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WavesTopic 4.4 Wave characteristics
Travelling Waves
There are two types of waves and pulses that we encounter in the
physical world.
Transverse In these waves the source that
produces the wave oscillates at right angles to the direction of travel of the wave
It means that the particles of the medium through which the wave travels also oscillates at right angle to the direction of travel of the wave.
Direction of travelof the wave
Direction of oscillationof the particles
Transverse Wave
Longitudinal In these waves the source that
produces the wave oscillates in the same direction as the direction of travel of the wave
It means that the particle of the medium through which the wave travels also oscillates in the same direction as the direction of travel of the wave.
Longitudinal Wave
Direction of travelof the wave
Direction of oscillationsof the particles
Discrete Pulses and Continuous Waves
A single shake of a slinky will send a discrete pulse down it
Shake the slinky up and down and a continuous travelling wave travels down it
This applies to longitudinal waves too
What is a Wave?
A wave is a means by which energy is transferred between two points in a medium without any net transfer of the medium itself.
The Medium
The substance or object in which the wave is travelling.
When a wave travels in a medium parts of the medium do not end up at different places
The energy of the source of the wave is carried to different parts of the medium by the wave.
Water waves however, can be a bit disconcerting.
Waves at sea do not transport water but the tides do.
Similarly, a wave on a lake does not transport water but water can actually be blown along by the wind.
However, if you set up a ripple tank you will see that water is not transported by the wave set up by the vibrating dipper.
A very important property associated with all waves is their so-called periodicity.
Waves in fact are periodic both in time and space and this sometimes makes it difficult to appreciate what actually is going on in wave motion.
Periodicity
If we drew a diagram that froze time on waves in water
an instantaneous snapshot of the whole of the water surface
The next diagram shows the periodicity of the wave in space
Displacement / Distance
displacement
distancep
The y-axis shows the displacement of the water from its equilibrium position
The graph is a displacement-distance graph.
We now look at one part of the wave that is labeled p and "unfreeze" time
The next diagram shows how the position of p varies with time
This illustrates the periodicity of the wave in time
Displacement / Time
displacement of point p from equilibrium position
time
The y-axis now shows the displacement of the point p from equilibrium
The graph is a displacement-time graph.
The space diagram and the time diagram are both identical in shape
If we mentally combine them we have the whole wave moving both in space and time.
And for Longitudinal Waves?
For the longitudinal wave in the slinky spring the displacement-distance graph actually shows the displacement of the individual turns of the spring from their equilibrium position as a function of distance along the spring.
However
It could equally show how the density of turns of the spring varies with length along the spring.
The displacement-time graph shows the displacement of one turn of the spring from its equilibrium positions as a function of time.
Definitions
The following definitions are given in terms of the particles that make up the medium through which the wave travels.
For the slinky spring a particle would be a single turn of the spring
For the water waves a particle would be a very small part of the water.
Wavefront
• All the points that started from a source at one time make up the whole of that wavefront,
• If it was a single point, it will be a circular wavefront
• If it is a straight line, it will be a straight wave front
Displacement
(s) is the distance that any particle is away from its equilibrium position at an instance
Measured in metres
Amplitude
(A, a) This is the maximum displacement of a particle from its equilibrium position
(It is also equal to the maximum displacement of the source that produces the wave).
Normally measured in metres
Period
(T) This is the time that it takes a particle to make one complete oscillation
(It also equals the time for the source of the wave to make one complete oscillation).
Measured in seconds
Frequency
(f) This is the number of oscillations made per second by a particle
(It is also equal to the number of oscillations made per second by the source of the wave)
The SI unit of frequency is the hertz -Hz. (1 Hz is 1 oscillation per second)
Clearly then, f = 1/T
Wavelength
() This is the distance along the medium between two successive particles that have the same displacement and the same phase of motion.
Measured in metres
Wave Speed
(v, c) This is the speed with which energy is carried in the medium by the wave.
Measured in ms-1
A very important fact is that wave speed depends only on the nature and properties of the medium
Crest
This is a term coined from water waves and refers to the points at the maximum height of the wave.
Trough
A term coined from water waves referring to the points at the lowest part of the wave.
Wavelength again!
Wavelength will therefore be equal to the distance between successive crests and successive troughs.
Compression
This is a term used in connection with longitudinal wave and refers to the region where the particles of the medium are "bunched up".
High density High pressure
Rarefaction
A term used in connection with longitudinal waves referring to the regions where the particles are "stretched out".
Low density Low pressure
Longitudinal Waves The wavelength will be equal to the
distance between successive points of maximum compression and successive points of maximum rarefaction.
The compression is the region in which the molecules of the air are pushed together
The rarefaction is the region where the molecules move apart.
rarefactions
wavelength
Sound Waves
A longitudinal wave in a slinky spring is analogous to a sound wave in which each turn of the spring represents an air molecule.
Interpreting Graphs - 1
displacement
distance
crest
trough
amplitude crestwavelength
amplitude
wavelength
Interpreting Graphs - 2
displacement
time
amplitudeperiod
period
Deriving v = f Imagine a wave with velocity v Being produced from a source of
frequency f In 1 second the 1st wavefront would
have travelled a distance of f As speed = distance / time v = f / 1 v = f
2 Important Points
1. The frequency of a wave depends only on the source producing the wave
It will therefore not change if the wave enters a different medium or the properties of the medium change
2. The Speed of waves only depends on the nature and the properties of the medium
Water waves do travel faster in deeper water
Light travels slower in more optically dense material
The EM Spectrum Itself
Short Long High fLow f
VISIBLERadioWaves
MicroWaves
Infrared
Gammarays
UltraViolet
Xrays
Frequencies of Regions (Hz)
• Gamma Rays >1021
• X-rays 1017- 1021
• Ultraviolet 1014 - 1017
• Violet 7.5 x 1014 > Visible > Red 4.3 x 1014
• Infrared 1011 -1014
• Microwaves 109 -1011
• Radio and TV < 109
The Different Regions In the context of wave motion, common
properties of all parts of the electromagnetic spectrum are
all transverse waves all travel at the speed of light in vacuo
(3.0 x 108 ms-1) all can travel in a vacuum
Sources of Regions Gamma – certain radioactive material’s nuclei X-rays – by firing an electron stream at a tungsten
metal target in a highly evacuated tube. Ultraviolet – the Sun, ultraviolet lamp Visible – hot bodies Infrared – the Sun (heat), hot bodies Microwaves – Ovens, communication systems Radio and TV – transmitter stations, Azteca TV