Sound waves

Sound is caused by small areas of high and low pressure progragating outward from the source.

Rogers 8.5

One convenient way to diagram a sound wave is to graph the pressure at each point in time, the way it might be picked up by a microphone for example:

Rogers 8-2
This simplest kind of pressure wave is called a sine wave. Interesting things to measure for a sine wave:

amplitude (or loudness, size of pressure differences)
usually measured in decibels (dB)
wavelength
frequency (or pitch)
usually measured in cycles per second, or Hertz (Hz)

Frequency and amplitude are independent of each other. Two sine waves may have the same frequency and different amplitudes, and vice versa.
Rogers 8-3

Wavelength is the converse of frequency: the shorter the wavelength, the higher the frequency; the longer the wavelength, the lower the frequency. (Sound will move at the same speed, about 330 metres per second. So if you want to double the frequency of a wave, you'll have to fit twice as many wavelengths into that 330 metres, and each wavelength will have to half as long.)

Combining waves

If you're listening to waves from two sources at the same time:

a high pressure from one will cancel out a low pressure from the other
two high pressures will reinforce each other
two low pressures will reinforce each other

You can get the overall effect by adding the waves' pressures together at each point in time. (You have to treat the normal air pressure as zero, so that a higher pressure is positive and a lower pressure is negative.) adding sine waves
The two red waves added together produce the blue wave. At the first green line, both red waves have high pressure and reinforce each other to give an extra high pressure in the blue wave. At the second green line, the two red waves have opposite pressures and cancel each other out.

The following two sounds have frequencies of 300 Hz and 500 Hz:
sound 300 Hz
slice of a 300 Hz sine wave

sound 500 Hz
slice of a 500 Hz sine wave

They can be added together:
adding 300 and 500 Hz
to produce a complex wave:
resulting wave

This is important because:

Any complex wave can be treated as a combination of simple sine waves.

We usually don't care about the actual complex wave itself. We're only interested in the frequencies and amplitudes of the simple waves that it's made up of. Two more examples:

sound 300 Hz and 2000 Hz added

sound 900 Hz and 1100 Hz

Comparison with light

We see simple light waves (with only one frequency) as one of the colours of the rainbow. Combining together two or more simple one-frequency sine waves produces more complex colours. The more frequencies you add, the whiter the colour gets. With light, you can easily separate the frequencies by shining the complex light wave through a prism.

$diffraction through prism$

The set of frequencies in light wave (as separated by a prism) is called its spectrum.

Scientists can identify different substances by looking at the spectrum of the light the substances emit when they're heated. Iron will glow with a different set of frequencies than nickel or sulphur.

The situation is similar with sound. The complex wave for an [i] will be composed of a different set of frequencies than the complex wave for [a].

We need a way to separate a complex sound wave out into its component frequencies (and their amplitudes) so that we can see what makes vowels different. A spectrograph is essentially just a prism for sound.

Next: Spectrum diagrams
Up: Table of contents