THERMAL MODELING and DESIGN of a MICRO-ROVER for LUNAR POLAR EXPLORATION Virtual Conference 19–23 October 2020 Paulo R.M
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The Surrender Software
Scientific image rendering for space scenes with the SurRender software Scientific image rendering for space scenes with the SurRender software R. Brochard, J. Lebreton*, C. Robin, K. Kanani, G. Jonniaux, A. Masson, N. Despré, A. Berjaoui Airbus Defence and Space, 31 rue des Cosmonautes, 31402 Toulouse Cedex, France [email protected] *Corresponding Author Abstract The autonomy of spacecrafts can advantageously be enhanced by vision-based navigation (VBN) techniques. Applications range from manoeuvers around Solar System objects and landing on planetary surfaces, to in -orbit servicing or space debris removal, and even ground imaging. The development and validation of VBN algorithms for space exploration missions relies on the availability of physically accurate relevant images. Yet archival data from past missions can rarely serve this purpose and acquiring new data is often costly. Airbus has developed the image rendering software SurRender, which addresses the specific challenges of realistic image simulation with high level of representativeness for space scenes. In this paper we introduce the software SurRender and how its unique capabilities have proved successful for a variety of applications. Images are rendered by raytracing, which implements the physical principles of geometrical light propagation. Images are rendered in physical units using a macroscopic instrument model and scene objects reflectance functions. It is specially optimized for space scenes, with huge distances between objects and scenes up to Solar System size. Raytracing conveniently tackles some important effects for VBN algorithms: image quality, eclipses, secondary illumination, subpixel limb imaging, etc. From a user standpoint, a simulation is easily setup using the available interfaces (MATLAB/Simulink, Python, and more) by specifying the position of the bodies (Sun, planets, satellites, …) over time, complex 3D shapes and material surface properties, before positioning the camera. -
Report Resumes
REPORT RESUMES ED 019 218 88 SE 004 494 A RESOURCE BOOK OF AEROSPACE ACTIVITIES, K-6. LINCOLN PUBLIC SCHOOLS, NEBR. PUB DATE 67 EDRS PRICEMF.41.00 HC-S10.48 260P. DESCRIPTORS- *ELEMENTARY SCHOOL SCIENCE, *PHYSICAL SCIENCES, *TEACHING GUIDES, *SECONDARY SCHOOL SCIENCE, *SCIENCE ACTIVITIES, ASTRONOMY, BIOGRAPHIES, BIBLIOGRAPHIES, FILMS, FILMSTRIPS, FIELD TRIPS, SCIENCE HISTORY, VOCABULARY, THIS RESOURCE BOOK OF ACTIVITIES WAS WRITTEN FOR TEACHERS OF GRADES K-6, TO HELP THEM INTEGRATE AEROSPACE SCIENCE WITH THE REGULAR LEARNING EXPERIENCES OF THE CLASSROOM. SUGGESTIONS ARE MADE FOR INTRODUCING AEROSPACE CONCEPTS INTO THE VARIOUS SUBJECT FIELDS SUCH AS LANGUAGE ARTS, MATHEMATICS, PHYSICAL EDUCATION, SOCIAL STUDIES, AND OTHERS. SUBJECT CATEGORIES ARE (1) DEVELOPMENT OF FLIGHT, (2) PIONEERS OF THE AIR (BIOGRAPHY),(3) ARTIFICIAL SATELLITES AND SPACE PROBES,(4) MANNED SPACE FLIGHT,(5) THE VASTNESS OF SPACE, AND (6) FUTURE SPACE VENTURES. SUGGESTIONS ARE MADE THROUGHOUT FOR USING THE MATERIAL AND THEMES FOR DEVELOPING INTEREST IN THE REGULAR LEARNING EXPERIENCES BY INVOLVING STUDENTS IN AEROSPACE ACTIVITIES. INCLUDED ARE LISTS OF SOURCES OF INFORMATION SUCH AS (1) BOOKS,(2) PAMPHLETS, (3) FILMS,(4) FILMSTRIPS,(5) MAGAZINE ARTICLES,(6) CHARTS, AND (7) MODELS. GRADE LEVEL APPROPRIATENESS OF THESE MATERIALSIS INDICATED. (DH) 4:14.1,-) 1783 1490 ,r- 6e tt*.___.Vhf 1842 1869 LINCOLN PUBLICSCHOOLS A RESOURCEBOOK OF AEROSPACEACTIVITIES U.S. DEPARTMENT OF HEALTH, EDUCATION & WELFARE OFFICE OF EDUCATION K-6) THIS DOCUMENT HAS BEEN REPRODUCED EXACTLY AS RECEIVED FROM THE PERSON OR ORGANIZATION ORIGINATING IT.POINTS OF VIEW OR OPINIONS STATED DO NOT NECESSARILY REPRESENT OFFICIAL OFFICE OF EDUCATION POSITION OR POLICY. 1919 O O Vj A PROJECT FUNDED UNDER TITLE HIELEMENTARY AND SECONDARY EDUCATION ACT A RESOURCE BOOK OF AEROSPACE ACTIVITIES (K-6) The work presentedor reported herein was performed pursuant to a Grant from the U. -
Project Selene: AIAA Lunar Base Camp
Project Selene: AIAA Lunar Base Camp AIAA Space Mission System 2019-2020 Virginia Tech Aerospace Engineering Faculty Advisor : Dr. Kevin Shinpaugh Team Members : Olivia Arthur, Bobby Aselford, Michel Becker, Patrick Crandall, Heidi Engebreth, Maedini Jayaprakash, Logan Lark, Nico Ortiz, Matthew Pieczynski, Brendan Ventura Member AIAA Number Member AIAA Number And Signature And Signature Faculty Advisor 25807 Dr. Kevin Shinpaugh Brendan Ventura 1109196 Matthew Pieczynski 936900 Team Lead/Operations Logan Lark 902106 Heidi Engebreth 1109232 Structures & Environment Patrick Crandall 1109193 Olivia Arthur 999589 Power & Thermal Maedini Jayaprakash 1085663 Robert Aselford 1109195 CCDH/Operations Michel Becker 1109194 Nico Ortiz 1109533 Attitude, Trajectory, Orbits and Launch Vehicles Contents 1 Symbols and Acronyms 8 2 Executive Summary 9 3 Preface and Introduction 13 3.1 Project Management . 13 3.2 Problem Definition . 14 3.2.1 Background and Motivation . 14 3.2.2 RFP and Description . 14 3.2.3 Project Scope . 15 3.2.4 Disciplines . 15 3.2.5 Societal Sectors . 15 3.2.6 Assumptions . 16 3.2.7 Relevant Capital and Resources . 16 4 Value System Design 17 4.1 Introduction . 17 4.2 Analytical Hierarchical Process . 17 4.2.1 Longevity . 18 4.2.2 Expandability . 19 4.2.3 Scientific Return . 19 4.2.4 Risk . 20 4.2.5 Cost . 21 5 Initial Concept of Operations 21 5.1 Orbital Analysis . 22 5.2 Launch Vehicles . 22 6 Habitat Location 25 6.1 Introduction . 25 6.2 Region Selection . 25 6.3 Locations of Interest . 26 6.4 Eliminated Locations . 26 6.5 Remaining Locations . 27 6.6 Chosen Location . -
Modification of the Lunar Surface Composition by Micro-Meteorite Impact Vaporization and Sputtering
EPSC Abstracts Vol. 13, EPSC-DPS2019-705-1, 2019 EPSC-DPS Joint Meeting 2019 c Author(s) 2019 Modification of the lunar surface composition by micro-meteorite impact vaporization and sputtering Audrey Vorburger (1), Peter Wurz (1), André Galli (1), Manuel Scherf (2), and Helmut Lammer (2) (1) Physikalisches Institut, University of Bern, Bern, Switzerland ([email protected]), (2) Space Research Institute, Austrian Academy of Sciences, Graz, Austria Abstract Late Heavy Bombardment model with a half-life time of 100 Myr. Time steps vary between 25 Myr (at the Over the past 4.5 billion years the Moon has been un- beginning) and 560 Myr (today). der constant bombardment by solar wind particles and The only required inputs for this study are the orig- micro-meteorites. These impactors liberate surface inal surface composition, the solar wind particle flux, material into space, and, over time, result in a modi- the solar UV flux, and the micro-meteorite impact rate. fication of the surface composition due to the species’ For the surface composition we implement at t=0 (at different loss rates. Here we model the loss of the the beginning) the BSE composition according to [3]. 7 major lunar surface elements over the past 4.5 bil- We run the simulations for O, Mg, Si, Fe, Al, Ca, and lion years and show how the lunar surface composition K, which together make up more than 99% of today’s changed over time. lunar soil [4]. After each time step we compute for each species the fraction lost from the lunar regolith, 1. -
Lunar Soil This Is Supplemented by Lunar Ice, Which Provides Hydrogen, Carbon and Nitrogen (Plus Many Other Elements)
Resources for 3D Additive Construction on the Moon, Asteroids and Mars Philip Metzger University of Central Florida The Moon Resources for 3D Additive Construction on 2 the Moon, Mars and Asteroids The Moon’s Resources • Sunlight • Regolith • Volatiles • Exotics – Asteroids? – Recycled spacecraft • Derived resources • Vacuum Resources for 3D Additive Construction on 3 the Moon, Mars and Asteroids Global Average Elemental Composition Elemental composition of Lunar Soil This is supplemented by lunar ice, which provides Hydrogen, Carbon and Nitrogen (plus many other elements) Resources for 3D Additive Construction on 4 the Moon, Mars and Asteroids Terminology • Regolith: broken up rocky material that blankets a planet, including boulders, gravel, sand, dust, and any organic material • Lunar Soil: regolith excluding pieces larger than about 1 cm – On Earth, when we say “soil” we mean material that has organic content – By convention “lunar soil” is valid terminology even though it has no organic content • Lunar Dust: the fraction of regolith smaller than about 20 microns (definitions vary) • Lunar geology does not generally separate these Resources for 3D Additive Construction on 5 the Moon, Mars and Asteroids Regolith Formation • Impacts are the dominant geological process • Larger impacts (asteroids & comets) – Fracture bedrock and throw out ejecta blankets – Mix regolith laterally and in the vertical column • Micrometeorite gardening – Wears down rocks into soil – Makes the soil finer – Creates glass and agglutinates – Creates patina on -
Planning a Mission to the Lunar South Pole
Lunar Reconnaissance Orbiter: (Diviner) Audience Planning a Mission to Grades 9-10 the Lunar South Pole Time Recommended 1-2 hours AAAS STANDARDS Learning Objectives: • 12A/H1: Exhibit traits such as curiosity, honesty, open- • Learn about recent discoveries in lunar science. ness, and skepticism when making investigations, and value those traits in others. • Deduce information from various sources of scientific data. • 12E/H4: Insist that the key assumptions and reasoning in • Use critical thinking to compare and evaluate different datasets. any argument—whether one’s own or that of others—be • Participate in team-based decision-making. made explicit; analyze the arguments for flawed assump- • Use logical arguments and supporting information to justify decisions. tions, flawed reasoning, or both; and be critical of the claims if any flaws in the argument are found. • 4A/H3: Increasingly sophisticated technology is used Preparation: to learn about the universe. Visual, radio, and X-ray See teacher procedure for any details. telescopes collect information from across the entire spectrum of electromagnetic waves; computers handle Background Information: data and complicated computations to interpret them; space probes send back data and materials from The Moon’s surface thermal environment is among the most extreme of any remote parts of the solar system; and accelerators give planetary body in the solar system. With no atmosphere to store heat or filter subatomic particles energies that simulate conditions in the Sun’s radiation, midday temperatures on the Moon’s surface can reach the stars and in the early history of the universe before 127°C (hotter than boiling water) whereas at night they can fall as low as stars formed. -
Rare Astronomical Sights and Sounds
Jonathan Powell Rare Astronomical Sights and Sounds The Patrick Moore The Patrick Moore Practical Astronomy Series More information about this series at http://www.springer.com/series/3192 Rare Astronomical Sights and Sounds Jonathan Powell Jonathan Powell Ebbw Vale, United Kingdom ISSN 1431-9756 ISSN 2197-6562 (electronic) The Patrick Moore Practical Astronomy Series ISBN 978-3-319-97700-3 ISBN 978-3-319-97701-0 (eBook) https://doi.org/10.1007/978-3-319-97701-0 Library of Congress Control Number: 2018953700 © Springer Nature Switzerland AG 2018 This work is subject to copyright. All rights are reserved by the Publisher, whether the whole or part of the material is concerned, specifically the rights of translation, reprinting, reuse of illustrations, recitation, broadcasting, reproduction on microfilms or in any other physical way, and transmission or information storage and retrieval, electronic adaptation, computer software, or by similar or dissimilar methodology now known or hereafter developed. The use of general descriptive names, registered names, trademarks, service marks, etc. in this publication does not imply, even in the absence of a specific statement, that such names are exempt from the relevant protective laws and regulations and therefore free for general use. The publisher, the authors, and the editors are safe to assume that the advice and information in this book are believed to be true and accurate at the date of publication. Neither the publisher nor the authors or the editors give a warranty, express or implied, with respect to the material contained herein or for any errors or omissions that may have been made. -
Moon Minerals a Visual Guide
Moon Minerals a visual guide A.G. Tindle and M. Anand Preliminaries Section 1 Preface Virtual microscope work at the Open University began in 1993 meteorites, Martian meteorites and most recently over 500 virtual and has culminated in the on-line collection of over 1000 microscopes of Apollo samples. samples available via the virtual microscope website (here). Early days were spent using LEGO robots to automate a rotating microscope stage thanks to the efforts of our colleague Peter Whalley (now deceased). This automation speeded up image capture and allowed us to take the thousands of photographs needed to make sizeable (Earth-based) virtual microscope collections. Virtual microscope methods are ideal for bringing rare and often unique samples to a wide audience so we were not surprised when 10 years ago we were approached by the UK Science and Technology Facilities Council who asked us to prepare a virtual collection of the 12 Moon rocks they loaned out to schools and universities. This would turn out to be one of many collections built using extra-terrestrial material. The major part of our extra-terrestrial work is web-based and we The authors - Mahesh Anand (left) and Andy Tindle (middle) with colleague have build collections of Europlanet meteorites, UK and Irish Peter Whalley (right). Thank you Peter for your pioneering contribution to the Virtual Microscope project. We could not have produced this book without your earlier efforts. 2 Moon Minerals is our latest output. We see it as a companion volume to Moon Rocks. Members of staff -
Cuberover Luxembourg PR Final
For Immediate Release Contact for CubeRover: John Walk Moosbruger [email protected] +1 (216) 906-2393 Contact for Astrobotic: Carolyn Pace [email protected] +1 (412) 682-3282 Contact for the Luxembourg Ministry of the Economy: Paul Zenners [email protected] (+352) 288 482-24 CubeRover to Develop Next Generation Planetary Rovers in Luxembourg CubeRover Platform to Revolutionize Lunar Access and Capability for Companies, Governments, Universities, and Non-Profits September 27, 2018 Luxembourg City, Luxembourg - CubeRover SARL (CubeRover) and Luxembourg announce today the agreement for the development of next-generation planetary rovers in Luxembourg. This historic agreement marks the establishment of CubeRover’s operations in the Grand Duchy as a spin out organization from Astrobotic Technology, Inc. (Astrobotic), a space robotics company based in Pittsburgh, Pennsylvania, USA. Astrobotic developed the CubeRover platform in partnership with Carnegie Mellon University under a NASA technology development contract at NASA’s Kennedy Space Center. The platform was developed to create low-cost, mobile robotic lunar access for companies, governments, universities and non-profits across the world. !1 The new headquarters in Luxembourg will be a hub for planetary rover design, manufacture, and assembly, as well as a one-stop shop for customers around the world to begin their planetary rover exploration programs. ! The CubeRover will revolutionize low mobile robotic access on the Moon. “We are excited to launch CubeRover in the Grand Duchy and enable customers around the world to begin pursuing lunar science, exploration, and commerce with their own low-cost rovers. The Ministry of the Economy and the newly established Luxembourg Space Agency have been terrific partners and great believers in CubeRover’s vision of opening access to the lunar surface,” says Mike Provenzano, President of CubeRover. -
Icebreaker: a Lunar South Pole Exploring Robot Cmu-Ri-Tr-97-22
ICEBREAKER: A LUNAR SOUTH POLE EXPLORING ROBOT CMU-RI-TR-97-22 Matthew C. Deans Alex D. Foessel Gregory A. Fries Diana LaBelle N. Keith Lay Stewart Moorehead Ben Shamah Kimberly J. Shillcutt Professor: Dr. William Whittaker The Robotics Institute Carnegie Mellon University Pittsburgh PA 15213 Spring 1996-97 Executive Summary Icebreaker: A Lunar South Pole Exploring Robot Due to the low angles of sunlight at the lunar poles, craters and other depressions in the polar regions can contain areas which are in permanent darkness and are at cryogenic temperatures. Many scientists have theorized that these cold traps could contain large quantities of frozen volatiles such as water and carbon dioxide which have been deposited over billions of years by comets, meteors and solar wind. Recent bistatic radar data from the Clementine mission has yielded results consistent with water ice at the South Pole of the Moon however Earth based observations from the Arecibo Radar Observatory indicate that ice may not exist. Due to the controversy surrounding orbital and Earth based observations, the only way to definitively answer the question of whether ice exists on the Lunar South Pole is in situ analysis. The discovery of water ice and other volatiles on the Moon has many important benefits. First, this would provide a source of rocket fuel which could be used to power rockets to Earth, Mars or beyond, avoiding the high cost of Earth based launches. Secondly, water and carbon dioxide along with nitrogen from ammonia form the essential elements for life and could be used to help support human colonies on the Moon. -
Lunar and Planetary Science XXXII (2001) 1074.Pdf
Lunar and Planetary Science XXXII (2001) 1074.pdf VOYAGER IMAGES REVISITED: NEW VIEWS OF THE SATELLITES OF SATURN AND URANUS. P. J. Stooke1, 1Department of Geography, University of Western Ontario, London, Ontario, Canada N6A 5C2; [email protected]; www.uwo.ca/geog/faculty/stooke.htm Introduction: Voyager images of Saturn and its near the sub-Uranus point. At top near the planetshine moons are 20 years old, and images of the Uranian sys- terminator, the sinuous graben complex Kachina Chas- tem are 15 years old. Although much was learned from mata extends far into the northern hemisphere, possibly them, more may still be done using recent image proc- to the far limb. Additional details may be revealed by essing methods. Here I present results of a program of better noise removal. Unfortunately, few other Uranus reprocessing of images of the icy satellites of these two satellite images show useful details in planetshine. planets. Highlights include the identification of fea- Either the satellite is too far from the planet, and so tures illuminated by planetshine on the northern hemi- more weakly illuminated, or the ‘dark’ side is seen only sphere of Ariel, enigmatic markings on Enceladus and very obliquely in low phase angle views. the identification of new features on Rhea and Umbriel. This program will result in new maps of the Saturnian satellites in time for Cassini’s arrival. Images and Processing: This study makes use of all available images from the PDS Ring Node archive. An interesting observation, which this program will rectify, is that the USGS maps of all these satellites do not make full use of the image sets. -
The Peaks of Eternal Light
The Peaks of Eternal Light: a Near-term Property Issue on the Moon Martin Elvis a,1, Tony Milligan b, Alanna Krolikowskic a Harvard-Smithsonian Center for Astrophysics, 60 Garden St., Cambridge MA 02138, USA; [email protected]; b Department of Theology and Religious Studies, King’s College London, Virginia Wolf Building, 22 Kingsway, London WC2B 6NR. c Georg-August Universität Göttingen, Heinrich-Düker-Weg 14, 37073, Göttingen, Germany; [email protected] ABSTRACT The Outer Space Treaty makes it clear that the Moon is the ‘province of all mankind’, with the latter ordinarily understood to exclude state or private appropriation of any portion of its surface. However, there are indeterminacies in the Treaty and in space law generally over the issue of appropriation. These indeterminacies might permit a close approximation to a property claim or some manner of ‘quasi-property’. The recently revealed highly inhomogeneous distribution of lunar resources changes the context of these issues. We illustrate this altered situation by considering the Peaks of Eternal Light. They occupy about one square kilometer of the lunar surface. We consider a thought experiment in which a Solar telescope is placed on one of the Peaks of Eternal Light at the lunar South pole for scientific research. Its operation would require non- disturbance, and hence that the Peak remain unvisited by others, effectively establishing a claim of protective exclusion and de facto appropriation. Such a telescope would be relatively easy to emplace with today’s technology and so poses a near-term property issue on the Moon. While effective appropriation of a Peak might proceed without raising some of the familiar problems associated with commercial development (especially lunar mining), the possibility of such appropriation nonetheless raises some significant issues concerning justice and the safeguarding of scientific practice on the lunar surface.