Gravitational Field Strength

g=GMr2g = \frac{GM}{r^{2}}

Worked example: Earth surface → g = 9.820 m/s^2 — press Try an example to run it live, then adjust anything.

Enter your known values, leave one input blank, and solves for the missing one. Tap a variable’s symbol to see what it means, with a typical value. Try different units for next level excitement!

Here the solver did the work — could you?

Little g from big G →

Grade 12Grade 12 Physics

Test your skills in the Exam Room: new numbers every attempt — free lessons for students, no sign-up, just pure learning. Find 1 more lesson on this formula.

See your Report Card
Compete with your friends
share your results
Learning zone

Gravitational Field Strength explained

Mrg

Divide Newton's law of gravitation by the test mass and what remains is the field itself: g = GM/r², the acceleration any object feels at distance r, regardless of what it is made of. At Earth's surface, g = 6.674 × 10⁻¹¹ × 5.97 × 10²⁴ / (6.371 × 10⁶)² ≈ 9.82 m/s² — matching the measured free-fall value once Earth's spin is accounted for. Cavendish's 1798 torsion-balance measurement of G turned this equation around and, as headlines put it, "weighed the Earth."

The inverse-square fall-off is steep near a planet but gentle far away: on the Moon (M = 7.35 × 10²² kg, r = 1.737 × 10⁶ m) the same formula gives 1.63 m/s², a sixth of Earth's pull, which is why Apollo astronauts bounded rather than walked. And at the ISS's altitude, g is still about 8.7 m/s² — nearly nine-tenths of surface gravity. Astronauts float not because gravity is absent, but because they and their station are falling together.

Gravitational Field Strength formula

g=GMr2g = \frac{GM}{r^{2}}
Where
  • gg= Field strength (m/s²)
  • MM= Central mass (kg)
  • rr= Distance (m)

Missing one of these? Work it out first, then come back