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Three-body problem

Physics problem related to laws of motion and gravity

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Unlike the two-body problem, the three-body problem has no general closed-form analytic solution. The differential equations that govern the motions of three gravitating bodies are not integrable and cannot be solved to give explicit formulas for the positions of the bodies as a function of time. For most initial conditions, the dynamical system for three orbiting bodies is chaotic, and the only way to predict their motions is to estimate them using numerical methods.

The three-body problem is a special case of the n-body problem. Historically, the first specific three-body problem to receive extended study was the one involving the Earth, the Moon, and the Sun. In an extended modern sense, a three-body problem is any problem in classical mechanics or quantum mechanics that models the motion of three particles.

Mathematical description

The mathematical statement of the three-body problem can be given in terms of the Newtonian equations of motion for vector positions ri=(xi,yi,zi) of three gravitationally interacting bodies with masses mi: r¨1=−Gm2(r1−r2)|r1−r2|3−Gm3(r1−r3)|r1−r3|3,r¨2=−Gm3(r2−r3)|r2−r3|3−Gm1(r2−r1)|r2−r1|3,r¨3=−Gm1(r3−r1)|r3−r1|3−Gm2(r3−r2)|r3−r2|3. where G is the gravitational constant.

As astronomer Juhan Frank describes, "These three second-order vector differential equations are equivalent to 18 first order scalar differential equations." As June Barrow-Green notes with regard to an alternative presentation, if Pi represent three particles with masses mi, distances PiPj=rij, and coordinates qij (i,j=1,2,3)in an inertial coordinate system ... the problem is described by nine second-order differential equations.

The problem can also be stated equivalently in the Hamiltonian formalism, in which case it is described by a set of 18 first-order differential equations, one for each component of the positions ri and momenta pi: dridt=∂H∂pi,dpidt=−∂H∂ri, where H is the Hamiltonian: H=−Gm1m2|r1−r2|−Gm2m3|r3−r2|−Gm3m1|r3−r1|+|p1|22m1+|p2|22m2+|p3|22m3.

In this case, H is simply the total energy of the system, gravitational plus kinetic.

Restricted three-body problem

In the restricted three-body problem formulation, in the description of Barrow-Green,

two... bodies revolve around their centre of mass in circular orbits under the influence of their mutual gravitational attraction, and... form a two-body system... [whose] motion is known. A third body (generally known as a planetoid), assumed massless with respect to the other two, moves in the plane defined by the two revolving bodies and, while being gravitationally influenced by them, exerts no influence of its own.

Per Barrow-Green, "[t]he problem is then to ascertain the motion of the third body."

The restricted three-body problem is easier to analyze theoretically than the full problem. It is of practical interest as well since it accurately describes many real-world problems, the most important example being the Earth–Moon–Sun system. For these reasons, it has occupied an important role in the historical development of the three-body problem.

The restricted 3-body problem has a 4-dimensional phase space, but only one conserved quantity, the Jacobi integral. It was shown by Heinrich Bruns that there are no more algebraic conserved quantities, and by Henri Poincaré in 1889 that there are no more analytic conserved quantities. Therefore, since the dimension of the phase space is larger than the number of constants of motion, the system is not exactly solvable; in fact, it is chaotic.

Depending on the value of the Jacobi integral, a body initially orbiting the larger mass may be able to be captured by the secondary mass or be ejected via Lagrange points L2 or L3.

A variant of this problem, where the two large bodies both exert radiation pressure, results in the addition of four additional equilibrium points in addition to the five classical Lagrange points.

More recent work on the circular restricted problem has drawn on symplectic geometry and contact geometry. A 2025 survey by Agustín Moreno describes the use of global surfaces of section and related geometric methods, and their connection with the design of spacecraft trajectories. Such methods also yield existence results: for energies slightly above the first critical value, Jungsoo Kang and Kevin Ruck used Rabinowitz Floer homology to show that the planar problem admits either a periodic symmetric collision orbit or infinitely many symmetric consecutive-collision orbits, and that for generic mass ratios and energies at least two geometrically distinct symmetric consecutive-collision orbits exist for each primary.

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