Inverse-square gravitation and near-Earth field

Key idea: Newton’s inverse-square law describes the gravitational interaction at any separation. Constant g is a useful near-Earth approximation, not a universal rule.

  • GCE A-Level H1 Physics 2027

H1 Physics 8867 · Lesson 2 of 3

Check your understanding

By the end of this lesson, you should be able to

  • Use Newton’s law of gravitation for two masses.
  • Relate gravitational field strength to free-fall acceleration.
  • Compare field strengths at different distances using the inverse-square dependence.

Learn the idea

Big question: When is constant g a safe approximation, and when must distance from a planet's centre be kept?

Apply the inverse-square interaction

Point masses, and spherically symmetric bodies viewed from outside, attract with F = Gm1m2/r². The separation r is centre to centre, not height above a surface.

The forces on the two masses are equal and opposite even when their masses differ. Their accelerations differ because a = F/m.

Check your understanding: Earth pulls an astronaut more strongly than the astronaut pulls Earth. True or false?

False. The forces are equal; Earth's much larger mass gives it a much smaller acceleration.

Turn force per mass into field strength

Gravitational field strength g = F/m gives g = GM/r² around a spherical mass M. A freely falling small body has acceleration equal to local g if other forces are negligible.

Near Earth's surface, small laboratory height changes barely alter r, so constant g is useful. Across planetary distances, the inverse-square variation is essential.

Check your understanding: At height R above a planet of radius R, what fraction of surface g remains?

The distance from the centre is 2R, so g is one quarter of its surface value.

Radial and approximately uniform gravitational fieldsA spherical mass has radial field lines pointing inward and concentric equipotential surfaces. A small region near a large spherical surface is represented by parallel downward field lines and horizontal equipotentials.Radial fieldMdashed circles: equipotentialsNear-surface modelgparallel lines: approximately constant g
Scroll diagram horizontally to read all labels.
Field lines point in the force direction on a small test mass and cross equipotentials at right angles. Near a planet's surface, a small region can be approximated as uniform.

Key ideas

  • Measure r from the centre of a spherical body.
  • Gravitational force is always attractive.
  • Doubling r reduces F and g to one quarter, not one half.

Relationships to know

  • F = Gm₁m₂/r²
  • g = F/m = GM/r²
  • near Earth, free-fall acceleration ≈ g

Follow the reasoning

Worked example

Find a planet's mass from surface field

Question: A spherical moon has radius 1.74 × 10⁶ m and surface gravitational field strength 1.62 N kg⁻¹. Find its mass. Use G = 6.67 × 10⁻¹¹ N m² kg⁻².

  1. Step 1: Choose the field equation

    Why: Surface field uses centre distance equal to the moon's radius.

    Working: g = GM/R², so M = gR²/G.

  2. Step 2: Substitute with the squared radius

    Why: The inverse-square relationship is a common source of power-of-ten mistakes.

    Working: M = 1.62(1.74 × 10⁶)²/(6.67 × 10⁻¹¹).

  3. Step 3: Calculate and check units

    Why: N kg⁻¹, m² and G combine to kilograms.

    Working: M = 7.35 × 10²² kg.

Answer: The moon's mass is approximately 7.35 × 10²² kg.

Check: Substitution back into GM/R² returns about 1.62 N kg⁻¹.

Now try it with support

Practise with support

Two 5.0 kg masses are 0.20 m apart centre to centre. Find their gravitational attraction using G = 6.67 × 10⁻¹¹ N m² kg⁻².

Hints

  1. Square the separation in metres.
  2. The force magnitudes on the two masses are equal.
View the guided answer

F = 6.67 × 10⁻¹¹(5.0)(5.0)/(0.20²) = 4.17 × 10⁻⁸ N, attractive.

Your turn

Practise independently

A moon orbits at three planetary radii from the centre. Express the local gravitational field strength as a fraction of the surface value.

Check your answer

At r = 3R, g/gₛ = R²/(3R)² = 1/9. The local field strength is one ninth of the surface value.

Common mistakes and exam guidance

Watch out for

  • Using height above the surface instead of distance from the planet’s centre.
  • Treating g as constant throughout space because it is nearly constant in a laboratory.

In an exam

  • A ratio method often cancels G and the planet mass cleanly.
  • State ‘centre-to-centre’ when defining r in Newton’s law.

Put the ideas together

Exam-style practice [6 marks]

A planet has surface field strength 12 N kg⁻¹ and radius R. Find the field strength at height 2R above its surface. A 5.0 kg probe is there: find the gravitational force and explain why using g = 12 N kg⁻¹ would be wrong.

Plan before you answer

  • Convert height above surface to centre distance.
  • Use a ratio to avoid needing G or planet mass.
  • Then use F = mg with the local field.
View the marking points and model answer

Marking points

  1. Uses centre distance 3R.
  2. Uses inverse-square ratio.
  3. Finds g = 12/9 = 1.33 N kg⁻¹.
  4. Finds force 6.67 N.
  5. States surface g is only a near-surface value.
  6. Explains the centre distance has changed substantially.

Model answer

At height 2R, the probe is 3R from the centre. Therefore g/g0 = R²/(3R)² = 1/9, so g = 12/9 = 1.33 N kg⁻¹. The force is 5.0(1.33) = 6.67 N towards the planet. Using 12 N kg⁻¹ would ignore the large change in centre-to-centre distance.

Finish from memory

Three-question recap

  1. State Newton's law of gravitation.

    Check

    F = Gm1m2/r², attractive along the line joining the masses.

  2. How is r measured for spherical bodies?

    Check

    Centre to centre.

  3. When does free-fall acceleration equal g?

    Check

    When gravity is the only significant force.

Try this next

Set gravitational force equal to the required centripetal force for a circular orbit.

Continue with the next resource in this course.

Course and syllabus information
Course
GCE A-Level H1 Physics
Edition
GCE A-Level H1 Physics 2027