The Resonant Population of Asteroids in Librating States of the Ν6 Linear Secular Resonance
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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. -
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1,. ,-- ,-- ~XECKDING PAGE BLANK WT FIL,,q DYNAMICAL EVIDENCE REGARDING THE RELATIONSHIP BETWEEN ASTEROIDS AND METEORITES GEORGE W. WETHERILL Department of Temcltricrl kgnetism ~amregie~mtittition of Washington Washington, D. C. 20025 Meteorites are fragments of small solar system bodies (comets, asteroids and Apollo objects). Therefore they may be expected to provide valuable information regarding these bodies. How- ever, the identification of particular classes of meteorites with particular small bodies or classes of small bodies is at present uncertain. It is very unlikely that any significant quantity of meteoritic material is obtained from typical ac- tive comets. Relatively we1 1-studied dynamical mechanisms exist for transferring material into the vicinity of the Earth from the inner edge of the asteroid belt on an 210~-~year time scale. It seems likely that most iron meteorites are obtained in this way, and a significant yield of complementary differec- tiated meteoritic silicate material may be expected to accom- pany these differentiated iron meteorites. Insofar as data exist, photometric measurements support an association between Apollo objects and chondri tic meteorites. Because Apol lo ob- jects are in orbits which come close to the Earth, and also must be fragmented as they traverse the asteroid belt near aphel ion, there also must be a component of the meteorite flux derived from Apollo objects. Dynamical arguments favor the hypothesis that most Apollo objects are devolatilized comet resiaues. However, plausible dynamical , petrographic, and cosmogonical reasons are known which argue against the simple conclusion of this syllogism, uiz., that chondri tes are of cometary origin. Suggestions are given for future theoretical , observational, experimental investigations directed toward improving our understanding of this puzzling situation. -
Aqueous Alteration on Main Belt Primitive Asteroids: Results from Visible Spectroscopy1
Aqueous alteration on main belt primitive asteroids: results from visible spectroscopy1 S. Fornasier1,2, C. Lantz1,2, M.A. Barucci1, M. Lazzarin3 1 LESIA, Observatoire de Paris, CNRS, UPMC Univ Paris 06, Univ. Paris Diderot, 5 Place J. Janssen, 92195 Meudon Pricipal Cedex, France 2 Univ. Paris Diderot, Sorbonne Paris Cit´e, 4 rue Elsa Morante, 75205 Paris Cedex 13 3 Department of Physics and Astronomy of the University of Padova, Via Marzolo 8 35131 Padova, Italy Submitted to Icarus: November 2013, accepted on 28 January 2014 e-mail: [email protected]; fax: +33145077144; phone: +33145077746 Manuscript pages: 38; Figures: 13 ; Tables: 5 Running head: Aqueous alteration on primitive asteroids Send correspondence to: Sonia Fornasier LESIA-Observatoire de Paris arXiv:1402.0175v1 [astro-ph.EP] 2 Feb 2014 Batiment 17 5, Place Jules Janssen 92195 Meudon Cedex France e-mail: [email protected] 1Based on observations carried out at the European Southern Observatory (ESO), La Silla, Chile, ESO proposals 062.S-0173 and 064.S-0205 (PI M. Lazzarin) Preprint submitted to Elsevier September 27, 2018 fax: +33145077144 phone: +33145077746 2 Aqueous alteration on main belt primitive asteroids: results from visible spectroscopy1 S. Fornasier1,2, C. Lantz1,2, M.A. Barucci1, M. Lazzarin3 Abstract This work focuses on the study of the aqueous alteration process which acted in the main belt and produced hydrated minerals on the altered asteroids. Hydrated minerals have been found mainly on Mars surface, on main belt primitive asteroids and possibly also on few TNOs. These materials have been produced by hydration of pristine anhydrous silicates during the aqueous alteration process, that, to be active, needed the presence of liquid water under low temperature conditions (below 320 K) to chemically alter the minerals. -
The Team Adarsh Rajguru
Asteroid Mapper / Hopper www.inl.gov Mapping and extraction of water from asteroids 1 in the main asteroid belt The team Adarsh Rajguru – University of Southern California (Systems Engineer) Juha Nieminen – University of Southern California (Astronautical Engineer) Nalini Nadupalli – University of Michigan (Electrical & Telecommunications Engineer) Justin Weatherford – George Fox University (Mechanical & Thermal Engineer) Joseph Santora – University of Utah (Chemical & Nuclear Engineer) 2 Mission Objectives Primary Objective – Map and tag the asteroids in the main asteroid belt for water. Secondary Objective – Potentially land on these water-containing asteroids, extract the water and use it as a propellant. Tertiary Objective – Map the asteroids for other important materials that can be valuable for resource utilization. 3 Introduction: Asteroid Commodities and Markets Water – Propellant and life support for future manned deep-space missions (Mapping market) Platinum group metals – Valuable on Earth and hence for future unmanned or manned deep-space mining missions (Mapping market) Regolith – Radiation shielding, 3D printing of structures (fuel tanks, trusses, etc.) for deep-space unmanned or manned spacecrafts, (Determining Regolith composition and material properties market) Aluminum, Iron, Nickel, Silicon and Titanium – Valuable structural materials for deep-space unmanned and manned colonies (Mapping market) 4 Asteroid Hopping: Main Asteroid Belt Class and Types (most interested) Resource Water Platinum Group Metals Metals Asteroid Class Type Hydrated C-Class M-Class M-Class Population (%) 10 5 5 Density (kg/m3) 1300 5300 5300 Resource Mass Fraction 8 % 35 ppm 88 % Asteroid Diameter (10 m) 44 tons 2 x 103 tons 97 kg Asteroid Diameter (100 m) 4350 tons 2 x 106 tons 97 tons Asteroid Diameter (500 m) 11000 tons 3 x 108 tons 12 x 103 tons [1] Badescu V., Asteroids: Prospective Energy and Material Resources, First edition, 2013. -
The Handbook of the British Astronomical Association
THE HANDBOOK OF THE BRITISH ASTRONOMICAL ASSOCIATION 2012 Saturn’s great white spot of 2011 2011 October ISSN 0068-130-X CONTENTS CALENDAR 2012 . 2 PREFACE. 3 HIGHLIGHTS FOR 2012. 4 SKY DIARY . .. 5 VISIBILITY OF PLANETS. 6 RISING AND SETTING OF THE PLANETS IN LATITUDES 52°N AND 35°S. 7-8 ECLIPSES . 9-15 TIME. 16-17 EARTH AND SUN. 18-20 MOON . 21 SUN’S SELENOGRAPHIC COLONGITUDE. 22 MOONRISE AND MOONSET . 23-27 LUNAR OCCULTATIONS . 28-34 GRAZING LUNAR OCCULTATIONS. 35-36 PLANETS – EXPLANATION OF TABLES. 37 APPEARANCE OF PLANETS. 38 MERCURY. 39-40 VENUS. 41 MARS. 42-43 ASTEROIDS AND DWARF PLANETS. 44-60 JUPITER . 61-64 SATELLITES OF JUPITER . 65-79 SATURN. 80-83 SATELLITES OF SATURN . 84-87 URANUS. 88 NEPTUNE. 89 COMETS. 90-96 METEOR DIARY . 97-99 VARIABLE STARS . 100-105 Algol; λ Tauri; RZ Cassiopeiae; Mira Stars; eta Geminorum EPHEMERIDES OF DOUBLE STARS . 106-107 BRIGHT STARS . 108 ACTIVE GALAXIES . 109 INTERNET RESOURCES. 110-111 GREEK ALPHABET. 111 ERRATA . 112 Front Cover: Saturn’s great white spot of 2011: Image taken on 2011 March 21 00:10 UT by Damian Peach using a 356mm reflector and PGR Flea3 camera from Selsey, UK. Processed with Registax and Photoshop. British Astronomical Association HANDBOOK FOR 2012 NINETY-FIRST YEAR OF PUBLICATION BURLINGTON HOUSE, PICCADILLY, LONDON, W1J 0DU Telephone 020 7734 4145 2 CALENDAR 2012 January February March April May June July August September October November December Day Day Day Day Day Day Day Day Day Day Day Day Day Day Day Day Day Day Day Day Day Day Day Day Day of of of of of of of of of of of of of of of of of of of of of of of of of Month Week Year Week Year Week Year Week Year Week Year Week Year Week Year Week Year Week Year Week Year Week Year Week Year 1 Sun. -
(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. -
The Minor Planet Bulletin, It Is a Pleasure to Announce the Appointment of Brian D
THE MINOR PLANET BULLETIN OF THE MINOR PLANETS SECTION OF THE BULLETIN ASSOCIATION OF LUNAR AND PLANETARY OBSERVERS VOLUME 33, NUMBER 1, A.D. 2006 JANUARY-MARCH 1. LIGHTCURVE AND ROTATION PERIOD Observatory (Observatory code 926) near Nogales, Arizona. The DETERMINATION FOR MINOR PLANET 4006 SANDLER observatory is located at an altitude of 1312 meters and features a 0.81 m F7 Ritchey-Chrétien telescope and a SITe 1024 x 1024 x Matthew T. Vonk 24 micron CCD. Observations were conducted on (UT dates) Daniel J. Kopchinski January 29, February 7, 8, 2005. A total of 37 unfiltered images Amanda R. Pittman with exposure times of 120 seconds were analyzed using Canopus. Stephen Taubel The lightcurve, shown in the figure below, indicates a period of Department of Physics 3.40 ± 0.01 hours and an amplitude of 0.16 magnitude. University of Wisconsin – River Falls 410 South Third Street Acknowledgements River Falls, WI 54022 [email protected] Thanks to Michael Schwartz and Paulo Halvorcem for their great work at Tenagra Observatory. (Received: 25 July) References Minor planet 4006 Sandler was observed during January Schmadel, L. D. (1999). Dictionary of Minor Planet Names. and February of 2005. The synodic period was Springer: Berlin, Germany. 4th Edition. measured and determined to be 3.40 ± 0.01 hours with an amplitude of 0.16 magnitude. Warner, B. D. and Alan Harris, A. (2004) “Potential Lightcurve Targets 2005 January – March”, www.minorplanetobserver.com/ astlc/targets_1q_2005.htm Minor planet 4006 Sandler was discovered by the Russian astronomer Tamara Mikhailovna Smirnova in 1972. (Schmadel, 1999) It orbits the sun with an orbit that varies between 2.058 AU and 2.975 AU which locates it in the heart of the main asteroid belt. -
Machine Learning Classification of New Asteroid Families Members
MNRAS 496, 540–549 (2020) doi:10.1093/mnras/staa1463 Advance Access publication 2020 May 28 Machine learning classification of new asteroid families members 1‹ 2 3 1 1 V. Carruba , S. Aljbaae, R. C. Domingos, A. Lucchini and P. Furlaneto Downloaded from https://academic.oup.com/mnras/article-abstract/496/1/540/5848208 by Instituto Nacional de Pesquisas Espaciais user on 04 August 2020 1School of Natural Sciences and Engineering, Sao˜ Paulo State University (UNESP), Guaratingueta,´ SP 12516-410, Brazil 2National Space Research Institute (INPE), Division of Space Mechanics and Control, C.P. 515, Sao˜ Jose´ dos Campos, SP 12227-310, Brazil 3Sao˜ Paulo State University (UNESP), Sao Joao˜ da Boa Vista, SP 13874-149, Brazil Accepted 2020 May 21. Received 2020 May 19; in original form 2020 March 20 ABSTRACT Asteroid families are groups of asteroids that are the product of collisions or of the rotational fission of a parent object. These groups are mainly identified in proper elements or frequencies domains. Because of robotic telescope surveys, the number of known asteroids has increased from 10 000 in the early 1990s to more than 750 000 nowadays. Traditional approaches for identifying new members of asteroid families, like the hierarchical clustering method (HCM), may struggle to keep up with the growing rate of new discoveries. Here we used machine learning classification algorithms to identify new family members based on the orbital distribution in proper (a, e,sin(i)) of previously known family constituents. We compared the outcome of nine classification algorithms from stand-alone and ensemble approaches. The extremely randomized trees (ExtraTree) method had the highest precision, enabling to retrieve up to 97 per cent of family members identified with standard HCM. -
Evidence for Asteroid Space Weathering from the Sloan Digital Sky Survey
Icarus 173 (2005) 132–152 www.elsevier.com/locate/icarus Evidence for asteroid space weathering from the Sloan Digital Sky Survey David Nesvorný a,∗, Robert Jedicke b, Robert J. Whiteley c, Željko Ivezic´ d a Southwest Research Institute, 1050 Walnut St, Suite 400, Boulder, CO 80302, USA b Institute for Astronomy, 2680 Woodlawn Drive, Honolulu, HI 96822, USA c Lunar and Planetary Laboratory, University of Arizona, Tucson, AZ 85721, USA d Princeton University Observatory, Princeton, NJ 08544, USA Received 11 April 2004; revised 29 July 2004 Available online 12 October 2004 Abstract By studying color variations between young and old asteroid families we find evidence for processes that modify colors of asteroids over time. We show that colors of aging surfaces of S-type asteroids become increasingly ‘redder’ and measure the rate of these spectral changes. ≈ −1 × We estimate that the mean spectral slope between 0.35 and 0.9 µm increases with time t (given in My) as 0.01 µm log10 t.This empirical fit is valid only for 2.5 t 3000 My (the time interval where we have data) and for the mean spectral slope determined from wide-wavelength filter photometry obtained by the Sloan Digital Sky Survey. We also find that Gy-old terrains of S-type asteroids reflect about 15% more light at ∼ 1-µm wavelengths than an ∼ 5-My-old S-type asteroid surface when the flux is normalized by the reflected light at 0.55 µm. We attribute these effects to space weathering. This result has important implications for asteroid geology and the origin of meteorites that reach the Earth. -
The Minor Planet Bulletin Semi-Major Axis of 2.317 AU, Eccentricity 0.197, Inclination 7.09 (Warner Et Al., 2018)
THE MINOR PLANET BULLETIN OF THE MINOR PLANETS SECTION OF THE BULLETIN ASSOCIATION OF LUNAR AND PLANETARY OBSERVERS VOLUME 45, NUMBER 3, A.D. 2018 JULY-SEPTEMBER 215. LIGHTCURVE ANALYSIS FOR TWO NEAR-EARTH 320ʺ/min during the close approach. The eclipse was observed, ASTEROIDS ECLIPSED BY EARTH’S SHADOW within minutes of the original prediction. Preliminary rotational and eclipse lightcurves were made available soon after the close Peter Birtwhistle approach (Birtwhistle, 2012; Birtwhistle, 2013; Miles, 2013) but it Great Shefford Observatory should be noted that a possible low amplitude 8.7 h period (Miles, Phlox Cottage, Wantage Road 2013) has been discounted in this analysis. Great Shefford, Berkshire, RG17 7DA United Kingdom Several other near-Earth asteroids are known to have been [email protected] eclipsed by the Earth’s shadow, e.g. 2008 TC3 and 2014 AA (both before impacting Earth), 2012 KT42, and 2016 VA (this paper) (Received 2018 March18) but internet searches have not found any eclipse lightcurves. The asteroid lightcurve database (LCDB; Warner et al., 2009) lists a Photometry was obtained from Great Shefford reference to an unpublished result for 2012 XE54 by Pollock Observatory of near-Earth asteroids 2012 XE54 in 2012 (2013) without lightcurve details, but these have been provided on and 2016 VA in 2016 during close approaches. A request and give the rotation period as 0.02780 ± 0.00002 h, superfast rotation period has been determined for 2012 amplitude 0.33 mag derived from 101 points over a period of 30 XE54 and H-G magnitude system coefficients have been minutes for epoch 2012 Dec 10.2 UT at phase angle 19.5°, estimated for 2016 VA. -
Footprints of a Possible Ceres Asteroid Paleo-Family
Mon. Not. R. Astron. Soc. 000, 1–12 (2016) Printed 8 October 2018 (MN LATEX style file v2.2) Footprints of a possible Ceres asteroid paleo-family V. Carruba1,2⋆, D. Nesvorn´y,2, S. Marchi2, S. Aljbaae1 1UNESP, Univ. Estadual Paulista, Grupo de dinˆamica Orbital e Planetologia, Guaratinguet´a, SP, 12516-410, Brazil. 2Department of Space Studies, Southwest Research Institute, Boulder, CO, 80302, USA. Accepted 2016 February 15. Received 2016 February 15; in original form 2016 January 8. ABSTRACT Ceres is the largest and most massive body in the asteroid main belt. Observational data from the Dawn spacecraft reveal the presence of at least two impact craters about 280 km in diameter on the Ceres surface, that could have expelled a significant num- ber of fragments. Yet, standard techniques for identifying dynamical asteroid families have not detected any Ceres family. In this work, we argue that linear secular reso- nances with Ceres deplete the population of objects near Ceres. Also, because of the high escape velocity from Ceres, family members are expected to be very dispersed, with a considerable fraction of km-sized fragments that should be able to reach the pristine region of the main belt, the area between the 5J:-2A and 7J:-3A mean-motion resonances, where the observed number of asteroids is low. Rather than looking for possible Ceres family members near Ceres, here we propose to search in the pristine re- gion. We identified 156 asteroids whose taxonomy, colors, albedo could be compatible with being fragments from Ceres. Remarkably, most of these objects have inclinations near that of Ceres itself. -
Klio, Chaldaea, Chimaera, and Svea
A&A 630, A141 (2019) Astronomy https://doi.org/10.1051/0004-6361/201935992 & © ESO 2019 Astrophysics The last pieces of the primitive inner belt puzzle: Klio, Chaldaea, Chimaera, and Svea? David Morate1, Julia de León2,3, Mário De Prá4, Javier Licandro2,3, Noemí Pinilla-Alonso4,5, Humberto Campins6, Anicia Arredondo6, Jorge Marcio Carvano1, Daniela Lazzaro1, and Antonio Cabrera-Lavers2,7 1 Observatório Nacional, Coordenação de Astronomia e Astrofísica, 20921-400 Rio de Janeiro, Brazil e-mail: [email protected] 2 Instituto de Astrofísica de Canarias (IAC), C/Vía Láctea s/n, 38205 La Laguna, Tenerife, Spain 3 Departamento de Astrofísica, Universidad de La Laguna, 38205 La Laguna, Tenerife, Spain 4 Florida Space Institute, University of Central Florida, Orlando, FL 32816, USA 5 Arecibo Observatory, University of Central Florida, HC-3 Box 53995, Arecibo 00612, Puerto Rico 6 Physics Department, University of Central Florida, PO Box 162385, Orlando, FL 32816-2385, USA 7 GTC Project Office, 38205 La Laguna, Tenerife, Spain Received 30 May 2019 / Accepted 16 July 2019 ABSTRACT Aims. Several primitive families in the inner region of the main asteroid belt were identified as potential sources for two near-Earth asteroids (NEAs), (101955) Bennu and (162173) Ryugu, targets of the sample-return missions OSIRIS-REx and Hayabusa2, respec- tively. Four of the families, located at high proper inclinations (i > 10◦), have not yet been compositionally studied: Klio, Chaldaea, Chimaera, and Svea. We want to characterize and analyze these families within the context of our PRIMitive Asteroid Spectroscopic Survey (PRIMASS), in order to complete the puzzle of the origins of the two NEAs.