Mercury Lander Mission Concept Study
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The Cassini Robot
THE CASSINI–HUYGENS MISSION LESSON The Cassini Robot 5 Students begin by examining their prior 3–4 hrs notions of robots and then consider the characteristics and capabilities of a robot like the Cassini–Huygens spacecraft that would be sent into space to explore another planet. Students compare robotic functions to human body functions. The lesson MEETS NATIONAL SCIENCE EDUCATION prepares students to design, build, diagram, STANDARDS: and explain their own models of robots for Unifying Concepts and Processes space exploration in the Saturn system. A computer-generated rendering of Cassini–Huygens. • Form and function PREREQUISITE SKILLS BACKGROUND INFORMATION Science and Drawing and labeling diagrams Background for Lesson Discussion, page 122 Technology • Abilities of Assembling a spacecraft model Questions, page 127 technological Some familiarity with the Saturn Answers in Appendix 1, page 225 design system (see Lesson 1) 56–63: The Cassini–Huygens Mission 64–69: The Spacecraft 70–76: The Science Instruments 81–94: Launch and Navigation 95–101: Communications and Science Data EQUIPMENT, MATERIALS, AND TOOLS For the teacher Materials to reproduce Photocopier (for transparencies & copies) Figures 1–6 are provided at the end of Overhead projector this lesson. Chart paper (18" × 22") FIGURE TRANSPARENCY COPIES Markers; clear adhesive tape 1 1 per group 21 For each group of 3 to 4 students 3 1 1 per student Chart paper (18" × 22") 4 1 per group Markers 51 Scissors 6 (for teacher only) Clear adhesive tape or glue Various household objects: egg cartons, yogurt cartons, film canisters, wire, aluminum foil, construction paper 121 Saturn Educator Guide • Cassini Program website — http://www.jpl.nasa.gov/cassini/educatorguide • EG-1998-12-008-JPL Background for Lesson Discussion LESSON craft components and those of human body 5 The definition of a robot parts. -
Ices on Mercury: Chemistry of Volatiles in Permanently Cold Areas of Mercury’S North Polar Region
Icarus 281 (2017) 19–31 Contents lists available at ScienceDirect Icarus journal homepage: www.elsevier.com/locate/icarus Ices on Mercury: Chemistry of volatiles in permanently cold areas of Mercury’s north polar region ∗ M.L. Delitsky a, , D.A. Paige b, M.A. Siegler c, E.R. Harju b,f, D. Schriver b, R.E. Johnson d, P. Travnicek e a California Specialty Engineering, Pasadena, CA b Dept of Earth, Planetary and Space Sciences, University of California, Los Angeles, CA c Planetary Science Institute, Tucson, AZ d Dept of Engineering Physics, University of Virginia, Charlottesville, VA e Space Sciences Laboratory, University of California, Berkeley, CA f Pasadena City College, Pasadena, CA a r t i c l e i n f o a b s t r a c t Article history: Observations by the MESSENGER spacecraft during its flyby and orbital observations of Mercury in 2008– Received 3 January 2016 2015 indicated the presence of cold icy materials hiding in permanently-shadowed craters in Mercury’s Revised 29 July 2016 north polar region. These icy condensed volatiles are thought to be composed of water ice and frozen Accepted 2 August 2016 organics that can persist over long geologic timescales and evolve under the influence of the Mercury Available online 4 August 2016 space environment. Polar ices never see solar photons because at such high latitudes, sunlight cannot Keywords: reach over the crater rims. The craters maintain a permanently cold environment for the ices to persist. Mercury surface ices magnetospheres However, the magnetosphere will supply a beam of ions and electrons that can reach the frozen volatiles radiolysis and induce ice chemistry. -
Tianwen-1: China's Mars Mission
Tianwen-1: China's Mars Mission drishtiias.com/printpdf/tianwen-1-china-s-mars-mission Why In News China will launch its first Mars Mission - Tianwen-1- in July, 2020. China's previous ‘Yinghuo-1’ Mars mission, which was supported by a Russian spacecraft, had failed after it did not leave the earth's orbit and disintegrated over the Pacific Ocean in 2012. The National Aeronautics and Space Administration (NASA) is also going to launch its own Mars mission in July, the Perseverance which aims to collect Martian samples. Key Points The Tianwen-1 Mission: It will lift off on a Long March 5 rocket, from the Wenchang launch centre. It will carry 13 payloads (seven orbiters and six rovers) that will explore the planet. It is an all-in-one orbiter, lander and rover system. Orbiter: It is a spacecraft designed to orbit a celestial body (astronomical body) without landing on its surface. Lander: It is a strong, lightweight spacecraft structure, consisting of a base and three sides "petals" in the shape of a tetrahedron (pyramid- shaped). It is a protective "shell" that houses the rover and protects it, along with the airbags, from the forces of impact. Rover: It is a planetary surface exploration device designed to move across the solid surface on a planet or other planetary mass celestial bodies. 1/3 Objectives: The mission will be the first to place a ground-penetrating radar on the Martian surface, which will be able to study local geology, as well as rock, ice, and dirt distribution. It will search the martian surface for water, investigate soil characteristics, and study the atmosphere. -
Paul Sykes Lecture – Sat, Jan 27 @ 7:30Pm Ice on Mercury, Featuring Dr
NOVANEWSLETTEROFTHEVANCOUVERCENTRERASC VOLUME2018ISSUE1JANUARYFEBRUARY2018 Paul Sykes Lecture – Sat, Jan 27 @ 7:30pm Ice on Mercury, Featuring Dr. Nancy Chabot of Johns Hopkins University SFU Burnaby Campus, Room SWH 10081 Even though Mercury is the Dr. Nancy L. Chabot is a and Case Western Reserve Uni- planet closest to the Sun, there planetary scientist at the Johns versity. She has been a mem- are places at its poles that never Hopkins Applied Physics Labo- ber of five field teams with the receive sunlight and are very ratory (apl). She received an Antarctic Search for Meteorites cold—cold enough to hold wa- (ansmet) program and served ter ice! In this presentation, Dr. as the Instrument Scientist for Chabot will show the multiple the Mercury Dual Imaging Sys- lines of evidence that regions tem (mdis) on the messenger near Mercury’s poles hold water mission. Her research interests ice—from the first discovery involve understanding the evo- by Earth-based radar observa- lution of rocky planetary bod- tions to multiple data sets from ies in the Solar System, and at nasa’s messenger spacecraft, apl she oversees an experimen- the first spacecraft ever to or- tal geochemistry laboratory bit the planet Mercury. These that is used to conduct experi- combined results suggest that ments related to this topic. Dr. Mercury’s polar ice deposits Chabot has served as an Associ- are substantial, perhaps compa- ate Editor for the journal Mete- rable to the amount of water in oritics and Planetary Science, Lake Ontario! Where did the chair of nasa’s Small Bodies ice come from and how did it undergraduate degree in physics Assessment Group, a member get there? Dr. -
Bepicolombo - a Mission to Mercury
BEPICOLOMBO - A MISSION TO MERCURY ∗ R. Jehn , J. Schoenmaekers, D. Garc´ıa and P. Ferri European Space Operations Centre, ESA/ESOC, Darmstadt, Germany ABSTRACT BepiColombo is a cornerstone mission of the ESA Science Programme, to be launched towards Mercury in July 2014. After a journey of nearly 6 years two probes, the Magneto- spheric Orbiter (JAXA) and the Planetary Orbiter (ESA) will be separated and injected into their target orbits. The interplanetary trajectory includes flybys at the Earth, Venus (twice) and Mercury (four times), as well as several thrust arcs provided by the solar electric propulsion module. At the end of the transfer a gravitational capture at the weak stability boundary is performed exploiting the Sun gravity. In case of a failure of the orbit insertion burn, the spacecraft will stay for a few revolutions in the weakly captured orbit. The arrival conditions are chosen such that backup orbit insertion manoeuvres can be performed one, four or five orbits later with trajectory correction manoeuvres of less than 15 m/s to compensate the Sun perturbations. Only in case that no manoeuvre can be performed within 64 days (5 orbits) after the nominal orbit insertion the spacecraft will leave Mercury and the mission will be lost. The baseline trajectory has been designed taking into account all operational constraints: 90-day commissioning phase without any thrust; 30-day coast arcs before each flyby (to allow for precise navigation); 7-day coast arcs after each flyby; 60-day coast arc before orbit insertion; Solar aspect angle constraints and minimum flyby altitudes (300 km at Earth and Venus, 200 km at Mercury). -
SPHERES Interact - Human-Machine Interaction Aboard the International Space Station
SPHERES Interact - Human-Machine Interaction aboard the International Space Station Enrico Stoll Steffen Jaekel Jacob Katz Alvar Saenz-Otero Space Systems Laboratory Massachusetts Institute of Technology 77 Massachusetts Avenue, Cambridge Massachusetts, 02139-4307, USA [email protected] [email protected] [email protected] [email protected] Renuganth Varatharajoo Department of Aerospace Engineering University Putra Malaysia 43400 Selangor, Malaysia [email protected] Abstract The deployment of space robots for servicing and maintenance operations, which are tele- operated from ground, is a valuable addition to existing autonomous systems since it will provide flexibility and robustness in mission operations. In this connection, not only robotic manipulators are of great use but also free-flying inspector satellites supporting the oper- ations through additional feedback to the ground operator. The manual control of such an inspector satellite at a remote location is challenging since the navigation in three- dimensional space is unfamiliar and large time delays can occur in the communication chan- nel. This paper shows a series of robotic experiments, in which satellites are controlled by astronauts aboard the International Space Station (ISS). The Synchronized Position Hold Engage Reorient Experimental Satellites (SPHERES) were utilized to study several aspects of a remotely controlled inspector satellite. The focus in this case study is to investigate different approaches to human-spacecraft interaction with varying levels of autonomy under zero-gravity conditions. 1 Introduction Human-machine interaction is a wide spread research topic on Earth since there are many terrestrial applica- tions, such as industrial assembly or rescue robots. Analogously, there are a number of possible applications in space such as maintenance, inspection and assembly amongst others. -
ESA & ESOC Overview
NASA PM Challenge 2010 Developing the International Program/Project Management Community 9/10 February 2010 Dr. Bettina Böhm Program & Project Manager Career at ESA | Bettina Böhm | ESA/HQ | 23/11/09 | Page 1 Used with Permission PURPOSE OF ESA / ACTIVITIES “To provide for and promote, for exclusively Space science peaceful purposes, cooperation among Human spaceflight European states in space research and Exploration technology and their space applications.” Earth observation Launchers [Article 2 of ESA Convention] Navigation ESA is one of the few space agencies Telecommunications in the world to combine responsibility Technology in all areas of space activity. Operations Program & Project Manager Career at ESA | Bettina Böhm | ESA/HQ | 23/11/09 | Page 2 ESA FACTS AND FIGURES Over 30 years of experience 18 Member States 2080 staff, thereof 880 in Program Directorates, 790 in Operations and Technical Support and 410 in other Support Directorates 3 500 million Euros budget Over 60 satellites designed and tested Over 60 satellites operated in-flight and 8 missions rescued 16 scientific satellites in operation Five types of launcher developed More than 180 launches made Program & Project Manager Career at ESA | Bettina Böhm | ESA/HQ | 23/11/09 | Page 3 ESA Locations EAC (Cologne) Salmijaervi ESTEC Astronaut training (Noordwijk) Satellite technology development and testing Harwell ESOC ESA HQ (Darmstadt) (Paris) Brussels Satellite operations and ground system technology development ESAC (Villanueva de la Cañada Oberpfaffenhofen -
Echo Exoplanet Characterisation Observatory
Exp Astron (2012) 34:311–353 DOI 10.1007/s10686-012-9303-4 ORIGINAL ARTICLE EChO Exoplanet characterisation observatory G. Tinetti · J. P. Beaulieu · T. Henning · M. Meyer · G. Micela · I. Ribas · D. Stam · M. Swain · O. Krause · M. Ollivier · E. Pace · B. Swinyard · A. Aylward · R. van Boekel · A. Coradini · T. Encrenaz · I. Snellen · M. R. Zapatero-Osorio · J. Bouwman · J. Y-K. Cho · V. Coudé du Foresto · T. Guillot · M. Lopez-Morales · I. Mueller-Wodarg · E. Palle · F. Selsis · A. Sozzetti · P. A. R. Ade · N. Achilleos · A. Adriani · C. B. Agnor · C. Afonso · C. Allende Prieto · G. Bakos · R. J. Barber · M. Barlow · V. Batista · P. Bernath · B. Bézard · P. Bordé · L. R. Brown · A. Cassan · C. Cavarroc · A. Ciaravella · C. Cockell · A. Coustenis · C. Danielski · L. Decin · R. De Kok · O. Demangeon · P. Deroo · P. Doel · P. Drossart · L. N. Fletcher · M. Focardi · F. Forget · S. Fossey · P. Fouqué · J. Frith · M. Galand · P. Gaulme · J. I. González Hernández · O. Grasset · D. Grassi · J. L. Grenfell · M. J. Griffin · C. A. Griffith · U. Grözinger · M. Guedel · P. Guio · O. Hainaut · R. Hargreaves · P. H. Hauschildt · K. Heng · D. Heyrovsky · R. Hueso · P. Irwin · L. Kaltenegger · P. Kervella · D. Kipping · T. T. Koskinen · G. Kovács · A. La Barbera · H. Lammer · E. Lellouch · G. Leto · M. A. Lopez Valverde · M. Lopez-Puertas · C. Lovis · A. Maggio · J. P. Maillard · J. Maldonado Prado · J. B. Marquette · F. J. Martin-Torres · P. Maxted · S. Miller · S. Molinari · D. Montes · A. Moro-Martin · J. I. Moses · O. Mousis · N. Nguyen Tuong · R. -
16. Ice in the Martian Regolith
16. ICE IN THE MARTIAN REGOLITH S. W. SQUYRES Cornell University S. M. CLIFFORD Lunar and Planetary Institute R. O. KUZMIN V.I. Vernadsky Institute J. R. ZIMBELMAN Smithsonian Institution and F. M. COSTARD Laboratoire de Geographie Physique Geologic evidence indicates that the Martian surface has been substantially modified by the action of liquid water, and that much of that water still resides beneath the surface as ground ice. The pore volume of the Martian regolith is substantial, and a large amount of this volume can be expected to be at tem- peratures cold enough for ice to be present. Calculations of the thermodynamic stability of ground ice on Mars suggest that it can exist very close to the surface at high latitudes, but can persist only at substantial depths near the equator. Impact craters with distinctive lobale ejecta deposits are common on Mars. These rampart craters apparently owe their morphology to fluidhation of sub- surface materials, perhaps by the melting of ground ice, during impact events. If this interpretation is correct, then the size frequency distribution of rampart 523 524 S. W. SQUYRES ET AL. craters is broadly consistent with the depth distribution of ice inferred from stability calculations. A variety of observed Martian landforms can be attrib- uted to creep of the Martian regolith abetted by deformation of ground ice. Global mapping of creep features also supports the idea that ice is present in near-surface materials at latitudes higher than ± 30°, and suggests that ice is largely absent from such materials at lower latitudes. Other morphologic fea- tures on Mars that may result from the present or former existence of ground ice include chaotic terrain, thermokarst and patterned ground. -
Tax List 1890
1890 Chester County Tax Index Last Name First Name Middle Name Suffix/Prefix Category Township/Borough Book Page Cabbot CharlesInmate/Freeman Phoenixville Borough 707 Cabbot MichaelInmate/Freeman Phoenixville Borough 707 Cable HoraceInmate/Freeman Phoenixville Borough 575 Cable L. W.Inmate/Freeman Phoenixville Borough 653 Cable LloydInmate/Freeman Phoenixville Borough 576 Cable MordecaiOccupier Phoenixville Borough 544 Cachell WilliamOccupier Honey Brook H‐O54 Cadwallader CharlesInmate/Freeman Coatesville Borough 118 Caffey John Inmate/Freeman Willistown P‐W972 Caffrey John S.Inmate/Freeman Schuylkill P‐W319 Caffrey M. A.Miss Occupier Spring City Borough 774 Caffrey PeterOccupier Schuylkill P‐W275 Caffrey Peter J.Inmate/Freeman Schuylkill P‐W319 Cahill DennisOccupier West Whiteland P‐W875 Cahill MichaelOccupier West Goshen B‐G850 Cahill PatrickOccupier Schuylkill P‐W276 Cahill RichardInmate/Freeman West Whiteland P‐W909 Cain Cary Inmate/Freeman Pocopson P‐W181 Cain Eli Inmate/Freeman Tredyffrin P‐W420 Chester County Archives and Record Services, West Chester, PA 19380 Last Name First Name Middle Name Suffix/Prefix Category Township/Borough Book Page Cain F. MadisonOccupier West Fallowfield B‐G715 Cain G. E.Occupier Downingtown Borough 197 Cain HenryInmate/Freeman West Whiteland P‐W909 Cain JeremiahEstate Occupier West Chester West Chester 27 Cain John Inmate/Freeman East Whiteland P‐W859 Cain John Inmate/Freeman Easttown B‐G601 Cain JosephInmate/Freeman Londonderry H‐O251 Cain MariaEstate Occupier West Chester West Chester 27 Cain Mary -
Volume 24, Number 04 (April 1906) Winton J
Gardner-Webb University Digital Commons @ Gardner-Webb University The tudeE Magazine: 1883-1957 John R. Dover Memorial Library 4-1-1906 Volume 24, Number 04 (April 1906) Winton J. Baltzell Follow this and additional works at: https://digitalcommons.gardner-webb.edu/etude Part of the Composition Commons, Ethnomusicology Commons, Fine Arts Commons, History Commons, Liturgy and Worship Commons, Music Education Commons, Musicology Commons, Music Pedagogy Commons, Music Performance Commons, Music Practice Commons, and the Music Theory Commons Recommended Citation Baltzell, Winton J.. "Volume 24, Number 04 (April 1906)." , (1906). https://digitalcommons.gardner-webb.edu/etude/513 This Book is brought to you for free and open access by the John R. Dover Memorial Library at Digital Commons @ Gardner-Webb University. It has been accepted for inclusion in The tudeE Magazine: 1883-1957 by an authorized administrator of Digital Commons @ Gardner-Webb University. For more information, please contact [email protected]. APRIL, 1906 ISO PER YEAR ‘TF'TnTT^ PRICE 15 CENTS 180.5 THE ETUDE 209 MODERN SIX-HAND^ LU1T 1 I1 3 Instruction Books PIANO MUSIC “THE ETUDE” - April, 1906 Some Recent Publications Musical Life in New Orleans.. .Alice Graham 217 FOR. THE PIANOFORTE OF «OHE following ensemb Humor in Music. F.S.Law 218 IT styles, and are usi caching purposes t The American Composer. C. von Sternberg 219 CLAYTON F. SUMMY CO. _la- 1 „ net rtf th ’ standard foreign co Experiences of a Music Student in Germany in The following works for beginners at the piano are id some of the lat 1905...... Clarence V. Rawson 220 220 Wabash Avenue, Chicago. -
Surface Residence Times of Regolith on the Lunar Maria
52nd Lunar and Planetary Science Conference 2021 (LPI Contrib. No. 2548) 1652.pdf 1 1 SURFACE RESIDENCE TIMES OF REGOLITH ON THE LUNAR MARIA. P. O’Brien and S. Byrne , 1 L unar and Planetary Laboratory, University of Arizona, Tucson, AZ 85721 ([email protected]) Introduction: The surfaces of airless bodies like Our model simulates mare-like surfaces evolving the Moon undergo microscopic chemical changes as a over time from flat surfaces to cratered landscapes. result of energetic processes operating in the space Impacts are randomly sampled from the present-day environment, collectively known as space weathering lunar impact flux [5] and the global population of [1,2]. Despite returned lunar soil samples, the rate of secondary craters produced by these impacts is space weathering on the Moon is not well understood. generated following empirical observations of The amount of chemical weathering incurred in the secondary production on airless bodies [6,7]. At each lunar regolith depends critically on the rate at which timestep, we compute the downslope flux of regolith regolith is excavated, transported, and buried by by solving the 2D diffusion equation [8]. The rate of macroscopic impact processes. These physical diffusion is calibrated by matching the average processes control how long regolith spends on the roughness of the model landscapes to the observed surface where it is exposed to the space environment. roughness of the lunar maria, as measured by the We have developed a Monte Carlo model that median bidirectional slope at 4 m baselines [9]. Figure simulates the evolution of lunar maria landscapes 1 shows how model surfaces subject to these physical under topographic relief-creation from impact cratering processes become rougher and more heavily-cratered and relief-reduction from micrometeorite gardening over time.