Optimal Trajectory Synthesis for Spacecraft Asteroid Rendezvous
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Discovery of Earth's Quasi-Satellite
Meteoritics & Planetary Science 39, Nr 8, 1251–1255 (2004) Abstract available online at http://meteoritics.org Discovery of Earth’s quasi-satellite Martin CONNORS,1* Christian VEILLET,2 Ramon BRASSER,3 Paul WIEGERT,4 Paul CHODAS,5 Seppo MIKKOLA,6 and Kimmo INNANEN3 1Athabasca University, Athabasca AB, Canada T9S 3A3 2Canada-France-Hawaii Telescope, P. O. Box 1597, Kamuela, Hawaii 96743, USA 3Department of Physics and Astronomy, York University, Toronto, ON M3J 1P3 Canada 4Department of Physics and Astronomy, University of Western Ontario, London, ON N6A 3K7, Canada 5Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California 91109, USA 6Turku University Observatory, Tuorla, FIN-21500 Piikkiö, Finland *Corresponding author. E-mail: [email protected] (Received 18 February 2004; revision accepted 12 July 2004) Abstract–The newly discovered asteroid 2003 YN107 is currently a quasi-satellite of the Earth, making a satellite-like orbit of high inclination with apparent period of one year. The term quasi- satellite is used since these large orbits are not completely closed, but rather perturbed portions of the asteroid’s orbit around the Sun. Due to its extremely Earth-like orbit, this asteroid is influenced by Earth’s gravity to remain within 0.1 AU of the Earth for approximately 10 years (1997 to 2006). Prior to this, it had been on a horseshoe orbit closely following Earth’s orbit for several hundred years. It will re-enter such an orbit, and make one final libration of 123 years, after which it will have a close interaction with the Earth and transition to a circulating orbit. -
Jjmonl 1712.Pmd
alactic Observer John J. McCarthy Observatory G Volume 10, No. 12 December 2017 Holiday Theme Park See page 19 for more information The John J. McCarthy Observatory Galactic Observer New Milford High School Editorial Committee 388 Danbury Road Managing Editor New Milford, CT 06776 Bill Cloutier Phone/Voice: (860) 210-4117 Production & Design Phone/Fax: (860) 354-1595 www.mccarthyobservatory.org Allan Ostergren Website Development JJMO Staff Marc Polansky Technical Support It is through their efforts that the McCarthy Observatory Bob Lambert has established itself as a significant educational and recreational resource within the western Connecticut Dr. Parker Moreland community. Steve Barone Jim Johnstone Colin Campbell Carly KleinStern Dennis Cartolano Bob Lambert Route Mike Chiarella Roger Moore Jeff Chodak Parker Moreland, PhD Bill Cloutier Allan Ostergren Doug Delisle Marc Polansky Cecilia Detrich Joe Privitera Dirk Feather Monty Robson Randy Fender Don Ross Louise Gagnon Gene Schilling John Gebauer Katie Shusdock Elaine Green Paul Woodell Tina Hartzell Amy Ziffer In This Issue "OUT THE WINDOW ON YOUR LEFT"............................... 3 REFERENCES ON DISTANCES ................................................ 18 SINUS IRIDUM ................................................................ 4 INTERNATIONAL SPACE STATION/IRIDIUM SATELLITES ............. 18 EXTRAGALACTIC COSMIC RAYS ........................................ 5 SOLAR ACTIVITY ............................................................... 18 EQUATORIAL ICE ON MARS? ........................................... -
Origin and Evolution of Trojan Asteroids 725
Marzari et al.: Origin and Evolution of Trojan Asteroids 725 Origin and Evolution of Trojan Asteroids F. Marzari University of Padova, Italy H. Scholl Observatoire de Nice, France C. Murray University of London, England C. Lagerkvist Uppsala Astronomical Observatory, Sweden The regions around the L4 and L5 Lagrangian points of Jupiter are populated by two large swarms of asteroids called the Trojans. They may be as numerous as the main-belt asteroids and their dynamics is peculiar, involving a 1:1 resonance with Jupiter. Their origin probably dates back to the formation of Jupiter: the Trojan precursors were planetesimals orbiting close to the growing planet. Different mechanisms, including the mass growth of Jupiter, collisional diffusion, and gas drag friction, contributed to the capture of planetesimals in stable Trojan orbits before the final dispersal. The subsequent evolution of Trojan asteroids is the outcome of the joint action of different physical processes involving dynamical diffusion and excitation and collisional evolution. As a result, the present population is possibly different in both orbital and size distribution from the primordial one. No other significant population of Trojan aster- oids have been found so far around other planets, apart from six Trojans of Mars, whose origin and evolution are probably very different from the Trojans of Jupiter. 1. INTRODUCTION originate from the collisional disruption and subsequent reaccumulation of larger primordial bodies. As of May 2001, about 1000 asteroids had been classi- A basic understanding of why asteroids can cluster in fied as Jupiter Trojans (http://cfa-www.harvard.edu/cfa/ps/ the orbit of Jupiter was developed more than a century lists/JupiterTrojans.html), some of which had only been ob- before the first Trojan asteroid was discovered. -
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. -
The High-Energy Environment and Atmospheric Escape of the Mini-Neptune K2-18 B? Leonardo A
A&A 634, L4 (2020) Astronomy https://doi.org/10.1051/0004-6361/201937327 & c ESO 2020 Astrophysics LETTER TO THE EDITOR The high-energy environment and atmospheric escape of the mini-Neptune K2-18 b? Leonardo A. dos Santos1, David Ehrenreich1, Vincent Bourrier1, Nicola Astudillo-Defru2, Xavier Bonfils3, François Forget4, Christophe Lovis1, Francesco Pepe1, and Stéphane Udry1 1 Observatoire Astronomique de l’Université de Genève, 51 Chemin des Maillettes, 1290 Versoix, Switzerland e-mail: [email protected] 2 Departamento de Matemática y Física Aplicadas, Universidad Católica de la Santísima Concepción, Alonso de Rivera, 2850 Concepción, Chile 3 Université Grenoble Alpes, CNRS, IPAG, 38000 Grenoble, France 4 Laboratoire de Météorologie Dynamique, Institut Pierre Simon Laplace, Université Paris 6 Boite Postale 99, 75252 Paris Cedex 05, France Received 16 December 2019 / Accepted 13 January 2020 ABSTRACT K2-18 b is a transiting mini-Neptune that orbits a nearby (38 pc), cool M3 dwarf and is located inside its region of temperate irradiation. We report on the search for hydrogen escape from the atmosphere K2-18 b using Lyman-α transit spectroscopy with the Space Telescope Imaging Spectrograph instrument installed on the Hubble Space Telescope. We analyzed the time-series of fluxes of the stellar Lyman-α emission of K2-18 in both its blue- and redshifted wings. We found that the average blueshifted emission of K2-18 decreases by 67% ± 18% during the transit of the planet compared to the pre-transit emission, tentatively indicating the presence of H atoms escaping vigorously and being blown away by radiation pressure. This interpretation is not definitive because it relies on one partial transit. -
Satellite Splat II: an Inelastic Collision with a Surface-Launched Projectile and the Maximum Orbital Radius for Planetary Impact
European Journal of Physics Eur. J. Phys. 37 (2016) 045004 (10pp) doi:10.1088/0143-0807/37/4/045004 Satellite splat II: an inelastic collision with a surface-launched projectile and the maximum orbital radius for planetary impact Philip R Blanco1,2,4 and Carl E Mungan3 1 Department of Physics and Astronomy, Grossmont College, El Cajon, CA 92020- 1765, USA 2 Department of Astronomy, San Diego State University, San Diego, CA 92182- 1221, USA 3 Physics Department, US Naval Academy, Annapolis, MD 21402-1363, USA E-mail: [email protected] Received 26 January 2016, revised 3 April 2016 Accepted for publication 14 April 2016 Published 16 May 2016 Abstract Starting with conservation of energy and angular momentum, we derive a convenient method for determining the periapsis distance of an orbiting object, by expressing its velocity components in terms of the local circular speed. This relation is used to extend the results of our previous paper, examining the effects of an adhesive inelastic collision between a projectile launched from the surface of a planet (of radius R) and an equal-mass satellite in a circular orbit of radius rs. We show that there is a maximum orbital radius rs ≈ 18.9R beyond which such a collision cannot cause the satellite to impact the planet. The difficulty of bringing down a satellite in a high orbit with a surface- launched projectile provides a useful topic for a discussion of orbital angular momentum and energy. The material is suitable for an undergraduate inter- mediate mechanics course. Keywords: orbital motion, momentum conservation, energy conservation, angular momentum, ballistics (Some figures may appear in colour only in the online journal) 4 Author to whom any correspondence should be addressed. -
Orbital Mechanics Course Notes
Orbital Mechanics Course Notes David J. Westpfahl Professor of Astrophysics, New Mexico Institute of Mining and Technology March 31, 2011 2 These are notes for a course in orbital mechanics catalogued as Aerospace Engineering 313 at New Mexico Tech and Aerospace Engineering 362 at New Mexico State University. This course uses the text “Fundamentals of Astrodynamics” by R.R. Bate, D. D. Muller, and J. E. White, published by Dover Publications, New York, copyright 1971. The notes do not follow the book exclusively. Additional material is included when I believe that it is needed for clarity, understanding, historical perspective, or personal whim. We will cover the material recommended by the authors for a one-semester course: all of Chapter 1, sections 2.1 to 2.7 and 2.13 to 2.15 of Chapter 2, all of Chapter 3, sections 4.1 to 4.5 of Chapter 4, and as much of Chapters 6, 7, and 8 as time allows. Purpose The purpose of this course is to provide an introduction to orbital me- chanics. Students who complete the course successfully will be prepared to participate in basic space mission planning. By basic mission planning I mean the planning done with closed-form calculations and a calculator. Stu- dents will have to master additional material on numerical orbit calculation before they will be able to participate in detailed mission planning. There is a lot of unfamiliar material to be mastered in this course. This is one field of human endeavor where engineering meets astronomy and ce- lestial mechanics, two fields not usually included in an engineering curricu- lum. -
Control of Long-Term Low-Thrust Small Satellites Orbiting Mars
SSC18-PII-26 Control of Long-Term Low-Thrust Small Satellites Orbiting Mars Christopher Swanson University of Florida 3131 NW 58th Blvd. Gainesville FL [email protected] Faculty Advisor: Riccardo Bevilacqua Graduate Advisor: Patrick Kelly University of Florida ABSTRACT As expansion of deep space missions continue, Mars is quickly becoming the planet of primary focus for science and exploratory satellite systems. Due to the cost of sending large satellites equipped with enough fuel to last the entire lifespan of a mission, inexpensive small satellites equipped with low thrust propulsion are of continuing interest. In this paper, a model is constructed for use in simulating the control of a small satellite system, equipped with low- thrust propulsion in orbit around Mars. The model takes into consideration the fuel consumption and can be used to predict the lifespan of the satellite based on fuel usage due to the natural perturbation of the orbit. This model of the natural perturbations around Mars implements a Lyapunov Based control law using a set of gains for the orbital elements calculated by obtaining the ratio of the instantaneous rate of change of the element over the maximum rate of change over the current orbit. The thrust model simulates the control of the semi-major axis, eccentricity, and inclination based upon a thrust vector fixed to a local vertical local horizontal reference frame of the satellite. This allows for a more efficient fuel usage over the long continuous thrust burns by prioritizing orbital elements in the control when they have a higher relative rate of change rather than the Lyapunov control prioritizing the element with the greatest magnitude rate of change. -
The Population of Near Earth Asteroids in Coorbital Motion with Venus
ARTICLE IN PRESS YICAR:7986 JID:YICAR AID:7986 /FLA [m5+; v 1.65; Prn:10/08/2006; 14:41] P.1 (1-10) Icarus ••• (••••) •••–••• www.elsevier.com/locate/icarus The population of Near Earth Asteroids in coorbital motion with Venus M.H.M. Morais a,∗, A. Morbidelli b a Grupo de Astrofísica da Universidade de Coimbra, Observatório Astronómico de Coimbra, Santa Clara, 3040 Coimbra, Portugal b Observatoire de la Côte d’Azur, BP 4229, Boulevard de l’Observatoire, Nice Cedex 4, France Received 13 January 2006; revised 10 April 2006 Abstract We estimate the size and orbital distributions of Near Earth Asteroids (NEAs) that are expected to be in the 1:1 mean motion resonance with Venus in a steady state scenario. We predict that the number of such objects with absolute magnitudes H<18 and H<22 is 0.14 ± 0.03 and 3.5 ± 0.7, respectively. We also map the distribution in the sky of these Venus coorbital NEAs and we see that these objects, as the Earth coorbital NEAs studied in a previous paper, are more likely to be found by NEAs search programs that do not simply observe around opposition and that scan large areas of the sky. © 2006 Elsevier Inc. All rights reserved. Keywords: Asteroids, dynamics; Resonances 1. Introduction object with a theory based on the restricted three body problem at high eccentricity and inclination. Christou (2000) performed In Morais and Morbidelli (2002), hereafter referred to as a 0.2 Myr integration of the orbits of NEAs in the vicinity of Paper I, we estimated the population of Near Earth Asteroids the terrestrial planets, namely (3362) Khufu, (10563) Izhdubar, (NEAs) that are in the 1:1 mean motion resonance (i.e., are 1994 TF2 and 1989 VA, showing that the first three could be- coorbital1) with the Earth in a steady state scenario where come coorbitals of the Earth while the fourth could become NEAs are constantly being supplied by the main belt sources coorbital of Venus. -
Horsing Around on Saturn
Horsing Around on Saturn Robert J. Vanderbei Operations Research and Financial Engineering, Princeton University [email protected] ABSTRACT Based on simple statistical mechanical models, the prevailing view of Sat- urn’s rings is that they are unstable and must therefore have been formed rather recently. In this paper, we argue that Saturn’s rings and inner moons are in much more stable orbits than previously thought and therefore that they likely formed together as part of the initial formation of the solar system. To make this argument, we give a detailed description of so-called horseshoe orbits and show that this horseshoeing phenomenon greatly stabilizes the rings of Saturn. This paper is part of a collaborative effort with E. Belbruno and J.R. Gott III. For a description of their part of the work, see their papers in these proceedings. 1. Introduction The currently accepted view (see, e.g., Goldreich and Tremaine (1982)) of the formation of Saturn’s rings is that a moon-sized object wandered inside Saturn’s Roche limit and was torn apart by tidal forces. The resulting array of remnant masses was dispersed and formed the rings we see today. In this model, the system dynamics are treated as a turbulent flow with no explicit mention of the law of gravitation. The ring shape is presumed to be maintained by the coralling effect of a few of the inner moons acting as so-called shepherds. Of course, a simpler explanation would be that the rings formed along with the planets and their moons as they condensed out of the solar nebula. -
Radar Detection of Asteroid 2002 AA29
Icarus 166 (2003) 271–275 www.elsevier.com/locate/icarus Radar detection of Asteroid 2002 AA29 Steven J. Ostro,a,∗ Jon D. Giorgini,a Lance A.M. Benner,a Alice A. Hine,b Michael C. Nolan,b Jean-Luc Margot,c Paul W. Chodas,a and Christian Veillet d a Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109-8099, USA b National Astronomy and Ionosphere Center, Arecibo Observatory, HC3 Box 53995, Arecibo, PR 00612, USA c California Institute of Technology, Pasadena, CA 91125, USA d Canada–France–Hawaii Telescope Corporation, 65-1238 Mamaloha Hwy, Kamuela, HI 96743, USA Received 24 June 2003; revised 27 August 2003 Abstract − Radar echoes from Earth co-orbital Asteroid 2002 AA29 yield a total-power radar cross section of 2.9 × 10 5 km2 ±25%, a circular polarization ratio of SC/OC = 0.26 ± 0.07, and an echo bandwidth of at least 1.5 Hz. Combining these results with the estimate of its visual absolute magnitude, HV = 25.23 ± 0.24, from reported Spacewatch photometry indicates an effective diameter of 25 ± 5 m, a rotation period − no longer than 33 min, and an average surface bulk density no larger than 2.0 g cm 3; the asteroid is radar dark and optically bright, and its statistically most likely spectral class is S. The HV estimate from LINEAR photometry (23.58 ± 0.38) is not compatible with either Spacewatch’s HV or our radar results. If a bias this large were generally present in LINEAR’s estimates of HV for asteroids it has discovered or observed, then estimates of the current completeness of the Spaceguard Survey would have to be revised downward. -
Arxiv:1304.1048V2 [Astro-Ph.EP] 26 Apr 2013 and Murray (1981A), General Properties of the Tadpole and Horseshoe Orbits Are Described in the Quasi- Circular Case
On the co-orbital motion of two planets in quasi-circular orbits Philippe Robutel and Alexandre Pousse IMCCE, Observatoire de Paris, UPMC, CNRS UMR8028, 77 Av. Denfert-Rochereau, 75014 Paris, France August 27, 2018 ABSTRACT We develop an analytical Hamiltonian formalism adapted to the study of the motion of two planets in co-orbital resonance. The Hamiltonian, averaged over one of the planetary mean lon- gitude, is expanded in power series of eccentricities and inclinations. The model, which is valid in the entire co-orbital region, possesses an integrable approximation modeling the planar and quasi-circular motions. First, focusing on the fixed points of this approximation, we highlight re- lations linking the eigenvectors of the associated linearized differential system and the existence of certain remarkable orbits like the elliptic Eulerian Lagrangian configurations, the Anti-Lagrange (Giuppone et al., 2010) orbits and some second sort orbits discovered by Poincar´e. Then, the variational equation is studied in the vicinity of any quasi-circular periodic solution. The funda- mental frequencies of the trajectory are deduced and possible occurrence of low order resonances are discussed. Finally, with the help of the construction of a Birkhoff normal form, we prove that the elliptic Lagrangian equilateral configurations and the Anti-Lagrange orbits bifurcate from the same fixed point L4. Subject headings: Co-orbitals; Resonance; Lagrange; Euler; Planetary problem; Three-body prob- lem 1. Introduction The co-orbital resonance has been extensively studied for more than one hundred years in the framework of the restricted three-body problem (RTBP). In most of the analytical works, the emphasis has been placed on the tadpole orbits, trajectories surrounding one of the two Lagrangian triangular equilibrium points, since these describe the motion of the Jovian Trojans.