Specific Orbital Energy Calculator
Specific orbital energy (ε) is the total mechanical energy per unit mass of a body in orbit around a massive central body. For an elliptical orbit, ε = -GM / (2a), where G is the universal gravitational constant (6.674 × 10^-11 N m²/kg²), M is the mass of the central body (kg), and a is the semi-major axis of the orbit (m). The result is always negative for bound orbits, zero for parabolic escape trajectories, and positive for hyperbolic flyby trajectories. This calculator uses Earth as the default central body (GM = 3.986 × 10^14 m³/s²) but allows custom values.
Specific orbital energy formula
ε = -GM / (2a)
Where G = 6.674 × 10^-11 N m²/kg² (gravitational constant), M is the central body mass (kg), and a is the semi-major axis (m). For Earth, GM = 3.986 × 10^14 m³/s². Energy is in Joules per kilogram (J/kg).
Reference orbital energies (Earth)
- Low Earth orbit (altitude 200 km, a = 6,571 km): epsilon = -30.3 MJ/kg
- International Space Station (altitude 408 km, a = 6,779 km): epsilon = -29.3 MJ/kg
- Geostationary orbit (altitude 35,786 km, a = 42,164 km): epsilon = -4.72 MJ/kg
- Moon (a = 384,400 km): epsilon = -0.519 MJ/kg
- Escape trajectory (parabolic): epsilon = 0
Specific orbital energy: frequently asked questions
What is specific orbital energy?
Specific orbital energy (epsilon) is the total mechanical energy per unit mass of an orbiting body: the sum of its kinetic and potential energy per unit mass. For a bound elliptical orbit, epsilon = -GM/(2a), where G is the gravitational constant, M is the central body mass, and a is the semi-major axis of the orbit.
Why is specific orbital energy negative for bound orbits?
A negative total energy means the object is bound to the gravitational field and cannot escape. Zero energy means it is at the escape boundary (parabolic trajectory). Positive energy means it is on a hyperbolic escape trajectory. This parallels atomic orbital energy levels, which are also negative for bound electrons.
What is the vis-viva equation?
The vis-viva equation relates orbital speed v at any point in the orbit to the distance r from the central body: v² = GM(2/r - 1/a). At periapsis (closest approach) speed is highest; at apoapsis (farthest point) speed is lowest. Specific orbital energy epsilon = -GM/(2a) is constant throughout the orbit.
What are typical values for Earth orbits?
For a low Earth orbit (a = 6,571 km = 6.571 x 10^6 m) with GM = 3.986 x 10^14 m³/s², epsilon = -30.3 MJ/kg. For a geostationary orbit (a = 42,164 km), epsilon = -4.72 MJ/kg. The closer the orbit, the more negative (more tightly bound) the energy.
How is this used in orbital mechanics?
Specific orbital energy is conserved in Keplerian orbits (no drag or thrust). Knowing epsilon allows calculation of the semi-major axis for any orbit. Changing epsilon by firing a rocket changes the orbit. Delta-v calculations for orbital maneuvers (like Hohmann transfers) rely on this relationship.
Official sources
- NIST Reference on Constants: Newtonian constant of gravitation.
- NASA Jet Propulsion Laboratory: Planetary Physical Parameters.
Reviewed by the CalculatorHub team, edited by James Graham, 15 June 2026. See our methodology.