Preparation of Papers for AIAA Technical Conferences
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Appendix 1: Venus Missions
Appendix 1: Venus Missions Sputnik 7 (USSR) Launch 02/04/1961 First attempted Venus atmosphere craft; upper stage failed to leave Earth orbit Venera 1 (USSR) Launch 02/12/1961 First attempted flyby; contact lost en route Mariner 1 (US) Launch 07/22/1961 Attempted flyby; launch failure Sputnik 19 (USSR) Launch 08/25/1962 Attempted flyby, stranded in Earth orbit Mariner 2 (US) Launch 08/27/1962 First successful Venus flyby Sputnik 20 (USSR) Launch 09/01/1962 Attempted flyby, upper stage failure Sputnik 21 (USSR) Launch 09/12/1962 Attempted flyby, upper stage failure Cosmos 21 (USSR) Launch 11/11/1963 Possible Venera engineering test flight or attempted flyby Venera 1964A (USSR) Launch 02/19/1964 Attempted flyby, launch failure Venera 1964B (USSR) Launch 03/01/1964 Attempted flyby, launch failure Cosmos 27 (USSR) Launch 03/27/1964 Attempted flyby, upper stage failure Zond 1 (USSR) Launch 04/02/1964 Venus flyby, contact lost May 14; flyby July 14 Venera 2 (USSR) Launch 11/12/1965 Venus flyby, contact lost en route Venera 3 (USSR) Launch 11/16/1965 Venus lander, contact lost en route, first Venus impact March 1, 1966 Cosmos 96 (USSR) Launch 11/23/1965 Possible attempted landing, craft fragmented in Earth orbit Venera 1965A (USSR) Launch 11/23/1965 Flyby attempt (launch failure) Venera 4 (USSR) Launch 06/12/1967 Successful atmospheric probe, arrived at Venus 10/18/1967 Mariner 5 (US) Launch 06/14/1967 Successful flyby 10/19/1967 Cosmos 167 (USSR) Launch 06/17/1967 Attempted atmospheric probe, stranded in Earth orbit Venera 5 (USSR) Launch 01/05/1969 Returned atmospheric data for 53 min on 05/16/1969 M. -
Catherinesaunders
The Utility of Robot Sensory Devices in a Collaborative Autonomic Environment Catherine Saunders, Roy Sterritt, George Wilkie School of Computing and Mathematics University of Ulster Northern Ireland [email protected], [email protected], [email protected] Abstract –-This paper proposes an Autonomic architecture that environment and relay meaningful information to each will enable mobile robots to self-manage and collaborate by other. using control loops to monitor their internal state and external environment. The Autonomic Computing MAPE-K control In this paper we discuss the sensor capabilities of the Dr loop is used to design a Robot Autonomic Element and a Robot X80-H platform that will be used for the research. A Mapping Autonomic Element; each can exchange data and collaborate to find an object located within a room. A review of design of the proposed system is included and explained. A the sensor capabilities of the X80-H mobile robot platform is brief literature review of robotic collaborative systems is undertaken with emphasis on how useful each sensor will be to also included. The Research Background section looks at the proposed research. A literature review of other projects why self-managing software systems are needed. that feature robot collaboration is also included. Keywords - autonomic computing; mobile robot; Dr Robot II. ROBOT SENSORY DEVICES X80-H; collaboration; MAPE-K This section gives an overview of the sensors that the Dr Robot X80-H is equipped with. We assess how reliable they are and how useful they will be for our research. We will be I. -
+ New Horizons
Media Contacts NASA Headquarters Policy/Program Management Dwayne Brown New Horizons Nuclear Safety (202) 358-1726 [email protected] The Johns Hopkins University Mission Management Applied Physics Laboratory Spacecraft Operations Michael Buckley (240) 228-7536 or (443) 778-7536 [email protected] Southwest Research Institute Principal Investigator Institution Maria Martinez (210) 522-3305 [email protected] NASA Kennedy Space Center Launch Operations George Diller (321) 867-2468 [email protected] Lockheed Martin Space Systems Launch Vehicle Julie Andrews (321) 853-1567 [email protected] International Launch Services Launch Vehicle Fran Slimmer (571) 633-7462 [email protected] NEW HORIZONS Table of Contents Media Services Information ................................................................................................ 2 Quick Facts .............................................................................................................................. 3 Pluto at a Glance ...................................................................................................................... 5 Why Pluto and the Kuiper Belt? The Science of New Horizons ............................... 7 NASA’s New Frontiers Program ........................................................................................14 The Spacecraft ........................................................................................................................15 Science Payload ...............................................................................................................16 -
Titan and the Moons of Saturn Telesto Titan
The Icy Moons and the Extended Habitable Zone Europa Interior Models Other Types of Habitable Zones Water requires heat and pressure to remain stable as a liquid Extended Habitable Zones • You do not need sunlight. • You do need liquid water • You do need an energy source. Saturn and its Satellites • Saturn is nearly twice as far from the Sun as Jupiter • Saturn gets ~30% of Jupiter’s sunlight: It is commensurately colder Prometheus • Saturn has 82 known satellites (plus the rings) • 7 major • 27 regular • 4 Trojan • 55 irregular • Others in rings Titan • Titan is nearly as large as Ganymede Titan and the Moons of Saturn Telesto Titan Prometheus Dione Titan Janus Pandora Enceladus Mimas Rhea Pan • . • . Titan The second-largest moon in the Solar System The only moon with a substantial atmosphere 90% N2 + CH4, Ar, C2H6, C3H8, C2H2, HCN, CO2 Equilibrium Temperatures 2 1/4 Recall that TEQ ~ (L*/d ) Planet Distance (au) TEQ (K) Mercury 0.38 400 Venus 0.72 291 Earth 1.00 247 Mars 1.52 200 Jupiter 5.20 108 Saturn 9.53 80 Uranus 19.2 56 Neptune 30.1 45 The Atmosphere of Titan Pressure: 1.5 bars Temperature: 95 K Condensation sequence: • Jovian Moons: H2O ice • Saturnian Moons: NH3, CH4 2NH3 + sunlight è N2 + 3H2 CH4 + sunlight è CH, CH2 Implications of Methane Free CH4 requires replenishment • Liquid methane on the surface? Hazy atmosphere/clouds may suggest methane/ ethane precipitation. The freezing points of CH4 and C2H6 are 91 and 92K, respectively. (Titan has a mean temperature of 95K) (Liquid natural gas anyone?) This atmosphere may resemble the primordial terrestrial atmosphere. -
Space Sector Brochure
SPACE SPACE REVOLUTIONIZING THE WAY TO SPACE SPACECRAFT TECHNOLOGIES PROPULSION Moog provides components and subsystems for cold gas, chemical, and electric Moog is a proven leader in components, subsystems, and systems propulsion and designs, develops, and manufactures complete chemical propulsion for spacecraft of all sizes, from smallsats to GEO spacecraft. systems, including tanks, to accelerate the spacecraft for orbit-insertion, station Moog has been successfully providing spacecraft controls, in- keeping, or attitude control. Moog makes thrusters from <1N to 500N to support the space propulsion, and major subsystems for science, military, propulsion requirements for small to large spacecraft. and commercial operations for more than 60 years. AVIONICS Moog is a proven provider of high performance and reliable space-rated avionics hardware and software for command and data handling, power distribution, payload processing, memory, GPS receivers, motor controllers, and onboard computing. POWER SYSTEMS Moog leverages its proven spacecraft avionics and high-power control systems to supply hardware for telemetry, as well as solar array and battery power management and switching. Applications include bus line power to valves, motors, torque rods, and other end effectors. Moog has developed products for Power Management and Distribution (PMAD) Systems, such as high power DC converters, switching, and power stabilization. MECHANISMS Moog has produced spacecraft motion control products for more than 50 years, dating back to the historic Apollo and Pioneer programs. Today, we offer rotary, linear, and specialized mechanisms for spacecraft motion control needs. Moog is a world-class manufacturer of solar array drives, propulsion positioning gimbals, electric propulsion gimbals, antenna positioner mechanisms, docking and release mechanisms, and specialty payload positioners. -
Page 1 of 18 Michael J. Malaska, Ph. D. Jet Propulsion Laboratory
Michael J. Malaska, Ph. D. Jet Propulsion Laboratory, California Institute of Technology 4800 Oak Grove Dr., MS 183-301 Pasadena, CA 91109-8099 818-354-7652 [email protected] OBJECTIVE Highly creative and enthusiastic individual with a broad background in planetary science, chemistry, and geology with a research program in planetary science at the interface of the sciences of geology, chemistry, and astrobiology with specific skills encompassing field science, laboratory research, and remote sensing. EDUCATION NASA/Jet Propulsion Laboratory, California Institute of Technology, NPP Senior Postdoctoral Fellow, 2012-2015 Mayo Clinic Jacksonville, postdoctoral position in Neurochemistry, 1991-1993. University of California, Berkeley, Ph.D. in Chemistry, 1991. Massachusetts Institute of Technology, S.B. in Chemistry, 1986. RESEARCH SUMMARY My planetary geology research program has focused on the interface of chemical and geological processes on Saturn's moon Titan based on data returned by the Cassini-Huygens spacecraft. These studies examine how liquid hydrocarbon rains and rivers on that world have eroded and dissolved a landscape made of organic materials layered upon rock-hard water ice. My key discoveries include the identification and characterization of labyrinth terrain on Titan, comparison of meandering channels to high-volume rivers on Earth, and the modelling of dissolution processes of Titan surface materials. My current program involves laboratory studies examining the dissolution geology of Titan and the geomorphological mapping of Titan's surface. My 20 year career as an organic chemist in drug discovery was located at the interface of chemistry and biology. This research has discovered new chemical compounds that can interact with enzymes and receptors to control cellular processes and treat diseases. -
Planetary Exploration : Progress and Promise
PLANET ARY EXPLORATION PROGRESS AND PROMISE CONTENTS: NASA PLANETARY EXPLORATION PLANS: SIGNIFICANT EVENTS PLANETARY EXPLORATION PROGRESS-1978 NASA SPACE SCIENCE PROGRAM FUNDING: 5 -YEAR PLAN NASA OSS 5-YEAR PLAN: PLANETARY PROGRAM FUNDING REFERENCE COP'I PLEASE DO NOT REMOVE compiled by Dr. Leonard Srnka, Staff Scientist Lunar and Planetary Institute 3303 NASA Road One Houston, Texas 77058 Lunar and Planetary Institute Contribution No. 297 (June 1978 update> NASA PLANETARY EXPLORATION PLANS SIGNIFICANT EVENTS MISSION EVENTS PIONEER VENUS ORBITER ORBIT INSERTION, DECEMBER 1978 PIONEER VENUS MULTIPROBE VENUS ENCOUNTER/ENTRY, DECEMBER 1978 PIONEER 11 SATURN ENCOUNTER, SEPTEMBER 1979 VOYAGER 1 JUPITER ENCOUNTER, MARCH 1979 SATURN ENCOUNTER, NOVEMBER 1980 VOYAGER 2 JUPITER ENCOUNTER, JULY 1979 SATURN ENCOUNTER, AUGUST 1981 URANUS ENCOUNTER, JANUARY 1986 SOLAR MAXIMUM MISSION LAUNCH, OCTOBER 1979 VENUS ORBITAL IMAGING RADAR VENUS ENCOUNTER, SPRING 1985 SOLAR POLAR MISSION JUPITER ENCOUNTER, 1984 SOLAR POLES PASSAGE, 1986 GALILEO MISSION MARS FLYBY, APRIL 1982 JUPITER ENCOUNTER (ORBIT INSERTION/ PROBE ENTRY), 1985 COMET HALLEYlTEMPEL, . 2'J MISSION• HALLEY ENCOUNTER, NOVEMBER 1985 TEMPEL 2 ENCOUNTER, JULY 1988 or COMET ENCKE RENDEZVOUS ENCKE ENCOUNTER, 1987 MARS GEOCHEMICAL ORBITER MARS ENCOUNTER, 1987 MARS SAMPLE RETURN MARS ENCOUNTER, 1989 EARTH RETURN, 1991 SATURN ORBITER DUAL PROBE SATURN ENCOUNTER, 1992 from NASA Headquarters 5-year plan May 1978 PLANETARY EXPLORATION -- PROGRESS AND PROMISE CONTENT S: Planetary exploration progress - 1977 fig. 1 The future fig. 2 Inner planets plan fig. 3 Outer planets plan fig. 4 Small bodies plan fig. 5 compiled by Dr. Leonard Srnka, Staff Scientist LUNAR SCIENCE INSTITUTE 3303 NASA Road One Houston, TX 77058 September 1977 LUNAR SCIENCE INSTITUTE CONTRIBUTION No. -
Pioneer Anomaly: What Can We Learn from Future Planetary Exploration Missions?
56th International Astronautical Congress, Paper IAC-05-A3.4.02 PIONEER ANOMALY: WHAT CAN WE LEARN FROM FUTURE PLANETARY EXPLORATION MISSIONS? Andreas Rathke EADS Astrium GmbH, Dept. AED41, 88039 Friedrichshafen, Germany. Email: [email protected] Dario Izzo ESA Advanced Concepts Team, ESTEC, Keplerlaan 1, 2200 AG Noordwijk, The Netherlands. Email: [email protected] The Doppler-tracking data of the Pioneer 10 and 11 spacecraft show an unmodelled constant acceleration in the direction of the inner Solar System. Serious efforts have been undertaken to find a conventional explanation for this effect, all without success at the time of writing. Hence the effect, commonly dubbed the Pioneer anomaly, is attracting considerable attention. Unfortunately, no other space mission has reached the long-term navigation accuracy to yield an independent test of the effect. To fill this gap we discuss strategies for an experimental verification of the anomaly via an upcoming space mission. Emphasis is put on two plausible scenarios: non-dedicated concepts employing either a planetary exploration mission to the outer Solar System or a piggybacked micro- spacecraft to be launched from an exploration spacecraft travelling to Saturn or Jupiter. The study analyses the impact of a Pioneer anomaly test on the system and trajectory design for these two paradigms. Both paradigms are capable of verifying the Pioneer anomaly and determine its magnitude at 10% level. Moreover they can discriminate between the most plausible classes of models of the anomaly. The necessary adaptions of the system and mission design do not impair the planetary exploration goals of the missions. I. -
The Lakes and Seas of Titan • Explore Related Articles • Search Keywords Alexander G
EA44CH04-Hayes ARI 17 May 2016 14:59 ANNUAL REVIEWS Further Click here to view this article's online features: • Download figures as PPT slides • Navigate linked references • Download citations The Lakes and Seas of Titan • Explore related articles • Search keywords Alexander G. Hayes Department of Astronomy and Cornell Center for Astrophysics and Planetary Science, Cornell University, Ithaca, New York 14853; email: [email protected] Annu. Rev. Earth Planet. Sci. 2016. 44:57–83 Keywords First published online as a Review in Advance on Cassini, Saturn, icy satellites, hydrology, hydrocarbons, climate April 27, 2016 The Annual Review of Earth and Planetary Sciences is Abstract online at earth.annualreviews.org Analogous to Earth’s water cycle, Titan’s methane-based hydrologic cycle This article’s doi: supports standing bodies of liquid and drives processes that result in common 10.1146/annurev-earth-060115-012247 Annu. Rev. Earth Planet. Sci. 2016.44:57-83. Downloaded from annualreviews.org morphologic features including dunes, channels, lakes, and seas. Like lakes Access provided by University of Chicago Libraries on 03/07/17. For personal use only. Copyright c 2016 by Annual Reviews. on Earth and early Mars, Titan’s lakes and seas preserve a record of its All rights reserved climate and surface evolution. Unlike on Earth, the volume of liquid exposed on Titan’s surface is only a small fraction of the atmospheric reservoir. The volume and bulk composition of the seas can constrain the age and nature of atmospheric methane, as well as its interaction with surface reservoirs. Similarly, the morphology of lacustrine basins chronicles the history of the polar landscape over multiple temporal and spatial scales. -
Titan a Moon with an Atmosphere
TITAN A MOON WITH AN ATMOSPHERE Ashley Gilliam Earth 450 – Satellites of Jupiter and Saturn 4/29/13 SATURN HAS > 60 SATELLITES, WHY TITAN? Is the only satellite with a dense atmosphere Has a nitrogen-rich atmosphere resembles Earth’s Is the only world besides Earth with a liquid on its surface • Possible habitable world Based on its size… Titan " a planet in its o# $ght! R = 6371 km R = 2576 km R = 1737 km Ch$%iaan Huy&ns (1629-1695) DISCOVERY OF TITAN Around 1650, Huygens began building telescopes with his brother Constantijn On March 25, 1655 Huygens discovered Titan in an attempt to study Saturn’s rings Named the moon Saturni Luna (“Saturns Moon”) Not properly named until the mid-1800’s THE DISCOVERY OF TITAN’S ATMOSPHERE Not much more was learned about Titan until the early 20th century In 1903, Catalan astronomer José Comas Solà claimed to have observed limb darkening on Titan, which requires the presence of an atmosphere Gerard P. Kuiper (1905-1973) José Comas Solà (1868-1937) This was confirmed by Gerard Kuiper in 1944 Image Credit: Ralph Lorenz Voyager 1 Launched September 5, 1977 M"sions to Titan Pioneer 11 Launched April 6, 1973 Cassini-Huygens Images: NASA Launched October 15, 1997 Pioneer 11 Could not penetrate Titan’s Atmosphere! Image Credit: NASA Vo y a &r 1 Image Credit: NASA Vo y a &r 1 What did we learn about the Atmosphere? • Composition (N2, CH4, & H2) • Variation with latitude (homogeneously mixed) • Temperature profile Mesosphere • Pressure profile Stratosphere Troposphere Image Credit: Fulchignoni, et al., 2005 Image Credit: Conway et al. -
NASA History Fact Sheet
NASA History Fact Sheet National Aeronautics and Space Administration Office of Policy and Plans NASA History Office NASA History Fact Sheet A BRIEF HISTORY OF THE NATIONAL AERONAUTICS AND SPACE ADMINISTRATION by Stephen J. Garber and Roger D. Launius Launching NASA "An Act to provide for research into the problems of flight within and outside the Earth's atmosphere, and for other purposes." With this simple preamble, the Congress and the President of the United States created the national Aeronautics and Space Administration (NASA) on October 1, 1958. NASA's birth was directly related to the pressures of national defense. After World War II, the United States and the Soviet Union were engaged in the Cold War, a broad contest over the ideologies and allegiances of the nonaligned nations. During this period, space exploration emerged as a major area of contest and became known as the space race. During the late 1940s, the Department of Defense pursued research and rocketry and upper atmospheric sciences as a means of assuring American leadership in technology. A major step forward came when President Dwight D. Eisenhower approved a plan to orbit a scientific satellite as part of the International Geophysical Year (IGY) for the period, July 1, 1957 to December 31, 1958, a cooperative effort to gather scientific data about the Earth. The Soviet Union quickly followed suit, announcing plans to orbit its own satellite. The Naval Research Laboratory's Project Vanguard was chosen on 9 September 1955 to support the IGY effort, largely because it did not interfere with high-priority ballistic missile development programs. -
The Origin of Titan's Atmosphere: Some Recent Advances
The origin of Titan’s atmosphere: some recent advances By Tobias Owen1 & H. B. Niemann2 1University of Hawaii, Institute for Astronomy, 2680 Woodlawn Drive, Honolulu, HI 96822, USA 2Laboratory for Atmospheres, Goddard Space Fight Center, Greenbelt, MD 20771, USA It is possible to make a consistent story for the origin of Titan’s atmosphere starting with the birth of Titan in the Saturn subnebula. If we use comet nuclei as a model, Titan’s nitrogen and methane could easily have been delivered by the ice that makes up ∼50% of its mass. If Titan’s atmospheric hydrogen is derived from that ice, it is possible that Titan and comet nuclei are in fact made of the same protosolar ice. The noble gas abundances are consistent with relative abundances found in the atmospheres of Mars and Earth, the sun, and the meteorites. Keywords: Origin, atmosphere, composition, noble gases, deuterium 1. Introduction In this note, we will assume that Titan originated in Saturn’s subnebula as a result of the accretion of icy planetesimals: particles and larger lumps made of ice and rock. Alibert & Mousis (2007) reached this same point of view using an evolutionary, turbulent model of Saturn’s subnebula. They found that planetesimals made in the solar nebula according to their model led to a huge overabundance of CO on Titan. We obviously have no direct measurements of the composition of these planetes- imals. We can use comets as a guide, always remembering that comets formed in the solar nebula where conditions must have been different from those in Saturn’s subnebula, e.g., much colder.