Gravitational Fields: Question 5

Syllabus 13.2

Structured A2 10 marks

An exoplanet named Halvane has mass 5.40×1024 kg5.40\times10^{24}\text{ kg} and rotates on its axis once every 30.030.0 hours. A communications satellite is to be placed in a geostationary orbit around Halvane, so that it remains above the same point on Halvane's surface at all times.

Take G=6.67×1011 N m2 kg2G = 6.67\times10^{-11}\text{ N m}^2\text{ kg}^{-2}.

(a) Besides having an orbital period equal to Halvane's rotation period, state two further conditions that the satellite's orbit must satisfy for it to remain geostationary. [2]

(b) By equating the gravitational force on the satellite to the centripetal force required for circular motion, and writing the centripetal force in terms of the orbital period TT, show that the orbital radius rr of a geostationary orbit is given by r=(GMT24π2)1/3r = \left(\frac{GMT^2}{4\pi^2}\right)^{1/3} [3]

(c) Calculate the radius of the geostationary orbit around Halvane. [3]

(d) Calculate the orbital speed of the satellite in this geostationary orbit. [2]

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Worked solution

Part (a): Conditions for a geostationary orbit

Besides matching Halvane’s rotation period, a geostationary satellite must also:

  1. orbit in the plane of Halvane’s equator (so that it stays above the same latitude, namely 0°); and
  2. orbit in the same direction as Halvane’s rotation, i.e. west to east.

(A circular, rather than elliptical, orbit is also required for the satellite to stay at constant radius and constant angular speed above the same point, but the two conditions above are the standard additional requirements alongside a circular orbit.)

Part (b): Deriving the geostationary radius formula

For the satellite (mass mm) in a circular orbit of radius rr with period TT, its angular speed is ω=2π/T\omega=2\pi/T, so its centripetal acceleration is ω2r=(2π/T)2r\omega^2r=(2\pi/T)^2r. Equating the gravitational force to the required centripetal force: GMmr2=m(2πT)2r\frac{GMm}{r^2} = m\left(\frac{2\pi}{T}\right)^2r

Cancelling mm from both sides: GMr2=4π2T2r\frac{GM}{r^2} = \frac{4\pi^2}{T^2}r

Multiplying both sides by r2r^2: GM=4π2r3T2GM = \frac{4\pi^2r^3}{T^2}

Rearranging for r3r^3: r3=GMT24π2r^3 = \frac{GMT^2}{4\pi^2}

Taking the cube root of both sides: r=(GMT24π2)1/3r = \left(\frac{GMT^2}{4\pi^2}\right)^{1/3}

as required.

Part (c): Radius of the geostationary orbit

First convert the rotation period to seconds: T=30.0 hours=30.0×3600=1.08×105 sT = 30.0\text{ hours} = 30.0\times3600 = 1.08\times10^5\text{ s}

With M=5.40×1024 kgM=5.40\times10^{24}\text{ kg}: GM=(6.67×1011)(5.40×1024)GM = (6.67\times10^{-11})(5.40\times10^{24})

6.67×5.40=36.0186.67\times5.40=36.018, and 1011×1024=101310^{-11}\times10^{24}=10^{13}, so GM=3.6018×1014 m3 s2GM=3.6018\times10^{14}\text{ m}^3\text{ s}^{-2}.

T2=(1.08×105)2=1.1664×1010 s2T^2 = (1.08\times10^5)^2 = 1.1664\times10^{10}\text{ s}^2

GMT2=3.6018×1014×1.1664×1010=4.2011×1024GMT^2 = 3.6018\times10^{14}\times1.1664\times10^{10} = 4.2011\times10^{24}

(Working the coefficient: 3.6018×1.1664=4.20113.6018\times1.1664=4.2011; working the powers: 1014×1010=102410^{14}\times10^{10}=10^{24}.)

Dividing by 4π2=39.4784\pi^2=39.478: r3=4.2011×102439.478=1.0642×1023 m3r^3 = \frac{4.2011\times10^{24}}{39.478} = 1.0642\times10^{23}\text{ m}^3

Taking the cube root. Writing 1.0642×1023=106.42×10211.0642\times10^{23}=106.42\times10^{21}, so that the power of ten is a multiple of 33: r=106.423×107=4.739×107 m4.74×107 mr = \sqrt[3]{106.42}\times10^{7} = 4.739\times10^{7}\text{ m} \approx 4.74\times10^7\text{ m}

Check by cubing the answer back: (4.739×107)3=4.7393×1021=106.4×1021=1.064×1023 m3(4.739\times10^7)^3 = 4.739^3\times10^{21}=106.4\times10^{21}=1.064\times10^{23}\text{ m}^3, which matches r3r^3 found above. Also, as a sanity check, Halvane’s mass is somewhat less than Earth’s (5.97×1024 kg5.97\times10^{24}\text{ kg}) but its rotation period (30.030.0 hours) is longer than Earth’s (2424 hours), and Earth’s real geostationary radius is about 4.22×107 m4.22\times10^7\text{ m}, so a somewhat larger radius here (4.74×107 m4.74\times10^7\text{ m}) is physically reasonable.

Part (d): Orbital speed in the geostationary orbit

Using v=2πr/Tv=2\pi r/T: v=2π(4.739×107)1.08×105=2.9776×1081.08×105=2757 m s12.76×103 m s1v = \frac{2\pi(4.739\times10^7)}{1.08\times10^5} = \frac{2.9776\times10^8}{1.08\times10^5} = 2757\text{ m s}^{-1} \approx 2.76\times10^3\text{ m s}^{-1}

Check using v=GM/rv=\sqrt{GM/r} instead: GM/r=3.6018×1014/(4.739×107)=7.600×106GM/r=3.6018\times10^{14}/(4.739\times10^7)=7.600\times10^6; 7.600×106=2757 m s1\sqrt{7.600\times10^6}=2757\text{ m s}^{-1}. Both methods agree.

Final answers

  • (a) Orbit in the plane of Halvane’s equator; orbit in the same direction as Halvane’s rotation (west to east)
  • (b) r=(GMT2/4π2)1/3r=\boxed{(GMT^2/4\pi^2)^{1/3}} (derived from equating gravitational and centripetal force, with v=2πr/Tv=2\pi r/T)
  • (c) r=4.74×107 mr = \boxed{4.74\times10^7}\text{ m}
  • (d) v=2.76×103 m s1v = \boxed{2.76\times10^3}\text{ m s}^{-1}