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Fabio ROMANELLI Dept. Earth Sciences Università degli studi di Trieste [email protected] SEISMOLOGY I Laurea Magistralis in Physics of the Earth and of the Environment Harmonic oscillators & 2&N DOF systems: Coupled oscillators 1

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Page 1: Harmonic oscillators 2&N DOF systems: Coupled oscillators · In SHM the total energy (E) of a system is constant but the kinetic energy (K) and the potential energy (U) vary wrt

Fabio ROMANELLI

Dept. Earth Sciences Università degli studi di Trieste

[email protected]

SEISMOLOGY I

Laurea Magistralis in Physics of the Earth and of the Environment

Harmonic oscillators&

2&N DOF systems: Coupled oscillators

1

Page 2: Harmonic oscillators 2&N DOF systems: Coupled oscillators · In SHM the total energy (E) of a system is constant but the kinetic energy (K) and the potential energy (U) vary wrt

Seismology I - Oscillators...

What is a wave?

Small perturbations of a stable equilibrium point

Linear restoring force

Harmonic Oscillation

2

Page 3: Harmonic oscillators 2&N DOF systems: Coupled oscillators · In SHM the total energy (E) of a system is constant but the kinetic energy (K) and the potential energy (U) vary wrt

Seismology I - Oscillators...

Oscillatory Motion

The motion of an object can be predicted if the external forces acting upon it are known.

A special type of motion occurs when the force on the object is proportional to the displacement of the object from equilibrium.

If this force always acts towards the equilibrium position a back and forth motion will results about the equilibrium position.

This is known as periodic or oscillatory motion.

3

Page 4: Harmonic oscillators 2&N DOF systems: Coupled oscillators · In SHM the total energy (E) of a system is constant but the kinetic energy (K) and the potential energy (U) vary wrt

Seismology I - Oscillators...

Familiar examples of periodic motion1. Pendulum

2. Vibrations of a stringed instrument

3. Mass on a springOther examples include

1. Molecules in a solid

2. Air molecules in a sound wave

3. Alternating electric current4

Page 5: Harmonic oscillators 2&N DOF systems: Coupled oscillators · In SHM the total energy (E) of a system is constant but the kinetic energy (K) and the potential energy (U) vary wrt

Seismology I - Oscillators...

Simple Harmonic Motion

If an object oscillates between two positions for an indefinite length of time with no loss of mechanical energy the motion is said to be simple harmonic motion.

Fixed point X=0

Equilibrium

Spring compressed

Spring stretched

Example: Mass on a spring.

5

Page 6: Harmonic oscillators 2&N DOF systems: Coupled oscillators · In SHM the total energy (E) of a system is constant but the kinetic energy (K) and the potential energy (U) vary wrt

Seismology I - Oscillators...

X=0

Spring exerts a force on the mass to restore it to its original position.

F ∝ -x or F = -kx (Hooke’s Law)where k is a +ve constant, the spring constant

F +ve

x -ve

F -ve

x +ve

6

Page 7: Harmonic oscillators 2&N DOF systems: Coupled oscillators · In SHM the total energy (E) of a system is constant but the kinetic energy (K) and the potential energy (U) vary wrt

Seismology I - Oscillators...

A mass under a restoring force

From Newton’s 2nd Law

This is the condition for simple harmonic motion

7

Page 8: Harmonic oscillators 2&N DOF systems: Coupled oscillators · In SHM the total energy (E) of a system is constant but the kinetic energy (K) and the potential energy (U) vary wrt

Seismology I - Oscillators...

Some definitions:The time taken to make one complete oscillation is the period T.

The frequency of oscillation, f = 1/T in s-1 or Hertz

The distance from equilibrium to maximum displacement is the amplitude of oscillation, A.

An object moves with simple harmonic motion (SHM) when the acceleration of the object is proportional to its displacement and in the opposite direction.

8

Page 9: Harmonic oscillators 2&N DOF systems: Coupled oscillators · In SHM the total energy (E) of a system is constant but the kinetic energy (K) and the potential energy (U) vary wrt

Seismology I - Oscillators...

Consider the following:

The general equation for the curve traced out by the pen is x = A cos (ωt + δ)

where (ωt + δ) is the phase of the motion

and δ is the phase constant

x

time

A

-A

9

Page 10: Harmonic oscillators 2&N DOF systems: Coupled oscillators · In SHM the total energy (E) of a system is constant but the kinetic energy (K) and the potential energy (U) vary wrt

Seismology I - Oscillators...

We can show that the expression x = A cos (ωt + δ)

is a solution of by differentiating wrt time

Compare this to a = -(k/m)x

x = A cos (ωt + δ) is a solution if

10

Page 11: Harmonic oscillators 2&N DOF systems: Coupled oscillators · In SHM the total energy (E) of a system is constant but the kinetic energy (K) and the potential energy (U) vary wrt

Seismology I - Oscillators...

We can determine the amplitude of the oscillation (A) and the phase constant (δ) from the initial position xo and the initial velocity vo

The system repeats the oscillation every T seconds

therefore x(t) = x(t+T)

and

The function will repeat when ωT = 2π

11

Page 12: Harmonic oscillators 2&N DOF systems: Coupled oscillators · In SHM the total energy (E) of a system is constant but the kinetic energy (K) and the potential energy (U) vary wrt

Seismology I - Oscillators...

We can relate ω, f and the spring constant k using the following expressions.

ω is known as the angular frequency and has units of rad.s-1

12

Page 13: Harmonic oscillators 2&N DOF systems: Coupled oscillators · In SHM the total energy (E) of a system is constant but the kinetic energy (K) and the potential energy (U) vary wrt

Seismology I - Oscillators...

Time dependence of x, v and a of an object undergoing SHM

v v =-ωAsin(ωt)

t

a a =-ω2Acos(ωt)

t

x x =Acos(ωt)

T/2 T

t

13

Page 14: Harmonic oscillators 2&N DOF systems: Coupled oscillators · In SHM the total energy (E) of a system is constant but the kinetic energy (K) and the potential energy (U) vary wrt

Seismology I - Oscillators...

Energy in Simple Harmonic Motion

In SHM the total energy (E) of a system is constant but the kinetic energy (K) and the potential energy (U) vary wrt.Consider a mass a distance x from equilibrium and acted upon by a restoring force

Kinetic Energy

Potential Energy

Substitute ω2=k/m

14

Page 15: Harmonic oscillators 2&N DOF systems: Coupled oscillators · In SHM the total energy (E) of a system is constant but the kinetic energy (K) and the potential energy (U) vary wrt

Seismology I - Oscillators...

Graphical representation

Potential

Energy

Kinetic

Energy

15

Page 16: Harmonic oscillators 2&N DOF systems: Coupled oscillators · In SHM the total energy (E) of a system is constant but the kinetic energy (K) and the potential energy (U) vary wrt

Seismology I - Oscillators...

Total energy E = K + U

but

In SHM the total energy of the system is proportional to the square of the amplitude of the motion

Total Energy

16

Page 17: Harmonic oscillators 2&N DOF systems: Coupled oscillators · In SHM the total energy (E) of a system is constant but the kinetic energy (K) and the potential energy (U) vary wrt

Seismology I - Oscillators...

Graphical representation

At maximum displacement K=0 ∴ E = UAt equilibrium U=0 and v=vmax ∴ E = KAt all times E = K + U is constant

Average energy = ½E

17

Page 18: Harmonic oscillators 2&N DOF systems: Coupled oscillators · In SHM the total energy (E) of a system is constant but the kinetic energy (K) and the potential energy (U) vary wrt

Seismology I - Oscillators...

Lennard-Jones potential

Potential energy

Interatomic distance

18

Page 19: Harmonic oscillators 2&N DOF systems: Coupled oscillators · In SHM the total energy (E) of a system is constant but the kinetic energy (K) and the potential energy (U) vary wrt

Seismology I - Oscillators...

The Simple Pendulum

A simple pendulum consists of a string of length L and a bob of mass m.

When the mass is displaced and released from an initial angle φ with the vertical it will swing back and forth with a period T.

We are going to derive an expression for T.

19

Page 20: Harmonic oscillators 2&N DOF systems: Coupled oscillators · In SHM the total energy (E) of a system is constant but the kinetic energy (K) and the potential energy (U) vary wrt

Seismology I - Oscillators...

Forces on mass: mg (downwards) tension (upwards)

When mass is at an angle φ to the vertical these forces have to be resolved.

Tangentially:weight = mg sin φ (towards 0)tension = T cos 90 = 0

+ve

0

20

Page 21: Harmonic oscillators 2&N DOF systems: Coupled oscillators · In SHM the total energy (E) of a system is constant but the kinetic energy (K) and the potential energy (U) vary wrt

Seismology I - Oscillators...

we find s = Lφ

+ve

0

Using

From Newton’s 2nd Law (N2)

21

Page 22: Harmonic oscillators 2&N DOF systems: Coupled oscillators · In SHM the total energy (E) of a system is constant but the kinetic energy (K) and the potential energy (U) vary wrt

Seismology I - Oscillators...

+ve

0

or

For small φ sinφ ~ φ

ie SHM with

This has the solution

φ = φo cos (ωt + δ)

22

Page 23: Harmonic oscillators 2&N DOF systems: Coupled oscillators · In SHM the total energy (E) of a system is constant but the kinetic energy (K) and the potential energy (U) vary wrt

Seismology I - Oscillators...

Period of the motion

ie the longer the pendulum the greater the period

Note: T does not depend upon amplitude of oscillation

even if a clock pendulum changes amplitude it will still keep time

23

Page 24: Harmonic oscillators 2&N DOF systems: Coupled oscillators · In SHM the total energy (E) of a system is constant but the kinetic energy (K) and the potential energy (U) vary wrt

Seismology I - Oscillators...

Period of the motion

This is only true for φ < 10o

Generally

Tipler Fig 14-16

24

Page 25: Harmonic oscillators 2&N DOF systems: Coupled oscillators · In SHM the total energy (E) of a system is constant but the kinetic energy (K) and the potential energy (U) vary wrt

Seismology I - Oscillators...

Dark blue pendulum is the simple approximation,

light blue pendulum shows the numerical solution of the nonlinear differential equation of motion.

If the initial angular displacement is significantly large the small angle approximation is no longer validThe error between the simple harmonic solution and the actual solution becomes apparent almost immediately, and grows as time progresses.

25

Page 26: Harmonic oscillators 2&N DOF systems: Coupled oscillators · In SHM the total energy (E) of a system is constant but the kinetic energy (K) and the potential energy (U) vary wrt

Seismology I - Oscillators...

What is a wave?

Small perturbations of a stable equilibrium point

Repulsive Potential ∝ 1/rm

Attractive Coulombic Potential ∝ 1/r

Total Potential

Linear restoring force

Harmonic Oscillation

26

Page 27: Harmonic oscillators 2&N DOF systems: Coupled oscillators · In SHM the total energy (E) of a system is constant but the kinetic energy (K) and the potential energy (U) vary wrt

Seismology I - Oscillators...

What is a wave? - 2

Small perturbations of a stable equilibrium point

Linear restoring force

Harmonic Oscillation

Coupling of harmonic oscillators

AB

0 0

the disturbances can propagate

27

Page 28: Harmonic oscillators 2&N DOF systems: Coupled oscillators · In SHM the total energy (E) of a system is constant but the kinetic energy (K) and the potential energy (U) vary wrt

Seismology I - Oscillators...

Coupled systems

Simplest example: Two identical pendula A and B connected by a light unstretched spring.(a) Move A to one side, while holding B fixed, then release.

AB

0 0

AB

0 0

x

A will oscillate with gradually decreasing amplitude.

28

Page 29: Harmonic oscillators 2&N DOF systems: Coupled oscillators · In SHM the total energy (E) of a system is constant but the kinetic energy (K) and the potential energy (U) vary wrt

Seismology I - Oscillators...

(b) Move A and B to same side by equal amounts then release.

The distance between A and B is constant and equal to the relaxed length of the spring, and the spring exerts no force on either mass.

Each pendulum is essentially free and oscillating with its natural frequency

AB

0 0

xx

AB

0 0Lg

o =ω

29

Page 30: Harmonic oscillators 2&N DOF systems: Coupled oscillators · In SHM the total energy (E) of a system is constant but the kinetic energy (K) and the potential energy (U) vary wrt

Seismology I - Oscillators...

If xA and xB are the displacements of A and B resp.The equations of motion are

ie both masses vibrate at the same frequency and with the same amplitude.

AB

0 0

xx

AB

0 0

)tcos(cx oA ω=

)tcos(cx oB ω=

This is one NORMAL MODE of a coupled system

30

Page 31: Harmonic oscillators 2&N DOF systems: Coupled oscillators · In SHM the total energy (E) of a system is constant but the kinetic energy (K) and the potential energy (U) vary wrt

Seismology I - Oscillators...

Move A and B to opposite sides by equal amounts then release.

The spring is first stretched then a half cycle later it will be compressed.

The motions of A and B will be mirror images.

AB

0 0

xx

AB

0 0

This is the second NORMAL MODE of the system

31

Page 32: Harmonic oscillators 2&N DOF systems: Coupled oscillators · In SHM the total energy (E) of a system is constant but the kinetic energy (K) and the potential energy (U) vary wrt

Seismology I - Oscillators...

Equation of motion for coupled oscillators

Consider the situation where both masses are free to move and both are displaced a small distance x

AB

0 0x xThe spring is stretched by 2x

and exerts a restoring force of 2kx on the masses

Equation of motion for mass A 0kx2xmdtxdm AA

2o2

A2

=+ω+

0x)2(dtxd

A2c

2o2

A2

=ω+ω+ mk2

c =ωwhere

32

Page 33: Harmonic oscillators 2&N DOF systems: Coupled oscillators · In SHM the total energy (E) of a system is constant but the kinetic energy (K) and the potential energy (U) vary wrt

Seismology I - Oscillators...

')2( 2c

2o ω=ω+ωif

+=ω

mk2

lg'then

This has the solution xA = D cos ω’t

Motion of B is the mirror image of A xB = -D cos ω’t

Each pendulum oscillates with SHM.

The coupling spring has increased the restoring force and therefore increased the frequency of oscillation.

A and B are always 180o (π) out of phase.

33

Page 34: Harmonic oscillators 2&N DOF systems: Coupled oscillators · In SHM the total energy (E) of a system is constant but the kinetic energy (K) and the potential energy (U) vary wrt

Seismology I - Oscillators...

What is a wave? - 2

Small perturbations of a stable equilibrium point

Linear restoring force

Harmonic Oscillation

Coupling of harmonic oscillators

the disturbances can propagate, superpose and stand

Normal modes of the system

34

Page 35: Harmonic oscillators 2&N DOF systems: Coupled oscillators · In SHM the total energy (E) of a system is constant but the kinetic energy (K) and the potential energy (U) vary wrt

Seismology I - Oscillators...

N coupled oscillators

Consider a flexible elastic string to which is attached N identical particles, each mass m, equally spaced a distance L apart. The ends of the string are fixed a distance L from mass 1 and mass N. The initial tension in the string is T.

Consider small transverse displacements of the masses x

y

1 2 3 N-2 N-1 N

Lm

35

Page 36: Harmonic oscillators 2&N DOF systems: Coupled oscillators · In SHM the total energy (E) of a system is constant but the kinetic energy (K) and the potential energy (U) vary wrt

Seismology I - Oscillators...

Suppose particle 1 is displaced to y1, particle 2 to y2 etc

Length of string between particles 1 and 2

= cos α1 = L / L’ ie L’ = L /cos α1

L’ ~ L (1 + α12 /2) ie the increase in length = L (α1

2 / 2)

for small angles this increase is small and can be ignored

for small α cos α ~ (1 - α12 /2)

TT

1 2 3

α1

α2

1 2

y2

y1α1L

L’

36

Page 37: Harmonic oscillators 2&N DOF systems: Coupled oscillators · In SHM the total energy (E) of a system is constant but the kinetic energy (K) and the potential energy (U) vary wrt

Seismology I - Oscillators...

consider masses p-1, p and p+1 at some point along string

for small displacements y (compared to L)

Resultant Force on p = -T sin αp-1 + T sin αp

p-1 p p+1

αp-1

αp

37

Page 38: Harmonic oscillators 2&N DOF systems: Coupled oscillators · In SHM the total energy (E) of a system is constant but the kinetic energy (K) and the potential energy (U) vary wrt

Seismology I - Oscillators...

yp+1yp

yp-1αp-1

L

L (αp-12/2)

ypαpL

L (αp2/2)

Force on particle

Fp = −Typ − yp−1

L

+ T

yp+1 − yp

L

sinαp =yp+1 − yp

L (1 +αp2 /2)

~yp+1 − yp

Lfor small α

sinαp−1 =yp − yp−1

L (1 + αp−12 /2)

~yp − yp−1

Lfor small α

38

Page 39: Harmonic oscillators 2&N DOF systems: Coupled oscillators · In SHM the total energy (E) of a system is constant but the kinetic energy (K) and the potential energy (U) vary wrt

Seismology I - Oscillators...

ppp amFbut =

Substitute T/mL = ωo2

)yy()yy(dtyd

p1p2o1pp

2o2

p2

−ω+−ω−=∴ +−

Fp = −Typ − yp−1

L

+ T

yp+1 − yp

L

md2yp

dt2= −T

yp − yp−1

L

+ T

yp+1 − yp

L

39

Page 40: Harmonic oscillators 2&N DOF systems: Coupled oscillators · In SHM the total energy (E) of a system is constant but the kinetic energy (K) and the potential energy (U) vary wrt

Seismology I - Oscillators...

0)yy(y2dtyd

or 1p1p2op

2o2

p2

=−ω−ω+ −+

We can write a similar expression for all N particles

Therefore we have a set of N (coupled) differential equations one for each value of p from p=1 to p=N.

N.B. at fixed ends: y0 = 0 and yN+1 = 0

+

40

Page 41: Harmonic oscillators 2&N DOF systems: Coupled oscillators · In SHM the total energy (E) of a system is constant but the kinetic energy (K) and the potential energy (U) vary wrt

Seismology I - Oscillators...

Special case N=1

This is transverse harmonic motion with angular frequency

T T

L L

m

1Nfor0)yy(y2dtyd

022o1

2o2

12

==−ω−ω+

0)yy(y2dtyd

Generally 1p1p2op

2o2

p2

=−ω−ω+ −+

no particle =0

0y2dtyd

12o2

12

=ω+

mLT22 2

o =ω

41

Page 42: Harmonic oscillators 2&N DOF systems: Coupled oscillators · In SHM the total energy (E) of a system is constant but the kinetic energy (K) and the potential energy (U) vary wrt

Seismology I - Oscillators...

Special case N=2

0yy2dtyd

22o1

2o2

12

=ω−ω+

0yy2dtyd

12o2

2o2

22

=ω−ω+

These are similar to the equations for coupled pendula but here we have the simplification that ωo = ωcWe get two normal modes of oscillation

Lower mode ω = ωo Upper mode ω = √3ωo

42

Page 43: Harmonic oscillators 2&N DOF systems: Coupled oscillators · In SHM the total energy (E) of a system is constant but the kinetic energy (K) and the potential energy (U) vary wrt

Seismology I - Oscillators...

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Page 44: Harmonic oscillators 2&N DOF systems: Coupled oscillators · In SHM the total energy (E) of a system is constant but the kinetic energy (K) and the potential energy (U) vary wrt

Seismology I - Oscillators...!

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