Photometry and Models of Selected Main Belt Asteroids
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Asteroid Shape and Spin Statistics from Convex Models J
Asteroid shape and spin statistics from convex models J. Torppa, V.-P. Hentunen, P. Pääkkönen, P. Kehusmaa, K. Muinonen To cite this version: J. Torppa, V.-P. Hentunen, P. Pääkkönen, P. Kehusmaa, K. Muinonen. Asteroid shape and spin statistics from convex models. Icarus, Elsevier, 2008, 198 (1), pp.91. 10.1016/j.icarus.2008.07.014. hal-00499092 HAL Id: hal-00499092 https://hal.archives-ouvertes.fr/hal-00499092 Submitted on 9 Jul 2010 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 Asteroid shape and spin statistics from convex models J. Torppa, V.-P. Hentunen, P. Pääkkönen, P. Kehusmaa, K. Muinonen PII: S0019-1035(08)00283-2 DOI: 10.1016/j.icarus.2008.07.014 Reference: YICAR 8734 To appear in: Icarus Received date: 18 September 2007 Revised date: 3 July 2008 Accepted date: 7 July 2008 Please cite this article as: J. Torppa, V.-P. Hentunen, P. Pääkkönen, P. Kehusmaa, K. Muinonen, Asteroid shape and spin statistics from convex models, Icarus (2008), doi: 10.1016/j.icarus.2008.07.014 This is a PDF file of an unedited manuscript that has been accepted for publication. -
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. -
Accurate Positions of Asteroids Observed in Bucharest During the Year 1931
ACCURATE POSITIONS OF ASTEROIDS OBSERVED IN BUCHAREST DURING THE YEAR 1931 GHEORGHE BOCŞA, MIHAELA LICULESCU, PETRE POPESCU Astronomical Institute of the Romanian Academy Str. Cuţitul de Argint 5, 040557 Bucharest, Romania E-mail: [email protected] Abstract. The paper contains the observations of minor planets performed in 1931 in Bucharest Astronomical Observatory with 380/6000 mm astrograph. Both Turner’s (constants) and Schlesinger’s (dependences) methods were used in the computation of the normal coordinates of the objects. Keywords: photographic astrometry – minor planets. 1. INTRODUCTION At Bucharest Observatory, within the framework of the Wide-Field Plate Archive Programme, part of the activities of the IAU Commission 9, 13 000 plates were catalogued. They were obtained through a systematic work beginning with the year 1930 until now, by means of the Prin-Merz refractor (f = 6 m, D = 38 cm). After a careful investigation of the whole plate archive, among other things, we discovered that a series of observations were not capitalized, such as a set of minor planets that were observed during 1930–1955. The lack of accurate star catalogues containing positions and proper motions, was one of the reasons for which the completion of the reductions has been neglected in that period. It is worth mentioning that the SAO Catalogue was issued starting from that period. Another thing worth mentioning is that the first Zeiss measuring machine was bought by the Observatory in 1957. However, systematic work on plate processing at Bucharest Observatory started beginning with 1956. The first paper on this subject was published by Cristescu et al. -
~XECKDING PAGE BLANK WT FIL,,Q
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. -
The Minor Planet Bulletin, Alan W
THE MINOR PLANET BULLETIN OF THE MINOR PLANETS SECTION OF THE BULLETIN ASSOCIATION OF LUNAR AND PLANETARY OBSERVERS VOLUME 42, NUMBER 2, A.D. 2015 APRIL-JUNE 89. ASTEROID LIGHTCURVE ANALYSIS AT THE OAKLEY SOUTHERN SKY OBSERVATORY: 2014 SEPTEMBER Lucas Bohn, Brianna Hibbler, Gregory Stein, Richard Ditteon Rose-Hulman Institute of Technology, CM 171 5500 Wabash Avenue, Terre Haute, IN 47803, USA [email protected] (Received: 24 November) Photometric data were collected over the course of seven nights in 2014 September for eight asteroids: 1334 Lundmarka, 1904 Massevitch, 2571 Geisei, 2699 Kalinin, 3197 Weissman, 7837 Mutsumi, 14927 Satoshi, and (29769) 1999 CE28. Eight asteroids were remotely observed from the Oakley Southern Sky Observatory in New South Wales, Australia. The observations were made on 2014 September 12-14, 16-19 using a 0.50-m f/8.3 Ritchey-Chretien optical tube assembly on a Paramount ME mount and SBIG STX-16803 CCD camera, binned 3x3, with a luminance filter. Exposure times ranged from 90 to 180 sec depending on the magnitude of the target. The resulting image scale was 1.34 arcseconds per pixel. Raw images were processed in MaxIm DL 6 using twilight flats, bias, and dark frames. MPO Canopus was used to measure the processed images and produce lightcurves. In order to maximize the potential for data collection, target asteroids were selected based upon their position in the sky approximately one hour after sunset. Only asteroids with no previously published results were targeted. Lightcurves were produced for 1334 Lundmarka, 1904 Massevitch, 2571 Geisei, 3197 Weissman, and (29769) 1999 CE28. -
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. -
Observer's Handbook 1980
OBSERVER’S HANDBOOK 1980 EDITOR: JOHN R. PERCY ROYAL ASTRONOMICAL SOCIETY OF CANADA CONTRIBUTORS AND ADVISORS A l a n H. B a t t e n , Dominion Astrophysical Observatory, Victoria, B.C., Canada V 8 X 3X3 (The Nearest Stars). Terence Dickinson, R.R. 3, Odessa, Ont., Canada K0H 2H0 (The Planets). M arie Fidler, Royal Astronomical Society of Canada, 124 Merton St., Toronto, Ont., Canada M4S 2Z2 (Observatories and Planetariums). V ictor Gaizauskas, Herzberg Institute of Astrophysics, National Research Council, Ottawa, Ont., Canada K1A 0R6 (Sunspots). J o h n A. G a l t , Dominion Radio Astrophysical Observatory, Penticton, B.C., Canada V2A 6K3 (Radio Sources). Ian Halliday, Herzberg Institute of Astrophysics, National Research Council, Ottawa, Ont., Canada K1A 0R6 (Miscellaneous Astronomical Data). H e le n S. H o g g , David Dunlap Observatory, University of Toronto, Richmond Hill, Ont., Canada L4C 4Y6 (Foreword). D o n a l d A. M a c R a e , David Dunlap Observatory, University of Toronto, Richmond Hill, Ont., Canada L4C 4Y6 (The Brightest Stars). B r ia n G. M a r s d e n , Smithsonian Astrophysical Observatory, Cambridge, Mass., U.S.A. 02138 (Comets). Janet A. M attei, American Association o f Variable Star Observers, 187 Concord Ave., Cambridge, Mass. U.S.A. 02138 (Variable Stars). P e t e r M. M illm a n , Herzberg Institute o f Astrophysics, National Research Council, Ottawa, Ont., Canada K1A 0R6 (Meteors, Fireballs and Meteorites). A n t h o n y F. J. M o f f a t , D épartement de Physique, Université de Montréal, Montréal, P.Q., Canada H3C 3J7 (Star Clusters). -
Spin States of Asteroids in the Eos Collisional Family
Spin states of asteroids in the Eos collisional family J. Hanuša,∗, M. Delbo’b, V. Alí-Lagoac, B. Bolinb, R. Jedicked, J. Durechˇ a, H. Cibulkováa, P. Pravece, P. Kušniráke, R. Behrendf, F. Marchisg, P. Antoninih, L. Arnoldi, M. Audejeanj, M. Bachschmidti, L. Bernasconik, L. Brunettol, S. Casullim, R. Dymockn, N. Esseivao, M. Estebanp, O. Gerteisi, H. de Grootq, H. Gullyi, H. Hamanowar, H. Hamanowar, P. Kraffti, M. Lehkýa, F. Manzinis, J. Michelett, E. Morelleu, J. Oeyv, F. Pilcherw, F. Reignierx, R. Royy, P.A. Salomp, B.D. Warnerz aAstronomical Institute, Faculty of Mathematics and Physics, Charles University, V Holešoviˇckách 2, 18000 Prague, Czech Republic bUniversité Côte d’Azur, OCA, CNRS, Lagrange, France cMax-Planck-Institut für extraterrestrische Physik, Giessenbachstraße, Postfach 1312, 85741 Garching, Germany dInstitute for Astronomy, University of Hawaii at Manoa, Honolulu, HI 96822, USA eAstronomical Institute, Academy of Sciences of the Czech Republic, Friˇcova 1, CZ-25165 Ondˇrejov, Czech Republic fGeneva Observatory, CH-1290 Sauverny, Switzerland gSETI Institute, Carl Sagan Center, 189 Bernado Avenue, Mountain View CA 94043, USA hObservatoire des Hauts Patys, F-84410 Bédoin, France iAix Marseille Université, CNRS, OHP (Observatoire de Haute Provence), Institut Pythéas (UMS 3470) 04870 Saint-Michel-l’Observatoire, France jObservatoire de Chinon, Mairie de Chinon, 37500 Chinon, France kObservatoire des Engarouines, 1606 chemin de Rigoy, F-84570 Malemort-du-Comtat, France lLe Florian, Villa 4, 880 chemin de Ribac-Estagnol, -
Infrared Spectroscopy of Large, Low-Albedo Asteroids: Are Ceres and Themis Archetypes Or Outliers?
Infrared Spectroscopy of Large, Low-Albedo Asteroids: Are Ceres and Themis Archetypes or Outliers? Andrew S. Rivkin1, Ellen S. Howell2, Joshua P. Emery3 1. Johns Hopkins University Applied Physics Laboratory 2. University of Arizona 3. University of Tennessee Corresponding author: Andrew Rivkin ([email protected]) Key points: • The largest low-albedo asteroids appear to be unrepresented in the meteorite collection • Reflectance spectra in the 3-µm spectral region, and presumably compositions, similar to Ceres and Themis appear to be common in low-albedo asteroids > 200 km diameter • The asteroid 324 Bamberga appears to have hemispherical-scale variation in its reflectance spectrum, and in places has a spectrum reminiscent of Comet 67P. Submitted to Journal of Geophysical Research 17 September 2018 Revised 27 February 2019 Accepted 12 April 2019 1 Abstract: Low-albedo, hydrated objects dominate the list of the largest asteroids. These objects have varied spectral shapes in the 3-µm region, where diagnostic absorptions due to volatile species are found. Dawn’s visit to Ceres has extended the view shaped by ground-based observing, and shown that world to be a complex one, potentially still experiencing geological activity. We present 33 observations from 2.2-4.0 µm of eight large (D > 200 km) asteroids from the C spectral complex, with spectra inconsistent with the hydrated minerals we see in meteorites. We characterize their absorption band characteristics via polynomial and Gaussian fits to test their spectral similarity to Ceres, the asteroid 24 Themis (thought to be covered in ice frost), and the asteroid 51 Nemausa (spectrally similar to the CM meteorites). -
Organic Matter and Associated Minerals on the Dwarf Planet Ceres
minerals Review Organic Matter and Associated Minerals on the Dwarf Planet Ceres Maria Cristina De Sanctis 1,* and Eleonora Ammannito 2 1 Istituto di Astrofisica e Planetologia Spaziali, Istituto Nazionale di Astrofisica (INAF), 00133 Rome, Italy 2 Agenzia Spaziale Italiana, Via del Politecnico, 00133 Roma, Italy; [email protected] * Correspondence: [email protected] Abstract: Ceres is the largest object in the main belt and it is also the most water-rich body in the inner solar system besides the Earth. The discoveries made by the Dawn Mission revealed that the composition of Ceres includes organic material, with a component of carbon globally present and also a high quantity of localized aliphatic organics in specific areas. The inferred mineralogy of Ceres indicates the long-term activity of a large body of liquid water that produced the alteration minerals discovered on its surface, including ammonia-bearing minerals. To explain the presence of ammonium in the phyllosilicates, Ceres must have accreted organic matter, ammonia, water and carbon present in the protoplanetary formation region. It is conceivable that Ceres may have also processed and transformed its own original organic matter that could have been modified by the pervasive hydrothermal alteration. The coexistence of phyllosilicates, magnetite, carbonates, salts, organics and a high carbon content point to rock–water alteration playing an important role in promoting widespread carbon occurrence. Keywords: Ceres; asteroids; organics; aliphatics; solar system Citation: De Sanctis, M.C.; Ammannito, E. Organic Matter and Associated Minerals on the Dwarf 1. Ceres: A Dwarf Planet in the Main Belt Planet Ceres. Minerals 2021, 11, 799. -
Nature and Degree of Aqueous Alteration of Outer Main Belt Asteroids and CM and CI Carbonaceous Chondrites
University of Tennessee, Knoxville TRACE: Tennessee Research and Creative Exchange Doctoral Dissertations Graduate School 5-2013 Nature and Degree of Aqueous Alteration of Outer Main Belt Asteroids and CM and CI Carbonaceous Chondrites Driss Takir [email protected] Follow this and additional works at: https://trace.tennessee.edu/utk_graddiss Part of the The Sun and the Solar System Commons Recommended Citation Takir, Driss, "Nature and Degree of Aqueous Alteration of Outer Main Belt Asteroids and CM and CI Carbonaceous Chondrites. " PhD diss., University of Tennessee, 2013. https://trace.tennessee.edu/utk_graddiss/1783 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 Driss Takir entitled "Nature and Degree of Aqueous Alteration of Outer Main Belt Asteroids and CM and CI Carbonaceous Chondrites." 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. Harry Y. McSween Jr., Joshua P. Emery, Major Professor We have read this dissertation and recommend its acceptance: Jeffery E. Moersch, Michael W. Guidry Accepted for the Council: Carolyn R. Hodges Vice Provost and Dean of the Graduate School (Original signatures are on file with official studentecor r ds.) Nature and Degree of Aqueous Alteration of Outer Main Belt Asteroids and CM and CI Carbonaceous Chondrites A Dissertation Presented for the Doctor of Philosophy Degree The University of Tennessee, Knoxville Driss Takir May 2013 Copyright © 2013 by Driss Takir All rights reserved. -
THE 3 Μm SPECTRUM of JUPITER's IRREGULAR
The Astrophysical Journal Letters, 793:L44 (3pp), 2014 October 1 doi:10.1088/2041-8205/793/2/L44 C 2014. The American Astronomical Society. All rights reserved. Printed in the U.S.A. THE 3 μm SPECTRUM OF JUPITER’s IRREGULAR SATELLITE HIMALIA M. E. Brown1 and A. R. Rhoden2 1 Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125, USA; [email protected] 2 Johns Hopkins University Applied Physics Laboratory, Laurel, MD 20723, USA; [email protected] Received 2014 August 6; accepted 2014 September 3; published 2014 September 19 ABSTRACT We present a medium resolution spectrum of Jupiter’s irregular satellite Himalia covering the critical 3 μm spectral region. The spectrum shows no evidence for aqueously altered phyllosilicates, as had been suggested from the tentative detection of a 0.7 μm absorption, but instead shows a spectrum strikingly similar to the C/CF type asteroid 52 Europa. 52 Europa is the prototype of a class of asteroids generally situated in the outer asteroid belt between less distant asteroids which show evidence for aqueous alteration and more distant asteroids which show evidence for water ice. The spectral match between Himalia and this group of asteroids is surprising and difficult to reconcile with models of the origin of the irregular satellites. Key words: planets and satellites: composition – planets and satellites: formation – planets and satellites: individual (Himalia) Online-only material: color figures 1. INTRODUCTION phyllosilicates. A spectrum of Himalia obtained from a distant encounter of the Cassini spacecraft shows the possibility of an The origin of the irregular satellites of the giant planets— absorption at 3 μm, but the low signal-to-noise and low spectral small satellites in distant, eccentric, and inclined orbits about resolution prohibits clear interpretation (Chamberlain & Brown their parent body—remains unclear.