New Discoveries Beyond the Neptune and the Pluto Orbit
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(145453) 2005 RR43: a Case for a Carbon-Depleted Population of Tnos?
A&A 468, L25–L28 (2007) Astronomy DOI: 10.1051/0004-6361:20077294 & c ESO 2007 Astrophysics Letter to the Editor The water ice rich surface of (145453) 2005 RR43: a case for a carbon-depleted population of TNOs? N. Pinilla-Alonso1, J. Licandro2,3, R. Gil-Hutton4, and R. Brunetto5,6 1 Fundación Galileo Galilei & Telescopio Nazionale Galileo, PO Box 565, 38700, S/C de La Palma, Tenerife, Spain e-mail: [email protected] 2 Isaac Newton Group, 38700 Santa Cruz de La Palma, Tenerife, Spain 3 Instituto de Astrofísica de Canarias, c/Vía Láctea s/n, 38205 La Laguna, Tenerife, Spain 4 Complejo Astronómico El Leoncito (Casleo) and San Juan National University, Av. España 1512 sur, J5402DSP, San Juan, Argentina 5 Dipartimento di Fisica, Università del Salento, via Arnesano, 73100 Lecce, Italy 6 INAF-Osservatorio Astrofisico di Catania, via S. Sofia 78, 95123 Catania, Italy Received 13 February 2007 / Accepted 23 April 2007 ABSTRACT Context. 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. These objects provide exciting laboratories for the study of the processes that prevent the formation of an evolved mantle of organics on the surfaces of the bodies in the trans-Neptunian belt (TNb). Aims. 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 the group. Methods. We report visible and near-infrared spectra in the 0.53−2.4 µm spectral range, obtained with the 4.2 m William Herschel Telescope and the 3.58 m Telescopio Nazionale Galileo at the “Roque de los Muchachos” Observatory (La Palma, Spain). -
Comparative Kbology: Using Surface Spectra of Triton, Pluto, and Charon
COMPARATIVE KBOLOGY: USING SURFACE SPECTRA OF TRITON, PLUTO, AND CHARON TO INVESTIGATE ATMOSPHERIC, SURFACE, AND INTERIOR PROCESSES ON KUIPER BELT OBJECTS by BRYAN JASON HOLLER B.S., Astronomy (High Honors), University of Maryland, College Park, 2012 B.S., Physics, University of Maryland, College Park, 2012 M.S., Astronomy, University of Colorado, 2015 A thesis submitted to the Faculty of the Graduate School of the University of Colorado in partial fulfillment of the requirement for the degree of Doctor of Philosophy Department of Astrophysical and Planetary Sciences 2016 This thesis entitled: Comparative KBOlogy: Using spectra of Triton, Pluto, and Charon to investigate atmospheric, surface, and interior processes on KBOs written by Bryan Jason Holler has been approved for the Department of Astrophysical and Planetary Sciences Dr. Leslie Young Dr. Fran Bagenal Date The final copy of this thesis has been examined by the signatories, and we find that both the content and the form meet acceptable presentation standards of scholarly work in the above mentioned discipline. ii ABSTRACT Holler, Bryan Jason (Ph.D., Astrophysical and Planetary Sciences) Comparative KBOlogy: Using spectra of Triton, Pluto, and Charon to investigate atmospheric, surface, and interior processes on KBOs Thesis directed by Dr. Leslie Young This thesis presents analyses of the surface compositions of the icy outer Solar System objects Triton, Pluto, and Charon. Pluto and its satellite Charon are Kuiper Belt Objects (KBOs) while Triton, the largest of Neptune’s satellites, is a former member of the KBO population. Near-infrared spectra of Triton and Pluto were obtained over the previous 10+ years with the SpeX instrument at the IRTF and of Charon in Summer 2015 with the OSIRIS instrument at Keck. -
A Search for Volatile Ices on the Surfaces of Cold Classical Kuiper Belt Objects
University of Tennessee, Knoxville TRACE: Tennessee Research and Creative Exchange Masters Theses Graduate School 5-2013 A search for volatile ices on the surfaces of cold classical Kuiper Belt Objects Daine Michael Wright [email protected] Follow this and additional works at: https://trace.tennessee.edu/utk_gradthes Part of the Other Astrophysics and Astronomy Commons, and the The Sun and the Solar System Commons Recommended Citation Wright, Daine Michael, "A search for volatile ices on the surfaces of cold classical Kuiper Belt Objects. " Master's Thesis, University of Tennessee, 2013. https://trace.tennessee.edu/utk_gradthes/1699 This Thesis is brought to you for free and open access by the Graduate School at TRACE: Tennessee Research and Creative Exchange. It has been accepted for inclusion in Masters Theses by an authorized administrator of TRACE: Tennessee Research and Creative Exchange. For more information, please contact [email protected]. To the Graduate Council: I am submitting herewith a thesis written by Daine Michael Wright entitled "A search for volatile ices on the surfaces of cold classical Kuiper Belt Objects." I have examined the final electronic copy of this thesis for form and content and recommend that it be accepted in partial fulfillment of the requirements for the degree of Master of Science, with a major in Geology. Joshua Emery, Major Professor We have read this thesis and recommend its acceptance: Harry McSween, Jeffrey Moersch Accepted for the Council: Carolyn R. Hodges Vice Provost and Dean of the Graduate School (Original signatures are on file with official studentecor r ds.) A search for volatile ices on the surfaces of cold classical Kuiper Belt Objects A Thesis Presented for The Master of Science Degree The University of Tennessee, Knoxville Daine Michael Wright May 2013 c by Daine Michael Wright, 2013 All Rights Reserved. -
Formation, Structure and Habitability of Super-Earth and Sub-Neptune
Formation, Structure and Habitability of Super-Earth and Sub-Neptune Exoplanets by Leslie Anne Rogers B.Sc., Honours Physics-Mathematics, University of Ottawa (2006) Submitted to the Department of Physics in partial fulfillment of the requirements for the degree of Doctor of Philosophy at the MASSACHUSETTS INSTITUTE OF TECHNOLOGY June 2012 c Massachusetts Institute of Technology 2012. All rights reserved. Author.............................................................. Department of Physics May 22, 2012 Certified by. Sara Seager Professor of Planetary Science Professor of Physics Class of 1941 Professor Thesis Supervisor Accepted by . Krishna Rajagopal Professor of Physics Associate Department Head for Education 2 Formation, Structure and Habitability of Super-Earth and Sub-Neptune Exoplanets by Leslie Anne Rogers Submitted to the Department of Physics on May 22, 2012, in partial fulfillment of the requirements for the degree of Doctor of Philosophy Abstract Insights into a distant exoplanet's interior are possible given a synergy between models and observations. Spectral observations of a star's radial velocity wobble induced by an orbiting planet's gravitational pull measure the planet mass. Photometric transit observations of a planet crossing the disk of its star measure the planet radius. This thesis interprets the measured masses and radii of super-Earth and sub-Neptune exoplanets, employing models to constrain the planets' bulk compositions, formation histories, and habitability. We develop a model for the internal structure of low-mass exoplanets consisting of up to four layers: an iron core, silicate mantle, ice layer, and gas layer. We quantify the span of plausible bulk compositions for low-mass transiting planets CoRoT-7b, GJ 436b, and HAT-P-11b, and describe how Bayesian analysis can be applied to rigorously account for observational, model, and inherent uncertainties. -
Phd. Compositional Variation of Small Bodies Across the Solar System
Observatoire de Paris Ecole´ Doctorale Astronomie et Astrophysique d'^Ile-de-France THESE` DE DOCTORAT pr´esent´eepour obtenir le grade de DOCTEUR DE L'OBSERVATOIRE DE PARIS Sp´ecialit´e:Astronomie & Astrophysique par Francesca E. DeMeo La variation compositionnelle des petits corps `atravers le syt`emesolaire soutenue le 16 juin 2010 devant le jury: Dr. Bruno Sicardy Pr´esident Dr. Hermann Boehnhardt Rapporteur Dr. Alberto Cellino Rapporteur Dr. Humberto Campins Examinateur Dr. Beth Clark Examinateur Dr. Daniel Hestroffer Examinateur Dr. M. Antonietta Barucci Co-Directrice de th`ese Dr. Richard P. Binzel Co-Directeur de th`ese LESIA, Observatoire de Paris-Meudon [email protected] The Paris Observatory Doctoral School of Astronomy and Astrophysics of ^Ile-de-France DOCTORAL THESIS presented to obtain the degree of DOCTOR OF THE PARIS OBSERVATORY Specialty: Astronomy & Astrophysics by Francesca E. DeMeo The compositional variation of small bodies across the Solar System defended the 16th of June 2010 before the jury: Dr. Bruno Sicardy President Dr. Hermann Boehnhardt Reviewer Dr. Alberto Cellino Reviewer Dr. Humberto Campins Examiner Dr. Beth Clark Examiner Dr. Daniel Hestroffer Examiner Dr. M. Antonietta Barucci Co-Advisor Dr. Richard P. Binzel Co-Advisor LESIA, Observatoire de Paris-Meudon [email protected] Abstract Small bodies hold keys to our understanding of the Solar System. By studying these populations we seek the information on the conditions and structure of the primordial and current Solar System, its evolution, and the formation process of the planets. Constraining the surface composition of small bodies provides us with the ingredients and proportions for this cosmic recipe. -
Absolute Magnitudes and Phase Coefficients of Trans-Neptunian Objects
A&A 586, A155 (2016) Astronomy DOI: 10.1051/0004-6361/201527161 & c ESO 2016 Astrophysics Absolute magnitudes and phase coefficients of trans-Neptunian objects A. Alvarez-Candal1, N. Pinilla-Alonso2, J. L. Ortiz3,R.Duffard3, N. Morales3, P. Santos-Sanz3, A. Thirouin4, and J. S. Silva1 1 Observatório Nacional / MCTI, Rua General José Cristino 77, 20921-400 Rio de Janeiro, RJ, Brazil e-mail: [email protected] 2 Department of Earth and Planetary Sciences, University of Tennessee, Knoxville, TN, 37996, USA 3 Instituto de Astrofísica de Andalucía, CSIC, Apt 3004, 18080 Granada, Spain 4 Lowell Observatory, 1400 W Mars Hill Rd, Flagstaff, 86001 Arizona, USA Received 10 August 2015 / Accepted 27 November 2015 ABSTRACT Context. Accurate measurements of diameters of trans-Neptunian objects (TNOs) are extremely difficult to obtain. Thermal modeling can provide good results, but accurate absolute magnitudes are needed to constrain the thermal models and derive diameters and geometric albedos. The absolute magnitude, HV , is defined as the magnitude of the object reduced to unit helio- and geocentric distances and a zero solar phase angle and is determined using phase curves. Phase coefficients can also be obtained from phase curves. These are related to surface properties, but only few are known. Aims. Our objective is to measure accurate V-band absolute magnitudes and phase coefficients for a sample of TNOs, many of which have been observed and modeled within the program “TNOs are cool”, which is one of the Herschel Space Observatory key projects. Methods. We observed 56 objects using the V and R filters. These data, along with those available in the literature, were used to obtain phase curves and measure V-band absolute magnitudes and phase coefficients by assuming a linear trend of the phase curves and considering a magnitude variability that is due to the rotational light-curve. -
Implications of Magnitude Distribution Comparisons Between Trans-Neptunian Objects and Comets
Implications of Magnitude Distribution Comparisons between Trans-Neptunian Objects and Comets by Alexander J. Willman, Jr. SpSt 997 “Independent Study” Department of Space Studies University of North Dakota Dr. C. A. Wood, Advisor December 1, 1995 Implications of Magnitude Distribution Comparisons between Trans-Neptunian Objects and Comets Abstract The population of observed trans-neptunian objects has a fairly well-defined magnitude distribution, however, the population of observed short-period comets does not. This analysis of the population distributions of observed trans-neptunian objects (TNOs) and short-period comets (SPCs) indicates that the observed number of TNOs and SPCs is insufficient to judge conclusively whether the trans-neptunian objects are related to the short-period comets or whether the TNOs are part of the Kuiper belt from which the SPCs are believed to be derived. Differences in the population distributions of TNOs and SPCs indicate that the TNOs are not representative of the Kuiper belt as a whole, even if they are part of the Kuiper belt. Further analysis of the population distributions of comets and the TNOs has provided additional information and some predictions about the populations’ characteristics. This derived information includes the facts that: the six brightest SPCs for which H10 magnitudes have been calculated likely belong to the Oort cloud population (long-period) of comets instead of the Kuiper belt population of comets; Pluto and Charon are likely to belong to the TNO population instead of the major planet population; there are likely to be ~109 TNOs in the Kuiper belt, including many Pluto-sized objects, massing a total of ~1025 kg in all. -
Volatile Evolution and Atmospheres of Trans-Neptunian Objects
Volatile evolution and atmospheres of Trans-Neptunian Objects Leslie A. Younga Felipe Braga-Ribasb Robert E. Johnsonc a Southwest Research Institute, Boulder CO, USA b Federal University of Technology - Paraná/Brazil - UTFPR/Curitiba c University of Virginia, Charlottesville, VA, USA Abstract At 30-50 K, the temperatures typical for surfaces in the Kuiper Belt (e.g. Stern & Trafton 2008), only seven species have sublimation pressures higher than 1 nbar (Fray & Schmitt 2009): Ne, N2, CO, Ar, O2, CH4, and Kr. Of these, N2, CO, and CH4 have been detected or inferred on the surfaces of Trans-Neptunian Objects (TNOs). The presence of tenuous atmospheres above these volatile ices depends on the sublimation pressures, which are very sensitive to the composition, temperatures, and mixing states of the volatile ices. Therefore, the retention of volatiles on a TNO is related to its formation environment and thermal history. The surface volatiles may be transported via seasonally varying atmospheres and their condensation might be responsible for the high surface albedos of some of these bodies. The most sensitive searches for tenuous atmospheres are made by the method of stellar occultation, which have been vital for the study of the atmospheres of Triton and Pluto, and has to-date placed upper limits on the atmospheres of 11 other bodies. The recent release of the Gaia astrometric catalog has led to a "golden age" in the ability to predict TNO occultations in order to increase the observational data base. Keywords: Trans Neptunian objects, Kuiper Belt Objects, ices, atmospheres 1. Introduction Several bodies in the Transneptunian region have volatiles on their surfaces that have significant vapor pressures at the temperatures of the outer solar system: CH4, N2, and CO (with CO only detected on Pluto and Triton). -
Volatile Evolution and Atmospheres of Trans-Neptunian Objects
Volatile evolution and atmospheres of Trans-Neptunian Objects Leslie A. Younga Felipe Braga-Ribasb Robert E. Johnsonc a Southwest Research Institute, Boulder CO, USA b Federal University of Technology - Paraná/Brazil - UTFPR/Curitiba c University of Virginia, Charlottesville, VA, USA Abstract At 30-50 K, the temperatures typical for surfaces in the Kuiper Belt (e.g. Stern & Trafton 2008), only seven species have sublimation pressures higher than 1 nbar (Fray & Schmitt 2009): Ne, N2, CO, Ar, O2, CH4, and Kr. Of these, N2, CO, and CH4 have been detected or inferred on the surfaces of Trans-Neptunian Objects (TNOs). The presence of tenuous atmospheres above these volatile ices depends on the sublimation pressures, which are very sensitive to the composition, temperatures, and mixing states of the volatile ices. Therefore, the retention of volatiles on a TNO is related to its formation environment and thermal history. The surface volatiles may be transported via seasonally varying atmospheres and their condensation might be responsible for the high surface albedos of some of these bodies. The most sensitive searches for tenuous atmospheres are made by the method of stellar occultation, which have been vital for the study of the atmospheres of Triton and Pluto, and has to-date placed upper limits on the atmospheres of 11 other bodies. The recent release of the Gaia astrometric catalog has led to a "golden age" in the ability to predict TNO occultations in order to increase the observational data base. Keywords: Trans Neptunian objects, Kuiper Belt Objects, ices, atmospheres 1. Spectral evidence of N2, CO, and CH4 on the surfaces of TNOs Methane ice has been reported or inferred on the surfaces Triton, Pluto, Eris, Makemake, Quaoar, Varuna, Sedna, and 2007 OR10. -
Neptune and Triton Essential Pieces of the Solar System Puzzle
Neptune and Triton: Essential pieces of the Solar System puzzle a, b,c d a e,f g A. Masters , N. Achilleos , C.B. Agnor , S. Campagnola , S. Charnoz , B. Christophe , A.J. Coates c,h, L.N. Fletcher i, G.H. Jones c,h, L. Lamy j, F. Marzari k, N. Nettelmann l, J. Ruiz m, R. Ambrosi n, N. Andre o, A. Bhardwaj p, J.J. Fortney l, C.J. Hansen q, R. Helled r, s t b,c u v G. Moragas-Klostermeyer , G. Orton , L. Ray , S. Reynaud , N. Sergis , R. Srama s, M. Volwerk w a Institute of Space and Astronautical Science, Japan Aerospace Exploration Agency, 3-1-1 Yoshinodai, Chuo-ku, Sagamihara, Kanagawa 252-5210, Japan b Atmospheric Physics Laboratory, Department of Physics and Astronomy, University College London, Gower Street, London WC1E 6BT, UK c The Centre for Planetary Sciences at UCL/Birkbeck, Gower Street, London, WC1E 6BT, UK d Astronomy Unit, School of Physics and Astronomy, Queen Mary University of London, Mile End Road, London, E1 4NS, UK e Laboratoire AIM, Université Paris Diderot/CEA/CNRS, 91191 Gif-sur-Yvette Cedex, France f Institut Universitaire de France, 103 Boulevard Saint Michel, 75005 Paris, France g ONERA – The French Aerospace Lab, 92322 Châtillon, France h Mullard Space Science Laboratory, Department of Space and Climate Physics, University College London, Holmbury St. Mary, Dorking, Surrey RH5 6NT, UK i Atmospheric, Oceanic & Planetary Physics, Clarendon Laboratory, University of Oxford, Parks Road, Oxford OX1 3PU, UK j LESIA, Observatoire de Paris, CNRS, Université Pierre et Marie Curie, Université Paris Diderot, Meudon, France -
The Compositional Variation of Small Bodies Across the Solar System F
The compositional variation of small bodies across the Solar System F. E. Demeo To cite this version: F. E. Demeo. The compositional variation of small bodies across the Solar System. Astrophysics [astro-ph]. Observatoire de Paris, 2010. English. tel-00514550 HAL Id: tel-00514550 https://tel.archives-ouvertes.fr/tel-00514550 Submitted on 2 Sep 2010 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Observatoire de Paris Ecole´ Doctorale Astronomie et Astrophysique d’ˆIle-de-France THESE` DE DOCTORAT pr´esent´eepour obtenir le grade de DOCTEUR DE L’OBSERVATOIRE DE PARIS Sp´ecialit´e:Astronomie & Astrophysique par Francesca E. DeMeo La variation compositionnelle des petits corps `atravers le syt`emesolaire soutenue le 16 juin 2010 devant le jury: Dr. Bruno Sicardy Pr´esident Dr. Hermann Boehnhardt Rapporteur Dr. Alberto Cellino Rapporteur Dr. Humberto Campins Examinateur Dr. Beth Clark Examinateur Dr. Daniel Hestroffer Examinateur Dr. M. Antonietta Barucci Co-Directrice de th`ese Dr. Richard P. Binzel Co-Directeur de th`ese LESIA, Observatoire de Paris-Meudon [email protected] The Paris Observatory Doctoral School of Astronomy and Astrophysics of ˆIle-de-France DOCTORAL THESIS presented to obtain the degree of DOCTOR OF THE PARIS OBSERVATORY Specialty: Astronomy & Astrophysics by Francesca E. -
1I/'Oumuamua As an N2 Ice Fragment of an Exo-Pluto Surface II
manuscript submitted to Journal of Geophysical Research 1I/‘Oumuamua as an N2 ice fragment of an exo-pluto surface II: Generation of N2 ice fragments and the origin of ‘Oumuamua S. J. Desch1* and A. P. Jackson1,^ 1School of Earth and Space Exploration, Arizona State University, Tempe, AZ 85287. Corresponding author: Steve Desch ([email protected]) * Corresponding author, ORC-ID 0000-0002-1571-0836 ^ ORC-ID 0000-0003-4393-9520 Key Points: 14 • A dynamical instability in the early Kuiper belt likely ejected ~10 N2 ice fragments from thousands of plutos. • A fragment of N2 ice from an “exo-Pluto” would match all known attributes of the interstellar object 1I/‘Oumuamua. • The dynamical instability in the Kuiper belt experienced by our Solar System may be common among stellar systems. 1 manuscript submitted to Journal of Geophysical Research Abstract The origin of the interstellar object 1I/‘Oumuamua, has defied explanation. In a companion paper (Jackson & Desch, 2021), we show that a body of N2 ice with axes 45 m × 44 m × 7.5 m at the time of observation would be consistent with its albedo, non-gravitational acceleration, and lack of observed CO or CO2 or dust. Here we demonstrate that impacts on the surfaces of Pluto- like Kuiper belt objects (KBOs) would have generated and ejected ~1014 collisional fragments— roughly half of them H2O ice fragments and half of them N2 ice fragments—due to the dynamical instability that depleted the primordial Kuiper belt. We show consistency between these numbers and the frequency with which we would observe interstellar objects like 1I/‘Oumuamua, and more comet-like objects like 2I/Borisov, if other stellar systems eject such objects with efficiency like that of the Sun; we infer that differentiated KBOs and dynamical instabilities that eject impact-generated fragments may be near-universal among extrasolar systems.