Kepler's third law — harmonic
Statement
The square of the orbital period T² is proportional to the cube of the semi-major axis a³ — for all planets orbiting the same star:
T² / a³ = 4π² / (G·M) = const
with G the gravitational constant and M the star's mass.
Why is it true?
Kepler found this ratio in 1619 by cross-checking astronomical data — without knowing why. Newton (1687) later proved it follows from the inverse-square law of gravitation.
Kepler III lets astronomers "weigh" stars: measure T and a of a planet or binary star and M falls out — a key tool of modern astronomy.
Applications
Estimating stellar and supermassive-black-hole masses, exoplanet detection (transit + RV), satellite orbit sizing, astronomical distance scales.
Topics that use this theorem
Related theorems
Step-by-step proofs
References
- Johannes Kepler (1619). Harmonices Mundi