scispace - formally typeset
Search or ask a question
Author

Mario Daniel Melita

Bio: Mario Daniel Melita is an academic researcher from National University of La Plata. The author has contributed to research in topics: Planet & Solar System. The author has an hindex of 15, co-authored 49 publications receiving 686 citations. Previous affiliations of Mario Daniel Melita include National Scientific and Technical Research Council & University of Buenos Aires.

Papers
More filters
Journal ArticleDOI
Karen J. Meech, Michael F. A'Hearn1, J. A. Adams2, P. Bacci  +194 moreInstitutions (62)
TL;DR: In this paper, the EPOXI spacecraft flyby of comet 103P/Hartley 2 was used to provide synergistic information for space mission encounters by providing data over longer timescales, at different wavelengths and using techniques that are impossible with an in situ flyby.
Abstract: Earth- and space-based observations provide synergistic information for space mission encounters by providing data over longer timescales, at different wavelengths and using techniques that are impossible with an in situ flyby. We report here such observations in support of the EPOXI spacecraft flyby of comet 103P/Hartley 2. The nucleus is small and dark, and exhibited a very rapidly changing rotation period. Prior to the onset of activity, the period was ~16.4 hr. Starting in 2010 August the period changed from 16.6 hr to near 19 hr in December. With respect to dust composition, most volatiles and carbon and nitrogen isotope ratios, the comet is similar to other Jupiter-family comets. What is unusual is the dominance of CO2-driven activity near perihelion, which likely persists out to aphelion. Near perihelion the comet nucleus was surrounded by a large halo of water-ice grains that contributed significantly to the total water production.

118 citations

Journal ArticleDOI
01 Nov 2002-Icarus
TL;DR: In this article, the effects of a Mars-like planetoid with a semimajor axis at about ∼60 AU orbiting embedded in the primordial Edgeworth-Kuiper belt (EKB) are studied.

70 citations

Journal ArticleDOI
01 May 2013-Icarus
TL;DR: In this paper, the authors present new visible and near-infrared spectra to demonstrate that thermally altered carbonaceous chondrites are plausible compositional analogs, however this is a tentative association due to a lack of prominent absorption features in their data.

57 citations

Journal ArticleDOI
TL;DR: In this article, two consecutive transits of planetary companion OGLE-TR-111b were observed in the I band, and the timing of the transits cannot be explained by a constant period and that the observed variations cannot be originated by the presence of a satellite.
Abstract: Two consecutive transits of planetary companion OGLE-TR-111b were observed in the I band. Combining these observations with data from the literature, we find that the timing of the transits cannot be explained by a constant period and that the observed variations cannot be originated by the presence of a satellite. However, a perturbing planet with the mass of the Earth in an exterior orbit could explain the observations if the orbit of OGLE-TR-111b is eccentric. We also show that the eccentricity needed to explain the observations is not ruled out by the radial velocity data found in the literature.

43 citations

Journal ArticleDOI
01 Jun 2008-Icarus
TL;DR: In this paper, the authors search for correlations between physical and dynamical properties, explore relationships between the following four quantities; the normalised visible reflectivity indexes (S ′ ), the absolute magnitudes, the observed albedos and the orbital stability of the Trojans.

30 citations


Cited by
More filters
Journal ArticleDOI
TL;DR: A detailed survey of more than 100 comets has been carried out by as mentioned in this paper, which enabled taxonomic groupings based on free radical species and on crystallinity of rocky grains.
Abstract: Cometary nuclei contain the least modified material from the formative epoch of our planetary system, and their compositions reflect a range of processes experienced by material prior to its incorporation in the cometary nucleus. Dynamical models suggest that icy bodies in the main cometary reservoirs (Kuiper Belt, Oort Cloud) formed in a range of environments in the protoplanetary disk, and (for the Oort Cloud) even in disks surrounding neighboring stars of the Sun's birth cluster. Photometric and spectroscopic surveys of more than 100 comets have enabled taxonomic groupings based on free radical species and on crystallinity of rocky grains. Since 1985, new surveys have provided emerging taxonomies based on the abundance ratios of primary volatiles. More than 20 primary chemical species are now detected in bright comets. Measurements of nuclear spin ratios (in water, ammonia, and methane) and of isotopic ratios (D/H in water and HCN; 14N/15N in CN and HCN) have provided critical insights on factors affec...

849 citations

Journal ArticleDOI
Bernard Marty1
TL;DR: For example, Pujol et al. as mentioned in this paper proposed that the Earth is not as volatile-poor as previously thought, and showed that it contains up to 2 (± 1) % contribution of carbonaceous chondrite (CI-CM) to a dry proto-Earth.

805 citations

Book
01 May 2011
TL;DR: In this paper, the authors present an overview of the solar system and its evolution, including the formation and evolution of stars, asteroids, and free-floating planets, as well as their internal and external structures.
Abstract: 1. Introduction 2. Radial velocities 3. Astrometry 4. Timing 5. Microlensing 6. Transits 7. Imaging 8. Host stars 9. Brown dwarfs and free-floating planets 10. Formation and evolution 11. Interiors and atmospheres 12. The Solar System Appendixes References Index.

527 citations

Journal ArticleDOI
13 Oct 2011-Nature
TL;DR: In this article, the deuterium-to-hydrogen ratio (D/H) of the Jupiter-family comet 103P/Hartley 2 was found to be (1.61 ± 0.24)
Abstract: For decades, the source of Earth's volatiles, especially water with a deuterium-to-hydrogen ratio (D/H) of (1.558 ± 0.001) × 10^(−4), has been a subject of debate. The similarity of Earth’s bulk composition to that of meteorites known as enstatite chondrites suggests a dry proto-Earth with subsequent delivery of volatiles by local accretion or impacts of asteroids or comets. Previous measurements in six comets from the Oort cloud yielded a mean D/H ratio of (2.96 ± 0.25) × 10^(−4). The D/H value in carbonaceous chondrites, (1.4 ± 0.1) × 10^(−4), together with dynamical simulations, led to models in which asteroids were the main source of Earth's water, with ≤10 per cent being delivered by comets. Here we report that the D/H ratio in the Jupiter-family comet 103P/Hartley 2, which originated in the Kuiper belt, is (1.61 ± 0.24) × 10^(−4). This result substantially expands the reservoir of Earth ocean-like water to include some comets, and is consistent with the emerging picture of a complex dynamical evolution of the early Solar System.

408 citations

Journal ArticleDOI
TL;DR: In this article, the authors investigate the evolution of a population of cores with initial masses in the range 0.1-1 M. All the simulations end with a population typically between two and five planets, with masses depending on the initial mass.
Abstract: The existence of extrasolar planets with short orbital periods suggests that planetary migration induced by tidal interaction with the protoplanetary disk is important. Cores and terrestrial planets may undergo migration as they form. In this paper we investigate the evolution of a population of cores with initial masses in the range 0.1-1 M⊕ embedded in a disk. Mutual interactions lead to orbit crossing and mergers, so that the cores grow during their evolution. Interaction with the disk leads to orbital migration, which results in the cores capturing each other in mean motion resonances. As the cores migrate inside the disk inner edge, scatterings and mergers of planets on unstable orbits, together with orbital circularization, causes strict commensurability to be lost. Near commensurability however is usually maintained. All the simulations end with a population typically between two and five planets, with masses depending on the initial mass. These results indicate that if hot super-Earths or Neptunes form by mergers of inwardly migrating cores, then such planets are most likely not isolated. We would expect to always find at least one, more likely a few, companions on close and often near-commensurable orbits. To test this hypothesis, it would be of interest to look for planets of a few to about 10 M⊕ in systems where hot super-Earths or Neptunes have already been found.

355 citations