There were 6 new TNO discoveries announced since the previous issue of Distant EKOs:
2010 RE64, 2010 RF43, 2010 RF64, 2010 RM45, 2010 RN45, 2010 RN64
and 5 new Centaur/SDO discoveries:
2010 BK118, 2010 RG43, 2010 RM64, 2010 RO64, 2010 TH
2009 YE7 (SDO TNO)
2010 PT66 (TNO SDO)
Objects recently assigned numbers:
2002 KY14 = (250112)
Current number of TNOs: 1155 (including Pluto)
Current number of Centaurs/SDOs: 289
Current number of Neptune Trojans: 7
Out of a total of 1451 objects:
632 have measurements from only one opposition
581 of those have had no measurements for more than a year
324 of those have arcs shorter than 10 days
(for more details, see:
The goal of the Herschel Open Time programme TNOs are Cool! is to derive the physical and thermal properties for a large sample of Centaurs, and trans-Neptunian objects (TNOs), including resonant, classical, detached and scattered disk objects. Based on observations of two targets we tried (i) to optimise the SPIRE observing technique for faint (close to the background confusion noise), slowly moving targets; (ii) to test different thermal model techniques; (iii) to determine radiometric diameter and albedo values; (iv) to compare with Spitzer results whenever possible. We obtained SPIRE photometry on two targets and PACS photometry on one of the targets. We present results for the two targets, (90482) Orcus and (136472) Makemake, observed with SPIRE and for one of those targets, Makemake, observed with PACS. We adopt pV = 0.27 and D = 850 km as our best estimate of the albedo and diameter of Orcus using single terrain models. With two-terrain models for Makemake, the bright terrain is fitted by, 0.78 < pV < 0.90, and the dark terrain 0.02 < pV < 0.12, giving 1360 < D < 1480 km. A single terrain model was derived for Orcus through the SPIRE photometry combined with MIPS data. The Makemake data from MIPS, PACS and SPIRE combined are not compatible with a single terrain model, but can be modelled with a two-terrain fit. These science demonstration observations have shown that the scanning technique, which allows us to judge the influence of background structures, has proved to be a good basis for this key programme.
Published in: Astronomy & Astrophysics, 315, 148L (2010 July)
Bernstein et al. (2004) found that the population of faint (R>26) trans-Neptunian objects (TNOs) known at that time was dominated by ``Classical'' objects, which have low inclinations () and distances 40-45 AU. Since those observations, the number of faint TNOs whose orbits are sufficiently well known to be classified as ``Classical'' or ``Excited'' has grown from 7 to 39. We analyze the dynamical classifications of faint TNOs known today and find that this population is dominated by Excited objects. We discuss some implications of this result.
To appear in: The Astrophysical Journal Letters
For preprints, contact firstname.lastname@example.org
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One of the main particular features of the structure of the Kuiper Belt is that it contains clusters of objects of small orbital eccentricity and inclination (``cold population''). In order to solve the problem of the origin of the objects, we considered the process of the gravitational interaction of a comparatively small-mass planet with a planetesimal disk. We found that one particular property of the process is that the planet changes its direction of migration. The interaction with the planet results in the transportation of a considerable portion of planetesimals from the inner zone out to the Kuiper Belt. After such a transition of the objects, the planet returns to the inner regions of the planetesimal disk. Numerical simulations show that the reversible migration of a planet of a mass similar to that of the Earth can explain the main properties of the Kuiper Belt’s cold population orbit distribution.
Published in: Solar System Research, 44, 281 (2010 August)
The Hill stability of the low mass binary system in the presence of a massive third body moving on a wider inclined orbit is investigated analytically. It is found that, in the case of the third body being on a nearly circular orbit, the region of Hill stability expands as the binary/third body mass ratio increases and the inclination (i) decreases. This i-dependence decreases very quickly with increasing eccentricity (e2) of the third body relative to the binary barycentre. In fact, if e2 is not extremely small, the Hill stable region can be approximately expressed in a closed form by setting , and it contracts with increasing e2 as e22 for sufficiently low mass binary. Our analytic results are then applied to the observed triple star systems and the Kuiper Belt Binaries.
Published in: Celestial Mechanics and Dynamical Astronomy, 107, 21 (2010 May)
The existence of extremely wide binaries in the low-inclination component of the Kuiper Belt provides a unique handle on the dynamical history of this population. Some popular frameworks of the formation of the Kuiper Belt suggest that planetesimals were moved there from lower semi-major axis orbits by scattering encounters with Neptune. We test the effects such events would have on binary systems, and find that wide binaries are efficiently destroyed by the kinds of scattering events required to create the Kuiper Belt with this mechanism. This indicates that a binary-bearing component of the cold Kuiper Belt was emplaced through a gentler mechanism or was formed in situ.
Published in: The Astrophysical Journal Letters, 722, L204 (2010 October 20)
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We present an ultra-deep survey for Neptune Trojans using the Subaru 8.2-m and Magellan 6.5-m telescopes. The survey reached a 50% detection efficiency in the R-band at mR=25.7 magnitudes and covered 49 square degrees of sky. mR=25.7 mags corresponds to Neptune Trojans that are about 16 km in radius (assuming an albedo of 0.05). A paucity of smaller Neptune Trojans (radii < 45 km) compared to larger ones was found. The brightest Neptune Trojans appear to follow a steep power-law slope () similar to the brightest objects in the other known stable reservoirs such as the Kuiper Belt, Jupiter Trojans and main belt asteroids. We find a roll-over for the Neptune Trojans that occurs around a radii of km ( ), which is also very similar to the other stable reservoirs. All the observed stable regions in the the solar system show evidence for Missing Intermediate Sized Planetesimals (MISPs). This indicates a primordial and not collisional origin, which suggests planetesimal formation proceeded directly from small to large objects. The scarcity of intermediate and smaller sized Neptune Trojans may limit them as being a strong source for the short period comets.
To appear in: The Astrophysical Journal Letters
For preprints, contact firstname.lastname@example.org
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Aims. We explore the orbital evolution of the four Jovian planets embedded in a self-gravitating planetesimal disk, and the simultaneous accretion of small bodies by proto-Uranus and proto-Neptune.
Methods. We adopt the code NBODY4 running on the GRAPE-type special-purpose computer for numerically simulating the primordial evolution of the outer Solar system, where the total gravitational forces due to the Sun, the four Jovian planets and the massive planetesimals are all taken into account.
Results. (1) There is no significant accretion of proto-Uranus and proto-Neptune during their migration stage, only by the order of 0.1 Earth mass. (2) The self-gravitating disk can provide a new replenishment of planetesimals outside a few AU beyond Neptune into the scattering zone, resulting in larger radial displacement of Neptune than in the non-self-gravitating disk. (3) The present location of Neptune requires an original planetesimal disk outer edge at 35AU. (4) The distribution of the surviving planetesimals is very similar to the observed Kuiper Belt.
To appear in: Astronomy & Astrophysics
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Estimating the Density of Intermediate Size KBOs from Considerations of Volatile Retention
Amit Levi1 and Morris Podolak1
Department of Geophysics & Planetary Science, Raymond and Beverly Sackler Faculty of Exact Sciences, Tel Aviv University, Tel Aviv. 69978, Israel
Submitted to: Icarus
Preprints available on the web at
Dust in the Edgeworth-Kuiper Belt Zone
J. Klacka1, L. Kómar1, P. Páastor1,2
1 Faculty of Mathematics, Physics and Informatics,
Comenius University Mlynská dolina, 842 48 Bratislava, Slovak Republic
2 Tekov Observatory, Sokolovská 21, 934 01, Levice, Slovak Republic
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Direct Detection of Seasonal Changes on Triton with HST
J.M. Bauer1, B.J. Buratti1, J-Y. Li 2, J.A. Mosher1, M.D. Hicks1, B.E. Schmidt3, and J.D. Goguen1
1 Jet Propulsion Laboratory, California Institute of Technology, 4800 Oak Grove Drive, MS 183-401, Pasadena, CA 91109, USA
2 University of Maryland, Department of Astronomy, College Park, MD 20742, USA
3 University of California, Los Angeles, Institute of Geophysics & Planetary Physics, 2240 1/2 S Carmelina Ave., Los Angeles, CA 90064, USA
To appear in: The Astrophysical Journal Letters, 723, L49 (2010 November 1)
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