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1.1 Exercises, examples & solutions

Updated: 28 May 2026
Solution to Exercise 1

The orbit of the earth around the sun is almost circular. Thus, we can estimate the velocity of the earth as V=2πRTV = \frac{2\pi R}{T} with R=150106  kmR=150 \cdot 10^6 \; \mathrm{km} and T=1 year=31.6106  sT = 1\ \mathrm{year} = 31.6 \cdot 10^6 \; \mathrm{s}. This gives V=30  km/sV = 30 \; \mathrm{km/s}.

We compute the traveling time from light leaving the beam splitter, reflecting at the mirror on the side of the table and reaching the beam splitter again. The rest of the path is identical for both light beams and does not lead to a time difference.

Time for light parallel to VV:

  • one part - tail wind from aether and velocity (according to Classical Mechanics with Galilean Transformation) c+Vc+V.

  • Other part: head wind with velocity cVc-V. Thus traveling time:

t//=LcV+Lc+V=2Lc11V2c2t_{//} = \frac{L}{c-V} + \frac{L}{c+V} = \frac{2L}{c} \frac{1}{1-\frac{V^2}{c^2}}

Time to travel perpendicular to VV:

t=Lc2V2+Lc2V2=2Lc11V2c2t_\perp = \frac{L}{\sqrt{c^2 - V^2}} + \frac{L}{\sqrt{c^2 - V^2}} = \frac{2L}{c} \frac{1}{\sqrt{1-\frac{V^2}{c^2}}}

Putting in the numbers, we find Δt=3.671016  s \Delta t = 3.67 \cdot 10^{-16} \; \mathrm{s}

This time difference may be way to small to measure. And indeed, no ‘stop-watch’ experiment will work. But Michelson & Morley used interferometry, i.e. interference of light. So, relevant is the difference in phase of the two light beams. This can be assessed by turning the time difference into a length: Δs=cΔt=1.1107m\Delta s = c \Delta t =1.1 \cdot 10^{-7} \mathrm{m}. Compare this to the wave length of the (yellow) light used by Michelson and Morley: λ500  nm=5107  m\lambda \approx 500 \; \mathrm{nm} = 5 \cdot 10^{-7} \; \mathrm{m}. Conclusion: the expected time difference is well in reach of interferometry.