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AP® Physics 1: Algebra-Based · Unit 3 · Topic 3.3

Potential Energy: Revision Notes (Physics 1 3.3)

One-page recap of potential energy for the algebra-based course: which systems have it, choosing the zero, spring and gravitational formulas, summing pairs, and the mistakes that cost marks.

Short on time? This page is the recap. For explanations, graphs and worked examples, use the full study guide. This is the algebra-based course: no calculus is needed.

Recap

  • Potential energy (U) is energy stored in the arrangement of a system whose objects interact through conservative forces (gravity, ideal springs).
  • A single object cannot have potential energy. Name the pair: ball–Earth, block–spring.
  • A conservative force does the same work on any path between two points. Friction is not conservative, so there is no friction potential energy.
  • U is a scalar fixed by the positions of the objects in the system.
  • The zero of U is your choice. Pick whatever makes the problem simplest and state it.
  • For three or more objects, add the potential energy of every pair.

Key relationships

Relationship Symbols and units Use it to
U_s = ½kΔx² k in N/m, Δx in m from the relaxed length find spring energy (never negative)
U_g = −Gm₁m₂ / r r centre to centre in m; zero at infinity find gravitational energy of two spheres (always negative)
ΔU_g = mgΔy Δy in m, + for upward; g = 9.8 N/kg find changes near a planet’s surface
ΔU = −W_conservative J link to work by a force inside the system
U_total = sum over pairs J three or more interacting objects

Factors of change: Δx × 2 → U_s × 4. r × 2 → U_g × ½ (less negative, so larger). Δy × 2 → ΔU_g × 2.

Assumptions behind the numbers

  • The spring is ideal: it obeys Hooke’s law and has negligible mass.
  • Planets, moons and stars are treated as spherical, so r is measured between centres.
  • ΔU_g = mgΔy assumes a constant field. It is accurate only when Δy is much smaller than the planet’s radius.
  • g = 9.8 N/kg at Earth’s surface. The course framework says exam questions use 10 N/kg (10 m/s²), and 9.8 is also accepted.

Mistakes to avoid

  1. Giving potential energy to one object. Write “the ball–Earth system”.
  2. Forgetting to square Δx, or using total spring length instead of the change from relaxed length.
  3. Leaving Δx in centimetres. Convert to metres first.
  4. Measuring r from the surface in U_g = −Gm₁m₂/r.
  5. Calling U_g = −5 J “less” than U_g = −10 J. −5 J is the larger value.
  6. Using mgΔy for satellites. Use the general form when Δy is comparable with the radius.
  7. Missing a pair in a three-object system: A, B and C have three pairs.

Quick self-check

  1. A spring with k = 400 N/m is stretched 5.0 cm. How much energy does it store? (0.50 J)
  2. A 2.0 kg box is lifted 3.0 m. What is ΔU_g for the box–Earth system? (+59 J)
  3. Two asteroids move to three times their original separation. What happens to U_g? (It becomes one third of the original value: still negative, but larger.)
  4. Can the ball–Earth system have negative potential energy near the ground? (Yes, if the ball is below the chosen zero.)

Next: practice questions.

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