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Scaling the Solar System Keeps Time

Irodov 1.204DifficultyDifficulty 2 of 5UniquenessUniqueness 3 of 5

Problem Irodov 1.204

A model of the Solar System is built at a fixed linear scale factor η\eta (every length, including every body’s own size and every orbital distance, shrinks by the factor η\eta), using the same materials, and therefore the same density, as the real Sun and each real planet. Determine how the orbital period of a planet in the model compares with the orbital period of the real planet it represents.

The actual system (black) and a model scaled down by η, built from the same density (gray). Every length shrinks by η; the question is what that does to T.

The actual system (black) and a model scaled down by η\eta, built from the same density (gray). Every length shrinks by η\eta; the question is what that does to TT.

Given
  • Linear scale factor η\eta
  • density unchanged for every body
Find
How does the orbital period TT change?

Solution

Step 1Write Kepler’s third law for the two-body system

For a planet of mass mm orbiting a star of mass MM with semi-major axis aa, the exact two-body form of Kepler’s third law is

T2=4π2a3G(M+m).(1)T^2 = \frac{4\pi^2 a^3}{G(M+m)}. \tag{1}
Step 2Find how mass scales under the model’s construction

Every linear dimension of the model, including the size of each body and every orbital distance, is η\eta times the actual one; since the density is kept the same, a body’s mass, proportional to density times volume, scales as the cube of its linear size,

M′=η3M,m′=η3m,a′=ηa.(2)M' = \eta^3 M, \qquad m' = \eta^3 m, \qquad a' = \eta a. \tag{2}
Step 3Substitute the scaled quantities into Kepler’s law
T′2=4π2(a′)3G(M′+m′)=4π2(ηa)3G η3(M+m)=η3η3⋅4π2a3G(M+m)=T2.\begin{align*} T'^2 &= \frac{4\pi^2 (a')^3}{G(M'+m')} = \frac{4\pi^2 (\eta a)^3}{G\,\eta^3(M+m)} \\ &= \frac{\eta^3}{\eta^3}\cdot\frac{4\pi^2 a^3}{G(M+m)} = T^2. \tag{3}\end{align*}
T′=TT' = T
(4)
Check

The same cancellation shows up in the orbital speed: since v=G(M+m)/av = \sqrt{G(M+m)/a}, the model’s speed is v′=Gη3(M+m)/(ηa)=η vv' = \sqrt{G\eta^3(M+m)/(\eta a)} = \eta\, v, a factor η\eta slower. The model’s orbit is also a factor η\eta shorter, so the ratio of path length to speed, the period, is unchanged either way it is computed.

Remark

The period depends on the body only through its mean density, not through its size: doubling every length while keeping the density fixed leaves TT untouched. A model built from a lighter material, rather than a smaller one, would change the period; a model merely scaled down in size, at the same density, would not.