1 Jet Propulsion Laboratory Memorandum IOM 343R-08-003
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The Composition of M-Type Asteroids II: Synthesis of Spectroscopic and Radar Observations ⇑ J.R
Icarus 238 (2014) 37–50 Contents lists available at ScienceDirect Icarus journal homepage: www.elsevier.com/locate/icarus The composition of M-type asteroids II: Synthesis of spectroscopic and radar observations ⇑ J.R. Neeley a,b,1, , B.E. Clark a,1, M.E. Ockert-Bell a,1, M.K. Shepard c,2, J. Conklin d, E.A. Cloutis e, S. Fornasier f, S.J. Bus g a Department of Physics, Ithaca College, Ithaca, NY 14850, United States b Department of Physics, Iowa State University, Ames, IA 50011, United States c Department of Geography and Geosciences, Bloomsburg University, Bloomsburg, PA 17815, United States d Department of Mathematics, Ithaca College, Ithaca, NY 14850, United States e Department of Geography, University of Winnipeg, Winnipeg, MB R3B 2E9, Canada f LESIA, Observatoire de Paris, 5 Place Jules Janssen, F-92195 Meudon Principal Cedex, France g Institute for Astronomy, 2680 Woodlawn Dr., Honolulu, HI 96822, United States article info abstract Article history: This work updates and expands on results of our long-term radar-driven observational campaign of Received 7 February 2012 main-belt asteroids (MBAs) focused on Bus–DeMeo Xc- and Xk-type objects (Tholen X and M class Revised 7 May 2014 asteroids) using the Arecibo radar and NASA Infrared Telescope Facilities (Ockert-Bell, M.E., Clark, B.E., Accepted 9 May 2014 Shepard, M.K., Rivkin, A.S., Binzel, R.P., Thomas, C.A., DeMeo, F.E., Bus, S.J., Shah, S. [2008]. Icarus 195, Available online 16 May 2014 206–219; Ockert-Bell, M.E., Clark, B.E., Shepard, M.K., Issacs, R.A., Cloutis, E.A., Fornasier, S., Bus, S.J. -
Photometry of Asteroids: Lightcurves of 24 Asteroids Obtained in 1993–2005
ARTICLE IN PRESS Planetary and Space Science 55 (2007) 986–997 www.elsevier.com/locate/pss Photometry of asteroids: Lightcurves of 24 asteroids obtained in 1993–2005 V.G. Chiornya,b,Ã, V.G. Shevchenkoa, Yu.N. Kruglya,b, F.P. Velichkoa, N.M. Gaftonyukc aInstitute of Astronomy of Kharkiv National University, Sumska str. 35, 61022 Kharkiv, Ukraine bMain Astronomical Observatory, NASU, Zabolotny str. 27, Kyiv 03680, Ukraine cCrimean Astrophysical Observatory, Crimea, 98680 Simeiz, Ukraine Received 19 May 2006; received in revised form 23 December 2006; accepted 10 January 2007 Available online 21 January 2007 Abstract The results of 1993–2005 photometric observations for 24 main-belt asteroids: 24 Themis, 51 Nemausa, 89 Julia, 205 Martha, 225 Henrietta, 387 Aquitania, 423 Diotima, 505 Cava, 522 Helga, 543 Charlotte, 663 Gerlinde, 670 Ottegebe, 693 Zerbinetta, 694 Ekard, 713 Luscinia, 800 Kressmania, 1251 Hedera, 1369 Ostanina, 1427 Ruvuma, 1796 Riga, 2771 Polzunov, 4908 Ward, 6587 Brassens and 16541 1991 PW18 are presented. The rotation periods of nine of these asteroids have been determined for the first time and others have been improved. r 2007 Elsevier Ltd. All rights reserved. Keywords: Asteroids; Photometry; Lightcurve; Rotational period; Amplitude 1. Introduction telescope of the Crimean Astrophysics Observatory in Simeiz. Ground-based observations are the main source of knowledge about the physical properties of the asteroid 2. Observations and their reduction population. The photometric lightcurves are used to determine rotation periods, pole coordinates, sizes and Photometric observations of the asteroids were carried shapes of asteroids, as well as to study the magnitude-phase out in 1993–1994 using one-channel photoelectric photo- relation of different type asteroids. -
Photometry and Models of Selected Main Belt Asteroids IX
A&A 545, A131 (2012) Astronomy DOI: 10.1051/0004-6361/201219542 & c ESO 2012 Astrophysics Photometry and models of selected main belt asteroids IX. Introducing interactive service for asteroid models (ISAM), A. Marciniak1, P. Bartczak1, T. Santana-Ros1, T. Michałowski1, P. Antonini2,R.Behrend3, C. Bembrick4, L. Bernasconi5, W. Borczyk1,F.Colas6, J. Coloma7, R. Crippa8, N. Esseiva9, M. Fagas1,M.Fauvaud10,S.Fauvaud10, D. D. M. Ferreira11,R.P.HeinBertelsen12, D. Higgins13,R.Hirsch1,J.J.E.Kajava14,K.Kaminski´ 1, A. Kryszczynska´ 1, T. Kwiatkowski1, F. Manzini8, J. Michałowski15,M.J.Michałowski16, A. Paschke17,M.Polinska´ 1, R. Poncy18,R.Roy19, G. Santacana9, K. Sobkowiak1, M. Stasik1, S. Starczewski20, F. Velichko21, H. Wucher9,andT.Zafar22 1 Astronomical Observatory Institute, Faculty of Physics, A. Mickiewicz University, Słoneczna 36, 60-286 Poznan,´ Poland e-mail: [email protected] 2 Observatoire de Bédoin, 47 rue Guillaume Puy, 84000 Avignon, France 3 Geneva Observatory, 1290 Sauverny, Switzerland 4 Bathurst, NSW, Australia 5 Les Engarouines Observatory, 84570 Mallemort-du-Comtat, France 6 IMCCE, Paris Observatory, UMR 8028, CNRS, 77 av. Denfert-Rochereau, 75014 Paris, France 7 Agrupación Astronómica de Sabadell, Apartado de Correos 50, PO Box 50, 08200 Sabadell, Barcelona, Spain 8 Stazione Astronomica di Sozzago, 28060 Sozzago, Italy 9 Association AstroQueyras, 05350 Saint-Véran, France 10 Observatoire du Bois de Bardon, 16110 Taponnat, France 11 DTU Space, Technical University of Denmark, Juliane Maries Vej 30, 2200 Copenhagen, Denmak 12 Kapteyn Astronomical Institute, University of Groningen, PO box 800, 9700 AV Groningen, The Netherlands 13 Canberra, ACT, Australia 14 Astronomy Division, Department of Physics, PO Box 3000, 90014 University of Oulu, Finland 15 Forte Software, Os. -
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. -
Temperature-Induced Effects and Phase Reddening on Near-Earth Asteroids
Planetologie Temperature-induced effects and phase reddening on near-Earth asteroids Inaugural-Dissertation zur Erlangung des Doktorgrades der Naturwissenschaften im Fachbereich Geowissenschaften der Mathematisch-Naturwissenschaftlichen Fakultät der Westfälischen Wilhelms-Universität Münster vorgelegt von Juan A. Sánchez aus Caracas, Venezuela -2013- Dekan: Prof. Dr. Hans Kerp Erster Gutachter: Prof. Dr. Harald Hiesinger Zweiter Gutachter: Dr. Vishnu Reddy Tag der mündlichen Prüfung: 4. Juli 2013 Tag der Promotion: 4. Juli 2013 Contents Summary 5 Preface 7 1 Introduction 11 1.1 Asteroids: origin and evolution . 11 1.2 The asteroid-meteorite connection . 13 1.3 Spectroscopy as a remote sensing technique . 16 1.4 Laboratory spectral calibration . 24 1.5 Taxonomic classification of asteroids . 31 1.6 The NEA population . 36 1.7 Asteroid space weathering . 37 1.8 Motivation and goals of the thesis . 41 2 VNIR spectra of NEAs 43 2.1 The data set . 43 2.2 Data reduction . 45 3 Temperature-induced effects on NEAs 55 3.1 Introduction . 55 3.2 Temperature-induced spectral effects on NEAs . 59 3.2.1 Spectral band analysis of NEAs . 59 3.2.2 NEAs surface temperature . 59 3.2.3 Temperature correction to band parameters . 62 3.3 Results and discussion . 70 4 Phase reddening on NEAs 73 4.1 Introduction . 73 4.2 Phase reddening from ground-based observations of NEAs . 76 4.2.1 Phase reddening effect on the band parameters . 76 4.3 Phase reddening from laboratory measurements of ordinary chondrites . 82 4.3.1 Data and spectral band analysis . 82 4.3.2 Phase reddening effect on the band parameters . -
Occultation Newsletter Volume 8, Number 4
Volume 12, Number 1 January 2005 $5.00 North Am./$6.25 Other International Occultation Timing Association, Inc. (IOTA) In this Issue Article Page The Largest Members Of Our Solar System – 2005 . 4 Resources Page What to Send to Whom . 3 Membership and Subscription Information . 3 IOTA Publications. 3 The Offices and Officers of IOTA . .11 IOTA European Section (IOTA/ES) . .11 IOTA on the World Wide Web. Back Cover ON THE COVER: Steve Preston posted a prediction for the occultation of a 10.8-magnitude star in Orion, about 3° from Betelgeuse, by the asteroid (238) Hypatia, which had an expected diameter of 148 km. The predicted path passed over the San Francisco Bay area, and that turned out to be quite accurate, with only a small shift towards the north, enough to leave Richard Nolthenius, observing visually from the coast northwest of Santa Cruz, to have a miss. But farther north, three other observers video recorded the occultation from their homes, and they were fortuitously located to define three well- spaced chords across the asteroid to accurately measure its shape and location relative to the star, as shown in the figure. The dashed lines show the axes of the fitted ellipse, produced by Dave Herald’s WinOccult program. This demonstrates the good results that can be obtained by a few dedicated observers with a relatively faint star; a bright star and/or many observers are not always necessary to obtain solid useful observations. – David Dunham Publication Date for this issue: July 2005 Please note: The date shown on the cover is for subscription purposes only and does not reflect the actual publication date. -
Thermophysical Characteristics of the Large Main-Belt Asteroid (349
Mon. Not. R. Astron. Soc. 000, 1–10 (2002) Printed 14 November 2018 (MN LATEX style file v2.2) Thermophysical characteristics of the large main-belt asteroid (349) Dembowska LiangLiang Yu1,2⋆, Bin Yang3,4, Jianghui Ji2 , Wing-Huen Ip1,5 1Space Science Institute, Macau University of Science and Technology, Taipa, Macau;† 2CAS Key Laboratory of Planetary Sciences, Purple Mountain Observatory, Chinese Academy of Sciences, Nanjing 210008, China; 3European Southern Observatory, Alonso de C´ordova 3107, Vitacura, Casilla 19001, Santiago, Chile; 4Yunnan Observatories, Chinese Academy of Sciences, Kunming 650011, China; 5Institute of Astronomy, National Central University, Jhongli, Taoyuan City 32001, Taiwan Received 2014 December 14; in original form 2014 December 30 ABSTRACT (349) Dembowska, a large, bright main-belt asteroid, has a fast rotation and oblique spin axis. It may have experienced partial melting and differentiation. We constrain Dembowska’s thermophysical properties, e.g., thermal inertia, roughness fraction, geometric albedo and ef- +12 2 0.5 1 +0.60 fective diameter within 3σ uncertainty of Γ = 20 7 Jm− s− K− , fr = 0.25 0.25, pv = +0.026 +7.5 − − 0.309 0.038, and Deff = 155.8 6.2 km, by utilizing the Advanced Thermophysical Model (ATPM)− to analyse four sets of− thermal infrared data obtained by IRAS, AKARI, WISE and Subaru/COMICS at different epochs. In addition, by modeling the thermal lightcurve ob- served by WISE, we obtain the rotational phases of each dataset. These rotationally resolved data do not reveal significant variations of thermal inertia and roughness across the surface, indicating the surface of Dembowska should be covered by a dusty regolith layer with few rocks or boulders. -
Orbital Stability Assessments of Satellites Orbiting Small Solar System Bodies a Case Study of Eros
Delft University of Technology, Faculty of Aerospace Engineering Thesis report Orbital stability assessments of satellites orbiting Small Solar System Bodies A case study of Eros Author: Supervisor: Sjoerd Ruevekamp Jeroen Melman, MSc 1012150 August 17, 2009 Preface i Contents 1 Introduction 2 2 Small Solar System Bodies 4 2.1 Asteroids . .5 2.1.1 The Tholen classification . .5 2.1.2 Asteroid families and belts . .7 2.2 Comets . 11 3 Celestial Mechanics 12 3.1 Principles of astrodynamics . 12 3.2 Many-body problem . 13 3.3 Three-body problem . 13 3.3.1 Circular restricted three-body problem . 14 3.3.2 The equations of Hill . 16 3.4 Two-body problem . 17 3.4.1 Conic sections . 18 3.4.2 Elliptical orbits . 19 4 Asteroid shapes and gravity fields 21 4.1 Polyhedron Modelling . 21 4.1.1 Implementation . 23 4.2 Spherical Harmonics . 24 4.2.1 Implementation . 26 4.2.2 Implementation of the associated Legendre polynomials . 27 4.3 Triaxial Ellipsoids . 28 4.3.1 Implementation of method . 29 4.3.2 Validation . 30 5 Perturbing forces near asteroids 34 5.1 Third-body perturbations . 34 5.1.1 Implementation of the third-body perturbations . 36 5.2 Solar Radiation Pressure . 36 5.2.1 The effect of solar radiation pressure . 38 5.2.2 Implementation of the Solar Radiation Pressure . 40 6 About the stability disturbing effects near asteroids 42 ii CONTENTS 7 Integrators 44 7.1 Runge-Kutta Methods . 44 7.1.1 Runge-Kutta fourth-order integrator . 45 7.1.2 Runge-Kutta-Fehlberg Method . -
ASTEROID SPECTROSCOPY and MINERALOGY 8:30 A.M
Lunar and Planetary Science XXXVI (2005) sess53.pdf Wednesday, March 16, 2005 ASTEROID SPECTROSCOPY AND MINERALOGY 8:30 a.m. Salon A Chairs: S. Erard L. A. McFadden 8:30 a.m. Gaffey M. J. * The Critical Importance of Data Reduction Calibrations in the Interpretability of S-type Asteroid Spectra [#1916] S-asteroid spectra are especially sensitive to distortion during the reduction of raw data to calibrated spectra. This can lead to major errors in mineralogical interpretations. Two major problems and the procedures to ameliorate them are discussed. 8:45 a.m. Sunshine J. M. * Bus S. J. Burbine T. H. McCoy T. J. Tracing Oxygen Fugacity in Asteroids and Meteorites Through Olivine Composition [#1203] We present new spectra of well-characterized olivine-rich meteorites and show that olivine Fa# can be accurately inferred from spectra. Using the same approach, new asteroid data are examined to infer the oxygen fugacity of olivine-rich asteroids. 9:00 a.m. Trigo-Rodríguez J. M. * Castro-Tirado A. J. Llorca J. Evidence of Hydrated 109P/Swift-Tuttle Meteoroids from Meteor Spectroscopy [#1485] Evidence for the possible presence of water in meteoroids released from comet 109P/Swift-Tuttle is presented. A Perseid fireball spectrum obtained during the 2004 campaign shows O and H lines, consistent with the presence of water in the mineral components of the meteoroid. 9:15 a.m. Emery J. P. * Cruikshank D. P. Van Cleve J. Stansberry J. A. Mineralogy of Asteroids from Observations with the Spitzer Space Telescope [#2072] Thermal emission measurements of the low-albedo Trojan asteroid 624 Hektor indicate a surface mineralogy of fine-grained silicates. -
An Ancient and a Primordial Collisional Family As the Main Sources of X-Type Asteroids of the Inner Main Belt
Astronomy & Astrophysics manuscript no. agapi2019.01.22_R1 c ESO 2019 February 6, 2019 An ancient and a primordial collisional family as the main sources of X-type asteroids of the inner Main Belt ∗ Marco Delbo’1, Chrysa Avdellidou1; 2, and Alessandro Morbidelli1 1 Université Côte d’Azur, CNRS–Lagrange, Observatoire de la Côte d’Azur, CS 34229 – F 06304 NICE Cedex 4, France e-mail: [email protected] e-mail: [email protected] 2 Science Support Office, Directorate of Science, European Space Agency, Keplerlaan 1, NL-2201 AZ Noordwijk ZH, The Netherlands. Received February 6, 2019; accepted February 6, 2019 ABSTRACT Aims. The near-Earth asteroid population suggests the existence of an inner Main Belt source of asteroids that belongs to the spec- troscopic X-complex and has moderate albedos. The identification of such a source has been lacking so far. We argue that the most probable source is one or more collisional asteroid families that escaped discovery up to now. Methods. We apply a novel method to search for asteroid families in the inner Main Belt population of asteroids belonging to the X- complex with moderate albedo. Instead of searching for asteroid clusters in orbital elements space, which could be severely dispersed when older than some billions of years, our method looks for correlations between the orbital semimajor axis and the inverse size of asteroids. This correlation is the signature of members of collisional families, which drifted from a common centre under the effect of the Yarkovsky thermal effect. Results. We identify two previously unknown families in the inner Main Belt among the moderate-albedo X-complex asteroids. -
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. -
Planetary Science Institute
PLANETARY SCIENCE INSTITUTE N7'6-3qo84 (NAS A'-CR:1'V7! 3 ) ASTEROIDAL AND PLANETARY ANALYSIS Final Report (Planetary Science Ariz.) 163 p HC $6.75 Inst., Tucson, CSCL 03A Unclas G3/89 15176 i-'' NSA tiFACIWj INP BRANC NASW 2718 ASTEROIDAL AND PLANETARY ANALYSIS Final Report 11 August 1975 Submitted by: Planetary Science Institute 252 W. Ina Road, Suite D Tucson, Arizona 85704 William K. Hartmann Manager TASK 1: ASTEROID SPECTROPHOTOMETRY AND INTERPRETATION (Principal Investigator: Clark R. Chapman) A.* INTRODUCTION The asteroid research program during 1974/5 has three major goals: (1) continued spectrophotometric reconnaissance of the asteroid belt to define compositional types; (2) detailed spectrophotometric observations of particular asteroids, especially to determine variations with rotational phase, if any; and (3) synthesis of these data with other physical studies of asteroids and interpretation of the implications of physical studies of the asteroids for meteoritics and solar system history. The program has been an especially fruitful one, yielding fundamental new insights to the nature of the asteroids and the implications for the early development of the terrestrial planets. In particular, it is believed that the level of understanding of the asteroids has been reached, and sufficiently fundamental questions raised about their nature, that serious consideration should be given to possible future spacecraft missions directed to study a sample of asteroids at close range. Anders (1971) has argued that serious consideration of asteroid missions should be postponed until ground-based techniques for studying asteroids had been sufficiently exploited so that we could intelligently select appropriate asteroids for spacecraft targeting. It is clear that that point has been reached, ,and now that relatively inexpensive fly-by missions have been discovered to be possible by utilizing Venus and Earth gravity assists (Bender and Friedlander, 1975), serious planning for such missions ought to begin.