Newton discovered that every two masses attract each other with a force that is proportional to the product of their masses and inversely proportional to the square of the distance between them. The formula is:
\$F = G \dfrac{m1 m2}{r^2}\$
Where:
When we talk about a “point mass”, we imagine all the mass concentrated at a single point. A uniform sphere (like a planet) is more realistic, but for a point that lies outside the sphere, the sphere’s gravity behaves exactly as if all its mass were at its centre. This is a powerful simplification that saves us from complex calculations.
The shell theorem tells us:
Think of the sphere as a collection of many tiny point masses. For a point outside the sphere, the forces from opposite sides cancel out, leaving only the effect of the total mass at the centre. This is like feeling the pull of a giant snowball from far away – you don’t feel the individual snowflakes, just the whole ball’s pull.
Suppose a satellite of mass \$ms = 500\,\text{kg}\$ orbits Earth at a distance \$r = 7.0\times10^6\,\text{m}\$ from Earth’s centre. Using Earth’s mass \$ME = 5.97\times10^{24}\,\text{kg}\$:
\$F = G \dfrac{ME\,ms}{r^2}\$
Plugging in the numbers gives the gravitational pull on the satellite. Notice we treated Earth as a point mass at its centre – no need to integrate over Earth’s volume!
| Scenario | Effective Mass | Formula |
|---|---|---|
| Point outside a uniform sphere | Total mass \$M\$ at centre | \$F = G \dfrac{M\,m}{r^2}\$ |
| Point inside a uniform sphere | Mass inside radius \$r\$: \$M_{\text{enc}} = M \left(\dfrac{r^3}{R^3}\right)\$ | \$F = G \dfrac{M_{\text{enc}}\,m}{r^2}\$ |
💡 Remember: For any object outside a uniform spherical body, you can treat the entire body as a point mass at its centre. This trick turns a complex problem into a simple one!