Asteroid Families Classification
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ESO's VLT Sphere and DAMIT
ESO’s VLT Sphere and DAMIT ESO’s VLT SPHERE (using adaptive optics) and Joseph Durech (DAMIT) have a program to observe asteroids and collect light curve data to develop rotating 3D models with respect to time. Up till now, due to the limitations of modelling software, only convex profiles were produced. The aim is to reconstruct reliable nonconvex models of about 40 asteroids. Below is a list of targets that will be observed by SPHERE, for which detailed nonconvex shapes will be constructed. Special request by Joseph Durech: “If some of these asteroids have in next let's say two years some favourable occultations, it would be nice to combine the occultation chords with AO and light curves to improve the models.” 2 Pallas, 7 Iris, 8 Flora, 10 Hygiea, 11 Parthenope, 13 Egeria, 15 Eunomia, 16 Psyche, 18 Melpomene, 19 Fortuna, 20 Massalia, 22 Kalliope, 24 Themis, 29 Amphitrite, 31 Euphrosyne, 40 Harmonia, 41 Daphne, 51 Nemausa, 52 Europa, 59 Elpis, 65 Cybele, 87 Sylvia, 88 Thisbe, 89 Julia, 96 Aegle, 105 Artemis, 128 Nemesis, 145 Adeona, 187 Lamberta, 211 Isolda, 324 Bamberga, 354 Eleonora, 451 Patientia, 476 Hedwig, 511 Davida, 532 Herculina, 596 Scheila, 704 Interamnia Occultation Event: Asteroid 10 Hygiea – Sun 26th Feb 16h37m UT The magnitude 11 asteroid 10 Hygiea is expected to occult the magnitude 12.5 star 2UCAC 21608371 on Sunday 26th Feb 16h37m UT (= Mon 3:37am). Magnitude drop of 0.24 will require video. DAMIT asteroid model of 10 Hygiea - Astronomy Institute of the Charles University: Josef Ďurech, Vojtěch Sidorin Hygiea is the fourth-largest asteroid (largest is Ceres ~ 945kms) in the Solar System by volume and mass, and it is located in the asteroid belt about 400 million kms away. -
I Corpi Minori Del Sistema Solare
UNIVERSITA' DEGLI STUDI DI BOLOGNA FACOLTA' DI SCIENZE MATEMATICHE, FISICHE E NATURALI Dipartimento di Astronomia Corso di Laurea in Astronomia Materia di Tesi: Astronomia I CORPI MINORI DEL SISTEMA SOLARE Tesi di Laurea di: Relatore: CLAUDIO ELIDORO Chiar.mo Prof. CORRADO BARTOLINI Sessione Autunnale Anno Accademico 1995 - 1996 INDICE INTRODUZIONE 1. UNA VISIONE D'INSIEME 3 2. L'ORIGINE DEL SISTEMA SOLARE 7 3. METODOLOGIE OSSERVATIVE DEI CORPI MINORI 14 PARTE PRIMA: GLI ASTEROIDI 1. NOTA STORICA 17 2. ORIGINE DEGLI ASTEROIDI 19 3. IL RUOLO DEGLI IMPATTI 25 4. FAMIGLIE DINAMICHE 31 5. CLASSIFICAZIONE 39 6. "INCONTRI RAVVICINATI" 48 951 GASPRA 49 243 IDA 52 433 EROS ED I N.E.A. 54 4179 TOUTATIS 61 7. LA TERRA COME BERSAGLIO 65 PARTE SECONDA: LE COMETE 1. NOTA STORICA 81 2. ORIGINE ED EVOLUZIONE 2.1 LA NUBE DI OORT E LA FASCIA DI KUIPER 82 2.2 LE COMETE A CORTO PERIODO 88 2.3 FASI EVOLUTIVE FINALI 94 3. MORFOLOGIA E FENOMENI FISICI CONNESSI 3.1 IL MODELLO DI WHIPPLE 100 3.2 IL NUCLEO 107 3.3 LA CHIOMA 111 3.4 LA CODA 116 PARTE TERZA: KUIPER-BELT OBJECTS 1. NOTA STORICA 119 2. IL SISTEMA PLUTONE - CARONTE 124 3. CHIRONE ED I CENTAURI 128 4. UNA POPOLAZIONE TUTTA DA SCOPRIRE 134 BIBLIOGRAFIA 139 - 2 - INTRODUZIONE 1. UNA VISIONE D'INSIEME Scorrendo le tappe fondamentali della Storia dell'Astronomia, appare evidente come il quadro complessivo del Sistema Solare si sia gradualmente modificato e ampliato man mano che la ricerca e la tecnologia mettevano a disposizione strumenti di indagine più adeguati. -
Asteroid Family Ages. 2015. Icarus 257, 275-289
Icarus 257 (2015) 275–289 Contents lists available at ScienceDirect Icarus journal homepage: www.elsevier.com/locate/icarus Asteroid family ages ⇑ Federica Spoto a,c, , Andrea Milani a, Zoran Knezˇevic´ b a Dipartimento di Matematica, Università di Pisa, Largo Pontecorvo 5, 56127 Pisa, Italy b Astronomical Observatory, Volgina 7, 11060 Belgrade 38, Serbia c SpaceDyS srl, Via Mario Giuntini 63, 56023 Navacchio di Cascina, Italy article info abstract Article history: A new family classification, based on a catalog of proper elements with 384,000 numbered asteroids Received 6 December 2014 and on new methods is available. For the 45 dynamical families with >250 members identified in this Revised 27 April 2015 classification, we present an attempt to obtain statistically significant ages: we succeeded in computing Accepted 30 April 2015 ages for 37 collisional families. Available online 14 May 2015 We used a rigorous method, including a least squares fit of the two sides of a V-shape plot in the proper semimajor axis, inverse diameter plane to determine the corresponding slopes, an advanced error model Keywords: for the uncertainties of asteroid diameters, an iterative outlier rejection scheme and quality control. The Asteroids best available Yarkovsky measurement was used to estimate a calibration of the Yarkovsky effect for each Asteroids, dynamics Impact processes family. The results are presented separately for the families originated in fragmentation or cratering events, for the young, compact families and for the truncated, one-sided families. For all the computed ages the corresponding uncertainties are provided, and the results are discussed and compared with the literature. The ages of several families have been estimated for the first time, in other cases the accu- racy has been improved. -
(704) Interamnia from Its Occultations and Lightcurves
International Journal of Astronomy and Astrophysics, 2014, 4, 91-118 Published Online March 2014 in SciRes. http://www.scirp.org/journal/ijaa http://dx.doi.org/10.4236/ijaa.2014.41010 A 3-D Shape Model of (704) Interamnia from Its Occultations and Lightcurves Isao Satō1*, Marc Buie2, Paul D. Maley3, Hiromi Hamanowa4, Akira Tsuchikawa5, David W. Dunham6 1Astronomical Society of Japan, Yamagata, Japan 2Southwest Research Institute, Boulder, USA 3International Occultation Timing Association, Houston, USA 4Hamanowa Astronomical Observatory, Fukushima, Japan 5Yanagida Astronomical Observatory, Ishikawa, Japan 6International Occultation Timing Association, Greenbelt, USA Email: *[email protected], [email protected], [email protected], [email protected], [email protected], [email protected] Received 9 November 2013; revised 9 December 2013; accepted 17 December 2013 Copyright © 2014 by authors and Scientific Research Publishing Inc. This work is licensed under the Creative Commons Attribution International License (CC BY). http://creativecommons.org/licenses/by/4.0/ Abstract A 3-D shape model of the sixth largest of the main belt asteroids, (704) Interamnia, is presented. The model is reproduced from its two stellar occultation observations and six lightcurves between 1969 and 2011. The first stellar occultation was the occultation of TYC 234500183 on 1996 De- cember 17 observed from 13 sites in the USA. An elliptical cross section of (344.6 ± 9.6 km) × (306.2 ± 9.1 km), for position angle P = 73.4 ± 12.5˚ was fitted. The lightcurve around the occulta- tion shows that the peak-to-peak amplitude was 0.04 mag. and the occultation phase was just be- fore the minimum. -
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. -
Small Vehicle Asteroid Mission Concept
The “Bering” Small Vehicle Asteroid Mission Concept The “Bering” Small Vehicle Asteroid Mission Concept. Rene Michelsen1, Anja Andersen2, Henning Haack3, John L. Jørgensen4, Maurizio Betto4, Peter S. Jørgensen4, 1Astronomical Observatory, University of Copenhagen, Juliane Maries Vej 30, 2100 Copenhagen Denmark, Phone: +45 3532 5929, Fax: +45 3532 5989, e-mail: [email protected] 2Nordita, Blegdamsvej 17, 2100 Copenhagen, Denmark, Phone: +45 3532 5501, Fax: +45 3538 9157, e-mail: [email protected]. 3Geological Museum, University of Copenhagen, Øster Voldgade 5-7, 1350 Copenhagen K, Denmark Phone: +45 3532 2367, Fax: +45 3532 2325, e-mail: [email protected] 4Ørsted*DTU, MIS, Building 327, Technical University of Denmark, 2800 Lyngby, Denmark, Phone +45 4525 3438, Fax: +45 4588 7133, e-mail: [email protected], mbe@…, psj@… Abstract The study of the Asteroids is traditionally performed by means of large Earth based telescopes, by which orbital elements and spectral properties are acquired. Space borne research, has so far been limited to a few occasional flybys and a couple of dedicated flights to a single selected target. While the telescope based research offers precise orbital information, it is limited to the brighter, larger objects, and taxonomy as well as morphology resolution is limited. Conversely, dedicated missions offers detailed surface mapping in radar, visual and prompt gamma, but only for a few selected targets. The dilemma obviously being the resolution vs. distance and the statistics vs. delta-V requirements. Using advanced instrumentation and onboard autonomy, we have developed a space mission concept whose goal is to map the flux, size and taxonomy distributions of the Asteroids. -
Asteroid Family Identification 613
Bendjoya and Zappalà: Asteroid Family Identification 613 Asteroid Family Identification Ph. Bendjoya University of Nice V. Zappalà Astronomical Observatory of Torino Asteroid families have long been known to exist, although only recently has the availability of new reliable statistical techniques made it possible to identify a number of very “robust” groupings. These results have laid the foundation for modern physical studies of families, thought to be the direct result of energetic collisional events. A short summary of the current state of affairs in the field of family identification is given, including a list of the most reliable families currently known. Some likely future developments are also discussed. 1. INTRODUCTION calibrate new identification methods. According to the origi- nal papers published in the literature, Brouwer (1951) used The term “asteroid families” is historically linked to the a fairly subjective criterion to subdivide the Flora family name of the Japanese researcher Kiyotsugu Hirayama, who delineated by Hirayama. Arnold (1969) assumed that the was the first to use the concept of orbital proper elements to asteroids are dispersed in the proper-element space in a identify groupings of asteroids characterized by nearly iden- Poisson distribution. Lindblad and Southworth (1971) cali- tical orbits (Hirayama, 1918, 1928, 1933). In interpreting brated their method in such a way as to find good agree- these results, Hirayama made the hypothesis that such a ment with Brouwer’s results. Carusi and Massaro (1978) proximity could not be due to chance and proposed a com- adjusted their method in order to again find the classical mon origin for the members of these groupings. -
Asteroid Regolith Weathering: a Large-Scale Observational Investigation
University of Tennessee, Knoxville TRACE: Tennessee Research and Creative Exchange Doctoral Dissertations Graduate School 5-2019 Asteroid Regolith Weathering: A Large-Scale Observational Investigation Eric Michael MacLennan University of Tennessee, [email protected] Follow this and additional works at: https://trace.tennessee.edu/utk_graddiss Recommended Citation MacLennan, Eric Michael, "Asteroid Regolith Weathering: A Large-Scale Observational Investigation. " PhD diss., University of Tennessee, 2019. https://trace.tennessee.edu/utk_graddiss/5467 This Dissertation 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 Doctoral Dissertations 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 dissertation written by Eric Michael MacLennan entitled "Asteroid Regolith Weathering: A Large-Scale Observational Investigation." I have examined the final electronic copy of this dissertation for form and content and recommend that it be accepted in partial fulfillment of the equirr ements for the degree of Doctor of Philosophy, with a major in Geology. Joshua P. Emery, Major Professor We have read this dissertation and recommend its acceptance: Jeffrey E. Moersch, Harry Y. McSween Jr., Liem T. Tran Accepted for the Council: Dixie L. Thompson Vice Provost and Dean of the Graduate School (Original signatures are on file with official studentecor r ds.) Asteroid Regolith Weathering: A Large-Scale Observational Investigation A Dissertation Presented for the Doctor of Philosophy Degree The University of Tennessee, Knoxville Eric Michael MacLennan May 2019 © by Eric Michael MacLennan, 2019 All Rights Reserved. -
Size–Frequency Distributions of Fragments from SPH/N-Body Simulations of Asteroid Impacts: Comparison with Observed Asteroid Families
Icarus 186 (2007) 498–516 www.elsevier.com/locate/icarus Size–frequency distributions of fragments from SPH/N-body simulations of asteroid impacts: Comparison with observed asteroid families Daniel D. Durda a,∗, William F. Bottke Jr. a, David Nesvorný a, Brian L. Enke a, William J. Merline a, Erik Asphaug b, Derek C. Richardson c a Southwest Research Institute, 1050 Walnut Street, Suite 400, Boulder, CO 80302, USA b Earth Sciences Department, University of California Santa Cruz, Santa Cruz, CA 95064, USA c Department of Astronomy, University of Maryland, College Park, MD 20742, USA Received 12 May 2006; revised 1 September 2006 Available online 28 November 2006 Abstract We investigate the morphology of size–frequency distributions (SFDs) resulting from impacts into 100-km-diameter parent asteroids, repre- sented by a suite of 161 SPH/N-body simulations conducted to study asteroid satellite formation [Durda, D.D., Bottke, W.F., Enke, B.L., Merline, W.J., Asphaug, E., Richardson, D.C., Leinhardt, Z.M., 2004. Icarus 170, 243–257]. The spherical basalt projectiles range in diameter from 10 to 46 km (in equally spaced mass increments in logarithmic space, covering six discrete sizes), impact speeds range from 2.5 to 7 km/s (generally in ◦ ◦ ◦ 1km/s increments), and impact angles range from 15 to 75 (nearly head-on to very oblique) in 15 increments. These modeled SFD morpholo- gies match very well the observed SFDs of many known asteroid families. We use these modeled SFDs to scale to targets both larger and smaller than 100 km in order to gain insights into the circumstances of the impacts that formed these families. -
8 Minor Planet Bulletin 40 (2013)
8 2 of the Trojan100 and 5 of the Hilda100 have published LIGHTCURVES FOR 1896 BEER, 2574 LADOGA, information on pole position/ shape as indicated by a “Y” in the 3301 JANSJE, 3339 TRESHNIKOV, 3833 CALINGASTA, SAM column in LC_SUM_PUB.TXT. 3899 WICHTERLE, 4106 NADA, 4801 OHRE, 4808 BALLAERO, AND (8487) 1989 SQ Information for observing Hildas. To assist observers who might wish to observe lightcurves of Hildas, I have prepared tables on my Larry E. Owings website showing the basic circumstances of the oppositions of each Barnes Ridge Observatory of the Hilda100 objects for the next 8 years. For example, here is 23220 Barnes Lane the entry for 1911 Schubart, the first object in the Hilda100 list that Colfax, CA 95713 USA has no published lightcurve information: [email protected] 1911 Schubart (1973 UD) (Received: 20 August) 2012-Sep-24 /=+02 mag=15.7 elong=177.9 r=4.1 2013-Nov-21 /=+21 mag=14.9 elong=178.3 r=3.5 2015-Feb-04 /=+15 mag=14.7 elong=178.8 r=3.4 Lightcurve observations have yielded period / 2016-Apr-09 =-09 mag=15.5 elong=177.8 r=3.9 determinations for the following asteroids: 1896 Beer, 2017-May-26 /=-22 mag=16.1 elong=178.5 r=4.4 2018-Jul-05 /=-22 mag=16.3 elong=179.9 r=4.6 2574 Ladoga, 3301 Jansje, 3339 Treshnikov, 2019-Aug-13 /=-13 mag=16.2 elong=178.8 r=4.5 3833 Calingasta, 3899 Wichterle, 4106 Nada, 4801 Ohre, 4808 Ballaero, and (8487) 1989 SQ. -
ALBEDOS of CENTAURS, JOVIAN TROJANS and HILDAS Submitted
Draft version April 30, 2018 Typeset using LATEX preprint style in AASTeX61 ALBEDOS OF CENTAURS, JOVIAN TROJANS AND HILDAS W. Romanishin1,2 and S. C. Tegler3 1Emeritus Professor, University of Oklahoma 21933 Whispering Pines Circle, Norman, OK 73072 3Department of Physics and Astronomy, Northern Arizona University, Flagstaff, AZ 86011, USA (Received; Revised; Accepted 30 April 2018) Submitted to AJ ABSTRACT We present optical V band albedo distributions for middle solar system minor bodies including Centaurs, Jovian Trojans and Hildas. Diameters come mostly from the NEOWISE catalog. Optical photometry (H values) for about 2/3 of the ∼2700 objects studied are from Pan-STARRS, supple- mented by H values from JPL Horizons (corrected to the Pan-STARRS photometric system). Optical data for Centaurs are from our previously published work. The albedos presented here should be su- perior to previous work because of the use of the Pan-STARRS optical data, which is a homogeneous dataset that has been transformed to standard V magnitudes. We compare the albedo distributions of pairs of samples using the nonparametric Wilcoxon test. We strengthen our previous findings that gray Centaurs have lower albedos than red Centaurs. The gray Centaurs have albedos that are not significantly different from those of the Trojans, suggesting a common origin for Trojans and gray Centaurs. The Trojan L4 and L5 clouds have median albedos that differ by ∼ 10% at a very high level of statistical significance, but the modes of their albedo distributions differ by only ∼ 1%. We suggest the presence of a common “true background” in the two clouds, with an additional more reflective component in the L4 cloud. -
The Minor Planet Bulletin
THE MINOR PLANET BULLETIN OF THE MINOR PLANETS SECTION OF THE BULLETIN ASSOCIATION OF LUNAR AND PLANETARY OBSERVERS VOLUME 38, NUMBER 2, A.D. 2011 APRIL-JUNE 71. LIGHTCURVES OF 10452 ZUEV, (14657) 1998 YU27, AND (15700) 1987 QD Gary A. Vander Haagen Stonegate Observatory, 825 Stonegate Road Ann Arbor, MI 48103 [email protected] (Received: 28 October) Lightcurve observations and analysis revealed the following periods and amplitudes for three asteroids: 10452 Zuev, 9.724 ± 0.002 h, 0.38 ± 0.03 mag; (14657) 1998 YU27, 15.43 ± 0.03 h, 0.21 ± 0.05 mag; and (15700) 1987 QD, 9.71 ± 0.02 h, 0.16 ± 0.05 mag. Photometric data of three asteroids were collected using a 0.43- meter PlaneWave f/6.8 corrected Dall-Kirkham astrograph, a SBIG ST-10XME camera, and V-filter at Stonegate Observatory. The camera was binned 2x2 with a resulting image scale of 0.95 arc- seconds per pixel. Image exposures were 120 seconds at –15C. Candidates for analysis were selected using the MPO2011 Asteroid Viewing Guide and all photometric data were obtained and analyzed using MPO Canopus (Bdw Publishing, 2010). Published asteroid lightcurve data were reviewed in the Asteroid Lightcurve Database (LCDB; Warner et al., 2009). The magnitudes in the plots (Y-axis) are not sky (catalog) values but differentials from the average sky magnitude of the set of comparisons. The value in the Y-axis label, “alpha”, is the solar phase angle at the time of the first set of observations. All data were corrected to this phase angle using G = 0.15, unless otherwise stated.