Reflection and Refraction — Question 10

Section 33-7 · Physics pages 5510–5511

Question 10 Boundary phase matching fixes frequency and tangential wave number Two plane waves meet a stationary flat interface at y=0. Their phases along the surface are kx1x −ω1t + ϕ1 and kx2x −ω2t + ϕ2. Assume a uniform interface and a nonzero transmitted wave. n2 n1 normal x Schematic; labels, not drawing lengths, specify the data. (a) Explain mathematically why equality of boundary phase dependence for all x and t requires equal frequencies and tangential wave numbers. (b) Use the result and k=n omega/c to derive Snells law and the wavelength ratio.
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Question 10 - Solution Boundary phase matching fixes frequency and tangential wave number n2 n1 normal x (a) Method and calculation ∂t(ϕsurf 1 −ϕsurf 2 ) = 0 ⇒ω1 = ω2 . ∂x(ϕsurf 1 −ϕsurf 2 ) = 0 ⇒kx1 = kx2 . (b) Interpretation and further calculation k1 sin θ1 = k2 sin θ2 ⇒n1 sin θ1 = n2 sin θ2 . λj = 2π/kj ⇒λ2/λ1 = n1/n2 . Physical check A constant boundary phase offset can be absorbed into an amplitude coefficient; different x or t dependence cannot match a uniform stationary boundary.

Question 10

Boundary phase matching fixes frequency and tangential wave number

Two plane waves meet a stationary flat interface at y=0. Their phases along the surface are kx1x−ω1t+ϕ1k_{x1}x-\omega_1t+\phi_1 and kx2x−ω2t+ϕ2k_{x2}x-\omega_2t+\phi_2. Assume a uniform interface and a nonzero transmitted wave.

Diagram shown in the original SVG worksheet.

  1. Explain mathematically why equality of boundary phase dependence for all x and t requires equal frequencies and tangential wave numbers.

  2. Use the result and k=n omega/c to derive Snells law and the wavelength ratio.

Question 10 - Solution

Boundary phase matching fixes frequency and tangential wave number

Diagram shown in the original SVG worksheet.

(a) Method and calculation

∂t(ϕ1surf−ϕ2surf)=0⇒ω1=ω2.\partial_t(\phi_1^{\mathrm{surf}}-\phi_2^{\mathrm{surf}})=0\Rightarrow\boxed{\omega_1=\omega_2}.∂x(ϕ1surf−ϕ2surf)=0⇒kx1=kx2.\partial_x(\phi_1^{\mathrm{surf}}-\phi_2^{\mathrm{surf}})=0\Rightarrow\boxed{k_{x1}=k_{x2}}.

(b) Interpretation and further calculation

k1sin⁡θ1=k2sin⁡θ2⇒n1sin⁡θ1=n2sin⁡θ2.k_1\sin\theta_1=k_2\sin\theta_2\Rightarrow\boxed{n_1\sin\theta_1=n_2\sin\theta_2}.λj=2π/kj⇒λ2/λ1=n1/n2.\lambda_j=2\pi/k_j\Rightarrow\boxed{\lambda_2/\lambda_1=n_1/n_2}.

Physical check

A constant boundary phase offset can be absorbed into an amplitude coefficient; different x or t dependence cannot match a uniform stationary boundary.