Unit 3 - Waves Flashcards
Source of waves
Produced by vibrations causing a disturbance which spreads out from the source
What waves transfer
Waves transfer energy from one place to another without transferring matter
Types of waves
- Transverse wave
- Longitudinal wave
Transverse wave
The particles oscillate perpendicular to the direction of propagation of the wave
Longitudinal wave
The particles oscillate parallel to the direction of propagation of the wave
Crest
The peak of the wave
Trough
The lowest point of the wave
Amplitude
The height of the wave
Frequency
The number of complete waves that pass a point each second
Unit of frequency
Hertz (Hz)
Wavelength
The distance between one wave crest and the next (or trough)
Wave speed calculation
Wave speed (m/s) = Frequency (Hz) x wavelength (m)
Relationship with amplitude and energy
If amplitude increases, more energy is transferred per second
Transverse wave examples
- Ripples along the surface of water
- Waves formed by shaken rope
- Visible light and electromagnetic radiation
Longitudinal wave examples
- Waves produced when ends of a stretched spring are moved
- Sound waves- series of compressions and rarefactions
Earthquake waves
- Primary waves - longitudinal - ground is compressed in the same direction as the wave travels
- Secondary waves - transverse - ground rises and falls as wave passes through
Reflection
When a wave ‘bounces’ off a boundary
Refraction
When a wave moves from one medium to another and changes speed and hence direction
Diffraction
When a wave spreads as it moves through a gap or passes and edge
Incident wave
The wave before it reaches a boundary
Reflected wave
The wave after it has hit the boundary and bounced off
Reflection constants
- Wave speed, frequency and wavelength doesn’t change
Increasing effect of diffraction
Gap and wavelength are of similar size
Normal line
Drawn to measure angle of incidence and reflection
Law of reflection
Angle of incidence = Angle of reflection
Virtual image
When rays of not pass through the place an image is seen - hence can’t be projected onto screens
Real image
An image that can be projected onto a screen because the rays of light actually pass through the position of the image
Refractive index
Shows how much the speed of light changes when it moves from a vacuum to a certain material
Refractive index equation
Refractive index (n) = Speed of light in vacuum ÷ Speed of light in a substance
Snell’s law
Relationship with angle of incidence and refraction is constant ration which is refractive index
n = sin i ÷ sin r
Light reflecting off the back surface of a medium
Internal reflection
Total internal reflection
When all of the light leaving a glass block is reflected back inside
Needs for total internal reflection
- Angle of incidence if greater than critical angle
- Wave needs to speed up after it passes across
Critical angle
The largest angle of incidence which allows light to escape the medium
Relationship of critical angle and refractive index
refractive index (n) = 1 ÷ sin c
Use of total internal reflection
Optical fibers - transmis optical pulses over long distances, pulse can be detected since the pulse doesn’t leave the fibre
- Optical fibers - endoscopes
Types of actions of lenses
- Diverging light (spreading it out)
- Converging light (bringing it towards a point)
Converging lens
- Refracts light rays to come together
- If light rays are parallel to each other and to the optical axis, rays will come together to the principal focus