In addition to the previous estimates, it is also interesting to study the dynamic evolution of our TCB orbits on a long time scale. This consents us to study the dynamic mechanisms at work, and to analyse whether the dynamic path that, according to the previous section, they took to achieve these orbits is actually completely lost as a consequence of the chaotic nature of planet-crossing orbits.
We have thus integrated the orbits of 20 bodies on the basis of their highest probability of coming from one of the four previous sources. The integrations have been carried out with an integrator based on the Bulirsch-Stoer technique (Stoer & Bulirsch 1980), and optimised for dealing accurately with planetary close encounters (cf. Michel et al. 1996). The dynamic model included all the planets except Pluto and Mercury, the mass of the latter being added to that of the Sun. The integration interval spanned at least 10 Myr backward and 10 Myr forward in time, resulting in a total timespan of 20 Myr (which was extended in some cases).
As is well known, the results of long-term integrations of planet-crossing orbits cannot be seen as deterministic reconstructions or predictions of the real evolutions. Nevertheless, they are very useful in providing qualitative and/or statistical information on the most frequent orbital behaviours, on the effectiveness of various dynamic mechanisms and the corresponding lifetimes. Moreover integrating backward and forward in time merely provides a simple way of doubling the size of the sample and thus of improving the statistics; we point out that backward integrations cannot provide information on the sources of the bodies either individually or statistically.
We have considered 4 orbits with probability P1 in the range between 0.54 and 0.60. The most frequent end-state of particles on these initial orbits is an impact with the Sun (4 in the backward integration and 3 in the forward one). Only one body has a semi-major axis, which becomes greater than 100 AU. The median lifetime of this sample is about 2 Myr, while the mean lifetime is of the order of 3 Myr. Most bodies (7/8) collide with the Sun while they are located in a mean motion resonance (5are in the 3:1 resonance - see e.g. Fig. 8 - and 2 in the 8:3 one).
During the integration time all the orbits are temporarily located in the 3:1
mean motion resonance, and 6 orbits are affected by secular resonance
with both the inner and outer planets. Note that, although they are based on a
limited sample of integrated orbits, our results agree with previous studies
(Gladman et al. 1997; Migliorini et al. 1998; Michel et al. 2000a).
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Figure 8: Time evolution (backward and forward) of the semi-major axis a (AU), eccentricity and inclination of a TCB orbit which has the greatest probability of coming from the 3:1 source. |
We have integrated 4 particles with probability P2 in the range 0.81
and 0.90. All the bodies have a semi-major axis smaller than 1.2 AU,
an eccentricity smaller than 0.23 and a small inclination
.
The 8 evolutions corresponding to the integrations both backward and forward in time, are dominated by close approaches with the terrestrial planets (Fig. 9). We found that only 2 bodies have a collision with Venus in the forward integration, at +4.6 Myr and +6.2 Myr, respectively, while up to 10 Myr backward all the bodies survive. Thus the median lifetime and the mean lifetime are larger than 10 Myr, as previously found by Michel et al. (2000b).
Since the 5 bodies have large eccentricities, a small increase in e is
sufficient to induce a collision with the Sun. All the end-states backward
and forward in time are solar collisions, the median and mean lifetimes being
about 2 Myr and 1.84 Myr, respectively. 8 solar
collisions occur while the bodies are located either in the region
where the secular resonances ,
and
overlap (e.g.
Fig. 10) or in the overlapping region of the
and
resonances. Only one impact into the Sun happens while the orbit is located in
the 3:1 mean motion resonance and the last one results from the
effect of the 5:1 mean motion resonance with Jupiter. As previously found
semianalytically by Michel & Froeschlé (1997), our numerical results show
that in the region a < 2 AU, the secular resonances with both the inner and
outer planets are effective dynamic mechanisms.
Over the 14 evolutions, 5 Sun-grazing were recorded (3 in the forward
integrations and 2 backward), 5 reached a semi-major axis larger than
100 AU, and the last 4 are ejected from the Solar System (the
eccentricities e > 1.0). We notice that the solar collisions always occur
when the bodies are inside the chaotic region of the 3:2 mean motion
resonance with Jupiter and also in the Kozai resonance with
librating
about
or
(Fig. 11).
Copyright ESO 2001