scholarly journals Surface composition and dynamical evolution of two retrograde objects in the outer solar system: 2008 YB3and 2005 VD

2013 ◽  
Vol 550 ◽  
pp. A13 ◽  
Author(s):  
N. Pinilla-Alonso ◽  
A. Alvarez-Candal ◽  
M. D. Melita ◽  
V. Lorenzi ◽  
J. Licandro ◽  
...  
2006 ◽  
Vol 2 (S236) ◽  
pp. 31-34
Author(s):  
E. L. Kiseleva ◽  
V. V. Emel'yanenko

AbstractThe dynamical interrelation between resonant trans-Neptunian objects and short-period comets is studied. Initial orbits of resonant objects are based on computations in the model of the outward transport of objects during Neptune's migration in the early history of the outer Solar system. The dynamical evolution of this population is investigated for 4.5 Gyr, using a symplectic integrator. Our calculations show that resonant trans-Neptunian objects give a substantial contribution to the planetary region. We have estimated that the relative fraction of objects captured per year from the 2/3 resonance to Jupiter-family orbits with perihelion distances q<2.5 AU is 0.4×10−10 near the present epoch.


2019 ◽  
Vol 488 (3) ◽  
pp. 3035-3044 ◽  
Author(s):  
Alvaro Alvarez-Candal ◽  
Carmen Ayala-Loera ◽  
Ricardo Gil-Hutton ◽  
José Luis Ortiz ◽  
Pablo Santos-Sanz ◽  
...  

ABSTRACT The study of the visible colours of the trans-Neptunian objects opened a discussion almost 20 yr ago which, in spite of the increase in the amount of available data, seems far from subside. Visible colours impose constraints to the current theories of the early dynamical evolution of the Solar system such as the environment of formation, initial surface composition, and how (if) they were scattered to regions closer to the inner planets. In this paper, we present an updated version of our data base of absolute colours and relative phase coefficients for 117 objects. We define the absolute colours as the difference of the absolute magnitudes HV − HR, and the relative phase coefficient as the difference of the slopes of the phase curves Δβ. These were obtained joining our own observations plus data from the literature. The methodology has been introduced in previous works and here we expand in some interesting results, in particular the strong anticorrelation found between HV − HR and Δβ, which means that redder objects have steeper phase curves in the R filter, while bluer objects have steeper phase curves in the V filter. We analyse a series of results published in the literature in view of our data base, which is free of phase effects, and show that their statistical meaning is not very strong. We point out that phase-colouring and observational errors play an important role in the understanding of these proposed relationships.


Icarus ◽  
1999 ◽  
Vol 140 (2) ◽  
pp. 341-352 ◽  
Author(s):  
Kevin R Grazier ◽  
William I Newman ◽  
William M Kaula ◽  
James M Hyman

Icarus ◽  
1999 ◽  
Vol 140 (2) ◽  
pp. 353-368 ◽  
Author(s):  
Kevin R. Grazier ◽  
William I. Newman ◽  
Ferenc Varadi ◽  
William M. Kaula ◽  
James M. Hyman

2020 ◽  
Author(s):  
Laura Buchanan ◽  
Megan Schwamb ◽  
Wesley Fraser ◽  
Michele Bannister ◽  
Michäel Marsset ◽  
...  

&lt;p&gt;The Colours of the Outer Solar System Origins Survey (Col-OSSOS, Schwamb et al., 2019) has examined the surface compositions of Kuiper Belt Objects (KBOs) by way of broadband g-, r- and J-band photometry, using the Gemini North Hawaii Telescope. This survey showed a bimodal distribution in the colours of the objects surveyed, consistent with previous colour surveys (Tegler et al., 2016). These broadband surface colours can be considered a proxy for surface composition of these KBOs, so this survey allows the frequency of different surface compositions within the outer Solar System to be explored. The bimodality of the observed colours suggests the presence of some sort of surface transition within the Kuiper belt, perhaps due to a volatile ice-line transition in the pristine planetesimal disk that existed before Neptune&amp;#8217;s migration. The Outer Solar System Origins Survey (OSSOS, Bannister et al., 2018), from which Col-OSSOS selected objects brighter than 23.6 r-band magnitude, has well characterised and quantified biases, so allowing for comparisons between the observations and numerical models of the Kuiper belt.&lt;/p&gt;&lt;p&gt;By applying different colour transitions to the primordial planetesimal disk, in this work we explore the possible positions for ice line/colour transitions within the planetesimal disk that existed before Neptune&amp;#8217;s migration. Within Schwamb et al. (2019), a simplified toy model was used to investigate the possible position of this transition. Nesvorny et al. (2020) has investigated the primordial colour fraction, in particular how it can create the inclination distribution that we see in the colours of KBOs today. In this work we use a full dynamical model of the Kuiper belt to more precisely pinpoint the possible location of this transition. We make use of the model by Nesvorny &amp; Vokrouhlicky (2016) of Neptune&amp;#8217;s migration from 23 au to 30 au, and the consequent perturbation of the Kuiper belt into its current form. This model allows precise tracking of the objects from their pre-Neptune migration to post-Neptune migration positions, allowing various colour transition positions in the initial disk, an example of which is shown in Figure 1, to be compared with the Col-OSSOS observations of the modern day disk.&lt;/p&gt;&lt;p&gt;&lt;img src=&quot;https://contentmanager.copernicus.org/fileStorageProxy.php?f=gnp.bd4fbe38b1fe56469982951/sdaolpUECMynit/0202CSPE&amp;app=m&amp;a=0&amp;c=74582d3581fd70b49ee8981e1366f7ec&amp;ct=x&amp;pn=gnp.elif&quot; alt=&quot;&quot;&gt;&lt;/p&gt;&lt;p&gt;Figure 1: An example red/neutral transition at 27 au. The left plots show the objects in the primordial disk, while the right plots show the objects post-Neptune migration from the model of Nesvorny &amp; Vokrouhlicky (2016).&lt;/p&gt;&lt;p&gt;The OSSOS survey simulator (Lawler et al., 2018) can then be used to calculate which of the simulated objects could have been observed by OSSOS, and so selected by Col-OSSOS for surface colour observations. The colour transition within the initial disk, shown in Figure 1, is moved radially outwards through the disk and the corresponding outputs are compared with the Col-OSSOS colour observations to see which initial disk colour transition positions are consistent with the modern day Kuiper belt. We will present results combing an accurate dynamical model of the Kuiper Belt&amp;#8217;s evolution by Nesvorny &amp; Vokrouhlicky (2016) with Col-OSSOS photometry. We will explore multiple radial colour distributions in the primordial planetesimal disk and implications for the the positions of ice line/colour transitions within the Kuiper Belt&amp;#8217;s progenitor populations.&lt;/p&gt;&lt;p&gt;&amp;#160;&lt;/p&gt;&lt;p&gt;&lt;strong&gt;References&lt;/strong&gt;&lt;/p&gt;&lt;p&gt;Bannister, M. T., Gladman, B. J., Kavelaars, J. J., et al. 2018, ApJS, 236, 18&lt;br&gt;Lawler, S. M., Kavelaars, J. J., Alexandersen, M., et al. 2018, Front. Astron. Space Sci., 5, 14&lt;br&gt;Nesvorny, D., Vokrouhlicky, D., Alexandersen, M., et al. 2020, AJ, in press&lt;br&gt;Nesvorny, D., &amp; Vokrouhlicky, D. 2016, ApJ, 825&lt;br&gt;Schwamb, M. E., Bannister, M. T., Marsset, M., et al. 2019, ApJS, 243, 12&lt;br&gt;Tegler, S. C., Romanishin, W., Consolmagno, G. J., &amp; J., S. 2016, AJ, 152, 210&lt;/p&gt;


1997 ◽  
Author(s):  
R. Lewis ◽  
G. Smith ◽  
B. Dundore ◽  
J. Fulmer ◽  
S. Chakrabarti ◽  
...  

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