Introduction
Many fields of science and engineering require a thorough understanding of different types of waves. Movement within the Earth's crust can cause devastating seismic waves. Medical scientists use ultrasound and other types of waves to scan the insides of the human body, while civil engineers need to know how vibrations affect buildings and other structures.
Waves are used for communicating information and for carrying energy. When sound waves, water waves, or mechanical waves pass through a substance, the particles in the substance vibrate in a specific order. Electromagnetic waves do not need a material medium to travel through, so they can travel through a vacuum.
Many fields of science and engineering require a thorough understanding of different types of waves. Movement within the Earth's crust can cause devastating seismic waves. Medical scientists use ultrasound and other types of waves to scan the insides of the human body, while civil engineers need to know how vibrations affect buildings and other structures.
Waves are used for communicating information and for carrying energy. When sound waves, water waves, or mechanical waves pass through a substance, the particles in the substance vibrate in a specific order. Electromagnetic waves do not need a material medium to travel through, so they can travel through a vacuum.
Nomenclature
In earlier courses you may have been introduced to waves by considering the type of motion shown in Fig.1.The particles in the medium through which a transverse wave passes move at right angles to the direction in which the disturbance travels.
Continuous transverse waves can be produced in Fig.2 by moving the end point up and down.
Another type of wave motion is shown in Fig.3. Move the point at the left-hand side of the stretched spring as indicated and note how the disturbance travels.
Sound
energy
A system has energy when it has the capacity to do work. The scientific unit of energy is the joule.energy is transmitted by the movement of the air molecules to and fro along the direction in which the energy is moving. Sound waves
are longitudinal waves. Sound, ultrasound, and some seismic (shock) waves are the most common examples of longitudinal waves.![]() |
So far we have seen that waves can be divided into two categories, transverse and longitudinal. However, we need to define a few more quantities before we can describe waves more fully: |
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The material through which a wave travels is called the medium. However, electromagnetic waves are exceptional. As their name suggests, they are disturbances in either an electric or a magnetic field. But, because a changing electric field creates a changing magnetic field and vice versa, they are self-sustaining. Thus they can pass through a vacuum. |
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The wave frequencyf is the number of complete waves passing any point each second. Frequency is measured in hertz, Hz. Once a wave leaves the source, its frequency cannot be altered. |
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The words crest and trough are used to describe the top and bottom respectively of a transverse wave. |
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The amplitude of the wave is the distance between the peak of the crest and the undisturbed position. The energy associated with a wave of a certain frequency depends on its amplitude. |
The wavelength is the distance from one point on a wave to the identical point on the next wave. This can be stated as the distance from
a crest on a wave to the next crest on the wave. |
Some of these terms can also be used to describe longitudinal waves, but additional descriptions must also be introduced.
The slider control in Fig.5 allows you to control the
amplitude
The amplitude of a wave is the distance between the peak of the crest and the undisturbed position. amplitude of the
longitudinal wave
A wave is said to be longitudinal when it causes the particles of the medium through which it passes to move parallel to the
direction in which the wave is moving.longitudinal wave. Press the 'pause' button to reveal the labels.Longitudinal sound waves passing through air produce a series of compressions and rarefactions.
Sound waves need a medium to travel through. This can be shown using the apparatus shown in Fig.6.
Click the button in Fig.6 to activate the bell and again to remove air from the jar. As air is removed from the bell jar the level of sound outside the jar reduces. The bell inside the jar can still be seen to be working properly but, since there is no air, no sound waves are being transmitted.
Polarization and phase
The amplitude and
wavelength
The wavelength
is the distance from one point on a wave to the identical point on the next wave. This can be stated as the distance from
a crest on a wave to the next crest on the wave.wavelength of a
transverse wave
A wave is said to be transverse when it causes the particles of the medium through which it passes to move at right-angles
to the direction in which the wave is moving.transverse wave can be represented as shown in Fig.7.The slider controls in Fig.7 allow you to observe the effect on a progressive transverse wave of altering its amplitude and/or wavelength.
The slider control labelled 'Phase' in Fig.8 turns on a second wave of the same wavelength. When corresponding points on the two waves reach maximum or minimum displacements at the same instant, the waves are said to be in phase. Otherwise there is a phase difference (measured in degrees or radians) between them.
So far we have only considered waves in two dimensions. The oscillations have been in one plane, (x, y). Looking end-on at an approaching wave you would simply see a vertical line.
Waves vibrating in just one plane are described as plane polarized.
Unpolarized waves such as those shown in Fig.10 cause vibrations in more than one plane.
Light waves emitted by a lamp or arriving at the Earth's surface from the sun are unpolarized. They can be polarized by passing the light through a polaroid filter. The filter only allows through light rays which oscillate in one preferred direction, determined by the filter itself. If two filters have their planes of polarization at 90° to each other, they are referred to as crossed polaroids. The light getting through the first filter will have no component capable of passing through the second, therefore crossed polaroids will appear dark.
Radiation intensity
The planets of our solar system can be represented as shown in Fig.11. Planets closer to the sun than the Earth are too warm
to sustain human life while those further away are too cold. The Earth is special because it is the correct distance from
the sun to receive just the right amount of energy. Common sense suggests that the energy collected by each planet in our solar system depends on its distance from the sun. Since the energy collected also depends on the time for which a planet is irradiated, we must consider the energy received over equal time intervals to achieve a fair comparison. We can do this by measuring the
power
The power of system is a measurement of the rate at which energy is transferred from one form to another. The scientific unit
of power is the watt.power, defined as the energy received per second. The quantity of energy collected also depends upon the size of the planet so when comparing the effect that the distance from the sun has on the energy received by planets, it is necessary to consider equal areas. The
intensity
The intensity at a particular point is described as the power per unit area.intensity at a particular point is described as the power per unit area.To calculate the intensity at a point some distance from a light source such as a lamp or a star, we assume that the source is a point radiating equally in all directions. Light travels, in all directions, away from this point source with a speed of 3 × 108 ms−1.
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If we consider a quantity of light leaving the point source at a particular time. One nanosecond (1 × 10−9 s) later, the light will have travelled a distance given by: |
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Therefore, 1 nanosecond after leaving the source, the energy is smeared out over a sphere of radius 0.3 m. The surface area
of a sphere is given by the formula, . |
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If the power of the source is P watts, the intensity at any point 1 nanosecond after the radiation leaves the source is given by: |
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A further nanosecond after leaving the source the radiation will have travelled twice as far, i.e. 0.6 m. |
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If the power of the source is P watts, the intensity at any point 2 nanoseconds after the radiation leaves the source is given by: |
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As the distance from the point source doubles, the intensity of the radiation reduces by a factor of four. The relationship between distance and intensity can be summarized mathematically as follows:

This relationship can be confirmed by the following experiment.
The intensity of radiation from the sun arriving at the top of the Earth's atmosphere is called the solar constant, S. It has a value of 1370 Wm−2. The Earth's atmosphere absorbs some of this radiation as it passes through, so the atmosphere warms up and the intensity at the Earth's surface is lower.
Luminosity
While radiation intensity allows us to compare the quantity of radiation arriving at any point,
luminosity
The luminosity of a light source is defined as the rate at which it radiates energy. In other words, the luminosity is the
total energy radiated per second.luminosity tells us the quantity of energy leaving a radiating object.The luminosity, L, of a star such as the sun is defined as the rate at which it radiates energy. In other words, the luminosity is the total energy radiated per second.
Luminosity has units of watts.
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We can use the values of the solar constant and the distance between the sun and the Earth to calculate the luminosity of the sun as follows: |
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The solar constant S = 1370 Wm−2 is the rate at which energy arrives per square metre at the Earth's distance from the sun. |
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Since the sun radiates the same amount of energy in all directions, the total rate at which it radiates energy will be given by |
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solar constant × surface area of a sphere with radius equal to the Earthsun distance |
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For the mean Earthsun distance (rE = 1.496 × 1011 m),
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| Therefore, the sun's luminosity L is 3.853 × 1026 W. A more sophisticated analysis can use this value to derive the sun's surface temperature, 5780 K. |
A star's luminosity depends upon both the temperature at its surface and its size. In the early twentieth century, scientists reasoned that the luminosity of a star could be related to its surface temperature. Two astronomers, Hertzprung and Russell independently experimented with plotting luminosity versus surface temperature. The resulting diagram came to be known as a Hertzprung-Russell diagram, or H-R diagram for short.
The position of a particular star on an H-R diagram can be used to indicate its type and give an estimate of its age.
Summary
When a transverse wave travels through a medium, the particles in the medium move at right angles to the direction in which the disturbance travels.
When a longitudinal wave travels through a medium, the particles in the medium move to and fro along the direction in which the wave travels.
Sound waves need a medium to travel through.
The phase relationship between two waves describes how the motion of particles in one wave compares with their motion in the other wave at any particular instant.
Waves vibrating in just one plane are described as plane polarized.
Intensity of radiation and the distance of the source are connected by the mathematical relationship,
.
The luminosity of a star such as the sun is defined as the rate at which it radiates energy.
Hertzprung-Russell diagrams plot luminosity versus surface temperature.
When a transverse wave travels through a medium, the particles in the medium move at right angles to the direction in which the disturbance travels.
When a longitudinal wave travels through a medium, the particles in the medium move to and fro along the direction in which the wave travels.
Sound waves need a medium to travel through.
The phase relationship between two waves describes how the motion of particles in one wave compares with their motion in the other wave at any particular instant.
Waves vibrating in just one plane are described as plane polarized.
Intensity of radiation and the distance of the source are connected by the mathematical relationship,
. The luminosity of a star such as the sun is defined as the rate at which it radiates energy.
Hertzprung-Russell diagrams plot luminosity versus surface temperature.

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