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Hill sphere
Hill sphere
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In sectional/side view, a two-dimensional representation of the three-dimensional concept of the Hill sphere, here showing the Earth's "gravity well" (gravitational potential of Earth, blue line), the same for the Moon (red line) and their combined potential (black thick line). Point P is the force free spot, where gravitational forces of Earth and Moon cancel. The sizes of Earth and Moon are in the proportion, but distances and energies are not to scale.

The Hill sphere is a common model for the calculation of a gravitational sphere of influence. It is the most commonly used model to calculate the spatial extent of gravitational influence of an astronomical body (m) in which it dominates over the gravitational influence of other bodies, particularly a primary (M).[1] It is sometimes confused with other models of gravitational influence, such as the Laplace sphere[1] or the Roche sphere, the latter of which causes confusion with the Roche limit.[2][3] It was defined by the American astronomer George William Hill, based on the work of the French astronomer Édouard Roche.[not verified in body]

To be retained by a more gravitationally attracting astrophysical object—a planet by a more massive star, a moon by a more massive planet—the less massive body must have an orbit that lies within the gravitational potential represented by the more massive body's Hill sphere.[not verified in body] That moon would, in turn, have a Hill sphere of its own, and any object within that distance would tend to become a satellite of the moon, rather than of the planet itself.[not verified in body]

A contour plot of the effective gravitational potential of a two-body system, here, the Sun and Earth, indicating the five Lagrange points.[clarification needed][citation needed]

One simple view of the extent of the Solar System is that it is bounded by the Hill sphere of the Sun (engendered by the Sun's interaction with the galactic nucleus or other more massive stars).[4][verification needed] A more complex example is the one at right, the Earth's Hill sphere, which extends between the Lagrange points L1 and L2,[clarification needed] which lie along the line of centers of the Earth and the more massive Sun.[not verified in body] The gravitational influence of the less massive body is least in that direction, and so it acts as the limiting factor for the size of the Hill sphere;[clarification needed] beyond that distance, a third object in orbit around the Earth would spend at least part of its orbit outside the Hill sphere, and would be progressively perturbed by the tidal forces of the more massive body, the Sun, eventually ending up orbiting the latter.[not verified in body]

For two massive bodies with gravitational potentials and any given energy of a third object of negligible mass interacting with them, one can define a zero-velocity surface in space which cannot be passed, the contour of the Jacobi integral.[not verified in body] When the object's energy is low, the zero-velocity surface completely surrounds the less massive body (of this restricted three-body system), which means the third object cannot escape; at higher energy, there will be one or more gaps or bottlenecks by which the third object may escape the less massive body and go into orbit around the more massive one.[not verified in body] If the energy is at the border between these two cases, then the third object cannot escape, but the zero-velocity surface confining it touches a larger zero-velocity surface around the less massive body[verification needed] at one of the nearby Lagrange points, forming a cone-like point there.[clarification needed][not verified in body] At the opposite side of the less massive body, the zero-velocity surface gets close to the other Lagrange point.[not verified in body]

Definition

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The Hill radius or sphere (the latter defined by the former radius[citation needed]) has been described as "the region around a planetary body where its own gravity (compared to that of the Sun or other nearby bodies) is the dominant force in attracting satellites," both natural and artificial.[5][better source needed]

As described by de Pater and Lissauer, all bodies within a system such as the Sun's Solar System "feel the gravitational force of one another", and while the motions of just two gravitationally interacting bodies—constituting a "two-body problem"—are "completely integrable ([meaning]...there exists one independent integral or constraint per degree of freedom)" and thus an exact, analytic solution, the interactions of three (or more) such bodies "cannot be deduced analytically", requiring instead solutions by numerical integration, when possible.[6]: p.26  This is the case, unless the negligible mass of one of the three bodies allows approximation of the system as a two-body problem, known formally as a "restricted three-body problem".[6]: p.26 

For such two- or restricted three-body problems as its simplest examples—e.g., one more massive primary astrophysical body, mass of , and a less massive secondary body, mass of —the concept of a Hill radius or sphere is of the approximate limit to the secondary mass's "gravitational dominance",[6] a limit defined by "the extent" of its Hill sphere, which is represented mathematically as follows:[6]: p.29 [7]

,

where, in this representation, semi-major axis "" can be understood as the "instantaneous heliocentric distance" between the two masses (elsewhere abbreviated rp).[6]: p.29 [7]

More generally, if the less massive body, , orbits a more massive body, (e.g., as a planet orbiting around the Sun), and has a semi-major axis , and an eccentricity of , then the Hill radius or sphere, of the less massive body, calculated at the pericenter, is approximately:[8][non-primary source needed][better source needed]

When eccentricity is negligible (the most favourable case for orbital stability), this expression reduces to the one presented above.[citation needed]

Example and derivation

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A schematic, not-to-scale representation of Hill spheres (as 2D radii) and Roche limits of each body of the Sun-Earth-Moon system. The actual Hill radius for the Moon is on the order of 60,000 km (i.e., extending less than one-sixth the distance of the 378,000 km between the Moon and the Earth).[9]

In the Earth-Sun example, the Earth (5.97×1024 kg) orbits the Sun (1.99×1030 kg) at a distance of 149.6 million km, or one astronomical unit (AU). The Hill sphere for Earth thus extends out to about 1.5 million km (0.01 AU). The Moon's orbit, at a distance of 0.384 million km from Earth, is comfortably within the gravitational sphere of influence of Earth and it is therefore not at risk of being pulled into an independent orbit around the Sun.

The earlier eccentricity-ignoring formula can be re-stated as follows:

, or ,

where M is the sum of the interacting masses.

Derivation

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The expression for the Hill radius can be found by equating gravitational and centrifugal forces acting on a test particle (of mass much smaller than ) orbiting the secondary body. Assume that the distance between masses and is , and that the test particle is orbiting at a distance from the secondary. When the test particle is on the line connecting the primary and the secondary body, the force balance requires that

where is the gravitational constant and is the (Keplerian) angular velocity of the secondary about the primary (assuming that ). The above equation can also be written as

which, through a binomial expansion to leading order in , can be written as

Hence, the relation stated above

If the orbit of the secondary about the primary is elliptical, the Hill radius is maximum at the apocenter, where is largest, and minimum at the pericenter of the orbit. Therefore, for purposes of stability of test particles (for example, of small satellites), the Hill radius at the pericenter distance needs to be considered.

To leading order in , the Hill radius above also represents the distance of the Lagrangian point L1 from the secondary.

Regions of stability

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The Hill sphere is only an approximation, and other forces (such as radiation pressure or the Yarkovsky effect) can eventually perturb an object out of the sphere.[citation needed] As stated, the satellite (third mass) should be small enough that its gravity contributes negligibly.[6]: p.26ff 

The region of stability for retrograde orbits at a large distance from the primary is larger than the region for prograde orbits at a large distance from the primary. This was thought to explain the preponderance of retrograde moons around Jupiter; however, Saturn has a more even mix of retrograde/prograde moons so the reasons are more complicated.[10] In a two-planet system, the mutual Hill radius of the two planets must exceed to be stable. Multi-planet systems of three or more with semi-major-axis differences of less than ten mutual Hill radii are always unstable. This is due to the loss of angular momentum due to perturbations by a third planet.[11]

Further examples

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It is possible for a Hill sphere to be so small that it is impossible to maintain an orbit around a body. For example, an astronaut could not have orbited the 104 ton Space Shuttle at an orbit 300 km above the Earth, because a 104-ton object at that altitude has a Hill sphere of only 120 cm in radius, much smaller than a Space Shuttle. A sphere of this size and mass would be denser than lead, and indeed, in low Earth orbit, a spherical body must be more dense than lead in order to fit inside its own Hill sphere, or else it will be incapable of supporting an orbit. Satellites further out in geostationary orbit, however, would only need to be more than 6% of the density of water to fit inside their own Hill sphere.[citation needed]

Within the Solar System, the planet with the largest Hill radius is Neptune, with 116 million km, or 0.775 au; its great distance from the Sun amply compensates for its small mass relative to Jupiter (whose own Hill radius measures 53 million km). An asteroid from the asteroid belt will have a Hill sphere that can reach 220,000 km (for 1 Ceres), diminishing rapidly with decreasing mass. The Hill sphere of 66391 Moshup, a Mercury-crossing asteroid that has a moon (named Squannit), measures 22 km in radius.[12]

A typical extrasolar "hot Jupiter", HD 209458 b,[13] has a Hill sphere radius of 593,000 km, about eight times its physical radius of approx 71,000 km. Even the smallest close-in extrasolar planet, CoRoT-7b,[14] still has a Hill sphere radius (61,000 km), six times its physical radius (approx 10,000 km). Therefore, these planets could have small moons close in, although not within their respective Roche limits.[citation needed]

Hill spheres for the solar system

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The following table and logarithmic plot show the radius of the Hill spheres of some bodies of the Solar System calculated with the first formula stated above (including orbital eccentricity), using values obtained from the JPL DE405 ephemeris and from the NASA Solar System Exploration website.[15]

Radius of the Hill spheres of some bodies of the Solar System
Body Million km au Body radii Arcminutes[note 1] Farthest moon (au)
Mercury 0.1753 0.0012 71.9 10.7
Venus 1.0042 0.0067 165.9 31.8
Earth 1.4714 0.0098 230.7 33.7 0.00257
Mars 0.9827 0.0066 289.3 14.9 0.00016
Jupiter 50.5736 0.3381 707.4 223.2 0.1662
Saturn 61.6340 0.4120 1022.7 147.8 0.1785
Uranus 66.7831 0.4464 2613.1 80.0 0.1366
Neptune 115.0307 0.7689 4644.6 87.9 0.3360
Ceres 0.2048 0.0014 433.0 1.7
Pluto 5.9921 0.0401 5048.1 3.5 0.00043
Eris 8.1176 0.0543 6979.9 2.7 0.00025
Logarithmic plot of the Hill radii (in km) for the bodies of the solar system

See also

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Explanatory notes

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References

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Further reading

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Revisions and contributorsEdit on WikipediaRead on Wikipedia
from Grokipedia
The Hill sphere, also known as the Hill radius, is a gravitational region surrounding a secondary celestial body (such as a or ) that orbits a more massive (such as a star), within which the secondary's dominates perturbations from the primary, enabling stable for satellites or other objects around the secondary. This concept defines the approximate boundary beyond which tidal forces from the primary overwhelm the secondary's gravitational hold, causing objects to be captured by or perturbed toward the primary's orbit. The Hill sphere was first formalized by American astronomer George William Hill in his 1878 paper "Researches in the ," where he analyzed the stability of lunar motion under solar perturbations as part of broader work on the . Hill's derivation built on earlier ideas by French astronomer Édouard , who in 1847–1850 explored similar gravitational limits in the context of satellite disruption, though the term "Hill sphere" specifically honors Hill's mathematical treatment. For a secondary body in a around the primary, the radius rHr_H of the Hill sphere is approximated by the formula rHa(m3M)1/3r_H \approx a \left( \frac{m}{3M} \right)^{1/3}, where aa is the semi-major axis of the secondary's orbit, mm is the mass of the secondary, and MM is the mass of the primary; for eccentric orbits, the formula adjusts to rHa(1e)(m3M)1/3r_H \approx a (1 - e) \left( \frac{m}{3M} \right)^{1/3}, with ee as the eccentricity. This approximation arises from equating the due to the secondary with the from the primary at the sphere's boundary. In the Solar System, Hill spheres determine the stability zones for natural satellites and artificial ; for example, Earth's Hill sphere has a radius of approximately 1.5 million kilometers (0.01 AU), enclosing the Moon's at about 384,000 km and allowing geostationary satellites to remain bound despite solar influences. For , the largest Hill sphere among planets at roughly 51 million km (0.34 AU), it accommodates the planet's extensive and irregular satellites, while smaller bodies like Mars have a modest radius of about 1 million km (0.007 AU), limiting stable outer satellites. Beyond the Solar System, the Hill sphere is crucial for studying exoplanetary systems, assessing the potential for moons around giant planets and the dynamical stability of multi-planet architectures against mutual perturbations.

Conceptual Foundations

Definition

The Hill sphere, also known as the gravitational sphere of influence, represents the region surrounding a secondary celestial body, such as a planet, within which its gravitational attraction on a test particle dominates over that of the primary body, typically a much more massive central star. This boundary delineates the approximate extent to which the secondary body can stably retain satellites or debris, beyond which perturbations from the primary's gravity become significant enough to disrupt orbits. In the context of a two-body system where the secondary orbits the primary, the Hill sphere defines the effective zone of control for the secondary's gravitational field. Although the Hill sphere is often approximated as spherical for analytical and practical purposes in , its actual shape in the circular restricted is more complex, resembling a teardrop or slightly form due to the tidal influences and the positions of the collinear Lagrange points L1 and L2, which mark the inner and outer boundaries along the line connecting the two bodies. This approximation as a sphere simplifies calculations while capturing the essential dynamics of gravitational dominance. The key parameters influencing the Hill sphere include the semi-major axis aa of the secondary's around the primary, the mm of the secondary, and the MM of the primary, with the assumption that mMm \ll M to ensure the primary's overwhelming influence. The Hill sphere was developed by American astronomer George William Hill in his 1878 paper "Researches in the ," where he analyzed the stability of the 's orbit under solar perturbations, building on earlier ideas by French astronomer Édouard Roche, who in 1847–1850 explored similar gravitational limits in the context of satellite disruption.

Physical Significance

The Hill sphere delineates the region around a secondary body, such as a or , where its gravitational attraction dominates over that of a more massive primary body, enabling the retention of smaller objects like satellites, , or debris in stable orbits relative to the secondary. Objects within this sphere experience perturbations from the primary that are weaker than the secondary's pull, allowing for long-term orbital stability without immediate capture by the primary; for instance, the major satellites of and Saturn occupy prograde, low-inclination orbits deeply embedded within their host planets' Hill spheres, preventing ejection during planetary migrations. In extrasolar systems, dust grains or irregular satellites that remain confined to the Hill sphere form circumplanetary debris disks, while those escaping contribute to broader circumstellar material, highlighting the sphere's role in material retention and loss dynamics. In space mission design, the Hill sphere, often equated with the sphere of influence, simplifies the analysis of trajectories in multi-body environments by approximating motion as a series of Keplerian orbits patched at the boundaries where one body's dominance transitions to another. This patched conic method divides interplanetary paths into heliocentric segments outside a planet's Hill sphere and planetocentric segments inside, providing an efficient initial approximation for in missions like Voyager, where low-thrust or high-velocity encounters require accounting for gravitational switches at these radii. For lunar or interplanetary transfers, such as Earth-to-Moon trajectories, the Hill sphere defines safe parking orbits and transfer zones, ensuring avoid unintended captures by the primary while optimizing fuel for insertions or escapes through energy manifolds near points. Beyond mission planning, the Hill sphere plays a pivotal role in astrophysical processes like planetary formation, where accrete planetesimals and gas primarily from within their Hill spheres, limiting growth to material gravitationally bound despite disk-wide dispersal. During the oligarchic phase of protoplanet assembly, the Hill sphere's size determines accretion efficiency, as planetesimals entering this region via gas drag or gravitational capture contribute to core buildup, with enhanced rates for atmospheres that dissipate and promote retention. In systems, the Hill radius around circumbinary planets expands for wide orbits, facilitating stability by providing larger zones shielded from stellar perturbations, potentially extending planetary lifetimes through tidal synchronization. For exomoons, orbits must lie within a reduced Hill radius—scaled by stability factors like 0.49 for prograde cases—to resist stellar torques, influencing detectability in systems with strong perturbers. Despite its utility, the Hill sphere serves as an approximation that overlooks higher-order effects, such as relativistic corrections in strong gravitational fields or perturbations from non-spherical primary bodies, which can induce secular variations in like rates. For planets like , the introduces J₂ zonal harmonics in the , causing deviations from spherical symmetry that the basic Hill model does not capture, leading to inaccuracies in close-in orbits or long-term predictions. These limitations necessitate refined models incorporating multipole expansions or full n-body simulations for precise applications in dense or asymmetric systems.

Mathematical Derivation

Derivation Process

The derivation of the Hill sphere begins with the setup of the circular restricted (CRTBP), which models the motion of a of negligible mass in the of two more massive bodies, referred to as the primary (mass MM) and secondary (mass mm), assuming mMm \ll M. In this framework, the primary is positioned at the origin, while the secondary orbits the primary in a circular path at a fixed aa, with the test particle's mass being insignificant enough not to perturb the orbits of the two primaries. The system is analyzed in a co-rotating reference frame that rotates with the ω\omega of the secondary's orbit, where ω2=GM/a3\omega^2 = GM / a^3, ensuring the primaries remain fixed relative to the frame. This setup, originally developed in the context of lunar motion, allows for the examination of the test particle's dynamics under combined gravitational and centrifugal influences. In the co-rotating frame, the equations of motion for the test particle incorporate fictitious forces due to the frame's rotation. The effective potential Φ\Phi governing the motion is given by Φ=GMrGmra12ω2ρ2,\Phi = -\frac{GM}{r} - \frac{Gm}{| \vec{r} - \vec{a} |} - \frac{1}{2} \omega^2 \rho^2,
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