3: Waves Flashcards
Progressive Wave
Waves, which transfer energy
Amplitude
The maximum displacement of a point on a wave from its rest position
Frequency
The amount of oscillations completed by a point on a wave per unit time
Wavelength
The length between two of the exact same points on a wave
Wave Speed
The speed at which waves travel
Wave Speed Formula
c = f λ
Frequency Formula
f = 1 / T
Longitudinal Waves
Waves where the direction of displacement of oscillating particles / fields is parallel to the direction of energy propagation
Transverse Waves
Waves where the direction of displacement of oscillating particles / fields is perpendicular to the direction of energy propagation
Phase
The fraction of a cycle that a point on a wave has completed since the start of that cycle
Phase Difference
Difference in phase between the exact same point on two waves measured in degrees, radians or fractions of a cycle
Polarisation
Where transverse waves are all oriented in the same direction – oscillating in the same plane (for EM waves, it is the electric fields, which can be polarised)
Applications of Polarisers (2)
- Polaroid material
- Alignment of aerials for transmission and reception
Polaroid material
A material, which polarises transverse waves (e.g., sunglasses)
Alignment of Aerials for Transmission & Reception (4)
- AC in transmitting aerial oscillates electromagnetic fields in one direction
- This produces a polarised EM waves
- EM waves oscillate electrons in receiving aerial producing the same frequency AC
- Transmitting and receiving aerials have to be aligned in the same orientation so that the waves are fully absorbed
Refractive Index of a Substance s
n = c / cₛ
n is refractive index of s
c is speed of light in vacuo in m s⁻¹
c is speed of light in s in m s⁻¹
Refractive Index of Air
~1
Refractive Index between Two Boundaries
₁n₂ = n₂ / n₁
₁n₂ is relative refractive index of a boundary (material 1 to material 2)
n₁ is refractive index of material 1
n₂ is refractive index of material 2
Snell’s Law of Refraction for a Boundary
n₁ sin θ₁ = n₂ sin θ₂
n₁ & n₂ are refractive indexes of materials 1 and 2
θ₁ is angle of incidence in °
θ₂ is angle of refraction in °
Total Internal Reflection (3)
When a ray travels from a more optically dense medium to a less, there will be a critical angle, θ. If:
- θᵢ < θ, there’s refraction and partial reflection
- θᵢ = θ, there’s refraction at 90° and partial reflection
- θᵢ > θ, there’s total reflection