Dynamics of the Hungaria Asteroids
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Dynamical Evolution of the Hungaria Asteroids ⇑ Firth M
Icarus 210 (2010) 644–654 Contents lists available at ScienceDirect Icarus journal homepage: www.elsevier.com/locate/icarus Dynamical evolution of the Hungaria asteroids ⇑ Firth M. McEachern, Matija C´ uk , Sarah T. Stewart Department of Earth and Planetary Sciences, Harvard University, 20 Oxford Street, Cambridge, MA 02138, USA article info abstract Article history: The Hungarias are a stable asteroid group orbiting between Mars and the main asteroid belt, with high Received 29 June 2009 inclinations (16–30°), low eccentricities (e < 0.18), and a narrow range of semi-major axes (1.78– Revised 2 August 2010 2.06 AU). In order to explore the significance of thermally-induced Yarkovsky drift on the population, Accepted 7 August 2010 we conducted three orbital simulations of a 1000-particle grid in Hungaria a–e–i space. The three simu- Available online 14 August 2010 lations included asteroid radii of 0.2, 1.0, and 5.0 km, respectively, with run times of 200 Myr. The results show that mean motion resonances—martian ones in particular—play a significant role in the destabili- Keywords: zation of asteroids in the region. We conclude that either the initial Hungaria population was enormous, Asteroids or, more likely, Hungarias must be replenished through collisional or dynamical means. To test the latter Asteroids, Dynamics Resonances, Orbital possibility, we conducted three more simulations of the same radii, this time in nearby Mars-crossing space. We find that certain Mars crossers can be trapped in martian resonances, and by a combination of chaotic diffusion and the Yarkovsky effect, can be stabilized by them. -
The Hungaria Asteroids: Close Encounters and Impacts with Terrestrial Planets
Mem. S.A.It. Suppl. Vol. 26, 38 Memorie della c SAIt 2014 Supplementi The Hungaria Asteroids: close encounters and impacts with terrestrial planets M. A. Galiazzo, A. Bazso, and R. Dvorak Institute of Astronomy, University of Vienna, Turkenschanzstr.¨ 17, A-1180 Wien, Austria e-mail: [email protected] Abstract. The Hungaria asteroid family (Named after (434) Hungaria), which consists of more than 5000 members with semi-major axes between 1.78 and 2.03 AU and have in- clinations of the order of 20◦, is regarded as one source for Near-Earth Asteroids (NEAs). They are mainly perturbed by Jupiter and Mars, and are ejected because of mean motion and secular resonances with these planets and then become Mars-crossers; later they may even cross the orbits of Earth and Venus. We are interested to analyze the close encounters and possible impacts with these planets. For 200 selected objects which are on the edge of the group we integrated their orbits over 100 million years in a simplified model of the planetary system (Mars to Saturn) subject to only gravitational forces. We picked out a sam- ple of 11 objects (each with 50 clones) with large variations in semi-major axis and some of them achieve high inclinations and eccentricities in connection with mean motion and secular resonances which then leads to relatively high velocity impacts on Venus, Earth and Mars. We report all close encounters and impacts with the terrestrial planets and statistically determine the mean life and the orbital distribution of the NEAs of these Hungarias. -
Absolute Magnitudes of Asteroids and a Revision of Asteroid Albedo Estimates from WISE Thermal Observations ⇑ Petr Pravec A, , Alan W
Icarus 221 (2012) 365–387 Contents lists available at SciVerse ScienceDirect Icarus journal homepage: www.elsevier.com/locate/icarus Absolute magnitudes of asteroids and a revision of asteroid albedo estimates from WISE thermal observations ⇑ Petr Pravec a, , Alan W. Harris b, Peter Kušnirák a, Adrián Galád a,c, Kamil Hornoch a a Astronomical Institute, Academy of Sciences of the Czech Republic, Fricˇova 1, CZ-25165 Ondrˇejov, Czech Republic b 4603 Orange Knoll Avenue, La Cañada, CA 91011, USA c Modra Observatory, Department of Astronomy, Physics of the Earth, and Meteorology, FMFI UK, Bratislava SK-84248, Slovakia article info abstract Article history: We obtained estimates of the Johnson V absolute magnitudes (H) and slope parameters (G) for 583 main- Received 27 February 2012 belt and near-Earth asteroids observed at Ondrˇejov and Table Mountain Observatory from 1978 to 2011. Revised 27 July 2012 Uncertainties of the absolute magnitudes in our sample are <0.21 mag, with a median value of 0.10 mag. Accepted 28 July 2012 We compared the H data with absolute magnitude values given in the MPCORB, Pisa AstDyS and JPL Hori- Available online 13 August 2012 zons orbit catalogs. We found that while the catalog absolute magnitudes for large asteroids are relatively good on average, showing only little biases smaller than 0.1 mag, there is a systematic offset of the cat- Keywords: alog values for smaller asteroids that becomes prominent in a range of H greater than 10 and is partic- Asteroids ularly big above H 12. The mean (H H) value is negative, i.e., the catalog H values are Photometry catalog À Infrared observations systematically too bright. -
Hungaria Asteroid Family As the Source of Aubrite Meteorites
Hungaria Asteroid Family as the Source of Aubrite Meteorites Matija Cuk´ 1, Brett J. Gladman2, David Nesvorn´y3 1Carl Sagan Center, SETI Institute 189 North Bernardo Avenue, Mountain View, CA 94043 2Department of Physics and Astronomy, University of British Columbia 6224 Agricultural Road, Vancouver, BC V6T 1Z1, Canada 3Southwest Research Institute 1050 Walnut St, Suite 400, Boulder, CO 80302 E-mail: [email protected] Re-submitted to Icarus May 23rd 2014. Manuscript Pages: 31 Figures: 6 Tables: 2 arXiv:1406.0825v1 [astro-ph.EP] 3 Jun 2014 1 Proposed Running Head: Aubrites from Hungaria Family Editorial Correspondence to: Matija Cuk´ Carl Sagan Center SETI Institute 189 N Bernardo Ave Mountain View, CA 94043 Phone: 650-810-0210 Fax: 650- E-mail: [email protected] 2 ABSTRACT: The Hungaria asteroids are interior to the main asteroid belt, with semimajor axes between 1.8 and 2 AU, low eccentricities and inclinations of 16-35 degrees. Small asteroids in the Hungaria region are dominated by a collisional family associated with (434) Hungaria. The dominant spectral type of the Hungaria group is the E or X-type (Warner et al., 2009), mostly due to the E-type composition of Hungaria and its genetic family. It is widely believed the E-type asteroids are related to the aubrite meteorites, also known as enstatite achondrites (Gaffey et al., 1992). Here we explore the hypothesis that aubrites originate in the Hungaria family. In order to test this connection, we compare model Cosmic Ray Exposure ages from orbital integrations of model meteoroids with those of aubrites. We show that long CRE ages of aubrites (longest among stony meteorite groups) reflect the delivery route of meteoroids from Hungarias to Earth being different than those from main-belt asteroids. -
Mineralogical Variations Among High Albedo E-Type Asteroids: Implications for Asteroid Igneous Processes
Lunar and Planetary Science XXXV (2004) 1812.pdf MINERALOGICAL VARIATIONS AMONG HIGH ALBEDO E-TYPE ASTEROIDS: IMPLICATIONS FOR ASTEROID IGNEOUS PROCESSES. Michael J. Gaffey1 and Michael S. Kelley2, 1Space Studies Department, University of North Dakota, Box 9008, Grand Forks, ND 58202, email: [email protected]; 2Department of Geology and Geography, Georgia Southern University, Statesboro, GA 30460; email: [email protected] The link between the E-type asteroids and the pyroxene-plus-feldspar assemblage. Aubrites are enstatite achondrites (aubrites) was first proposed for mantle rocks from a highly reduced (E-chondrite-like) the original E-asteroid, 44 Nysa [1]. The association parent body(ies) which has undergone melting and was based on the high albedos and the featureless differentiation. The corresponding feldspar-rich spectra shared by the E-asteroids and the aubrites. basaltic rocks have not been identified in the meteorite Among the plausible geologic and meteoritic materials, collections and may have been erupted as gas-driven only enstatite (the magnesium end-member of the pyroclastic materials at velocities sufficient to escape pyroxene solid solution series) is sufficiently abundant their parent bodies and thus never formed discrete to comprise asteroid-sized bodies [2]. However, the lithologic units [7]. The E[I]-subtype probably presence of a weak 0.89 µm absorption feature in the represent mantle (and possibly crustal) material from a spectrum of 44 Nysa indicates that its pyroxene differentiated, highly reduced parent body of contains a small amount of Fe2+ but still substantially approximately enstatite chondrite composition. Based more than any aubrite present in the meteorite on melting experiments on enstatite chondrites, the collection [3]. -
2-Meter Diameter Near-Earth Asteroid 2015 TC25: a Possible Boulder from E-Type Asteroid (44) Nysa
Physical Characterization of ~2-meter Diameter Near-Earth Asteroid 2015 TC25: A possible boulder from E-type Asteroid (44) Nysa Authors: Vishnu Reddy, Juan A. Sanchez, William F. Bottke, Audrey Thirouin, Edgard G. Rivera-Valentin, Michael S. Kelley, William Ryan, Edward A. Cloutis, Stephen C. Tegler, Eileen V. Ryan, Patrick A. Taylor, James E. Richardson, Nicholas Moskovitz, Lucille Le Corre Abstract Small near-Earth asteroids (>20 meters) are interesting because they are progenitors for meteorites in our terrestrial collection. Crucial to our understanding of the effectiveness of our atmosphere in filtering low-strength impactors is the physical characteristics of these small near-Earth asteroids (NEAs). In the past, characterization of small NEAs has been a challenge because of the difficulty in detecting them prior to close Earth flyby. In this study we physically characterized the 2-meter diameter near-Earth asteroid 2015 TC25 using ground-based optical, near-infrared and radar assets during a close flyby of the Earth (distance 69,000 miles) in Oct. 2015. Our observations suggest that its surface composition is similar to aubrites, a rare class of high albedo differentiated meteorites. Aubrites make up only 0.14 % of all know meteorites in our terrestrial meteorite collection. 2015 TC25 is also a very fast rotator with a rotation period of 133 seconds. We compared spectral and dynamical properties of 2015 TC25 and found the best candidate source body in the inner main belt to be the 70-km diameter E-type asteroid (44) Nysa. We attribute difference in spectral slope between the two objects to the lack of regolith on the surface of 2015 TC25. -
Orbit Determination of Eclipsing Binary Asteroids from Photometry
Orbit determination of eclipsing binary asteroids from photometry Petr Scheirich, Petr Pravec Ondrejov obs., Czech Republic and many observers Orbiting couples: "pas de deux" in the Solar System and the Milky Way Paris, October 10-12, 2011 Lightcurve of ordinary asteroid First binaries resolved from photometry 1994 AW1 (Pravec and Hahn, 1997) First binaries resolved from photometry 1996 FG3 (Pravec et al, 2000) Asynchronous binary Models of binaries derived from photometry • 10 NEA binaries (22 oppositions) • 15 MBA binaries (33 oppositions) Where all the data come from? 2006 Why to do photometry of binaries? Why to do photometry of binaries? • poles distribution • dynamical evolution Lightcurve of binary asteroid Primary Secondary Primary event Secondary event Long-period component extraction L.p. component = mutual events + rotation of secondary (The long period component of) Lightcurve simulation – the direct problem Input parameters: • Heliocentric orbit geometry • Keplerian elements of mutual orbit (circular, eccentric) • Shape and size ratio of components • Scattering law Two-axis ellipsoids or any arbitrary shape approximated by polyhedra with triangular facets The lightcurve of the system is computed using simple ray-traycing code. The inverse problem Fitted parameters: • Keplerian elements of mutual orbit: • a/Ap – semimajor axis • lP – ecl. longitude of orbit’s pole • bP – ecl. latitude of orbit’s pole • Porb – sidereal orbital period • L0 – mean length of secondary at given epoch • e – eccentricity • w – argument of pericenter • Shape and size ratio of components: • flattening of primary Ap /Cp, • elongation of secondary As /Cs, • size ratio of both bodies As / Ap Pre-estimates of initial parameters • Synodic orbital period • Components size ratio Pre-estimates of initial parameters Sidereal orbital period and L0 (argument of mean length of secondary for JD0): Visual identification of contacts: Time-increasing L of contacts should lie on a straight line defined by where n = 2/Psid. -
Cumulative Index to Volumes 1-45
The Minor Planet Bulletin Cumulative Index 1 Table of Contents Tedesco, E. F. “Determination of the Index to Volume 1 (1974) Absolute Magnitude and Phase Index to Volume 1 (1974) ..................... 1 Coefficient of Minor Planet 887 Alinda” Index to Volume 2 (1975) ..................... 1 Chapman, C. R. “The Impossibility of 25-27. Index to Volume 3 (1976) ..................... 1 Observing Asteroid Surfaces” 17. Index to Volume 4 (1977) ..................... 2 Tedesco, E. F. “On the Brightnesses of Index to Volume 5 (1978) ..................... 2 Dunham, D. W. (Letter regarding 1 Ceres Asteroids” 3-9. Index to Volume 6 (1979) ..................... 3 occultation) 35. Index to Volume 7 (1980) ..................... 3 Wallentine, D. and Porter, A. Index to Volume 8 (1981) ..................... 3 Hodgson, R. G. “Useful Work on Minor “Opportunities for Visual Photometry of Index to Volume 9 (1982) ..................... 4 Planets” 1-4. Selected Minor Planets, April - June Index to Volume 10 (1983) ................... 4 1975” 31-33. Index to Volume 11 (1984) ................... 4 Hodgson, R. G. “Implications of Recent Index to Volume 12 (1985) ................... 4 Diameter and Mass Determinations of Welch, D., Binzel, R., and Patterson, J. Comprehensive Index to Volumes 1-12 5 Ceres” 24-28. “The Rotation Period of 18 Melpomene” Index to Volume 13 (1986) ................... 5 20-21. Hodgson, R. G. “Minor Planet Work for Index to Volume 14 (1987) ................... 5 Smaller Observatories” 30-35. Index to Volume 15 (1988) ................... 6 Index to Volume 3 (1976) Index to Volume 16 (1989) ................... 6 Hodgson, R. G. “Observations of 887 Index to Volume 17 (1990) ................... 6 Alinda” 36-37. Chapman, C. R. “Close Approach Index to Volume 18 (1991) .................. -
The Minor Planet Bulletin, We Feel Safe in Al., 1989)
THE MINOR PLANET BULLETIN OF THE MINOR PLANETS SECTION OF THE BULLETIN ASSOCIATION OF LUNAR AND PLANETARY OBSERVERS VOLUME 43, NUMBER 3, A.D. 2016 JULY-SEPTEMBER 199. PHOTOMETRIC OBSERVATIONS OF ASTEROIDS star, and asteroid were determined by measuring a 5x5 pixel 3829 GUNMA, 6173 JIMWESTPHAL, AND sample centered on the asteroid or star. This corresponds to a 9.75 (41588) 2000 SC46 by 9.75 arcsec box centered upon the object. When possible, the same comparison star and check star were used on consecutive Kenneth Zeigler nights of observation. The coordinates of the asteroid were George West High School obtained from the online Lowell Asteroid Services (2016). To 1013 Houston Street compensate for the effect on the asteroid’s visual magnitude due to George West, TX 78022 USA ever changing distances from the Sun and Earth, Eq. 1 was used to [email protected] vertically align the photometric data points from different nights when constructing the composite lightcurve: Bryce Hanshaw 2 2 2 2 George West High School Δmag = –2.5 log((E2 /E1 ) (r2 /r1 )) (1) George West, TX USA where Δm is the magnitude correction between night 1 and 2, E1 (Received: 2016 April 5 Revised: 2016 April 7) and E2 are the Earth-asteroid distances on nights 1 and 2, and r1 and r2 are the Sun-asteroid distances on nights 1 and 2. CCD photometric observations of three main-belt 3829 Gunma was observed on 2016 March 3-5. Weather asteroids conducted from the George West ISD Mobile conditions on March 3 and 5 were not particularly favorable and so Observatory are described. -
The Minor Planet Bulletin
THE MINOR PLANET BULLETIN OF THE MINOR PLANETS SECTION OF THE BULLETIN ASSOCIATION OF LUNAR AND PLANETARY OBSERVERS VOLUME 34, NUMBER 3, A.D. 2007 JULY-SEPTEMBER 53. CCD PHOTOMETRY OF ASTEROID 22 KALLIOPE Kwee, K.K. and von Woerden, H. (1956). Bull. Astron. Inst. Neth. 12, 327 Can Gungor Department of Astronomy, Ege University Trigo-Rodriguez, J.M. and Caso, A.S. (2003). “CCD Photometry 35100 Bornova Izmir TURKEY of asteroid 22 Kalliope and 125 Liberatrix” Minor Planet Bulletin [email protected] 30, 26-27. (Received: 13 March) CCD photometry of asteroid 22 Kalliope taken at Tubitak National Observatory during November 2006 is reported. A rotational period of 4.149 ± 0.0003 hours and amplitude of 0.386 mag at Johnson B filter, 0.342 mag at Johnson V are determined. The observation of 22 Kalliope was made at Tubitak National Observatory located at an elevation of 2500m. For this study, the 410mm f/10 Schmidt-Cassegrain telescope was used with a SBIG ST-8E CCD electronic imager. Data were collected on 2006 November 27. 305 images were obtained for each Johnson B and V filters. Exposure times were chosen as 30s for filter B and 15s for filter V. All images were calibrated using dark and bias frames Figure 1. Lightcurve of 22 Kalliope for Johnson B filter. X axis is and sky flats. JD-2454067.00. Ordinate is relative magnitude. During this observation, Kalliope was 99.26% illuminated and the phase angle was 9º.87 (Guide 8.0). Times of observation were light-time corrected. -
Visible and Near Infrared Spectroscopic Investigation of E-Type Asteroids, Including 2867 Steins, a Target of the Rosetta Mission S
Visible and near infrared spectroscopic investigation of E-type asteroids, including 2867 Steins, a target of the Rosetta mission S. Fornasier, A. Migliorini, E. Dotto, M.A. Barucci To cite this version: S. Fornasier, A. Migliorini, E. Dotto, M.A. Barucci. Visible and near infrared spectroscopic investiga- tion of E-type asteroids, including 2867 Steins, a target of the Rosetta mission. Icarus, Elsevier, 2009, 196 (1), pp.119. 10.1016/j.icarus.2008.02.015. hal-00567271 HAL Id: hal-00567271 https://hal.archives-ouvertes.fr/hal-00567271 Submitted on 20 Feb 2011 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. Accepted Manuscript Visible and near infrared spectroscopic investigation of E-type asteroids, including 2867 Steins, a target of the Rosetta mission S. Fornasier, A. Migliorini, E. Dotto, M.A. Barucci PII: S0019-1035(08)00104-8 DOI: 10.1016/j.icarus.2008.02.015 Reference: YICAR 8619 To appear in: Icarus Received date: 10 October 2007 Revised date: 26 February 2008 Accepted date: 28 February 2008 Please cite this article as: S. Fornasier, A. Migliorini, E. Dotto, M.A. Barucci, Visible and near infrared spectroscopic investigation of E-type asteroids, including 2867 Steins, a target of the Rosetta mission, Icarus (2008), doi: 10.1016/j.icarus.2008.02.015 This is a PDF file of an unedited manuscript that has been accepted for publication. -
Asteroids : Space- and Ground-Based Observational Data
C4PO research themes 7. Asteroids : space- and ground-based observational data A. Context and state of the art The ESA cornerstone mission Gaia, that started its 5-years all-sky survey in July 2014, will characterize all astrophysical sources down to V=20, including about 350,000 asteroids, by measuring their position, motion and spectral properties. The ultra-precise astrometry (~25 as at V=15) is the unbeatable driver for Gaia science, promising a revolution in astrophysics, with the first data release at end 2016. Gaia will continue to operate until 2019 (nominal mission) and probably more (extended). The Data Processing and Analysis Consortium of Gaia (DPAC) gathers ~450 scientists and engineers from all over Europe tasked with the mass processing of the data of the mission. The goal of DPAC is to produce a calibrated, first-level data product containing the main properties (positions, proper motions, statistics, classifications, etc.) of the largest possible number of astrophysical objects, as observed by Gaia. More specific analyses, e.g. combination with external data, is excluded from DPAC’s scope – although it is needed to really exploit the advances that Gaia will bring in different branches of astrophysics. Concerning solar system objects, DPAC will produce asteroid positions (by epoch) and provide a first-level physical characterization, including spectral classes from Gaia data. Fig. 1 - The Gaia satellite is continuously However, unleashing the full potential of Gaia will require levels of scanning the sky from the Lagrangian processing well beyond the possibilities of DPAC, in terms of Point “L2” at 1.5 million km from the available manpower and funding.