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Problem Irodov 1.201

Jupiter takes 12 times as long as the Earth to complete one orbit around the Sun. Treating both orbits as circles centered on the Sun, find:

  1. the ratio of Jupiter’s orbital radius to the Earth’s;

  2. Jupiter’s orbital speed and acceleration, both in the heliocentric (Sun-centred, non-rotating) reference frame.

The Earth E and Jupiter J on their circular orbits about the Sun M, each with its orbital velocity v_E, v_J along its circle. The two radii are not drawn to scale.

The Earth EE and Jupiter JJ on their circular orbits about the Sun MM, each with its orbital velocity vE\vect v_E, vJ\vect v_J along its circle. The two radii are not drawn to scale.

Given
  • TJ=12 TET_J = 12\,T_E
Find
(a) rJ/rEr_J/r_E, (b) vJv_J, aJa_J

Solution

Step 1Kepler’s third law from the circular-orbit balance

For any planet of mass mm in a circular orbit of radius rr about the Sun, gravity supplies the centripetal force; writing the speed as the circumference over the period, v=2πr/Tv = 2\pi r/T, and eliminating vv gives a relation between TT and rr that holds, with the same constant, for every planet orbiting the same Sun.

γMmr2=mr(2πrT)2  ⟹  γM=4π2r3T2\frac{\gamma M m}{r^2} = \frac{m}{r}\left(\frac{2\pi r}{T}\right)^2 \;\Longrightarrow\; \gamma M = \frac{4\pi^2 r^3}{T^2}
T2=4π2γMr3T^2 = \dfrac{4\pi^2}{\gamma M}r^3
(1)
Step 2Distance ratio from the period ratio

Since γM\gamma M is the same Sun for both planets, applying (1) to Earth and to Jupiter and dividing one by the other cancels that constant, leaving the radius ratio in terms of the given period ratio alone.

(TJTE)2=(rJrE)3\left(\frac{T_J}{T_E}\right)^2 = \left(\frac{r_J}{r_E}\right)^3
rJrE=(TJTE)2/3=122/3\frac{r_J}{r_E} = \left(\frac{T_J}{T_E}\right)^{2/3} = 12^{2/3}
rJrE=122/3=5.2\dfrac{r_J}{r_E} = 12^{2/3} = 5.2
(2)
Step 3Jupiter’s orbital speed

The orbital speed is the circumference covered in one period. Writing Jupiter’s radius and period through the Earth’s own orbital data turns this into a number.

vJ=2πrJTJv_J = \frac{2\pi r_J}{T_J}

The Earth’s orbital radius and period are rE=1.50×1011 mr_E = 1.50\times10^{11}\ \mathrm{m} and TE=3.156×107 sT_E = 3.156\times10^{7}\ \mathrm{s}, so with rJ=122/3rEr_J = 12^{2/3}r_E and TJ=12 TET_J = 12\,T_E, the radius evaluates first,

rJ=122/3×1.50×1011 m=7.86×1011 m,(3)r_J = 12^{2/3}\times1.50\times10^{11}\ \mathrm m = 7.86\times10^{11}\ \mathrm m, \tag{3}

and then the speed,

vJ=2π(7.86×1011 m)12×3.156×107 s=1.30×104 m/s.v_J = \frac{2\pi\left(7.86\times10^{11}\ \mathrm m\right)}{12\times3.156\times10^{7}\ \mathrm s} = 1.30\times10^{4}\ \mathrm{m/s}.
vJ=2πrE121/3TE=13 km/sv_J = \dfrac{2\pi r_E}{12^{1/3}T_E} = 13\text{ km/s}
(4)
Step 4Jupiter’s centripetal acceleration

In uniform circular motion the centripetal acceleration is v2/rv^2/r; the speed (4) and the radius (3) give the number directly.

aJ=vJ2rJa_J = \frac{v_J^2}{r_J}
aJ=(1.30×104 m/s)27.86×1011 m=2.2×10−4 m/s2.a_J = \frac{(1.30\times10^{4}\ \mathrm{m/s})^2}{7.86\times10^{11}\ \mathrm m} = 2.2\times10^{-4}\ \mathrm{m/s^2}.
aJ=vJ2rJ=2.2×10−4 m/s2a_J = \dfrac{v_J^2}{r_J} = 2.2\times10^{-4}\text{ m/s}^2
(5)
Check

The same acceleration follows from the inverse square law directly, without ever going through vJv_J: γM/rJ2=(6.67×10−11)(1.97×1030)/(7.86×1011)2=2.1×10−4 m/s2\gamma M/r_J^2 = (6.67\times10^{-11})(1.97\times10^{30})/(7.86\times10^{11})^2 = 2.1\times10^{-4}\ \mathrm{m/s^2}, agreeing with the 2.2×10−4 m/s22.2\times10^{-4}\ \mathrm{m/s^2} of (5) to about two percent. That gap is not rounding: it is the mild inconsistency between the tabulated γM⊙\gamma M_\odot and the Earth’s own tabulated rEr_E, TET_E (the two imply values of γM⊙\gamma M_\odot that differ by about 1.8 percent), and both routes still express the same centripetal requirement.

Remark

Steps 1 and 2 never needed a value for γ\gamma or the Sun’s mass, only the given period ratio: any two planets sharing the same Sun can be compared this way without knowing γ\gamma or the Sun’s mass individually, because both cancel from the ratio. Only when an absolute distance or speed is wanted, as in Steps 3 and 4, does the Earth’s own orbit have to supply the missing scale, which is exactly how the Earth’s orbit serves as the meter stick for the rest of the solar system.