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Astronomy Principles and Practice Fourth Edition.pdf

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14.3 General properties of the many-body problem<br />

General perturbation theories 187<br />

If the masses of the planets were vanishingly small compared to the Sun’s mass, then the orbit of any<br />

planet would be unchanging <strong>and</strong> the six elements would be constant. Indeed, Kepler’s three laws are<br />

the solution to the many-body problem in such a case. But the planetary masses are by no means<br />

negligible <strong>and</strong>, in the case of comets, near approaches to planets can occur so that, in general, the<br />

problem is much more complicated.<br />

In the past three centuries, it has inspired (<strong>and</strong> frustrated!) many eminent astronomers <strong>and</strong><br />

mathematicians. It is perhaps not obvious that even the three-body problem is of a much higher degree<br />

of complexity than the two-body problem. But if we consider that each body is subject to a complicated<br />

variable gravitational field due to its attraction by the other two, such that close encounters with either<br />

may be brought about, the result of each near-collision being an entirely new type of orbit, we see that<br />

it would require a general formula of unimaginable complexity to describe all the consequences of all<br />

such encounters.<br />

In point of fact, several general <strong>and</strong> useful statements may be made concerning the many-body<br />

problem <strong>and</strong> these were proved quite early on in its history. They were known to Euler (1707–83) but<br />

since then no further overall properties have been discovered or are likely to be.<br />

The statements follow from the only known integrals of the differential equations <strong>and</strong> refer to the<br />

centre of mass of the system, the total energy of the system <strong>and</strong> its total angular momentum. Without<br />

saying anything about the trajectories of the individual particles, the following statements can be made:<br />

(a) The centre of mass of the system moves through space with constant velocity, i.e. it moves in a<br />

straight line at a fixed speed.<br />

(b) The total energy of the system (the sum of all the kinetic energies <strong>and</strong> potential energy) is constant.<br />

Thus, although there is a continual trade-off among the members in kinetic energy <strong>and</strong> potential<br />

energy, the total energy is unaffected.<br />

(c) The total angular momentum of the system is constant.<br />

In addition to these properties, particular solutions of the three-body problem that exist when<br />

certain relationships hold among the velocities <strong>and</strong> mutual distances of the particles were found by<br />

Lagrange. He showed that if the three bodies occupy the vertices of an equilateral triangle, their speeds<br />

being equal in magnitude <strong>and</strong> inclined at the same angle to each mutual radius vector, they will remain<br />

in an equilateral triangle formation, though the triangle will rotate <strong>and</strong> may change its size. Lagrange<br />

also showed that if the three bodies are placed on a straight line at mutual distances depending upon<br />

the ratios of their masses, they will remain on that line, though it will rotate. Although these equilateral<br />

triangle <strong>and</strong> collinear solutions of the three-body problem were thought to be of theoretical interest only<br />

at the time of their presentation, it was subsequently discovered that they occur in the Solar System.<br />

Two groups of asteroids, called the Trojans, revolve about the Sun in Jupiter’s orbit, so that their<br />

periods of revolution equal that of Jupiter. In their orbit about the Sun, they oscillate about one or<br />

other of the two points 60 ◦ ahead or behind Jupiter’s heliocentric position. Among Saturn’s moons,<br />

Telesto <strong>and</strong> Calypso remain 60 ◦ ahead or behind the more massive Tethys while Helene, in Dione’s<br />

orbit, keeps 60 ◦ ahead of Dione.<br />

14.4 General perturbation theories<br />

It has been seen that, because the planets’ mutual attractions are so much smaller than the Sun’s<br />

attraction upon them, the planets’ orbits, to a high degree of approximation, are ellipses about the<br />

Sun. This two-body approximation has been the starting point in many attempts to obtain theories of<br />

the planets’ motions. The two-body orbit of a planet about the Sun is supposed to vary in size, shape<br />

<strong>and</strong> orientation as if it were a soft plasticine ring moulded by the spectral fingers of the other planets’<br />

gravitational fields.

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