ASTR 120 ยท Lecture 04

Planetary Interiors and Differentiation

Solar-system evidence, physics, and exploration

Why This Question Matters

Seismology transformed Earth science; planetary missions extend similar inference to the Moon, Mars, and icy worlds.

Learning Goals

Terms for This Lecture

Mean density

Definition: The total mass of a world divided by the volume set by its mean radius.

Why it matters and connects: It constrains broad rock, metal, ice, gas, and porosity fractions before a detailed interior model is attempted.

Boundary or common confusion: Different mixtures and compression states can share the same mean density.

\(\bar{\rho}=3M/(4\pi R^3)\)

Opening Phenomenon

Density, gravity, magnetic fields, and heat flow reveal interiors we cannot sample directly.

Interior Evidence Is Indirect

Density: average composition, not a layer-by-layer map.

Shape and gravity: mass distribution and possible differentiated interiors.

Magnetism: clues to conductive liquids, rotation, and present internal motion.

Why Differentiation Happens

When a young body is warm enough to partially melt, dense metal can sink and lighter silicate or ice can rise. Accretion energy, radioactive decay, and giant impacts all help determine whether a world separates into layers.

Evidence We Need

Layered Worlds from Sparse Measurements

Interpret the diagram as a model constrained by mass, radius, density, field measurements, and heat flow. The layers are an inference, not something directly photographed.

Differentiated Interior metal core rocky mantle volatile layer Density and magnetic evidence constrain unseen interiors.
Density and magnetic evidence constrain unseen interiors.

Density Calculation: Saturn Is Not Rock

\[ \rho={M\over (4/3)\pi R^3} \]

Using the planetary-property table, Saturn's mean density is about 0.69 g/cm3, below liquid water. A low mean density requires abundant hydrogen and helium, even though pressure deep inside produces unfamiliar material states.

Worked Inference: Mercury Versus Mars

Evidence Boundary: Mean Density Has Degeneracy

The same average density can come from different mixtures of rock, metal, ice, porosity, or compression. Interior claims become stronger when density is paired with moment of inertia, gravity field, magnetic field, and seismic or tidal response.

Reasoning Prompt: Pick the Interior Test

A moon has density 1.9 g/cm3 and a weak induced magnetic signal. Which interior model is better supported: dry rock plus porosity, rock mixed with ice, or a salty subsurface ocean? What measurement would most reduce the ambiguity?

Evidence Bridge: Magnetic Fields Need Mechanisms

A magnetic field can be intrinsic, induced, or absent for different reasons. Distinguish a dynamo in a moving conductive layer from an induced response to a parent planet's field before turning magnetism into an interior claim.

Synthesis: Interiors Are Model-Built

References and Visual Credits