The Foundations of Universal Gravitation
The gravitational field and weight
From the gravitational field to weight
A celestial body of mass M and radius R creates a gravitational field around itself. At the surface of this celestial body, the intensity of this field, denoted by g, is given by: g = G * M / R^2
This field g is expressed in N/kg (or, equivalently, in m/s²). The weight P of an object of mass m placed in this field is therefore: P = m * g
Weight is a force directed towards the centre of the celestial body; whilst the mass m is an intrinsic property of the object that never changes.
Weight depending on the celestial body
| Celestial body | g (N/kg) | Weight of a 70 kg mass |
|---|---|---|
| Earth | 9.8 | 686 N |
| Moon | 1.6 | 112 N |
| Mars | 3.7 | 259 N |
| Jupiter | 24.8 | 1736 N |
g also varies with altitude
The further away you are from the centre of the celestial body (using R + altitude instead of R), the lower g becomes, as g is inversely proportional to the square of the distance from the centre. This is why g is slightly weaker at the top of a mountain than at sea level, and much weaker in orbit.
Common pitfalls
- Mass and weight are not synonymous: mass (in kg) is constant throughout the universe, whilst weight (in N) depends on location.
- In everyday language, we say ‘weigh 70 kg’, which is a misnomer: we should say ‘have a mass of 70 kg’.
- Remember to use R + altitude (and not just R) when the object is not exactly on the surface of the celestial body.

