Waves
move energy from one place to another, but the particles of the medium do not travel with the wave.
wave motion
movement of energy through a medium caused by vibrations (oscillations) of particles.
2 main types of wave
-transverse
-longitudinal
transverse
a wave where the particles vibrate perpendicular (at right angles) to the direction the wave travels.
longitidunal
a wave where the particles vibrate parallel to the direction the wave travels.
examples of transverse
-light wave
-water surface wave
example of longitudinal
-sound wave
-ultrasound wave
-waves in a spring
wavelength
distance between two consecutive points that are in phase (e.g., crest to crest or trough to trough).
frequency
The number of waves passing a point per second.
higher the frequency?
more wave per second
crest(peak)
highest point of a transverse wave
trough
lowest point in a transverse wave
wave speed
speed at which the wave travels through a medium.
wave speed formula
v=fλ
v = wave speed
f = frequency
λ = wavelength
amplitude
maximum distance between the equilibrium (rest) position and a crest or trough.
higher the amplitude?
more energy
refraction
when a wave changes direction because its speed changes when it enters a new medium.
reflection
when a wave bounces back into the same medium after hitting a surface.
diffraction
the spreading out of waves when they pass through a gap or around an obstacle.
how does a wave diffract
When waves pass through a narrow gap, they spread out (diffract) and bend into different directions.
wavelenghts and gap influence on diffraction
Large wavelength + small gap → More diffraction
Small wavelength + large gap → Less diffraction
normal
line drawn at 90° (perpendicular) to the surface at the point where the ray hits.
angle of incidence
angle between the incident ray and the normal.
angle of refraction
angle between the reflected ray and the normal.