Asteroid Family Ages. 2015. Icarus 257, 275-289
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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. -
The Minor Planet Bulletin
THE MINOR PLANET BULLETIN OF THE MINOR PLANETS SECTION OF THE BULLETIN ASSOCIATION OF LUNAR AND PLANETARY OBSERVERS VOLUME 36, NUMBER 3, A.D. 2009 JULY-SEPTEMBER 77. PHOTOMETRIC MEASUREMENTS OF 343 OSTARA Our data can be obtained from http://www.uwec.edu/physics/ AND OTHER ASTEROIDS AT HOBBS OBSERVATORY asteroid/. Lyle Ford, George Stecher, Kayla Lorenzen, and Cole Cook Acknowledgements Department of Physics and Astronomy University of Wisconsin-Eau Claire We thank the Theodore Dunham Fund for Astrophysics, the Eau Claire, WI 54702-4004 National Science Foundation (award number 0519006), the [email protected] University of Wisconsin-Eau Claire Office of Research and Sponsored Programs, and the University of Wisconsin-Eau Claire (Received: 2009 Feb 11) Blugold Fellow and McNair programs for financial support. References We observed 343 Ostara on 2008 October 4 and obtained R and V standard magnitudes. The period was Binzel, R.P. (1987). “A Photoelectric Survey of 130 Asteroids”, found to be significantly greater than the previously Icarus 72, 135-208. reported value of 6.42 hours. Measurements of 2660 Wasserman and (17010) 1999 CQ72 made on 2008 Stecher, G.J., Ford, L.A., and Elbert, J.D. (1999). “Equipping a March 25 are also reported. 0.6 Meter Alt-Azimuth Telescope for Photometry”, IAPPP Comm, 76, 68-74. We made R band and V band photometric measurements of 343 Warner, B.D. (2006). A Practical Guide to Lightcurve Photometry Ostara on 2008 October 4 using the 0.6 m “Air Force” Telescope and Analysis. Springer, New York, NY. located at Hobbs Observatory (MPC code 750) near Fall Creek, Wisconsin. -
(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. -
Ages of Asteroid Families Estimated Using the YORP-Eye Method
MNRAS 484, 1815–1828 (2019) doi:10.1093/mnras/sty3446 Advance Access publication 2018 December 31 Ages of asteroid families estimated using the YORP-eye method Paolo Paolicchi ,1‹ F. Spoto,2‹ Z. Knezeviˇ c´3‹ and A. Milani4† 1Department of Physics, University of Pisa, Largo Pontecorvo 3, I-56127 Pisa, Italy 2IMMCE, Observatoire de Paris, Av. Denfert–Rochereau 77, F-75014 Paris, France 3Serbian Academy of Sciences and Arts, Kneza Mihaila 35, 11000 Belgrade, Serbia Downloaded from https://academic.oup.com/mnras/article-abstract/484/2/1815/5267148 by Università di Pisa user on 27 February 2019 4Department of Mathematics, University of Pisa, Largo Pontecorvo 5, I-56127 Pisa, Italy Accepted 2018 December 14. Received 2018 December 13; in original form 2018 October 18 ABSTRACT Recently, we have shown that it is possible, despite several biases and uncertainties, to find footprints of the Yarkovsky–O’Keefe–Radzievskii–Paddack (YORP) effect, concerning the members of asteroid dynamical families, in a plot of the proper semimajor axis versus magnitude (the so-called V-plot). In our previous work, we introduced the concept of the YORP-eye, the depopulated region in the V-plot, whose location can be used to diagnose the age of the family. In this present paper, we complete the analysis using an improved algorithm and an extended data base of families, and we discuss the potential errors arising from uncertainties and from the dispersion of the astronomical data. We confirm that the analysis connected to the search for the YORP-eye can lead to an estimate of the age, which is similar and strongly correlated to that obtained by the analysis of the V-slope size-dependent spreading due to the Yarkovsky effect. -
Effect of Main Belt Perturbers on Asteroid-Pair Age Estimation
A&A 548, A25 (2012) Astronomy DOI: 10.1051/0004-6361/201219847 & c ESO 2012 Astrophysics Effect of main belt perturbers on asteroid-pair age estimation A. Galád1,2 1 Dept. of Astronomy, Physics of the Earth, and Meteorology, FMFI, Comenius University, 842 48 Bratislava, Slovakia e-mail: [email protected] 2 Astronomical Institute, AS CR, 251 65 Ondrejov,ˇ Czech Republic Received 20 June 2012 / Accepted 6 September 2012 ABSTRACT Context. Asteroid-pair age estimations are usually performed by backward integration of possible orbits of pair components, taking planetary perturbations into account along with the Yarkovsky effect. It is assumed that uncertainties coming from the backward integration process itself are small, so to reduce uncertainties in estimations, effort usually focuses on reducing uncertainties in the initial orbital elements and the dimensions of the pair components. Aims. This work aims to evaluate the role of the frequently ignored nonplanetary perturbers in asteroid-pair age estimation. When their role is not negligible, the ages of the youngest known pairs can be roughly re-estimated. Methods. The orbital evolution of several asteroid-pair components and the close approaches between components during the last ≈43 kyr are investigated. Initially, the force equations consisted of only planetary perturbers. The three largest main belt perturbers were added afterwards. Finally, as many as 262 massive main belt perturbers were included. The effect of main belters on age estimation is assessed by comparing the dates of the closest approaches between pair components. The range of the Yarkovsky effect is simulated very roughly, only for comparison purposes. -
Dynamical Evolution of V-Type Asteroids in the Central Main Belt
MNRAS Advance Access published February 24, 2014 MNRAS (2014) doi:10.1093/mnras/stu192 Dynamical evolution of V-type asteroids in the central main belt V. Carruba,1‹ M. E. Huaman,1 R. C. Domingos,1,2 C. R. Dos Santos1 and D. Souami3,4,5 1UNESP, Univ. Estadual Paulista, Grupo de dinamicaˆ Orbital e Planetologia, Guaratingueta,´ SP 12516-410, Brazil 2INPE, Instituto Nacional de Pesquisas Espaciais, So Jos dos Campos, SP 12227-010, Brazil 3NAXYS, Namur Center for Complex Systems, Department of Mathematics, University of Namur, B-5000 Namur, Belgium 4UPMC, Universite´ Pierre et Marie Curie, 4 Place Jussieu, F-75005 Paris, France 5SYRTE, Observatoire de Paris, Systemes` de Ref´ erence´ Temps Espace, CNRS/UMR 8630, UPMC, Paris, France Downloaded from Accepted 2014 January 24. Received 2014 January 23; in original form 2013 December 9 ABSTRACT V-type asteroids are associated with basaltic composition, and are supposed to be fragments of crust of differentiated objects. Most V-type asteroids in the main belt are found in the http://mnras.oxfordjournals.org/ inner main belt, and are either current members of the Vesta dynamical family (Vestoids), or past members that drifted away. However, several V-type photometric candidates have been recently identified in the central and outer main belt. The origin of this large population of V-type objects is not well understood. Since it seems unlikely that Vestoids crossing the 3J:-1A mean-motion resonance with Jupiter could account for the whole population of V-type asteroids in the central and outer main belt, origin from local sources, such as the parent bodies of the Eunomia, and of the Merxia and Agnia asteroid families, has been proposed as an alternative mechanism. -
The Minor Planet Bulletin 44 (2017) 142
THE MINOR PLANET BULLETIN OF THE MINOR PLANETS SECTION OF THE BULLETIN ASSOCIATION OF LUNAR AND PLANETARY OBSERVERS VOLUME 44, NUMBER 2, A.D. 2017 APRIL-JUNE 87. 319 LEONA AND 341 CALIFORNIA – Lightcurves from all sessions are then composited with no TWO VERY SLOWLY ROTATING ASTEROIDS adjustment of instrumental magnitudes. A search should be made for possible tumbling behavior. This is revealed whenever Frederick Pilcher successive rotational cycles show significant variation, and Organ Mesa Observatory (G50) quantified with simultaneous 2 period software. In addition, it is 4438 Organ Mesa Loop useful to obtain a small number of all-night sessions for each Las Cruces, NM 88011 USA object near opposition to look for possible small amplitude short [email protected] period variations. Lorenzo Franco Observations to obtain the data used in this paper were made at the Balzaretto Observatory (A81) Organ Mesa Observatory with a 0.35-meter Meade LX200 GPS Rome, ITALY Schmidt-Cassegrain (SCT) and SBIG STL-1001E CCD. Exposures were 60 seconds, unguided, with a clear filter. All Petr Pravec measurements were calibrated from CMC15 r’ values to Cousins Astronomical Institute R magnitudes for solar colored field stars. Photometric Academy of Sciences of the Czech Republic measurement is with MPO Canopus software. To reduce the Fricova 1, CZ-25165 number of points on the lightcurves and make them easier to read, Ondrejov, CZECH REPUBLIC data points on all lightcurves constructed with MPO Canopus software have been binned in sets of 3 with a maximum time (Received: 2016 Dec 20) difference of 5 minutes between points in each bin. -
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. -
On the Astrid Asteroid Family
MNRAS 461, 1605–1613 (2016) doi:10.1093/mnras/stw1445 Advance Access publication 2016 June 16 On the Astrid asteroid family Downloaded from https://academic.oup.com/mnras/article-abstract/461/2/1605/2608554 by Universidade Estadual Paulista J�lio de Mesquita Filho user on 29 May 2019 V. Carruba‹ UNESP, Univ. Estadual Paulista, Grupo de dinamicaˆ Orbital e Planetologia, 12516-410 Guaratingueta,´ SP, Brazil Accepted 2016 June 14. Received 2016 June 10; in original form 2016 May 2 ABSTRACT Among asteroid families, the Astrid family is peculiar because of its unusual inclination distribution. Objects at a 2.764 au are quite dispersed in this orbital element, giving the family a ‘crab-like’ appearance. Recent works showed that this feature is caused by the interaction of the family with the s − sC nodal secular resonance with Ceres, that spreads the inclination of asteroids near its separatrix. As a consequence, the currently observed distribution of the vW component of terminal ejection velocities obtained from inverting Gauss equation is quite leptokurtic, since this parameter mostly depends on the asteroids inclination. The peculiar orbital configuration of the Astrid family can be used to set constraints on key parameters describing the strength of the Yarkovsky force, such as the bulk and surface density and the thermal conductivity of surface material. By simulating various fictitious families with different values of these parameters, and by demanding that the current value of the kurtosis of the distribution in vW be reached over the estimated lifetime of the family, we obtained that the thermal conductivity of Astrid family members should be 0.001 W m−1 K−1, and that the surface and bulk density should be higher than 1000 kg m−3. -
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. -
New Double Stars from Asteroidal Occultations, 1971 - 2008
Vol. 6 No. 1 January 1, 2010 Journal of Double Star Observations Page 88 New Double Stars from Asteroidal Occultations, 1971 - 2008 Dave Herald, Canberra, Australia International Occultation Timing Association (IOTA) Robert Boyle, Carlisle, Pennsylvania, USA Dickinson College David Dunham, Greenbelt, Maryland, USA; Toshio Hirose, Tokyo, Japan; Paul Maley, Houston, Texas, USA; Bradley Timerson, Newark, New York, USA International Occultation Timing Association (IOTA) Tim Farris, Gallatin, Tennessee, USA Volunteer State Community College Eric Frappa and Jean Lecacheux, Paris, France Observatoire de Paris Tsutomu Hayamizu, Kagoshima, Japan Sendai Space Hall Marek Kozubal, Brookline, Massachusetts, USA Clay Center Richard Nolthenius, Aptos, California, USA Cabrillo College and IOTA Lewis C. Roberts, Jr., Pasadena, California, USA California Institute of Technology/Jet Propulsion Laboratory David Tholen, Honolulu, Hawaii, USA University of Hawaii E-mail: [email protected] Abstract: Observations of occultations by asteroids and planetary moons can detect double stars with separations in the range of about 0.3” to 0.001”. This paper lists all double stars detected in asteroidal occultations up to the end of 2008. It also provides a general explanation of the observational method and analysis. The incidence of double stars with a separation in the range 0.001” to 0.1” with a magnitude difference less than 2 is estimated to be about 1%. Vol. 6 No. 1 January 1, 2010 Journal of Double Star Observations Page 89 New Double Stars from Asteroidal Occultations, 1971 - 2008 tions. More detail about the method of analysis is set Introduction out in the Appendix. Asteroids and planetary moons will naturally oc- cult many stars as they move through the sky. -
Asteroidal Source of L Chondrite Meteorites ∗ David Nesvorný A, , David Vokrouhlický A,B, Alessandro Morbidelli A,C, William F
ARTICLE IN PRESS YICAR:8854 JID:YICAR AID:8854 /SCO [m5G; v 1.79; Prn:12/02/2009; 11:10] P.1 (1-4) Icarus ••• (••••) •••–••• Contents lists available at ScienceDirect Icarus www.elsevier.com/locate/icarus Note Asteroidal source of L chondrite meteorites ∗ David Nesvorný a, , David Vokrouhlický a,b, Alessandro Morbidelli a,c, William F. Bottke a a Department of Space Studies, Southwest Research Institute, 1050 Walnut St., Suite 300, Boulder, CO 80302, USA b Institute of Astronomy, Charles University, V Holešoviˇckách2,CZ-18000,Prague8,CzechRepublic c Observatoire de la Côte d’Azur, Boulevard de l’Observatoire, B.P. 4229, 06304 Nice Cedex 4, France article info abstract Article history: Establishing connections between meteorites and their parent asteroids is an important goal of planetary science. Received 28 July 2008 Several links have been proposed in the past, including a spectroscopic match between basaltic meteorites and (4) Revised 19 November 2008 Vesta, that are helping scientists understand the formation and evolution of the Solar System bodies. Here we show Accepted 11 December 2008 that the shocked L chondrite meteorites, which represent about two thirds of all L chondrite falls, may be fragments Available online xxxx of a disrupted asteroid with orbital semimajor axis a = 2.8 AU. This breakup left behind thousands of identified 1– 15 km asteroid fragments known as the Gefion family. Fossil L chondrite meteorites and iridium enrichment found Keywords: in an ≈467 Ma old marine limestone quarry in southern Sweden, and perhaps also ∼5 large terrestrial craters Meteorites with corresponding radiometric ages, may be tracing the immediate aftermath of the family-forming collision when Asteroids numerous Gefion fragments evolved into the Earth-crossing orbits by the 5:2 resonance with Jupiter.