Published by Patrick Mutisya · 8 days ago
Derive, from Newton’s law of gravitation and the definition of gravitational field, the equation
\$g = \frac{GM}{r^{2}}\$
for the gravitational field strength due to a point mass.
| Symbol | Quantity | SI Unit | Typical \cdot alue (if applicable) |
|---|---|---|---|
| \$G\$ | Universal gravitational constant | m³·kg⁻¹·s⁻² | \$6.674 \times 10^{-11}\$ |
| \$M\$ | Mass of the source (point mass) | kg | – |
| \$m\$ | Test mass placed in the field | kg | – |
| \$r\$ | Distance between the centres of the two masses | m | – |
| \$\mathbf{F}\$ | Gravitational force on the test mass | N (kg·m·s⁻²) | – |
| \$\mathbf{g}\$ | Gravitational field strength at distance \$r\$ | m·s⁻² | – |
Start with Newton’s law of universal gravitation for two point masses:
\$\mathbf{F} = -\,\frac{G M m}{r^{2}}\,\hat{\mathbf{r}}\$
where \$\hat{\mathbf{r}}\$ is a unit vector directed from the source mass \$M\$ to the test mass \$m\$, and the negative sign indicates that the force is attractive.
Define the gravitational field (or field strength) \$\mathbf{g}\$ at a point in space as the force per unit test mass:
\$\mathbf{g} = \frac{\mathbf{F}}{m}\$
Substitute the expression for \$\mathbf{F}\$ from step 1 into the definition of \$\mathbf{g}\$:
\$\$\mathbf{g} = \frac{-\,G M m}{r^{2}}\,\frac{\hat{\mathbf{r}}}{m}
= -\,\frac{G M}{r^{2}}\,\hat{\mathbf{r}}\$\$
Since the magnitude of the field is usually denoted by \$g\$ (without the vector sign), take the absolute value of the vector expression:
\$g = \frac{G M}{r^{2}}\$
The direction of \$\mathbf{g}\$ is radially inward toward the mass \$M\$.
The equation \$g = GM/r^{2}\$ tells us that the gravitational field strength:
Find the gravitational field strength at the surface of the Earth (radius \$R{\oplus}=6.37\times10^{6}\,\text{m}\$, mass \$M{\oplus}=5.97\times10^{24}\,\text{kg}\$).
Using \$g = GM/r^{2}\$:
\$\$g_{\oplus} = \frac{(6.674\times10^{-11})\,(5.97\times10^{24})}{(6.37\times10^{6})^{2}}
\approx 9.81\ \text{m·s}^{-2}\$\$
This matches the standard value of the acceleration due to gravity at sea level.
Starting from Newton’s law of gravitation and the definition of gravitational field, we derived the simple yet powerful relation \$g = GM/r^{2}\$. This expression underpins many calculations in astrophysics, orbital mechanics, and everyday problems involving gravity.