[FPSPACE] The water ice rich surface of (145453) 2005 RR43: a case for a population of tra
LARRY KLAES
ljk4 at msn.com
Wed Mar 7 10:06:05 EST 2007
Astrophysics, abstract
astro-ph/0703098
From: Noemi Pinilla-Alonso [view email]
Date: Tue, 6 Mar 2007 00:36:32 GMT (26kb)
The water ice rich surface of (145453) 2005 RR43: a case for a population of
trans-neptunian objects?
Authors: N. Pinilla-Alonso (1), J. Licandro (2,3), R. Gil-Hutton (4), R.
Brunetto (5,6) ((1) Fundacion Galileo Galilei, (2) Isaac Newton Group, (3)
Instituto de Astrofisica de Canarias, (4) Complejo Astronomico el Leoncito,
(5) Dipartamento di Fisica, Universita di Lecce, (6) INAF-Osservatorio
Astrofisico di Catania)
Comments: 5 pages, 3 figures submitted to Astronomy & Astrophysics
Recent results suggest that there is a group of trans-Neptunian objects
(TNOs) (2003 EL61 being the biggest member), with surfaces composed of
almost pure water ice and with very similar orbital elements. We study the
surface composition of another TNO that moves in a similar orbit, (145453)
2005 RR43, and compare it with the surface composition of the other members
of this group. We report visible and near-infrared spectra in the
0.53-2.4\mu spectral range, obtained with the 4.2m William Herschel
Telescope and the 3.58m Telescopio Nazionale Galileo at the "Roque de los
Muchachos" Observatory (La Palma, Spain). The spectrum of 2005 RR43 is
neutral in color in the visible and dominated by very deep water ice
absorption bands in the near infrared (D= 70.3 +/- 2.1 % and 82.8 +/- 4.9 %
at 1.5 \mu and 2.0 \mu respectively). It is very similar to the spectrum of
the group of TNOs already mentioned. All of them present much deeper water
ice absorption bands (D>40 %) than any other TNO except Charon. Scattering
models show that its surface is covered by water ice, a significant fraction
in crytalline state with no trace (5 % upper limit) of complex organics.
Possible scenarios to explain the existence of this population of TNOs are
discussed: a giant collision, an originally carbon depleted composition, or
a common process of continuous resurfacing. We conclude that TNO 2005 RR43
is member of a group, may be a population, of TNOs clustered in the space of
orbital parameters that show abundant water ice and no signs of complex
organics and which origin needs to be further investigated. A carbon
depleted population of TNOs could be the origin of the population of carbon
depleted Jupiter family comets already noticed by A'Hearn et al. (1995).
http://arxiv.org/abs/astro-ph/0703098
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