The Curiosity Rover: Robotic Geologist and Explorer

Total Page:16

File Type:pdf, Size:1020Kb

The Curiosity Rover: Robotic Geologist and Explorer Start recording—title slide—1 of 3 LIVE INTERACTIVE LEARNING @ YOUR DESKTOP The Curiosity Rover: Robotic Geologist and Explorer Presented by: Jordan Evans May 21, 2013 6:30 p.m. – 8:00 p.m. Eastern time 1 NSTA Learning Center—2 of 3 2 http://learningcenter.nsta.org About the NSTA Learning Center—3 of 3 NSTA Learning Center • 10,800+ resources – 3,700+ free! – Add to “My Library” to access at your convenience • Community forums • Online advisors to assist you • Tools to plan and document your learning • http://learningcenter.nsta.org 3 Introducing today’s presenters Introducing today’s presenter… Jordan Evans NASA’s Jet Propulsion Laboratory Pasadena, CA 4 Jet Propulsion Laboratory California Institute of Technology The Curiosity Rover: Robotic Geologist and Explorer Jordan Evans JPL/Caltech/NASA 5 @Jordan2Mars Brief Biography… • Led the “Flight System” design, build, test, launch, and operations on the Mars Science Laboratory Project • Aerospace Engineering – San Diego State University and University of Maryland • Worked on both Aircraft and Spacecraft • Jazz Musician (Bass) • Bacon Maker • Science Advisor • Woodworker • Camper Restorer 6 Blaine Baggett Executive Manager, Office of Communications and Education Jet Propulsion Laboratory Pasadena, CA 7 Why Mars? 8 The wonderful future From the 1956 book, The Exploration of Mars, by von Braun and Willy Ley, with paintings by Chesley Bonestell Mars Exploration is CHALLENGING 10 Did you watch Curiosity’s landing on the night of August 5th (PT)? ✔ Yes ✖ No 11 Did you watch Curiosity’s landing on the night of August 5th (PT)? An estimated 50 million people watched the landing! 12 13 Only 50% of Mars landers launched have worked USSR: Mars 2 1971 (crashed) USSR: Mars 3 1971 (landed, radio died) USSR: Mars 6 1973 (aero data, crashed?) USSR: Mars 7 1974 (missed Mars) US: Viking 1 1975 US: Viking 2 1975 USSR: Mars ‘96 (2) 1996 (failed launch) US: Mars Pathfinder 1996 US: Mars Polar Lander 1998 (crashed?) US: DS-2 Microprobes (2) 1998 (crashed?) EU/UK: Beagle II 2003 (crashed?) US: MER Spirit 2003 US: MER Opportunity 2003 US: Phoenix 2007 US: MSL Curiosity 2011 [launch dates] 14 Thousands of problems to solve. 15 Testing 17 More testing More testing More testing 2010 Finally, a real Mars Science Lab! Rover Packaging Ready for flight Ready for the fairing Encapsulation at KSC ATLAS V fairing Launch Complex 41 NASA/KSC Atlas V Careful …. MSL Launch: Nov 26, 2011 Does every Mars-faring nation use the same approach to get to Mars? ✔ Yes ✖ No 30 Does every Mars-faring nation use the same approach to get to Mars? 31 The mission …. Mission Overview ENTRY, DESCENT, LANDING • Guided entry and powered “sky crane” descent • 20×25-km landing ellipse • Access to landing sites ±30° CRUISE/APPROACH latitude, <0 km elevation • 8.5-month cruise • 900-kg rover • Arrived August 5, 2012 SURFACE MISSION • Prime mission is one Mars year (687 days) LAUNCH • Latitude-independent and long- lived power source • Nov. 26, 2011 • Ability to drive out of landing • Atlas V (541) ellipse • 84 kg of science payload • Direct (uplink) and relayed (downlink) communication • Fast CPU and large data storage 33 Rover Family Portrait ChemCam (Chemistry) Mastcam APXS (Imaging) RAD (Chemistry) MAHLI (Radiation) (Imaging) REMS (Weather) DAN (Subsurface Hydrogen) Drill Scoop Brush Sieves SAM (Chemistry CheMin MARDI and Isotopes) (Mineralogy) (Imaging) Curiosity’s Science Payload 35 What’s Under the Hood? UHF Radio Thermal Fluid Loop Spacecraft Computers Rover Motor Controller ChemMin Power Electronics & Batteries X-Band Radio SAM 36 The Complexity and Beauty of Curiosity 37 Entry, Descent, and Landing (EDL) How Did it Go? 38 39 40 41 Landing area (photo taken by Mars Reconnaissance orbiter) Curiosity’s Descent stage Before After (photo taken by Mars Reconnaissance orbiter) (photos taken by Mars Reconnaissance orbiter) 44 EDL Performance Summary Rover Cruise Stage Separation Separation Sky Crane Detail ERT: 10:14:34 PM All Times in ERT PDT Alt: 21.5 m Velo: 0.77 m/s Note: gnd solution Flyaway change of ~1m near Impact ERT: <10:32:40 PM rover sep CBMD Distance: 640 m Separation Mobility Note: Impact pattern may be different than expected ERT: 10:16:24 PM Entry Interface Deploy ERT: 10:24:33 PM Alt: 21.1 Delivery error: 0.013 deg FPA Parachute Deploy ERT: 10:28:53 PM Peak Heating Mach: 1.72 Touchdown ERT: Pending Deceleration: ~6 g’s ERT: 10:31:49 PM Qmax: Pending Note: Lower than Velo: 0.75 m/s expected parachute Lat/Lon: - Peak Deceleration inflation loads 4.5895°/137.4417° ERT: 10:17:44 PM Deceleration: ~12.2 g’s Hypersonic Backshell Aero-maneuvering Separation Variance from Numb of bank reversals: 3 ERT: 10:30:51 prediction Heatshield Guidance performance: Separation Radar Altitude: 1670 m < 1 s Great ERT: 10:29:13 Ground Solution Velocity: 78.6 m/s Note: Possible tailwind/low Mach: Pending ERT: 10:29:21 Note: density during final 50-100 km Note: Separation Powered Descent 1-2 s FS Infrastructure Alt: 8.3 km of flight rates as expected, Duration: 37 Voltage at TD: 32.1 V Error (alt): 113.4 m no tumbling Fuel usage: 260 kg Comm: Great Error (velo): 0.7 Note: Fuel usage >2 s Prop: Good m/s was lower than Thermal: Good Note: Better range expected Mech: Good at lock-up and AVS/FSW: Good lower error than SECC: N/A expected ISAs: 52822, 52845, 53000 (see following) Sky Crane Flyaway 45 Gale Crater and Mount Sharp 46 24 47 Mt. Sharp 48 49 Curiosity’s Exploration and Science Since Landing 50 51 52 53 54 Looking North to Crater Rim 55 56 Timekeeping on Mars Timekeeping on Mars Martian Day = “Sol” 1 Sol = 24h 39m 35s Timekeeping on Mars Martian Day = “Sol” 1 Sol = 24h 39m 35s “Yestersol” Timekeeping on Mars Martian Day = “Sol” 1 Sol = 24h 39m 35s “Yestersol” “Tosol” Timekeeping on Mars Martian Day = “Sol” 1 Sol = 24h 39m 35s “Yestersol” “Tosol” “Nextersol” “Morrowsol” “Sol-orrow” Timekeeping on Mars Martian Day = “Sol” 1 Sol = 24h 39m 35s “Yestersol” “Tosol” “Nextersol” “Morrowsol” “Sol-orrow” Recent Mars Weather June 63 Ear-Popping Daily Pressure Changes 100 Pa swing is… 15% of Mars Pressure 0.15% of Earth Pressure 64 Driving! 65 Sol 24 Navcam: Bradbury Landing Site 66 Rover tracks (photo taken by Mars Reconnaissance orbiter) Stretching Out the Arm for Contact Science on Rock Named “Jake Matijevic” NASA/JPL- Caltech/MSSS Science Instruments at the End of Curiosity’s Robotic Arm 70 71 72 . --- . --. .-- . --- J . --. P . .-- L Curiosity’s primary scientific goal is to explore and quantitatively assess a local region on Mars’ surface as a potential habitat for life, past or present • Biological potential • Geology and geochemistry • Role of water • Surface radiation NASA/JPL-Caltech Curiosity’s Science Objectives 77 ChemCam Laser 78 Target: Beechey (Sol 19) Power: 1 Gigawatt Shots per spot: 50 8 Before After cm( 3”) NASA/JPL- Caltech/LANL/CNES/IRAP/LPGN/CNRS ChemCam’s laser induced breakdown 79 spectrometer acquires a 5-spot raster 80 81 Remnants of Ancient Streambed on Mars 82 Atmospheric Gas SAM found that argon, Abundances rather than nitrogen is the Measured by SAM second most abundant gas SAM also found that Mars’ atmosphere is enriched in the heavy versions of isotopes, indicating that atmospheric loss has occurred Methane has not been definitively detected NASA/JPL-Caltech/Goddard TLS uses infrared lasers and mirrors to measure the absorption of light by atmospheric gases The SAM Tunable Laser Spectrometer and Mass 83 Spectrometer measure atmospheric composition Scoop and Delivery for Chemistry and Mineralogy 84 85 Sol 61: First Scoop! 86 What did Curiosity discover in the Rocknest Sand Dune? A. A habitable environment conducive to microbial life B. Mars dust and sand dunes are a global phenomenon and aren’t necessarily habitable C. The “Rocknest Monster” 87 Gases SAM and released CheMin during SAM analyses experiments of Rocknest Sand composed of unaltered basaltic NASA/JPL- Caltech/Ames minerals, NASA/JPL- similar to soils Caltech/MSSSNASA/JPL- on Mars Caltech/Goddard Also evidence for water, sulfates, carbonates, and X-ray potentially perchlorates diffraction pattern from 88 CheMin How far across SDSU would Curiosity have travelled in the 9 months thus far? How far across SDSU would Curiosity have travelled in the 9 months thus far? Aztec Center Current Position ✖ Sols 55-100 Sol Sol Sol 120 43 39 MSL Rotary-Percussive Drill in Testbed at JPL Heading into Yellowknife Bay NASA/JPL- Caltech/MSSS 94 NASA/JPL-Caltech/MSSS Postcards from Yellowknife Bay 95 NASA/JPL-Caltech ChemCam Remote Micro- Imager NASA/JPL- Caltech/LANL/CNES/IRAP/ LPGNantes/CNRS/LGLyon/Planet- Terre ChemCam spectra from sol 125 “Crest” and 135 “Rapitan” “Sheepbed” rocks contain 1 to 5-mm fractures filled with calcium sulfate minerals that precipitated from fluids at low to moderate temperatures 96 NASA/JPL-Caltech/MSSS Spherules Suggest Water Percolation 97 NASA/JPL- Caltech/LANL/CNES/IRAP/LPG Nantes/CNRS 101 Drilling at John Klein: A “Goldmine” of Info 102 Drilling at John Klein: A “Goldmine” of Info Wet Neutral pH Energy Gradients (Oxidation) Mildly Salty Key Chemicals (C,H,N,O,P,S) 103 Drilling at John Klein: A “Goldmine” of Info Wet Neutral pH Energy Gradients (Oxidation) Mildly Salty Key Chemicals (C,H,N,O,P,S) Conditions Favorable for Life! 104 105 “Cumberland” – Curiosity’s Second Drill Target What’s Next for Curiosity? 108 Curiosity’s Ultimate Goal: Mount Sharp NASA/JPL-Caltech/Univ. of 109 Arizona 110 NASA/JPL- Caltech/MSSS 111 NASA/JPL- Caltech/MSSS Layers, Canyons, and Buttes of Mount Sharp 112 This boulder is the size of Curiosity Layers, Canyons, and Buttes of Mount Sharp 113 114 Questions? 115 Introducing today’s presenters Thanks to today’s presenter! Jordan Evans NASA’s Jet Propulsion Laboratory Pasadena, CA 116 Thank you to the sponsor of tonight’s web seminar—1 of 6 Thank you to the sponsor of tonight’s web seminar: This web seminar contains information about programs, products, and services offered by third parties, as well as links to third-party websites.
Recommended publications
  • Telling Time on Mars 41
    Telling Time on Mars 41 The InSight Lander will arrive at Mars on September 20, 2016 according to Earth Time, but when will it arrive according to Mars Time? One Earth Day is exactly 24 hours long, so that the time between two High Noons is exactly 24 hours. But Mars rotates a bit more slowly and by Earth units, one Mars Day (called a Sol) is 24 hours and 40 minutes long. This photo was taken by the NASA Phoenix Lander on Sol 90, which is Earth date August 25, 2008 The Curiosity Rover can only safely move during the Martian daytime. This is when scientists on Earth can use TV cameras to watch where the rover is traveling. The Martian day is 40 minutes longer then the Earth day. That means scientists have to move their work schedule forward by 40 minutes each Earth day to keep up with sunrise and sunset on Mars. The rover landed on August 5, 2012 at about 10:30 pm Pacific Daylight Time (PDT), which was defined as Sol 0 for this mission. All of the navigation is performed by Navigation Engineers working at the Jet Propulsion Laboratory in Pasadena, California. Problem 1 - What time and date will it be on Earth on Sol 5? Problem 2 - Suppose that sunrise at the Curiosity lander happened on February 16, 2013 at 5:20 pm Pacific Standard Time (Sol 190 at 6:00 am Local Mars Time). A Navigation Engineer begins his work shift exactly at that moment. When will his shift have to start after 5 Sols have passed on Mars? Problem 3 – How many Sols have to elapse before his work shift once again starts at the same Earth time of 5:20 pm PST? Space Math http://spacemath.gsfc.nasa.gov Answer Key 41 Mars Sunrise and Sunset Tables http://www.curiosityrover.com/sundata/ Problem 1 - What time and date will it be on Earth on Sol 5? Answer: This will be 5 x (1 day and 40 minutes) added to August 5 at 10:30 pm PDT.
    [Show full text]
  • Human Mars Architecture
    National Aeronautics and Space Administration Human Mars Architecture Tara Polsgrove NASA Human Mars Study Team 15th International Planetary Probe Workshop June 11, 2018 Space Policy Directive-1 “Lead an innovative and sustainable program of exploration with commercial and international partners to enable human expansion across the solar system and to bring back to Earth new knowledge and opportunities. Beginning with missions beyond low-Earth orbit, the United States will lead the return of humans to the Moon for long-term exploration and utilization, followed by human missions to Mars and other destinations.” 2 EXPLORATION CAMPAIGN Gateway Initial ConfigurationLunar Orbital Platform-Gateway (Notional) Orion 4 5 A Brief History of Human Exploration Beyond LEO America at DPT / NEXT NASA Case the Threshold Constellation National Studies Program Lunar Review of Commission First Lunar Architecture U.S. Human on Space Outpost Team Spaceflight Plans Committee Pathways to Exploration Columbia Challenger 1980 1990 2000 2010 Bush 41 Bush 43 7kObama HAT/EMC MSC Speech Speech Speech Report of the 90-Day Study on Human Exploration of the Moon and Mars NASA’s Journey to National Aeronautics and November 1989 Global Leadership Space Administration Mars Exploration and 90-Day Study Mars Design Mars Design Roadmap America’s Reference Mars Design Reference Future in Reference Mission 1.0 Exploration Architecture Space Mission 3.0 System 5.0 Exploration Architecture Blueprint Study 6 Exploring the Mars Mission Design Tradespace • A myriad of choices define
    [Show full text]
  • Alternative Ad.Qxd
    P020_NELE_JAN12.qxp:Layout 1 6/1/10 12:27 Page 20 Built to last Well beyond their ‘best by’ dates, Spirit and Opportunity continue to collect data from the surface of Mars. By Graham Pitcher. hen NASA sent the Spirit and put together and flown in Pathfinder. Opportunity Rovers to Mars in There were similar sensing elements, a W2003, the plan was for the camera and in situ investigation vehicles to operate for 90 days; anything equipment. It was just a matter of more would be a bonus. But six years putting it all together on a new platform.” later, the Rovers are still working; even if NASA had wanted to include sample one of them is currently bogged down in storage, but that element dropped from the equivalent of a Martian sand trap. the mission because there wasn’t Bearing in mind that Mars is not the enough funding. friendliest of environments for such Matijevic said the Rovers ‘decide’ devices to work in, what was so special what to look at using input from their about their design? Why are the Rovers remote sensing instruments. “They work still in action? out what looks like an interesting target. Jake Matijevic, chief engineer for the Once in position, local instruments – Mars Rovers with NASA’s Jet Propulsion such as a spectrometer and an alpha Laboratory (JPL), said there is no particle analyser – are deployed and difference between the two vehicles. work together.” “They’re identical in that they were built These operations are controlled by a using the same environmental central computer.
    [Show full text]
  • INFORMATION and SOCIAL REALITY Elliott Ayers Hauser A
    MAKING CERTAIN: INFORMATION AND SOCIAL REALITY Elliott Ayers Hauser A dissertation submitted to the faculty of the University of North Carolina at Chapel Hill in partial fulfillment of the requirements for the degree of Doctor of Philosophy in Information Science in the School of Information and Library Science. Chapel Hill 2019 Approved by: Geoffrey Bowker Melanie Feinberg Stephanie Haas Ryan Shaw Neal Thomas ©2019 Elliott Ayers Hauser ALL RIGHTS RESERVED ii ABSTRACT Elliott Ayers Hauser: Making Certain: Information and Social Reality (Under the direction of Ryan Shaw) This dissertation identifies and explains the phenomenon of the production of certainty in information systems. I define this phenomenon pragmatically as instances where practices of justification end upon information systems or their contents. Cases where information systems seem able to produce social reality without reference to the external world indicate that these systems contain facts for determining truth, rather than propositions rendered true or false by the world outside the system. The No Fly list is offered as a running example that both clearly exemplifies the phenomenon and announces the stakes of my project. After an operationalization of key terms and a review of relevant literature, I articulate a research program aimed at characterizing the phenomenon, its major components, and its effects. Notable contributions of the dissertation include: • the identification of the production of certainty as a unitary, trans-disciplinary phenomenon; • the synthesis of a sociolinguistic method capable of unambiguously identifying a) the presence of this phenomenon and b) distinguishing the respective contributions of systemic and social factors to it; and • the development of a taxonomy of certainty that can distinguish between types of certainty production and/or certainty-producing systems.
    [Show full text]
  • The Rock Abrasion Record at Gale Crater: Mars Science Laboratory
    PUBLICATIONS Journal of Geophysical Research: Planets RESEARCH ARTICLE The rock abrasion record at Gale Crater: Mars 10.1002/2013JE004579 Science Laboratory results from Bradbury Special Section: Landing to Rocknest Results from the first 360 Sols of the Mars Science Laboratory N. T. Bridges1, F. J. Calef2, B. Hallet3, K. E. Herkenhoff4, N. L. Lanza5, S. Le Mouélic6, C. E. Newman7, Mission: Bradbury Landing D. L. Blaney2,M.A.dePablo8,G.A.Kocurek9, Y. Langevin10,K.W.Lewis11, N. Mangold6, through Yellowknife Bay S. Maurice12, P.-Y. Meslin12,P.Pinet12,N.O.Renno13,M.S.Rice14, M. E. Richardson7,V.Sautter15, R. S. Sletten3,R.C.Wiens6, and R. A. Yingst16 Key Points: • Ventifacts in Gale Crater 1Applied Physics Laboratory, Laurel, Maryland, USA, 2Jet Propulsion Laboratory, Pasadena, California, USA, 3Department • Maybeformedbypaleowind of Earth and Space Sciences, College of the Environments, University of Washington, Seattle, Washington, USA, 4U.S. • Can see abrasion textures at range 5 6 of scales Geological Survey, Flagstaff, Arizona, USA, Los Alamos National Laboratory, Los Alamos, New Mexico, USA, LPGNantes, UMR 6112, CNRS/Université de Nantes, Nantes, France, 7Ashima Research, Pasadena, California, USA, 8Universidad de Alcala, Madrid, Spain, 9Department of Geological Sciences, Jackson School of Geosciences, University of Texas at Austin, Supporting Information: Austin, Texas, USA, 10Institute d’Astrophysique Spatiale, Université Paris-Sud, Orsay, France, 11Department of • Figure S1 12 fi • Figure S2 Geosciences, Princeton University, Princeton, New Jersey, USA, Centre National de la Recherche Scienti que, Institut 13 • Table S1 de Recherche en Astrophysique et Planétologie, CNRS-Université Toulouse, Toulouse, France, Department of Atmospheric, Oceanic, and Space Science; College of Engineering, University of Michigan, Ann Arbor, Michigan, USA, Correspondence to: 14Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, California, USA, 15Lab N.
    [Show full text]
  • The Water Traces on the Martian Moons and Structural Lineaments
    Flow folds of viscous ice-rock mixture in Phobos and Deimos(Martian moons) Pedram Aftabi * Introduction: Mars has two very small satellites called soil change to dry soils after few Phobos and Deimos( Hall 1887 reviewed in[7]) with minutes(subscribed).Therefore the ice rock mixture 22.2 and 12.6 km across respectively[15]which decreased in the volume and contracted in two type of surfaced by deposits[5]as a thick regolith or dust and the external shape as ellipsoid and the spherical(Fig4). with a significant interior ice or ice and rock mixture[8,4&6]. The small rocky moons of Mars, Deimos and Phobos, are irregular in shape and comparable in size to the asteroid Gaspra (Fig1[7]). Fig4-Shrinkage of the moon by evaporation of the ice matrix. Fig1-Martian moons Phobos,Deimos and the asteroid Gaspra(see b)spherical shrinkage c)ellipsoid shrinkage d)shrinkage folds in www.NASA.Gov). section2 of b e)shrinkage folds in the section3 of c compare to All Martian moons have irregular shapes(to ellipsoid), the primary phobos. F)The folds from top to the bottom in the upper most part of phobos. testament to their violent histories(Figs2&4). Their surfaces are distinctly different, most likely because of The PDMS 36[10] suggested for modeling viscous materials very different impact histories(Fig3 from like salt or ice [9, 1, 2&3]. Sand and PDMS mixture is good www.NASA.Gov).but the lines in this fig seen both in material for the simulations of the Ice and basalt articles in the phobos and Deimos[12,13]but presented sharp on the Martian moons[15].
    [Show full text]
  • Imagining Outer Space Also by Alexander C
    Imagining Outer Space Also by Alexander C. T. Geppert FLEETING CITIES Imperial Expositions in Fin-de-Siècle Europe Co-Edited EUROPEAN EGO-HISTORIES Historiography and the Self, 1970–2000 ORTE DES OKKULTEN ESPOSIZIONI IN EUROPA TRA OTTO E NOVECENTO Spazi, organizzazione, rappresentazioni ORTSGESPRÄCHE Raum und Kommunikation im 19. und 20. Jahrhundert NEW DANGEROUS LIAISONS Discourses on Europe and Love in the Twentieth Century WUNDER Poetik und Politik des Staunens im 20. Jahrhundert Imagining Outer Space European Astroculture in the Twentieth Century Edited by Alexander C. T. Geppert Emmy Noether Research Group Director Freie Universität Berlin Editorial matter, selection and introduction © Alexander C. T. Geppert 2012 Chapter 6 (by Michael J. Neufeld) © the Smithsonian Institution 2012 All remaining chapters © their respective authors 2012 All rights reserved. No reproduction, copy or transmission of this publication may be made without written permission. No portion of this publication may be reproduced, copied or transmitted save with written permission or in accordance with the provisions of the Copyright, Designs and Patents Act 1988, or under the terms of any licence permitting limited copying issued by the Copyright Licensing Agency, Saffron House, 6–10 Kirby Street, London EC1N 8TS. Any person who does any unauthorized act in relation to this publication may be liable to criminal prosecution and civil claims for damages. The authors have asserted their rights to be identified as the authors of this work in accordance with the Copyright, Designs and Patents Act 1988. First published 2012 by PALGRAVE MACMILLAN Palgrave Macmillan in the UK is an imprint of Macmillan Publishers Limited, registered in England, company number 785998, of Houndmills, Basingstoke, Hampshire RG21 6XS.
    [Show full text]
  • Radar Imager for Mars' Subsurface Experiment—RIMFAX
    Space Sci Rev (2020) 216:128 https://doi.org/10.1007/s11214-020-00740-4 Radar Imager for Mars’ Subsurface Experiment—RIMFAX Svein-Erik Hamran1 · David A. Paige2 · Hans E.F. Amundsen3 · Tor Berger 4 · Sverre Brovoll4 · Lynn Carter5 · Leif Damsgård4 · Henning Dypvik1 · Jo Eide6 · Sigurd Eide1 · Rebecca Ghent7 · Øystein Helleren4 · Jack Kohler8 · Mike Mellon9 · Daniel C. Nunes10 · Dirk Plettemeier11 · Kathryn Rowe2 · Patrick Russell2 · Mats Jørgen Øyan4 Received: 15 May 2020 / Accepted: 25 September 2020 © The Author(s) 2020 Abstract The Radar Imager for Mars’ Subsurface Experiment (RIMFAX) is a Ground Pen- etrating Radar on the Mars 2020 mission’s Perseverance rover, which is planned to land near a deltaic landform in Jezero crater. RIMFAX will add a new dimension to rover investiga- tions of Mars by providing the capability to image the shallow subsurface beneath the rover. The principal goals of the RIMFAX investigation are to image subsurface structure, and to provide information regarding subsurface composition. Data provided by RIMFAX will aid Perseverance’s mission to explore the ancient habitability of its field area and to select a set of promising geologic samples for analysis, caching, and eventual return to Earth. RIM- FAX is a Frequency Modulated Continuous Wave (FMCW) radar, which transmits a signal swept through a range of frequencies, rather than a single wide-band pulse. The operating frequency range of 150–1200 MHz covers the typical frequencies of GPR used in geology. In general, the full bandwidth (with effective center frequency of 675 MHz) will be used for The Mars 2020 Mission Edited by Kenneth A.
    [Show full text]
  • AST101 Lecture 17 Barsoom
    AST101 Lecture 17 Barsoom There are 4 Terrestrial Planets • Mercury • Venus • Earth • Mars Mercury From the Messenger Orbiter, March 2011. Rayed crater: Debussy Venus From the Venus Express, 2007. H2SO4 clouds Earth (Terra) Apollo 17 Mars Hubble Space Telescope Barsoom A world like our own? Populated by aliens? Telescopic Observations Mars is dynamic • Polar caps wax and wane • Surface features change shape regularly • Clouds obscure the surface Giovanni Schiaparelli Published a map of Mars in 1877 Identified surface features he called “canali” Schiaparelli’s Mars Percival Lowell Mistranslated “canali” (channels) as canals Established Lowell Observatory on Mars Hill, Flagstaff AZ Lowell’s map of Mars (excerpt) Lowell’s Mars Canals imply • intelligent life, and • deliberate construction Lowell created a Mars that is • a dying planet, • whose intelligent denizens built canals – to collect the melting polar ice, and – to distribute the water among the oases Camille Flammarion (1884) Chesley Bonestell: Surface of Mars © Bonestell Space Art No one would have believed in the last years of the nineteenth century that this world was being watched keenly and closely by intelligences greater than man's and yet as mortal as his own; that as men busied themselves about their various concerns they were scrutinised and studied, perhaps almost as narrowly as a man with a microscope might scrutinise the transient creatures that swarm and multiply in a drop of water. H. G. WELLS THE WAR OF THE WORLDS Illusions of Mars. I. This mythos arose from two optical illusions. 1. The human brain tends to connect the dots, which results in apparent linear features.
    [Show full text]
  • THE PETROCHEMISTRY of JAKE M: a MARTIAN MUGEARITE. Stolper
    44th Lunar and Planetary Science Conference (2013) 1685.pdf THE PETROCHEMISTRY OF JAKE_M: A MARTIAN MUGEARITE. Stolper, E.M.1, Baker, M.B.1, Fisk, M.2, Gellert, R.3, King, P.L.4, McLennan, S.M.5, Minitti, M.6, Newcombe, M.1, Schmidt, M.E. 7, Treiman, A.H.8, and the MSL Science Team. 1Caltech, Pasadena, CA 91125, 2Oregon State Univ., 3Univ. Guelph, 4Res. School Earth Sci., ANU, 5SUNY, Stony Brook, 6Applied Phys. Lab., Johns Hopkins Univ., 7Brock Univ., 8Lunar & Planet. Inst. Introduction: Rock “Jake_M” (JM; named for JPL The surface of JM was not brushed or abraded prior engineer Jake Matijevic) was the first sample analyzed to analysis, so the APXS analyses probably include by the Alpha Particle X-ray Spectrometer (APXS) in- contributions from surface coatings, including adhering strument on MSL [1]. Although it is an isolated frag- dust, and these are the probable source of the S and Cl ment lacking field context, its dark color and apparently in JM. Experience with MER, however, indicates that fine-grained texture suggested it was a relatively homo- the characteristics of rock compositions are typically geneous igneous rock and thus an appropriate sample to not obscured by surface components, and the levels of S initiate the APXS analytical program. We report here and Cl in JM are lower than virtually all unbrushed the preliminary APXS analyses of JM and a plausible analyses from the Spirit rover and lower than many of interpretation of their significance for petrogenesis. the brushed analyses, so the level of surface contamina- Results: Three spots on JM were analyzed with the tion and alteration are likely relatively minor [5].
    [Show full text]
  • Mars Pathfinder
    NASA Facts National Aeronautics and Space Administration Jet Propulsion Laboratory California Institute of Technology Pasadena, CA 91109 Mars Pathfinder Mars Pathfinder was the first completed mission events, ending in a touchdown which left all systems in NASAs Discovery Program of low-cost, rapidly intact. developed planetary missions with highly focused sci- The landing site, an ancient flood plain in Mars ence goals. With a development time of only three northern hemisphere known as Ares Vallis, is among years and a total cost of $265 million, Pathfinder was the rockiest parts of Mars. It was chosen because sci- originally designed entists believed it to as a technology be a relatively safe demonstration of a surface to land on way to deliver an and one which con- instrumented lander tained a wide vari- and a free-ranging ety of rocks robotic rover to the deposited during a surface of the red catastrophic flood. planet. Pathfinder In the event early in not only accom- Mars history, sci- plished this goal but entists believe that also returned an the flood plain was unprecedented cut by a volume of amount of data and water the size of outlived its primary North Americas design life. Great Lakes in Pathfinder used about two weeks. an innovative The lander, for- method of directly mally named the entering the Carl Sagan Martian atmos- Memorial Station phere, assisted by a following its suc- parachute to slow cessful touchdown, its descent through and the rover, the thin Martian atmosphere and a giant system of named Sojourner after American civil rights crusader airbags to cushion the impact.
    [Show full text]
  • Mars Rover Opportunity Working at 'Matijevic Hill' Site 30 September 2012
    Mars rover Opportunity working at 'Matijevic Hill' site 30 September 2012 reminiscent of, but different from, the iron-rich spheres nicknamed "blueberries" at the rover's landing site nearly 22 driving miles ago (35 kilometers). The small spheres at Matijevic Hill have different composition and internal structure. Opportunity's science team is evaluating a range of possibilities for how they formed. The spheres are up to about an eighth of an inch (3 millimeters) in diameter. The "blueberries" found earlier are concretions formed by the action of mineral-laden water inside rocks, but that is only one of the ways nature can make small, rounded particles. One working hypothesis, out of several, is that the new-found spherules are also concretions but with a different Rock fins up to about 1 foot (30 centimeters) tall composition. Others include that they may be dominate this scene from the panoramic camera accretionary lapilli formed in volcanic ash eruptions, (Pancam) on NASA's Mars Exploration Rover Opportunity. The component images were taken during impact spherules formed in impact events, or the 3,058th Martian day, or sol, of Opportunity's work on devitrification spherules resulting from formation of Mars (Aug. 23, 2012). The view spans an area of terrain crystals from formerly melted material. There are about 30 feet (9 meters) wide. Orbital investigation of the other possibilities, too. area has identified a possibility of clay minerals in this area of the Cape York segment of the western rim of "Right now we have multiple working hypotheses, Endeavour Crater. The view combines exposures taken and each hypothesis makes certain predictions through Pancam filters centered on wavelengths of 753 about things like what the spherules are made of nanometers (near infrared), 535 nanometers (green) and and how they are distributed," said Opportunity's 432 nanometers (violet).
    [Show full text]