AstronomyThe Solar SystemMS-ESS1-3

Planet Densities: Rock or Gas?

A planet's mass and radius give its average density, about 4 to 5.5 g/cm³ for rocky planets and 0.7 to 1.6 g/cm³ for the giants.

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In Planets, Moons and Small Bodies you sorted the planets into small rocky ones near the Sun and giants farther out. One number tells the two families apart and reveals what each planet is made of, even ones no spacecraft has landed on: its average density.

Why it works

Density is mass divided by volume, $\rho = \frac{M}{V}$. We can measure both from far away. A planet's mass comes from the orbits of its moons or of passing spacecraft (see weighing with orbits), and its radius from its angular size and distance. A planet is close to a sphere, so $V = \frac{4}{3}\pi r^3$ (volume of spheres). Then we compare with known materials: water is $1$ g/cm³, rock about $3$, iron about $8$, and hydrogen and helium far less. A planet's average density tells the mix.

Key idea

Average density $= \dfrac{M}{\frac{4}{3}\pi r^3}$. Rocky (terrestrial) planets come out at about $4$ to $5.5$ g/cm³: rock with iron cores. The giants come out at about $0.7$ to $1.6$ g/cm³: mostly hydrogen and helium (Jupiter, Saturn) or ices (Uranus, Neptune) around small dense cores.
The planets' masses, radii and average densities (NASA planetary fact sheets).
PlanetMass (Earths)Radius (km)Density (g/cm³)Family
Mercury0.0552,4405.43rocky
Venus0.8156,0525.24rocky
Earth16,3715.51rocky
Mars0.1073,3903.93rocky
Jupiter31869,9111.33gas giant
Saturn9558,2320.69gas giant
Uranus14.525,3621.27ice giant
Neptune17.124,6221.64ice giant
The eight planets drawn to the same scale. The giants are huge, but much less dense.

Worked examples

Worked example: Earth's density

Earth's mass is $5.97 \times 10^{24}$ kg and its radius $6371$ km. Find its average density.
  1. Radius in meters: $6.371 \times 10^{6}$ m.
  2. $V = \frac{4}{3}\pi (6.371 \times 10^{6})^3 = 1.083 \times 10^{21}\ \text{m}^3$ (scientific notation keeps this manageable).
  3. $\rho = \frac{5.97 \times 10^{24}}{1.083 \times 10^{21}} = 5510$ kg/m³ $= 5.51$ g/cm³.
  4. Surface rocks are only about $2.7$ to $3$ g/cm³, so the inside must be denser: Earth has an iron core.

Answer: $5.51$ g/cm³.

Worked example: A planet that floats

Saturn's mass is $5.68 \times 10^{26}$ kg and its radius $58{,}232$ km. Find its density.
  1. $V = \frac{4}{3}\pi (5.8232 \times 10^{7})^3 = 8.27 \times 10^{23}\ \text{m}^3$.
  2. $\rho = \frac{5.68 \times 10^{26}}{8.27 \times 10^{23}} = 687$ kg/m³ $= 0.69$ g/cm³.
  3. Less than water: in a big enough ocean, Saturn would float.

Answer: $0.69$ g/cm³.

Common mistake

It is tempting to think the biggest planets must be the densest. The opposite is true: Jupiter is 318 times Earth's mass but about 1300 times its volume, so it is only a quarter as dense. Density compares mass with volume; size alone tells nothing. Check: Earth, a small planet, is the densest of all.
Earth's density is a little higher than it would be uncompressed, because its own weight squeezes the deep rock and iron. The Moon, at $3.34$ g/cm³, has only a small iron core.

Practice

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Sources and further reading

  • OpenStax, Astronomy 2e, section 7.2, Composition and Structure of Planets
  • NASA Planetary Fact Sheet (masses, radii, densities)
  • NGSS MS-ESS1-3
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