Physics · Gravitation

Kepler Third Law

The squares of the orbital periods behave like the cubes of the semi-major axes; the quotient T²/a³ is the same for all bodies orbiting the same central body.

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Formula

LaTeX: \frac{T^2}{a^3} = \frac{4\pi^2}{G \cdot M}
T in s · a in m · G = 6.674×10⁻¹¹ N·m²/kg² · M in kg

Variables & units – Kepler Third Law

SymbolMeaningUnit
TOrbital period of the celestial bodys
aSemi-major axis of the orbitm
GGravitational constant (6.674×10⁻¹¹)N·m²/kg²
MMass of the central bodykg

Derivation & background – Kepler Third Law

Johannes Kepler found the law empirically in 1618 from Tycho Brahe observational data. Newton later derived it from his law of gravitation: for circular orbits, gravitational force = centripetal force gives G·M·m/r² = m·ω²·r and thus T²/r³ = 4π²/(G·M). Practically important: measuring T and a of a satellite or moon yields the mass of the central body; this is how solar and planetary masses were determined.

Exam blueprint

Validity range

Applies to orbits around the same central body when its mass M far exceeds that of the satellite. a is the semi-major axis of the ellipse; for circular orbits a is the orbital radius.

Derivation steps

Gravity provides exactly the centripetal force of the circular orbit.

  1. 1Force balance: G·M·m/r² = m·ω²·r with ω = 2π/T.
  2. 2Solving gives T² = 4π²·r³/(G·M), hence T²/r³ = 4π²/(G·M) = constant.

Rearrangements

Mass of the central body

This is how solar and planetary masses are determined from orbital data.

Orbital period

Larger orbits mean disproportionately longer periods.

Semi-major axis

Yields, for example, the altitude of geostationary satellites.

Task variant

Jupiter needs 11.86 years per solar orbit. What is its semi-major axis in AU?

In Earth-orbit units a³ = T²: a³ = 11.86² = 140.7, so a = ∛140.7 ≈ 5.2 AU.

The Moon orbits Earth in 27.32 days at a = 3.844×10⁸ m. Determine the Earth mass.

T = 2.36×10⁶ s. M = 4π²a³/(G·T²) = 39.48 × 5.68×10²⁵/(6.674×10⁻¹¹ × 5.57×10¹²) ≈ 6.0×10²⁴ kg.

Common mistakes

Using a satellite altitude above ground as the orbital radius.

Add the Earth radius (6,371 km) to the altitude: r = R_E + h.

Substituting periods in days or years into the SI form.

The form with G and M needs T in seconds; AU-year units only for pure ratios in the solar system.

Comparing orbits around different central bodies.

T²/a³ is constant only for the same central body; the constant contains its mass.

Exam context

  • Typical: computing the geostationary orbit altitude, determining central masses from moon or satellite data and checking planetary data via the ratio T²/a³.

These mistakes cost points in real exams. The set drills them until they stick.

Formula cluster

Gravity and orbits

Follows from the law of gravitation plus circular motion, the tool of celestial mechanics.

Worked example

Mars: a = 1.524 AU. In Earth-orbit units T = √(a³) = √(1.524³) = √3.54 ≈ 1.88 years. Geostationary satellites (T = 1 sidereal day) orbit at a ≈ 42,160 km.

Applications

Satellite orbits (GPS, geostationary), mass determination of stars and planets, exoplanet detection, spaceflight mission planning

Quanta exam set

Curated exam set for "Kepler Third Law":

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Which formula describes Kepler Third Law?

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How do you rearrange T²/a³ = 4π²/(G·M) for Mass of the central body?

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Which common mistake happens with Kepler Third Law?

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Scientific sources

Common notations & search queries

T^2/a^3=constT² a³ Gesetzdrittes Keplersches Gesetz FormelKepler 3 FormelUmlaufzeit Satellit berechnenKepler's third lawgeostationärer Satellit Höhe

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Frequently asked questions about Kepler Third Law

How do you apply Kepler third law in practice?+

There are two calculation routes. Within the solar system you use the pure ratio: in the units AU and years, T² = a³ holds for the Sun, because the Earth orbit sets both constants to 1. Mars with a = 1.524 AU therefore has T = √(1.524³) ≈ 1.88 years. For satellites or other central bodies you need the SI form T² = 4π²·a³/(G·M) with T in seconds, a in metres and M in kilograms. Choose the route by the question: ratios between planets work without G and M, absolute quantities such as a satellite altitude demand the full formula.

How do you calculate the altitude of a geostationary satellite?+

A geostationary satellite appears fixed above one point of the equator, so its period is one sidereal day T = 86,164 s. Rearrange the law for the semi-major axis: a³ = G·M·T²/(4π²). With G·M_Earth = 3.986×10¹⁴ m³/s² you get a³ = 3.986×10¹⁴ × 7.42×10⁹/39.48 ≈ 7.50×10²², so a ≈ 42,160 km from the Earth centre. Subtracting the Earth radius of 6,371 km leaves an orbital altitude of about 35,790 km above the equator. Television and weather satellites sit there. The most common mistakes are not subtracting the Earth radius or using the 24-hour solar day instead of the sidereal day.

How do you determine the mass of a celestial body with Kepler 3?+

Rearrange the SI form for the central mass: M = 4π²·a³/(G·T²). You only need the orbital data of one satellite. Example, Earth mass from the lunar orbit: a = 3.844×10⁸ m and T = 27.32 days = 2.36×10⁶ s give M = 39.48 × 5.68×10²⁵/(6.674×10⁻¹¹ × 5.57×10¹²) ≈ 6.0×10²⁴ kg, in good agreement with the literature value 5.97×10²⁴ kg. The solar mass (from the Earth orbit), the Jupiter mass (from the Galilean moons) and the masses of exoplanet systems were determined by the same pattern. Important: the mass of the small satellite cancels; you always obtain the mass of the central body.

Why is T²/a³ the same for all planets?+

Because the constant contains only properties of the central body. Newton derivation shows it: the gravitational force G·M·m/r² provides the centripetal force m·ω²·r of the orbit. The planet mass m cancels, and with ω = 2π/T what remains is T²/r³ = 4π²/(G·M). The right side holds only natural constants and the solar mass M, so Mercury through Neptune yield the same numerical value although their periods range from 88 days to 165 years. Exactly this told Newton that his theory of gravity was right: it reproduces Kepler empirically found law. Around another central body, such as Earth or Jupiter, the same structure holds with a different M and therefore a different constant.

What is the semi-major axis of an elliptical orbit?+

According to Kepler first law, planetary orbits are ellipses with the Sun at one focus. The semi-major axis a is half the length of the longest axis of the ellipse and at the same time the mean of the smallest and largest solar distances: a = (r_perihelion + r_aphelion)/2. Exactly this a enters the third law, not the current distance, which changes constantly. For the nearly circular Earth orbit a is practically the orbital radius (1 AU = 1.496×10¹¹ m). Remarkably, the period depends only on a, not on the eccentricity. A comet with the same semi-major axis as a planet takes exactly as long per orbit, no matter how elongated its path is.

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Create a curated FSRS exam set for T²/a³ = 4π²/(G·M): formula recall, variables, derivation, rearrangement, worked example, common mistakes and exam context.

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How do you calculate with Kepler Third Law?

Here is how to work through a typical Kepler Third Law (T²/a³ = 4π²/(G·M)) task step by step:

  1. 1

    Task

    Jupiter needs 11.86 years per solar orbit. What is its semi-major axis in AU?

    Solution path

    In Earth-orbit units a³ = T²: a³ = 11.86² = 140.7, so a = ∛140.7 ≈ 5.2 AU.

  2. 2

    Task

    The Moon orbits Earth in 27.32 days at a = 3.844×10⁸ m. Determine the Earth mass.

    Solution path

    T = 2.36×10⁶ s. M = 4π²a³/(G·T²) = 39.48 × 5.68×10²⁵/(6.674×10⁻¹¹ × 5.57×10¹²) ≈ 6.0×10²⁴ kg.