what is a particles rest position called
equilibrium position
how do particles return to their equilibrium position in a wave
particles in the medium exert a force on each other. A displaced particle experiences a restoring force from its neighbour and it pulls it back to its og position
transverse vs longitudinal
t- perpendicular to oscillation or energy transfer
l- parallel to oscillation or energy transfer
how do longitudinal particles revert to their equilibrium position
displaced particles bounce off their neighbour providing the restoring force
period
time taken for one oscillation
frequency
number of complete wavelengths in one second
how to calculate wave speed
frequency x wavelength
how to find frequency from period
they are inversely proportional so f= 1/T
what is a wave profile
a graph showing the displacement of the particles in a wave against the distance along the wave
phase difference
How far out of step the oscillations of two points on the same wave are measured in degrees or radians
what is in phase
if two particles reach max positive or max negative displacement at the same time
what is anti phase
if one particles reach max positive while the other reaches max negative at the same time - completely out of phase represented as 180*
snell law
sin i/sin r = n (n is refractive index)
how is refractive index calculated
n= c/v ( c= speed of light through a vacuum and v= speed of light through material)
what does a large refractive index entail
there the light entering is refracted towards the normal
refractive law
n sin i = constant
what does the refractive law entail
n1 sin 0 1 = n2 sin 02
total internal reflection
occurs at the boundary between two different medians
conditions for TIR
how to work out critical angle
sin C = 1/n
partially polarised
description of a transverse wave in which there are more oscillations in one particular plane, but the wave is not completely plane polarised- occurs when transverse waves reflect off a surface
plane polarised
description of a transverse wave in which the oscillations are limited to only one plane
unpolarised
description of a transverse wave in which oscillations occur in many planes
relationship between intensity and amplitude
intensity is directly proportional to amplitude squared