2008/03/07 by N. Pinilla-ALonso, N. Pinilla-Alonso, R. Brunetto +4 · 2 citations
Earth and Planetary Sciences · Physics and Astronomy · #Astro and Planetary Science #Geology and Paleoclimatology Research #Planetary Science and Exploration #astro-ph
paper · pdf · doi:10.1051/0004-6361/200809733
9 pages, 7 graphs. Keywords: water ice, carbon-depleted, Kuiper Belt, astrochemistry, spectroscopy
arxiv created 2008/03/07 · openalex publication_date 2009/01/30 · arxiv updated 2009/12/01 · openalex created_date 2016/06/24 · openalex updated_date 2026/07/31
<i>Context. <i/>Previously known as 2003 EL<sub>61<sub/>, (136108) Haumea, is the largest member of a group of trans-Neptunian objects (TNOs) with similar orbits and “unique” spectral characteristics in the form of a neutral slope in the visible and the deepest water ice absorption bands observed in the trans-Neptunian belt (TNb). Studying the surface of 2003 EL<sub>61<sub/> provides useful constraints of the origin of this particular group of TNOs and about the outer Solar System's history.<i>Aims. <i/>We attempt to study the composition of the surface of 2003 EL<sub>61<sub/>.<i>Methods. <i/>We present visible and near-infrared spectra of 2003 EL<sub>61<sub/> obtained with the 4.2 m WHT and the 3.6 m TNG telescopes at the “Roque de los Muchachos” Observatory (Canary Islands, Spain). Near-infrared spectra were obtained at different rotational phases covering almost one complete rotational period. Spectra are fitted using scattering models based on Hapke theory and constraints on the surface composition are derived.<i>Results. <i/>The observations confirm previous results that the 2003 EL<sub>61<sub/> spectrum is neutral in color and exhibits deep water-ice absorption bands. They also provide new facts about the surface of this object: the lack of significant variations in the spectral slope (in the near-infrared) and the depth of the water-ice absorption bands at different rotational phases clearly evident in the data, suggest that the surface of 2003 EL<sub>61<sub/> is homogeneous. The scattering models indicate that a 1:1 intimate mixture of crystalline and amorphous water ice is the most probable surface composition of this big TNO, and constrain the presence of other minor constituents to a maximum traction of 8%.<i>Conclusions. <i/>The derived composition suggests that: a) cryovolcanism is unlikely to be the resurfacing process that retains the surface of this TNO, and the other members of this population, covered mainly by water ice; b) the surface is older than 10<sup>8<sup/> yr which constrains the timescale of any catastrophic event. such as the collision suggested to be the origin of this population, to at least 10<sup>8<sup/> yr; c) the surface of 2003 EL<sub>61<sub/> is depleted of carbon-bearing species. According to the orbital parameters of the population, this implies that is a possible source of carbon-depleted, Jupiter-Family comets.