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Kepler Orbital Period

Compute orbital period T = 2π√(a³/GM) from semi-major axis (m) and central mass (kg).

Kepler's laws: T² = a³ (AU and years)

Kepler formulated three laws of planetary motion between 1609 and 1619, based on Tycho Brahe's observations. 1st law: planets orbit in ellipses with the Sun at one focus (not a circle, as previously believed). 2nd law: the radius vector sweeps equal areas in equal times — a direct consequence of angular momentum conservation, so planets move faster at perihelion than aphelion. 3rd law: T² = k·a³; expressed in astronomical units (AU) and years for the solar system, the constant becomes exactly 1, giving T² = a³. The generalized form is T² = (4π²/GM)·a³, valid for any central body of mass M. Example: Mercury orbits with a = 0.387 AU, so T² = 0.058 → T = 0.24 years (about 88 days), matching observation. Modern exoplanet missions (TESS, James Webb) detect distant worlds by the transit method — dimming as the planet crosses the host star.

Applications

Space mission design (Hohmann transfer orbits, gravitational slingshots used by Voyager 1 and 2 to leave the solar system), GPS constellation (satellites orbit at ~20,200 km with T = 12 h, a = 26,560 km), geostationary satellites for TV and communications (T = 23 h 56 min sidereal day, a = 42,164 km from Earth's center), determining stellar masses in binary systems, and confirming exoplanet detection.

FAQ

Why does T² = a³ work without units in the solar system? Choosing AU for distance and years for period makes the constant 4π²/GM equal to 1 when M is one solar mass. For other systems (Jupiter's moons, exoplanets), you need the full equation with G and M.

Do the laws apply to artificial satellites? Yes — they apply to anything orbiting a central mass under gravity, using Earth's mass instead of the Sun's. A satellite at a = 7,000 km from Earth's center has T ≈ 97 min.

How did Newton explain Kepler's laws? Newton derived all three from his law of universal gravitation (F = GMm/r²) plus F = ma — turning Kepler's empirical descriptions into mathematical consequences of a single physical law.

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