Descent Trajectory Reconstruction and Landing Site Positioning of Changâ
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China's Touch on the Moon
commentary China’s touch on the Moon Long Xiao As well as being a milestone in technology, the Chang’e lunar exploration programme establishes China as a contributor to space science. With much still to learn about the Moon, fieldwork beyond Earth’s orbit must be an international effort. hen China’s Chang’e 3 spacecraft geological history of the landing site. touched down on the lunar High-resolution images have shown rocky Wsurface on 14 December 2013, terrain with outcrops of porphyritic basalt, it was the first soft landing on the Moon such as Loong Rock (Fig. 2). Analysis since the Soviet Union’s Luna 24 mission of data collected by the penetrating in 1976. Following on from the decades- Chang’e 3 radar should lead to identification of the old triumphs of the Luna missions and underlying layers of regolith, impact breccia NASA’s Apollo programme, the Chang’e and basalt. lunar exploration programme is leading the China’s robotic field geologist Yutu has charge of a new generation of exploration Basalt outcrop Yutu rover stalled in its traverse of the lunar surface, on the lunar surface. Much like the earlier but plans for the Chang’e 5 sample-return space programmes, the China National mission are moving forward. The primary Space Administration (CNSA) has been objective of the mission will be to return developing its capabilities and technologies 100 m 2 kg of samples from the surface and depths step by step in a series of Chang’e missions UNIVERSITY STATE © NASA/GSFC/ARIZONA of up to 2 m, probably also in the relatively of increasing ambition: orbiting and Figure 1 | The Chinese Chang’e 3 spacecraft and smooth northern Mare Imbrium. -
Mars Reconnaissance Orbiter
Chapter 6 Mars Reconnaissance Orbiter Jim Taylor, Dennis K. Lee, and Shervin Shambayati 6.1 Mission Overview The Mars Reconnaissance Orbiter (MRO) [1, 2] has a suite of instruments making observations at Mars, and it provides data-relay services for Mars landers and rovers. MRO was launched on August 12, 2005. The orbiter successfully went into orbit around Mars on March 10, 2006 and began reducing its orbit altitude and circularizing the orbit in preparation for the science mission. The orbit changing was accomplished through a process called aerobraking, in preparation for the “science mission” starting in November 2006, followed by the “relay mission” starting in November 2008. MRO participated in the Mars Science Laboratory touchdown and surface mission that began in August 2012 (Chapter 7). MRO communications has operated in three different frequency bands: 1) Most telecom in both directions has been with the Deep Space Network (DSN) at X-band (~8 GHz), and this band will continue to provide operational commanding, telemetry transmission, and radiometric tracking. 2) During cruise, the functional characteristics of a separate Ka-band (~32 GHz) downlink system were verified in preparation for an operational demonstration during orbit operations. After a Ka-band hardware anomaly in cruise, the project has elected not to initiate the originally planned operational demonstration (with yet-to-be used redundant Ka-band hardware). 201 202 Chapter 6 3) A new-generation ultra-high frequency (UHF) (~400 MHz) system was verified with the Mars Exploration Rovers in preparation for the successful relay communications with the Phoenix lander in 2008 and the later Mars Science Laboratory relay operations. -
Mro High Resolution Imaging Science Experiment (Hirise)
Sixth International Conference on Mars (2003) 3287.pdf MROHIGHRESOLUTIONIMAGINGSCIENCEEXPERIMENT(HIRISE): INSTRUMENTDEVELOPMENT.AlanDelamere,IraBecker,JimBergstrom,JonBurkepile,Joe Day,DavidDorn,DennisGallagher,CharlieHamp,JeffreyLasco,BillMeiers,AndrewSievers,Scott StreetmanStevenTarr,MarkTommeraasen,PaulVolmer.BallAerospaceandTechnologyCorp.,PO Box1062,Boulder,CO80306 Focus Introduction:Theprimaryfunctionalre- Mechanism PrimaryMirror quirementoftheHiRISEimager,figure1isto PrimaryMirrorBaffle 2nd Fold allowidentificationofbothpredictedandun- Mirror knownfeaturesonthesurfaceofMarstoa muchfinerresolutionandcontrastthanprevi- ouslypossible[1],[2].Thisresultsinacam- 1st Fold erawithaverywideswathwidth,6kmat Mirror 300kmaltitude,andahighsignaltonoise ratio,>100:1.Generationofterrainmaps,30 Filters cmverticalresolution,fromstereoimages Focal requiresveryaccurategeometriccalibration. Plane Theprojectlimitationsofmass,costand schedulemakethedevelopmentchallenging. FocalPlane SecondaryMirror Inaddition,thespacecraftstability[3]must Electronics TertiaryMirror SecondaryMirrorBaffle notbeamajorlimitationtoimagequality. Thenominalorbitforthesciencephaseofthe missionisa3pmorbitof255by320kmwith Figure1Cameraopticalpathoptimizedforlowmass periapsislockedtothesouthpole.Thetrack Integration(TDI)tocreateveryhigh(100:1)signalnoise velocityisapproximately3,400m/s. ratioimages. HiRISEFeatures:TheHiRISEinstrumentperformance Theimagerdesignisanall-reflectivethreemirrorastig- goalsarelistedinTable1.Thedesignfeaturesa50cm matictelescopewithlight-weightedZeroduropticsanda -
To the Moon and Beyond! Article
3/12/2020 Achieve3000: Lesson Printed by: Jessica Christian Printed on: March 12, 2020 To the Moon and Beyond! Article PART 1 NEW DELHI, India. Both India and China are moving ahead in space exploration. Both countries launched space missions in 2013. India's Mars Orbiter Mission (MOM) was sent to Mars in November. China's Chang'e 3 spaceship blasted off on its way to the moon in December. India India launched its first spacecraft bound for Mars on November 5, 2013. The craft spent almost a month in Earth's orbit. Then, on November 30, 2013, the orbiter went on its way to the Red Planet. "The Earth orbiting phase of the spacecraft ended. The spacecraft is now on a course to reach Mars after a journey of about 10 months around the sun," the Indian Space Research Organisation (ISRO) said in early December. The 3,000-pound (1,350-kilogram) orbiter is called Mangalyaan. That means "Mars craft" in Hindi. It must travel 485 million miles (780 million Photo credit and all related images: kilometers) to reach an orbit around Mars. It will take about 300 days. It is Arun Sankar K/AP expected to do this by September 2014. This is the Satish Dhawan Space Center in southern India. India sent its first spaceship to Mars in The orbiter will gather images and data. They will help in determining how November 2013. Martian weather systems work. India is also looking to MOM to figure out what happened to the large quantities of water that are believed to have once existed on Mars. -
The Moon Is a Harsh Chromatogram: the Most Strategic Knowledge Gap (Skg) at the Lunar Surface E
50th Lunar and Planetary Science Conference 2019 (LPI Contrib. No. 2132) 2766.pdf THE MOON IS A HARSH CHROMATOGRAM: THE MOST STRATEGIC KNOWLEDGE GAP (SKG) AT THE LUNAR SURFACE E. Patrick, R. Blase, M. Libardoni, Southwest Research Institute®, 6220 Culebra Rd., San Antonio, TX 78238 ([email protected]) Introduction: Data from analytical instruments de- a gas chromatograph mass spectrometer (GCMS) and ployed during multiple lunar missions, combined with revealed 97% of the composition in that mass channel laboratory results[1], suggest the regolith surface of the to be N2. Henderson et al.[5] also identified amino ac- Moon traps more volatiles in gas-surface interactions ids which were attributed to contamination, but results than is currently understood. We assert that the lunar from recent more sensitive LCMS and GCMS experi- surface behaves as a giant 3-D surface chromatogram, ments by Elsila et al.[1] found some amino acid and separating gas molecules by species as each wafts other organic signatures to be extraterrestrial in origin. across the regolith according to its mobility and ad- While these and other investigations suggest contami- sorption characteristics before eventually becoming nation from the Apollo spacecraft as a likely source for trapped. Herein we present supporting evicence for this a number of observed signatures[1,2,4,5], what is not claim. explained is the nature of the trapping mechanism for In gas chromatography (GC), components of a the N2 feature in 10086, and demonstrates gas retention sample are separated within a column according to from a gas that, under most circumstances, exhibits no their individual partitioning coefficients and by such retention at temperatures around 300 K[3]. -
The Sun As a Gravitational Lens : a Target for Space Missions a Target
“New Trends in Astrodynamics and Applications - V” Po litecn ico di Mil ano, Mil ano (It al y) , 30 J une, 1 -2 Ju ly 2008 The Sun as a Gravitational Lens : A Target for Space Missions Reaching 550 AU to 1000 AU Claudio Maccone Member of the International Academy of Astronautics Home Paggpe: http://www.maccone.com/ E-mail: [email protected] 1 Gravitational Lens of the Sun Figure 1: Basic geometry of the gravitational lens of the Sun: the minimal focal length at 550 AU and the FOCAL spacecraft position. 2 Gravitational Lens of the Sun • The geometry of the Sun gravitational lens is easily described: incoming electromagnetic waves (arriving, for instance, from the center of the Galaxy) pass outside the Sun and pass wihiithin a certain distance r of its center. • Then a basic result following from General Relativity shows that the corresponding dfltideflection angle ()(r) at the distance r from the Sun center is given by (Einstein, 1907): 4GM α (r ) = Sun . c 2 r 3 Gravitational Lens of the Sun • Let’s set the following parameters for the Sun: 1. Assumed Mass of the Sun: 1.9889164628 . 1030 kg, that is μSun = 132712439900 kg3s-2 2. Assumed Radius of the Sun: 696000 km 3. Sun Mean Density: 1408.316 kgm-3 4. Sc hwarzsc hild radi us of th e S un: 2 .953 k m One then finds the BASIC RESULT: MINIMAL FOCAL DISTANCE OF THE SUN: 548.230 AU ~ 3.17 light days ~ 13. 86 times th e Sun-to-Plut o di st ance. -
PROJECT PENGUIN Robotic Lunar Crater Resource Prospecting VIRGINIA POLYTECHNIC INSTITUTE & STATE UNIVERSITY Kevin T
PROJECT PENGUIN Robotic Lunar Crater Resource Prospecting VIRGINIA POLYTECHNIC INSTITUTE & STATE UNIVERSITY Kevin T. Crofton Department of Aerospace & Ocean Engineering TEAM LEAD Allison Quinn STUDENT MEMBERS Ethan LeBoeuf Brian McLemore Peter Bradley Smith Amanda Swanson Michael Valosin III Vidya Vishwanathan FACULTY SUPERVISOR AIAA 2018 Undergraduate Spacecraft Design Dr. Kevin Shinpaugh Competition Submission i AIAA Member Numbers and Signatures Ethan LeBoeuf Brian McLemore Member Number: 918782 Member Number: 908372 Allison Quinn Peter Bradley Smith Member Number: 920552 Member Number: 530342 Amanda Swanson Michael Valosin III Member Number: 920793 Member Number: 908465 Vidya Vishwanathan Dr. Kevin Shinpaugh Member Number: 608701 Member Number: 25807 ii Table of Contents List of Figures ................................................................................................................................................................ v List of Tables ................................................................................................................................................................vi List of Symbols ........................................................................................................................................................... vii I. Team Structure ........................................................................................................................................................... 1 II. Introduction .............................................................................................................................................................. -
Comparisions of Ground Penetrating Radar Results at Chang’E-3 and Chang’E-4 Landing Sites
51st Lunar and Planetary Science Conference (2020) 1125.pdf COMPARISIONS OF GROUND PENETRATING RADAR RESULTS AT CHANG’E-3 AND CHANG’E-4 LANDING SITES. J. L. Lai1, Y. Xu1, X. P. Zhang1, L. Xiao1,2, Q. Yan1, X. Meng1, B. Zhou3, Z. H. Dong3, and D. Zhao3 1State Key Laboratory of Lunar and Planetary Sciences, Macau University of Science and Technology, Macau ([email protected]) , 2Planetary Science Institute, School of Earth Sciences, China University of Geosciences, Wu- han, China, 3Key Laboratory of Electromagnetic Radiation and Detection Technology, Institute of Electronics, Chinese Acade- my of Science, Beijing, China. Introduction: On 14 December 2013, Chang’e-3 (CE-3) landed at 340.49°E, 44.12°N in northern Mare Imbrium and released the Yutu rover. On 3 January 2019, Chang’e-4 (CE-4) landed at 177.588° E, 45.457° S (Statio Tianhe) in the Von Kármán crater of the SPA basin and released the Yutu-2 rover. The two rovers both equipped with ground-penetrating radars (hereaf- ter referred to as Lunar Penetrating Radar, LPR) pro- vide unique data sets of in situ measurements of the lunar regolith [1]. The aim of this work is to report the first five lunar days of CE-4 LPR results at 500 MHz and compare the results between the two sites. Chang’e-3 and Chang’e-4 Landing sites CE-3 probe landed in the Imbrium basin on bas- alts inferred as Eratosthenian in age. These represent some of the youngest units on the Moon at about 2.35- Figure 1 (a) The CE-3 landing site on TiO2 map 2.5 billion years (Gy) old[2], for instance compared derived from Lunar Reconnaissance Orbiter Camera with samples returned by the Apollo and Luna mis- (LROC) Wide-Angle Camera (WAC) images (Sato et sions. -
ESA's Gaia Mission: a Billion Stars with a Billion Pixels
FOCUS I PHOTONIC TECHNIQUES AND TECHNOLOGIES ESA’S GAIA MISSION: a billion stars with a billion pixels Jos DE BRUIJNE 1 Astrometry is the astronomical discipline of measuring the positions, 2 Matthias ERDMANN and changes therein, of celestial bodies. Accurate astrometry from 1 Directorate of Science, European Space Agency, ESA/ESTEC, the ground is limited by the blurring effects induced by the Earth’s The Netherlands atmosphere. Since decades, Europe has been at the forefront of 2 Directorate of Earth Observation, making astrometric measurements from space. The European Space European Space Agency, ESA/ ESTEC, The Netherlands Agency (ESA) launched the first satellite dedicated to astrometry, [email protected] named Hipparcos, in 1989, culminating in the release of the Hipparcos Catalogue containing astrometric data for 117 955 stars in 1997. Since mid 2014, Hipparcos’ successor, Gaia, has been collecting astrometric data, with a 100 times improved precision, for 10 000 times as many stars. lthough astrometry sounds revolves around the sun – and of pro- the telescope in 1608, the first reliable boring, it is of fundamental per motion – the continuous, true parallax measurement of a star other Aimportance to many branches displacement of a star on the sky as than the sun was only made in 1838. of astronomy and astrophysics. The a result of its velocity in space relative The reason for this late success is the reason for this is that astrometry can to the sun. Measuring the distances fact that stars are located at extremely determine -
An Implementation Concept for the ASPIRE Mission
An Implementation Concept for the ASPIRE Mission. W. D. Deininger* ([email protected]), W. Purcell,* P. Atcheson,*G. Mills,* S. A Sandford,** R. P. Hanel,** M. McKelvey,** and R. McMurray** *Ball Aerospace & Technologies Corp. (BATC) P. O. Box 1062 Boulder, CO, USA 80306-1062 **NASA Ames Research Center Moffett Field, CA, USA 94035 Abstract—The Astrobiology Space Infrared Explorer complex and tied to the cyclic process whereby these (ASPIRE) is a Probe-class mission concept developed as elements are ejected into the diffuse interstellar medium part of NASA’s Astrophysics Strategic Mission Concept (ISM) by dying stars, gathered into dense clouds and studies. 1 2 ASPIRE uses infrared spectroscopy to explore formed into the next generation of stars and planetary the identity, abundance, and distribution of molecules, systems (Figure 1). Each stage in this cycle entails chemical particularly those of astrobiological importance throughout alteration of gas- and solid-state species by a diverse set of the Universe. ASPIRE’s observational program is focused astrophysical processes: hocks, stellar winds, radiation on investigating the evolution of ices and organics in all processing by photons and particles, gas-phase neutral and phases of the lifecycle of carbon in the universe, from ion chemistry, accretion, and grain surface reactions. These stellar birth through stellar death while also addressing the processes create new species, destroy old ones, cause role of silicates and gas-phase materials in interstellar isotopic enrichments, shuffle elements between chemical organic chemistry. ASPIRE achieves these goals using a compounds, and drive the universe to greater molecular Spitzer-derived, cryogenically-cooled, 1-m-class telescope complexity. -
50 Years of Dust on the Moon: from Apollo to Cheng'e-4
DUST ON THE MOON: FROM APOLLO TO CHENG’E-4 Prof. Brian J. O’Brien School of Physics, University of Western Australia [email protected] www.uwa.edu.au/people/brian.obrien Ph. 61 8 9387 3827 DAP2017 Boulder, Colorado 12 January 2017 Presented by courtesy of Dr William M. Farrell, GSFC LDAP2010: OVERVIEW BY O’BRIEN 1. 1st REVIEW OF DDE, TDS AND LEAM EXPTS 2. DDE: 8 DISCOVERIES O’Brien 1970-2009 3. TDS: FIRST MODERN DISCUSSION GOLD’s DISCOVERY OF COHESIVE FORCES IN 1971 4. LEAM: SUGGESTED ALTERNATIVE CAUSE AS NOISE BITS IN BURSTS, PERHAPS FROM EMI 5. FINAL O’B IN 2011 “BUT WHO WILL LISTEN?” 6. LADEE FINDINGS CONSISTENT WITH #3 + #4? COHESIVE FORCES OF LUNAR DUST SURFACE DUST ON MOON: MAJOR ITEMS SINCE LDAP2010 O’BRIEN 2010-16 CHENG’E-3 & CHENG’E-4 • 2011:O’BRIEN LDAP-2010 • CHENG’E-3 & YUTU doi:10.1016/j.pss.2011.04.016 • YUTU FIFTH LUNAR ROVER • 2013: LUNAR WEATHER AT • IN 2013 FIRST IN 40 YEARS 3 APOLLO SITES • MOVED 100m LUNAR DAY 1 http:dx.doi.org/10.1016/j.pss. • NO MOVEMENTS AFTER 1st 2013.1002/2013SW000978 SUNRISE: WHY NOT? • 2015: SUNRISE-DRIVEN GROUND-TRUTH FACTS • CHENG’E-4 (2018): dx.doi.org/10.1016/j.pss.2015 #1 PRIORITY CHANGED 2016 .09.018 TO LUNAR DUST STUDIES SUNRISE DRIVEN EFFECTS APOLLO 12 DUST SYNERGIES WITH 2 SOLAR DETECTOR DDE CELLS AT RIGHT ANGLES INVENTED 12/01/1966 1 VSCE VERTICAL SOLAR CELL FACES EAST (SUNRISE MAX) 2 HSC HORIZONTAL CELL FACING UP (NOON MAX.). -
Mission to the Solar Gravity Lens Focus: Natural Highground for Imaging Earth-Like Exoplanets L
Planetary Science Vision 2050 Workshop 2017 (LPI Contrib. No. 1989) 8203.pdf MISSION TO THE SOLAR GRAVITY LENS FOCUS: NATURAL HIGHGROUND FOR IMAGING EARTH-LIKE EXOPLANETS L. Alkalai1, N. Arora1, M. Shao1, S. Turyshev1, L. Friedman8 ,P. C. Brandt3, R. McNutt3, G. Hallinan2, R. Mewaldt2, J. Bock2, M. Brown2, J. McGuire1, A. Biswas1, P. Liewer1, N. Murphy1, M. Desai4, D. McComas5, M. Opher6, E. Stone2, G. Zank7, 1Jet Propulsion Laboratory, Pasadena, CA 91109, USA, 2California Institute of Technology, Pasadena, CA 91125, USA, 3The Johns Hopkins University Applied Physics Laboratory, Laurel, MD 20723, USA,4Southwest Research Institute, San Antonio, TX 78238, USA, 5Princeton Plasma Physics Laboratory, Princeton, NJ 08543, USA, 6Boston University, Boston, MA 02215, USA, 7University of Alabama in Huntsville, Huntsville, AL 35899, USA, 8Emritus, The Planetary Society. Figure 1: A SGL Probe Mission is a first step in the goal to search and study potential habitable exoplanets. This figure was developed as a product of two Keck Institute for Space Studies (KISS) workshops on the topic of the “Science and Enabling Technologies for the Exploration of the Interstellar Medium” led by E. Stone, L. Alkalai and L. Friedman. Introduction: Recent data from Voyager 1, Kepler and New Horizons spacecraft have resulted in breath-taking discoveries that have excited the public and invigorated the space science community. Voyager 1, the first spacecraft to arrive at the Heliopause, discovered that Fig. 2. Imaging of an exo-Earth with solar gravitational Lens. The exo-Earth occupies (1km×1km) area at the image plane. Using a 1m the interstellar medium is far more complicated and telescope as a 1 pixel detector provides a (1000×1000) pixel image! turbulent than expected; the Kepler telescope According to Einstein’s general relativity, gravity discovered that exoplanets are not only ubiquitous but induces refractive properties of space-time causing a also diverse in our galaxy and that Earth-like exoplanets massive object to act as a lens by bending light.