![]() | ![]() |
Astron. Astrophys. 354, 1091-1100 (2000) 3. Numerical setupThe equations of motion for (1868) Thersites, as well as for a distribution of fictitious asteroids, were integrated for 50 Myrs using the Lie integration method (Lichtenegger, 1984; Hanslmeier & Dvorak, 1984). The dynamical model used in this integration was the Outer Solar System (OSS), consisting of the Sun and the four giant planets (Jupiter-Saturn-Uranus-Neptune) gravitationally interacting. The mass of the Sun was increased by the sum of the masses of the inner planets 2. Relativistic corrections were not taken into account. Our initial distribution can be separated into a group of Thersites' `clones' (C-group) and a group of `neighbors' (N-group). The N-group is composed of 16 fictitious asteroids whose
initial conditions were taken by adding small deviations
Table 1. Classification of the orbits. A `name' is given to each orbit in the first column. The initial deviation from the elements of (1868) Thersites is given in the second column. The third column labels the orbit, according to the classification made in Sect. 3. The escape time, Since Thersites lies on a chaotic orbit, it is only natural to
expect that the results of two numerical integrations conducted in two
different machines will not be the same; this is certainly true for
integration times much longer than the Lyapunov time,
![]() ![]() ![]() ![]() © European Southern Observatory (ESO) 2000 Online publication: February 25, 2000 ![]() |