Academy
Kepler Models of Orbits
Level 1 - Physics topic page in Gravitation.
Principle
Kepler's orbit model describes bound gravitational motion with ellipse geometry, constant areal sweep rate, and a period that scales with orbital size.
Notation
Method
Derivation 1: Use the central-force property
Gravity acts along the line joining the orbiting body to the source, so the torque about the source is zero. Zero torque means angular momentum is conserved.
Derivation 2: Turn angular momentum into Kepler's second law
In a short time \(\\Delta t\), the swept region is approximately a triangle. Its area depends on the perpendicular part of the velocity.
Derivation 3: Build the period-size law
For a circular orbit, the inverse-square gravity model gives the full period formula. In the full Kepler problem, the same scaling survives when the orbit is elliptical, with radius replaced by the semi-major axis.
Solving the full inverse-square equations gives Kepler's first law: bound orbits are ellipses with the central mass at one focus, not at the geometric center.
Rules
These are the compact results from the method above.
Examples
Checks
- The central mass sits at a focus of the ellipse, not at the center of the ellipse.
- Equal areas in equal times mean the orbiting body moves faster when it is closer to the source.
- Kepler's third law compares orbits around the same central mass unless the constant is written explicitly.
- The semi-major axis, not the instantaneous radius, sets the period for an elliptical orbit.