A Study of 3-Dimensional Shapes of Asteroid Families with an Application to Eos T ⁎ M
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Color Study of Asteroid Families Within the MOVIS Catalog David Morate1,2, Javier Licandro1,2, Marcel Popescu1,2,3, and Julia De León1,2
A&A 617, A72 (2018) Astronomy https://doi.org/10.1051/0004-6361/201832780 & © ESO 2018 Astrophysics Color study of asteroid families within the MOVIS catalog David Morate1,2, Javier Licandro1,2, Marcel Popescu1,2,3, and Julia de León1,2 1 Instituto de Astrofísica de Canarias (IAC), C/Vía Láctea s/n, 38205 La Laguna, Tenerife, Spain e-mail: [email protected] 2 Departamento de Astrofísica, Universidad de La Laguna, 38205 La Laguna, Tenerife, Spain 3 Astronomical Institute of the Romanian Academy, 5 Cu¸titulde Argint, 040557 Bucharest, Romania Received 6 February 2018 / Accepted 13 March 2018 ABSTRACT The aim of this work is to study the compositional diversity of asteroid families based on their near-infrared colors, using the data within the MOVIS catalog. As of 2017, this catalog presents data for 53 436 asteroids observed in at least two near-infrared filters (Y, J, H, or Ks). Among these asteroids, we find information for 6299 belonging to collisional families with both Y J and J Ks colors defined. The work presented here complements the data from SDSS and NEOWISE, and allows a detailed description− of− the overall composition of asteroid families. We derived a near-infrared parameter, the ML∗, that allows us to distinguish between four generic compositions: two different primitive groups (P1 and P2), a rocky population, and basaltic asteroids. We conducted statistical tests comparing the families in the MOVIS catalog with the theoretical distributions derived from our ML∗ in order to classify them according to the above-mentioned groups. We also studied the background populations in order to check how similar they are to their associated families. -
Ice& Stone 2020
Ice & Stone 2020 WEEK 51: DECEMBER 13-19 Presented by The Earthrise Institute # 51 Authored by Alan Hale COMET OF THE WEEK: The Great Comet of 1680 Perihelion: 1680 December 18.49, q = 0.006 AU The Great Comet of 1680 over Rotterdam in The Netherlands, during late December 1680 as painted by the Dutch artist Lieve Verschuier. This particular comet was undoubtedly one of the brightest comets of the 17th Century, but it is also one of the most important comets in history from a scientific perspective, and perhaps even from the perspective of overall human history. While there were certainly plenty of superstitions attached to the comet’s appearance, the scientific investigations made of it were among the beginnings of the era in European history we now call The Enlightenment, and indeed, in a sense the Great Comet of 1680 can perhaps be considered as one of the sparks of that era. The significance began with the comet’s discovery, which was made on the morning of November 14, 1680, by a German astronomer residing in Coburg, Gottfried Kirch – the first comet ever to be discovered by means of a telescope. It was already around 4th magnitude at that time, and located near the star Regulus in the constellation Leo; from that point it traveled eastward and brightened rapidly, being closest to Earth (0.42 AU) on November 30. By that time it was a conspicuous naked-eye object with a tail 20 to 30 degrees long, and it remained visible for another week before disappearing into morning twilight. -
Cosmic History and a Candidate Parent Asteroid for the Quasicrystal-Bearing Meteorite Khatyrka
COSMIC HISTORY AND A CANDIDATE PARENT ASTEROID FOR THE QUASICRYSTAL-BEARING METEORITE KHATYRKA Matthias M. M. Meier1*, Luca Bindi2,3, Philipp R. Heck4, April I. Neander5, Nicole H. Spring6,7, My E. I. Riebe1,8, Colin Maden1, Heinrich Baur1, Paul J. Steinhardt9, Rainer Wieler1 and Henner Busemann1 1Institute of Geochemistry and Petrology, ETH Zurich, Zurich, Switzerland. 2Dipartimento di Scienze della Terra, Università di Firenze, Florence, Italy. 3CNR-Istituto di Geoscienze e Georisorse, Sezione di Firenze, Florence, Italy. 4Robert A. Pritzker Center for Meteoritics and Polar Studies, Field Museum of Natural History, Chicago, USA. 5De- partment of Organismal Biology and Anatomy, University of Chicago, Chicago, USA. 6School of Earth and Environ- mental Sciences, University of Manchester, Manchester, UK. 7Department of Earth and Atmospheric Sciences, Uni- versity of Alberta, Edmonton, Canada. 8Current address: Department of Terrestrial Magnetism, Carnegie Institution of Washington, Washington, USA. 9Department of Physics, and Princeton Center for Theoretical Science, Princeton University, Princeton, USA. *corresponding author: [email protected]; (office phone: +41 44 632 64 53) Submitted to Earth and Planetary Science Letters. Abstract The unique CV-type meteorite Khatyrka is the only natural sample in which “quasicrystals” and associated crystalline Cu,Al-alloys, including khatyrkite and cupalite, have been found. They are suspected to have formed in the early Solar System. To better understand the origin of these ex- otic phases, and the relationship of Khatyrka to other CV chondrites, we have measured He and Ne in six individual, ~40-μm-sized olivine grains from Khatyrka. We find a cosmic-ray exposure age of about 2-4 Ma (if the meteoroid was <3 m in diameter, more if it was larger). -
Can CO CV Meteorites Come from the Eos Family?
60th Annual Meteoritical Society Meeting 5049.pdf Can CO/CV meteorites come from the Eos family? Eos asteroid family is one of the largest groupings in the main b elt [1] and currently its memb ership consists of more than 480 ob jects [2]. The family is cut by the 9:4 mean-motion resonance with Jupiter, and 5 resonant asteroids have b een found within this resonance [3]. The family memb ers b elong to the rare K taxonomic class and show a sp ectral app earance in b etween C- and S-typ e asteroids [4,5]. Many authors suggest, on the basis of sp ectra and alb edo similarities, that K-typ e asteroids mayhave a mineralogical comp osition close to that of the anhydrous CO/CV carb onaceous chondrites [6,7,8]; however, the sp ec- trum of 221 Eos do es not show clear evidence for the calcium-aluminium-rich inclusions CAI absorption features typical of CO meteorites [9]. In order to test the link b etween CO/CV meteorites and K-typ e aster- oids, in the context of the broader GAPTEC pro ject [10], wehave b egan a massive and long-term numerical integration of a sample of synthetic ob jects aimed at simulating real family memb ers injected into the 9:4 mean-motion resonance. In this analysis, we use the SWIFT RMVS3 integrator package [11,12]. The chaotic region asso ciated with the 9:4 mean-motion resonance spans at least the region b etween 3.026 AU and 3.032 AUatlow eccentricityi.e. -
(2000) Forging Asteroid-Meteorite Relationships Through Reflectance
Forging Asteroid-Meteorite Relationships through Reflectance Spectroscopy by Thomas H. Burbine Jr. B.S. Physics Rensselaer Polytechnic Institute, 1988 M.S. Geology and Planetary Science University of Pittsburgh, 1991 SUBMITTED TO THE DEPARTMENT OF EARTH, ATMOSPHERIC, AND PLANETARY SCIENCES IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY IN PLANETARY SCIENCES AT THE MASSACHUSETTS INSTITUTE OF TECHNOLOGY FEBRUARY 2000 © 2000 Massachusetts Institute of Technology. All rights reserved. Signature of Author: Department of Earth, Atmospheric, and Planetary Sciences December 30, 1999 Certified by: Richard P. Binzel Professor of Earth, Atmospheric, and Planetary Sciences Thesis Supervisor Accepted by: Ronald G. Prinn MASSACHUSES INSTMUTE Professor of Earth, Atmospheric, and Planetary Sciences Department Head JA N 0 1 2000 ARCHIVES LIBRARIES I 3 Forging Asteroid-Meteorite Relationships through Reflectance Spectroscopy by Thomas H. Burbine Jr. Submitted to the Department of Earth, Atmospheric, and Planetary Sciences on December 30, 1999 in Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy in Planetary Sciences ABSTRACT Near-infrared spectra (-0.90 to ~1.65 microns) were obtained for 196 main-belt and near-Earth asteroids to determine plausible meteorite parent bodies. These spectra, when coupled with previously obtained visible data, allow for a better determination of asteroid mineralogies. Over half of the observed objects have estimated diameters less than 20 k-m. Many important results were obtained concerning the compositional structure of the asteroid belt. A number of small objects near asteroid 4 Vesta were found to have near-infrared spectra similar to the eucrite and howardite meteorites, which are believed to be derived from Vesta. -
Clementine Observations of the Zodiacal Light and the Dust Content of the Inner Solar System
Clementine Observations of the Zodiacal Light and the Dust Content of the Inner Solar System Joseph M. Hahn Saint Mary’s University Institute for Computational Astrophysics February 13, 2004 with Herb Zook (NASA/JSC), Bonnie Cooper (OSS), Sunny Sunkara (LPI) 1 What is the Zodiacal Light? The zodiacal light (ZL) is sunlight that is scattered and/or reradiated by interplanetary dust. The inner ZL is observed towards the sun, usually at optical wavelengths. The outer ZL is observed away from the sun, usually at infrared wavelengths. photo by Marco Fulle. 2 Why Study Interplanetary Dust? “Someone unfamiliar with astrophysical problems would certainly consider the study of interplanetary dust as an exercise of pure academic interest and may even smile at the fact that much theoretical machinery is devoted to tiny dust grains” Philippe Lamy, 1975, Ph.D. thesis. 3 Why Study Interplanetary Dust? • Dust are samples of small bodies that formed in remote niches throughout the solar system, and they place constraints on conditions in the solar nebula during the planet–forming epoch. – dust from asteroids tell us of solar nebula conditions at r ∼ 3 AU – dust from long–period Oort Cloud comets tell us of nebula conditions at 5 . r . 30 AU – dust from short–period Jupiter–Family comets tell us of conditions in the Kuiper Belt at r & 30 AU • IF the information carried by dust samples (collected by U2 aircraft, Stardust, spacecraft dust collection experiments, etc.) are indeed decipherable, then their mineralogy will inform us of nebula conditions and its history over 3 . r . 30 AU. • However interpreting this dust requires understanding their sources (asteroid & comets), their spatial distributions, transport mechanisms, and sampling biases (e.g., certain sources may be more effective at delivering dust to your detector than other sources). -
Constraining Meteorite Analogs for the Eos Dynamical Family Via Mineralogical Band Analysis
42nd Lunar and Planetary Science Conference (2011) 2184.pdf CONSTRAINING METEORITE ANALOGS FOR THE EOS DYNAMICAL FAMILY VIA MINERALOGICAL BAND ANALYSIS. P. S. Hardersen1, T. Mothe’-Diniz2, and E. A. Cloutis3. 1University of North Dakota, Department of Space Studies, 4149 University Avenue, 530 Clifford Hall, Box 9008, Grand Forks, ND 58202, [email protected], 2Universidade Federal do Rio de Janeiro/Observatorio do Valongo, Lad. Pedro Antonio, 43-20080-090 Rio de Janeiro, Brazil, [email protected]. 3Department of Geography, University of Winnipeg, Winnipeg, MB R3B 2E9. Introduction: The Eos dynamical family was Two Eos family asteroids in [8] and two additional classified by [1] and is located in the main asteroid belt asteroids in [7] display Band I features only. Table 2 beyond the 5:2 mean-motion resonance. The archetype below shows the derived Band I centers for these as- of the family, 221 Eos, has a = 3.01AU, i = 10.9°, and teroids. e = 0.105. This asteroid family includes 202 members Table 2: according to [1]. Early work by [2] suggested that Eos family members were populated by S-type asteroids, Asteroid Band I (µm) but more recent work by [3] analyzing visible-λ spectra 766 Moguntia 1.068 ± 0.004 suggested compositional diversity, evidence for space 798 Ruth 1.056 ± 0.004 weathering, and possible affinities to the CO and CV 1903 Adzhimushkaj 1.049 ± 0.003 chondrites for the Eos family. [4] and [5] have exam- 2957 Tatsuo 1.044 ± 0.003 ined collisional and dynamical evolution of the Eos family with [4] identifying likely Eos family members Methodology: This work will conduct band center in the 9:4 mean-motion resonance. -
Main-Belt Asteroids with Wise/Neowise: Near-Infrared Albedos
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Caltech Authors The Astrophysical Journal, 791:121 (11pp), 2014 August 20 doi:10.1088/0004-637X/791/2/121 C 2014. The American Astronomical Society. All rights reserved. Printed in the U.S.A. MAIN-BELT ASTEROIDS WITH WISE/NEOWISE: NEAR-INFRARED ALBEDOS Joseph R. Masiero1, T. Grav2, A. K. Mainzer1,C.R.Nugent1,J.M.Bauer1,3, R. Stevenson1, and S. Sonnett1 1 Jet Propulsion Laboratory/Caltech, 4800 Oak Grove Drive, MS 183-601, Pasadena, CA 91109, USA; [email protected], [email protected], [email protected], [email protected], [email protected], [email protected] 2 Planetary Science Institute, Tucson, AZ, USA; [email protected] 3 Infrared Processing and Analysis Center, Caltech, Pasadena, CA, USA Received 2014 May 14; accepted 2014 June 25; published 2014 August 6 ABSTRACT We present revised near-infrared albedo fits of 2835 main-belt asteroids observed by WISE/NEOWISE over the course of its fully cryogenic survey in 2010. These fits are derived from reflected-light near-infrared images taken simultaneously with thermal emission measurements, allowing for more accurate measurements of the near- infrared albedos than is possible for visible albedo measurements. Because our sample requires reflected light measurements, it undersamples small, low-albedo asteroids, as well as those with blue spectral slopes across the wavelengths investigated. We find that the main belt separates into three distinct groups of 6%, 16%, and 40% reflectance at 3.4 μm. -
Physical and Dynamical Properties of Asteroid Families
Zappalà et al.: Properties of Asteroid Families 619 Physical and Dynamical Properties of Asteroid Families V. Zappalà, A. Cellino, A. Dell’Oro Istituto Nazionale di Astrofisica, Osservatorio Astronomico di Torino P. Paolicchi University of Pisa The availability of a number of statistically reliable asteroid families and the independent confirmation of their likely collisional origin from dedicated spectroscopic campaigns has been a major breakthrough, making it possible to develop detailed studies of the physical properties of these groupings. Having been produced in energetic collisional events, families are an invaluable source of information on the physics governing these phenomena. In particular, they provide information about the size distribution of the fragments, and on the overall properties of the original ejection velocity fields. Important results have been obtained during the last 10 years on these subjects, with important implications for the general understanding of the collisional history of the asteroid main belt, and the origin of near-Earth asteroids. Some important problems have been raised from these studies and are currently debated. In particular, it has been difficult so far to reconcile the inferred properties of family-forming events with current understanding of the physics of catastrophic collisional breakup. Moreover, the contribution of families to the overall asteroid inventory, mainly at small sizes, is currently controversial. Recent investigations are also aimed at understanding which kind of dynamical evolution might have affected family members since the time of their formation. In addition to potential consequences on the interpretation of current data, there is some speculative possibility of obtaining some estimate of the ages of these groupings. -
SDSS-Based Taxonomic Classification and Orbital Distribution of Main Belt Asteroids
A&A 510, A43 (2010) Astronomy DOI: 10.1051/0004-6361/200913322 & c ESO 2010 Astrophysics SDSS-based taxonomic classification and orbital distribution of main belt asteroids J. M. Carvano1, P. H. Hasselmann1,2, D. Lazzaro1, and T. Mothé-Diniz2 1 Observatório Nacional (COAA), rua Gal. José Cristino 77, São Cristóvão, CEP 20921-400 Rio de Janeiro RJ, Brazil e-mail: [email protected] 2 Universidade Federal do Rio de Janeiro/Observatório do Valongo, Lad.Pedro Antônio, 43, 20080-090 Rio de Janeiro, Brazil Received 18 September 2009 / Accepted 4 November 2009 ABSTRACT Aims. The present paper aims to derive a new classification scheme for SDSS MOC asteroid colors that is compatible with previous taxonomies based on spectroscopic data. The distribution of these can give important clues to the formation and evolution of this region of the Solar System, as well as to locate candidates with mineralogically interesting spectra for detailed observations. Methods. The methodology is based on the large database SDSS MOC4. Templates of the main taxonomic classes are derived and then used to classify the asteroid observations in the SDSS MOC4. The derived taxonomic scheme is compatible with the Bus taxonomy and is suitable to the peculiarities of the SDSS observations, in particular, the low spectral resolution. Results. Density maps of the seven classes defined by the method reproduce classical results for the background which is mainly dominated by the S p class in the inner belt and by the Xp and the Cp classes beyond 2.8 AU. It also shows new structures, such as the fact that the Xp and Cp seem evenly distributed in the inner belt while in the outer belt the S p class increase in density only at the location of asteroid families. -
Small Bodies in Planetary Systems.Pdf
Lecture Notes in Physics Founding Editors: W. Beiglbock,¨ J. Ehlers, K. Hepp, H. Weidenmuller¨ Editorial Board R. Beig, Vienna, Austria W. Beiglbock,¨ Heidelberg, Germany W. Domcke, Garching, Germany B.-G. Englert, Singapore U. Frisch, Nice, France F. Guinea, Madrid, Spain P. Hanggi,¨ Augsburg, Germany G. Hasinger, Garching, Germany W. Hillebrandt, Garching, Germany R. L. Jaffe, Cambridge, MA, USA W. Janke, Leipzig, Germany H. v. Lohneysen,¨ Karlsruhe, Germany M. Mangano, Geneva, Switzerland J.-M. Raimond, Paris, France D. Sornette, Zurich, Switzerland S. Theisen, Potsdam, Germany D. Vollhardt, Augsburg, Germany W. Weise, Garching, Germany J. Zittartz, Koln,¨ Germany The Lecture Notes in Physics The series Lecture Notes in Physics (LNP), founded in 1969, reports new developments in physics research and teaching – quickly and informally, but with a high quality and the explicit aim to summarize and communicate current knowledge in an accessible way. Books published in this series are conceived as bridging material between advanced grad- uate textbooks and the forefront of research and to serve three purposes: • to be a compact and modern up-to-date source of reference on a well-defined topic • to serve as an accessible introduction to the field to postgraduate students and nonspecialist researchers from related areas • to be a source of advanced teaching material for specialized seminars, courses and schools Both monographs and multi-author volumes will be considered for publication. Edited volumes should, however, consist of a very limited number of contributions only. Pro- ceedings will not be considered for LNP. Volumes published in LNP are disseminated both in print and in electronic formats, the electronic archive being available at springerlink.com. -
Forming the Flora Family: Implications for the Near-Earth Asteroid Population and Large Terrestrial Planet Impactors
The Astronomical Journal, 153:172 (23pp), 2017 April https://doi.org/10.3847/1538-3881/aa64dc © 2017. The American Astronomical Society. All rights reserved. Forming the Flora Family: Implications for the Near-Earth Asteroid Population and Large Terrestrial Planet Impactors David Vokrouhlický1, William F. Bottke2, and David Nesvorný2 1 Institute of Astronomy, Charles University, V Holešovičkách 2, CZ–18000 Prague 8, Czech Republic; [email protected] 2 Department of Space Studies, Southwest Research Institute, 1050 Walnut Street, Suite 300, Boulder, CO 80302, USA Received 2017 February 5; revised 2017 March 3; accepted 2017 March 4; published 2017 March 23 Abstract Formed from a catastrophic collision of a parent body larger than 150 km in diameter, the Flora family is located in the innermost part of the main belt near the n6 secular resonance. Objects in this region, when pushed onto planet- crossing orbits, tend to have relatively high probabilities of striking the Earth. These factors suggest that Flora may be a primary source of present-day LL chondrite-like NEOs and Earth/Moon impactors. To investigate this possibility, we used collisional and dynamical models to track the evolution of Flora family members. We created an initial Flora family and followed test asteroids 1 and 3 km in diameter using a numerical code that accounted for both planetary perturbations and nongravitational effects. Our Flora family members reproduce the observed semimajor axis, eccentricity, and inclination distributions of the real family after 1 to 1.4 Gyr. A consistency with the surface age inferred from crater spatial densities found on (951)Gaspra may favor the latter age.