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Topic 4 - Waves
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Waves transfer
energy
and
information
, but not
matter
The two types of waves include
longitudinal
and
transverse
Transverse
waves are waves that oscillate
perpendicular
to the direction of energy transfer.
Longitudinal
Waves are waves that oscillate
parallel
to the direction of energy transfer.
Examples of
transverse
waves include
electromagnetic
waves,
seismic
s-waves
Examples of longitudinal waves include
sound
waves and
seismic
p-waves
The two parts of a longitudinal wave are called
compressions
and
rarefactions
The two parts of transverse waves are called
peaks
and
troughs
The
amplitude
of a wave is the maximum
displacement
point on a wave from its
stationary
position
Wavelength
is the distance from a point on a
wave
to the same position on the adjacent
wave
The
frequency
of a
wave
is the number of complete waves passing a point per
second.
The unit for requency is
Hertz
Wave speed
is the speed at which energy is transferred through a medium
Waves transfer
energy
Wave speed =
Frequency
x
Wavelength
The unit for wavelength is
meters
The
period
of a
wave
is the time taken for one complete
wave
to pass through a point
Reflection
is the word used to describe when a wave
bounces
off a surface
The
normal
is a vertical imaginary line that is
perpendicular
to the boundary
When light is REFLECTED off a boundary the angle of
incidence
is the same as the angle of
reflection
Refraction
is the
bending
of
light
as it passes from one medium to another.
When light is
REFRACTED
off a boundary the light
speed
and
direction
change when travelling through the new medium
When light enters a
denser
material the waves
slow
down and bend
towards
the normal
When light enters a
less
dense material the waves
speed
up and bend
away
from the normal
Sound waves travel through a solid by the particles in the solid vibrating and transferring
kinetic energy
through the material
1kHz
= 1000Hz
The frequency range of a human being is
20Hz
to
20
,
000Hz
Sounds with frequencies above
20,000Hz
are called
ultrasounds
Sounds with frequencies below
20,000Hz
are called
infrasounds
Earthquakes produce both
seismic
s-waves and
p-waves
P-waves travel through both
solids
and
liquids
S-waves travel through
solids
only