OlympIQ
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Write g as GM/R² and Change Only the Quantity That Changes

Gravity questions mostly ask how g, or the weight of a body, changes when the mass, the radius, the height or the depth changes. Write g = GM/R² once and scale it.

NSEJS · Gravitation · 17 linked questions · 100% coverage
Know this first

Motion and force questions become simpler when direction, starting condition, time and the acting forces are marked first.

Distance · Length of the path travelledDisplacement · Straight-line change in positionResultant force · Net force including direction
Study deeper: NCERT Science · Gravitation
See it

Draw every push or pull as an arrow

Push / pull
Resultant
Motion

Balanced arrows: no change · unbalanced: acceleration

Arrows show direction. Balanced arrows give no change in motion; an unbalanced resultant points toward the acceleration.

Newton's law and the surface value of g

The force between two masses is F = G m1 m² / r², and by Newton's third law the force of the Earth on the Moon equals the force of the Moon on the Earth, whatever their masses, a ratio of 1 : 1.

At the surface
g=GM/R2g = GM/R²
A planet of diameter D has
g=4GM/D2g = 4GM/D²

Mars, with 0.5 of Earth's diameter and 0.1 of its mass, has g ratio 0.1 / (0.5)² = 0.4.

The mass of the Earth follows from
M=gR2/GM = g R² / G

If the radius shrinks by 1% with the mass fixed, g rises by about 2%, because g is proportional to R⁻².

Height and depth

At height h above the surface, g' = g R²/(R + h)², which is about g (1 - 2h/R) for small h.

So g falls to g/4 at
h = R and to g/2 at h = (√2 - 1) R, and at 32 km up (h/R = 0.005) it is 0.99 g

Inside a uniform Earth, g' = g (1 - d/R) at depth d, falling linearly to zero at the centre.

If the weight drops 1% at a height h, then 2h/
R = 0.01, and at depth h the drop is half as large, 0.5%

Plotted against distance from the centre, g rises linearly inside, peaks at the surface and then falls as 1/r².

Rotation, balances and other worlds

Rotation reduces the effective g everywhere except at the poles, so if the Earth stopped rotating, g would increase at every place other than the poles. A spring balance measures weight, which varies with g, while a physical (beam) balance compares masses, so it reads the same at the poles and equator. The Moon's g is one sixth of the Earth's and it has no atmosphere, so a hydrogen balloon does not float up there but falls with acceleration g/6, and a stone dropped from the same height takes sqrt(6) times as long to land. For a 60 kg passenger flying from Earth to Mars the weight is 600 N at Earth's surface and 240 N at Mars's surface, with a much smaller net pull for most of the journey, since both pulls weaken with distance.

Adding gravitational forces as vectors

The force on a mass from several others is a vector sum. For three 1 kg masses at (0, 0), (0, 0.2 m) and (0.2 m, 0), each neighbour pulls the mass at the origin with G m²/r² = 6.67 x 10⁻¹¹ / 0.04 = 1.67 x 10⁻⁹ N, one along +y and one along +x, so the net force is 1.67 x 10⁻⁹ (i + j) N.

OlympIQ exam lens

  • ✓g = GM/R²; for diameter D, g = 4GM/D²; M = gR²/G
  • ✓Above the surface g' = gR²/(R + h)² ≈ g(1 - 2h/R); below it g' = g(1 - d/R)
  • ✓Third law: the pull of A on B equals the pull of B on A
  • ✓Rotation lowers effective g except at the poles; a spring balance shows weight, a beam balance compares mass
  • ✓Sum forces from several masses as vectors
OlympIQ trap

Do not apply g' = g(1 - 2h/R) when h is comparable to R. For large heights use g' = gR²/(R + h)²; the linear approximation fails, and at h = R the value is g/4, not zero.

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