Categories of Waves
Categories of Waves
Waves come in many shapes and forms. While all waves share some basic
characteristic properties and behaviors, some waves can be
distinguished from others based on some observable (and some
non-observable) characteristics. It is common to categorize waves based
on these distinguishing characteristics.
Longitudinal versus Transverse Waves versus Surface Waves
One way to categorize waves is on the basis of the direction of
movement of the individual particles of the medium relative to the
direction that the waves travel. Categorizing waves on this basis leads
to three notable categories: transverse waves, longitudinal waves, and
surface waves.
A transverse wave is a wave in which particles of the medium move in a direction perpendicular
to the direction that the wave moves. Suppose that a slinky is
stretched out in a horizontal direction across the classroom and that a
pulse is introduced into the slinky on the left end by vibrating the
first coil up and down. Energy will begin to be transported through the
slinky from left to right. As the energy is transported from left to
right, the individual coils of the medium will be displaced upwards and
downwards. In this case, the particles of the medium move perpendicular
to the direction that the pulse moves. This type of wave is a transverse
wave. Transverse waves are always characterized by particle motion
being perpendicular to wave motion.
A longitudinal wave is a wave in which particles of the medium move in a direction parallel
to the direction that the wave moves. Suppose that a slinky is
stretched out in a horizontal direction across the classroom and that a
pulse is introduced into the slinky on the left end by vibrating the
first coil left and right. Energy will begin to be transported through
the slinky from left to right. As the energy is transported from left to
right, the individual coils of the medium will be displaced leftwards
and rightwards. In this case, the particles of the medium move parallel
to the direction that the pulse moves. This type of wave is a
longitudinal wave. Longitudinal waves are always characterized by
particle motion being parallel to wave motion.
A sound wave traveling through air is a classic
example of a longitudinal wave. As a sound wave moves from the lips of a
speaker to the ear of a listener, particles of air vibrate back and
forth in the same direction and the opposite direction of energy
transport. Each individual particle pushes on its neighboring particle
so as to push it forward. The collision of particle #1 with its
neighbor serves to restore particle #1 to its original position and
displace particle #2 in a forward direction. This back and forth motion
of particles in the direction of energy transport creates regions within
the medium where the particles are pressed together and other regions
where the particles are spread apart. Longitudinal waves can always be
quickly identified by the presence of such regions. This process
continues along the chain of particles until the sound wave reaches the ear of the listener. A detailed discussion of sound is presented in another unit of The Physics Classroom Tutorial.
Waves traveling through a solid medium can be either
transverse waves or longitudinal waves. Yet waves traveling through the
bulk of a fluid (such as a liquid or a gas) are always longitudinal
waves. Transverse waves require a relatively rigid medium in order to
transmit their energy. As one particle begins to move it must be able to
exert a pull on its nearest neighbor. If the medium is not rigid as is
the case with fluids, the particles will slide past each other. This
sliding action that is characteristic of liquids and gases prevents one
particle from displacing its neighbor in a direction perpendicular to
the energy transport. It is for this reason that only longitudinal waves
are observed moving through the bulk of liquids such as our oceans.
Earthquakes are capable of producing both transverse and longitudinal
waves that travel through the solid structures of the Earth. When
seismologists began to study earthquake waves they noticed that only
longitudinal waves were capable of traveling through the core of the
Earth. For this reason, geologists believe that the Earth's core
consists of a liquid - most likely molten iron.
While waves that travel within the depths of the
ocean are longitudinal waves, the waves that travel along the surface of
the oceans are referred to as surface waves. A surface wave
is a wave in which particles of the medium undergo a circular motion.
Surface waves are neither longitudinal nor transverse. In longitudinal
and transverse waves, all the particles in the entire bulk of the medium
move in a parallel and a perpendicular direction (respectively)
relative to the direction of energy transport. In a surface wave, it is
only the particles at the surface of the medium that undergo the
circular motion. The motion of particles tends to decrease as one
proceeds further from the surface.
Any wave moving through a medium has a source.
Somewhere along the medium, there was an initial displacement of one of
the particles. For a slinky wave, it is usually the first coil that
becomes displaced by the hand of a person. For a sound wave, it is
usually the vibration of the vocal chords or a guitar string that sets
the first particle of air in vibrational motion. At the location where
the wave is introduced into the medium, the particles that are displaced
from their equilibrium position always moves in the same direction as
the source of the vibration. So if you wish to create a transverse wave
in a slinky, then the first coil of the slinky must be displaced in a
direction perpendicular to the entire slinky. Similarly, if you wish to
create a longitudinal wave in a slinky, then the first coil of the
slinky must be displaced in a direction parallel to the entire slinky.
Electromagnetic versus Mechanical Waves
Another way to categorize waves is on the basis of their ability or
inability to transmit energy through a vacuum (i.e., empty space).
Categorizing waves on this basis leads to two notable categories:
electromagnetic waves and mechanical waves.
An electromagnetic wave
is a wave that is capable of transmitting its energy through a vacuum
(i.e., empty space). Electromagnetic waves are produced by the vibration
of charged particles. Electromagnetic waves that are produced on the
sun subsequently travel to Earth through the vacuum of outer space. Were
it not for the ability of electromagnetic waves to travel to through a
vacuum, there would undoubtedly be no life on Earth. All light waves are
examples of electromagnetic waves. Light waves are the topic of another unit at The Physics Classroom Tutorial.
While the basic properties and behaviors of light will be discussed,
the detailed nature of an electromagnetic wave is quite complicated and
beyond the scope of The Physics Classroom Tutorial.
A mechanical wave
is a wave that is not capable of transmitting its energy through a
vacuum. Mechanical waves require a medium in order to transport their
energy from one location to another. A sound wave is an example of a
mechanical wave. Sound waves are incapable of traveling through a
vacuum. Slinky waves, water waves, stadium waves, and jump rope waves
are other examples of mechanical waves; each requires some medium in
order to exist. A slinky wave requires the coils of the slinky; a water
wave requires water; a stadium wave requires fans in a stadium; and a
jump rope wave requires a jump rope.
The above categories represent just a few of the
ways in which physicists categorize waves in order to compare and
contrast their behaviors and characteristic properties. This listing of
categories is not exhaustive; there are other categories as well. The
five categories of waves listed here will be used periodically
throughout this unit on waves as well as the units on sound and light.
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