Robotic Asteroid Prospector
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Return to the Moon Mission Overview
Return to the Moon Mission Overview The new millennium is still young, but humans using the lastest in transport technology to are preparing to Return to the Moon, reduce the travel time. In addition to verifying spurred on by the verification of ice water on the best site for the establishment of the the lunar surface by Lunar Prospector in lunar base, during the course of the mission, 1998. Composed of hydrogen and oxygen – the crew will recover a probe that is the elements that make up water – the lunar stranded in space and access the damage to ice provides a core resource for long-term the probe, and then build and launch an human presence on the lunar surface. equipment module to the lunar surface. Lunar Prospector was followed by a series of Some information has been previously successful robotic missions designed to obtained from the potential lunar base sites. probe the concept that the ice water could A detailed study has determined that the be harvested. Once collected, the ice water base site must contain solid, metals, and can be turned into drinking water, oxygen for potentially useful resources such as helium-3. life support of a lunar base, nutrients as the Rock and soil samples, soil composition, and basis for agriculture, components needed for seismic information have been gathered by rocket fuel, or when combined with lunar soil, previous missions from a portion of the the basics for construction materials. Not potential sites. Experiments on soil and rock only did those robotic missions successfully samples from other possible sites must be prove that concept, but since then, additional performed in order to determine the best robotic staging missions have landed and site for the lunar base. -
Physical Characterization of the Potentially-Hazardous High-Albedo Asteroid (33342) 1998 WT from Thermal-Infrared Observations Alan W
Physical Characterization of the Potentially-Hazardous High-Albedo Asteroid (33342) 1998 WT from Thermal-Infrared Observations Alan W. Harris, Michael Mueller, Marco Delbó, Schelte J. Bus To cite this version: Alan W. Harris, Michael Mueller, Marco Delbó, Schelte J. Bus. Physical Characterization of the Potentially-Hazardous High-Albedo Asteroid (33342) 1998 WT from Thermal-Infrared Observations. Icarus, Elsevier, 2007, 188 (2), pp.414. 10.1016/j.icarus.2006.12.003. hal-00499067 HAL Id: hal-00499067 https://hal.archives-ouvertes.fr/hal-00499067 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 Physical Characterization of the Potentially-Hazardous High-Albedo Asteroid (33342) 1998 WT24 from Thermal-Infrared Observations Alan W. Harris, Michael Mueller, Marco Delbó, Schelte J. Bus PII: S0019-1035(06)00446-5 DOI: 10.1016/j.icarus.2006.12.003 Reference: YICAR 8146 To appear in: Icarus Received date: 27 September 2006 Revised date: 6 December 2006 Accepted date: 8 December 2006 Please cite this article as: A.W. Harris, M. Mueller, M. Delbó, S.J. Bus, Physical Characterization of the Potentially-Hazardous High-Albedo Asteroid (33342) 1998 WT24 from Thermal-Infrared Observations, Icarus (2006), doi: 10.1016/j.icarus.2006.12.003 This is a PDF file of an unedited manuscript that has been accepted for publication. -
Physical Properties of Near-Earth Asteroids
Planet. Space Sci., Vol. 46, No. 1, pp. 47-74, 1998 Pergamon N~I1998 Elsevier Science Ltd All rights reserved. Printed in Great Britain 00324633/98 $19.00+0.00 PII: SOO32-0633(97)00132-3 Physical properties of near-Earth asteroids D. F. Lupishko’ and M. Di Martino’ ’ Astronomical Observatory of Kharkov State University, Sumskaya str. 35, Kharkov 310022, Ukraine ‘Osservatorio Astronomic0 di Torino, I-10025 Pino Torinese (TO), Italy Received 5 February 1997; accepted 20 June 1997 rather small objects, usually of the order of a few kilo- metres or less. MBAs of such sizes are generally not access- ible to ground-based observations. Therefore, when NEAs approach the Earth (at distances which can be as small as 0.01-0.02 AU and sometimes less) they give a unique chance to study objects of such small sizes. Some of them possibly represent primordial matter, which has preserved a record of the earliest stages of the Solar System evolution, while the majority are fragments coming from catastrophic collisions that occurred in the asteroid main- belt and could provide “a look” at the interior of their much larger parent bodies. Therefore, NEAs are objects of special interest for sev- eral reasons. First, from the point of view of fundamental science, the problems raised by their origin in planet- crossing orbits, their life-time, their possible genetic relations with comets and meteorites, etc. are closely connected with the solution of the major problem of “We are now on the threshold of a new era of asteroid planetary science of the origin and evolution of the Solar studies” System. -
Conceptual Human-System Interface Design for a Lunar Access Vehicle
Conceptual Human-System Interface Design for a Lunar Access Vehicle Mary Cummings Enlie Wang Cristin Smith Jessica Marquez Mark Duppen Stephane Essama Massachusetts Institute of Technology* Prepared For Draper Labs Award #: SC001-018 PI: Dava Newman HAL2005-04 September, 2005 http://halab.mit.edu e-mail: [email protected] *MIT Department of Aeronautics and Astronautics, Cambridge, MA 02139 TABLE OF CONTENTS 1 INTRODUCTION..................................................................................................... 1 1.1 THE GENERAL FRAMEWORK................................................................................ 1 1.2 ORGANIZATION.................................................................................................... 2 2 H-SI BACKGROUND AND MOTIVATION ........................................................ 3 2.1 APOLLO VS. LAV H-SI........................................................................................ 3 2.2 APOLLO VS. LUNAR ACCESS REQUIREMENTS ...................................................... 4 3 THE LAV CONCEPTUAL PROTOTYPE............................................................ 5 3.1 HS-I DESIGN ASSUMPTIONS ................................................................................ 5 3.2 THE CONCEPTUAL PROTOTYPE ............................................................................ 6 3.3 LANDING ZONE (LZ) DISPLAY............................................................................. 8 3.3.1 LZ Display Introduction................................................................................. -
DART Mission Update
Kinetic Impactor Andy Cheng JHU/APL 15 Nov 2018 DART Mission Update Goddard Space Flight Center Johnson Space Center Langley Research Center Glenn Research Center Marshall Space Flight Center Planetary Defense Coordination Office 1 Regimes of Primary Applicability for Planetary Defense Mitigation Defending Planet Earth (2010) Zero PHAs National Academy of Sciences Deep Impact Recommendation: “the first priority for a space About 150 PHAs mission in the mitigation area is an experimental test of a kinetic impactor” About 5,000 PHAs DART is the first kinetic DART impact test at a realistic scale for planetary Too small to be Defending Planet Earth (2010) considered PHAs defense 2 Launch June 15, 2021 March 6, 2022 IMPACT: October 5, 2022 2001 CB21 flyby S-type, 578 meters, 3.3-hour rotation rate LICIA (Light Italian Cubesat for Imaging of Asteroids) ASI contribution, under consideration DART Spacecraft 65803 Didymos 560 kg arrival mass Didymos-B (1996 GT) Didymos-A 12.5 m × 2.4 m × 2.0 m 163 meters 1,180-meter separation 780 meters, S-type 6 km/s closing speed 11.92-hour orbital period between centers of A and B 2.26-hour rotation period Earth-Based Observations • Target the binary asteroid Didymos system 0.07 AU range at impact Predicted ~8-minute change • Impact Didymos-B and change its orbital period in binary orbit period • Measure the period change from Earth DART – Double Asteroid Redirection Test 3 DART Program Update .DART mission confirmed by NASA in August, 2018. DART is in PHASE C-D .NASA has re-affirmed decision to use NEXT- C ion propulsion system for DART Autonomous navigation .NASA will procure launch services for DART using imager to guide to target through NLS; LV selection is in process ─ DART will have dedicated LV .LICIACube, an ASI-contributed cubesat ─ Letters exchanged between NASA and ASI ─ Studying operations concept and cubesat NEXT-C ion propulsion accommodations on DART first flight 4 DART Ion Propulsion Mission First flight of NASA NEXT-C ion engine . -
Reviewing the Contribution of GRAIL to Lunar Science and Planetary Missions Maria T
EPSC Abstracts Vol. 12, EPSC2018-575, 2018 European Planetary Science Congress 2018 EEuropeaPn PlanetarSy Science CCongress c Author(s) 2018 Reviewing the contribution of GRAIL to lunar science and planetary missions Maria T. Zuber and David E. Smith Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 02139- 4307, USA. ([email protected], [email protected]) Abstract Q of the Moon determined to be 41±4 at the monthly frequency. The GRAIL Discovery mission to the Moon in 2011 provided an unprecedentedly accurate gravity field model for the Moon. The goal of the mission was to provide insight into the structure of the Moon from its interior to the surface but it also made significant contributions to lunar spacecraft operations for all future lunar missions to the Moon. We discuss the science and the broader contributions from this mission that completed its objectives in December 2012 when the spacecraft impacted the lunar surface. 1. Introduction Figure 1: Free-air gravity of the Moon from GRAIL. GRAIL was a mission designed to measure the Full uniform resolution spherical harmonic models gravity field of the Moon with both high accuracy were obtained out to degree & order 1200 with and high resolution. The measurement goal was to special fields with higher resolutions over certain obtain the gravity at resolutions that would enable areas to degree and order 1800. interpretation of the crust at fractions of its thickness, estimated at the time of launch to be about 45 km. To 3. Mission Operations obtain a surface resolution of less than 10 km required the spacecraft to orbit the Moon at less than The significant improvement in our knowledge of the 20 km, an altitude that was considered dangerous at gravity field of the Moon by GRAIL enabled the re- that time without an accurate gravity field model. -
Distribution and Orientation of Boulders on Asteroid 25143 Itokawa
Distribution and Orientation of Boulders on Asteroid 25143 Itokawa Sara Mazrouei-Seidani A Thesis submitted to the Faculty of Graduate Studies in Partial Fulfillment of the Requirements for the Degree of Master of Science Graduate Program in Earth and Space Science, York University, Toronto, Ontario September 2012 © Sara Mazrouei-Seidani 2012 Library and Archives Bibliotheque et Canada Archives Canada Published Heritage Direction du 1+1 Branch Patrimoine de I'edition 395 Wellington Street 395, rue Wellington Ottawa ON K1A0N4 Ottawa ON K1A 0N4 Canada Canada Your file Votre reference ISBN: 978-0-494-91769-5 Our file Notre reference ISBN: 978-0-494-91769-5 NOTICE: AVIS: The author has granted a non L'auteur a accorde une licence non exclusive exclusive license allowing Library and permettant a la Bibliotheque et Archives Archives Canada to reproduce, Canada de reproduire, publier, archiver, publish, archive, preserve, conserve, sauvegarder, conserver, transmettre au public communicate to the public by par telecommunication ou par I'lnternet, preter, telecommunication or on the Internet, distribuer et vendre des theses partout dans le loan, distrbute and sell theses monde, a des fins commerciales ou autres, sur worldwide, for commercial or non support microforme, papier, electronique et/ou commercial purposes, in microform, autres formats. paper, electronic and/or any other formats. The author retains copyright L'auteur conserve la propriete du droit d'auteur ownership and moral rights in this et des droits moraux qui protege cette these. Ni thesis. Neither the thesis nor la these ni des extraits substantiels de celle-ci substantial extracts from it may be ne doivent etre imprimes ou autrement printed or otherwise reproduced reproduits sans son autorisation. -
Bias-Corrected Population, Size Distribution, and Impact Hazard for the Near-Earth Objects ✩
Icarus 170 (2004) 295–311 www.elsevier.com/locate/icarus Bias-corrected population, size distribution, and impact hazard for the near-Earth objects ✩ Joseph Scott Stuart a,∗, Richard P. Binzel b a MIT Lincoln Laboratory, S4-267, 244 Wood Street, Lexington, MA 02420-9108, USA b MIT EAPS, 54-426, 77 Massachusetts Avenue, Cambridge, MA 02139, USA Received 20 November 2003; revised 2 March 2004 Available online 11 June 2004 Abstract Utilizing the largest available data sets for the observed taxonomic (Binzel et al., 2004, Icarus 170, 259–294) and albedo (Delbo et al., 2003, Icarus 166, 116–130) distributions of the near-Earth object population, we model the bias-corrected population. Diameter-limited fractional abundances of the taxonomic complexes are A-0.2%; C-10%, D-17%, O-0.5%, Q-14%, R-0.1%, S-22%, U-0.4%, V-1%, X-34%. In a diameter-limited sample, ∼ 30% of the NEO population has jovian Tisserand parameter less than 3, where the D-types and X-types dominate. The large contribution from the X-types is surprising and highlights the need to better understand this group with more albedo measurements. Combining the C, D, and X complexes into a “dark” group and the others into a “bright” group yields a debiased dark- to-bright ratio of ∼ 1.6. Overall, the bias-corrected mean albedo for the NEO population is 0.14 ± 0.02, for which an H magnitude of 17.8 ± 0.1 translates to a diameter of 1 km, in close agreement with Morbidelli et al. (2002, Icarus 158 (2), 329–342). -
Near Earth Objects As Resources for Space Industrialization
Solar System Development Journal (2001) 1(1), 1-31 http://www.resonance-pub.com ISSN:1534-8016 NEAR EARTH OBJECTS AS RESOURCES FOR SPACE INDUSTRIALIZATION MARK SONTER Consultant, Asteroid Enterprises Pty Ltd, 28 Ian Bruce Crescent, Balgownie, New South Wales 2519, Australia [email protected] (Received 11 February 2001, and in final form 13 August 2001*) This paper reviews concepts for mining the Near-Earth Asteroids for supply of resources to future in-space industrial activities. It identifies Expectation Net Present Value as the appropriate measure for determining the technical and economic feasibility of a hypothetical asteroid mining venture, just as it is the appropriate measure for the feasibility of a proposed terrestrial mining venture. In turn, ENPV can obviously be used as a ‘design driver’ to sieve the alternative options, in selection of target, mission profile, mining and processing methods, propulsion for return trajectory, and earth-capture mechanism. 1. INTRODUCTION The Near Earth Asteroids are potential impact threats to Earth, but also a particularly accessible subset of them does provide potentially attractive targets for resources to support space industrialization. Robust technical and economic approaches to evaluation of the feasibility of proposed projects are necessary for assessment of such space mining ventures. This paper discusses the technical engineering and mission–planning choices and shows how the concept of probabilistic Net Present Value can be used to optimize these choices, and hence select between alternative asteroid mining mission designs. The generic mission reviewed envisages a lightweight remote (teleoperated) or semiautonomous miner, recovering products such as water or nickel-iron metal, from highly- accessible NEAs, and returning it to Low Earth Orbit (LEO), for sale and use in LEO, using solar power and some of the recovered mass as propellant. -
Asteroids + Comets
Datasets for Asteroids and Comets Caleb Keaveney, OpenSpace intern Rachel Smith, Head, Astronomy & Astrophysics Research Lab North Carolina Museum of Natural Sciences 2020 Contents Part 1: Visualization Settings ………………………………………………………… 3 Part 2: Near-Earth Asteroids ………………………………………………………… 5 Amor Asteroids Apollo Asteroids Aten Asteroids Atira Asteroids Potentially Hazardous Asteroids (PHAs) Mars-crossing Asteroids Part 3: Main-Belt Asteroids …………………………………………………………… 12 Inner Main Asteroid Belt Main Asteroid Belt Outer Main Asteroid Belt Part 4: Centaurs, Trojans, and Trans-Neptunian Objects ………………………….. 15 Centaur Objects Jupiter Trojan Asteroids Trans-Neptunian Objects Part 5: Comets ………………………………………………………………………….. 19 Chiron-type Comets Encke-type Comets Halley-type Comets Jupiter-family Comets C 2019 Y4 ATLAS About this guide This document outlines the datasets available within the OpenSpace astrovisualization software (version 0.15.2). These datasets were compiled from the Jet Propulsion Laboratory’s (JPL) Small-Body Database (SBDB) and NASA’s Planetary Data Service (PDS). These datasets provide insights into the characteristics, classifications, and abundance of small-bodies in the solar system, as well as their relationships to more prominent bodies. OpenSpace: Datasets for Asteroids and Comets 2 Part 1: Visualization Settings To load the Asteroids scene in OpenSpace, load the OpenSpace Launcher and select “asteroids” from the drop-down menu for “Scene.” Then launch OpenSpace normally. The Asteroids package is a big dataset, so it can take a few hours to load the first time even on very powerful machines and good internet connections. After a couple of times opening the program with this scene, it should take less time. If you are having trouble loading the scene, check the OpenSpace Wiki or the OpenSpace Support Slack for information and assistance. -
Amun Mining Mission
“TUDOR VIANU” National High School of Computer Science ODYSSEUS Amun Mining Mission Dare to dream… Dare to discover… Dare to create Elena Nica Alexandra Voinea 15/02/2013 Contents Introduction 1.Methodology and Sustainability 1.1 Feasibility 1.2 Finding and Choosing Asteroids 1.2.1 GEO telescopes 1.2.2 Astrometrica 1.3 Composition 1.4 Location 1.5 Research (Part One) 1.6 Mission Outline 1.7 Landing 1.8 Resources 1.9 Mining 1.9.1 Mining Season 1.9.2 Processing 1.9.3 Permanent atomized mining bases 1.10 Transport of Goods 2. Structural Design 2.1 General Layout 2.2 Sizes and dimensions 2.3 Views 2.4 Shape and Payload 2.5 Orbit Transfer for the Amun Mission 2.6 Orbit Rendezvous 3. Technical Engineering Part 1 3.1 Payload 3.2 ADCS 3.3 Power and Energy 3.3.1 Solar panels 3.3.2 RTG 3.3.3 The Uranium Reactor 3.3.4 Mini-Nuclear Reactors 3.4 Materials 3.5 Thermal Insulation 3.6 Radiation Insulation 3.7 Telecommunications 3.7.1 Noise 3.7.2 Amplification 3.7.3 Coding and Multiple Access Amun Mining Mission 3.8 Launchers 3.8.1 Further travel, orbital transfer and adjustment thrusters 3.8.2 Chemical Rockets 3.8.3 Thrusters 5. Construction 5.1 Building Materials 5.2 Location 5.3 Building phases Launching, Landing and Transporting Loads Description of Procedure 6. Research 6.1 Asteroid Bases 6.1.1.Base One 6.1.2 Base Two 6.2 Other materials, new compounds 6.3 Conclusion 7. -
BOULDERS on ASTEROIDS DIDYMOS and DIMORPHOS: FUTURE DART-Liciacube OBSERVATIONS
52nd Lunar and Planetary Science Conference 2021 (LPI Contrib. No. 2548) 1116.pdf BOULDERS ON ASTEROIDS DIDYMOS AND DIMORPHOS: FUTURE DART-LICIACube OBSERVATIONS M. Pajola1, A. Lucchetti1, S. Ivanovski2, G. Poggiali3,4, S. Ieva5, D. Perna5, E. Dotto5, V. Della Corte6, G. Cremonese1, M. Amoroso7, S. Pirrotta7, E. Mazzotta Epifani5, A. Cheng8, N. Chabot8, A. Rivkin8, O. Barnouin8, C. Ernst8, R.T. Daly8, M. Hirabayashi9, E. Asphaug10, S.R. Schwartz10, J.M. Trigo-Rodriguez11, E.G. Fahnestock12, P. Michel13, I. Bertini14, J.R. Brucato3, A. Capannolo15, B. Cotugno16, V. Di Tana16, I. Gai17, G. Impresario7, M. Lavagna15, A. Meneghin3, F. Miglioretti16, D. Modenini17, P. Palumbo14,6, A. Rossi18, E. Simioni1, S. Simonetti16, P. Tortora17, M. Zannoni17, G. Zanotti15, A. Zinzi19,7. 1INAF-Astronomical Observatory of Padova, Vic. Osservatorio 5, 35122 Padova, Italy ([email protected]); 2INAF Osservatorio Astronomico di Trieste, Trieste, Italy; 3INAF Osservatorio Astrofisico di Arcetri, Firenze, Italy; 4Università di Firenze, Dipartimento di Fisica e Astronomia, Sesto Fiorentino (Firenze), Italy; 5INAF Osservatorio Astronomico di Roma, Monte Porzio Catone (Roma), Italy; 6INAF Istituto di Astrofisica e Planetologia Spaziali, Roma, Italy; 7Agenzia Spaziale Italiana, via del Politecnico, 00133 Roma, Italy; 8Johns Hopkins University Applied Physics Laboratory, Laurel, MD-USA; 9Auburn University, Auburn, AL-USA; 10Lunar and Planetary Laboratory, University of Arizona, Tucson, AZ-USA; 11Institute of Space Sciences (IEEC-CSIC), Dept. of Astrophysics,