Particles oscillate perpendicular to the direction of energy transfer. example is seismic S waves
Longitudinal waves
Particles oscillate parallel to the direction of energy transfer, made up of compressions and rarefactions. example of this are sound waves
Time period
Time taken for one complete wave to pass a point
Frequency
Number of complete waves passing a point every second, calculated as 1 / time period
Wave speed
Equals frequency times wavelength (V = f * Lambda)
Polarization
Transverse waves can be polarized by a filter that only transmits waves oscillating in a particular direction
Interference/Superposition
When displacements of individual waves sum at each point, can be constructive or destructive
Harmonics
Occur when wavelength is equal to 2x or 1x the length of the string
Nodes and antinodes
Nodes have destructive interference and no energy transfer, antinodes have both constructive and destructive interference with energy transfer
Young's double slit experiment
Uses coherent sources (in phase) at the double slit to produce a diffraction pattern, fringe width W = Lambda * D / s where D is distance and s is slit separation
Single slit diffraction
Has a large central maximum that falls away quickly, with smaller secondary maxima
Diffraction grating
Equation: n * Lambda = d * sin(Theta), where n is order, Lambda is wavelength, d is line spacing
Refraction
Equation: n1 * sin(Theta1) = n2 * sin(Theta2), where n1 and n2 are refractive indices of the two media
Total internal reflection (TIR)
Occurs when angle of incidence is greater than the critical angle, and the refractive index of the first medium is greater than the second