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Topic 1: Gravity and motion

Apply the relationships for orbital motion of satellites and planets, including Kepler's third law T^2 / r^3 = 4 pi^2 / (G M), orbital speed v = sqrt(G M / r), and the energy of an orbit (kinetic, gravitational potential and total)

A focused answer to the QCE Physics Unit 3 dot point on orbital motion. Derives orbital speed from setting gravitational force equal to centripetal force, applies Kepler's third law to satellites and planets, and works the kinetic and gravitational potential energies of a circular orbit with the standard QCAA geostationary-satellite example.

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What this dot point is asking

QCAA wants you to derive orbital relationships from first principles by setting gravitational force equal to centripetal force, apply Kepler's third law T2/r3=4Ο€2/(GM)T^2 / r^3 = 4 \pi^2 / (G M) to planetary and satellite systems, and compute the kinetic, gravitational potential and total energies of a circular orbit. This dot point appears in IA1 (orbital data tables to interpret), EA Paper 1 multiple choice on Kepler proportions, and EA Paper 2 derivations.

The answer

Orbital speed from gravity equals centripetal force

For a satellite of mass mm in a circular orbit of radius rr around a central body of mass MM, the gravitational force supplies all of the centripetal force:

GMmr2=mv2r\frac{G M m}{r^2} = \frac{m v^2}{r}

Cancelling mm and rearranging:

v=GMrv = \sqrt{\frac{G M}{r}}

Important features:

  • IMATH_15 does not depend on the satellite mass mm. A spaceship and a bolt would orbit at the same speed at the same altitude.
  • IMATH_17 decreases with increasing rr. Distant orbits are slower.
  • The satellite is in continuous free fall toward the central body, but its tangential velocity keeps it perpetually missing.

Kepler's third law

Substituting v=2Ο€r/Tv = 2 \pi r / T into v2=GM/rv^2 = G M / r:

4Ο€2r2T2=GMr\frac{4 \pi^2 r^2}{T^2} = \frac{G M}{r}

T2r3=4Ο€2GM\boxed{\frac{T^2}{r^3} = \frac{4 \pi^2}{G M}}

For all bodies orbiting the same central mass, the ratio T2/r3T^2 / r^3 is constant. This is Kepler's third law (originally stated for planets around the Sun, but applicable to any central-body system).

In ratio form, between two satellites of the same central body:

TA2TB2=rA3rB3\frac{T_A^2}{T_B^2} = \frac{r_A^3}{r_B^3}

This is the working form for QCAA problems that do not give you MM directly.

Try it: Kepler's third law calculator. Enter central mass and radius (or period) to get the other.

Kepler's first and second laws (qualitative)

QCAA may ask you to state these as background.

  • First law. Planetary orbits are ellipses with the Sun at one focus. Circular orbits are the special case of zero eccentricity.
  • Second law. A line from a planet to the Sun sweeps out equal areas in equal times. Equivalently, a planet moves faster when it is closer to the Sun (consistent with conservation of angular momentum).

Most calculations in QCE Physics use the circular-orbit simplification, but you may need to invoke the second law in IA1 when given an elliptical-orbit stimulus.

Energy of a circular orbit

The kinetic energy of a satellite in a circular orbit of radius rr is:

Ek=12mv2=GMm2rE_k = \tfrac{1}{2} m v^2 = \frac{G M m}{2 r}

(using v2=GM/rv^2 = G M / r). The gravitational potential energy, taking zero at infinity, is:

Ep=βˆ’GMmrE_p = - \frac{G M m}{r}

The total mechanical energy is:

Etot=Ek+Ep=GMm2rβˆ’GMmr=βˆ’GMm2rE_{\text{tot}} = E_k + E_p = \frac{G M m}{2 r} - \frac{G M m}{r} = - \frac{G M m}{2 r}

Key features:

  • IMATH_25 is negative, indicating a bound orbit.
  • IMATH_26 for any circular orbit. This is the virial theorem for an inverse-square force.
  • To raise a satellite to a higher orbit, you must add energy (move EtotE_{\text{tot}} closer to zero), and the satellite ends up moving more slowly. The work done lifts it against gravity faster than the kinetic energy can be replenished.

Escape velocity

The minimum launch speed from radius rr that lets a projectile reach infinity with zero kinetic energy:

12mvesc2=GMmr\tfrac{1}{2} m v_{\text{esc}}^2 = \frac{G M m}{r}

vesc=2GMr=2 vorbitv_{\text{esc}} = \sqrt{\frac{2 G M}{r}} = \sqrt{2} \, v_{\text{orbit}}

From Earth's surface, vescβ‰ˆ11.2v_{\text{esc}} \approx 11.2 km/s. From low Earth orbit, the orbital speed is about vorbitβ‰ˆ7.9v_{\text{orbit}} \approx 7.9 km/s, and the additional Ξ”v\Delta v to escape from there is about 3.33.3 km/s.

Try it: Escape velocity calculator and orbital energy calculator.

Worked example: a low Earth orbit

A satellite orbits 400 km above Earth's surface (r=RE+h=6.77Γ—106r = R_E + h = 6.77 \times 10^6 m). Orbital speed:

v=GMEr=6.67Γ—10βˆ’11Γ—5.97Γ—10246.77Γ—106=7.67Γ—103Β m/sv = \sqrt{\frac{G M_E}{r}} = \sqrt{\frac{6.67 \times 10^{-11} \times 5.97 \times 10^{24}}{6.77 \times 10^6}} = 7.67 \times 10^3 \text{ m/s}.

Period:

T=2Ο€rv=2π×6.77Γ—1067670=5550Β sβ‰ˆ92Β minutesT = \frac{2 \pi r}{v} = \frac{2 \pi \times 6.77 \times 10^6}{7670} = 5550 \text{ s} \approx 92 \text{ minutes}.

This matches the orbital period of the International Space Station.

How this appears in IA1 and IA2

IA1 data test. Expect a satellite or moon table (radii and periods, sometimes a missing column) with a question asking you to verify Kepler's third law or extract MM of the central body. Alternatively, a stimulus showing the orbital energies as a function of radius with questions on the virial theorem.

IA2 student experiment. A practical IA2 on orbits is hard to engineer directly, but a frequent design is the simple pendulum used to measure local gg, then comparing the inferred GME/RE2G M_E / R_E^2 against the textbook value. The orbital framework provides the EA-level theory for the Unit 3 justification.

Common traps

Forgetting that rr is measured from the centre of the central body, not the surface. Always add the planetary radius for satellites: r=RE+hr = R_E + h.

Treating vv or TT as depending on the satellite mass. Both depend only on MM (the central body) and rr.

Reversing the sign of EpE_p. Gravitational potential energy is negative with zero at infinity. The deeper into the well, the more negative.

Forgetting the factor of 2 in Etot=βˆ’GMm/(2r)E_{\text{tot}} = -G M m / (2 r). A common slip when working under exam time pressure.

Confusing escape velocity with orbital velocity. vesc=2 vorbitv_{\text{esc}} = \sqrt{2} \, v_{\text{orbit}} at the same radius. Escape is from infinity; orbit is a bound circular trajectory.

Using inconsistent units in Kepler's third law. If you mix days and seconds, or kilometres and metres, the constant changes. Always work in SI metres and seconds for QCAA problems.

In one sentence

For a satellite or planet in a circular orbit of radius rr around a central mass MM, gravitational force equals centripetal force, giving v=GM/rv = \sqrt{G M / r}, Kepler's third law T2/r3=4Ο€2/(GM)T^2 / r^3 = 4 \pi^2 / (G M), and a total mechanical energy Etot=βˆ’GMm/(2r)E_{\text{tot}} = - G M m / (2 r) that is negative for a bound orbit.

Past exam questions, worked

Real questions from past QCAA papers on this dot point, with our answer explainer.

2023 QCAA-style6 marksA geostationary communications satellite orbits Earth at a period of 24 hours. (a) Derive an expression for the orbital radius of a circular orbit by equating gravitational force and centripetal force. (b) Calculate the orbital radius and the altitude above Earth's surface. (c) Calculate the orbital speed. (Mass of Earth = 5.97 x 10^24 kg, radius of Earth = 6.37 x 10^6 m, G = 6.67 x 10^-11 N m^2 / kg^2; treat the period as exactly 86400 s.)
Show worked answer β†’

A 6-mark answer needs the derivation, the radius and altitude, and the orbital speed.

(a) Derivation. Gravitational force supplies centripetal force:

GMmr2=mv2r\frac{G M m}{r^2} = \frac{m v^2}{r}

so v2=GM/rv^2 = G M / r. Substituting v=2Ο€r/Tv = 2 \pi r / T:

IMATH_3
IMATH_4
T2r3=4Ο€2GM\frac{T^2}{r^3} = \frac{4 \pi^2}{G M} (Kepler's third law).

(b) Orbital radius. With T=86400T = 86400 s:

r3=6.67Γ—10βˆ’11Γ—5.97Γ—1024Γ—(86400)24Ο€2r^3 = \frac{6.67 \times 10^{-11} \times 5.97 \times 10^{24} \times (86400)^2}{4 \pi^2}

r3=3.98Γ—1014Γ—7.46Γ—10939.48=7.52Γ—1022r^3 = \frac{3.98 \times 10^{14} \times 7.46 \times 10^9}{39.48} = 7.52 \times 10^{22} m3^3.

r=(7.52Γ—1022)1/3=4.22Γ—107r = (7.52 \times 10^{22})^{1/3} = 4.22 \times 10^7 m.

Altitude above the surface = rβˆ’RE=4.22Γ—107βˆ’6.37Γ—106=3.59Γ—107r - R_E = 4.22 \times 10^7 - 6.37 \times 10^6 = 3.59 \times 10^7 m, that is, about 35 900 km.

(c) Orbital speed.

v=2Ο€rT=2π×4.22Γ—10786400=3.07Γ—103Β m/sv = \frac{2 \pi r}{T} = \frac{2 \pi \times 4.22 \times 10^7}{86400} = 3.07 \times 10^3 \text{ m/s}.

Markers reward the equating step, the substitution of v=2Ο€r/Tv = 2 \pi r / T to land Kepler's third law, the correct geostationary altitude (about 36 000 km), and the speed in m/s with consistent significant figures.

2022 QCAA-style3 marksTwo moons orbit a planet of mass M. Moon A has an orbital radius of 1.0 x 10^8 m and a period of 1.5 days. Moon B has an orbital radius of 4.0 x 10^8 m. Calculate the period of moon B.
Show worked answer β†’

Kepler's third law: T2/r3T^2 / r^3 is the same for both moons around the same central mass.

IMATH_1
IMATH_2
TB=12Β daysT_B = 12 \text{ days}.

Markers reward the explicit ratio form of Kepler's third law (no need to know MM), and the substitution kept in matching units (days here is fine because both periods are in the same unit).

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