In astrodynamics or celestial mechanics a parabolictrajectory is a Kepler orbit with the eccentricity equal to 1 and is an unbound orbit that is exactly on the border between elliptical and hyperbolic. When moving away from the source it is called an escape orbit, otherwise a capture orbit. It is also sometimes referred to as a C3 = 0 orbit. Under standard assumptions a body traveling along an escape orbit will coast along a parabolic trajectory to infinity, with velocity relative to the central body tending to zero, and therefore will never return. Parabolic trajectories are minimum-energy escape trajectories, separating positive-energy hyperbolic trajectories from negative-energy elliptic orbits.
Velocity
The orbital velocity of a body travelling along parabolic trajectory can be computed as: where:
At any position the orbiting body has the escape velocity for that position. If the body has the escape velocity with respect tothe Earth, this is not enough to escape the Solar System, so near the Earth the orbit resembles a parabola, but further away it bends into an elliptical orbitaround the Sun. This velocity is closely related to the orbital velocity of a body in a circular orbit of the radius equal to the radial position of orbiting body on the parabolic trajectory: where:
is orbital velocity of a body in circular orbit.
Equation of motion
For a body moving along this kind of trajectory an orbital equation becomes: where:
is radial distance of orbiting body from central body,
More generally, the time between any two points on an orbit is Alternately, the equation can be expressed in terms of periapsis distance, in a parabolic orbit rp = p/2: Unlike Kepler's equation, which is used to solve for true anomalies in elliptical and hyperbolic trajectories, the true anomaly in Barker's equation can be solved directly for t. If the following substitutions are made then
Radial parabolic trajectory
A radial parabolic trajectory is a non-periodic trajectory on a straight line where the relative velocity of the two objects is always the escape velocity. There are two cases: the bodies move away from each other or towards each other. There is a rather simple expression for the position as function of time: where
μ is the standard gravitational parameter
corresponds to the extrapolated time of the fictitious starting or ending at the center of the central body.
At any time the average speed from is 1.5 times the current speed, i.e. 1.5 times the local escape velocity. To have at the surface, apply a time shift; for the Earth as central body this time shift is 6 minutes and 20 seconds; seven of these periods later the height above the surface is three times the radius, etc.