Spacecraft Deliberately Crashed on the Lunar Surface
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Master Table of All Deep Space, Lunar, and Planetary Probes, 1958–2000 Official Name Spacecraft / 1958 “Pioneer” Mass[Luna] No
Deep Space Chronicle: Master Table of All Deep Space, Lunar, and Planetary Probes, 1958–2000 Official Spacecraft / Mass Launch Date / Launch Place / Launch Vehicle / Nation / Design & Objective Outcome* Name No. Time Pad No. Organization Operation 1958 “Pioneer” Able 1 38 kg 08-17-58 / 12:18 ETR / 17A Thor-Able I / 127 U.S. AFBMD lunar orbit U [Luna] Ye-1 / 1 c. 360 kg 09-23-58 / 09:03:23 NIIP-5 / 1 Luna / B1-3 USSR OKB-1 lunar impact U Pioneer Able 2 38.3 kg 10-11-58 / 08:42:13 ETR / 17A Thor-Able I / 130 U.S. NASA / AFBMD lunar orbit U [Luna] Ye-1 / 2 c. 360 kg 10-11-58 / 23:41:58 NIIP-5 / 1 Luna / B1-4 USSR OKB-1 lunar impact U Pioneer 2 Able 3 39.6 kg 11-08-58 / 07:30 ETR / 17A Thor-Able I / 129 U.S. NASA / AFBMD lunar orbit U [Luna] Ye-1 / 3 c. 360 kg 12-04-58 / 18:18:44 NIIP-5 / 1 Luna / B1-5 USSR OKB-1 lunar impact U Pioneer 3 - 5.87 kg 12-06-58 / 05:44:52 ETR / 5 Juno II / AM-11 U.S. NASA / ABMA lunar flyby U 1959 Luna 1 Ye-1 / 4 361.3 kg 01-02-59 / 16:41:21 NIIP-5 / 1 Luna / B1-6 USSR OKB-1 lunar impact P Master Table of All Deep Space, Lunar, andPlanetary Probes1958–2000 ofAllDeepSpace,Lunar, Master Table Pioneer 4 - 6.1 kg 03-03-59 / 05:10:45 ETR / 5 Juno II / AM-14 U.S. -
Low-Energy Lunar Trajectory Design
LOW-ENERGY LUNAR TRAJECTORY DESIGN Jeffrey S. Parker and Rodney L. Anderson Jet Propulsion Laboratory Pasadena, California July 2013 ii DEEP SPACE COMMUNICATIONS AND NAVIGATION SERIES Issued by the Deep Space Communications and Navigation Systems Center of Excellence Jet Propulsion Laboratory California Institute of Technology Joseph H. Yuen, Editor-in-Chief Published Titles in this Series Radiometric Tracking Techniques for Deep-Space Navigation Catherine L. Thornton and James S. Border Formulation for Observed and Computed Values of Deep Space Network Data Types for Navigation Theodore D. Moyer Bandwidth-Efficient Digital Modulation with Application to Deep-Space Communication Marvin K. Simon Large Antennas of the Deep Space Network William A. Imbriale Antenna Arraying Techniques in the Deep Space Network David H. Rogstad, Alexander Mileant, and Timothy T. Pham Radio Occultations Using Earth Satellites: A Wave Theory Treatment William G. Melbourne Deep Space Optical Communications Hamid Hemmati, Editor Spaceborne Antennas for Planetary Exploration William A. Imbriale, Editor Autonomous Software-Defined Radio Receivers for Deep Space Applications Jon Hamkins and Marvin K. Simon, Editors Low-Noise Systems in the Deep Space Network Macgregor S. Reid, Editor Coupled-Oscillator Based Active-Array Antennas Ronald J. Pogorzelski and Apostolos Georgiadis Low-Energy Lunar Trajectory Design Jeffrey S. Parker and Rodney L. Anderson LOW-ENERGY LUNAR TRAJECTORY DESIGN Jeffrey S. Parker and Rodney L. Anderson Jet Propulsion Laboratory Pasadena, California July 2013 iv Low-Energy Lunar Trajectory Design July 2013 Jeffrey Parker: I dedicate the majority of this book to my wife Jen, my best friend and greatest support throughout the development of this book and always. -
Insights from the Thorium Abundance Distribution in South Pole-Aitken Basin
Lunar and Planetary Science XXXVIII (2007) 1697.pdf DID A KREEP-LIKE COMPONENT EXIST ON THE FAR SIDE OF THE MOON?: INSIGHTS FROM THE THORIUM ABUNDANCE DISTRIBUTION IN SOUTH POLE-AITKEN BASIN. J. J. Hagerty1, D. J. Lawrence1, B. R. Hawke2, R. C. Elphic1, T. H. Prettyman1, and W. C. Feldman1, 1Los Alamos National Laboratory, ISR-1, MS D466, Los Alamos, NM 87545, email: [email protected]. 2University of Hawaii, Honolulu, HI 96822. Introduction: Most models for the evolution of materials on top of those basalt ponds. These results the Moon predict that 99% fractional crystallization of provide important information that help us to evaluate a lunar magma ocean will produce a layer of melt en- the source of Th enhancements in SPA basin. riched in incompatible elements such as K, REE, and P Forward Modeling: As part of the forward model- (i.e., KREEP) [1]. The lateral extent and distribution of ing process, we re-create a specific portion of the lunar this “KREEP” layer, which contains an abundance of surface in which we can control the Th abundances of heat-producing elements such as Th and U, is currently specific geologic features [12,13]. We must also know a matter of debate. However some workers [2] have what Th abundances can be reasonably assigned to any proposed that the surficial distribution of Th, which given feature and/or lithology, which is why we use has been measured on a global-scale [3,4,5], can be analyses from the lunar sample suite to constrain the used as a proxy for determining the global distribution upper and lower bounds of our Th estimates. -
Exploration of the Moon
Exploration of the Moon The physical exploration of the Moon began when Luna 2, a space probe launched by the Soviet Union, made an impact on the surface of the Moon on September 14, 1959. Prior to that the only available means of exploration had been observation from Earth. The invention of the optical telescope brought about the first leap in the quality of lunar observations. Galileo Galilei is generally credited as the first person to use a telescope for astronomical purposes; having made his own telescope in 1609, the mountains and craters on the lunar surface were among his first observations using it. NASA's Apollo program was the first, and to date only, mission to successfully land humans on the Moon, which it did six times. The first landing took place in 1969, when astronauts placed scientific instruments and returnedlunar samples to Earth. Apollo 12 Lunar Module Intrepid prepares to descend towards the surface of the Moon. NASA photo. Contents Early history Space race Recent exploration Plans Past and future lunar missions See also References External links Early history The ancient Greek philosopher Anaxagoras (d. 428 BC) reasoned that the Sun and Moon were both giant spherical rocks, and that the latter reflected the light of the former. His non-religious view of the heavens was one cause for his imprisonment and eventual exile.[1] In his little book On the Face in the Moon's Orb, Plutarch suggested that the Moon had deep recesses in which the light of the Sun did not reach and that the spots are nothing but the shadows of rivers or deep chasms. -
An Impacting Descent Probe for Europa and the Other Galilean Moons of Jupiter
An Impacting Descent Probe for Europa and the other Galilean Moons of Jupiter P. Wurz1,*, D. Lasi1, N. Thomas1, D. Piazza1, A. Galli1, M. Jutzi1, S. Barabash2, M. Wieser2, W. Magnes3, H. Lammer3, U. Auster4, L.I. Gurvits5,6, and W. Hajdas7 1) Physikalisches Institut, University of Bern, Bern, Switzerland, 2) Swedish Institute of Space Physics, Kiruna, Sweden, 3) Space Research Institute, Austrian Academy of Sciences, Graz, Austria, 4) Institut f. Geophysik u. Extraterrestrische Physik, Technische Universität, Braunschweig, Germany, 5) Joint Institute for VLBI ERIC, Dwingelo, The Netherlands, 6) Department of Astrodynamics and Space Missions, Delft University of Technology, The Netherlands 7) Paul Scherrer Institute, Villigen, Switzerland. *) Corresponding author, [email protected], Tel.: +41 31 631 44 26, FAX: +41 31 631 44 05 1 Abstract We present a study of an impacting descent probe that increases the science return of spacecraft orbiting or passing an atmosphere-less planetary bodies of the solar system, such as the Galilean moons of Jupiter. The descent probe is a carry-on small spacecraft (< 100 kg), to be deployed by the mother spacecraft, that brings itself onto a collisional trajectory with the targeted planetary body in a simple manner. A possible science payload includes instruments for surface imaging, characterisation of the neutral exosphere, and magnetic field and plasma measurement near the target body down to very low-altitudes (~1 km), during the probe’s fast (~km/s) descent to the surface until impact. The science goals and the concept of operation are discussed with particular reference to Europa, including options for flying through water plumes and after-impact retrieval of very-low altitude science data. -
50. Obletnica Pristanka Na Luni in Pomen Osvajanja Vesolja Za Geodezijo 50Th Anniversary of the Moon Landing and the Importance
GEODETSKI VESTNIK | 63/4 | 50. OBLETNICA PRISTANKA 50TH ANNIVERSARY OF NA LUNI IN POMEN THE MOON LANDING AND OSVAJANJA VESOLJA ZA THE IMPORTANCE OF GEODEZIJO CONQUERING SPACE FOR GEODESY Sandi Berk STROKOVNE RAZPRAVE | PROFESSIONAL DISCUSSIONS RAZPRAVE STROKOVNE 1 UVOD Letos mineva petdeset let od prvega obiska človeka na edini Zemljini luni – Mesecu (v nadaljevanju kar: Luna). Ta »majhen korak za človeka, a velikanski skok za človeštvo« je bil storjen 20. julija 1969, ko sta Neil Armstrong in Edwin Aldrin v lunarnem modulu Eagle (tj. Orel) pristala poleg Malega zahodnega kraterja v Morju tišine (slika 1). Okrogla obletnica je priložnost, da se ozremo nazaj in osvežimo dogod- ke iz pionirskih časov osvajanja vesolja. Hkrati lahko osvetlimo pomen takratnih podvigov ter njihove učinke na tehnološki razvoj in tudi napredek geodezije. Slika 1: Armstrongova fotografija Aldrina ob nameščenem seizmografu; nad njim je reflektor za lasersko merjenje oddaljenosti od Zemlje, desno zgoraj pa je lunarni modul Eagle (vir: NASA, 2019). | 589 | | 63/4 | GEODETSKI VESTNIK Kje se sploh prične vesolje – kako visoko je treba poleteti? Mejo med Zemljino atmosfero in vesoljskim prostorom (angl. outer space) imenujemo Kármánova ločnica in je približno sto kilometrov nad površjem Zemlje. Nad to višino za letenje ne veljajo več zakoni aerodinamike, ampak je mogoče zgolj še letenje po zakonih balistike, torej na raketni pogon. Pomembna je tudi v pravnem smislu, saj se tu konča zračni prostor držav in začne veljati mednarodno vesoljsko pravo. Kot vemo, letijo potniška letala na višini približno deset kilometrov. Nedavni rekordni polet z jadralnim letalom je dosegel višino 23 kilometrov nad morjem, vendar s pomočjo stratosferskih zavetrnih valov, ki nastajajo zaradi izredno močnih zračnih tokov med visokimi gorskimi vrhovi Andov (Ebbesen Jensen, 2019). -
Scientists Provide New Explanation for the Far Side of the Moon's Strange
PRESS RELEASE Source: ELSI, Tokyo Institute of Technology, Japan For immediate release: June 22, 2020 Title: Scientists provide new explanation for the far side of the Moon’s strange asymmetry Subtitle: Earth’s Moon has a ‘near side’ that is perpetually Earth‐facing and a ‘far side’, which always faces away from Earth. The composition of the Moon’s near side is oddly different from its far side, and scientists think they finally understand why. Release summary: The Earth‐Moon system’s history remains mysterious. Scientists believe the two formed when a Mars‐sized body collided with the proto‐Earth. Earth ended up being the larger daughter of this collision and retained enough heat to become tectonically active. The Moon, being smaller, likely cooled down faster and geologically ‘froze’. The apparent dynamism of the Moon challenges this idea. New data suggest this is because radioactive elements were distributed uniquely after the catastrophic Moon‐forming collision. Full‐text release: The Earth‐Moon system’s history remains mysterious. Scientists believe the two formed when a Mars‐sized body collided with the proto‐Earth. Earth ended up being the larger daughter of this collision and retained enough heat to become tectonically active. The Moon, being smaller, likely cooled down faster and geologically ‘froze’. The apparent early dynamism of the Moon challenges this idea. New data suggest this is because radioactive elements were distributed uniquely after the catastrophic Moon‐ forming collision. Earth’s Moon, together with the Sun, is a dominant object in our sky and offers many observable features which keep scientists busy trying to explain how our planet and the Solar System formed. -
THE SOVIET MOON PROGRAM in the 1960S, the United States Was Not the Only Country That Was Trying to Land Someone on the Moon and Bring Him Back to Earth Safely
AIAA AEROSPACE M ICRO-LESSON Easily digestible Aerospace Principles revealed for K-12 Students and Educators. These lessons will be sent on a bi-weekly basis and allow grade-level focused learning. - AIAA STEM K-12 Committee. THE SOVIET MOON PROGRAM In the 1960s, the United States was not the only country that was trying to land someone on the Moon and bring him back to Earth safely. The Union of Soviet Socialist Republics, also called the Soviet Union, also had a manned lunar program. This lesson describes some of it. Next Generation Science Standards (NGSS): ● Discipline: Engineering Design ● Crosscutting Concept: Systems and System Models ● Science & Engineering Practice: Constructing Explanations and Designing Solutions GRADES K-2 K-2-ETS1-1. Ask questions, make observations, and gather information about a situation people want to change to define a simple problem that can be solved through the development of a new or improved object or tool. Have you ever been busy doing something when somebody challenges you to a race? If you decide to join the race—and it is usually up to you whether you join or not—you have to stop what you’re doing, get up, and start racing. By the time you’ve gotten started, the other person is often halfway to the goal. This is the sort of situation the Soviet Union found itself in when President Kennedy in 1961 announced that the United States would set a goal of landing a man on the Moon and returning him safely to the Earth before the end of the decade. -
The Soviet Space Program
C05500088 TOP eEGRET iuf 3EEA~ NIE 11-1-71 THE SOVIET SPACE PROGRAM Declassified Under Authority of the lnteragency Security Classification Appeals Panel, E.O. 13526, sec. 5.3(b)(3) ISCAP Appeal No. 2011 -003, document 2 Declassification date: November 23, 2020 ifOP GEEAE:r C05500088 1'9P SloGRET CONTENTS Page THE PROBLEM ... 1 SUMMARY OF KEY JUDGMENTS l DISCUSSION 5 I. SOV.IET SPACE ACTIVITY DURING TfIE PAST TWO YEARS . 5 II. POLITICAL AND ECONOMIC FACTORS AFFECTING FUTURE PROSPECTS . 6 A. General ............................................. 6 B. Organization and Management . ............... 6 C. Economics .. .. .. .. .. .. .. .. .. .. .. ...... .. 8 III. SCIENTIFIC AND TECHNICAL FACTORS ... 9 A. General .. .. .. .. .. 9 B. Launch Vehicles . 9 C. High-Energy Propellants .. .. .. .. .. .. .. .. .. 11 D. Manned Spacecraft . 12 E. Life Support Systems . .. .. .. .. .. .. .. .. 15 F. Non-Nuclear Power Sources for Spacecraft . 16 G. Nuclear Power and Propulsion ..... 16 Te>P M:EW TCS 2032-71 IOP SECl<ET" C05500088 TOP SECRGJ:. IOP SECREI Page H. Communications Systems for Space Operations . 16 I. Command and Control for Space Operations . 17 IV. FUTURE PROSPECTS ....................................... 18 A. General ............... ... ···•· ................. ····· ... 18 B. Manned Space Station . 19 C. Planetary Exploration . ........ 19 D. Unmanned Lunar Exploration ..... 21 E. Manned Lunar Landfog ... 21 F. Applied Satellites ......... 22 G. Scientific Satellites ........................................ 24 V. INTERNATIONAL SPACE COOPERATION ............. 24 A. USSR-European Nations .................................... 24 B. USSR-United States 25 ANNEX A. SOVIET SPACE ACTIVITY ANNEX B. SOVIET SPACE LAUNCH VEHICLES ANNEX C. SOVIET CHRONOLOGICAL SPACE LOG FOR THE PERIOD 24 June 1969 Through 27 June 1971 TCS 2032-71 IOP SLClt~ 70P SECRE1- C05500088 TOP SEGR:R THE SOVIET SPACE PROGRAM THE PROBLEM To estimate Soviet capabilities and probable accomplishments in space over the next 5 to 10 years.' SUMMARY OF KEY JUDGMENTS A. -
Smart Landing Technology for Lunar/Planetary Exploration
IOSR Journal of Computer Engineering (IOSR-JCE) e-ISSN: 2278-0661, p-ISSN: 2278-8727, Volume 18, Issue 2, Ver. I (Mar-Apr. 2016), PP 85-90 www.iosrjournals.org Smart GNC Scheme for Autonomous Planetary Landing Ibrahim Mustafa Mehedi Center of Excellence in Intelligent Engineering Systems (CEIES) King Abdulaziz University, Jeddah, Saudi Arabia AND Electrical and Computer Engineering Department, King Abdulaziz University Jeddah 21589, Saudi Arabia Abstract: The moon or other nearest planets are important destinations for space science and the smart landing is key technology for exploring the different planets without fail. Due to the long round-trip delay of communication with the earth a pinpoint autonomous GNC (guidance-navigation-control) system will be suitable for precise landing. Hazard avoidance is another key issue for a safe landing of future planetary missions. Employing sensors and computers onboard, the lander detects hazards in the landing region, makes quick decision considering mission constraints within exigent time limit and generate trajectory to provide necessary command for guidance module that transfers the lander to a suitable safe landing site. Real time onboard terrain mapping Navigation and Guidance is one which has received much attention in the frame of planetary exploration. The paper illustrates the investigations concerning soft landing for planetary exploration and finally proposed a smart and autonomous GNC scheme based on real time range image measurements technique using laser range finder. Keywords: Planetary landing; Autonomous; Hazard detection and avoidance I. Introduction A several lunar or planetary missions were accomplished in last few decades; the guidance-navigation- control (GNC) technology is getting more important than ever. -
Apollo Over the Moon: a View from Orbit (Nasa Sp-362)
chl APOLLO OVER THE MOON: A VIEW FROM ORBIT (NASA SP-362) Chapter 1 - Introduction Harold Masursky, Farouk El-Baz, Frederick J. Doyle, and Leon J. Kosofsky [For a high resolution picture- click here] Objectives [1] Photography of the lunar surface was considered an important goal of the Apollo program by the National Aeronautics and Space Administration. The important objectives of Apollo photography were (1) to gather data pertaining to the topography and specific landmarks along the approach paths to the early Apollo landing sites; (2) to obtain high-resolution photographs of the landing sites and surrounding areas to plan lunar surface exploration, and to provide a basis for extrapolating the concentrated observations at the landing sites to nearby areas; and (3) to obtain photographs suitable for regional studies of the lunar geologic environment and the processes that act upon it. Through study of the photographs and all other arrays of information gathered by the Apollo and earlier lunar programs, we may develop an understanding of the evolution of the lunar crust. In this introductory chapter we describe how the Apollo photographic systems were selected and used; how the photographic mission plans were formulated and conducted; how part of the great mass of data is being analyzed and published; and, finally, we describe some of the scientific results. Historically most lunar atlases have used photointerpretive techniques to discuss the possible origins of the Moon's crust and its surface features. The ideas presented in this volume also rely on photointerpretation. However, many ideas are substantiated or expanded by information obtained from the huge arrays of supporting data gathered by Earth-based and orbital sensors, from experiments deployed on the lunar surface, and from studies made of the returned samples. -
Deep Space Chronicle Deep Space Chronicle: a Chronology of Deep Space and Planetary Probes, 1958–2000 | Asifa
dsc_cover (Converted)-1 8/6/02 10:33 AM Page 1 Deep Space Chronicle Deep Space Chronicle: A Chronology ofDeep Space and Planetary Probes, 1958–2000 |Asif A.Siddiqi National Aeronautics and Space Administration NASA SP-2002-4524 A Chronology of Deep Space and Planetary Probes 1958–2000 Asif A. Siddiqi NASA SP-2002-4524 Monographs in Aerospace History Number 24 dsc_cover (Converted)-1 8/6/02 10:33 AM Page 2 Cover photo: A montage of planetary images taken by Mariner 10, the Mars Global Surveyor Orbiter, Voyager 1, and Voyager 2, all managed by the Jet Propulsion Laboratory in Pasadena, California. Included (from top to bottom) are images of Mercury, Venus, Earth (and Moon), Mars, Jupiter, Saturn, Uranus, and Neptune. The inner planets (Mercury, Venus, Earth and its Moon, and Mars) and the outer planets (Jupiter, Saturn, Uranus, and Neptune) are roughly to scale to each other. NASA SP-2002-4524 Deep Space Chronicle A Chronology of Deep Space and Planetary Probes 1958–2000 ASIF A. SIDDIQI Monographs in Aerospace History Number 24 June 2002 National Aeronautics and Space Administration Office of External Relations NASA History Office Washington, DC 20546-0001 Library of Congress Cataloging-in-Publication Data Siddiqi, Asif A., 1966 Deep space chronicle: a chronology of deep space and planetary probes, 1958-2000 / by Asif A. Siddiqi. p.cm. – (Monographs in aerospace history; no. 24) (NASA SP; 2002-4524) Includes bibliographical references and index. 1. Space flight—History—20th century. I. Title. II. Series. III. NASA SP; 4524 TL 790.S53 2002 629.4’1’0904—dc21 2001044012 Table of Contents Foreword by Roger D.