The Ginger-Shaped Asteroid 4179 Toutatis: New in Asteroids III (Eds
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AAS 13-484 PASSIVE SORTING OF ASTEROID MATERIAL USING SOLAR RADIATION PRESSURE D. García Yárnoz,* J. P. Sánchez Cuartielles,† and C. R. McInnes ‡ Understanding dust dynamics in asteroid environments is key for future science missions to asteroids and, in the long-term, also for asteroid exploitation. This paper proposes a novel way of manipulating asteroid material by means of solar radiation pressure (SRP). We envisage a method for passively sorting material as a function of its grain size where SRP is used as a passive in-situ ‘mass spec- trometer’. The analysis shows that this novel method allows an effective sorting of regolith material. This has immediate applications for sample return, and in- situ resource utilisation to separate different regolith particle sizes INTRODUCTION Asteroids have lately become prime targets for space exploration missions. This interest is jus- tified as asteroids are among the least evolved bodies in the Solar System and they can provide a better understanding of its formation from the solar nebula. Under NASA’s flexible path plan,1 asteroids have also become one of the feasible “planetary” surfaces to be visited by crewed mis- sions, with the benefit of not requiring the capability to land and take-off from a deep gravity well. In addition, they may well be the most affordable source of in-situ resources to underpin future space exploration ventures. Considerable efforts have been made in the study of the perturbing forces and space environ- ment around cometary and asteroid bodies.2, 3 These forces and harsh environments need to be considered and will have direct implications for the operations of spacecraft around and on small bodies. -
Twenty Years of Toutatis
EPSC Abstracts Vol. 6, EPSC-DPS2011-297, 2011 EPSC-DPS Joint Meeting 2011 c Author(s) 2011 Twenty Years of Toutatis M.W. Busch (1), L.A.M. Benner (2), D.J. Scheeres (3), J.-L. Margot (1), C. Magri (4), M.C. Nolan (5), and J.D. Giorgini (2) (1) Department of Earth and Space Sciences, UCLA, Los Angeles, California, USA (2) Jet Propulsion Laboratory, Pasadena, California, USA (3) Aerospace Engineering Sciences, University of Colorado, Boulder, Colorado, USA (4) University of Maine at Farmington, Farmington, Maine, USA (5) Arecibo Observatory, Arecibo, Puerto Rico, USA Abstract Near-Earth asteroid 4179 Toutatis is near a particularly if the moments of inertia are 4:1 orbital resonance with the Earth. consistent with a uniform internal density. Following its discovery in 1989, Toutatis Toutatis’ last close-Earth-approach for was observed extensively with the Arecibo several decades will be in December 2012, and Goldstone radars during flybys in 1992, when it will be 0.046 AU away. We will 1996, 2000, 2004, and 2008. The 1992 and make predictions for what radar 1996 data show that Toutatis is a bifurcated observations at that time should see. object with overall dimensions of 4.6 x 2.3 x 1.9 km and a surface marked with prominent impact craters. Most significantly, Toutatis References is in a non-principal-axis tumbling rotation [1] Hudson, R.S. and Ostro, S.J.: Shape and non-principal state, spinning about its long axis with a axis spin state of asteroid 4179 Toutatis, Science 270 84-86, period of 5.41 days while that axis precesses 1995. -
Planetary Defence Activities Beyond NASA and ESA
Planetary Defence Activities Beyond NASA and ESA Brent W. Barbee 1. Introduction The collision of a significant asteroid or comet with Earth represents a singular natural disaster for a myriad of reasons, including: its extraterrestrial origin; the fact that it is perhaps the only natural disaster that is preventable in many cases, given sufficient preparation and warning; its scope, which ranges from damaging a city to an extinction-level event; and the duality of asteroids and comets themselves---they are grave potential threats, but are also tantalising scientific clues to our ancient past and resources with which we may one day build a prosperous spacefaring future. Accordingly, the problems of developing the means to interact with asteroids and comets for purposes of defence, scientific study, exploration, and resource utilisation have grown in importance over the past several decades. Since the 1980s, more and more asteroids and comets (especially the former) have been discovered, radically changing our picture of the solar system. At the beginning of the year 1980, approximately 9,000 asteroids were known to exist. By the beginning of 2001, that number had risen to approximately 125,000 thanks to the Earth-based telescopic survey efforts of the era, particularly the emergence of modern automated telescopic search systems, pioneered by the Massachusetts Institute of Technology’s (MIT’s) LINEAR system in the mid-to-late 1990s.1 Today, in late 2019, about 840,000 asteroids have been discovered,2 with more and more being found every week, month, and year. Of those, approximately 21,400 are categorised as near-Earth asteroids (NEAs), 2,000 of which are categorised as Potentially Hazardous Asteroids (PHAs)3 and 2,749 of which are categorised as potentially accessible.4 The hazards posed to us by asteroids affect people everywhere around the world. -
Arecibo Radar Observations of 14 High-Priority Near-Earth Asteroids in CY2020 and January 2021 Patrick A
Arecibo Radar Observations of 14 High-Priority Near-Earth Asteroids in CY2020 and January 2021 Patrick A. Taylor (LPI, USRA), Anne K. Virkki, Flaviane C.F. Venditti, Sean E. Marshall, Dylan C. Hickson, Luisa F. Zambrano-Marin (Arecibo Observatory, UCF), Edgard G. Rivera-Valent´ın, Sriram S. Bhiravarasu, Betzaida Aponte-Hernandez (LPI, USRA), Michael C. Nolan, Ellen S. Howell (U. Arizona), Tracy M. Becker (SwRI), Jon D. Giorgini, Lance A. M. Benner, Marina Brozovic, Shantanu P. Naidu (JPL), Michael W. Busch (SETI), Jean-Luc Margot, Sanjana Prabhu Desai (UCLA), Agata Rozek˙ (U. Kent), Mary L. Hinkle (UCF), Michael K. Shepard (Bloomsburg U.), and Christopher Magri (U. Maine) Summary We propose the continuation of the long-running project R3037 to physically and dynamically characterize the population of near-Earth asteroids with the Arecibo S-band (2380 MHz; 12.6 cm) planetary radar system. The objectives of project R3037 are to: (1) collect high-resolution radar images of and (2) report ultra-precise radar astrometry for the strongest predicted radar targets for the 2020 calendar year plus early January 2021. Such images will be used for three-dimensional shape modeling as the data sets allow. These observations will be carried out as part of the NASA- funded Arecibo planetary radar program, Grant No. 80NSSC19K0523, to PI Anne Virkki (Arecibo Observatory, University of Central Florida) with Patrick Taylor as Institutional PI at the Lunar and Planetary Institute (Universities Space Research Association). Background Radar is arguably the most powerful Earth-based technique for post-discovery physical and dynamical characterization of near-Earth asteroids (NEAs) and plays a crucial role in the nation’s planetary defense initiatives led through the NASA Planetary Defense Coordination Office. -
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 . -
Planets Days Mini-Conference (Friday August 24)
Planets Days Mini-Conference (Friday August 24) Session I : 10:30 – 12:00 10:30 The Dawn Mission: Latest Results (Christopher Russell) 10:45 Revisiting the Oort Cloud in the Age of Large Sky Surveys (Julio Fernandez) 11:00 25 years of Adaptive Optics in Planetary Astronomy, from the Direct Imaging of Asteroids to Earth-Like Exoplanets (Franck Marchis) 11:15 Exploration of the Jupiter Trojans with the Lucy Mission (Keith Noll) 11:30 The New and Unexpected Venus from Akatsuki (Javier Peralta) 11:45 Exploration of Icy Moons as Habitats (Athena Coustenis) Session II: 13:30 – 15:00 13:30 Characterizing ExOPlanet Satellite (CHEOPS): ESA's first s-class science mission (Kate Isaak) 13:45 The Habitability of Exomoons (Christopher Taylor) 14:00 Modelling the Rotation of Icy Satellites with Application to Exoplanets (Gwenael Boue) 14:15 Novel Approaches to Exoplanet Life Detection: Disequilibrium Biosignatures and Their Detectability with the James Webb Space Telescope (Joshua Krissansen-Totton) 14:30 Getting to Know Sub-Saturns and Super-Earths: High-Resolution Spectroscopy of Transiting Exoplanets (Ray Jayawardhana) 14:45 How do External Giant Planets Influence the Evolution of Compact Multi-Planet Systems? (Dong Lai) Session III: 15:30 – 18:30 15:30 Titan’s Global Geology from Cassini (Rosaly Lopes) 15:45 The Origins Space Telescope and Solar System Science (James Bauer) 16:00 Relationship Between Stellar and Solar System Organics (Sun Kwok) 16:15 Mixing of Condensible Constituents with H/He During Formation of Giant Planets (Jack Lissauer) -
Imaging of Near-Earth Asteroids
Imaging of Near-Earth Asteroids. Michael C. Nolan, Arecibo Observatory / Cornell University. [email protected] (787) 878-2612 ext 212 Lance A. M. Benner (Jet Propulsion Laboratory / California Institute of Technology) Marina Brozovič (Jet Propulsion Laboratory / California Institute of Technology) Ellen S. Howell (Arecibo Observatory / Cornell University) Jean-Luc Margot (UCLA) Abstract As remnants of accretion, building blocks of planets, space resources and potential impactors, the asteroids offer insights to solar system formation and evolution. Recent results show that this population is extremely diverse, compositionally, texturally and structurally. As a result, spacecraft cannot explore the population of asteroids in a reasonable time or at a reasonable cost without guidance from Earth-based reconnaissance. Compositional variation can be studied using remote-sensing spectroscopic techniques, either ground-based or from general-purpose space-based telescopes such as HST and JWST. Study of the textural and structural properties of asteroids requires imaging and shape determination. In addition, the largest uncertainties in orbit determination arise from non-gravitational forces, such as the Yarkovsky effect, that depend on the detailed shapes of asteroids. This shape determination can be done crudely using visible lightcurves and in detail using direct imaging (generally using adaptive optics), interferometric and radar techniques. Of these, only ground-based radar using the Arecibo and Goldstone radar systems has been routinely used for asteroid imaging, typically yielding shapes with tens to hundreds of pixels across a diameter and an absolute size accuracy of 5% or better. Other groundbased techniques are unlikely to achieve this level of precision in the upcoming decade, and space-based techniques will visit no more than a few targets. -
Spin State and Moment of Inertia Characterization of 4179 Toutatis
The Astronomical Journal, 146:95 (10pp), 2013 October doi:10.1088/0004-6256/146/4/95 C 2013. The American Astronomical Society. All rights reserved. Printed in the U.S.A. SPIN STATE AND MOMENT OF INERTIA CHARACTERIZATION OF 4179 TOUTATIS Yu Takahashi1,3, Michael W. Busch2,4, and D. J. Scheeres1,5 1 University of Colorado at Boulder, 429 UCB, Boulder, CO 80309-0429, USA 2 National Radio Astronomy Observatory, 1003 Lopezville Road, Box O, Socorro, NM 87801, USA Received 2013 May 17; accepted 2013 August 6; published 2013 September 12 ABSTRACT The 4.5 km long near-Earth asteroid 4179 Toutatis has made close Earth flybys approximately every four years between 1992 and 2012, and has been observed with high-resolution radar imaging during each approach. Its most recent Earth flyby in 2012 December was observed extensively at the Goldstone and Very Large Array radar telescopes. In this paper, Toutatis’ spin state dynamics are estimated from observations of five flybys between 1992 and 2008. Observations were used to fit Toutatis’ spin state dynamics in a least-squares sense, with the solar and terrestrial tidal torques incorporated in the dynamical model. The estimated parameters are Toutatis’ Euler angles, angular velocity, moments of inertia, and the center-of-mass–center-of-figure offset. The spin state dynamics as well as the uncertainties of the Euler angles and angular velocity of the converged solution are then propagated to 2012 December in order to compare the dynamical model to the most recent Toutatis observations. The same technique of rotational dynamics estimation can be applied to any other tumbling body, given sufficiently accurate observations. -
RADAR OBSERVATIONS of NEAR-EARTH ASTEROIDS Lance Benner Jet Propulsion Laboratory California Institute of Technology
RADAR OBSERVATIONS OF NEAR-EARTH ASTEROIDS Lance Benner Jet Propulsion Laboratory California Institute of Technology Goldstone/Arecibo Bistatic Radar Images of Asteroid 2014 HQ124 Copyright 2015 California Institute of Technology. Government sponsorship acknowledged. What Can Radar Do? Study physical properties: Image objects with 4-meter resolution (more detailed than the Hubble Space Telescope), 3-D shapes, sizes, surface features, spin states, regolith, constrain composition, and gravitational environments Identify binary and triple objects: orbital parameters, masses and bulk densities, and orbital dynamics Improve orbits: Very precise and accurate. Measure distances to tens of meters and velocities to cm/s. Shrink position uncertainties drastically. Predict motion for centuries. Prevent objects from being lost. à Radar Imaging is analogous to a spacecraft flyby Radar Telescopes Arecibo Goldstone Puerto Rico California Diameter = 305 m Diameter = 70 m S-band X-band Small-Body Radar Detections Near-Earth Asteroids (NEAs): 540 Main-Belt Asteroids: 138 Comets: 018 Current totals are updated regularly at: http://echo.jpl.nasa.gov/asteroids/index.html Near-Earth Asteroid Radar Detection History Big increase started in late 2011 NEA Radar Detections Year Arecibo Goldstone Number 1999 07 07 10 2000 16 07 18 2001 24 08 25 2002 22 09 27 2003 25 10 29 2004 21 04 23 2005 29 10 33 2006 13 07 16 2007 10 06 15 2008 25 13 26 2009 16 14 19 2010 15 07 22 2011 21 06 22 2012 67 26 77 2013 66 32 78 2014 81 31 96 2015 29 12 36 Number of NEAs known: 12642 (as of June 3) Observed by radar: 4.3% H N Radar Fraction 9.5 1 1 1.000 10.5 0 0 0.000 11.5 1 1 1.000 12.5 4 0 0.000 Fraction of all potential NEA 13.5 10 3 0.300 targets being observed: ~1/3 14.5 39 11 0.282 15.5 117 22 0.188 See the talk by Naidu et al. -
Asteroids Do Have Satellites 289
Merline et al.: Asteroids Do Have Satellites 289 Asteroids Do Have Satellites William J. Merline Southwest Research Institute Stuart J. Weidenschilling Planetary Science Institute Daniel D. Durda Southwest Research Institute Jean-Luc Margot California Institute of Technology Petr Pravec Astronomical Institute of the Academy of Sciences of the Czech Republic Alex D. Storrs Towson University After years of speculation, satellites of asteroids have now been shown definitively to exist. Asteroid satellites are important in at least two ways: (1) They are a natural laboratory in which to study collisions, a ubiquitous and critically important process in the formation and evolu- tion of the asteroids and in shaping much of the solar system, and (2) their presence allows to us to determine the density of the primary asteroid, something which otherwise (except for certain large asteroids that may have measurable gravitational influence on, e.g., Mars) would require a spacecraft flyby, orbital mission, or sample return. Binaries have now been detected in a variety of dynamical populations, including near-Earth, main-belt, outer main-belt, Tro- jan, and transneptunian regions. Detection of these new systems has been the result of improved observational techniques, including adaptive optics on large telescopes, radar, direct imaging, advanced lightcurve analysis, and spacecraft imaging. Systematics and differences among the observed systems give clues to the formation mechanisms. We describe several processes that may result in binary systems, all of which involve collisions of one type or another, either physi- cal or gravitational. Several mechanisms will likely be required to explain the observations. 1. INTRODUCTION sons between, for example, asteroid taxonomic types and our inventory of meteorites. -
Stable Orbits in the Small-Body Problem an Application to the Psyche Mission
Stable Orbits in the Small-Body Problem An Application to the Psyche Mission Stijn Mast Technische Universiteit Delft Stable Orbits in the Small-Body Problem Front cover: Artist illustration of the Psyche mission spacecraft orbiting asteroid (16) Psyche. Image courtesy NASA/JPL-Caltech. ii Stable Orbits in the Small-Body Problem An Application to the Psyche Mission by Stijn Mast to obtain the degree of Master of Science at Delft University of Technology, to be defended publicly on Friday August 31, 2018 at 10:00 AM. Student number: 4279425 Project duration: October 2, 2017 – August 31, 2018 Thesis committee: Ir. R. Noomen, TU Delft Dr. D.M. Stam, TU Delft Ir. J.A. Melkert, TU Delft Advisers: Ir. R. Noomen, TU Delft Dr. J.A. Sims, JPL Dr. S. Eggl, JPL Dr. G. Lantoine, JPL An electronic version of this thesis is available at http://repository.tudelft.nl/. Stable Orbits in the Small-Body Problem This page is intentionally left blank. iv Stable Orbits in the Small-Body Problem Preface Before you lies the thesis Stable Orbits in the Small-Body Problem: An Application to the Psyche Mission. This thesis has been written to obtain the degree of Master of Science in Aerospace Engineering at Delft University of Technology. Its contents are intended for anyone with an interest in the field of spacecraft trajectory dynamics and stability in the vicinity of small celestial bodies. The methods presented in this thesis have been applied extensively to the Psyche mission. Conse- quently, the work can be of interest to anyone involved in the Psyche mission. -
Radar Observations and a Physical Model of Asteroid 4660 Nereus, a Prime Space Mission Target ∗ Marina Brozovic A, ,Stevenj.Ostroa, Lance A.M
Icarus 201 (2009) 153–166 Contents lists available at ScienceDirect Icarus www.elsevier.com/locate/icarus Radar observations and a physical model of Asteroid 4660 Nereus, a prime space mission target ∗ Marina Brozovic a, ,StevenJ.Ostroa, Lance A.M. Benner a, Jon D. Giorgini a, Raymond F. Jurgens a,RandyRosea, Michael C. Nolan b,AliceA.Hineb, Christopher Magri c, Daniel J. Scheeres d, Jean-Luc Margot e a Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109-8099, USA b Arecibo Observatory, National Astronomy and Ionosphere Center, Box 995, Arecibo, PR 00613, USA c University of Maine at Farmington, Preble Hall, 173 High St., Farmington, ME 04938, USA d Aerospace Engineering Sciences, University of Colorado, Boulder, CO 80309-0429, USA e Department of Astronomy, Cornell University, 304 Space Sciences Bldg., Ithaca, NY 14853, USA article info abstract Article history: Near–Earth Asteroid 4660 Nereus has been identified as a potential spacecraft target since its 1982 Received 11 June 2008 discovery because of the low delta-V required for a spacecraft rendezvous. However, surprisingly little Revised 1 December 2008 is known about its physical characteristics. Here we report Arecibo (S-band, 2380-MHz, 13-cm) and Accepted 2 December 2008 Goldstone (X-band, 8560-MHz, 3.5-cm) radar observations of Nereus during its 2002 close approach. Available online 6 January 2009 Analysis of an extensive dataset of delay–Doppler images and continuous wave (CW) spectra yields a = ± = ± Keywords: model that resembles an ellipsoid with principal axis dimensions X 510 20 m, Y 330 20 m and +80 Radar observations Z = 241− m.