Wave Properties -- Diagnostic Tests
Intuition
Section titled “Intuition”Physics describes the fundamental rules of the universe — from the tiniest particles to the vastness of space.
Wave Properties — Diagnostic Tests
Section titled “Wave Properties — Diagnostic Tests”Unit Tests
Section titled “Unit Tests”UT-1: Electromagnetic Wave Properties
Section titled “UT-1: Electromagnetic Wave Properties”Question:
A plane electromagnetic wave in vacuum has an electric field amplitude of and frequency .
(a) Calculate the wavelength, the magnetic field amplitude And the intensity of the wave.
(b) The wave is incident normally on a surface of area . Calculate the radiation pressure on the surface if it is (i) perfectly absorbing and (ii) perfectly reflecting.
(c) Calculate the energy of a single photon of this radiation.
Take c = 3.00 \times 10^8\,\text{m}\,\text{s}^{-1}$$\varepsilon_0 = 8.85 \times 10^{-12}\,\text{F}\,\text{m}^{-1}$$\mu_0 = 4\pi \times 10^{-7}\,\text{H}\,\text{m}^{-1}$$h = 6.63 \times 10^{-34}\,\text{J}\,\text{s}.
Solution:
(a) Wavelength: (visible light, orange)
Magnetic field amplitude:
Intensity:
Alternatively:
(b) Radiation pressure:
(i) Perfectly absorbing:
Force on surface:
(ii) Perfectly reflecting:
Force:
(c)
UT-2: Intensity and Amplitude Relationship
Section titled “UT-2: Intensity and Amplitude Relationship”Question:
Two coherent sources and emit waves of wavelength in phase. A point is located from and from .
(a) Determine whether point is at a maximum, minimum, or neither, and calculate the ratio of the amplitude at to the amplitude from a single source.
(b) If the amplitude from each source alone at is Derive the general expression for the amplitude at in terms of the path difference .
(c) Calculate the ratio of the intensity at to the intensity from a single source alone.
Solution:
(a) Path difference:
Since the path difference is an integer number of wavelengths (), is at a maximum (constructive interference).
The amplitude at is (double slit maximum).
(b) Phase difference:
The resultant amplitude from two waves of amplitude with phase difference :
In terms of path difference:
(c) Intensity is proportional to amplitude squared:
At a maximum, the intensity is four times the intensity from a single source.
At a minimum (): and .
UT-3: Polarisation and Malus”s Law
Section titled “UT-3: Polarisation and Malus”s Law”Question:
Unpolarised light of intensity passes through two polarising filters. The first has its transmission axis vertical. The second is rotated by an angle from the vertical.
(a) Calculate the intensity transmitted through both filters as a function of .
(b) At what angle is the transmitted intensity equal to ?
(c) A third polariser is inserted between the first two, with its transmission axis at to the vertical. Calculate the transmitted intensity when .
Solution:
(a) After the first (vertical) polariser, the intensity is (unpolarised light loses half its intensity through any polariser).
After the second polariser (at angle ), by Malus’s law:
(b)
(c) First polariser (vertical): intensity Polarised vertically.
Second polariser (at ): Polarised at .
Third polariser (horizontal, from vertical): the angle between the polarisation and horizontal is .
Without the middle polariser, at the transmitted intensity would be zero (crossed polarisers). The insertion of a third polariser at allows light to pass through, demonstrating that polarisers project the electric field onto their transmission axis rather than blocking light.
Integration Tests
Section titled “Integration Tests”IT-1: Doppler Effect and EM Waves (with Superposition)
Section titled “IT-1: Doppler Effect and EM Waves (with Superposition)”Question:
A galaxy is moving away from Earth at a speed of . A spectral line of wavelength (hydrogen alpha) is observed from this galaxy.
(a) Calculate the observed wavelength of this line. (Use the non-relativistic Doppler formula.)
(b) Calculate the percentage change in the observed frequency.
(c) A space probe approaching Jupiter at transmits a radio signal at . Calculate the frequency received by an observer on Jupiter.
Take .
Solution:
(a) For a source moving away from the observer:
Observed wavelength: (redshifted)
(b) So
The frequency decreases by .
(c) The probe approaches Jupiter, so the observed frequency is higher:
The shift is .
IT-2: Standing Waves on a String (with Oscillations)
Section titled “IT-2: Standing Waves on a String (with Oscillations)”Question:
A string of length and mass is fixed at both ends and stretched to a tension of .
(a) Calculate the speed of transverse waves on the string.
(b) Calculate the fundamental frequency and the frequencies of the next two harmonics.
(c) The string is plucked at its centre. Explain which harmonics are excited and calculate the wavelength of the fundamental mode.
Solution:
(a) Wave speed: Where
(b) For a string fixed at both ends, :
Fundamental ():
Second harmonic ():
Third harmonic ():
(c) Plucking at the centre excites the odd harmonics () most strongly because the centre is an antinode for odd harmonics and a node for even harmonics. Even harmonics () have a node at the centre, so plucking there does not excite them.
Fundamental wavelength:
The fundamental mode has one antinode at the centre and nodes at both ends.
IT-3: Seismic Waves Through Earth Layers (with Properties of Materials)
Section titled “IT-3: Seismic Waves Through Earth Layers (with Properties of Materials)”Question:
P-waves (longitudinal) travel through the Earth’s crust at and through the mantle at . The crust is thick. A P-wave is detected at a seismograph from the epicentre.
(a) Calculate the time for the P-wave to reach the seismograph via the direct path through the crust only.
(b) The wave refracts at the crust-mantle boundary. Using Snell’s law, calculate the critical angle and determine whether total internal reflection occurs for the direct path.
(c) Explain why S-waves (transverse) are not detected on the opposite side of the Earth from a large earthquake.
Solution:
(a) Direct path through crust:
(b) The wave travels from crust (slower) into mantle (faster), so it bends away from the normal.
Critical angle (for TIR from mantle to crust):
For the direct path, the wave enters the mantle at some angle. Since the wave goes from a slower medium (crust) to a faster medium (mantle), TIR cannot occur at this boundary. TIR only occurs when going from a slower medium to a faster medium if the wave is already inside the slower medium — which is not the case here. The wave always enters the mantle (it refracts away from the normal).
For a wave travelling through the mantle and hitting the crust-mantle boundary from below (trying to exit to the crust), TIR occurs at angles exceeding from the normal.
(c) S-waves are transverse and cannot propagate through liquids. The Earth’s outer core is liquid, so S-waves are blocked by it. This creates an S-wave shadow zone on the opposite side of the Earth. The detection of this shadow zone was key evidence for the existence of a liquid outer core.
Common Mistakes
Section titled “Common Mistakes”Confusing current and voltage: Current (A) is the flow of charge; voltage (V) is the energy per unit charge. Resistance opposes current, not voltage. Students often say “the resistor uses up the voltage” when they should say “the voltage drops across the resistor.”
Forgetting Ohm’s law applies only to ohmic conductors: = IR gives the resistance at that point, not a constant.
Confusing the conventions for electron flow and conventional current: Conventional current flows from positive to negative (the direction a positive charge would move). Electron flow is from negative to positive (the actual movement of electrons). Most circuit analysis uses conventional current. Using electron flow when conventional current is expected gives reversed directions.
Cross-References
Section titled “Cross-References”- Mechanics: Mechanics covers motion, forces, and energy
- Waves: Waves transfer energy through oscillations
- Electricity: Electricity covers circuits and fields