Planetary Science Division Status Report
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A Comprehensive Entry, Descent, Landing, And
A Comprehensive Entry, Descent, Landing, and Locomotion (EDLL) Vehicle for Planetary Exploration Kevin Schroeder Dissertation submitted to the Faculty of the Virginia Polytechnic Institute and State University in partial fulfillment of the requirements for the degree of Doctor of Philosophy in Mechanical Engineering Javid Bayandor, Chair Jamshid Samareh Sasan Armand Francine Battaglia Walter O’Brien Wayne Scales July 18th, 2017 Blacksburg, Virginia Keywords: Entry Descent Landing (EDL), Tensegrity, Venus Rover, Deployable Heat Shield Copyright 2017, Kevin Schroeder A Comprehensive Entry, Descent, Landing, and Locomotion (EDLL) Vehicle for Planetary Exploration Kevin Schroeder Abstract The 2012 Decadal Survey has stated that there is a critical role for a Venus In-situ Explore (VISE) missions to a variety of important sites, specifically the Tessera terrain. This work aims to answer the Decadal Survey’s call by developing a new comprehensive Entry, Descent, Landing, and Locomotion (EDLL) vehicle for in-situ exploration of Venus, especially in the Tessera regions. TANDEM, the Tension Adjustable Network for Deploying Entry Membrane, is a new planetary probe concept in which all of EDLL is achieved by a single multifunctional tensegrity structure. The concept uses same fundamental concept as the ADEPT (Adaptable Deployable Entry and Placement Technology) deployable heat shield but replaces the standard internal structure with the structure from the tensegrity- actuated rover to provide a combined aeroshell and rover design. The tensegrity system implemented by TANDEM reduces the mass of the overall system while enabling surface locomotion and mitigating risk associated with landing in the rough terrain of Venus’s Tessera regions, which is otherwise nearly inaccessible to surface missions. -
The Vast Venus Conspiracy, Part III
The Vast Venus Conspiracy, Part III By Dr. Raymond A. Keller, a.k.a. the “Cosmic Ray,” author of the international awards-winning Venus Rising trilogy (Headline Books, Terra Alta, West Virginia, 2015-2017) Why is Lady Gaga depicted with a scorpion in her “Venus” single’s cover art? To find out the amazing answer, go to the end of this article. See also http://gagadaily.com/forums/topic/188509-why-is-there-a-scorpion-on-the-venus- single-cover-art/. Many Surprises The photographs of the Venusian surface transmitted back to the Earth by the Soviet Union’s Venera 13 and Venera 14 landing probes provided many surprises. Planetary geologists were expecting to see a sandy desert under a very dim and distorted light. But what turned up in the photographs was a brightly-lit, orange-tinted landscape with jagged rocks strewn all about. In accordance with the findings of American space probes previously sent to our sister planet, as announced by spokespersons of the National Aeronautics and Space Administration (NASA) in the United States, scientists from around the globe were not anticipating such clear, bright pictures. It was even noted that the distant Venusian horizon was plainly visible in the corner imagery from the Venera photographs. If what the NASA specialists had been telling us all along, that Venus had such an extremely high atmospheric density approaching one hundred times that of the Earth’s, then the Venusian atmosphere would have been found to be as dense as water at a depth of 2,000 feet below sea level. -
New Views of the Moon Enabled by Combined Remotely Sensed and Lunar Sample Data Sets, a Lunar Initiative
New Views of the Moon Enabled by Combined Remotely Sensed and Lunar Sample Data Sets, A Lunar Initiative Using the hand tool on your Reader, click on the links below to view that particular section of the proposal. Proposal Summary Scientific/Technical/Management Objectives and Expected Significance Background and Impact Approach and Methodology: The Role of Integration in Fundamental Problems of Lunar Geoscience Workshop 2: New Views of the Moon II: Understanding the Moon Through the Integration of Diverse Datasets. Abstract Volume and Subsequent Publications Statement of Relevance Work Plan Potential Workshop (2000): Thermal and Magmatic Evolution of the Moon Potential Workshop (2001): Early Lunar Differentiation, Core Formation, Effects of Early Planetesimal Impacts, and the Origin of the Moon’s Global Asymmetry Potential Workshop (2002): Selection of Sites for Future Sample Return Capstone Publication Timeline for the New Views of the Moon Initiative Personnel: Initiative Management and Proposal Management References Facilities: The LPI Appendix 1. Workshop on New Views of the Moon: Integrated Remotely Sensed, Geophysical, and Sample Datasets. List of presentations Appendix 2. LPSC 30 (1999) special sessions related to the Lunar Initiative. List of presentations (oral and poster) Appendix 3. Lunar Initiative Steering Committee Web Note: This is the text of a proposal submitted on behalf of the Lunar Science Community to support ongoing workshops and activities associated with the CAPTEM Lunar Initiative. It was submitted in May, 1999, in response to the ROSS 99 NRA, which solicits such proposals to be submitted to the relevant research programs. This proposal was submitted jointly to Cosmo- chemistry and Planetary Geology and Geophysics. -
CRATER MORPHOMETRY on VENUS. C. G. Cochrane, Imperial College, London ([email protected])
Lunar and Planetary Science XXXIV (2003) 1173.pdf CRATER MORPHOMETRY ON VENUS. C. G. Cochrane, Imperial College, London ([email protected]). Introduction: Most impact craters on Venus are propagating east and north/south. Can be minimised if pristine, and provide probably the best available ana- framelets have good texture on the left-hand side. logs for craters on Earth soon after impact; hence the Prominence extension – features extend down value of measuring their 3-D shape to known accuracy. range into a ridge, eg central peak linked to the rim. The USGS list 967 craters: from the largest, Mead at Probably due to radar shadowing differences, these are 270 km diameter, to the smallest, unnamed at 1.3 km. easily recognised and avoided during analysis. Initially, research focussed on the larger craters. Araration (from Latin: Arare to plough) consists of Schaber et al [1] (11 craters >50 km) and Ivanov et al parallel furrows some 50 pixels apart, oriented north- [2] (31 craters >70 km) took crater depth from Magel- south, and at least tens of metres deep. Fig 2, a lan altimetry. Sharpton [3] (94 craters >18 km) used floor-offsets in Synthetic Aperture Radar (SAR) F- MIDR pairs, as did Herrick & Phillips [4]. They list many parameters but not depth for 891 craters. The LPI database1 now numbers 941. Herrick & Sharpton [5] made Digital Elevation Models (DEMs) of all cra- ters at least partially imaged twice down to 12 km, and 20 smaller craters down to 3.6 km. Using FMAP im- ages and the Magellan Stereo Toolkit (MST) v.1, they automated matches every 900m but then manually ed- ited the resultant data. -
Atlas V Launches LRO/LCROSS Mission Overview
Atlas V Launches LRO/LCROSS Mission Overview Atlas V 401 Cape Canaveral Air Force Station, FL Space Launch Complex-41 AV-020/LRO/LCROSS United Launch Alliance is proud to be a part of the Lunar Reconnaissance Orbiter (LRO) and the Lunar Crater Observation and Sensing Satellite (LCROSS) mission with the National Aeronautics and Space Administration (NASA). The LRO/LCROSS mission marks the sixteenth Atlas V launch and the seventh flight of an Atlas V 401 configuration. LRO/LCROSS is a dual-spacecraft (SC) launch. LRO is a lunar orbiter that will investigate resources, landing sites, and the lunar radiation environment in preparation for future human missions to the Moon. LCROSS will search for the presence of water ice that may exist on the permanently shadowed floors of lunar polar craters. The LCROSS mission will use two Lunar Kinetic Impactors, the inert Centaur upper stage and the LCROSS SC itself, to produce debris plumes that may reveal the presence of water ice under spectroscopic analysis. My thanks to the entire Atlas team for its dedication in bringing LRO/LCROSS to launch, and to NASA for selecting Atlas for this ground-breaking mission. Go Atlas, Go Centaur, Go LRO/LCROSS! Mark Wilkins Vice President, Atlas Product Line Atlas V Launch History Flight Config. Mission Mission Date AV-001 401 Eutelsat Hotbird 6 21 Aug 2002 AV-002 401 HellasSat 13 May 2003 AV-003 521 Rainbow 1 17 Jul 2003 AV-005 521 AMC-16 17 Dec 2004 AV-004 431 Inmarsat 4-F1 11 Mar 2005 AV-007 401 Mars Reconnaissance Orbiter 12 Aug 2005 AV-010 551 Pluto New Horizons 19 Jan 2006 AV-008 411 Astra 1KR 20 Apr 2006 AV-013 401 STP-1 08 Mar 2007 AV-009 401 NROL-30 15 Jun 2007 AV-011 421 WGS SV-1 10 Oct 2007 AV-015 401 NROL-24 10 Dec 2007 AV-006 411 NROL-28 13 Mar 2008 AV-014 421 ICO G1 14 Apr 2008 AV-016 421 WGS-2 03 Apr 2009 Payload Fairing Number of Solid Atlas V Size (meters) Rocket Boosters Flight/Configuration Key AV-XXX ### Number of Centaur Engines 3-digit Tail Number 3-digit Configuration Number LRO Overview LRO is the first mission in NASA’s planned return to the Moon. -
Protons in the Near Lunar Wake Observed by the SARA Instrument on Board Chandrayaan-1
FUTAANA ET AL. PROTONS IN DEEP WAKE NEAR MOON 1 Protons in the Near Lunar Wake Observed by the SARA 2 Instrument on Board Chandrayaan-1 3 Y. Futaana, 1 S. Barabash, 1 M. Wieser, 1 M. Holmström, 1 A. Bhardwaj, 2 M. B. Dhanya, 2 R. 4 Sridharan, 2 P. Wurz, 3 A. Schaufelberger, 3 K. Asamura 4 5 --- 6 Y. Futaana, Swedish Institute of Space Physics, Box 812, Kiruna, SE-98128, Sweden. 7 ([email protected]) 8 9 10 1 Swedish Institute of Space Physics, Box 812, Kiruna, SE-98128, Sweden 11 2 Space Physics Laboratory, Vikram Sarabhai Space Center, Trivandrum 695 022, India 12 3 Physikalisches Institut, University of Bern, Sidlerstrasse 5, CH-3012 Bern, Switzerland 13 4 Institute of Space and Astronautical Science, 3-1-1 Yoshinodai, Sagamihara, Japan 14 Index Terms 15 6250 Moon 16 5421 Interactions with particles and fields 17 2780 Magnetospheric Physics: Solar wind interactions with unmagnetized bodies 18 7807 Space Plasma Physics: Charged particle motion and acceleration 19 Abstract 20 Significant proton fluxes were detected in the near wake region of the Moon by an ion mass 21 spectrometer on board Chandrayaan-1. The energy of these nightside protons is slightly higher than 22 the energy of the solar wind protons. The protons are detected close to the lunar equatorial plane at 23 a 140˚ solar zenith angle, i.e., ~50˚ behind the terminator at a height of 100 km. The protons come 24 from just above the local horizon, and move along the magnetic field in the solar wind reference 25 frame. -
A Systematic Concept Exploration Methodology Applied to Venus in Situ Explorer
Session III: Probe Missions to the Giant Planets, Titan and Venus A Systematic Concept Exploration Methodology Applied to Venus In Situ Explorer Jarret M. Lafleur *, Gregory Lantoine *, Andrew L. Hensley *, Ghislain J. Retaureau *, Kara M. Kranzusch *, Joseph W. Hickman *, Marc N. Wilson *, and Daniel P. Schrage † Georgia Institute of Technology Atlanta, Georgia 30332 ABSTRACT One of the most critical tasks in the design of a complex system is the initial conversion of mission or program objectives into a baseline system architecture. Presented in this paper is a methodology to aid in this process that is frequently used for aerospace problems at the Georgia Institute of Technology. In this paper, the methodology is applied to initial concept formulation for the Venus In Situ Explorer (VISE) mission. Five primary steps are outlined which encompass program objective definition through evaluation of candidate designs. Tools covered include the Analytic Hierarchy Process (AHP), Technique for Order Preference by Similarity to Ideal Solution (TOPSIS), and morphological matrices. Direction is given for the application of modeling and simulation as well as for subsequent iterations of the process. The paper covers both theoretical and practical aspects of the tools and process in the context of the VISE example, and it is hoped that this methodology may find future use in interplanetary probe design. 1. INTRODUCTION One of the most critical tasks in the design of a complex engineering system is the initial conversion of mission or program objectives and requirements into a baseline system architecture. In completing this task, the challenge exists to comprehensively but efficiently explore the global trade space of potential designs. -
+ 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 -
Global Mapping of Elemental Abundance on Lunar Surface by SELENE Gamma-Ray Spectrometer
Lunar and Planetary Science XXXVI (2005) 2092.pdf Global Mapping of elemental abundance on lunar surface by SELENE gamma-ray spectrometer. 1M. -N. Kobayashi, 1A. A. Berezhnoy, 6C. d’Uston, 1M. Fujii, 1N. Hasebe, 3T. Hiroishi, 4H. Kaneko, 1T. Miyachi, 5K. Mori, 6S. Maurice, 4M. Nakazawa, 3K. Narasaki, 1O. Okudaira, 1E. Shibamura, 2T. Takashima, 1N. Yamashita, 1Advanced Research Institute of Sci.& Eng., Waseda Univ., 3-4-1, Okubo, Shinjuku-ku, Tokyo, 169-8555, Japan, (masa- [email protected]), 2Institute of Space and Astronautical Science, Japan Aerospace Exploration Agency, 3-1-1 Yoshinodai, Sagamihara, Kanagawa, 229-8510, 3Niihama Works, Sumitomo Heavy Industry Ltd., Niihama, Ehime, Japan, Moriya Works, 4Meisei Electric Co., Ltd., 3-249-1, Yuri-ga-oka, Moriya-shi, Ibaraki, 302-0192, 5Clear Pulse Co., 6-25-17, Chuo, Ohta-ku, Tokyo, Japan, 143-0024, 6Centre d’Etude Spatiale des Rayonnements, CNRS/UPS, Colonel Roche, B.P 4346, France. Introduction: Elemental composition on the sur- face of a planet is very important information for solv- ing the origin and the evolution of the planet and also very necessary for understanding the origin and the evolution of solar system. Planetary gamma-ray spec- troscopy is extremely powerful approach for the ele- mental composition measurement. Gamma-ray spec- trometer (GRS) will be on board SELENE, advanced lunar polar orbiter, and employ a large-volume Ge detector of 252cc as the main detector [1]. SELENE GRS is, therefore, approximately twice more sensitiv- ity than Lunar Prospector GRS, four times more sensi- Figure 1: The schematic drawing of SELENE Gamma- tive than APOLLO GRS. -
Investigating Mineral Stability Under Venus Conditions: a Focus on the Venus Radar Anomalies Erika Kohler University of Arkansas, Fayetteville
University of Arkansas, Fayetteville ScholarWorks@UARK Theses and Dissertations 5-2016 Investigating Mineral Stability under Venus Conditions: A Focus on the Venus Radar Anomalies Erika Kohler University of Arkansas, Fayetteville Follow this and additional works at: http://scholarworks.uark.edu/etd Part of the Geochemistry Commons, Mineral Physics Commons, and the The unS and the Solar System Commons Recommended Citation Kohler, Erika, "Investigating Mineral Stability under Venus Conditions: A Focus on the Venus Radar Anomalies" (2016). Theses and Dissertations. 1473. http://scholarworks.uark.edu/etd/1473 This Dissertation is brought to you for free and open access by ScholarWorks@UARK. It has been accepted for inclusion in Theses and Dissertations by an authorized administrator of ScholarWorks@UARK. For more information, please contact [email protected], [email protected]. Investigating Mineral Stability under Venus Conditions: A Focus on the Venus Radar Anomalies A dissertation submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy in Space and Planetary Sciences by Erika Kohler University of Oklahoma Bachelors of Science in Meteorology, 2010 May 2016 University of Arkansas This dissertation is approved for recommendation to the Graduate Council. ____________________________ Dr. Claud H. Sandberg Lacy Dissertation Director Committee Co-Chair ____________________________ ___________________________ Dr. Vincent Chevrier Dr. Larry Roe Committee Co-chair Committee Member ____________________________ ___________________________ Dr. John Dixon Dr. Richard Ulrich Committee Member Committee Member Abstract Radar studies of the surface of Venus have identified regions with high radar reflectivity concentrated in the Venusian highlands: between 2.5 and 4.75 km above a planetary radius of 6051 km, though it varies with latitude. -
Baltic-Show-2020» Cacib-Fci Интернациональная Выставка Собак «Балтик-Шоу-2020» Каталог
FÉDÉRATION CYNOLOGIQUE INTERNATIONALE RUSSIAN KINOLOGICAL FEDERATION МЕЖДУНАРОДНАЯ КИНОЛОГИЧЕСКАЯ ФЕДЕРАЦИЯ РОССИЙСКАЯ КИНОЛОГИЧЕСКАЯ ФЕДЕРАЦИЯ INTERNATIONAL DOG SHOW «BALTIC-SHOW-2020» CACIB-FCI ИНТЕРНАЦИОНАЛЬНАЯ ВЫСТАВКА СОБАК «БАЛТИК-ШОУ-2020» КАТАЛОГ 26.09.2020 Россия, Санкт-Петербург / Russia, Saint-Petersburg Организатор - КЦ «Северная Венеция», СПб, ул. Шаврова, 9-64 Место проведения - СПб, Петербургское ш., 64/1, ЭКСПОФОРУМ Organizer – CC «Severnaya Venetsiya», SPb,Shavrova st., 9-64 Location – SPb, Peterburgskoe sh., 64/1, EXPOFORUM 26.09.2020, КЦ «Северная Венеция», СПб, Интернациональная выставка собак «Балтик-Шоу-2020» (САСIB-FCI) 1 УВАЖАЕМЫЕ ГОСТИ И УЧАСТНИКИ ВЫСТАВКИ! Мы рады видеть на нашей выставке Мы желаем Вам успехов в рингах и хорошего настроения! МЕСТО ПРОВЕДЕНИЯ: СПб, Петербургское ш., 64/1, ЭКСПОФОРУМ ДАТА ПРОВЕДЕНИЯ: 26 сентября 2020 г. ОРГАНИЗАТОР: Санкт-Петербургская Регионгальная Общественная Организация Кинологический Центр «Северная Венеция» СПб, ул. Шаврова, 9-64, тел. 8-905-215-15-35, E-mail: sony-boni@mailru ОРГКОМИТЕТ: Коврова И. (Председатель оргкомитета) Ларина Е., Иванова Н., Кирина А., Симакова М., Хвостина В. СУДЬИ: Ринг 1. Реваз Хомасуридзе (Россия) / Revaz Khomasuridze (Russia) Ринг 2. Лариса Галиаскарова (Россия) / Larisa Galiaskarova (Russia) Ринг 3. Олег Васильев (Россия) / Oleg Vasiliev (Russia) Ринг 4. Душан Паунович (Cербия) / Dusan Paunovic (Serbia) Ринг 5. Виктор Лобакин (Азербайджан) / Victor Lobakin (Azerbaijan) Ринг 6. Дмитрий Прозоров (Россия) / Dmitry Prozorov (Russia) Ринг 7. Марина Коваленко (Россия) / Marina Kovalenko (Russia) СТАЖЕРЫ: Егорова О., Тёниг М. Начало регистрации участников выставки в 8:00 Начало конкурса ЮНЫЙ ХЕНДЛЕР в 16:30 на главном ринге Эксперт / Judge : Дмитрий Прозоров (Россия) / Dmitry Prozorov (Russia) 1. Андреева Таисия, 13 лет, вельш корги кардиган 2. Баранова Александра, 13 лет, сибирский хаски 3. -
The Magellan Spacecraft at Venus by Andrew Fraknoi, Astronomical Society of the Pacific
www.astrosociety.org/uitc No. 18 - Fall 1991 © 1991, Astronomical Society of the Pacific, 390 Ashton Avenue, San Francisco, CA 94112. The Magellan Spacecraft at Venus by Andrew Fraknoi, Astronomical Society of the Pacific "Having finally penetrated below the clouds of Venus, we find its surface to be naked [not hidden], revealing the history of hundreds of millions of years of geological activity. Venus is a geologist's dream planet.'' —Astronomer David Morrison This fall, the brightest star-like object you can see in the eastern skies before dawn isn't a star at all — it's Venus, the second closest planet to the Sun. Because Venus is so similar in diameter and mass to our world, and also has a gaseous atmosphere, it has been called the Earth's "sister planet''. Many years ago, scientists expected its surface, which is perpetually hidden beneath a thick cloud layer, to look like Earth's as well. Earlier this century, some people even imagined that Venus was a hot, humid, swampy world populated by prehistoric creatures! But we now know Venus is very, very different. New radar images of Venus, just returned from NASA's Magellan spacecraft orbiting the planet, have provided astronomers the clearest view ever of its surface, revealing unique geological features, meteor impact craters, and evidence of volcanic eruptions different from any others found in the solar system. This issue of The Universe in the Classroom is devoted to what Magellan is teaching us today about our nearest neighbor, Venus. Where is Venus, and what is it like? Spacecraft exploration of Venus's surface Magellan — a "recycled'' spacecraft How does Magellan take pictures through the clouds? What has Magellan revealed about Venus? How does Venus' surface compare with Earth's? What is the next step in Magellan's mission? If Venus is such an uninviting place, why are we interested in it? Reading List Why is it so hot on Venus? Where is Venus, and what is it like? Venus orbits the Sun in a nearly circular path between Mercury and the Earth, about 3/4 as far from our star as the Earth is.