Esa Standard Document

Total Page:16

File Type:pdf, Size:1020Kb

Esa Standard Document Technology Reference Study Final Report GRL The Gamma Ray Lens SCI-A/2005.058/GRL/CB Craig Brown July 2005 s Page 1 of 172 T ECHNOLOGY R EFERENCE S TUDIES The Science Payload and Advanced Concepts Office (SCI-A) at the European Space Agency (ESA) conducts Technology Reference Studies (TRSs), hypothetical science driven missions that are not currently part of the ESA science programme. Most science missions are in many ways very challenging from a technology point of view. It is critical that these technologies are identified as early as possible in order to ensure their development in a timely manner, as well as allowing the feasibility of a mission to be determined. Technology reference studies are used as a means to identify such technology developments. The Technology Reference Study begins by establishing a series of preliminary scientific requirements. From these requirements, a hypothetical mission is designed that is capable of achieving the scientific goals. Critical issues and mission drivers are identified from the new mission concept and, from these drivers, a series of technology development activities are recommended. One such TRS has been conducted on a Gamma Ray Lens (GRL) mission. The GRL is an ideal candidate for a TRS due to the challenging nature of the technologies involved with focusing gamma rays. Identifying the key areas requiring technology development in this field prepares for any future high-energy astrophysics mission that the science community may propose, as well as establishes common technology development requirements possibly shared by different science missions. s page 2 of 172 A BSTRACT This is the final report for the Gamma Ray Lens (GRL) technology reference study performed by SCI-AM. The Gamma Ray Lens concept arrises in response to the desire for high-energy observations of increased sensitivity in the soft gamma-ray regime. Part one of this report is concerned with the theoretical aspects of the gamma ray lens. In particular, this section establishes a reference science case and science requirements for the GRL, as well as outlines the theory of multilayer mirrors and Laue crystals – the two technologies considered for gamma ray focusing in this report. Focal plane instrumentation is also investigated, with possible GRL detectors introduced and discussed. Finally, a sensitivity analysis model is introduced, used in part two as a tool to investgate potential GRL Laue lens configurations. Part two contains the detail relating to the GRL mission design. This section outlines two Gamma Ray Lens profiles that were investigated for the TRS; a smaller Soyuz Fregat spacecraft and a larger Ariane 5 scenario. Effective area profiles and sensitivity analyses were conducted for both configurations, technology drivers were derived, and conclusions were made based on the science requirements outlined in part one. It was found that the smaller Soyuz Fregat configuration, although achieveing two orders of magnitude improvement on the sensitivity of SPI-INTEGRAL, was not capable of achieving all of the science requirements set out in part one. The Soyuz configuration failed to observe all energy bands of interest due to the mass constraints of the launcher. The complexity of two separate launches for the GRL optic and detector spacecraft, also make the smaller configuration undesirable. The Ariane 5 configuration achieved all of the science requirements introduced in part one. A third Extended Ariane 5 lens configuration also demonstrated further potential by greatly increasing the energy band of the instrument. For this reason, the Ariane 5 configuration was chosen as the GRL mission baseline. From the conclusions of the mission design, a series of future actions and potential technology development activities (TDA) were identified. 2 s page 3 of 172 T ABLE O F C ONTENTS 1. Introduction 9 Part I – Theoretical Aspects of the Gamma Ray Lens Mission 2. A Reference Science Case for the Gamma Ray Lens 11 2.1 Sources of interest in the Soft Gamma Ray regime 11 2.2 Preliminary Science Requirements Applicable to the GRL 16 2.3 The INTEGRAL Mission 18 2.4 References 25 3. High Energy Focusing Technologies 27 3.1 Graded Multilayer Mirrors 27 3.1.1 Hard X-ray and Soft Gamma Ray Astronomy 27 3.1.2 Principles of Multilayer Mirrors 28 3.1.3 Optic Design 32 3.1.4 Conclusions 36 3.1.5 References 37 3.2 Laue Crystals 38 3.2.1 Laue Diffraction 38 3.2.2 Direction of Diffraction 38 3.2.3 Throughput of the Diffracted Ray 39 3 s page 4 of 172 3.2.4 Mosaicity 40 3.2.5 Temperature Effects 42 3.2.6 Gradient Crystals 43 3.3 The Basic Laue Lens Principle 44 3.3.1 The Focal Spot 45 3.3.2 Effective Area of the Gamma Ray Lens 46 3.3.3 Lens Size and Deployable Optics 48 3.3.4 References 49 4. Focal Plane Instrumentation and Technologies 50 4.1 Gamma Ray Interaction with Matter 50 4.1.1 Photoelectric Absorption 50 4.1.2 Compton Scattering 51 4.1.3 Pair Production 52 4.2 High Energy Photon Detectors 53 4.2.1 Germanium Detectors 53 4.2.2 Scintillator Detectors 54 4.2.3 Compton Detectors 57 4.2.4 Polarisation Detectors 59 4.3 The Miniature 50-80 K Pulse Tube Cooler 60 4.4 References 61 4 s page 5 of 172 5. Sensitivity Analysis 62 5.1 Input to the Model 62 5.2 Model Description 63 5.3 Model Output 65 5.4 Results 66 5.5 References 66 Part II – Gamma Ray Lens Mission Design 6. Other Missions Useful to the GRL Design 68 6.1 Claire and MAX 68 6.1.1 Claire 68 6.1.2 MAX 72 6.1.3 Conclusions 76 6.1.4 References 77 6.2 XEUS 78 6.2.1 The XEUS Mission 78 6.2.2 Gamma Ray Lens: XEUS Similarities 82 6.2.3 Conclusions 83 6.2.4 References 83 5 s page 6 of 172 7. Orbit Selection 84 7.1 Orbit Type and Trade-off 84 7.2 L2 Orbit Type 86 7.2.1 Lissajous Orbits 86 7.2.2 Halo Orbits 87 7.3 Orbit Selection Conclusions 89 7.4 References 90 8. Mission Profile 1 – Soyuz Fregat 91 8.1 Orbit Insertion 91 8.1.1 Direct Insertion 91 8.1.2 L2 Insertion via Highly Elliptical Transfer Orbit 91 8.1.3 Launch Windows 92 8.1.4 Launch Profile Conclusions 93 8.2 Optics Spacecraft (OSC) 94 8.2.1 Payload 94 8.2.2 Subsystems 94 8.2.3 System Budgets 97 8.3 Detector Spacecraft (DSC) 99 8.3.1 Payload 99 8.3.2 Subsystems 100 8.3.3 System Budgets 101 6 s page 7 of 172 8.4 Mission Configuration 102 8.4.1 Effective Area 103 8.4.2 Sensitivity Analysis 104 8.5 Soyuz Fregat Mission Profile Conclusions 105 8.6 References 106 9. Mission Profile 2 – Ariane 5 107 9.1 Single Launch Mission Analysis 107 9.1.1 Direct Launch 107 9.1.2 HEO Launch 107 9.1.3 Launch Profile Conclusions 108 9.2 GRL Optics Spacecraft (OSC) 109 9.2.1 OSC Configuration 109 9.2.2 Payload 112 9.2.3 Subsystems 115 9.2.4 Mass Budget 117 9.2.5 Power Budget 119 9.3 GRL Detector Spacecraft 120 9.3.1 DSC Configuration 120 9.3.2 Payload 123 9.3.3 Subsystems 125 9.3.4 Mass Budget 125 9.3.5 Power budget 126 7 s page 8 of 172 9.4 GRL Mission Configuration 127 9.4.1 Mission Architecture 127 9.4.2 Link Budget and Ground Segment 131 9.4.3 Laue Lens Effective Area 134 9.4.4 Sensitivity Analysis 135 9.5 Ariane 5 Mission Profile Discussion 136 9.6 Ariane 5 Mission Profile Conclusions 141 9.7 References 141 10. Future Work and Potential Technology Development Activities 142 10.1 Future Activities 142 10.2 Technology Development Activities 144 10.3 References 146 11. Appendices 147 11.1 Appendix A - Soyuz Launchers; Current Status and 147 Proposed Upgrades for use to L2 11.2 Appendix B - Point Spread Function Size – Derivation 152 11.3 Appendix C - Structural Requirements for the Gamma Ray Lens 155 11.4 Appendix D – XEUS Mission and MSC Design 160 11.5 Appendix E – Ariane 5 GRL Systems Mass Budget 163 11.6 Appendix F - Margin Philosophy for Assesment Studies 166 8 s page 9 of 172 1. Introduction The Science Payloads and Advanced Concepts Office has introduced the idea of performing Technology Reference Studies (TRS) in order to recognise and encourage the development of new technology concepts for possible future scientific missions. There are four primary areas of investigation in the TRS programme; Planetary, Solar, Astrophysics and Fundamental physics missions. As part of the Astrophysics missions theme, it has been decided to include the preliminary study of a gamma ray focuser. This study will aim to establish the advances in instrumentation required to make such a mission viable in the future. The progression of gamma ray astronomy relies on the development of higher sensitivity instrumentation. Current technologies utilised in the field operate in the background-limited regime and have thus reached a critical point in their development. Any further increase in instrument sensitivity requires an unreasonable increase in spacecraft mass, resulting effectively in unviable space missions. This suggests the need to develop a gamma ray focuser – an optic capable of concentrating gamma rays onto a small detector, thus minimising background and maximising sensitivity. This report will detail the scientific justification of such a mission, describing the potential return from the use of a ‘Gamma-Ray Lens’.
Recommended publications
  • The Moon Beyond 2002: Next Steps in Lunar Science and Exploration
    The Moon Beyond 2002: Next Steps in Lunar Science and Exploration September 12-14, 2002 Taos, New Mexico Sponsors Los Alamos National laboratory The University of California Institute of Geophysics and Planetary Physics (ICPP) Los Alamos Center for Space Science and Exploration Lunar and Planetary Institute Meeting Organizer David J. Lawrence (Los Alamos National Laboratory) Scientific Organizing Committee Mike Duke (Colorado School of Mines) Sarah Dunkin (Rutherford Appleton Laboratory) Rick Elphic (Los Alamos National Laboratory) Ray Hawke (University of Hawai’i) Lon Hood (University of Arizona) Brad Jolliff (Washington University) David Lawrence (Los Alamos National Laboratory) Chip Shearer (University of New Mexico) Harrison Schmitt (University of Wisconsin) Lunar and Planetary Institute 3600 Bay Area Boulevard Houston TX 77058-1113 LPI Contribution No. 1128 Compiled in 2002 by LUNAR AND PLANETARY INSTITUTE The Institute is operated by the Universities Space Research Association under Contract No. NASW-4574 with the National Aeronautics and Space Administration. Material in this volume may be copied without restraint for library, abstract service, education, or personal research purposes; however, republication of any paper or portion thereof requires the written permission of the authors as well as the appropriate acknowledgment of this publication. Abstracts in this volume may be cited as Author A. B. (2002) Title of abstract. In The Moon Beyond 2002: Next Steps in Lunar Science and Exploration, P. XX. LPI Contribution No. 1128, Lunar and Planetary Institute, Houston. The volume is distributed by ORDER DEPARTMENT Lunar and Planetary Institute 3600 Bay Area Boulevard Houston TX 77058-1113, USA Phone: 281-486-2172 Fax: 281-486-2186 E-mail: [email protected] Mail order requestors will be invoiced for the cost of shipping and handling.
    [Show full text]
  • Flynn Creek Crater, Tennessee: Final Report, by David J
    1967010060 ASTROGEOLOGIC STUDIES / ANNUAL PROGRESS REPORT " July 1, 1965 to July 1, 1966 ° 'i t PART B - h . CRATERINVESTIGATIONS N 67_1_389 N 57-" .]9400 (ACCEC_ION [4U _" EiER! (THRU} .2_ / PP (PAGLS) (CO_ w ) _5 (NASA GR OR I"MX OR AD NUMBER) (_ATEGORY) DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOQICAL SURVEY • iri i i i i iiii i i 1967010060-002 ASTROGEOLOGIC STUDIES ANNUAL PROGRESS REPORT July i, 1965 to July I, 1966 PART B: CRATER INVESTIGATIONS November 1966 This preliminary report is distributed without editorial and technical review for conformity with official standards and nomenclature. It should not be quoted without permission. This report concerns work done on behalf of the National Aeronautics and Space Administration. DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY 1967010060-003 • #' C OING PAGE ,BLANK NO/" FILMED. CONTENTS PART B--CRATER INVESTIGATIONS Page Introduction ........................ vii History and origin of the Flynn Creek crater, Tennessee: final report, by David J. Roddy .............. 1 Introductien ..................... 1 Geologic history of the Flynn Creek crater ....... 5 Origin of the Flynn Creek crater ............ ii Conc lusions ...................... 32 References cited .................... 35 Geology of the Sierra Madera structure, Texas: progress report, by H. G. Wilshire ............ 41_ Introduction ...................... 41 Stratigraphy ...................... 41 Petrography and chemical composition .......... 49 S truc ture ....................... 62 References cited ............. ...... 69 Some aspects of the Manicouagan Lake structure in Quebec, Canada, by Stephen H. Wolfe ................ 71 f Craters produced by missile impacts, by H. J. Moore ..... 79 Introduction ...................... 79 Experimental procedure ................. 80 Experimental results .................. 81 Summary ........................ 103 References cited .................... 103 Hypervelocity impact craters in pumice, by H. J. Moore and / F.
    [Show full text]
  • The Disintegration of the Wolf Creek Meteorite and the Formation of Pecoraite, the Nickel Analog of Clinochrysotile
    The Disintegration of the Wolf Creek Meteorite and the Formation of Pecoraite, the Nickel Analog of Clinochrysotile GEOLOGICAL SURVEY PROFESSIONAL PAPER 384-C 1 mm ^^ 5 -fc;- Jj. -f->^ -J^' ' _." ^P^-Arvx^B^ »""*- 'S y^'ir'*'*'/?' trK* ^-7 A5*^v;'VvVr*'^**s! ^^^^V'^"^"''"X^^i^^?l^"%^ - ! ^ Pecoraite, Wolf Creek meteorite of Australia. Upper, Pecoraite grains separated by hand picking from crack fillings in the meteorite (X 25). Lower, Pecoraite grains lining the walls of some cracks in the meteorite. The extent of disintegration of the original metal­ lic phases into new phases, chiefly goethite and maghemite, is apparent (X 2.3). THE DISINTEGRATION OF THE WOLF CREEK METEORITE AND THE FORMATION OF PECORAITE, THE NICKEL ANALOG OF CLINOCHRYSOTILE The Disintegration of the Wolf Creek Meteorite and the Formation of Pecoraite, the Nickel Analog of Clinochrysotile By GEORGE T. FAUST, JOSEPH J. FAHEY, BRIAN H. MASON and EDWARD J. DWORNIK STUDIES OF THE NATURAL PHASES IN THE SYSTEM MgO-SiO2 -H2O AND THE SYSTEMS CONTAINING THE CONGENERS OF MAGNESIUM GEOLOGICAL SURVEY PROFESSIONAL PAPER 384-C Origin of pecoraite elucidated through its properties and in terms of the geochemical balance in its desert environment UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1973 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress catalog-card No. 73-600160 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price $1.30 Stock
    [Show full text]
  • Ages of Large Lunar Impact Craters and Implications for Bombardment During the Moon’S Middle Age ⇑ Michelle R
    Icarus 225 (2013) 325–341 Contents lists available at SciVerse ScienceDirect Icarus journal homepage: www.elsevier.com/locate/icarus Ages of large lunar impact craters and implications for bombardment during the Moon’s middle age ⇑ Michelle R. Kirchoff , Clark R. Chapman, Simone Marchi, Kristen M. Curtis, Brian Enke, William F. Bottke Southwest Research Institute, 1050 Walnut Street, Suite 300, Boulder, CO 80302, United States article info abstract Article history: Standard lunar chronologies, based on combining lunar sample radiometric ages with impact crater den- Received 20 October 2012 sities of inferred associated units, have lately been questioned about the robustness of their interpreta- Revised 28 February 2013 tions of the temporal dependance of the lunar impact flux. In particular, there has been increasing focus Accepted 10 March 2013 on the ‘‘middle age’’ of lunar bombardment, from the end of the Late Heavy Bombardment (3.8 Ga) until Available online 1 April 2013 comparatively recent times (1 Ga). To gain a better understanding of impact flux in this time period, we determined and analyzed the cratering ages of selected terrains on the Moon. We required distinct ter- Keywords: rains with random locations and areas large enough to achieve good statistics for the small, superposed Moon, Surface crater size–frequency distributions to be compiled. Therefore, we selected 40 lunar craters with diameter Cratering Impact processes 90 km and determined the model ages of their floors by measuring the density of superposed craters using the Lunar Reconnaissance Orbiter Wide Angle Camera mosaic. Absolute model ages were computed using the Model Production Function of Marchi et al.
    [Show full text]
  • Time-Resolved Biological and Perturbation Chemical Crystallography
    Invited Paper Time-resolvedbiological and perturbation chemical crystallography: Laue and monochromatic developments G. Bradbrook, A. Deacon, J. Habash, J.R. Helliwell*, M. Helliwell, Y.P. Nieh, E.H. Snell, & S. Trapani Department of Chemistry, University of Manchester Manchester M13 9PL, U.K. A.W. Thompson & J.W. Campbell Daresbury Laboratory, Daresbury, Warrington, Cheshire, WA4 4AD, UK N.M. Allinson & K. Moon Department of Electronics, University of York, Heslington, York, YOl 5DD, UK T. Ursby & M. Wulif ESRF, BP220, Grenoble Cedex, France *To whom correspondence should be addressed +Present address: EMBL/ESRF, Avenue des Martyrs, Grenoble Cedex, France ABSTRACT Time-resolved macromolecular X-ray crystallography is a new capability for structural analysis driven by continuing improvements in synchrotron X-ray sources, optics and detectors (image plates and CCDs). Protein crystal Laue data (stationary crystal and polychromatic X-rays) were recorded at SRS Daresbury station 9.5 and ESRF Grenoble beamline 3, and processed with the Daresbury Laue software package. The Laue method allows exposure times set by the synchrotron electron bunch width, eg. 50 picoseconds. The instruments and methods developments widen opportunities for perturbation chemical crystallography studies too. A temperature depen- dent phase transition of a liquid crystal nickel-octahexylphthalocyanine is studied with a rapid readout CCD detector. Structure solution by molecular replacement methods with Laue data is reported for orthorhombic lysozyme. By use of tetragonal lysozyrne as a test case it is shown that with fine angular intervals, wide total angular coverage of Laue exposures and the deconvolution of multiples, good connectivity of electron density maps can be realised. The monochromatic rotating crystal method offers possibilities of extremely fast rotations which allow a complete data set to be recorded onto a single image -Large-angleoscillation technique (LOT).
    [Show full text]
  • Bulk Mineralogy of Lunar Crater Central Peaks Via Thermal Infrared Spectra from the Diviner Lunar Radiometer - a Study of the Moon’S Crustal Composition at Depth
    Bulk mineralogy of Lunar crater central peaks via thermal infrared spectra from the Diviner Lunar Radiometer - A study of the Moon’s crustal composition at depth Eugenie Song A thesis submitted in partial fulfillment of the requirements for the degree of Master of Sciences University of Washington 2012 Committee: Joshua Bandfield Alan Gillespie Bruce Nelson Program Authorized to Offer Degree: Earth and Space Sciences 1 Table of Contents List of Figures ............................................................................................................................................... 3 List of Tables ................................................................................................................................................ 3 Abstract ......................................................................................................................................................... 4 1 Introduction .......................................................................................................................................... 5 1.1 Formation of the Lunar Crust ................................................................................................... 5 1.2 Crater Morphology ................................................................................................................... 7 1.3 Spectral Features of Rock-Forming Silicates in the Lunar Environment ................................ 8 1.4 Compositional Studies of Lunar Crater Central Peaks ...........................................................
    [Show full text]
  • Uzbek Diction a Ry of Nano Тес Hnol Og Y and Microelectronics
    С.З. ЗАЙНОБИДИНОВ, И.Н.КАРИМОВ, А.Р.ТУРАЕВ ENGLISH-R USSIA N- UZBEK DICTION A RY OF NANO ТЕС HNOL OG Y AND MICROELECTRONICS АНГЛО-РУССКО-УЗБЕКСКИЙ СЛОВАРЬ ПО НАНОТЕХНОЛОГИЯМ И МИКРОЭЛЕКТРОНИКЕ НАНОТЕХНОЛОГИЯЛАР ВА МИКРОЭЛЕКТРОНИКАДА Н ИНГЛИЗ ЧА-РУСЧА - УЗБЕК ЧА ЛУГ АТ С.З. ЗАЙ1ЮБИДИНОВ, И.Н.КАРИМОВ, А.Р.ТУРАЕВ ENGLISH-RUSSIAN-UZBEK DICTIONARY OF NANOTECHNOLOGY AND MICROELECTRONICS АНГЛО-РУССКО-УЗБЕКСКИЙ СЛОВАРЬ ПО НАНОТЕХНОЛОГИЯМ И МИКРОЭЛЕКТРОНИКЕ НАНОТЕХНОЛОГИЯЛАР ВА МИКРОЭЛЕКТРОНИКАДАН ИНГЛИЗ ЧА-РУСЧА- УЗБЕКЧА ЛУГ АТ \ Узбекистан Республикам Олий ва урта ' таълим вспирлиглшииг 2018 йил 14 гпоидаги \ 53J~6yupy,?iL’a асосаи 5140200 — Физика \ мушахчссислиги талабалари учупуцув ! адабиёши сифишида тавсия эптлгаи. « х ;а ё т » Андижон-2018 йил УДК: 621.3.049.77 ББК: 32.844.1я2 3-22 Академик С.З.Зайнобидинов умумий мухаррирлигида Масъул муя;аррирлар: Инглиз тили кафедраси доценти, филология фанлари номзоди Алимов Шаробидцин Солиевич Узбек тили ва адабиёти кафедраси доценти, филология фанлари номзоди Саидхонов Маъмиржон Мухаммедович Рус тили ва адабиёти кафедраси катта укитувчиси Богданович Геннадий Александрович Такризчи: Техника фанлари доктори, профессор Алиев Раимжон Усмонович Под общей редакцией академика С.З.Зайнабидинова Отвественные редакторы: Кандидат филологических наук, доцент кафедры Английского языка Алимов Шаробидцин Солиевич Кандидат филологических наук, доцент кафедры Узбекского языка и литературы Саидхонов Маъмиржон Мухаммедович Старший преподаватель кафедры Русского языка и литературы Богданович Г еннадий Александрович Рецензент: Доктор технических наук, профессор Алиев Раимжан Усманович JSBN'97S-9f43-5353-4-3 © «ХАЁТ», 2018 й С^З БОШИ Такдим этилаётган ушбу уч тилли Нанотехнологиялар ва микроэлектроникадан инглизча-русча-Узбекча лугат микроэлектроника, каттик жисмлар, яримутказгичлар ва диэлектриклар физикаси, хамда наноэлектроника сохаларига таалукди. булган 13 мингга якин суз ва ибораларидан иборат.
    [Show full text]
  • Moon Clementine Topographic Maps
    GEOLOGIC INVESTIGATIONS SERIES I–2769 U.S. DEPARTMENT OF THE INTERIOR Prepared for the LUNAR NEAR SIDE AND FAR SIDE HEMISPHERES U.S. GEOLOGICAL SURVEY NORTH NATIONAL AERONAUTICS AND SPACE ADMINISTRATION NORTH SHEET 1 OF 3 90° 90° 80° . 80° 80° 80° Peary Hermite Nansen Byrd Rozhdestvenskiy 70° 70° Near Side Far Side 70° 70° Hemisphere Hemisphere Plaskett Pascal . Petermann . Poinsot . Cremona . Scoresby v Hayn SHEET 1 . Milankovic 60° Baillaud 60° 60° Schwarzschild . Mezentsev 60° . Seares Ricco Meton Bel'kovich . Philolaus Bel'kovich . Karpinskiy . Hippocrates Barrow MARE Roberts . Poczobutt Xenophanes Pythagoras HUMBOLDTIANUM . Kirkwood Arnold West East Gamow Volta Strabo Stebbins 50° . 50° Hemisphere Hemisphere 50° Compton 50° Sommerfeld Babbage J. Herschel W. Bond . Kane De La Avogadro . South Rue Emden . Coulomb Galvani SHEET 2 Olivier Tikhov Birkhoff Endymion . MARE FR . Störmer IG O . von Rowland Harpalus R Békésy . IS Sarton 40° IS 40° 40° . Chappell . Stefan 40° . Mercurius Carnot OR Lacus North South Fabry . Millikan Wegener . Plato Tempor Hemisphere Hemisphere D'Alembert . Paraskevopoulos Bragg Ju ra . Aristoteles is Atlas . Schlesinger SINUS R s Montes . Slipher Wood te Harkhebi n Vallis Alpes . Montgolfier o SHEET 3 SINUS Lacus Hercules Landau Nernst M H. G. Campbell Mons . Bridgman Alpes Gauss Wells Rümker . Mortis INDEX . Vestine IRIDUM Eudoxus Messala . Cantor Ley Lorentz Wiener Frost 30° 30° 30° Szilard . 30° LA . Von Neumann CUS SOMNIOR . Kurchatov Charlier Hahn Maxwell . Appleton . Gadomski MARE UM Laue la Joliot o Montes Caucasus . Bartels ric . Aristillus Seyfert . Kovalevskaya . Russell Ag IMBRIUM . Posidonius tes Shayn n . Larmor o Cleomedes Plutarch . Cockcroft . M Montes . Berkner O Mare Struve er A .
    [Show full text]
  • Image Map of the Moon
    U.S. Department of the Interior Prepared for the Scientific Investigations Map 3316 U.S. Geological Survey National Aeronautics and Space Administration Sheet 1 of 2 180° 0° 5555°° –55° Rowland 150°E MAP DESCRIPTION used for printing. However, some selected well-known features less that 85 km in diameter or 30°E 210°E length were included. For a complete list of the IAU-approved nomenclature for the Moon, see the This image mosaic is based on data from the Lunar Reconnaissance Orbiter Wide Angle 330°E 6060°° Gazetteer of Planetary Nomenclature at http://planetarynames.wr.usgs.gov. For lunar mission C l a v i u s –60°–60˚ Camera (WAC; Robinson and others, 2010), an instrument on the National Aeronautics and names, only successful landers are shown, not impactors or expended orbiters. Space Administration (NASA) Lunar Reconnaissance Orbiter (LRO) spacecraft (Tooley and others, 2010). The WAC is a seven band (321 nanometers [nm], 360 nm, 415 nm, 566 nm, 604 nm, 643 nm, and 689 nm) push frame imager with a 90° field of view in monochrome mode, and ACKNOWLEDGMENTS B i r k h o f f Emden 60° field of view in color mode. From the nominal 50-kilometer (km) polar orbit, the WAC This map was made possible with thanks to NASA, the LRO mission, and the Lunar Recon- Scheiner Avogadro acquires images with a 57-km swath-width and a typical length of 105 km. At nadir, the pixel naissance Orbiter Camera team. The map was funded by NASA's Planetary Geology and Geophys- scale for the visible filters (415–689 nm) is 75 meters (Speyerer and others, 2011).
    [Show full text]
  • []ASA-CR-150945) SCIENTIFIC SUPPORT of the N76-31277 ?OLLO INFRARED SCANNING RADIOMETER EXPERIMENT Final Report (Rice Univ.) 236 P HC $8.00 CSCL Igb Unclas
    1976024189 / Jt []ASA-CR-150945) SCIENTIFIC SUPPORT OF THE N76-31277 ?OLLO INFRARED SCANNING RADIOMETER EXPERIMENT Final Report (Rice Univ.) 236 p HC $8.00 CSCL IgB Unclas I G3/19 02973 FINAL REPORT Scientific Support of the Apollo Infrared Scanning Radiometer Experiment Contract NAS9-I0428 Rice University 1976024189-002 %_ The enclosed collection of publications constitutes the final report for Co_tract NAS9-I0428, "Scientific Support of the Apollo Infrared Scanning Radiometer Experiment". The principal document for reference is entitled, "The Apollo 17 Infrared Scanning Radiometer" by Wendell W. Mendell. It contains a detailed discussion of the experimental objectives, instrument design and development, and radiometric calibration. In later chapters of the document the instrument performance is analyzed and the nature of the scientific results is estab- lished. The other documents address more specific topics and generally are earlier results. The collection as a whole represents the Principal Investigator's effort for Apollo Experiment S-171. : This effort established the utility of _¢anning radio- metry for the study of planetary surface processes. The quantitative, two-dimensional thermal "image" produced by the scanning technique permits an exchange of information between the radiometric results and photogeologic mapping. Collections of point radiometric measurements are difficult to interpret without reference to the surface geology. Thermal maps clarify the correlations. Once the geological context of the : thermal data is clear, then the physical properties of the geologic units can be quantified from the thermal emission data. 8 1976024189-003 i 1 I : i ' -2- _" The Infrared Scanning Radiometer also proved out the concept of mapping low temperature surfaces using an uncooled bolometer detector.
    [Show full text]
  • Insritut.MAX VON LAUE-PAUL [ANGEVIN-GRENOBLE-FRANCE ^
    INSriTUT.MAX VON LAUE-PAUL [ANGEVIN-GRENOBLE-FRANCE ^ for the use of the ILL facilities All research proposals have to be submitted to the Scientific Commercially exploitable results Council for approval. The Council meets twice each year and the closing dates for the acceptance of applications are: Visitors and ILL scientists may occasionally be involved in ex­ February 15 and August 31. periments which have possible commercial applications. If any The completed research proposal forms should be sent to: scientist considers that this is the case, he should get in touch Scientific Coordination and Public Relations Office with the Scientific Secretary. (SCAPRO) Institut Max von Laue — Paul Langevin Other publications available 156 X Neutron Research Facilities at the ILL High Flux Reactor, Edi­ 38042 Grenoble Cedex tion June 1986. France Information and Regulations for Reactor Users, Long-Term Tel. 76 48 72 44 B. Maier Visitors and New Scientific Staff, Edition March 1984 76 48 71 79 G. Briggs Brochure "20 years ILL" issued on the occasion of the 20th 76 48 70 41 K. Mayer-Jenkins (Secretary) anniversary of the ILL on 19 January 1987 76 48 70 82 F. Cook (Secretary) all available from SCAPRO Telex: 320621 F Experimental Reports and Theory College Activities 1986 (Appropriate application forms may be obtained on I equest available from the ILL Library. from the above office). Under normal circumstances the ILL makes no charge for the use of its facilities. However, special equipment (other than the existing instruments, counters, standard cryostats and shielding requirements) must be provided by the user. This ap­ plies particularly to the experimental samples which must, in all cases, be provided by the user.
    [Show full text]
  • Utilization of a Solar Sail to Perform a Lunar Cubesat Science Mission
    Utilization of a Solar Sail to Perform a Lunar CubeSat Science Mission 2nd Interplanetary CubeSat Workshop Ithaca, New York May 28 -29, 2013 The University of Texas at Austin (UT): Texas Spacecraft Laboratory (TSL) Peter Z. Schulte Undergraduate Research Assistant E. Glenn Lightsey Professor Katharine M. Brumbaugh Graduate Research Assistant Jet Propulsion Laboratory, California Institute of Technology (JPL) Robert L. Staehle Assistant Manager for Advanced Concepts, Instruments Division 1 Overview • Demonstrate use of solar sail propulsion to enable unique lunar science missions • Six-unit (6U) CubeSat configuration with spacecraft mass ≈ 12 kg • Deliver as secondary payload to circular Low-Lunar Orbit (LLO) • Deploy solar sail and raise orbit to accomplish science objectives • Show an example destination: enter an L2 halo orbit 2 Solar Sail Technology • Constant low-thrust propulsion with reduced mass and limited propellant use • Several 400 m 2 sails have been deployed on the ground in demonstrations by NASA and DLR 1 • Recent and upcoming Earth-orbiting solar sail technology demonstration flights 2-4: IKAROS Spacecraft (JAXA) 2 Name Organization Sail Size Date Spacecraft IKAROS JAXA 200 m 2 June 2010 Custom NanoSail-D2 NASA/AFRL 10 m 2 January 2011 3U CubeSat CubeSail NASA/CU 25 m 2 Planned 2013 3U CubeSat Aerospace/ Univ. of Illinois DeOrbitSail Univ. of Surrey 25 m 2 Planned 2014 3U CubeSat LightSail TM -1 Planetary 32 m 2 Planned 2015 3U CubeSat Society NanoSail-D2 Spacecraft (NASA) 3 3 Concept of Operations 1.) Launch 2.) Deliver to Moon 3.) Deploy 6U 4.) Cruise Phase in on MPCV CubeSat from MPCV Lunar Circular Orbit 5.) Deploy Solar Sail 6.) Orbit Raising 7.) Transfer to L2 8.) Halo Orbit at L2 Image Sources: Panels 1,2, and 4 - various public NASA websites.
    [Show full text]