Physics • Year 12 • Module 5 • Lesson 11

Gravitational Orbits

Apply orbital velocity, Kepler’s Third Law, and geostationary conditions to real satellite data, calculations, and multi-step reasoning tasks.

Apply · Data & Reasoning

1. Satellite orbital speed calculations

The table below lists four Earth-orbiting satellites with their orbital altitudes. Use the constants provided to calculate the orbital speed of each. Show all working including r = RE + h. 8 marks (2 each)

Constants: G = 6.67 × 10−11 N m2 kg−2, ME = 5.97 × 1024 kg, RE = 6.37 × 106 m

Satellite Altitude h (km) Orbital radius r (m) Orbital speed v (m s−1)
ISS 400
Hubble Space Telescope 547
GPS satellite 20 200
Geostationary satellite 35 900

1.1 Describe the pattern between orbital altitude and orbital speed. Explain this relationship using the formula v = √(GM/r). 2 marks

Stuck? Calculate r = RE + h first (convert km to m), then substitute into v = √(GM/r).

2. Kepler’s Third Law — Jupiter’s moons

The table below shows the four Galilean moons of Jupiter with their orbital data. Use the data to verify Kepler’s Third Law for the Jovian system. 7 marks

Moon Period T (days) T (s) Orbital radius r (m) T² / r³ (s² m−3)
Io 1.769 4.22 × 108
Europa 3.551 6.71 × 108
Ganymede 7.155 1.07 × 109
Callisto 16.69 1.88 × 109

2.1 Convert each period to seconds and calculate T²/r³ for each moon. Record your values in the table. 4 marks

2.2 Are the T²/r³ values consistent with Kepler’s Third Law? Explain your reasoning, including what the constant represents physically. 2 marks

2.3 Use the constant T²/r³ = 4π²/(GMJ) to calculate the mass of Jupiter MJ. Show your working. 1 mark

Stuck? Multiply each day-period by 86 400 to get seconds. Then compute T2 and r3 separately before dividing.

3. Predict and justify — changing orbits

Answer each scenario question using physics reasoning and relevant formulas. 9 marks (3 each)

3.1 A satellite at radius r1 is boosted to a new orbit at radius r2 = 4r1. By what factor does its orbital speed change? By what factor does its period change? Show your working clearly.

3.2 A student claims: “Satellites in orbit need to fire engines continuously to stop falling into Earth.” Identify the physics error in this claim and write a corrected explanation of why a satellite does not fall to Earth.

3.3 Two satellites A and B orbit Earth at 400 km and 800 km altitude respectively. Satellite A has mass 500 kg and satellite B has mass 5000 kg. Compare their orbital speeds. Explain whether the mass difference affects the result.

Stuck? For Q3.1: use vr−1/2 and Tr3/2. For Q3.2: revisit the misconceptions box in the lesson.

4. Interpret a graph — T² vs r³ for Solar System planets

The graph below plots T² (in years2) against r³ (in AU3) for the eight planets of the Solar System. Each data point is labelled. 6 marks

0 2000 4000 6000 8000 10000 0 2000 4000 6000 8000 r³ (AU³) T² (years²) Mer/Ven/Ear/Mar Jupiter Saturn Uranus Neptune

Figure 4. T² vs r³ for the Solar System (AU and years units). Inner planets (Mercury, Venus, Earth, Mars) cluster near the origin and are shown as a single cluster. Best-fit dashed line shown.

4.1 Describe the shape of the best-fit line and explain what this tells you about the relationship between T² and r³. 2 marks

4.2 The gradient of this line equals 1 in AU/years units. Use T²/r³ = 4π²/(GM) to explain why the gradient would not equal 1 if you plotted the graph in SI units (seconds and metres). 2 marks

4.3 A newly discovered exoplanet orbits a star with the same mass as our Sun, at a distance of 2 AU. Use the graph trend to predict its orbital period in years. 2 marks

Stuck? The gradient is T²/r³ = constant = 1 in AU/year units (for the Sun). Apply T² = r³ to find T.
Answers — Do not peek before attempting

Q1 — Orbital speed calculations

Using r = RE + h and v = √(GM/r):

ISS: r = 6.37 × 106 + 4.00 × 105 = 6.77 × 106 m. v = √(6.67 × 10−11 × 5.97 × 1024 / 6.77 × 106) = 7.66 × 103 m s−1.

Hubble: r = 6.37 × 106 + 5.47 × 105 = 6.917 × 106 m. v = √(3.981 × 1014 / 6.917 × 106) = 7.59 × 103 m s−1.

GPS: r = 6.37 × 106 + 2.02 × 107 = 2.657 × 107 m. v = √(3.981 × 1014 / 2.657 × 107) = 3.87 × 103 m s−1.

Geostationary: r = 6.37 × 106 + 3.59 × 107 = 4.227 × 107 m. v = √(3.981 × 1014 / 4.227 × 107) = 3.07 × 103 m s−1.

Q1.1: As altitude increases, orbital speed decreases. From v = √(GM/r), speed is inversely proportional to the square root of orbital radius: v ∝ 1/√r. A larger radius means weaker gravitational pull and a lower speed needed to maintain orbit. Award 1 mark for identifying the inverse relationship, 1 mark for the formula-based explanation.

Q2 — Jupiter’s moons

Io: T = 1.769 × 86 400 = 1.528 × 105 s; T² = 2.335 × 1010 s2; r³ = (4.22 × 108)3 = 7.52 × 1025 m3; T²/r³ = 3.10 × 10−16 s2 m−3.

Europa: T = 3.551 × 86 400 = 3.068 × 105 s; T² = 9.41 × 1010 s2; r³ = (6.71 × 108)3 = 3.02 × 1026 m3; T²/r³ = 3.11 × 10−16 s2 m−3.

Ganymede: T = 7.155 × 86 400 = 6.182 × 105 s; T² = 3.82 × 1011 s2; r³ = (1.07 × 109)3 = 1.225 × 1027 m3; T²/r³ = 3.12 × 10−16 s2 m−3.

Callisto: T = 16.69 × 86 400 = 1.442 × 106 s; T² = 2.079 × 1012 s2; r³ = (1.88 × 109)3 = 6.645 × 1027 m3; T²/r³ = 3.13 × 10−16 s2 m−3.

Q2.2: Yes, all four values are approximately 3.1 × 10−16 s2 m−3 — consistent with Kepler’s Third Law. The constant equals 4π²/(GMJ) and depends only on the mass of Jupiter, not on which moon is used [1]. This confirms that T²/r³ = constant for all bodies orbiting the same central mass [1].

Q2.3: MJ = 4π² / (G × 3.11 × 10−16) = 39.48 / (6.67 × 10−11 × 3.11 × 10−16) ≈ 1.90 × 1027 kg (actual: 1.898 × 1027 kg). Award 1 mark for correct rearrangement and substitution with a value in the correct order of magnitude.

Q3.1 — Changing orbits

From v = √(GM/r): if r → 4r, then v → √(GM/4r) = v/2. Speed halves [1]. From T² = 4π²r³/(GM): if r → 4r, then T² → 4π²(4r)3/(GM) = 64 × 4π²r³/(GM), so T → 8T. Period increases by a factor of 8 [1]. Award 1 mark per correct factor with working shown.

Q3.2 — Satellite misconception

Error: the claim assumes a satellite needs continuous thrust to maintain orbit, as if it were “fighting gravity” [1]. Correct explanation: in a stable circular orbit, the gravitational force provides exactly the centripetal force needed to deflect the satellite’s path in a circle — no tangential thrust is required. The satellite is continuously “falling” toward Earth but its horizontal speed is large enough that it keeps missing the curved Earth beneath it. This is Newton’s concept of an orbit as perpetual free-fall [1]. Award 1 mark for identifying the error, 1 mark for the correct explanation involving gravity as centripetal force.

Q3.3 — Mass comparison

Satellite A (400 km): r = 6.77 × 106 m, vA ≈ 7.66 km s−1. Satellite B (800 km): r = 6.37 × 106 + 8.00 × 105 = 7.17 × 106 m; vB = √(3.981 × 1014/7.17 × 106) ≈ 7.45 km s−1 [1]. Satellite A is faster than B because it is at a lower orbit [1]. The mass difference (500 kg vs 5000 kg) has no effect on orbital speed; both masses cancel in the derivation GMm/r² = mv²/r, so orbital speed is independent of satellite mass [1].

Q4.1 — Graph shape

The best-fit line is a straight line through the origin [1]. This shows that T² is directly proportional to r³ — confirming Kepler’s Third Law: T² ∝ r³ with a constant ratio T²/r³ that is the same for all planets orbiting the Sun [1].

Q4.2 — Gradient in SI units

In AU/year units the gradient equals 1 because AU and year are defined so that Earth’s orbital data gives T²/r³ = 1 year²/AU³ by definition [1]. In SI units the gradient is 4π²/(GMSun) = 4π² / (6.67 × 10−11 × 1.99 × 1030) ≈ 2.97 × 10−19 s2 m−3, which is a very different numerical value [1].

Q4.3 — Exoplanet period prediction

In the same stellar system (same Sun-like mass), T² = r³ (AU, years). For r = 2 AU: T² = (2)3 = 8; T = √8 = 2√2 ≈ 2.83 years [1]. Award 1 mark for correct setup, 1 mark for final answer with units.