Waves Flashcards
Total internal reflection
When a ray of light leaving an optically dense material
Travelling into a less dense one
Is not refracted outside
But totally reflected back inside
When is Snells law not applicable
If the angle of incidence is grater than the critical angle
Because total internal relection occurs
Angle of refraction at critic angle
90°
Critical angle
Angle of refraction is 90°
Incident less than means reflection
Incident more than means TIR
Fibre optics
Thin flexible tubes Glass/plastic Carry light signs over long distance Round corners High refractive index Narrow so light says hits at angle bigger than critical for TIR to occur
Cladding
Protects core from scratches and fluid contamination so light can’t escape
Increases critical angle
Lower refractive index than optical fibre allowing for TIR
Modal dispersion
Light enters at different angles so takes different paths
Longer path means longer to reach end than those that travel down middle
Single mode fibre only let’s light take one path
Stopping modal dispersion
Material dispersion
Chromatic dispersion
Light consists of different wavelengths that travel at different speeds
Some reach end before others
Using monochromatic light can stop material dispersion
Uses of fibre optics
Lighting and decoration
Telephones
Microscopy and biomedical research
Computer networking easier and faster
Critical angle formula
Sin¤c=n2/n1
Explain one advantage of having a small core in fibre optics
Less light is lost so better quality signal
Increased probability of total internal reflection
Diffraction
Wave spreading out as it passes through a gap
Condition for max diffraction
Wavelength similar to size of the gap
Waves are either … or …
Longitudinal
Transverse
Longitudinal
The direction of vibration of particles (oscillations) are parallel to the direction in which the wave travels (propagation of wave)
Composed of compressions and rarefactions
Compressions
Regions of high pressure
Due to particles being close together
On a longitudinal wave
Rarefactions
Regions of low pressure
Due to particles being spread further apart
On a longitudinal wave
Transverse
The direction of vibration of particles (oscillations) are perpendicular to the direction in which the wave travels (propagation of wave)
Examples of longitudinal waves
Seismic P-waves
Sound
Springs (left to right)
Ultrasound
Examples of transverse waves
Seismic S-waves
Electromagnetic
Spring (up and down)
Ripples on water
Displacement
How far a point on a wave has moved from the undisturbed position
Vector (+/-)
Measured in metres
Amplitude
The maximum displacement of the wave from the undisturbed position/equilibrium position
Measured in metres
Wavelength
Length of one whole wave oscillation or wave cycle
Measured in metres
Frequency
Number of whole wave cycles (oscillations) per second passing a given point
Measured in Hz
Period
Time taken for one whole wave cycle
Crest to crest/trough to trough
Measured in seconds
Where can amplitude be measured
Crest
Trough
Crest
Point of positive amplitude (maximum positive displacement from the undisturbed position)
Trough
Point of negative amplitude (maximum negative displacement from the undisturbed position)
One oscillation/wave cycle
The point of a wave from crest to crest or trough to trough
Phase
Measurement of the position of a certain point along the wave cycle
Measured in degrees or radians or fractions of a cycle
Phase difference
Amount by which one wave lags behind another
Measured in degrees or radians or fractions of a cycle
1 Hz is equivalent to
Per second
1s^-1
What happens to sound if you increase the frequency
Wave is compressed
Wavelength decreases
Pitch increases
Amplitude stays the same
What happens to sound if you increase amplitude
Wavelength stays the same
Frequency stays the same
Wave is stretched vertically
Sounds louder
What happens to sound if you double the wavelength
Half the frequency
Wave is stretched horizontally
Pitch decreases
Amplitude stays the same
Frequency relation to time period
f=1/T
Wave equation
c=fλ
Deriving the wave equation
Speed=Distance/Time
Time=1/frequency
Speed=Distance/(1/f)
c=fλ
Frequency of sound
20-20000Hz
Order of EM spectrum
Radio Waves Microwaves Infrared Visible Light Ultraviolet X-Rays Gamma Rays
Mechanical waves
Require a medium to transfer energy from one location to another location
Do not transmit energy in a vacuum
Wavelengths of EM spectrum in powers of 10m
R
3
- 2
- 5
- 6
- 8
- 10
- 12
G
Frequencies of EM spectrum in powers of 10Hz
R
4 8 12 15 16 18 20
G
Examples of mechanical waves
Sound waves
Ripples on water
Seismic S and P waves
Radio waves
f
λ
4
3
Microwaves
f
λ
8
-2
Infrared
f
λ
12
-5
Visible light
f
λ
15
0.5x10^-6
Ultraviolet
f
λ
16
-8
X-Rays
f
λ
18
-10
Gamma
f
λ
20
-12
Speed of EM waves in a vacuum
3x10^8
Range of wavelengths of visible light in nm
700 (red)
400 (violet)
Wavelength of green light
495-570nm