Waves and Oscillations
Department of
Mathematics
University of Glasgow
Why look at waves?
Waves are the key to sound
and colour.
Mobile phone signals, microwave ovens all use energy carried by
waves.
Earthquakes and tsunamis are destructive waves of energy.
Waves affect our everyday lives in many ways.
A wave is a pulse of energy. Waves carry energy away from a central transmitter. Mechanical waves, such as sound waves, need some medium of transmission. Electromagnetic waves, for example radio waves, can carry energy through a vacuum. If a wave is travelling through a medium, the particles of the medium do not move along with it. They vibrate about their equilibrium position, and the energy is transmitted through the interaction of neighbouring particles.
Here is a Maple program that plots a simple travelling sine wave. It is animated so that you can see the wave motion along the axis. The dots represent particles in the medium. If you watch the line of dots closest to the vertical axis, you will see that they oscillate up and down, but do not move with the wave.
> with(plots):
> p1:=animate(sin(x-t),x=0..4*Pi,t=0..20,frames=100,style=point,colour=magenta):
> p2:=animate(sin(x-t)-.1,x=0..4*Pi,t=0..20,frames=100,style=point,colour=magenta):
> p3:=animate(sin(x-t)-.2,x=0..4*Pi,t=0..20,frames=100,style=point,colour=magenta):
>
> display({p1,p2,p3});
A wave is travelling energy: all waves -- radio, light, x-ray, sound or water waves radiate in all directions from a central source.
An oscillation is when a mass moves back and forth in a regular rhythm: a swing, the tide, a duck sitting still on a wavy pond all oscillate.
Even though oscillations and waves are different phenomena, the same mathematical functions are used to describe them and graph their motion. These functions are the sine and cosine functions.
Differential equations are used to model physical, biological and other systems. A good model explains the behaviour we see and predicts future behaviour. The wave equation is used for all linear wave motion where the speed is constant.
Here is the 3 dimensional plot of a typical solution to the wave equation.
> plot3d(sin(x-t)+sin(x+t),x=0..4*Pi,t=0..10);
Sound and water waves
transmit energy through a medium. The molecules vibrate and their interaction
transmits the energy. Such waves are called mechanical waves. There are two
main types:
Transverse waves: the molecules vibrate at right angles to the
direction of travel.

Longitudinal waves: the
molecules vibrate along the direction of travel.

Imagine a long rope stretched out straight along the ground. If you vibrate one end periodically, then a transverse wave will move along it. A snapshot would look like this:
The line through BH gives
the equilibrium or rest position.
The amplitude
A measures the maximum displacement of a particle from equilibrium:
rest to crest. The amplitude is related to the amount of energy the
wave is carrying.
The wavelength measures the
length of one complete cycle.
The period is the time a
particle on the rope takes to do one cycle.
The frequency is the number
of cycles a particle makes/unit time.
The mathematical functions that
model periodic behaviour with a constant amplitude and wavelength are sines and
cosines.
A mechanical wave is a
disturbance that travels through a medium. The crest moves from particle to
particle in the form of a sine wave. It will continue to move in the same form
until something interferes with it. This could be because it meets another wave
or it reflects off a boundary.
If two single pulses meet, as they pass they
interact, but as they separate, their shape is the same as before the
interaction.
The picture above shows pulses that are moving in opposite
directions. You can see how they cancel each other out as they cross, but once
they have passed each other the energy travels on with the same wavelength and
amplitude.
Now, pulses moving at different speeds in the same direction:
The one carrying more energy is moving faster. Notice that as they cross the amplitudes add. After the interaction the wave shapes are unchanged, but the faster one has overtaken the slow one.
When travelling waves
interact, they form another waveform. In general it will not be a simple sine
wave, but there will be a periodic pattern and a fixed wavelength. In the
picture below, the red graph is the function
.
The green and blue graphs give each of these
functions -- which is which?
Although the wave form is not a simple sine wave it is clearly periodic and has a fixed maximum amplitude. Below is a picture showing how the waveforms move. Again, there is a fixed wavelength and amplitude.
A guitar string is fixed at
both ends, so waves are reflected and interact in the length of the string. As
both ends have to be at rest, this restricts the possible wavelengths. The
possible waves are called modes of vibration.
As the length and thickness
of the string is fixed, the pitch of the note is determined by its tension. The
tone is made up of harmonics which are the different frequencies of the modes
of vibration.
Here is a picture of the
first harmonic for a guitar string. Below are animations of the first 4 modes
of vibration. You can see that as the wavelength shortens the frequency
increases. The higher the frequency, the higher the pitch.
Because the ends of the
guitar string are fixed, the waves are reflected back into the string. As the
last section said, only certain wavelengths are possible as solutions of the
wave equation.
As a result, if the string is made to vibrate with the
frequency of one of the harmonic modes, you see a standing wave. The incident
and reflected wave interact so that certain points -- the nodes -- are standing
still. A standing wave looks as if the string is vibrating at right angles to
its length and there is no wave transmitting energy along the string.

Written by Frances Goldman; research by Shona Maclean
© Copyright 2000, Frances Goldman, University of Glasgow