Oscillations - UMD Physics€¦ · Damped Oscillations The time constant, τ, is a property of the...
Transcript of Oscillations - UMD Physics€¦ · Damped Oscillations The time constant, τ, is a property of the...
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Oscillations
• Simple Harmonic Motion (SHM)
• Position, Velocity, Acceleration
• SHM Forces
• SHM Energy
• Period of oscillation
• Damping and Resonance
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Revision problem
Please try problem #31 on page 480
A pendulum clock keeps time by the swinging of a uniform solid rod…
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Simple Harmonic Motion
• Pendulums
• Waves, tides
• Springs
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Simple Harmonic Motion
Requires a force to return the system back toward equilibrium
• Spring – Hooke’s Law
• Pendulum and waves and tides – gravity
Oscillation about an equilibrium position with a linear restoring force is always simple harmonic motion (SHM)
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Springs
Hooke’s Law F=-kx
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Springs
Hooke’s Law F=-kx
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Pendulum
For a small angle, the force is proportional to angle of deflection, θ.
sinmgFreturn
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Pendulum
For a small angle, the return force is proportional to the distance from the equilibrium point:
sL
mgmgF
L
s
return
sin
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Kinematics of SHM
Simple Harmonic motion can be described by a sinusoidal wave for displacement, velocity and acceleration:
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Kinematics of SHM
• The angle for the sinusoidal wave changes with time.
• It goes full circle 0 to 2π radians in one period of revolution, T.
T
tAtx
2cos)(
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Kinematics of SHM
•We define the frequency of revolution as
Frequency, f, has units s-1 or Hertz, Hz
ftAtx
Tf
2cos)(
1
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Kinematics of SHM
• Velocity is 90o or π/2 radians out of phase:
ftvtv 2sin)( max
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Kinematics of SHM
• Acceleration is 180o or π radians out of phase
ftata 2cos)( max
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Kinematics of SHM
SHM equations of motion
ftata
ftvtv
ftAtx
2cos)(
)2sin()(
)2cos()(
max
max
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Calculating vmax
A circular motion when looked end-on gives us a velocity like:
)2sin(max ftvv
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Calculating vmax
The velocity around the circle will be
fAv
T
A
T
Dv
2
2
max
max
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Calculating amax
For circular motion, we know about acceleration and forces
A
va
r
mvFmaF
2
maxmax
2
,
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Kinematics of SHM
SHM equations of motion
ftAfta
ftfAtv
ftAtx
2cos)2()(
)2sin(2)(
)2cos()(
2
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SHM and Energy
• Energy is conserved:
• Bounces between kinetic and potential energy
2
2
2
1
2
1
kxE
mvE
EEE
potential
kinetic
potentialkinetictotal
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SHM and Energy
• The max KE must equal the max PE:
Am
kv
kAvm
max
22
max2
1)(
2
1
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Finding the period of oscillation for a spring
We now have 2 equations for vmax:
Period of oscillation is independent of the amplitude of the oscillation.
k
mT
m
kf
fAAm
kv
2,2
1
2max
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Finding the period of oscillation for a pendulum
Consider the acceleration using the equation for the return force, and the relation between acceleration and displacement:
AL
gAfa
sL
mg
mm
Fa
2
max )2(
1
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Finding the period of oscillation for a pendulum
We can calculate the period of oscillation
Period is independent of the mass, and depends on the effective length of the pendulum.
g
LT
L
gf
2,
2
1
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Damped Oscillations
All the oscillating systems have friction, which removes energy, damping the oscillations
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Damped Oscillations
We have an exponential decay of the total amplitude
/max )( tAetx
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Damped Oscillations
The time constant, τ, is a property of the system, measured in seconds
•A smaller value of τ means more damping – the oscillations will die out more quickly.
•A larger value of τ means less damping, the oscillations will carry on longer.
/max )( tAetx
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Damped Oscillations
• under-damped τ>>T
• critically-damped τ~T
• over-damped τ<<T
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Driven Oscillations and Resonance
An oscillator can be driven at a different frequency than its resonance or natural frequency.
The amplitude can be large if the system is undamped.
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Tidal resonances
• Ocean tides are produced from the Moon (and Sun) gravitational pull on the oceans to make a 20cm wave.
• Moon drives the wave at 12 hours 25 minutes
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Tidal resonances
The natural resonance of local geography can affect this: e.g. Bay of Fundy in Canada where the tidal range is amplified from the 20cm wave to 16m.
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Tidal resonances
Natural geography can also make double tides:
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Undamped driven resonance
Tacoma Narrows Bridge, Washington State, 1940
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Summary
• Simple Harmonic Motion (SHM)
• Position, Velocity, Acceleration
• SHM Forces
• SHM Energy
• Period of oscillation
• Damping and Resonance
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Homework problems
Chapter 14 Problems
48, 49, 50, 52, 54, 59, 62, 63