (18)

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109

One can see that:

1. ω decreases for a larger ã

2. Free vibrations are not harmonic (presence of term with 3ω)

Note that the above solution is valid for x<1 (rad) .

ω0

ω

ã

1 2

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110

IX SELF EXCITED OSCILLATIONS

1. SYSTEMS WITH ‘NEGATIVE FRICTION’ 1.1. A mass on the moving belt

Consider a simple example of a mass m placed on the moving belt. Let us

assume that the kinetic friction force F is a function of the relative velocity

( )xvFFeivxv && −==− 00 .., . Apply Newton’s second law:

( )xvFkxxcxm &&&& −=++ 0 (1)

Here 2121 , ccckkk +=+= (for clarity dashpots are not shown in the

Figure).

m

x k1 k2

F v0

belt

( )xvF 0 &−

0 xv0 &−

Exp. data

Page 111: Dyn Lect Notes 2007

111

Let us assume that 0vx <<& . Then

( ) ( ) ( ) ...' 000 +−=− vFxvFxvF &&

Rewrite Equation (1):

( )[ ] ( )00' vFkxxvFcxm =+++ &&& .

The term ( )0vF = const, and it is only causing a static displacement

( ) kvFxst /0= . If v0 is not too large, then ( ) 0' 0 <vF and it is possible that

( ) 0' 0 <+ vFc as well, which means that the system has a ‘negative friction’.

Then for a dynamic displacement x we have

0=++ kxxxm &&& α , (2)

where

( )[ ] 0' 0 <+= vFcα

Equation (2) with α<0 describes the increase of the amplitude of vibration

with time t. Let us introduce

mkwhere

m nn

== ωω

αξ ,2

~

Then we can rewrite Equation (2) as

0~2 2 =++ xxx nn ωωξ&&

( )ϕω

ξξ

ωξ+=

<<

tCex

thenandIf

ntn cos

,1~0~

~

(3)

Page 112: Dyn Lect Notes 2007

112

In real situations the amplitude becomes stable for larger t due to

nonlinearity (we did not consider that range of t)

The mechanism of ‘negative friction’ is responsible, in particular, for

generating string vibrations by bow movement and for the associated

structure-borne sound of violins, cellos, etc. It also causes brake squeal and

many other types of noise and vibration.

Instability

t

x

t

x

Page 113: Dyn Lect Notes 2007

113

1.2. Froude’s pendulum

This is a similar example for rotational movement:.

The value of 0ϕ for equilibrium position ( 0=ϕ=ϕ &&& ) can be obtained from

the equation:

( )Ω=ϕ Fsinmgl 0 .

Let us assume that

( ) ,.cossin~sin;

000

0ψϕϕψϕ

ψϕϕ+−+

+= then

and the resulting equation takes the form

( )[ ] 0.cos' 0 =+Ω++ ψϕψψβ

mglFbI &43421

&& (4)

or

020 =++ ψψγψ wI &&& , (5)

where I

mglI

020

cos,

ϕωβγ ==

If ( ) 0' <ΩF it may be that 0<γ as well. Then we have the same time

behaviour as in the previous example.

Ω

ϕ

G

l Let the moment of the friction force

( ) )( ϕϕ && −Ω=−Ω FM F Then ( )ϕϕϕϕ &&&& −Ω=++ FmglbI sin , where b is the damping coefficient

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114

2. SIMPLE THEORY OF WING FLUTTER: 2-DOF MODEL.

Flutter is a type of dynamic instability of coupled bending and torsional

vibrations of a wing that can develop at high speeds of air flows.

Let us consider a simple 2-DOF model of wing flutter (following R. Granger

1991)

2.1. Coupled bending and torsional vibrations. Let us first consider free vibrations (no air flow) of this 2-DOF system.

Lagrange’s equations for free vibrations are:

0

0

=++

=++

αα

α

αkIhS

hkShM h

&&&&

&&&&. (1)

Let us introduce the partial frequencies:

IkandMkhh // ααωω == ,

kh

G h

e.a.

v

α dMrI

rdMSdMMhere

khkV

hSIhMT

S

SS

h

∫∫

=

==

+=

++=

2

22

2.2.

,21

21

21

21

α

αα

α

&&&&

Page 115: Dyn Lect Notes 2007

115

and let us seek the solution in the form:

titi AeHeh ωω α == , .

Substituting the above expressions into Equations (1) and equalising the

resulting determinant to zero,

( ) ( ) 0242 =++−− αα ωω kkIkMkSMI hh ,

one can obtain the two natural frequencies of the system: ω1 and ω2 , and

the corresponding mode shapes: ( )( )1/ AH and ( )( )2/ AH .

2.2. Effects of aerodynamic lift and moment

Now let us take into account the aerodynamics. This can be done by adding

the appropriate generalised forces to the right-hand side of Equations (1)

MkIhS

LhkShM h

=++

=++

αα

α

α&&&&

&&&& (2)

where L and M are aerodynamic lift and moment respectively.

The simplest expressions for L and M are:

...

...

++++=

++++=

αα

αα

αα

αα

&&

&&

&&

&&

MMhMhMM

LLhLhLL

hh

hh (3)

Here αααα &&&& MMMMLLLL hhhh ,,,,,,, are the coefficients that

depend on aircraft speed v and wing parameters.

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116

Now Equation (2) can be rewritten in the form

( )( ) 0

0

=−−+−−+

=−−+−−+

hMMkMhMIhS

LhLkLhLShM

hh

hhh

ααα

ααα

ααα

αα

&&&&&&

&&&&&&

&&

&& (4)

Equations (4) describe the equivalent ‘free’ 2-DOF system in which the

inertial, stiffness and damping coefficients are modified by aerodynamic

influence.

2.3. Conditions of instability.

Now we are in a position to investigate the conditions of instability of the

solutions of Equations (4) which correspond to the development of flutter.

Note that always M > 0 , I > 0, whereas S may be positive, negative or

zero (for a mass balanced wing).

Other coefficients: ( ) 0,0,0,0,0 =<>−≤≤ hhhh MandLLkML αα&& .

The stability of the system described by Equations (4) (a system of two

simultaneous equations) can be analysed using the general approach (the

Routh method). This approach is convenient because it does not require

direct solution of a system of simultaneous equations.

According to the Routh method, the following expression is to be analysed:

214

230321 AAAAAAAR −−= , (5)

where

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117

( )

( )αα

ααα

ααα

α

MkkA

MkMkLA

SLIkMLMkA

ILMMASMIA

h

hh

hh

h

−=

−−−=

+++=

−−=−=

4

3

2

1

20

&&

&&

&&

(6)

If R > 0, the system is stable.

If R < 0 the system is unstable, i.e. vibration amplitudes grow exponentially

in time.

Thus the condition R = 0 is the borderline case. The corresponding speed

of the air flow (or aircraft) is called the critical flutter speed, cfv .

The problem for an aircraft designer is to design the wings in such a way that

R > 0 in the range of operating speeds v, so that v < cfv . This can be

achieved, in particular, by making the frequency of wing torsional vibrations

much larger than the frequency of bending vibrations.

Page 118: Dyn Lect Notes 2007

118

RECOMMENDED LITERATURE

1. Meriam, J. L. and Kraige, L. G. , Engineering Mechanics, Volume 2

Dynamics (5th Edition), Wiley, 2003.

2. Thomson, W. T., Theory of Vibration with Applications,

Chapman and Hall, 1993.

3. Landau, L. D. and Lifshitz, E. M., Mechanics,

Butterworth- Heinemann, 1995.

4. Beer, F.P., Johnston, E.R., Eisenberg, E.R. and Clausen, W.E.,

Vector Mechanics for Engineers: Statics and Dynamics (8th Edition),

McGraw Hill, 2006.

5. Curtis, H.D., Orbital Mechanics for Engineering Students, Elsevier,

2005.


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