Issue |
A&A
Volume 590, June 2016
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Article Number | A111 | |
Number of page(s) | 5 | |
Section | Planets and planetary systems | |
DOI | https://doi.org/10.1051/0004-6361/201628184 | |
Published online | 25 May 2016 |
Comet candidates among quasi-Hilda objects
1 Grupo de Ciencias Planetarias, Complejo Astronómico El Leoncito, UNLP, UNC, UNSJ, CONICET, Av. España 1512 sur, J5402DSP, San Juan, Argentina
e-mail: rgilhutton@casleo.gov.ar
2 Universidad Nacional de San Juan, J. I. de la Roza 590 oeste, 5400 Rivadavia, San Juan, Argentina
Received: 25 January 2016
Accepted: 9 April 2016
Aims. We present the results of a search for quasi-Hilda comets. We wanted to find objects that have recently arrived from the Centaur zone that could became active near the perihelion of their orbits.
Methods. Two hundred and seventy-seven objects from the ASTORB database were selected following a dynamical criteria to constrain the unstable quasi-Hilda region. These objects were integrated backward 50 000 yr in order to identify those that have recently arrived from the outer regions of the solar system.
Results. The backward integration showed that 11 objects could be Centaurs or transneptunian objects that ended their dynamical evolution as quasi-Hilda comets. The dynamical evolution of these objects from a statistical point of view was studied by computing the time-averaged distribution of a number of clones as a function of the aphelion and perihelion distances. All the candidates show a dynamical behavior that is expected for comets injected in the inner solar system from the Centaur or transneptunian regions and reaching the quasi-Hilda region.
Key words: minor planets, asteroids: general / comets: general
© ESO, 2016
1. Introduction
Comets are objects that have a nucleus of mixed ice and dust and are characterized by their activity when they reach the inner solar system. Among them, the Jupiter-family comets (JFCs) are a group of the cometary population with unstable orbits that are strongly affected by the gravitational perturbation of Jupiter. These objects have evolved from the transneptunian region and have reached the zone inside the Jupiter orbit after suffering the perturbations of the external planets during the period they behaved as Centaurs (Fernández 1980; Duncan et al. 1995; Levison & Duncan 1997).
One of the outermost dynamically stable zones of the asteroid belt is the Hilda region, where a group of asteroids is trapped in the 3:2 mean motion resonance with Jupiter (Schubart 1968, 1982, 1991; Nesvorný & Ferraz-Mello 1997; Ferraz-Mello et al. 1998). These objects have semimajor axes in the range 3.7 ≤ a ≤ 4.2 au, eccentricities e ≤ 0.3, and inclinations i ≤ 20°; the critical argument for the resonance librates around 0° (Zellner et al. 1985). During the last century, several JFCs have stayed in the Hilda region, but in an unstable 3:2 mean motion resonance with Jupiter. They have moved from outside of Jupiter’s orbit to inside the orbit, and some of them have undergone a temporary satellite capture by this planet (e.g., Carusi & Valsecchi 1979). These objects were called quasi-Hilda comets (QHCs) by Kresak (1979) and currently there are several comets in this region, including the pre-captured orbit of D/Shoemaker-Levy 9 (Chodas & Yeomans 1996).
The quasi-Hilda region is not only occupied by the QHCs, but it is also visited by Hilda objects escaping from the stable mean motion resonance. Di Sisto et al. (2005) performed numerical simulations to study the dynamical evolution of Hilda asteroids and found that 99% of the objects escaping from the resonance behave like JFCs, at least during the first 1000 yr. From the physical point of view, it is not easy to differentiate between escaped Hildas and QHCs because both populations are mainly D- and P-types (Fitzsimmons et al. 1994; Dahlgren & Lagerkvist 1995; Dahlgren et al. 1997, 1999; Jewitt 2002; Gil-Hutton & Brunini 2008); to distinguish comets from asteroids in the external zone of the main belt it is necessary to study the orbital evolution of these objects.
After the suggestion of Di Sisto et al. that escaped Hildas and asteroids in the quasi-Hilda region could show a dynamical behavior similar to that of JFCs, Toth (2006) gave an update of the QHCs in this zone, found new members of this cometary group, and identified 23 objects that could be dormant or extinct comet nuclei. Recently, Cheng & Ip (2013) have detected coma activity in the quasi-Hilda object 2000 YN30, presently known as 212P/NEAT, and have shown that 47 000 yr ago it could have been captured into a short-period orbit from a Centaur-like orbit as a result of a close encounter with Jupiter.
We searched for new QHCs candidates by looking for objects that have recently arrived in the quasi-Hilda region from the Centaur zone. In Sect. 2 we explain how the objects were selected and in Sect. 3 we present the results. Finally, in Sect. 4 we summarize our conclusions.
Quasi-Hilda objects coming from the outer solar system.
2. Selection criteria
We extracted from the ASTORB database1 the orbital elements for all the asteroids with semimajor axis in the range 3.7 ≤ a ≤ 4.2 au and an orbital arc spanned by the observations used in the orbit computation greater than 180 days. This first sample includes 2439 objects that fulfill the selection criteria.
Then, following Toth (2006) we define the quasi-Hilda region in Lagrangian elements where the orbits are unstable. The horizontal and vertical components of the eccentricity in Lagrangian elements are(1)where e and ϖ are the eccentricity and the longitude of perihelion of the object, respectively, and ϖJ is the longitude of the perihelion of Jupiter. The objects in the unstable quasi-Hilda zone are those that have elements outside a circle with center (k,h) ≃ (0.075,0) and radius ~0.24 (Toth 2006). This final sample contains 277 objects.
Since we are interested in objects that have recently arrived in the quasi-Hilda region, we integrate these 277 objects backward in time for 50 000 yr looking for changes in their semimajor axes that put them into the Centaur zone (a> 5.2 au). We used a Bulirsch-Stoer integrator with a step size of 1 day, and included all the planets from Mercury to Neptune. We found 11 objects that had a dynamical evolution showing they could recently have come from the outer solar system. They are listed in Table 1.
As an example, in Fig. 1 we show the evolution of the semimajor axis, and the perihelion and aphelion distances of (18916) 2000 OG44 during the 50 000 yr backward integration. This object jumps to a Jupiter’s external orbit at −10 200 yr changing its perihelion distance with the semimajor axis and semimajor axis with the aphelion distance. Later, it is captured in several mean-motion resonances and reaches the transneptunian belt at ≈−27 000 yr. The other objects have a similar behavior.
Fig. 1 Dynamical evolution of the semimajor axis (red line), perihelion (green), and aphelion (blue) distances for the object (18916) 2000 OG44 during the numerical integration. |
3. Results
The backward integration showed that these objects could be Centaurs or transneptunian objects that ended their dynamical evolution as QHCs, but owing to the uncertainties in their initial orbital elements the integration scheme could be affected by numerical effects that produce an incorrect final result. Then, it is important to study the dynamical evolution of these objects from a statistical point of view by integrating clones of each candidate and following the same procedure used to identify them and computing the time spent by each particle in different combinations of orbital elements to obtain statistical results of the dynamical behavior of the original object. One possibility for estimating the dynamical evolution of these QHCs is to obtain the time-averaged distribution of the clones as a function of the aphelion (Q) and perihelion (q) distances (e.g., Tiscareno & Malhotra 2003) dividing the coordinate plane into grids of 0.5 au × 0.5 au. Figures 2 and 3 show in a gray scale the time spent by 100 clones of each candidate per 0.25 au2 in the (Q,q) plane during a backward integration of 50 000 yr, which could be interpreted as the probability of finding a clone in a certain point of the grid in that period.
Fig. 2 Probability distribution per square au in (Q,q) space for the clones of (18916)2000 OG44, (371837)2007 VM318, 2001 QG288, 2002 UP36, 2003 UR267, and 2006 XL5. Continuous black lines indicate eccentricities of 0.0, 0.3, and 0.6, and dashed lines indicate semimajor axes of 5.2 and 9.5 au. |
Fig. 3 Probability distribution per square au in (Q,q) space for the clones of 2007 UC9, 2008 GO98, 2009 KF37, 2009 SR143, and 2013 QR90. Continuous black lines indicate eccentricities of 0.0, 0.3, and 0.6, and dashed lines indicate semimajor axes of 5.2 and 9.5 au. |
In all the cases shown in Figs. 2 and 3 it is possible to observe a strong influence of Jupiter and Saturn on the dynamical evolution of these objects indicated by horizontal strips with q almost fixed at ~5 au and, to a lesser extent, ~10 au. These two patterns are produced by the gravitational scattering of the particles by these planets to larger aphelion distances. This behavior is what would be expected of comets injected in the inner solar system from the Centaur or transneptunian regions and is similar to that found by Tiscareno & Malhotra (2003) for the Centaur population, indicating that the candidates found could have originated in the outer solar system and reached the quasi-Hilda region by the gravitational scattering of the giant planets.
On the other hand, the probability distributions shown in Figs. 2 and 3 indicate that almost all the candidates could visit the region where q< 1 au. If these objects were in fact comets they could be affected by strong activity due to the outgassing produced by their perihelion passage and they could become dormant or inactive comets. Fernández (1984) found that the average physical lifetime for short-period comets with q ~ 1 au is ≈500–1000 revolutions or ≈4–8 × 103 yr for objects in an orbit with a semimajor axis of ~4 au. Since this period is not very long and it is also an order of magnitude shorter that the total integration time used, it is important to test if any one of the comet candidates remained in an orbit with q< 1 au for at least ≈103 yr since this could indicate that it has a high probability of becoming inactive. The average time that the clones of the comet candidates stay in orbits with q< 1 au is 429 ± 21 yr for (18916)2000 OG44, 162 ± 13 yr for (371837)2007 VM318, 189 ± 14 yr for 2001 QG288, 349 ± 19 yr for 2002 UP36, 733 ± 27 yr for 2003 UR267, 93 ± 10 yr for 2006 XL5, 174 ± 13 yr for 2007 UC9, 387 ± 20 yr for 2008 GO98, 104 ± 10 yr for 2009 KF37, 494 ± 22 yr for 2009 SR143, and <1 ± 0.05 yr for 2013 QR90. Thus, the best candidates that will show cometary activity in the near future are (371837)2007 VM318, 2013 QR90, 2006 XL5, 2009 KF37, 2007 UC9, and 2001 QG288.
The best way to test whether these objects are comets is to observe them near the perihelion of their orbits and to search for cometary activity. They will be difficult to observe because these objects are very small: assuming a 4% albedo and the absolute magnitudes listed in Table 1, their diameters are between 9.6 and 2.8 km. Three of our best candidates (2007 VM318, 2013 QR90, 2006 XL5) are now near the aphelion of their orbits: 2009 KF37 had its perihelion passage in July 2015, and the other two, 2007 UC9 and 2001 QG288, will be at perihelion in September 2017 and February 2018, respectively. The other five objects in our list will be at perihelion during 2016 (2000 OG44, 2008 GO98, and 2009 SR143) and 2018 (2002 UP36 and 2003 UR267), but the simulations show a high probability that they spent some time in orbits with q< 1 and therefore they have already exhausted their volatile material.
4. Conclusions
The dynamical evolution of 277 objects with unstable orbits in the quasi-Hilda region were analyzed to search for those that have arrived in the last 50 000 yr and could have their origin in the Centaur region. These objects were originally selected from the ASTORB database considering asteroids with semimajor axes in the range 3.7 ≤ a ≤ 4.2 au, orbital arcs spanned by the observations greater than 180 days, and Lagrangian elements indicating that their orbits are unstable (Toth 2006).
The orbits of these objects were integrated backward in time to look for changes that put them into the Centaur zone; there are 11 candidates that had a dynamical evolution showing they could have recently come from the outer solar system.
The analysis indicates that almost all the candidates could visit the inner region of the solar system and five of them could be affected by strong activity, occasionally becoming dormant or inactive comets. The remaining five candidates have a good chance of still being active and will pass the perihelion of their orbits during the following 2–3 yr, offering a good opportunity to detect activity on them.
Acknowledgments
The authors thank the referee, J. A. Fernández, for his useful review, which led to an improvement of the paper. R.G.H. gratefully acknowledges financial support by CONICET through PIP 114-201101-00358.
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All Tables
All Figures
Fig. 1 Dynamical evolution of the semimajor axis (red line), perihelion (green), and aphelion (blue) distances for the object (18916) 2000 OG44 during the numerical integration. |
|
In the text |
Fig. 2 Probability distribution per square au in (Q,q) space for the clones of (18916)2000 OG44, (371837)2007 VM318, 2001 QG288, 2002 UP36, 2003 UR267, and 2006 XL5. Continuous black lines indicate eccentricities of 0.0, 0.3, and 0.6, and dashed lines indicate semimajor axes of 5.2 and 9.5 au. |
|
In the text |
Fig. 3 Probability distribution per square au in (Q,q) space for the clones of 2007 UC9, 2008 GO98, 2009 KF37, 2009 SR143, and 2013 QR90. Continuous black lines indicate eccentricities of 0.0, 0.3, and 0.6, and dashed lines indicate semimajor axes of 5.2 and 9.5 au. |
|
In the text |
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