Bibcode
Pinilla-Alonso, N.; Licandro, J.; Campins, H.
Bibliographical reference
American Astronomical Society, DPS meeting #36, #11.07; Bulletin of the American Astronomical Society, Vol. 36, p.1088
Advertised on:
11
2004
Citations
3
Refereed citations
3
Description
TNOs (50000) Quaoar and 2002 TX300 were observed in the
framework of a long-term program to study the surface properties of
TNOs, Centaurs and comet nuclei using the Italian 3.58 m Telescopio
Nazionale Galileo (TNG) at "El Roque de los Muchachos" Observatory (La
Palma, Spain). Near-infrared spectra of both TNOs and visible spectrum
of 2002 TX300 were obtained. Combining our spectra and the
visible spectrum of (50000) Quaoar done by Marchi et al. (2004, A&A,
408, 17), and using the simple one-dimensional geometrical-optics
formulation by Shkuratov et al. (1999, Icarus 137, 235), the visible and
near-infrared spectra covering the 0.5-2.4 μ m range of both TNOs are
analyzed in order to obtain mineralogical information of their surfaces.
A large fraction of big water ice particles is needed to reproduce the
large absorption bands observed in both objects, while other component,
may be methanol, is needed to reproduce the absorption around 2.2 μ m
observed in Quaoar (also reported by Brown & Trujillo 2004, AJ in
press). Quaoar surface is very red, and a large fraction of complex
organics is needed to reproduce the slope and general shape of the
spectrum. On the other hand, the neutral color of the surface of
TX300 and the huge water ice absorption bands suggest a very
low abundance of complex organics. The very different fraction of
tholins and water ice in the surface of both objects is indicative
either of a very different original composition or a different
resurfacing history. The results are discussed in the framework of the
different resurfacing models already proposed.
This work was supported by the grants from the National Science
Foundation and the NASA Planetary Astronomy program.