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In physics (specifically, celestial mechanics), escape velocity is the minimum speed needed for a free, nonpropelled object to escape from the gravitational influence of a massive body, that is, to eventually reach an infinite distance from it. Escape velocity rises with the body's mass (body to be escaped) and falls with the escaping object's distance from its center. The escape velocity thus depends on how far the object has already traveled, and its calculation at a given distance takes into account the fact that without new acceleration it will slow down as it travels—due to the massive body's gravity—but it will never quite slow to a stop.
A rocket, continuously accelerated by its exhaust, can escape without ever reaching escape velocity, since it continues to add kinetic energy from its engines. It can achieve escape at any speed, given sufficient propellant to provide new acceleration to the rocket to counter gravity's deceleration and thus maintain its speed.
The escape velocity from Earth's surface is about 11,186 m/s (6.951 mi/s; 40,270 km/h; 36,700 ft/s; 25,020 mph; 21,744 kn).^{[1]} More generally, escape velocity is the speed at which the sum of an object's kinetic energy and its gravitational potential energy is equal to zero;^{[nb 1]} an object which has achieved escape velocity is neither on the surface, nor in a closed orbit (of any radius). With escape velocity in a direction pointing away from the ground of a massive body, the object will move away from the body, slowing forever and approaching, but never reaching, zero speed. Once escape velocity is achieved, no further impulse need be applied for it to continue in its escape. In other words, if given escape velocity, the object will move away from the other body, continually slowing, and will asymptotically approach zero speed as the object's distance approaches infinity, never to come back.^{[2]} Speeds higher than escape velocity retain a positive speed at infinite distance. Note that the minimum escape velocity assumes that there is no friction (e.g., atmospheric drag), which would increase the required instantaneous velocity to escape the gravitational influence, and that there will be no future acceleration or extraneous deceleration (for example from thrust or from gravity of other bodies), which would change the required instantaneous velocity.
For a spherically symmetric, massive body such as a star, or planet, the escape velocity for that body, at a given distance, is calculated by the formula^{[3]}
where G is the universal gravitational constant (G ≈ 6.67×10^{−11} m^{3}·kg^{−1}·s^{−2}), M the mass of the body to be escaped from, and r the distance from the center of mass of the body to the object.^{[nb 2]} The relationship is independent of the mass of the object escaping the massive body. Conversely, a body that falls under the force of gravitational attraction of mass M, from infinity, starting with zero velocity, will strike the massive object with a velocity equal to its escape velocity given by the same formula.
When given an initial speed greater than the escape speed the object will asymptotically approach the hyperbolic excess speed satisfying the equation:^{[4]}
In these equations atmospheric friction (air drag) is not taken into account.
Overview
The existence of escape velocity is a consequence of conservation of energy and an energy field of finite depth. For an object with a given total energy, which is moving subject to conservative forces (such as a static gravity field) it is only possible for the object to reach combinations of locations and speeds which have that total energy; and places which have a higher potential energy than this cannot be reached at all. By adding speed (kinetic energy) to the object it expands the possible locations that can be reached, until, with enough energy, they become infinite.
For a given gravitational potential energy at a given position, the escape velocity is the minimum speed an object without propulsion needs to be able to "escape" from the gravity (i.e. so that gravity will never manage to pull it back). Escape velocity is actually a speed (not a velocity) because it does not specify a direction: no matter what the direction of travel is, the object can escape the gravitational field (provided its path does not intersect the planet).
An elegant way to derive the formula for escape velocity is to use the principle of conservation of energy (for another way, based on work, see below). For the sake of simplicity, unless stated otherwise, we assume that an object will escape the gravitational field of a uniform spherical planet by moving away from it and that the only significant force acting on the moving object is the planet's gravity. Imagine that a spaceship of mass m is initially at a distance r from the center of mass of the planet, whose mass is M, and its initial speed is equal to its escape velocity, . At its final state, it will be an infinite distance away from the planet, and its speed will be negligibly small. Kinetic energy K and gravitational potential energy U_{g} are the only types of energy that we will deal with (we will ignore the drag of the atmosphere), so by the conservation of energy,
We can set K_{ƒinal} = 0 because final velocity is arbitrarily small, and U_{gƒinal} = 0 because final distance is infinity, so
where μ is the standard gravitational parameter.
The same result is obtained by a relativistic calculation, in which case the variable r represents the radial coordinate or reduced circumference of the Schwarzschild metric.^{[6]}^{[7]}
Defined a little more formally, "escape velocity" is the initial speed required to go from an initial point in a gravitational potential field to infinity and end at infinity with a residual speed of zero, without any additional acceleration.^{[8]} All speeds and velocities are measured with respect to the field. Additionally, the escape velocity at a point in space is equal to the speed that an object would have if it started at rest from an infinite distance and was pulled by gravity to that point.
In common usage, the initial point is on the surface of a planet or moon. On the surface of the Earth, the escape velocity is about 11.2 km/s, which is approximately 33 times the speed of sound (Mach 33) and several times the muzzle velocity of a rifle bullet (up to 1.7 km/s). However, at 9,000 km altitude in "space", it is slightly less than 7.1 km/s. Note that this escape velocity is relative to a nonrotating frame of reference, not relative to the moving surface of the planet or moon (see below).
The escape velocity is independent of the mass of the escaping object. It does not matter if the mass is 1 kg or 1,000 kg; what differs is the amount of energy required. For an object of mass the energy required to escape the Earth's gravitational field is GMm / r, a function of the object's mass (where r is the radius of the Earth, G is the gravitational constant, and M is the mass of the Earth, M = 5.9736 × 10^{24} kg). A related quantity is the specific orbital energy which is essentially the sum of the kinetic and potential energy divided by the mass. An object has reached escape velocity when the specific orbital energy is greater than or equal to zero.
Scenarios
From the surface of a body
An alternative expression for the escape velocity particularly useful at the surface on the body is:
where r is the distance between the center of the body and the point at which escape velocity is being calculated and g is the gravitational acceleration at that distance (i.e., the surface gravity).^{[9]}
For a body with a sphericallysymmetric distribution of mass, the escape velocity from the surface is proportional to the radius assuming constant density, and proportional to the square root of the average density ρ.
where
Note that this escape velocity is relative to a nonrotating frame of reference, not relative to the moving surface of the planet or moon, as we now explain.
From a rotating body
The escape velocity relative to the surface of a rotating body depends on direction in which the escaping body travels. For example, as the Earth's rotational velocity is 465 m/s at the equator, a rocket launched tangentially from the Earth's equator to the east requires an initial velocity of about 10.735 km/s relative to the moving surface at the point of launch to escape whereas a rocket launched tangentially from the Earth's equator to the west requires an initial velocity of about 11.665 km/s relative to that moving surface. The surface velocity decreases with the cosine of the geographic latitude, so space launch facilities are often located as close to the equator as feasible, e.g. the American Cape Canaveral (latitude 28°28′ N) and the French Guiana Space Centre (latitude 5°14′ N).
Practical considerations
In most situations it is impractical to achieve escape velocity almost instantly, because of the acceleration implied, and also because if there is an atmosphere, the hypersonic speeds involved (on Earth a speed of 11.2 km/s, or 40,320 km/h) would cause most objects to burn up due to aerodynamic heating or be torn apart by atmospheric drag. For an actual escape orbit, a spacecraft will accelerate steadily out of the atmosphere until it reaches the escape velocity appropriate for its altitude (which will be less than on the surface). In many cases, the spacecraft may be first placed in a parking orbit (e.g. a low Earth orbit at 160–2,000 km) and then accelerated to the escape velocity at that altitude, which will be slightly lower (about 11.0 km/s at a low Earth orbit of 200 km). The required additional change in speed, however, is far less because the spacecraft already has a significant orbital speed (in low Earth orbit speed is approximately 7.8 km/s, or 28,080 km/h).
From an orbiting body
The escape velocity at a given height is times the speed in a circular orbit at the same height, (compare this with the velocity equation in circular orbit). This corresponds to the fact that the potential energy with respect to infinity of an object in such an orbit is minus two times its kinetic energy, while to escape the sum of potential and kinetic energy needs to be at least zero. The velocity corresponding to the circular orbit is sometimes called the first cosmic velocity, whereas in this context the escape velocity is referred to as the second cosmic velocity.^{[10]}
For a body in an elliptical orbit wishing to accelerate to an escape orbit the required speed will vary, and will be greatest at periapsis when the body is closest to the central body. However, the orbital speed of the body will also be at its highest at this point, and the change in velocity required will be at its lowest, as explained by the Oberth effect.
Barycentric escape velocity
Technically escape velocity can either be measured as a relative to the other, central body or relative to center of mass or barycenter of the system of bodies. Thus for systems of two bodies, the term escape velocity can be ambiguous, but it is usually intended to mean the barycentric escape velocity of the less massive body. In gravitational fields, escape velocity refers to the escape velocity of zero mass test particles relative to the barycenter of the masses generating the field. In most situations involving spacecraft the difference is negligible. For a mass equal to a Saturn V rocket, the escape velocity relative to the launch pad is 253.5 am/s (8 nanometers per year) faster than the escape velocity relative to the mutual center of mass.^{[citation needed]}
Height of lowervelocity trajectories
Ignoring all factors other than the gravitational force between the body and the object, an object projected vertically at speed from the surface of a spherical body with escape velocity and radius will attain a maximum height satisfying the equation^{[11]}
which, solving for h results in
where is the ratio of the original speed to the escape velocity
Unlike escape velocity, the direction (vertically up) is important to achieve maximum height.
Trajectory
If an object attains exactly escape velocity, but is not directed straight away from the planet, then it will follow a curved path or trajectory. Although this trajectory does not form a closed shape, it can be referred to as an orbit. Assuming that gravity is the only significant force in the system, this object's speed at any point in the trajectory will be equal to the escape velocity at that point due to the conservation of energy, its total energy must always be 0, which implies that it always has escape velocity; see the derivation above. The shape of the trajectory will be a parabola whose focus is located at the center of mass of the planet. An actual escape requires a course with a trajectory that does not intersect with the planet, or its atmosphere, since this would cause the object to crash. When moving away from the source, this path is called an escape orbit. Escape orbits are known as C3 = 0 orbits. C3 is the characteristic energy, = −GM/2a, where a is the semimajor axis, which is infinite for parabolic trajectories.
If the body has a velocity greater than escape velocity then its path will form a hyperbolic trajectory and it will have an excess hyperbolic velocity, equivalent to the extra energy the body has. A relatively small extra deltav above that needed to accelerate to the escape speed can result in a relatively large speed at infinity. Some orbital manoeuvres make use of this fact. For example, at a place where escape speed is 11.2 km/s, the addition of 0.4 km/s yields a hyperbolic excess speed of 3.02 km/s:
If a body in circular orbit (or at the periapsis of an elliptical orbit) accelerates along its direction of travel to escape velocity, the point of acceleration will form the periapsis of the escape trajectory. The eventual direction of travel will be at 90 degrees to the direction at the point of acceleration. If the body accelerates to beyond escape velocity the eventual direction of travel will be at a smaller angle, and indicated by one of the asymptotes of the hyperbolic trajectory it is now taking. This means the timing of the acceleration is critical if the intention is to escape in a particular direction.
If the speed at periapsis is v, then the eccentricity of the trajectory is given by:
This is valid for elliptical, parabolic, and hyperbolic trajectories. If the trajectory is hyperbolic or parabolic, it will asymptotically approach an angle from the direction at periapsis, with
The speed will asymptotically approach
List of escape velocities
In this table, the lefthand half gives the escape velocity from the visible surface (which may be gaseous as with Jupiter for example), relative to the centre of the planet or moon (that is, not relative to its moving surface). In the righthand half, V_{e} refers to the speed relative to the central body (for example the sun), whereas V_{te} is the speed (at the visible surface of the smaller body) relative to the smaller body (planet or moon).
Location  Relative to  V_{e} (km/s)^{[12]}  Location  Relative to  V_{e} (km/s)^{[12]}  System escape, V_{te} (km/s)  

On the Sun  The Sun's gravity  617.5  
On Mercury  Mercury's gravity  4.25  At Mercury  The Sun's gravity  ~ 67.7  ~ 20.3  
On Venus  Venus's gravity  10.36  At Venus  The Sun's gravity  49.5  17.8  
On Earth  Earth's gravity  11.186  At Earth  The Sun's gravity  42.1  16.6  
On the Moon  The Moon's gravity  2.38  At the Moon  The Earth's gravity  1.4  2.42  
On Mars  Mars' gravity  5.03  At Mars  The Sun's gravity  34.1  11.2  
On Ceres  Ceres's gravity  0.51  At Ceres  The Sun's gravity  25.3  7.4  
On Jupiter  Jupiter's gravity  60.20  At Jupiter  The Sun's gravity  18.5  60.4  
On Io  Io's gravity  2.558  At Io  Jupiter's gravity  24.5  7.6  
On Europa  Europa's gravity  2.025  At Europa  Jupiter's gravity  19.4  6.0  
On Ganymede  Ganymede's gravity  2.741  At Ganymede  Jupiter's gravity  15.4  5.3  
On Callisto  Callisto's gravity  2.440  At Callisto  Jupiter's gravity  11.6  4.2  
On Saturn  Saturn's gravity  36.09  At Saturn  The Sun's gravity  13.6  36.3  
On Titan  Titan's gravity  2.639  At Titan  Saturn's gravity  7.8  3.5  
On Uranus  Uranus' gravity  21.38  At Uranus  The Sun's gravity  9.6  21.5  
On Neptune  Neptune's gravity  23.56  At Neptune  The Sun's gravity  7.7  23.7  
On Triton  Triton's gravity  1.455  At Triton  Neptune's gravity  6.2  2.33  
On Pluto  Pluto's gravity  1.23  At Pluto  The Sun's gravity  ~ 6.6  ~ 2.3  
At Solar System galactic radius  The Milky Way's gravity  492–594^{[13]}^{[14]}  
On the event horizon  A black hole's gravity  299,792.458 (speed of light) 
The last two columns will depend precisely where in orbit escape velocity is reached, as the orbits are not exactly circular (particularly Mercury and Pluto).
Deriving escape velocity using calculus
Let G be the gravitational constant and let M be the mass of the earth (or other gravitating body) and m be the mass of the escaping body or projectile. At a distance r from the centre of gravitation the body feels an attractive force
The work needed to move the body over a small distance dr against this force is therefore given by
The total work needed to move the body from the surface r_{0} of the gravitating body to infinity is then^{[15]}
In order to do this work to reach infinity, the body's minimal kinetic energy at departure must match this work, so the escape velocity v_{0} satisfies
which results in
See also
 Black hole – an object with an escape velocity greater than the speed of light
 Characteristic energy (C_{3})
 Deltav budget – speed needed to perform manoeuvres.
 Gravitational slingshot – a technique for changing trajectory
 Gravity well
 List of artificial objects in heliocentric orbit
 List of artificial objects leaving the Solar System
 Newton's cannonball
 Oberth effect – burning propellant deep in a gravity field gives higher change in kinetic energy
 Twobody problem
Notes
 ^ The gravitational potential energy is negative since gravity is an attractive force and the potential energy has been defined for this purpose to be zero at infinite distance from the centre of gravity.
 ^ The value GM is called the standard gravitational parameter, or μ, and is often known more accurately than either G or M separately.
References
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 ^ Giancoli, Douglas C. (2008). Physics for Scientists and Engineers with Modern Physics. AddisonWesley. p. 199. ISBN 9780131495081.
 ^ Khatri, Poudel, Gautam, M.K., P.R., A.K. (2010). Principles of Physics. Kathmandu: Ayam Publication. pp. 170, 171. ISBN 9789937903844.CS1 maint: multiple names: authors list (link)
 ^ Bate, Roger R.; Mueller, Donald D.; White, Jerry E. (1971). Fundamentals of Astrodynamics (illustrated ed.). Courier Corporation. p. 39. ISBN 9780486600611.
 ^ NASA – NSSDC – Spacecraft – Details
 ^ Taylor, Edwin F.; Wheeler, John Archibald; Bertschinger, Edmund (2010). Exploring Black Holes: Introduction to General Relativity (2nd revised ed.). AddisonWesley. pp. 2–22. ISBN 9780321512864. Sample chapter, page 222
 ^ ChoquetBruhat, Yvonne (2015). Introduction to General Relativity, Black Holes, and Cosmology (illustrated ed.). Oxford University Press. pp. 116–117. ISBN 9780199666461.
 ^ "escape velocity  physics". Retrieved 21 August 2015.
 ^ Bate, Mueller and White, p. 35
 ^ Teodorescu, P. P. (2007). Mechanical systems, classical models. Springer, Japan. p. 580. ISBN 9781402054419., Section 2.2.2, p. 580
 ^ Bajaj, N. K. (2015). Complete Physics: JEE Main. McGrawHill Education. p. 6.12. ISBN 9789339220327. Example 21, page 6.12
 ^ ^{a} ^{b} For planets: "Planets and Pluto : Physical Characteristics". NASA. Retrieved 18 January 2017.
 ^ Smith, Martin C.; Ruchti, G. R.; Helmi, A.; Wyse, R. F. G. (2007). "The RAVE Survey: Constraining the Local Galactic Escape Speed". Proceedings of the International Astronomical Union. 2 (S235): 755–772. arXiv:astroph/0611671. doi:10.1017/S1743921306005692.
 ^ Kafle, P.R.; Sharma, S.; Lewis, G.F.; BlandHawthorn, J. (2014). "On the Shoulders of Giants: Properties of the Stellar Halo and the Milky Way Mass Distribution". The Astrophysical Journal. 794 (1): 17. arXiv:1408.1787. Bibcode:2014ApJ...794...59K. doi:10.1088/0004637X/794/1/59. S2CID 119040135.
 ^ Muncaster, Roger (1993). Alevel Physics (illustrated ed.). Nelson Thornes. p. 103. ISBN 9780748715848. Extract of page 103