IB Physics HL Topic 4 — Force Fields Paper 1 & 2 No work done along one ~15 min read

Gravitational Equipotentials

A walking map has contour lines. Follow one round a hillside and you never climb, never descend, never break a sweat. Cut straight across them and you are gasping within minutes. Gravitational fields have contour lines too. They are called equipotentials, and the same rule holds with beautiful exactness: travel along one and gravity charges you nothing at all.

📘 What you need to know

What an equipotential is

Pick a value of potential — say −3.0 × 10⁷ J kg−1. Now find every single point in space where the potential has exactly that value, and join them up. That’s an equipotential.

Equipotential — definition a line (2D) or surface (3D) joining points
that all have the same gravitational potential

Around a lone planet the answer is obvious once you say it out loud. Potential depends only on r, through Vg = −GM/r. So “all the points with the same potential” means “all the points at the same distance from the centre” — a sphere. Drawn on paper, a circle.

Radial and uniform fields

Two standard pictures. Learn to draw both, with a ruler, in about twenty seconds.

Solid lines have arrows. Dashed lines never do. radial field concentric circles, further apart outwardsuniform field parallel and equally spaced
Dashed = equipotential, solid + arrowhead = field line. In both pictures they meet at exactly 90°, and in both the field points from high potential to low.
Why do the circles spread apart as you go out? Draw them at equal steps of potential — say every 1.0 × 107 J kg−1. Near the surface the potential is changing fast, so you only have to move a short way to drop by that step. Far out it changes lazily, so you must travel enormously further for the same drop. Crowded equipotentials mean a steep gradient, and a steep gradient means a strong field. They are a contour map, and the contours bunch up where the hill is steep.

No work done along an equipotential

This is the result the whole page exists for. Move a mass from one point to another on the same equipotential and the potential has not changed — so ΔV = 0, and the work done is zero.

Work done moving a mass W = mΔVg along an equipotential, ΔVg = 0, so W = 0  •  work is only done moving between equipotentials

It does not matter how long the journey is, or how winding. A satellite in a perfectly circular orbit is sliding around a single equipotential the whole way, which is precisely why it needs no engine to keep going.

Around a contour: free. Across contours: you pay. A B CA to B: along an equipotential ΔV = 0, so W = 0 B to C: across the gap W = mΔV a circular orbit rides a single equipotential — which is why it needs no engine
The green journey is free however far it winds. The orange one costs mΔV, and only the endpoints matter — not the route taken.

Why must they be perpendicular?

Not a coincidence, and not a drawing convention. It is forced on us by the last result. Suppose an equipotential met a field line at some angle other than 90°.

Anything other than 90° breaks the rule not perpendicular g component along ita force acts along the line — so work would be done. Impossible. perpendicular g no component along the line — so no work is done. Allowed.
The argument in one line: no work along an equipotential means no force along it, which means the field must be at right angles to it.
Follow that logic once and you will never forget it. If the field had any component along the equipotential, that component would push a mass sideways and do work on it — but moving along an equipotential is defined to cost nothing. The only way to have a force and yet do no work is for the force to be at right angles to the motion. So perpendicular it is. The same reasoning, incidentally, is why the tension in a string does no work on a mass swinging in a circle.
Field linesEquipotentials
Drawn asSolid lines with arrowsDashed lines, no arrows
ShowDirection of the force on a massPoints of equal potential
Vector or scalar?Vector quantity, gScalar quantity, Vg
Radial fieldStraight, pointing at the centreConcentric circles, spreading out
Uniform fieldParallel, equally spaced, downwardsHorizontal, parallel, equally spaced
Crowded together meansStrong fieldStrong field (steep gradient)
Angle between themAlways 90°
Same potential
everywhere on it
so ΔV = 0
along it
No work done
W = mΔV = 0
so no force
component along it
Field must be
perpendicular

🗺️ Drawing equipotentials for full marks

  1. Dashed or dotted lines only. Solid lines are field lines, and the examiner will read them as such.
  2. No arrowheads. Potential is a scalar; there is nothing for an arrow to point at.
  3. Radial field: concentric circles about the centre, with the gaps growing as you move out.
  4. Uniform field: straight, horizontal, equally spaced. Use a ruler.
  5. Check the angle. Every crossing with a field line must be a clean 90°.
WE 1

A satellite of mass 1200 kg moves in a circular orbit around a planet. (a) State the work done by the gravitational force during one complete orbit. (b) The satellite is then raised from an equipotential where Vg = −4.0 × 10⁷ J kg⁻¹ to one where Vg = −2.5 × 10⁷ J kg⁻¹. Calculate the work done.

(a) one complete orbit A circular orbit lies entirely on one equipotential, so ΔV = 0. W = 0 J (b) Step 1 — find the change in potential ΔV = (−2.5 × 10⁷) − (−4.0 × 10⁷) = +1.5 × 10⁷ J kg⁻¹ Step 2 — multiply by the mass W = mΔV = 1200 × (1.5 × 10⁷) W = 1.8 × 10¹⁰ J The potential went up (less negative), so ΔV is positive and work had to be done on the satellite. If you got a negative answer, you subtracted the wrong way round.
WE 2

For a planet with GM = 4.0 × 10¹⁴ N m² kg⁻¹, equipotentials are drawn at −4.0, −3.0, −2.0 and −1.0 (× 10⁷ J kg⁻¹). Calculate the radius of each, and use your answers to explain why equipotentials spread out with distance.

Step 1 — rearrange the potential equation V = −GM/r  →  r = GM / |V| Step 2 — work through the four values r = 4.0×10¹⁴ / 4.0×10⁷ = 1.0 × 10⁷ m r = 4.0×10¹⁴ / 3.0×10⁷ = 1.3 × 10⁷ m r = 4.0×10¹⁴ / 2.0×10⁷ = 2.0 × 10⁷ m r = 4.0×10¹⁴ / 1.0×10⁷ = 4.0 × 10⁷ m Step 3 — look at the gaps 3.3 × 10⁶  then  6.7 × 10⁶  then  2.0 × 10⁷ m the gaps grow rapidly Equal steps of potential need ever larger steps of distance, because the field out there is weak. Six times further apart by the last step. Since g = −ΔV/Δr, a bigger Δr for the same ΔV simply is a smaller g. The picture and the equation agree.
WE 3

Explain why gravitational equipotential surfaces must always be perpendicular to gravitational field lines.

Step 1 — state the defining property All points on an equipotential have the same potential, so ΔV = 0 between any two of them. Step 2 — apply the work equation W = mΔV = 0, so no work is done moving a mass along the surface. Step 3 — the contradiction If the field had a component along the surface, that force would do work on a mass moving along it. Step 4 — conclude So the field can have no component along the surface. the field must be at 90° to the equipotential Four sentences, four marks. The exam wants the logic chain, not the phrase “because they just are”.

💡 Top tips

⚠ Common mistakes

Quick recap: Equipotentials join points of equal potential. They are drawn dashed, without arrows, and are always perpendicular to the field lines — because no work is done along them, so the field can have no component along them. In a radial field they are concentric circles that spread apart with distance; in a uniform field they are parallel and equally spaced. Moving along one: W = 0. Moving between them: W = mΔV, and only the endpoints matter.
We have now mapped gravity every way there is: as a force, as a field, as a potential, and as a contour map. Time to point all of it at the sky. Planets do not wander at random — they obey three precise rules, worked out by Kepler from naked-eye observations decades before anyone knew why. Next page: Kepler’s Laws of Planetary Motion.

Equipotentials and field lines getting tangled?

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