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Inquiry Question 3: How does the force of gravity determine the motion of planets and satellites?

Derive and apply the concept of gravitational potential energy in a radial gravitational field, U = -G M m / r, including the concept of escape velocity

A focused answer to the HSC Physics Module 5 dot point on gravitational potential energy in radial fields. Why U is negative, how it differs from the mgh approximation, the derivation of escape velocity, and the standard worked example using Earth.

Generated by Claude Opus 4.88 min answer

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  1. What this dot point is asking
  2. The answer
  3. Examples in context
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What this dot point is asking

NESA wants you to extend the idea of gravitational potential energy from the near-Earth U=mghU = mgh approximation to the full radial-field formula U=GMm/rU = -G M m / r, explain why it is negative, and apply it to problems including escape velocity. This dot point underpins every energy-based question on orbital motion in the second half of Module 5.

The answer

From mghmgh to the radial formula

Near Earth's surface, gravitational field strength gg is approximately constant, and U=mghU = mgh works fine. At astronomical scales, gg falls off as 1/r21/r^2, so the potential energy must be obtained by integrating the gravitational force from infinity inward:

U(r)=rFdr=r(GMmr2)dr=GMmrU(r) = -\int_{\infty}^{r} F \, dr = -\int_{\infty}^{r} \left(-\frac{G M m}{r^2}\right) dr = -\frac{G M m}{r}

The negative sign reflects two choices:

  1. Zero potential energy at infinity (the natural reference for radial fields).
  2. Attractive force, so moving inward releases energy.

A bound mass (closer than infinity) therefore has U<0U < 0.

Why negative U makes physical sense

Gravitational potential energy versus distance A plot of gravitational potential energy U on the y axis against distance r from a central mass on the x axis. U is zero at infinity and falls steeply negative as r approaches zero, forming a potential well. Escape from the well requires kinetic energy equal in magnitude to U at the starting radius. U r 0 U = −GMm⁄r U → 0 as r → ∞ Bound objects have U < 0. Escape velocity makes total energy zero at infinity.

Imagine releasing a stationary object from far away. Gravity does positive work pulling it inward, increasing kinetic energy. By conservation of energy, potential energy must decrease. Since we set U=0U = 0 at infinity, UU becomes negative as the object approaches the source.

The deeper into the well, the more negative UU becomes. To free a mass from the well (push it to infinity), positive work must be done equal to U=GMmr|U| = \frac{G M m}{r}.

Escape velocity

Escape velocity vescv_{\text{esc}} is the minimum speed needed at a distance rr for an object to reach infinity with zero remaining kinetic energy. By conservation of energy:

12mvesc2+(GMmr)=0+0\frac{1}{2} m v_{\text{esc}}^2 + \left(-\frac{G M m}{r}\right) = 0 + 0

Solving:

vesc=2GMrv_{\text{esc}} = \sqrt{\frac{2 G M}{r}}

Key features:

  • Independent of the mass of the escaping object.
  • Depends on the mass MM of the source and the launch distance rr.
  • At Earth's surface: vesc11.2v_{\text{esc}} \approx 11.2 km/s.
  • For a black hole, rr shrinks until vescv_{\text{esc}} approaches the speed of light.

Change in potential energy

When a mass moves from r1r_1 to r2r_2:

ΔU=U(r2)U(r1)=GMmr2(GMmr1)=GMm(1r11r2)\Delta U = U(r_2) - U(r_1) = -\frac{G M m}{r_2} - \left(-\frac{G M m}{r_1}\right) = G M m \left(\frac{1}{r_1} - \frac{1}{r_2}\right)

If r2>r1r_2 > r_1 (moving away), ΔU>0\Delta U > 0: potential energy increases (becomes less negative).

Examples in context

Example 1. Escape velocity for an ANU Mt Stromlo deep-space probe. A research probe is launched from Earth's surface (ME=5.97×1024 kgM_E = 5.97 \times 10^{24} \text{ kg}, rE=6.37×106 mr_E = 6.37 \times 10^6 \text{ m}). The escape speed is vesc=2GME/rE=2×6.674×1011×5.97×1024/6.37×106=1.12×104 m/sv_{\text{esc}} = \sqrt{2 G M_E / r_E} = \sqrt{2 \times 6.674 \times 10^{-11} \times 5.97 \times 10^{24} / 6.37 \times 10^6} = 1.12 \times 10^4 \text{ m/s} (about 11.2 km/s11.2 \text{ km/s}). At the standard rocket exhaust speed of 4.4 km/s4.4 \text{ km/s}, the Tsiolkovsky equation requires a mass ratio e11.2/4.4=12.7e^{11.2/4.4} = 12.7, so a 1000 kg1000 \text{ kg} probe needs 12.7\sim 12.7 tonnes of propellant. This is why Australian Mt Stromlo deep-space work relies on overseas launchers with multi-stage Saturn-class capacity.

Example 2. Lifting water in Snowy Hydro 2.0 pumped storage. Snowy 2.0 lifts water from Talbingo reservoir to Tantangara reservoir through a vertical head of h=700 mh = 700 \text{ m}. For each 1.0 kg1.0 \text{ kg} of water raised, the gain in gravitational PE is ΔU=mgh=1.0×9.8×700=6.86×103 J\Delta U = m g h = 1.0 \times 9.8 \times 700 = 6.86 \times 10^3 \text{ J}. At a flow rate of 300 m3/s300 \text{ m}^3/\text{s} (so 3.0×105 kg/s3.0 \times 10^5 \text{ kg/s}), the pumping power required is P=3.0×105×6.86×103=2.06×109 W=2.06 GWP = 3.0 \times 10^5 \times 6.86 \times 10^3 = 2.06 \times 10^9 \text{ W} = 2.06 \text{ GW}, matching the station's nameplate generating capacity once the energy is later released through the Francis turbines.

Try this

Q1. Write the formula for gravitational potential energy of a mass mm at distance rr from a body of mass MM and explain the choice of zero. [2 marks]

  • Cue. U=GMm/rU = -G M m / r; zero taken at r=r = \infty, so all finite-rr values are negative.

Q2. A 250 kg250 \text{ kg} payload is moved from the surface of Earth to a circular orbit at altitude 500 km500 \text{ km}. Calculate the change in gravitational PE. [4 marks]

  • Cue. ΔU=GMEm(1/r21/r1)\Delta U = -G M_E m (1/r_2 - 1/r_1) with r1=6.37×106r_1 = 6.37 \times 10^6, r2=6.87×106r_2 = 6.87 \times 10^6. Compute ΔU1.14×109 J\Delta U \approx 1.14 \times 10^9 \text{ J}.

Q3. A 1500 kg1500 \text{ kg} spacecraft is fired straight up at 9.0 km/s9.0 \text{ km/s} from Earth's surface. (a) Calculate its total mechanical energy. (b) Find the maximum height above Earth's centre reached. (c) Determine whether it escapes Earth's gravity. [2+3+2 marks]

  • Cue. (a) E=12mv2GMEm/rE=6.08×10109.38×1010=3.30×1010 JE = \tfrac{1}{2} m v^2 - G M_E m / r_E = 6.08 \times 10^{10} - 9.38 \times 10^{10} = -3.30 \times 10^{10} \text{ J}. (b) rmax=GMEm/E=1.81×107 mr_{\max} = -G M_E m / E = 1.81 \times 10^7 \text{ m}. (c) E<0E < 0, does not escape.

Exam-style practice questions

Practice questions written in the style of NESA exam questions on this dot point, with worked answer explainers. The year tag is the paper they imitate, not the source.

2021 HSC4 marksCalculate the escape velocity from the surface of the Earth. (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.)
Show worked answer →

Escape velocity is the minimum speed an object needs at a distance rr from the centre of a mass MM to just barely escape to infinity with zero kinetic energy remaining.

Conservation of energy from the surface to infinity (where both UU and KK are zero):

12mvesc2GMmr=0\frac{1}{2} m v_{\text{esc}}^2 - \frac{G M m}{r} = 0.

Solving for vescv_{\text{esc}}:

vesc=2GMrv_{\text{esc}} = \sqrt{\frac{2 G M}{r}}.

Substituting:

vesc=2×6.67×1011×5.97×10246.37×106v_{\text{esc}} = \sqrt{\frac{2 \times 6.67 \times 10^{-11} \times 5.97 \times 10^{24}}{6.37 \times 10^6}}
vesc=7.96×10146.37×106v_{\text{esc}} = \sqrt{\frac{7.96 \times 10^{14}}{6.37 \times 10^6}}
vesc=1.25×108v_{\text{esc}} = \sqrt{1.25 \times 10^8}
vesc=1.12×104v_{\text{esc}} = 1.12 \times 10^4 m/s, or about 11.211.2 km/s.

Markers reward the derivation from conservation of energy, the correct identification of the boundary conditions (zero energy at infinity), and the final answer with units. Note that escape velocity does not depend on the mass of the escaping object.

2019 HSC3 marksExplain why gravitational potential energy in a radial field is taken to be negative, and why this is physically reasonable.
Show worked answer →

Gravitational potential energy in a radial field is defined as:

U=GMmrU = -\frac{G M m}{r}.

The negative sign arises from the choice of zero potential energy at infinity (the natural reference point for radial fields). Because gravity is always attractive, the gravitational force does positive work on a mass as it moves from infinity inward, reducing its potential energy below zero.

Physically, this means a mass that is bound to a gravitational source (such as a planet in orbit) has less energy than a free mass at infinity. To escape the field, work must be done against gravity equal to GMmr\frac{G M m}{r}, which raises the potential energy to zero at infinity.

The familiar formula U=mghU = m g h is the linear approximation valid near a planet's surface where gg is approximately constant. At astronomical scales, gg varies with rr and the full radial formula must be used.

Markers reward the explicit reference point at infinity, the link between attractive force and negative potential energy, and the comparison with mghmgh.

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