OCR A Level Physics · H556 · 5.4.1–5.4.4 · Gravitational fields

Gravitational fields: worked solutions

OCR A A-level gravitational fields worked solutions: satellites, Kepler laws, potential graphs, launch energy and escape, with applications and examiner guidance.

14 original questions · 93 marks

Read the OCR A gravitational fields notes

Constants and assumptions: Use G = 6.67 × 10⁻¹¹ N m² kg⁻² unless GM is supplied. Distance r is measured from the source’s centre; altitude h is added to surface radius R. Potential and gravitational potential energy are zero at infinity. Signed radial components use outward as positive unless another direction is defined. Retain unrounded intermediate values; model planets and probes as stated in each question.

Attempt each question before opening the hints. Show equations, substitutions, units and the reason for your method. The mark checklists below are PhysicsUK's own schemes.

Lessons from the examiner reports

These reports identify skills worth practising. The questions below are original PhysicsUK examples, with our own mark schemes.

Question 1 · Exam-style Newton’s law and interaction pair · 5 marks

Gravity between laboratory spheres

Specification: 5.4.1(b), 5.4.2(a), 3.2.1(e)

Two identical, non-overlapping spheres each have mass 5.00 × 10³ kg and radius 0.600 m. Their mass distributions are spherically symmetric. The gap between their nearest surfaces is 2.40 m. Neglect other gravitational sources.

  1. Calculate the magnitude of the gravitational force between them. [3]
  2. One sphere is held fixed by a support. Describe the gravitational forces the two spheres exert on each other and explain whether holding one fixed changes the gravitational interaction. [2]
Small hint

Newton’s law uses the separation of the centres. Include both radii.

Method hint

Use r = gap + 2R, then F = GMm/r². The interaction pair acts on different objects.

Complete worked solution and marks

Answer: Centre separation = 3.60 m; force magnitude = 1.29 × 10⁻⁴ N. The mutual forces remain equal in magnitude and opposite in direction.

  1. r = 2.40 + 0.600 + 0.600 = 3.60 m. Spherical symmetry permits the external point-mass model.
  2. F = GMm/r² = (6.67 × 10⁻¹¹)(5.00 × 10³)²/(3.60)² = 1.29 × 10⁻⁴ N.
  3. Each force points along the line of centres towards the other sphere. They are a Newton’s third-law pair: equal magnitudes, opposite directions, acting on different spheres.
  4. The support balances the force on the held sphere. It changes that sphere’s resultant force and acceleration, not the mutual gravitational force at the same masses and separation.
Use both radii to find centre separation. Mutual gravitational forces act on different spheres.
Use both radii to find centre separation. Mutual gravitational forces act on different spheres. Open the larger diagram

Check: G has units N m² kg⁻², so GMm/r² is in newtons. A tiny force is reasonable even for substantial laboratory masses.

Mark checklist · 5 marks

  • 1 mark — Uses centre separation r = 3.60 m.
  • 1 mark — Substitutes masses and distance into F = GMm/r².
  • 1 mark — Obtains F ≈ 1.29 × 10⁻⁴ N.
  • 1 mark — Describes equal, opposite attractive forces acting on different objects.
  • 1 mark — Explains the support changes the resultant, not the interaction at fixed separation.

Common mistake: Using 2.40 m overestimates the force. Do not add the interaction pair to get a zero force on one sphere; its partner force acts on the other sphere.

Exam technique: Show the chosen physical model, centre-to-centre distances and units before substituting. These original questions use PhysicsUK mark guidance; linked OCR lessons concern the named source parts.

Try a changed context

Move the same spheres so their centres are 7.20 m apart. What is the force, and what is the new surface gap?

Check the transfer answer

Doubling centre separation divides force by four: F = 3.22 × 10⁻⁵ N. The gap is 7.20 − 1.20 = 6.00 m; doubling the gap would not double the centre separation.

Question 2 · Exam-style field definition, uncertainty and field lines · 7 marks

A lander measures a planet’s mass

Specification: 5.4.1(a), 5.4.1(c), 5.4.1(d), 5.4.2(b), 5.4.2(c), 2.2.1(c)

A stationary lander measures gravitational field-strength magnitude at the surface of a spherical, non-rotating planet: g = (8.00 ± 0.16) N kg⁻¹. Imaging gives its radius R = (6.00 ± 0.06) × 10⁶ m. Other bodies have negligible effects. Treat G as exact and use the conservative rule that fractional uncertainties add, with powers multiplying them.

  1. Define gravitational field strength. [1]
  2. Calculate the planet’s mass. [2]
  3. Estimate the percentage and absolute uncertainty in this mass. [2]
  4. Sketch the field lines outside the planet. State how the pattern changes when viewing a small region just above the surface. [2]
Small hint

g is force per unit mass. Radius is squared in M = gR²/G, so its fractional uncertainty is counted twice.

Method hint

Use M = gR²/G and ΔM/M ≈ Δg/g + 2ΔR/R. Compare a global radial field with a local approximately uniform field.

Complete worked solution and marks

Answer: M = 4.32 × 10²⁴ kg; uncertainty ≈ 4.0%, or 0.17 × 10²⁴ kg. Field lines point radially inward; locally they are approximately parallel and equally spaced.

  1. Gravitational field strength is force per unit mass on a small test mass: g = F/m.
  2. M = gR²/G = 8.00(6.00 × 10⁶)²/(6.67 × 10⁻¹¹) = 4.32 × 10²⁴ kg.
  3. ΔM/M ≈ 0.16/8.00 + 2(0.06/6.00) = 0.040 = 4.0%.
    ΔM = 0.040M ≈ 0.17 × 10²⁴ kg, giving M ≈ (4.32 ± 0.17) × 10²⁴ kg.
  4. For the full planet, draw radial lines with arrows pointing towards its centre. Lines spread out with increasing radius, indicating weaker field. In a patch whose size and height range are small compared with R, they are approximately parallel and equally spaced, so g is approximately uniform.
Outside a spherical source, field lines are radial and point inward. A small surface patch is approximately uniform.
Outside a spherical source, field lines are radial and point inward. A small surface patch is approximately uniform. Open the larger diagram

Check: The uncertainty is a conservative first-order estimate, as instructed, not a statistical quadrature result. More precise local g does not remove a radius uncertainty.

Mark checklist · 7 marks

  • 1 mark — Defines g as force per unit mass on a test mass.
  • 1 mark — Uses M = gR²/G with radius in metres.
  • 1 mark — Obtains M ≈ 4.32 × 10²⁴ kg.
  • 1 mark — Adds 2.0% from g and twice 1.0% from R to obtain 4.0%.
  • 1 mark — Gives absolute uncertainty ≈ 0.17 × 10²⁴ kg with matching scale.
  • 1 mark — Sketches radial inward arrows outside the sphere.
  • 1 mark — Describes approximately parallel, equally spaced lines in a small surface region.

Common mistake: Mass is proportional to R² in this rearrangement, not inversely proportional. “Gravity acts down” is a local description; globally it points towards the centre.

Exam technique: Show the chosen physical model, centre-to-centre distances and units before substituting. These original questions use PhysicsUK mark guidance; linked OCR lessons concern the named source parts.

Try a changed context

For the exterior field, plot y = lg[g/(N kg⁻¹)] against x = lg[r/m]. What gradient do you predict?

Check the transfer answer

Since g = GM/r² in magnitude, y = lg[GM/(m³ s⁻²)] − 2x. The gradient is −2, showing an inverse-square power law. lg means base-10 log, and the logarithm arguments are dimensionless.

Question 3 · Exam-style radius, field strength and circular motion · 7 marks

A mapping satellite and its weightless crew

Specification: 5.4.1(d), 5.4.2(b), 5.4.3(b), 5.4.3(c), 5.2.2(a)

A crewed mapping satellite follows a circular orbit 400 km above a spherical planet of radius 6.40 × 10⁶ m. For this planet GM = 4.00 × 10¹⁴ m³ s⁻². Ignore atmosphere, rotation and other bodies. A crew member floats without touching the cabin.

  1. Calculate gravitational field-strength magnitude at the satellite. [2]
  2. Calculate orbital speed and period. [3]
  3. Explain the crew member’s apparent weightlessness without claiming gravity has vanished. [2]
Small hint

Add the altitude to the radius. Gravity supplies the inward acceleration of both cabin and crew.

Method hint

Use r = R + h, g = GM/r², v = √(GM/r) and T = 2πr/v. Apparent weight depends on contact force.

Complete worked solution and marks

Answer: r = 6.80 × 10⁶ m; g = 8.65 N/kg; v = 7.67 × 10³ m/s; T = 5.57 × 10³ s (92.8 min). Cabin and crew share free-fall acceleration, so the floating crew member has no support force.

  1. r = 6.40 × 10⁶ + 400 × 10³ = 6.80 × 10⁶ m.
    g = GM/r² = 8.65 N kg⁻¹, towards the centre.
  2. GMm/r² = mv²/r, so v = √(GM/r) = 7.67 × 10³ m s⁻¹.
  3. T = 2πr/v = 5.57 × 10³ s = 92.8 min.
  4. Both cabin and crew accelerate towards the planet at approximately the same g. The floating crew member needs no cabin support/contact force. This absence produces apparent weightlessness, even though the gravitational force remains substantial.
Tangent velocity and inward acceleration coexist. Cabin and floating crew share the same free-fall acceleration.
Tangent velocity and inward acceleration coexist. Cabin and floating crew share the same free-fall acceleration. Open the larger diagram

Check: Surface g = 9.77 N/kg, so the orbital field is about 89% of its surface value. The period is much shorter than a day, so this is not a stationary communications orbit.

Mark checklist · 7 marks

  • 1 mark — Uses orbital radius R + h in metres.
  • 1 mark — Obtains g ≈ 8.65 N/kg.
  • 1 mark — Equates gravity to centripetal force or uses v² = GM/r.
  • 1 mark — Obtains v ≈ 7.67 × 10³ m/s.
  • 1 mark — Uses circumference to obtain T ≈ 5.57 × 10³ s.
  • 1 mark — Explains cabin and crew share gravitational/free-fall acceleration.
  • 1 mark — Links apparent weightlessness to absent support/contact force, not absent gravity.

Common mistake: A vacuum removes air resistance, not gravity. “No resultant force” would imply straight-line constant velocity and is incompatible with this orbit.

Exam technique: Show the chosen physical model, centre-to-centre distances and units before substituting. These original questions use PhysicsUK mark guidance; linked OCR lessons concern the named source parts.

Try a changed context

Double the satellite’s mass while keeping the same circular radius. What changes in g, v, T and gravitational force?

Check the transfer answer

g, v and T are unchanged; satellite mass cancels from the orbit equation. Its gravitational force doubles, as does the required mv²/r. The larger force accelerates twice the mass.

Question 4 · Exam-style Kepler derivation and ratio application · 6 marks

Two exoplanets around the same star

Specification: 5.4.3(b), 5.4.3(c), 5.4.3(d)

Two planets of negligible mass compared with their host star have circular orbits. Planet A has radius 0.200 AU and period 20.0 days. Planet B has radius 0.320 AU. You do not need the numerical size of an AU for the ratio calculation.

  1. Starting with Newton’s law of gravitation and circular motion, derive T² = (4π²/GM)r³. [3]
  2. Calculate B’s orbital period and explain why the same proportionality constant applies to both planets. [3]
Small hint

The planet mass cancels. The shared constant depends on the star’s mass, not the orbiting planet’s mass.

Method hint

Equate GMm/r² to m(2πr/T)²/r, rearrange, then use (TB/TA)² = (rB/rA)³ with consistent ratio units.

Complete worked solution and marks

Answer: T² = (4π²/GM)r³; B’s period = 40.5 days. Both orbits share the same central stellar mass M.

  1. GMm/r² = mv²/r, with v = 2πr/T.
  2. GM/r² = 4π²r/T², giving T² = (4π²/GM)r³.
  3. For the same host star and negligible planet masses, 4π²/GM is constant. The circular orbit’s radius is measured from the star’s centre.
  4. TB = TA(rB/rA)^(3/2) = 20.0(0.320/0.200)^(3/2) = 40.5 days. Consistent AU and day units cancel in the ratios.

Check: The radius ratio is 1.60, so period increases by 1.60^(3/2) ≈ 2.02, not by 1.60 or 1.60³. Dimensional check: r³/(GM) has unit s².

Mark checklist · 6 marks

  • 1 mark — Equates gravitational force with the required centripetal force.
  • 1 mark — Substitutes v = 2πr/T and cancels m.
  • 1 mark — Rearranges to T² = (4π²/GM)r³.
  • 1 mark — Forms the correct squared-period/cubed-radius ratio.
  • 1 mark — Obtains TB ≈ 40.5 days.
  • 1 mark — Explains the same central mass gives the same constant.

Common mistake: T² = r³ is only true for specially chosen units and normalization. In SI, keep the physical constant. A ratio from different stars cannot assume that it cancels.

Exam technique: Show the chosen physical model, centre-to-centre distances and units before substituting. These original questions use PhysicsUK mark guidance; linked OCR lessons concern the named source parts.

Try a changed context

If a second star had twice the mass, what period would a negligible-mass planet have at the same 0.320 AU radius?

Check the transfer answer

At fixed radius T ∝ M⁻¹/², so its period is 40.477/√2 = 28.6 days. This comparison requires the stated double stellar mass.

Question 5 · Exam-style data consistency and scaled graph gradient · 7 marks

Use orbit data to weigh an unseen planet

Specification: 5.4.3(c), 5.4.3(d), 1.1.3(d)(ii)

Three small moons orbit the same spherical planet in approximately circular orbits. The measured data are below. A best-fit plot has T²/(10⁸ s²) vertically and r³/(10²¹ m³) horizontally; its gradient is 4.93. Treat moon masses as negligible. Assess consistency at the precision of the rounded data.

  1. Calculate T²/r³ for each moon, using SI units, and decide whether these observations support Kepler’s third law. [3]
  2. Use the supplied graph gradient to calculate the planet’s mass. [3]
  3. State a physical assumption needed for this inference. [1]
Moon observations
Moonr / 10⁶ mT / hours
A8.004.42
B12.08.11
C16.012.49
Small hint

Hours must become seconds. The numerical gradient 4.93 includes different scale factors on the two axes.

Method hint

Calculate T²/r³ row by row. The physical gradient is 4.93 × 10⁸/10²¹ s²/m³, equal to 4π²/(GM).

Complete worked solution and marks

Answer: T²/r³ ≈ (4.95, 4.93, 4.94) × 10⁻¹³ s²/m³. Physical gradient = 4.93 × 10⁻¹³ s²/m³; M = 1.20 × 10²⁴ kg.

  1. TA = 4.42 × 3600 = 15 912 s.
    TA²/rA³ = 15 912²/(8.00 × 10⁶)³ = 4.95 × 10⁻¹³ s² m⁻³.
  2. TB = 29 196 s gives 4.93 × 10⁻¹³; TC = 44 964 s gives 4.94 × 10⁻¹³ s² m⁻³. These are approximately constant at the stated precision, supporting T² ∝ r³.
  3. S = 4.93(10⁸ s²)/(10²¹ m³) = 4.93 × 10⁻¹³ s² m⁻³.
  4. M = 4π²/(GS) = 4π²/[(6.67 × 10⁻¹¹)(4.93 × 10⁻¹³)] = 1.20 × 10²⁴ kg.
  5. One valid additional assumption is that other bodies provide negligible perturbations, so the planet supplies essentially all of the centripetal force. The supplied circular and negligible-moon-mass assumptions also matter; the inverse-square field must be appropriate at these exterior radii.
Original moon data on scaled T²–r³ axes. Restore both axis scale factors before using the gradient to find M.
Original moon data on scaled T²–r³ axes. Restore both axis scale factors before using the gradient to find M. Open the larger diagram

Check: The physical gradient has units s²/m³; GS has units kg⁻¹, so 4π²/(GS) is a mass. Moon C’s radius is twice A’s, so its period should be about √8 times A’s.

Mark checklist · 7 marks

  • 1 mark — Converts hour periods into seconds.
  • 1 mark — Correctly evaluates T²/r³ for at least two named rows.
  • 1 mark — Evaluates the remaining row and justifies approximate constancy, rather than exact identity.
  • 1 mark — Restores both graph axis scale factors to obtain S = 4.93 × 10⁻¹³ s²/m³.
  • 1 mark — Uses M = 4π²/(GS).
  • 1 mark — Obtains M ≈ 1.20 × 10²⁴ kg.
  • 1 mark — States a relevant gravitational/circular-orbit/negligible-moon-mass assumption.

Common mistake: Unlabelled calculations make the comparison hard to assess. A plot of T against r is not straight: use T² and r³. Do not insert the unscaled number 4.93 into the SI formula.

Exam technique: Show the chosen physical model, centre-to-centre distances and units before substituting. These original questions use PhysicsUK mark guidance; linked OCR lessons concern the named source parts.

Try a changed context

What is the period of a fourth circular moon at r = 20.0 × 10⁶ m using the fitted gradient?

Check the transfer answer

T = √(Sr³) = √[(4.93 × 10⁻¹³)(20.0 × 10⁶)³] = 6.28 × 10⁴ s = 17.4 hours. Use the physical gradient and retain unrounded working.

Question 6 · Exam-style geostationary design and mission reasoning · 6 marks

Choose an orbit for a communications network

Specification: 5.4.3(c), 5.4.3(e)

Use a spherical-Earth model with GM = 4.00 × 10¹⁴ m³ s⁻², radius 6.40 × 10⁶ m and rotation period 86 164 s. A broadcaster wants a satellite that appears fixed to an equatorial ground antenna. A separate mission needs close-up atmospheric measurements over many latitudes.

  1. State the conditions for the broadcaster’s geostationary orbit. [2]
  2. Calculate its orbital radius and height above the surface. [2]
  3. Give one advantage for broadcasting and one mission-specific reason this orbit is unsuitable for the atmospheric mission. [2]
Small hint

Matching the period alone is not sufficient. A geostationary orbit must remain in the equatorial plane and rotate with Earth.

Method hint

Use r³ = GMT²/(4π²), then h = r − R. Tie each orbital choice to what the instruments or ground system need.

Complete worked solution and marks

Answer: Circular equatorial orbit, eastward with Earth, T = 86 164 s. r = 4.22 × 10⁷ m; h = 3.58 × 10⁷ m. A fixed antenna is useful; a lower orbit visiting many latitudes better serves close atmospheric sampling.

  1. The orbit must be circular, in the equatorial plane, in the same eastward sense as Earth’s rotation, with T equal to Earth’s rotation period. Together these give a fixed position relative to the surface.
  2. r = [GMT²/(4π²)]^(1/3) = 4.22 × 10⁷ m.
  3. h = r − R = 4.2213 × 10⁷ − 6.40 × 10⁶ = 3.58 × 10⁷ m, about 35 800 km.
  4. The apparent fixed direction permits a fixed receiving/transmitting ground antenna and continuous contact with the chosen region when it is in view.
  5. For the atmospheric mission, this large altitude prevents close-up sampling of the upper atmosphere; the equatorial orbit also does not pass over many latitudes. A suitably inclined low orbit can address those goals. Either clearly linked limitation answers the requested one reason.
Separate orbital radius from surface altitude. The geostationary conditions concern motion relative to Earth’s surface.
Separate orbital radius from surface altitude. The geostationary conditions concern motion relative to Earth’s surface. Open the larger diagram

Check: 86 164 s is the supplied sidereal rotation period. Using the rounded 24 h value instead would alter r slightly; use the data given. Relative to Earth’s centre the satellite moves at about 3.08 km/s.

Mark checklist · 6 marks

  • 1 mark — States circular orbit in the equatorial plane.
  • 1 mark — States same rotational sense and period as Earth.
  • 1 mark — Uses the supplied period to obtain r ≈ 4.22 × 10⁷ m.
  • 1 mark — Subtracts Earth’s radius to obtain h ≈ 3.58 × 10⁷ m.
  • 1 mark — Links fixed apparent direction/continuous regional coverage to broadcasting.
  • 1 mark — Links altitude or latitude coverage to the stated atmospheric mission.

Common mistake: “It stays still” is incomplete: name the reference frame. A tilted orbit with a matching period is geosynchronous but would not remain fixed above one ground point.

Exam technique: Show the chosen physical model, centre-to-centre distances and units before substituting. These original questions use PhysicsUK mark guidance; linked OCR lessons concern the named source parts.

Try a changed context

Can a geostationary satellite be placed directly above a ground station at latitude 55° N?

Check the transfer answer

No. A geostationary orbit is equatorial, so its sub-satellite point is at 0° latitude. A station at 55° N may see a suitable satellite lower in its sky, but the satellite cannot remain directly overhead there.

Question 7 · Exam-style linearization and variable-field fall · 6 marks

An asteroid landing from a potential graph

Specification: 5.4.4(a), 5.4.4(b), 5.4.4(d), 1.1.3(d)(ii)

A spherical non-rotating asteroid has radius 500 m. Measurements of its gravitational potential are plotted against reciprocal centre distance, with a straight line through (0 m⁻¹, 0 J kg⁻¹) and (2.00 × 10⁻³ m⁻¹, −0.120 J kg⁻¹). The latter point is its surface. A probe is released from rest at r = 1500 m and falls radially to the surface. Ignore other bodies.

  1. Define gravitational potential and use the graph gradient to find the asteroid’s mass. [3]
  2. Calculate the impact speed without treating g as constant. [3]
Original asteroid potential versus reciprocal-radius measurements; exact coordinates also appear in the question.
Original asteroid potential versus reciprocal-radius measurements; exact coordinates also appear in the question. Open the larger diagram
Small hint

For Vg = −GM(1/r), the gradient is negative and its magnitude is GM. The potential drop supplies kinetic energy per unit mass.

Method hint

Find ΔV/Δ(1/r), divide its magnitude by G, then use ½v² = GM(1/R − 1/rstart).

Complete worked solution and marks

Answer: Gradient = −60.0 m³/s²; M = 9.00 × 10¹¹ kg. Potential falls from −0.0400 to −0.120 J/kg, giving impact speed 0.400 m/s.

  1. Gravitational potential is the work done by an external agent per unit mass in bringing a small test mass slowly from infinity to the point, with zero potential at infinity. In an attractive field this external work is negative because the agent restrains the fall.
  2. Gradient = (−0.120 − 0)/(2.00 × 10⁻³ − 0) = −60.0 J m kg⁻¹ = −60.0 m³ s⁻².
  3. Vg = −GM(1/r), so GM = 60.0 m³ s⁻².
    M = 60.0/G = 9.00 × 10¹¹ kg.
  4. Vstart = −60.0/1500 = −0.0400 J kg⁻¹; Vsurface = −0.120 J kg⁻¹.
  5. Conservation: ½v² = Vstart − Vsurface = 0.0800 J kg⁻¹.
    v = √0.160 = 0.400 m s⁻¹. Probe mass cancels.
  6. The fall spans a threefold radius change, so field strength changes by a factor of nine. Constant-g SUVAT across this interval is unsuitable.
The gradient of Vg against 1/r is −GM. The potential decrease supplies the probe’s kinetic-energy gain.
The gradient of Vg against 1/r is −GM. The potential decrease supplies the probe’s kinetic-energy gain. Open the larger diagram

Check: Surface escape speed is √(2GM/R) = 0.490 m/s. Falling from a finite distance gives a smaller speed than falling from rest at infinity.

Mark checklist · 6 marks

  • 1 mark — Defines gravitational potential as work done per unit mass from infinity to the point, with zero at infinity.
  • 1 mark — Calculates signed scaled gradient −60.0 m³/s² and identifies gradient = −GM.
  • 1 mark — Obtains M ≈ 9.00 × 10¹¹ kg.
  • 1 mark — Evaluates initial and final potentials or their difference correctly.
  • 1 mark — Equates kinetic-energy gain per mass to the potential decrease.
  • 1 mark — Obtains speed 0.400 m/s.

Common mistake: The horizontal axis is 1/r, not r. Subtract signed potentials in the correct order for the energy gain; do not take a square root of a negative kinetic energy.

Exam technique: Show the chosen physical model, centre-to-centre distances and units before substituting. These original questions use PhysicsUK mark guidance; linked OCR lessons concern the named source parts.

Try a changed context

The same probe has initial inward speed 0.300 m/s at r = 1500 m. What is its impact speed?

Check the transfer answer

½vfinal² = ½(0.300)² + 0.0800, so vfinal = 0.500 m/s. Kinetic energies add; speeds do not. It began with positive total specific energy and would not be gravitationally bound in the collision-free model.

Question 8 · Exam-style signed energy and supplied gradient relation · 6 marks

Read a potential curve for a moving probe

Specification: 5.4.4(b), 5.4.4(d)

A potential–radius curve outside an isolated planet is shown. The tabulated points also give its readings; r is measured from the centre and potential is zero at infinity. A 120 kg probe moves freely from A at rA = 2.00 × 10⁷ m to B at rB = 1.00 × 10⁷ m, with initial speed 2.00 × 10³ m/s. No thrust or drag acts. For the graph interpretation, you are given the relation signed outward field component gr = −dVg/dr.

  1. Find the change in the probe’s gravitational potential energy. [2]
  2. Use conservation of energy to find its speed at B. [2]
  3. Use the supplied relation to explain the field direction and where on the displayed curve its magnitude is largest. [2]
Coordinates on the original potential curve
r / 10⁷ mVg / MJ kg⁻¹
0.800−50.0
1.00 (B)−40.0
2.00 (A)−20.0
4.00−10.0
Original exterior potential curve. Read A and B with the signed MJ/kg scale; tabulated values are provided.
Original exterior potential curve. Read A and B with the signed MJ/kg scale; tabulated values are provided. Open the larger diagram
Small hint

The vertical axis is potential, in energy per unit mass. ΔEp = m(VB − VA).

Method hint

The potential decrease is 20.0 MJ/kg. Add that to the initial ½v² before finding final speed; use the slope sign for gr.

Complete worked solution and marks

Answer: ΔEp = −2.40 × 10⁹ J; kinetic-energy gain = +2.40 × 10⁹ J; speed at B = 6.63 × 10³ m/s. Positive Vg–r slope gives inward gr; the largest displayed field magnitude is at the smallest radius.

  1. ΔVg = VB − VA = −40.0 − (−20.0) = −20.0 MJ kg⁻¹.
    ΔEp = mΔVg = −2.40 × 10⁹ J.
  2. ½vB² = ½vA² + (VA − VB) = 2.00 × 10⁶ + 20.0 × 10⁶ = 22.0 × 10⁶ J kg⁻¹.
    vB = √(44.0 × 10⁶) = 6.63 × 10³ m s⁻¹.
  3. Vg increases as r increases, so dVg/dr is positive. The supplied relation makes gr negative: force/acceleration is inward. At the smallest displayed radius, the curve’s gradient magnitude is greatest, so the field magnitude is greatest.
  4. The curve approaches zero from below at large r. This is inverse-distance variation, not exponential decay. The displayed model applies outside the spherical planet; it is not extended through the interior.
Inward motion makes potential more negative. Potential-energy loss equals kinetic-energy gain during unpowered flight.
Inward motion makes potential more negative. Potential-energy loss equals kinetic-energy gain during unpowered flight. Open the larger diagram

Check: Initial kinetic energy is 2.40 × 10⁸ J; final is 2.64 × 10⁹ J. Their difference matches −ΔEp. A negative potential is not a negative kinetic energy.

Mark checklist · 6 marks

  • 1 mark — Finds signed ΔVg = −20.0 MJ/kg.
  • 1 mark — Multiplies by 120 kg to obtain signed ΔEp = −2.40 × 10⁹ J.
  • 1 mark — Adds initial kinetic energy per mass to the potential-energy loss per mass.
  • 1 mark — Obtains vB ≈ 6.63 × 10³ m/s.
  • 1 mark — Uses the positive gradient and supplied minus sign to identify inward field.
  • 1 mark — Identifies steepest slope and strongest field at smallest displayed radius.

Common mistake: A graph reading in MJ/kg becomes an energy only after multiplying by mass and 10⁶. Starting with ½vA² = 0 would ignore the supplied initial speed.

Exam technique: Show the chosen physical model, centre-to-centre distances and units before substituting. These original questions use PhysicsUK mark guidance; linked OCR lessons concern the named source parts.

Try a changed context

Reverse the outward move from B to A and let the probe arrive at A at rest. What minimum initial speed is needed at B, with no thrust during flight?

Check the transfer answer

½vB² = VA − VB = 20.0 × 10⁶ J/kg gives vB = 6.32 × 10³ m/s, directed radially outward. It spends all this kinetic energy reaching A, not escaping to infinity.

Question 9 · Exam-style force–distance area and work signs · 6 marks

Tow a cargo slowly through a changing field

Specification: 5.4.4(b), 5.4.4(c), 5.4.4(d)

A tug moves a 200 kg cargo radially outward, very slowly, from r1 = 8.00 × 10⁶ m to r2 = 1.60 × 10⁷ m around a spherical planet. Use GM = 4.00 × 10¹⁴ m³ s⁻². The graph shows the positive magnitude Fext = GMm/r² of the outward force needed to balance gravity. The speed change is negligible; there are no other losses.

  1. Calculate the initial force and identify what the shaded graph area represents. [2]
  2. Calculate external work and gravitational work over the move. [2]
  3. A student uses W = F(r1)(r2 − r1). Evaluate this approximation and explain the direction of its error. [2]
Positive outward balancing force versus centre radius. The selected area belongs to the specified outward move.
Positive outward balancing force versus centre radius. The selected area belongs to the specified outward move. Open the larger diagram
Small hint

The balancing force decreases with radius. Use the two endpoint potentials for exact work, not one force for the whole journey.

Method hint

Wext = ΔEp = GMm(1/r1 − 1/r2); Wgravity = −ΔEp for this slow move. Compare with the rectangle using the initial force.

Complete worked solution and marks

Answer: Fext(r1) = 1.25 × 10³ N; Wext = +5.00 × 10⁹ J; Wgravity = −5.00 × 10⁹ J. The initial-force rectangle gives 1.00 × 10¹⁰ J, twice the correct work.

  1. Fext(r1) = GMm/r1² = 1.25 × 10³ N; at r2 it is only 312.5 N.
  2. The area under the positive outward balancing-force curve, between r1 and r2, is positive external work for outward displacement. It equals the increase in gravitational potential energy because ΔEk ≈ 0.
  3. Wext = ΔEp = GMm(1/r1 − 1/r2) = +5.00 × 10⁹ J.
    Gravity is opposite to outward motion: Wgravity = −5.00 × 10⁹ J.
  4. Wrectangle = F(r1)(r2 − r1) = 1250(8.00 × 10⁶) = 1.00 × 10¹⁰ J.
  5. That rectangle stays above the decreasing curve, overestimating work by a factor of 2 (100%). FΔr is exact only for a constant force along the displacement; the local mgΔh approximation is unsuitable for doubling this radius.
The curve area is outward external work. An initial-force rectangle overestimates work because the force decreases.
The curve area is outward external work. An initial-force rectangle overestimates work because the force decreases. Open the larger diagram

Check: The tug and gravity nearly cancel at each point, so their works sum to approximately zero and the cargo’s kinetic energy stays almost constant. Positive potential-energy change is compatible with negative absolute potential energy.

Mark checklist · 6 marks

  • 1 mark — Obtains the initial balancing force 1250 N.
  • 1 mark — Identifies shaded area as external work/positive ΔEp for outward slow motion.
  • 1 mark — Calculates Wext = +5.00 × 10⁹ J from the endpoint potential energies.
  • 1 mark — Gives Wgravity = −5.00 × 10⁹ J.
  • 1 mark — Evaluates initial-force rectangle as 1.00 × 10¹⁰ J.
  • 1 mark — Explains overestimate using decreasing force/rectangle above curve; quantifies factor 2.

Common mistake: The plotted positive force is the external balancing force, not the signed inward gravitational force. The same positive shaded area cannot be labelled positive work by gravity for this outward move.

Exam technique: Show the chosen physical model, centre-to-centre distances and units before substituting. These original questions use PhysicsUK mark guidance; linked OCR lessons concern the named source parts.

Try a changed context

Move the cargo slowly back from r2 to r1. What work does the tug do, and what work does gravity do?

Check the transfer answer

Wtug = −5.00 × 10⁹ J and Wgravity = +5.00 × 10⁹ J. The tug still pulls outward while displacement is inward, so it removes energy. This ideal result does not imply a real propulsion system can recover all that work.

Question 10 · Exam-style vector superposition and negative potential · 7 marks

Where can two gravitational fields cancel?

Specification: 5.4.1(c), 5.4.2(b), 5.4.4(b)

Two fixed, spherical sources A and B have masses 9.00 × 10²⁴ kg and 1.00 × 10²⁴ kg. Their centres are d = 4.00 × 10⁸ m apart. Their radii are negligible compared with the distances considered. Let x be distance from A’s centre towards B; right is positive. Ignore all other bodies and rotation. This is a fixed-source model.

  1. Find the zero-field point between the sources. [3]
  2. Calculate total gravitational potential there, taking zero at infinity. [2]
  3. Explain why zero field does not mean zero potential, and state which way a test mass accelerates after a small displacement towards B along the line. [2]
Small hint

At the neutral point the field magnitudes are equal and opposite. The distances are x and d − x, not two independent radii.

Method hint

Solve MA/x² = MB/(d − x)², then add the two negative potentials. Move slightly right and compare how the two field magnitudes change.

Complete worked solution and marks

Answer: x = 3.00 × 10⁸ m from A, or 1.00 × 10⁸ m from B. Each field magnitude = 0.00667 N/kg; resultant = 0. Total potential = −2.668 × 10⁶ J/kg. A small rightward displacement accelerates the test mass towards B.

  1. gA = −GMA/x²; gB = +GMB/(d − x)².
    Zero resultant requires MA/x² = MB/(d − x)².
  2. x/(d − x) = √(MA/MB) = 3.
    x = 3(d − x), so x = 3d/4 = 3.00 × 10⁸ m.
  3. Vtotal = −G[MA/x + MB/(d − x)] = −2.668 × 10⁶ J kg⁻¹.
    Each field magnitude is 0.00667 N kg⁻¹, but the directions are opposite.
  4. Fields are vectors and cancel at this point. Potential is a scalar: both contributions are negative and add, so it remains negative.
  5. Displacing the mass slightly right increases B’s field magnitude and decreases A’s. The resultant is rightwards, further from the neutral point: it is unstable along this line in the fixed-source model. This is not an orbital Lagrange-point calculation.
Fields cancel as vectors, while the two negative scalar potentials add. This is a fixed-source model.
Fields cancel as vectors, while the two negative scalar potentials add. This is a fixed-source model. Open the larger diagram

Check: The neutral point lies closer to the smaller mass, which must be nearer to match the larger mass’s field. Using the mass ratio 9 directly as a distance ratio would fail the inverse-square equality.

Mark checklist · 7 marks

  • 1 mark — Sets equal and opposite field magnitudes using x and d − x.
  • 1 mark — Takes the square root of the mass ratio to obtain distance ratio 3.
  • 1 mark — Finds x = 3.00 × 10⁸ m from A.
  • 1 mark — Adds both signed point-mass potentials.
  • 1 mark — Obtains Vtotal = −2.668 × 10⁶ J/kg.
  • 1 mark — Explains vector cancellation versus scalar addition.
  • 1 mark — Identifies acceleration towards B after a small displacement towards B and justifies it.

Common mistake: Zero gravitational force at one point does not make the entire region field-free. The fixed-source equilibrium discussed here must not be called a stable parking orbit.

Exam technique: Show the chosen physical model, centre-to-centre distances and units before substituting. These original questions use PhysicsUK mark guidance; linked OCR lessons concern the named source parts.

Try a changed context

Replace B with mass 4.00 × 10²⁴ kg, keeping A and d unchanged. Where is the new zero-field point?

Check the transfer answer

x/(d − x) = √(9/4) = 3/2, so x = 0.600d = 2.40 × 10⁸ m from A. Increasing B’s mass moves the neutral point away from B, towards A.

Question 11 · Exam-style Kepler laws and changing kinetic energy · 8 marks

An elliptical probe orbit around a star

Specification: 5.4.3(a), 5.4.3(d), 5.4.4(b), 5.4.4(d)

A 300 kg probe follows an unpowered elliptical orbit around a star with GM = 2.00 × 10²⁰ m³ s⁻². Its closest distance is rp = 4.00 × 10¹⁰ m and its furthest distance is ra = 1.20 × 10¹¹ m. Other bodies have negligible effects. The orbital velocities at these two turning points are perpendicular to the star–probe line. For applying Kepler’s third law to this ellipse, use a = (rp + ra)/2, the semi-major axis, in place of circular radius. A negligible-mass reference planet around this same star has a0 = 1.00 × 10¹¹ m and measured T0 = 1.40 × 10⁷ s (rounded).

  1. Apply Kepler’s first and second laws to identify the star’s position, the fastest point, and the ratio vp/va. [3]
  2. Find a and the probe’s period from the reference orbit. [2]
  3. Calculate the signed kinetic-energy change from the furthest point to the closest point. [3]
Original elliptical probe orbit. Geometry follows the stated 1:3 turning-point radius ratio; source size is schematic.
Original elliptical probe orbit. Geometry follows the stated 1:3 turning-point radius ratio; source size is schematic. Open the larger diagram
Small hint

The star is at a focus, not at the ellipse centre. Equal areas per equal times connect radius and speed at the perpendicular turning points.

Method hint

Use ½rpvpΔt = ½ravaΔt for the endpoint speed ratio; T/T0 = (a/a0)^(3/2); ΔEk = −GMm(1/ra − 1/rp).

Complete worked solution and marks

Answer: Star at one focus; fastest at closest approach; vp/va = 3.00. a = 8.00 × 10¹⁰ m; T = 1.00 × 10⁷ s (116 days). From far to near: ΔEp = −1.00 × 10¹² J and ΔEk = +1.00 × 10¹² J.

  1. Kepler’s first law places the star at one focus of the ellipse. The joining line sweeps equal areas in equal times. Near the star, the smaller radius requires a larger distance along the orbit in the same short time, so speed is greatest at closest approach.
  2. At the two turning points, swept area in a short Δt is ½rvΔt.
    rpvp = rava, so vp/va = ra/rp = 3.00.
  3. a = (4.00 × 10¹⁰ + 1.20 × 10¹¹)/2 = 8.00 × 10¹⁰ m.
    T = T0(a/a0)^(3/2) = 1.40 × 10⁷(0.800)^(3/2) = 1.00 × 10⁷ s, about 116 days.
  4. ΔEp = Ep,near − Ep,far = −GMm(1/rp − 1/ra) = −1.00 × 10¹² J.
  5. No thrust or drag: Ek + Ep is constant, so ΔEk = −ΔEp = +1.00 × 10¹² J.
  6. Do not use v = √(GM/r) at each point of an elliptical orbit: that is the circular-orbit speed relation. This solution uses Kepler’s area law and energy conservation instead.
Apply the focus and equal-area laws to the named probe. Use semi-major axis for the period comparison.
Apply the focus and equal-area laws to the named probe. Use semi-major axis for the period comparison. Open the larger diagram

Check: The orbit period is between those of circular orbits at rp and ra. Its total energy is conserved while both kinetic and potential energy change. Rounded reference data explain tiny differences from the direct GM formula.

Mark checklist · 8 marks

  • 1 mark — Places the star at one focus.
  • 1 mark — Uses equal areas in equal times to locate maximum speed at closest approach.
  • 1 mark — Uses perpendicular endpoint geometry to obtain vp/va = 3.00.
  • 1 mark — Calculates semi-major axis a = 8.00 × 10¹⁰ m.
  • 1 mark — Uses the same-star Kepler ratio to obtain T ≈ 1.00 × 10⁷ s.
  • 1 mark — Evaluates endpoint potential energies or GMm(1/rp − 1/ra).
  • 1 mark — Obtains signed ΔEp = −1.00 × 10¹² J.
  • 1 mark — Applies conservation to obtain ΔEk = +1.00 × 10¹² J.

Common mistake: A focus is not the centre. Do not describe all three Kepler laws when a particular law is requested: apply that law to the named probe. Gravitational acceleration need not be perpendicular to velocity except at the turning points.

Exam technique: Show the chosen physical model, centre-to-centre distances and units before substituting. These original questions use PhysicsUK mark guidance; linked OCR lessons concern the named source parts.

Try a changed context

Compare acceleration magnitudes at closest and furthest approach. Is their ratio the same as the speed ratio?

Check the transfer answer

g ∝ 1/r², so ap/aa = (ra/rp)² = 9.00. The endpoint speed ratio is 3.00 from Kepler’s second law, so the two ratios differ.

Question 12 · Exam-style complete energy budget and evidence-based evaluation · 8 marks

Evaluate an aircraft-assisted launch claim

Specification: 5.4.3(b), 5.4.4(b), 5.4.4(d), 3.3.2(a)

In a non-rotating spherical-planet model, a 1.00 kg satellite starts at rest on the surface and must end in a circular orbit of radius 7.20 × 10⁶ m. The planet has GM = 4.00 × 10¹⁴ m³ s⁻² and surface radius R = 6.40 × 10⁶ m. A proposal first carries the satellite to 12.0 km altitude at 250 m/s in the planet-centred frame. It claims this supplies at least 1% of the satellite’s minimum required mechanical-energy gain. Neglect air resistance for the ideal energy budget. For the aircraft’s small altitude change you may use g0 = 9.77 N/kg. This model deliberately ignores planetary rotation in both starting cases.

  1. Derive the circular-orbit relation Ek = GMm/(2r). [2]
  2. Calculate the minimum mechanical-energy gain from rest on the surface to the final orbit, including both Ep and Ek. [3]
  3. Use calculations to evaluate the 1% claim and give one physical limitation of predicting real launch fuel from this ideal budget. [3]
Small hint

Arrival at orbital altitude is not enough: the satellite must have the tangential speed required for a circular orbit.

Method hint

Final Etotal = −GMm/(2r); initial Etotal = −GMm/R. For the aircraft credit, add mg0h and ½mv², then compare with the full required gain.

Complete worked solution and marks

Answer: Minimum gain = 34.7 MJ. Aircraft supplies about 0.148 MJ (0.428%), so the 1% claim fails. Fuel requirements also depend on propulsion efficiency, drag, gravity losses and the trajectory.

  1. GMm/r² = mv²/r gives v² = GM/r.
    Ek = ½mv² = GMm/(2r).
  2. Initial Etotal = Ep,surface = −GMm/R = −62.5 MJ.
    Final Ep = −55.6 MJ; final Ek = +27.8 MJ; final Etotal = −27.8 MJ.
  3. ΔErequired = Efinal − Einitial = +34.7 MJ.
    Equivalently, ΔEp = +6.94 MJ and ΔEk = +27.8 MJ. Add them.
  4. Aircraft credit ≈ mg0h + ½mv² = 1.00(9.77)(12 000) + ½(1.00)(250)² = 1.485 × 10⁵ J = 0.148 MJ.
  5. Fraction = 0.14849/34.7222 × 100% = 0.428%, below 1%. In this ideal model the remaining required mechanical gain is about 34.6 MJ.
  6. The ideal endpoint budget is not a fuel-energy prediction. For example, finite-time powered flight has gravity losses and drag; real engines have efficiency limits and expend energy on propellant. These change the fuel required. The altitude and speed credit is small but does not rule out operational advantages of an aircraft launch.
Include the final circular-orbit kinetic energy as well as the gravitational potential-energy increase.
Include the final circular-orbit kinetic energy as well as the gravitational potential-energy increase. Open the larger diagram

Check: The change is positive although both initial and final total energies are negative. Exact endpoint potential for 12 km gives an aircraft credit only about 0.00027 MJ smaller, which cannot rescue the 1% claim.

Mark checklist · 8 marks

  • 1 mark — Equates gravitational and centripetal forces.
  • 1 mark — Derives Ek = GMm/(2r).
  • 1 mark — Finds initial energy −62.5 MJ and final potential −55.6 MJ.
  • 1 mark — Includes final orbital kinetic energy +27.8 MJ.
  • 1 mark — Finds total required gain ≈ 34.7 MJ.
  • 1 mark — Adds aircraft altitude and kinetic credits to obtain ≈ 0.148 MJ.
  • 1 mark — Quantifies ≈ 0.428% and rejects the stated 1% energy claim.
  • 1 mark — Gives a physical limitation connecting the ideal endpoint budget to actual fuel/flight.

Common mistake: Using only ΔEp misses most of the launch energy. Do not mix ground-relative aircraft speed with planet-centred speed or introduce rotation into only one side of the stated non-rotating comparison.

Exam technique: Show the chosen physical model, centre-to-centre distances and units before substituting. These original questions use PhysicsUK mark guidance; linked OCR lessons concern the named source parts.

Try a changed context

Suppose the aircraft speed doubles at the same altitude. Would the 1% claim become correct?

Check the transfer answer

Aircraft KE quadruples to 0.125 MJ, while altitude credit remains 0.117 MJ. Total credit ≈ 0.242 MJ, or 0.698% of 34.7 MJ: still below 1%.

Question 13 · Exam-style orbital energy accounting · 7 marks

Raising an orbit: slower speed, greater total energy

Specification: 5.4.3(b), 5.4.4(b), 5.4.4(d), 5.4.4(e)

A 600 kg satellite begins in a circular orbit of radius 8.00 × 10⁶ m. Thrusters transfer it to a final circular orbit of radius 1.60 × 10⁷ m around a planet with GM = 4.00 × 10¹⁴ m³ s⁻². Ignore mass change and losses for this endpoint comparison. The intermediate transfer path is not assumed circular. For either circular endpoint, use Ek = GMm/(2r) and Ep = −GMm/r.

  1. Calculate initial and final orbital speed. [2]
  2. Calculate the changes in kinetic, gravitational potential and total energy. [3]
  3. Explain why positive work is needed even though the final circular speed is lower. [2]
Small hint

“Slower” only tells you about kinetic energy. Gravitational potential energy also changes.

Method hint

Make an initial/final table of Ek, Ep and Etotal. Subtract final minus initial for each; compare the magnitudes of ΔEk and ΔEp.

Complete worked solution and marks

Answer: vi = 7.07 km/s; vf = 5.00 km/s. ΔEk = −7.50 GJ; ΔEp = +15.0 GJ; ΔEtotal = +7.50 GJ. The potential increase is twice the kinetic decrease, so net energy must be supplied.

  1. vi = √(GM/ri) = 7.07 × 10³ m s⁻¹; vf = √(GM/rf) = 5.00 × 10³ m s⁻¹.
  2. Circular endpoint energies
    EndpointEk / GJEp / GJEtotal / GJ
    Initial+15.0−30.0−15.0
    Final+7.50−15.0−7.50
  3. ΔEk = −7.50 GJ;
    ΔEp = +15.0 GJ;
    ΔEtotal = +7.50 GJ.
  4. Gravitational potential becomes less negative as the satellite moves outwards. Its increase is larger than the kinetic-energy decrease, so the satellite’s total energy rises. In the ideal fixed-mass model, thrusters must supply net positive mechanical work.
  5. A brief prograde burn initially increases speed and changes the path; later speed varies along the transfer. The lower final circular speed does not imply that the manoeuvre begins by simply braking into a higher circular orbit. No transfer-burn timing or fuel calculation is requested.
A lower final circular speed can accompany a higher total energy. Compare both endpoint energy stores.
A lower final circular speed can accompany a higher total energy. Compare both endpoint energy stores. Open the larger diagram

Check: At each circular endpoint Ek = −Ep/2 and Etotal = Ep/2. Doubling r halves the magnitudes of all three energies but reduces speed by √2.

Mark checklist · 7 marks

  • 1 mark — Obtains vi ≈ 7.07 km/s.
  • 1 mark — Obtains vf = 5.00 km/s.
  • 1 mark — Obtains signed ΔEk = −7.50 GJ.
  • 1 mark — Obtains signed ΔEp = +15.0 GJ.
  • 1 mark — Adds them to obtain ΔEtotal = +7.50 GJ.
  • 1 mark — Explains potential-energy increase exceeds the kinetic decrease, so work is positive.
  • 1 mark — Distinguishes the two circular endpoints from the powered intermediate transfer path.

Common mistake: Do not assume total mechanical energy is conserved through firing thrusters. Conservation applies to unpowered gravity-only motion; here the satellite gains net mechanical energy.

Exam technique: Show the chosen physical model, centre-to-centre distances and units before substituting. These original questions use PhysicsUK mark guidance; linked OCR lessons concern the named source parts.

Try a changed context

Compare two otherwise identical satellites already in these two circular orbits. Which one needs less extra energy to just escape to infinity, and how much?

Check the transfer answer

For just escape Efinal = 0, so extra energy is −Etotal. The inner satellite needs 15.0 GJ; the outer one needs 7.50 GJ. The outer orbit is less tightly bound.

Question 14 · Exam-style energy derivation and gas application · 7 marks

Escape speed and a planet’s atmosphere

Specification: 5.4.4(a), 5.4.4(d), 5.4.4(e), 5.1.4(f), 5.1.4(h)

An isolated non-rotating spherical planet has GM = 7.20 × 10¹² m³ s⁻² and radius R = 1.20 × 10⁶ m. Neglect atmospheric drag for a single-particle escape calculation. Its upper-atmosphere model is at 300 K. Particle masses are 6.64 × 10⁻²⁷ kg for helium and 4.65 × 10⁻²⁶ kg for nitrogen. Use k = 1.38 × 10⁻²³ J/K and the supplied rms relation crms = √(3kT/m). This comparison is qualitative evidence about thermal escape, not a complete atmosphere model.

  1. Derive the minimum escape-speed expression from energy and calculate it at the surface. [3]
  2. Calculate rms speed for each gas and use the results to explain which is more vulnerable to thermal escape. Explain why rms speed alone cannot prove the atmosphere is completely retained. [3]
  3. An unpowered probe at r = 3.00 × 10⁶ m is launched radially outward at 2.50 × 10³ m/s. Decide whether it escapes. [1]
Small hint

Just escape means zero final speed and zero potential energy at infinity. A gas has a distribution of speeds, not one common speed.

Method hint

Set ½mvesc² − GMm/R = 0. Compare each rms speed with vesc; then use vesc(r) at the probe’s launch radius.

Complete worked solution and marks

Answer: Surface vesc = 3.46 km/s. Helium crms = 1.37 km/s; nitrogen crms = 0.517 km/s. Helium is more vulnerable, but the high-speed tail matters. At r = 3.00 × 10⁶ m, vesc = 2.19 km/s, so the 2.50 km/s outward probe escapes.

  1. For just escape, Etotal at infinity = 0. Energy conservation gives ½mvesc² − GMm/R = 0.
    vesc = √(2GM/R); launched mass cancels.
  2. vesc(R) = √[2(7.20 × 10¹²)/(1.20 × 10⁶)] = 3.46 × 10³ m s⁻¹.
  3. crms,He = √[3k(300)/(6.64 × 10⁻²⁷)] = 1.37 × 10³ m s⁻¹.
    crms,N₂ = √[3k(300)/(4.65 × 10⁻²⁶)] = 517 m s⁻¹.
  4. At the same temperature, lighter helium particles have higher typical speeds and a larger high-speed tail above the escape threshold, so helium is more vulnerable to thermal escape. Both rms values are below vesc, but rms is not a maximum: some particles can be faster. Escape also depends on direction, collisions, altitude and heating. These estimates cannot establish complete long-term retention.
  5. At the probe launch point, vesc = √[2GM/(3.00 × 10⁶)] = 2.19 × 10³ m s⁻¹.
    2.50 × 10³ > vesc, so the outward probe escapes in the stated isolated model.
Rms speed is not the maximum gas-particle speed. These bars compare characteristic speeds, not escape fractions.
Rms speed is not the maximum gas-particle speed. These bars compare characteristic speeds, not escape fractions. Open the larger diagram

Check: Surface g = GM/R² = 5.00 N/kg, so √(2gR) reproduces 3.46 km/s. Mass independence applies to a probe’s required escape speed; gas-particle mass affects the thermal speed, which is a different calculation.

Mark checklist · 7 marks

  • 1 mark — Uses zero potential and minimum zero kinetic energy at infinity.
  • 1 mark — Equates initial kinetic and binding-energy magnitude to derive vesc = √(2GM/R).
  • 1 mark — Obtains surface vesc ≈ 3.46 km/s.
  • 1 mark — Calculates both gas rms speeds ≈ 1.37 km/s and 517 m/s.
  • 1 mark — Links higher helium speed at equal T to greater vulnerability to escape.
  • 1 mark — Explains rms is not a maximum and a speed distribution/high-speed tail prevents a complete-retention conclusion.
  • 1 mark — Uses local vesc ≈ 2.19 km/s to conclude the outward 2.50 km/s probe escapes.

Common mistake: A lower gas mass does not change the gravitational escape threshold at the same point. It changes the distribution of particle speeds at a given temperature. Escape speed also depends on launch radius; it is not one fixed number throughout space.

Exam technique: Show the chosen physical model, centre-to-centre distances and units before substituting. These original questions use PhysicsUK mark guidance; linked OCR lessons concern the named source parts.

Try a changed context

What is the escaping probe’s speed at infinity in the same model?

Check the transfer answer

½v∞² = ½vlaunch² − GM/r gives v∞ = √[(2500)² − 2(7.20 × 10¹²)/(3.00 × 10⁶)] = 1.20 × 10³ m/s. Its speed falls as it climbs, remaining positive at infinity.

Use the simulation to check your predictions

In the two-mass sandbox set the left mass to 9.0 and the right mass to 1.0 (each in 10²⁴ kg). The centre separation is fixed at 4.00 × 10⁸ m. Predict the zero-field distance 3.00 × 10⁸ m from the left centre and negative total potential −2.668 × 10⁶ J/kg. The position slider maps an allowed track from rleft = 1.50 × 10⁷ m to 3.85 × 10⁸ m, so choose about 77.0%, not 75%, to get near the neutral point. Expect a small rounding residual rather than an exact zero at a discrete slider step. Move either side and compare the signed resultant field and acceleration prediction; potentials stay negative. This model holds the sources fixed and predicts direction; it does not integrate a moving probe or orbit. In the work-area investigation choose planet mass M = 6.0 (in 10²⁴ kg), cargo mass m = 1 (in 10³ kg), radius markers 1.00 and 2.00 (in R⊕, with R⊕ = 6.37 × 10⁶ m). Predict positive outward external work 3.14 × 10¹⁰ J and equal negative gravitational work. Double cargo mass to 2: work doubles to 6.28 × 10¹⁰ J. Its curve auto-scales vertically, so use numerical readings to compare different masses. The interval readout orders markers from low to high radius; swapping them does not itself represent inward travel. Reverse-motion work signs must be interpreted separately.

Open the two-mass field model in the notes · Try the force–distance work investigation

Coverage and exam guidance

OCR A A-level H556 5.4.1–5.4.4: point/spherical source models, field lines and g = F/m, Newton’s law and inverse-square fields, uniform near-surface approximation, all three Kepler laws, gravity as the centripetal force, period derivation and exoplanet/data applications, geostationary conditions and mission choice, potential with zero at infinity, signed energy changes, force–distance work and escape. The atmosphere task uses supporting 5.1.4 gas-speed ideas. The potential-gradient relation is supplied for interpretation; calculus is not required recall. Elliptical third-law use is supplied in terms of semi-major axis, not instantaneous radius. Two-mass equilibrium uses fixed sources, not rotating-frame Lagrange points. Orbital transfers compare endpoints; no Hohmann-burn, rocket equation, relativity or interior-sphere formula is required. These gravitational-field outcomes are A-level content, not OCR AS H156 content.

All fourteen questions, numerical data, diagrams, transfer tasks and mark checklists are original PhysicsUK resources. Fifteen linked lessons paraphrase checked OCR A H556 questions, mark schemes and examiner reports from June 2018, November 2020, June 2022, June 2023, June 2024 and June 2025. Some applications, including our laboratory spheres, uncertainty data, orbit transfer and gas comparison, are original specification-led extensions; no report is claimed to discuss those exact new tasks. The displayed marks are PhysicsUK guidance, not copied OCR allocations. No topic-frequency analysis or future-paper prediction is implied.

OCR A A-level Physics H556 specification, version 3.0 (2026), pp. 36–37

Original questions and solutions by PhysicsUK. Review date: 9 October 2026.