Surveyor a Press Kit 66-127 May 26 1966
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Selection of the Insight Landing Site M. Golombek1, D. Kipp1, N
Manuscript Click here to download Manuscript InSight Landing Site Paper v9 Rev.docx Click here to view linked References Selection of the InSight Landing Site M. Golombek1, D. Kipp1, N. Warner1,2, I. J. Daubar1, R. Fergason3, R. Kirk3, R. Beyer4, A. Huertas1, S. Piqueux1, N. E. Putzig5, B. A. Campbell6, G. A. Morgan6, C. Charalambous7, W. T. Pike7, K. Gwinner8, F. Calef1, D. Kass1, M. Mischna1, J. Ashley1, C. Bloom1,9, N. Wigton1,10, T. Hare3, C. Schwartz1, H. Gengl1, L. Redmond1,11, M. Trautman1,12, J. Sweeney2, C. Grima11, I. B. Smith5, E. Sklyanskiy1, M. Lisano1, J. Benardino1, S. Smrekar1, P. Lognonné13, W. B. Banerdt1 1Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109 2State University of New York at Geneseo, Department of Geological Sciences, 1 College Circle, Geneseo, NY 14454 3Astrogeology Science Center, U.S. Geological Survey, 2255 N. Gemini Dr., Flagstaff, AZ 86001 4Sagan Center at the SETI Institute and NASA Ames Research Center, Moffett Field, CA 94035 5Southwest Research Institute, Boulder, CO 80302; Now at Planetary Science Institute, Lakewood, CO 80401 6Smithsonian Institution, NASM CEPS, 6th at Independence SW, Washington, DC, 20560 7Department of Electrical and Electronic Engineering, Imperial College, South Kensington Campus, London 8German Aerospace Center (DLR), Institute of Planetary Research, 12489 Berlin, Germany 9Occidental College, Los Angeles, CA; Now at Central Washington University, Ellensburg, WA 98926 10Department of Earth and Planetary Sciences, University of Tennessee, Knoxville, TN 37996 11Institute for Geophysics, University of Texas, Austin, TX 78712 12MS GIS Program, University of Redlands, 1200 E. Colton Ave., Redlands, CA 92373-0999 13Institut Physique du Globe de Paris, Paris Cité, Université Paris Sorbonne, France Diderot Submitted to Space Science Reviews, Special InSight Issue v. -
Materials for Liquid Propulsion Systems
https://ntrs.nasa.gov/search.jsp?R=20160008869 2019-08-29T17:47:59+00:00Z CHAPTER 12 Materials for Liquid Propulsion Systems John A. Halchak Consultant, Los Angeles, California James L. Cannon NASA Marshall Space Flight Center, Huntsville, Alabama Corey Brown Aerojet-Rocketdyne, West Palm Beach, Florida 12.1 Introduction Earth to orbit launch vehicles are propelled by rocket engines and motors, both liquid and solid. This chapter will discuss liquid engines. The heart of a launch vehicle is its engine. The remainder of the vehicle (with the notable exceptions of the payload and guidance system) is an aero structure to support the propellant tanks which provide the fuel and oxidizer to feed the engine or engines. The basic principle behind a rocket engine is straightforward. The engine is a means to convert potential thermochemical energy of one or more propellants into exhaust jet kinetic energy. Fuel and oxidizer are burned in a combustion chamber where they create hot gases under high pressure. These hot gases are allowed to expand through a nozzle. The molecules of hot gas are first constricted by the throat of the nozzle (de-Laval nozzle) which forces them to accelerate; then as the nozzle flares outwards, they expand and further accelerate. It is the mass of the combustion gases times their velocity, reacting against the walls of the combustion chamber and nozzle, which produce thrust according to Newton’s third law: for every action there is an equal and opposite reaction. [1] Solid rocket motors are cheaper to manufacture and offer good values for their cost. -
Mapping the Surveyor III Crater Large-Scale Maps May Be Produced from Lunar Oribiter Photographs
FIG. 1. The Surveyor I II Crater. CHARLES W. SHULL t LYNN A. SCHENK U. S. Army TOPOCOM Washington, D. C.20315 Mapping the Surveyor III Crater large-scale maps may be produced from lunar Oribiter photographs (Abstract on next page) INRODUCTlON Because of the inclination of the camera, lunar features were viewed more clearly than URVEYOR III spacecraft was launched Son April 17, 1967 toward the moon on a would have been possible on flat terrain. mission to explore possible Apollo landing This crater, then, became an object of in sites. On April 19 the Surveyor landed on the tense interest to the scientific community, moon's Ocean of Storms and almost imme especially to astrogeologists who had the diately began transmitting television pictures unique opportunity of observing high quality back to Earth. When the lunar day ended pictures of the interior of a lunar crater for on May 3, over 6,300 photographs had been the first time. Because of this unusual characteristic, the received from Surveyor III by the Jet Pro pulsion Laboratory.* ational Aeronautics and Space Administra vVhen the spacecraft landed, it came to tion (NASA) requested that the Department of Defense prepare two maps of the crater rest on the inside slope of crater giving it a 12.40 tilt from the local vertical (Figure 1). and surrounding areas. The request was for a photo mosaic at 1 :2,000 scale with 10-meter t Presented at the Annual Convention of the contours and a shaded relief map with con American Society of Photogrammetry in Washing tours at the smallest interval possible. -
The Moon After Apollo
ICARUS 25, 495-537 (1975) The Moon after Apollo PAROUK EL-BAZ National Air and Space Museum, Smithsonian Institution, Washington, D.G- 20560 Received September 17, 1974 The Apollo missions have gradually increased our knowledge of the Moon's chemistry, age, and mode of formation of its surface features and materials. Apollo 11 and 12 landings proved that mare materials are volcanic rocks that were derived from deep-seated basaltic melts about 3.7 and 3.2 billion years ago, respec- tively. Later missions provided additional information on lunar mare basalts as well as the older, anorthositic, highland rocks. Data on the chemical make-up of returned samples were extended to larger areas of the Moon by orbiting geo- chemical experiments. These have also mapped inhomogeneities in lunar surface chemistry, including radioactive anomalies on both the near and far sides. Lunar samples and photographs indicate that the moon is a well-preserved museum of ancient impact scars. The crust of the Moon, which was formed about 4.6 billion years ago, was subjected to intensive metamorphism by large impacts. Although bombardment continues to the present day, the rate and size of impact- ing bodies were much greater in the first 0.7 billion years of the Moon's history. The last of the large, circular, multiringed basins occurred about 3.9 billion years ago. These basins, many of which show positive gravity anomalies (mascons), were flooded by volcanic basalts during a period of at least 600 million years. In addition to filling the circular basins, more so on the near side than on the far side, the basalts also covered lowlands and circum-basin troughs. -
NASA News National Aeronautics and Space Administration Washington
NASA News National Aeronautics and Space Administration Washington. D C 20546 AC 202 755-8370 For Release IMMEDIATE Press Kit Project Intelsat V-D RELEASE NO: 82-30 Contents GENERAL RELEASE 1 ATLAS CENTAUR, LAUNCH VEHICLE STATISTICS 3 LAUNCH OPERATIONS 4 LAUNCH SEQUENCE FOR INTELSAT V-D 5 THE NASA INTELSAT TEAM 6 CONTRACTORS 7 /lNASA-News-Belease-82^TOl INTELSAT N82-22295 "\ (SATELLITE SCHEDULED FOR LAUNCH (National (Aeronautics and Space Administration) 8 p I CSCL 22A Unclas I 00/15 18771 February 26, 1982 NASA News National Aeronautics and Space Administration Washington. D C 20546 AC 202 755-8370 For Release Dick McCormack Headquarters, Washington, D.C. IMMEDIATE (Phone: 202/755-8104) RELEASE NO: 82-30 INTELSAT SATELLITE SCHEDULED FOR LAUNCH Intelsat V-D, the fourth of a new series of nine inter- national telecommunications satellites owned and operated by the 105-nation International Telecommunications Satellite Organiza- tion (Intelsat), is scheduled to be launched by the NASA Kennedy Space Center on board an Atlas Centaur launch vehicle no earlier than March 4, 1982, from Cape Canaveral, Fla. The three Intelsat Vs were successfully launched by NASA in December 1980, May 1981 and December 1981. Intelsat V-D weighs 1,928 kilograms (4,251 pounds) at launch and has almost double the communications capability of early satellites in the Intelsat series — 12,000 voice circuits and two color television channels. It will be positioned in geosyn- chronous orbit over the Indian Ocean as the prime Intelsat satel- lite to provide communications services between Europe, the Middle East and the Far East. -
Water on the Moon, III. Volatiles & Activity
Water on The Moon, III. Volatiles & Activity Arlin Crotts (Columbia University) For centuries some scientists have argued that there is activity on the Moon (or water, as recounted in Parts I & II), while others have thought the Moon is simply a dead, inactive world. [1] The question comes in several forms: is there a detectable atmosphere? Does the surface of the Moon change? What causes interior seismic activity? From a more modern viewpoint, we now know that as much carbon monoxide as water was excavated during the LCROSS impact, as detailed in Part I, and a comparable amount of other volatiles were found. At one time the Moon outgassed prodigious amounts of water and hydrogen in volcanic fire fountains, but released similar amounts of volatile sulfur (or SO2), and presumably large amounts of carbon dioxide or monoxide, if theory is to be believed. So water on the Moon is associated with other gases. Astronomers have agreed for centuries that there is no firm evidence for “weather” on the Moon visible from Earth, and little evidence of thick atmosphere. [2] How would one detect the Moon’s atmosphere from Earth? An obvious means is atmospheric refraction. As you watch the Sun set, its image is displaced by Earth’s atmospheric refraction at the horizon from the position it would have if there were no atmosphere, by roughly 0.6 degree (a bit more than the Sun’s angular diameter). On the Moon, any atmosphere would cause an analogous effect for a star passing behind the Moon during an occultation (multiplied by two since the light travels both into and out of the lunar atmosphere). -
Gao-21-306, Nasa
United States Government Accountability Office Report to Congressional Committees May 2021 NASA Assessments of Major Projects GAO-21-306 May 2021 NASA Assessments of Major Projects Highlights of GAO-21-306, a report to congressional committees Why GAO Did This Study What GAO Found This report provides a snapshot of how The National Aeronautics and Space Administration’s (NASA) portfolio of major well NASA is planning and executing projects in the development stage of the acquisition process continues to its major projects, which are those with experience cost increases and schedule delays. This marks the fifth year in a row costs of over $250 million. NASA plans that cumulative cost and schedule performance deteriorated (see figure). The to invest at least $69 billion in its major cumulative cost growth is currently $9.6 billion, driven by nine projects; however, projects to continue exploring Earth $7.1 billion of this cost growth stems from two projects—the James Webb Space and the solar system. Telescope and the Space Launch System. These two projects account for about Congressional conferees included a half of the cumulative schedule delays. The portfolio also continues to grow, with provision for GAO to prepare status more projects expected to reach development in the next year. reports on selected large-scale NASA programs, projects, and activities. This Cumulative Cost and Schedule Performance for NASA’s Major Projects in Development is GAO’s 13th annual assessment. This report assesses (1) the cost and schedule performance of NASA’s major projects, including the effects of COVID-19; and (2) the development and maturity of technologies and progress in achieving design stability. -
Surveyor 1 Space- Craft on June 2, 1966 As Seen by the Narrow Angle Camera of the Lunar Re- Connaissance Orbiter Taken on July 17, 2009 (Also See Fig
i “Project Surveyor, in particular, removed any doubt that it was possible for Americans to land on the Moon and explore its surface.” — Harrison H. Schmitt, Apollo 17 Scientist-Astronaut ii Frontispiece: Landing site of the Surveyor 1 space- craft on June 2, 1966 as seen by the narrow angle camera of the Lunar Re- connaissance Orbiter taken on July 17, 2009 (also see Fig. 13). The white square in the upper photo outlines the area of the enlarged view below. The spacecraft is ca. 3.3 m tall and is casting a 15 m shadow to the East. (NASA/LROC/ ASU/GSFC photos) iii iv Surveyor I: America’s First Moon Landing by William F. Mellberg v © 2014, 2015 William F. Mellberg vi About the author: William Mellberg was a marketing and public relations representative with Fokker Aircraft. He is also an aerospace historian, having published many articles on both the development of airplanes and space vehicles in various magazines. He is the author of Famous Airliners and Moon Missions. He also serves as co-Editor of Harrison H. Schmitt’s website: http://americasuncommonsense.com Acknowledgments: The support and recollections of Frank Mellberg, Harrison Schmitt, Justin Rennilson, Alexander Gurshstein, Paul Spudis, Ronald Wells, Colin Mackellar and Dwight Steven- Boniecki is gratefully acknowledged. vii Surveyor I: America’s First Moon Landing by William F. Mellberg A Journey of 250,000 Miles . December 14, 2013. China’s Chang’e 3 spacecraft successfully touched down on the Moon at 1311 GMT (2111 Beijing Time). The landing site was in Mare Imbrium, the Sea of Rains, about 25 miles (40 km) south of the small crater, Laplace F, and roughly 100 miles (160 km) east of its original target in Sinus Iridum, the Bay of Rainbows. -
Surveyor Ill Mission Report Part I
\ NAT IONAL AERONAUT ICS AND SPAC E ADMIN ISTRATION Technical Report 32-1177 Surveyor Ill Mission Report Part I. Mission Description and Performance JET PROPULSION LAB ORATOR Y CALIFORNIA INS TITUTE OF TECHNOLOGY PASAD E NA, CALIFORNIA September 1, 1967 NAT IONAL AERONA UT ICS AND SPAC E AD MINISTRAT ION Technical Report 32-1177 Surveyor Ill Mission Report Part I. Mission Description and Performance Approved for publication by: H. H. Haglund Surveyor Project Manager JET PROPULSION LAB ORA TOR Y CAL I FORNIA INSTITUTE OF TECHNOLO GY PASAD E NA, CAL I FORNI A September 1, 1967 TECHNICAL REPORT 32-1 177 Copyright © 7 196 Jet Propulsion laboratory California Institute of Technology Prepared Under Contract No. NAS 7-100 National Aeronautics Space Administration & Preface This three-part document constitutes the Surveyor III Mission Report. It describes the third in a series of unmanned missions designed to soft-land on the moon and return data from the lunar surface. Part I of this report consists of a technical description and an evaluation of engineering results of the systems utilized in the Surveyor III mission. Analysis of the data received from the Surveyor III mission is continuing, and it is expected that additional results will be obtained together with some improvement in accuracy. Part I was compiled using the contributions of many individuals in the major systems which support the Project. Some of the information for this report was obtained from other published documents; a list of these documents is con tained in a bibliography. Part II of this report presents the scientific data derived from the mission and the results of scientific analyses which have been conducted. -
Open Research Online Oro.Open.Ac.Uk
Open Research Online The Open University’s repository of research publications and other research outputs Analysis of Lunar Boulder Tracks: Implications for Trafficability of Pyroclastic Deposits Journal Item How to cite: Bickel, V. T.; Honniball, C. I.; Martinez, S. N.; Rogaski, A.; Sargeant, Hannah; Bell, S. K.; Czaplinski, E. C.; Farrant, B. E.; Harrington, E. M.; Tolometti, G. D. and Kring, D. A. (2019). Analysis of Lunar Boulder Tracks: Implications for Trafficability of Pyroclastic Deposits. Journal of Geophysical Research: Planets, 124(5) pp. 1296–1314. For guidance on citations see FAQs. c 2019 American Geophysical Union https://creativecommons.org/licenses/by-nc-nd/4.0/ Version: Version of Record Link(s) to article on publisher’s website: http://dx.doi.org/doi:10.1029/2018JE005876 Copyright and Moral Rights for the articles on this site are retained by the individual authors and/or other copyright owners. For more information on Open Research Online’s data policy on reuse of materials please consult the policies page. oro.open.ac.uk RESEARCH ARTICLE Analysis of Lunar Boulder Tracks: Implications 10.1029/2018JE005876 for Trafficability of Pyroclastic Deposits Key Points: V. T. Bickel1,2 , C. I. Honniball3, S. N. Martinez4, A. Rogaski5, H. M. Sargeant6, S. K. Bell7, • Bearing capacity of pyroclastic, 8 7 9 9 10,11 mare, and highland regions is E. C. Czaplinski , B. E. Farrant , E. M. Harrington , G. D. Tolometti , and D. A. Kring calculated based on measurements 1 2 of boulder tracks in orbital images Department Planets & Comets, Max -
Shoot the Moon – 1967
Video Transcript for Archival Research Catalog (ARC) Identifier 45011 Assignment: Shoot the Moon – 1967 Narrator: The assignment was specific: get photographs of the surface of the Moon that are good enough to determine whether or not it’s safe for a man to land there. But appearances can be deceiving, just as deceiving as trying to get a good picture of, well, a candy apple. Doesn’t seem to be too much of a problem, just set it up, light it, and snap the picture. Easy, quick, simple. But it can be tough. To begin with, the apple is some distance away, so you can’t get to it to just set it up, light it, and so on. To make things even more difficult, it isn’t even holding still; it’s moving around in circles. Now timing is important. You have to take your picture when the apple is nearest to you so you get the most detail and when the light that’s available is at the best angle for the photo. And even that’s not all. You are moving too, in circles. You’re both turning and circling about the apple. Now, about that assignment. As the technology of man in space was developing, it became more and more apparent that our knowledge of the Moon’s surface as a possible landing site was not sufficient. To land man safely on the Moon and get him safely off again, we had to know whether we could set up a precise enough trajectory to reach the Moon. -
Analysis of a Heavy Lift Launch Vehicle Design Using Small Liquid
Analysis of a Heavy Lift Launch Vehicle Design Using Small Liquid Rocket Engines by DAVID PHILLIP RUSS S.B., Massachusetts Institute of Technology 1987 SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE IN AERONAUTICS AND ASTRONAUTICS at the MASSACHUSETTS INSTITUTE OF TECHNOLOGY May 1988 ® David P. Russ 1988 The author hereby grants M.I.T. and Hughes Aircraft Company permission to reproduce and to distribute copies of this thesis document in whole or in part. Signature of Author Department of Aeronautics and Astronautics December 18, 1987 Reviewed by C. P. Rubin Hughes Aircraft Company Certified by Professor Walter M. Hollister Thesis Supervjsor, Departmer of Aeronautics and Astronautics .. Accepted by , .AU Professor Harold Y. Wachman Chairman, Depart'rmental Graduate Committee Department of Aeronautics and Astronautics MAY i od ;WITHDRAWfIN i M.I.1W.i..: P. I LBRARt S UBAer 7:Ir_ Aero Analysis of a Heavy Lift Launch Vehicle Design Using Small Liquid Rocket Engines by David P. Russ Submitted to the Department of Aeronautics and Astronautics in partial fulfillment of the requirements for the degree of Master of Science in Aeronautics and Astronautics May, 1988 Abstract The trend in launch vehicle design has been to increase performance by using en- gines of greater and greater complexity, which has a negative effect on cost and reliability. However, a design making use of over 300 small, simple rocket engines can deliver over 340,000 lbs to low Earth orbit. This design, derived by using the rocket equations to size the major components, features a 42 ft.