Bibcode
Lorenzi, Vania; Pinilla-Alonso, N.; Licandro, J.; Emery, J. P.; Dalle Ore, C. M.
Bibliographical reference
American Astronomical Society, DPS meeting #45, #414.04
Advertised on:
10
2013
Citations
0
Refereed citations
0
Description
Trans-Neptunian objects (TNOs) are considered some of the most pristine
objects in the Solar System. Their surfaces display a wide range of
compositions, going from surfaces covered by dark irradiation mantels,
to surfaces totally covered by ices. According to models of the
retention of volatiles, only TNOs with a diameter d > 1000 km are
expected to retain any of their original complement of volatile ices on
their surface. However, surface refreshing processes on smaller bodies
(e.g., collisions, transient atmospheres and cometary activity) could
bring to the surface some amount of ices that are stable at depth. When
these processes affect only part of the surface they cause surface
heterogeneity. The study of rotational variability of medium and large
sized TNOs is important to better understand the physical processes
affecting their surfaces, and if these processes are local in scale or,
on the contrary, extend across the whole surface. We present
rotationally resolved spectroscopy of two TNOs, (20000) Varuna and
(136472) Makemake. Varuna is a medium sized TNO ( 621 km). We observed
Varuna with NICS@TNG telescope, in the NIR, covering two entire
rotations of the object. The analysis of the data shows a homogeneous
surface composed of a mixture of complex organics, silicates and water
ice. Our data also indicate an upper limit of 10% of methane ice on the
surface. The Dwarf Planet Makemake is also studied in this work. The
surface of this large TNO shows that, similar to Pluto and Eris, it
clearly retains large amounts of volatile ices. Moreover, thermal
observations indicate that Makemake has a heterogeneous surface that
could be the result of volatile migration. We present new visible
spectra of Makemake, obtained with ISIS@WHT telescope, covering 80% of
the surface. We present a detailed study of the differences in the
absorption bands across the surface that are indicative of changes in
the relative abundances of ices, temperature, and/or particle size.
Moreover, we collect all data available from literature, after 8 year
from the discovery of Makemake, and compare with our data to investigate
possible rotational and secular variations.