Autonomous Optical Navigation for Intclplanctary Missions S
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1922MNRAS..82..149G Jan. 1922. Long-Period Inequalities In
Jan. 1922. Long-Period Inequalities in Movements of Asteroids. 149 In the case = an integer ~ is a multiple of and the solutions X2 X2 a1 1922MNRAS..82..149G with period nearly equal to — may also be regarded as periodic solution» Ai with period nearly equal to —-. A . But we have not been able (in the case when ^ is an integer) to A2 prove the existence of periodic solutions with period ^ which are not A2 • • • 2 TT at the same time periodic with period nearly equal to — . Ax Note.—The above work was completed in 1920 November, before the appearance of Moulton’s Periodic Orbits. The details of the exist- ence proofs are different from those of Buck, and it is hoped that they may be of interest. In Buck’s paper, which apparently was completed in 1912 or earlier, the equations of motion are transformed and the jacobians take a relatively simple form. In this paper only two of the families of periodic orbits treated by Buck are discussed. A full account of the other families, and also of the actual development in series of the periodic solutions, is given in Back’s paper. On Long-Period Inequalities in the Movements of Asteroids ivhose Mean Motions are nearly half that of Mars. By Wt M. H. Greaves, B. A., Isaac Newton Student in the University of Cambridge. (Communicated by Professor H. F. Baker.) In the ordinary theory of the movements of the planets as developed by Laplace and Le Verrier, the equations of motion are integrated by a method of successive approximation with regard to the masses. -
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. -
Cumulative Index to Volumes 1-45
The Minor Planet Bulletin Cumulative Index 1 Table of Contents Tedesco, E. F. “Determination of the Index to Volume 1 (1974) Absolute Magnitude and Phase Index to Volume 1 (1974) ..................... 1 Coefficient of Minor Planet 887 Alinda” Index to Volume 2 (1975) ..................... 1 Chapman, C. R. “The Impossibility of 25-27. Index to Volume 3 (1976) ..................... 1 Observing Asteroid Surfaces” 17. Index to Volume 4 (1977) ..................... 2 Tedesco, E. F. “On the Brightnesses of Index to Volume 5 (1978) ..................... 2 Dunham, D. W. (Letter regarding 1 Ceres Asteroids” 3-9. Index to Volume 6 (1979) ..................... 3 occultation) 35. Index to Volume 7 (1980) ..................... 3 Wallentine, D. and Porter, A. Index to Volume 8 (1981) ..................... 3 Hodgson, R. G. “Useful Work on Minor “Opportunities for Visual Photometry of Index to Volume 9 (1982) ..................... 4 Planets” 1-4. Selected Minor Planets, April - June Index to Volume 10 (1983) ................... 4 1975” 31-33. Index to Volume 11 (1984) ................... 4 Hodgson, R. G. “Implications of Recent Index to Volume 12 (1985) ................... 4 Diameter and Mass Determinations of Welch, D., Binzel, R., and Patterson, J. Comprehensive Index to Volumes 1-12 5 Ceres” 24-28. “The Rotation Period of 18 Melpomene” Index to Volume 13 (1986) ................... 5 20-21. Hodgson, R. G. “Minor Planet Work for Index to Volume 14 (1987) ................... 5 Smaller Observatories” 30-35. Index to Volume 15 (1988) ................... 6 Index to Volume 3 (1976) Index to Volume 16 (1989) ................... 6 Hodgson, R. G. “Observations of 887 Index to Volume 17 (1990) ................... 6 Alinda” 36-37. Chapman, C. R. “Close Approach Index to Volume 18 (1991) .................. -
The Minor Planet Bulletin, We Feel Safe in Al., 1989)
THE MINOR PLANET BULLETIN OF THE MINOR PLANETS SECTION OF THE BULLETIN ASSOCIATION OF LUNAR AND PLANETARY OBSERVERS VOLUME 43, NUMBER 3, A.D. 2016 JULY-SEPTEMBER 199. PHOTOMETRIC OBSERVATIONS OF ASTEROIDS star, and asteroid were determined by measuring a 5x5 pixel 3829 GUNMA, 6173 JIMWESTPHAL, AND sample centered on the asteroid or star. This corresponds to a 9.75 (41588) 2000 SC46 by 9.75 arcsec box centered upon the object. When possible, the same comparison star and check star were used on consecutive Kenneth Zeigler nights of observation. The coordinates of the asteroid were George West High School obtained from the online Lowell Asteroid Services (2016). To 1013 Houston Street compensate for the effect on the asteroid’s visual magnitude due to George West, TX 78022 USA ever changing distances from the Sun and Earth, Eq. 1 was used to [email protected] vertically align the photometric data points from different nights when constructing the composite lightcurve: Bryce Hanshaw 2 2 2 2 George West High School Δmag = –2.5 log((E2 /E1 ) (r2 /r1 )) (1) George West, TX USA where Δm is the magnitude correction between night 1 and 2, E1 (Received: 2016 April 5 Revised: 2016 April 7) and E2 are the Earth-asteroid distances on nights 1 and 2, and r1 and r2 are the Sun-asteroid distances on nights 1 and 2. CCD photometric observations of three main-belt 3829 Gunma was observed on 2016 March 3-5. Weather asteroids conducted from the George West ISD Mobile conditions on March 3 and 5 were not particularly favorable and so Observatory are described. -
The Minor Planet Bulletin
THE MINOR PLANET BULLETIN OF THE MINOR PLANETS SECTION OF THE BULLETIN ASSOCIATION OF LUNAR AND PLANETARY OBSERVERS VOLUME 34, NUMBER 3, A.D. 2007 JULY-SEPTEMBER 53. CCD PHOTOMETRY OF ASTEROID 22 KALLIOPE Kwee, K.K. and von Woerden, H. (1956). Bull. Astron. Inst. Neth. 12, 327 Can Gungor Department of Astronomy, Ege University Trigo-Rodriguez, J.M. and Caso, A.S. (2003). “CCD Photometry 35100 Bornova Izmir TURKEY of asteroid 22 Kalliope and 125 Liberatrix” Minor Planet Bulletin [email protected] 30, 26-27. (Received: 13 March) CCD photometry of asteroid 22 Kalliope taken at Tubitak National Observatory during November 2006 is reported. A rotational period of 4.149 ± 0.0003 hours and amplitude of 0.386 mag at Johnson B filter, 0.342 mag at Johnson V are determined. The observation of 22 Kalliope was made at Tubitak National Observatory located at an elevation of 2500m. For this study, the 410mm f/10 Schmidt-Cassegrain telescope was used with a SBIG ST-8E CCD electronic imager. Data were collected on 2006 November 27. 305 images were obtained for each Johnson B and V filters. Exposure times were chosen as 30s for filter B and 15s for filter V. All images were calibrated using dark and bias frames Figure 1. Lightcurve of 22 Kalliope for Johnson B filter. X axis is and sky flats. JD-2454067.00. Ordinate is relative magnitude. During this observation, Kalliope was 99.26% illuminated and the phase angle was 9º.87 (Guide 8.0). Times of observation were light-time corrected. -
Some Aspects of Asteroid Mass Determination
Proc. VI Serbian-Bulgarian Astronomical Conference, Belgrade 7-11 May 2008, Eds. M. S. Dimitrijeviü, M. Tsvetkov, L. ý. Popoviü, V. Golev Publ. Astr. Soc. "Rudjer Boškoviü", No. 9, 2009, 67-78 SOME ASPECTS OF ASTEROID MASS DETERMINATION ANDJELKA KOVAýEVIû Faculty of mathematics, Studentski trg 16, 11000 Belgrade, Serbia e-mail: [email protected] Abstract. There is great variety of astronomical objects in the Universe. Each of these classes of objects follows a certain distribution function in size, luminosity or mass. Most individual mass distributions approximately follow a power law of the form f(M)vM-2. A notable exception are planets and small bodies which seem to obey a flatter distribution. In spite of the rapidly growing number of newly detected extrasolar planets, our knowledge of the mass function of planetary and small bodies relay entirely on the our Solar System. If is there a ’universal’ mass distribution for astronomical objects on all scales, it will be very important to know mass distribtuion of small solar system bodies. Having in mind mentioned reasons we will present methods for asteroid mass determination as well as some of most interesting results. 1. INTRODUCTION As it is well known, the architecture of the Universe is made up by a great variety of astronomical objects. Usually, they are classified by increasing average size or mass: from asteroids (as the smallest objects) to clusters of galaxies (as the largest entities). Each class follows, generaly not well known, distribution function in size, luminosity or mass of objects. It could be noticed that the most common feature of all distribution of objects is that smaller objects of given kind are more abundant than larger ones. -
University Microfilms International 300 N
ASTEROID TAXONOMY FROM CLUSTER ANALYSIS OF PHOTOMETRY. Item Type text; Dissertation-Reproduction (electronic) Authors THOLEN, DAVID JAMES. Publisher The University of Arizona. Rights Copyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author. Download date 01/10/2021 21:10:18 Link to Item http://hdl.handle.net/10150/187738 INFORMATION TO USERS This reproduction was made from a copy of a docum(~nt sent to us for microfilming. While the most advanced technology has been used to photograph and reproduce this document, the quality of the reproduction is heavily dependent upon the quality of ti.e material submitted. The following explanation of techniques is provided to help clarify markings or notations which may ap pear on this reproduction. I. The sign or "target" for pages apparently lacking from the document photographed is "Missing Page(s)". If it was possible to obtain the missing page(s) or section, they are spliced into the film along with adjacent pages. This may have necessitated cutting through an image alld duplicating adjacent pages to assure complete continuity. 2. When an image on the film is obliterated with a round black mark, it is an indication of either blurred copy because of movement during exposure, duplicate copy, or copyrighted materials that should not have been filmed. For blurred pages, a good image of the pagt' can be found in the adjacent frame. -
Mineralogy of Asteroids 183
Gaffey et al.: Mineralogy of Asteroids 183 Mineralogy of Asteroids M. J. Gaffey University of North Dakota E. A. Cloutis University of Winnipeg M. S. Kelley NASA Johnson Space Center and Georgia Southern University K. L. Reed The Space Development Institute The past decade has seen a significant expansion both in the interpretive methodologies used to extract mineralogical information from asteroid spectra and other remote-sensing data and in the number of asteroids for which mineralogical characterizations exist. Robust miner- alogical characterizations now exist for more than 40 asteroids, an order a magnitude increase since Asteroids II was published. Such characterizations have allowed significant progress to be made in the identification of meteorite parent bodies. Although considerable progress has been made, most asteroid spectra have still only been analyzed by relatively ambiguous curve- matching techniques. Where appropriate and feasible, such data should be subjected to a quanti- tative analysis based on diagnostic mineralogical spectral features. The present paper reviews the recent advances in interpretive methodologies and outlines procedures for their application. 1. INTRODUCTION cated investigation. The central questions of current aster- oid studies focus on geologic issues related to the original In the beginning (ca 1801), asteroids were points of light compositions of asteroidal parent bodies and the chemical in the sky. The primary measurements were positional, and and thermal processes that altered and modified the -
Oxygen and Asteroids Thomas H
Reviews in Mineralogy & Geochemistry Vol. 68, pp. XXX-XXX, 2008 12 Copyright © Mineralogical Society of America Oxygen and Asteroids Thomas H. Burbine1, Andrew S. Rivkin2, Sarah K. Noble3, Thais Mothé-Diniz4, William F. Bottke5, Timothy J. McCoy6, M. Darby Dyar1, and Cristina A. Thomas7 1Dept. of Astronomy, Mount Holyoke College, South Hadley, MA 01075, U.S.A. 2Johns Hopkins University Applied Physics Laboratory, Laurel, MD 20723, U.S.A. 3NASA Johnson Space Center, Houston, TX 77058, U.S.A. 4Observatoire de Paris, 92195 Meudon Cedex, France 5Southwest Research Institute, Boulder, CO 80302, U.S.A. 6Department of Mineral Sciences, National Museum of Natural History, Smithsonian Institution, Washington, D.C. 20560-0119, U.S.A. 7Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 02139, U.S.A. contact e-mail: [email protected] ABSTRACT Hundreds of thousands of asteroids have been discovered in the asteroid belt and in near- Earth space. Oxygen is an abundant element in meteorites and presumably in most asteroids. Spectral refl ectance measurements of asteroids in the visible and near-infrared can identify oxygen-bearing minerals such as those found in the olivine, pyroxene, and serpentine groups due to their distinctive absorption features. Interpretation of the mineralogy of asteroids is complicated by the effects of space weathering, which tends to redden and darken the surfaces of asteroids. Asteroids are primarily classifi ed into a number of taxonomic classes and subclasses according to their spectral properties in the visible wavelength region. However, asteroids with similar spectral properties in the visible may have different spectral properties in the near- infrared and, therefore, different interpreted mineralogies. -
Catalogue of Minor Planet Names and Discovery Circumstances
Catalogue of Minor Planet Names and Discovery Circumstances Addendum 2006–2008 L.D. Schmadel, Dictionary of Minor Planet Names, DOI 10.1007/978-3-642-01965-4_2, © Springer-Verlag Berlin Heidelberg 2009 Title page of Giuseppe Piazzi’s book “On the discovery of the new planet CERES FERDINANDEA, the eighth of those known in our solar system”. The vignette, against the background of Monte Pelegrini and the city of Palermo, shows an angel observing the goddess Ceres sitting in a carriage drawn by two snakes. The inscription on the telescope “CERES ADDITA COELI” (Ceres was added to the heavens) celebrates this epoch-making discovery of the first minor planets (Courtesy of A. Baldi, Bologne) (29) Amphitrite 15 (29) Amphitrite [2.55, 0.07, 6.1] que l’une de vos lectrices ´etrang`eres, dont la philosophie Discovered 1854 Mar. 1 by A. Marth at London. astronomique enseign´ee par vos ouvrages ´etait devenue (* AN 38, 125) Independently discovered 1854 Mar. la religion, Mlle Antoinette Horneman, est d´ec´ed´ee 2 by N. R. Pogson at Oxford and March 3 by dans le calme d’une conscience ´eclair´ee et tranquille J. Chacornac at Paris. sur l’evolution future, le 14 decembre dernier. Par Named after an Oceanid, wife of Poseidon {see testament authentique et pour aider `a votre œvre planet (4341)} and mother of Triton. (H 5) si utile au progr`es, si d´evou´ee, si d´esinteress´ee, et Named by G. Bishop at whose private South quelle admirait au del`ade toute expression, elle vous Villa Observatory in Regent’s Park the planet was a l´egu’e une somme de cinq mille florins (environ dix discovered. -
Study of Ephemeris Accuracy of the Minor Planets
LMSC-0420943 27 APRIL 1974 NASA CR-132455 STUDY OF EPHEMERIS ACCURACY OF THE MINOR PLANETS (NASA-CR-132455) STUDY OF EPHEMERIS N74-32264 ACCURACY OF THE MINOR PLANETS (Lockheed Missiles and Space Co.) 173 p HC $11.75 CSCL 03B Unclas G3/30 46739 STUDY PERFORMED UNDER CONTRACT NAS111609, 0 For NASA-LANGLEY RESEARCH CENTER HAMPTON, VIRGINIA Prepared by SPACE SYSTEMS DIVISION LOCKHEED MISSILES & SPACE COMPANY, INC. (A SUBSIDIARY OF LOCKHEED AIRCRAFT CORPORATION) SUNNYVALE, CALIFORNIA 94088 LMSC-D420943 27 April 1974 NASA CR-132455 STUDY OF EPHEMERIS ACCURACY OF THE MINOR PLANETS Study Performed Under Contract NAS1-11609 For NASA-Langley Research Center Hampton, Virginia Prepared by Space Systems Division LOCKHEED MISSILES & SPACE COMPANY, INC. (A Subsidiary of Lockheed Aircraft Corporation) Sunnyvale, California 94088 LOCKHEED MISSILES & SPACE COMPANY LMSC-D420943 FOREWORD The study described in this report was conducted by Lockheed Missiles & Space Company, Inc. (LMSC) for Langley Research Center, National Aeronautics and Space Administration, Hampton, Virginia, under Contract NAS1-11609. The study was conducted under the direction of D. R. Brooks of the Space Technology Division. L. E. Cunningham, Professor of Astronomy at the University of California, Berkeley, contributed signifi- cantly to the effort under a consulting agreement with LMSC. iii O DING PAGE BLANK NOT FILMED LOCKHEED MISSILES & SPACE COMPANY LMSC-D420943 CONTENTS Section Page FOREWORD iii 1 INTRODUCTION AND SUMMARY 1-1 2 HISTORICAL PROCEDURES 2-1 2.1 Astronomical Position -
Multiple and Fast: the Accretion of Ordinary Chondrite Parent Bodies
Multiple and fast: the accretion of ordinary chondrite parent bodies The MIT Faculty has made this article openly available. Please share how this access benefits you. Your story matters. Citation Vernazza, P., B. Zanda, R. P. Binzel, T. Hiroi, F. E. DeMeo, M. Birlan, R. Hewins, L. Ricci, P. Barge, and M. Lockhart. “Multiple and Fast: The Accretion of Ordinary Chondrite Parent Bodies.” The Astrophysical Journal 791, no. 2 (August 6, 2014): 120. © 2014 The American Astronomical Society As Published http://dx.doi.org/10.1088/0004-637x/791/2/120 Publisher IOP Publishing Version Final published version Citable link http://hdl.handle.net/1721.1/92793 Terms of Use Article is made available in accordance with the publisher's policy and may be subject to US copyright law. Please refer to the publisher's site for terms of use. The Astrophysical Journal, 791:120 (22pp), 2014 August 20 doi:10.1088/0004-637X/791/2/120 C 2014. The American Astronomical Society. All rights reserved. Printed in the U.S.A. MULTIPLE AND FAST: THE ACCRETION OF ORDINARY CHONDRITE PARENT BODIES P. Vernazza1,B.Zanda2,5,6,R.P.Binzel3,7, T. Hiroi4,F.E.DeMeo3, M. Birlan5,R.Hewins2,6, L. Ricci8, P. Barge1, and M. Lockhart3 1 Aix Marseille Universite,´ CNRS, LAM (Laboratoire d’Astrophysique de Marseille) UMR 7326, F-13388 Marseille, France 2 Institut de Mineralogie,´ de Physique des Materiaux,´ et de Cosmochimie (IMPMC), Sorbonne Universites,´ Museum´ National d’Histoire Naturelle, UPMC Universite´ Paris 06, UMR CNRS 7590, IRD UMR 206, 61 rue Buffon, F-75005 Paris, France 3 Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 02139, USA 4 Department of Geological Sciences, Brown University, Providence, RI 02912, USA 5 IMCCE, Observatoire de Paris, 77 Av.