Model Development and Testing for Themis Controlled Mars Mosaics

Total Page:16

File Type:pdf, Size:1020Kb

Model Development and Testing for Themis Controlled Mars Mosaics Lunar and Planetary Science XXXVI (2005) 2052.pdf MODEL DEVELOPMENT AND TESTING FOR THEMIS CONTROLLED MARS MOSAICS. B. A. Ar- chinal1, S. Sides1, L. Weller1, G. Cushing1, T. Titus1, R. L. Kirk1, L. A. Soderblom1, and T. C. Duxbury2, 1U. S. Geological Survey (2255 N. Gemini Drive, Flagstaff, AZ 86001, USA, [email protected]), 2Jet Propulsion Labo- ratory (4800 Oak Grove Drive, M/S: 264-379, Pasadena, CA 91109, USA, [email protected]). Introduction: As part of our work [1] to develop tech- orientation while the line scanner image is being collected, niques and procedures to create regional and eventually thus [4, pp. 290-291]: global THEMIS mosaics of Mars, we are developing algo- ⎡ 2⎤ X 0 + X1(t − tR ) + X 2 (t −t ) rithms and software to photogrammetrically control ⎡X s ⎤ ⎢ R ⎥ ⎢ ⎥ 2 , THEMIS IR line scanner camera images. We have found Y = ⎢ Y + Y (t − t ) + Y (t −t ) ⎥ from comparison of a limited number of images to MOLA ⎢ s ⎥ ⎢ 0 1 R 2 R ⎥ ⎢Z ⎥ 2 digital image models (DIMs) [2] that the a priori geometry ⎣ s ⎦ ⎢ Z + Z (t − t ) + Z (t −t ) ⎥ ⎢ 0 1 R 2 R ⎥ information (i.e. SPICE [3]) for THEMIS images generally ⎣ ⎦ allows their relative positions to be specified at the several ⎡ 2⎤ αˆ +αˆ (t − t ) +αˆ (t −t ) pixel level (e.g. ~5 to 13 pixels). However a need for con- ⎡αˆ⎤ ⎢ 0 1 R 2 R ⎥ 2 , trolled solutions to improve this geometry to the sub-pixel ⎢ ˆ⎥ ⎢ ˆ ˆ ˆ ⎥ δ = δ0 + δ1(t − tR ) + δ 2 (t −t ) level still exists. Only with such solutions can seamless ⎢ ⎥ ⎢ R ⎥ ⎢κ ⎥ 2 mosaics be obtained and likely distortion from spacecraft ⎣ ⎦ ⎢κ + κ (t − t ) + κ (t −t ) ⎥ ⎣⎢ 0 1 R 2 R ⎦⎥ motion during image collection removed at such levels. Past experience has shown clearly that such mosaics are in heavy where X0, Y0, and Z0 is the position of the spacecraft at some demand by users for operational and scientific use, and that reference time tR, e.g. the time of the central line of a particu- they are needed over large areas or globally (as opposed to lar image. Similarly, the camera orientation at that moment being available only on a limited basis via labor intensive is given by the J2000.0 right ascension and declina- custom mapping projects). Uses include spacecraft naviga- ˆ ˆ tionαˆ0 ,δ 0 , and twist angleκ0 . Xs, Ys, Zs,αˆ , δ , and tion, landing site planning and mapping, registration of mul- tiple data types and image sets, registration of multispectral κ are the corresponding values at the time t of any line in images, registration of images with topographic information, the image. To allow for unknown variations in the space- recovery of thermal properties, change detection searches, craft position and orientation while the image is being ob- etc. tained, we will solve for some or all of the additional un- knowns shown. Algorithms for Adjustment of THEMIS IR images: Procedures for the photogrammetric adjustment of standard Of course, with such a technique there are still a number framing camera (e.g. using film or electronic detectors such of additional issues that must be addressed. For example, as vidicons or areal CCDs) have been well developed, ini- this procedure could result in up to 9 additional parameters tially for terrestrial photogrammetry [4], but also since the for positions (3 in position, velocity, and acceleration) and 6 1970’s for planetary photogrammetry [5]. Attempts at pho- in orientation (3 in both velocity and acceleration, in addition togrammetric adjustments using line-scanner camera images to the 3 orientation angles) per image. If an image is in some however are fairly recent, having first been developed for way collected discontinuously – e.g. due to data dropouts or terrestrial aerial and orbital uses in the 1980’s and ‘90’s [6], sudden spacecraft motion – additional sets of parameters will and for limited mapping with Mars Orbiter Camera (MOC) also need to be determined for each image segment. To narrow angle images in the last few years [7]. However, solve for such additional parameters, additional tie points general procedures for handling such images and particularly will indeed be needed between overlapping images. THEMIS IR images have not yet been developed and are Additional effort will also be needed to estimate the a now the focus of our work. priori values of the polynomial parameters, based on the Our adjustment procedure is based primarily on an ex- initial estimates of exterior orientation (derived from the tension of the techniques and software used for the adjust- input SPICE data). ment of framing camera image measurements, e.g. those The polynomial parameters will also likely be highly developed at RAND and currently used at USGS [8]. The correlated. In fact, in our past planetary mapping photo- fundamental difference with line scanner images vs. framing grammetric solutions [5, 8], spacecraft position has always camera images is that the camera position and orientation been held fixed and never been solved for along with space- must be determined at the exposure of every line, rather than craft orientation, since for the relatively narrow angle cam- more simply at the exposure of every image. Obviously a eras in use, these parameters are highly correlated. It will be direct extension of solving independently for such informa- necessary to address these correlations – so that a solution tion (exterior orientation) at every line of a line scanner cam- can be achieved – by weighting the polynomial parameters era, even assuming a much larger number of image tie point based on realistic accuracy estimates for the a priori exterior measurements were available, would result in an underde- orientation information (e.g. orbit position and camera point- termined system of equations. As has been done in terres- ing accuracy). We will also experiment with various image trial mapping [6] we therefore propose to reduce the number sets in order to determine the usefulness of solving for the of parameters required for a solution to a reasonable level, higher order parameters, e.g. spacecraft acceleration and by solving for simple polynomial expressions for the exterior orientation acceleration. It is likely that for many solutions, e.g. with images that do not cover substantial arcs along the Lunar and Planetary Science XXXVI (2005) 2052.pdf planetary surface, the full parameterization will not be any given pair of images. Different matching algorithms needed in order to obtain sub-pixel accuracy. might be used, e.g. for different instruments, area matching, Current testing. We are currently completing the man- point of interest matching, texture matching, feature match- ual measurement of tie points (using ISIS qmatch) [9] for a ing (craters), etc. A third part will be the automatic rejection number of THEMIS IR images covering the two MER land- of outliers to the photogrammetric adjustment software, in ing site ellipses. We also plan to work on one additional area order to minimize or even eliminate manual checking of tie (such as any prime Phoenix landing site ellipse). We are point measurements. making a dense set of tie point measurements between a few In large photogrammetric solutions (e.g. with tens of pairs of images in order to ascertain the best initial set of thousands or more of measures, images, and parameters) the parameters, weights to be used and numbers of tie points method of conjugate gradients [10] can be used to complete needed for image pairs. Tie points are also being measured solutions. However a better solution method would be true between the THEMIS images and MOLA DIMs in order to block adjustment solutions, i.e. solutions where image cov- provide absolute control for the images (at least at the ~100 erage is broken into regions and correlations between regions m (~1 THEMIS IR pixel) accuracy of the MOLA data [2]. (except for image overlap between regions) are ignored. Once photogrammetric solutions are successfully completed, This would reduce the solution round-off error, and allow for we will use the updated exterior orientation information nested (blocked) matrix inversion solutions. The latter could (updated SPICE) in ISIS to generate controlled mosaics of provide any desired parameter uncertainties, and possibly these areas, both to assist in the final evaluation of our tech- provide for faster solutions (vs. conjugate gradient solu- niques and as useful products for use in the study of these tions). sites. So scaling up solutions from using a few images to re- Future development. An immediate goal of this work gional or global datasets is still an area that needs thus, to be will be to demonstrate the control of THEMIS IR to addressed. However, the basic adjustment procedures (de- THEMIS VIS images by adjustment of a limited set of VIS scribed here) and the likely necessary block adjustment tech- images to the IR mosaics. This will assist in the evaluation niques are tractable. Beyond this, the significant issues that of such a line scanner to framing camera image adjustment will require future attention are developing reliable auto- technique and also provide absolutely controlled VIS mosa- matic tie pointing procedures – to provide the measurement ics of these areas. Later we also hope to demonstrate the use input to the solutions – and to handle the sheer volume of of this technique to adjust other types of images and combi- images and measurements involved. nations of images, such as THEMIS IR band to band, Summary: We are in the process of developing the al- THEMIS IR to other framing camera images (e.g. Viking), gorithms and software to make controlled mosaics of Mars Express HSRC images, Mars Reconnaissance orbiter THEMIS IR images.
Recommended publications
  • Jjmonl 1603.Pmd
    alactic Observer GJohn J. McCarthy Observatory Volume 9, No. 3 March 2016 GRAIL - On the Trail of the Moon's Missing Mass GRAIL (Gravity Recovery and Interior Laboratory) was a NASA scientific mission in 2011/12 to map the surface of the moon and collect data on gravitational anomalies. The image here is an artist's impres- sion of the twin satellites (Ebb and Flow) orbiting in tandem above a gravitational image of the moon. See inside, page 4 for information on gravitational anomalies (mascons) or visit http://solarsystem. nasa.gov/grail. The John J. McCarthy Observatory Galactic Observer New Milford High School Editorial Committee 388 Danbury Road Managing Editor New Milford, CT 06776 Bill Cloutier Phone/Voice: (860) 210-4117 Production & Design Phone/Fax: (860) 354-1595 www.mccarthyobservatory.org Allan Ostergren Website Development JJMO Staff Marc Polansky It is through their efforts that the McCarthy Observatory Technical Support has established itself as a significant educational and Bob Lambert recreational resource within the western Connecticut Dr. Parker Moreland community. Steve Barone Jim Johnstone Colin Campbell Carly KleinStern Dennis Cartolano Bob Lambert Mike Chiarella Roger Moore Route Jeff Chodak Parker Moreland, PhD Bill Cloutier Allan Ostergren Cecilia Dietrich Marc Polansky Dirk Feather Joe Privitera Randy Fender Monty Robson Randy Finden Don Ross John Gebauer Gene Schilling Elaine Green Katie Shusdock Tina Hartzell Paul Woodell Tom Heydenburg Amy Ziffer In This Issue "OUT THE WINDOW ON YOUR LEFT" ............................... 4 SUNRISE AND SUNSET ...................................................... 13 MARE HUMBOLDTIANIUM AND THE NORTHEAST LIMB ......... 5 JUPITER AND ITS MOONS ................................................. 13 ONE YEAR IN SPACE ....................................................... 6 TRANSIT OF JUPITER'S RED SPOT ....................................
    [Show full text]
  • Grail): Extended Mission and Endgame Status
    44th Lunar and Planetary Science Conference (2013) 1777.pdf GRAVITY RECOVERY AND INTERIOR LABORATORY (GRAIL): EXTENDED MISSION AND ENDGAME STATUS. Maria T. Zuber1, David E. Smith1, Sami W. Asmar2, Alexander S. Konopliv2, Frank G. Lemoine3, H. Jay Melosh4, Gregory A. Neumann3, Roger J. Phillips5, Sean C. Solomon6,7, Michael M. Watkins2, Mark A. Wieczorek8, James G. Williams2, Jeffrey C. Andrews-Hanna9, James W. Head10, Wal- ter S. Kiefer11, Isamu Matsuyama12, Patrick J. McGovern11, Francis Nimmo13, G. Jeffrey Taylor14, Renee C. Weber15, Sander J. Goossens16, Gerhard L. Kruizinga2, Erwan Mazarico3, Ryan S. Park2 and Dah-Ning Yuan2. 1Dept. of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 02129, USA ([email protected]); 2Jet Propulsion Laboratory, California Institute of Technol- ogy, Pasadena, CA 91109, USA; 3NASA Goddard Space Flight Center, Greenbelt, MD 20771, USA; 4Dept. of Earth and Atmospheric Sciences, Purdue University, West Lafayette, IN 47907, USA; 5Planetary Science Directorate, Southwest Research Institute, Boulder, CO 80302, USA; 6 Lamont-Doherty Earth Observatory, Columbia University, Palisades, NY 10964, USA; 7Dept. of Terrestrial Magnetism, Carnegie Institution of Washington, Washington, DC 20015, USA; 8Institut de Physique du Globe de Paris, 94100 Saint Maur des Fossés, France; 9Dept. of Geophysics and Center for Space Resources, Colorado School of Mines, Golden, CO 80401, USA; 10Dept. of Geological Sciences, Brown University, Providence, RI 02912, USA; 11Lunar and Planetary Institute, Houston, TX 77058, USA; 12Lunar and Planetary Laborato- ry, University of Arizona, Tucson, AZ 85721, USA; 13Dept. of Earth and Planetary Sciences, University of California, Santa Cruz, CA 95064, USA; 14Hawaii Institute of Geophysics and Planetology, University of Hawaii, Honolulu, HI 96822, USA; 15NASA Marshall Space Flight Center, Huntsville, AL 35805, USA, 16University of Maryland, Baltimore County, Baltimore, MD 21250, USA.
    [Show full text]
  • 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.
    [Show full text]
  • Reviewing the Contribution of GRAIL to Lunar Science and Planetary Missions Maria T
    EPSC Abstracts Vol. 12, EPSC2018-575, 2018 European Planetary Science Congress 2018 EEuropeaPn PlanetarSy Science CCongress c Author(s) 2018 Reviewing the contribution of GRAIL to lunar science and planetary missions Maria T. Zuber and David E. Smith Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 02139- 4307, USA. ([email protected], [email protected]) Abstract Q of the Moon determined to be 41±4 at the monthly frequency. The GRAIL Discovery mission to the Moon in 2011 provided an unprecedentedly accurate gravity field model for the Moon. The goal of the mission was to provide insight into the structure of the Moon from its interior to the surface but it also made significant contributions to lunar spacecraft operations for all future lunar missions to the Moon. We discuss the science and the broader contributions from this mission that completed its objectives in December 2012 when the spacecraft impacted the lunar surface. 1. Introduction Figure 1: Free-air gravity of the Moon from GRAIL. GRAIL was a mission designed to measure the Full uniform resolution spherical harmonic models gravity field of the Moon with both high accuracy were obtained out to degree & order 1200 with and high resolution. The measurement goal was to special fields with higher resolutions over certain obtain the gravity at resolutions that would enable areas to degree and order 1800. interpretation of the crust at fractions of its thickness, estimated at the time of launch to be about 45 km. To 3. Mission Operations obtain a surface resolution of less than 10 km required the spacecraft to orbit the Moon at less than The significant improvement in our knowledge of the 20 km, an altitude that was considered dangerous at gravity field of the Moon by GRAIL enabled the re- that time without an accurate gravity field model.
    [Show full text]
  • Planetary Science
    Mission Directorate: Science Theme: Planetary Science Theme Overview Planetary Science is a grand human enterprise that seeks to discover the nature and origin of the celestial bodies among which we live, and to explore whether life exists beyond Earth. The scientific imperative for Planetary Science, the quest to understand our origins, is universal. How did we get here? Are we alone? What does the future hold? These overarching questions lead to more focused, fundamental science questions about our solar system: How did the Sun's family of planets, satellites, and minor bodies originate and evolve? What are the characteristics of the solar system that lead to habitable environments? How and where could life begin and evolve in the solar system? What are the characteristics of small bodies and planetary environments and what potential hazards or resources do they hold? To address these science questions, NASA relies on various flight missions, research and analysis (R&A) and technology development. There are seven programs within the Planetary Science Theme: R&A, Lunar Quest, Discovery, New Frontiers, Mars Exploration, Outer Planets, and Technology. R&A supports two operating missions with international partners (Rosetta and Hayabusa), as well as sample curation, data archiving, dissemination and analysis, and Near Earth Object Observations. The Lunar Quest Program consists of small robotic spacecraft missions, Missions of Opportunity, Lunar Science Institute, and R&A. Discovery has two spacecraft in prime mission operations (MESSENGER and Dawn), an instrument operating on an ESA Mars Express mission (ASPERA-3), a mission in its development phase (GRAIL), three Missions of Opportunities (M3, Strofio, and LaRa), and three investigations using re-purposed spacecraft: EPOCh and DIXI hosted on the Deep Impact spacecraft and NExT hosted on the Stardust spacecraft.
    [Show full text]
  • Planetary Science Update & Perspectives on Venus Exploration
    Planetary Science Update & Perspectives on Venus Exploration Presentation at VEXAG James L. Green Director, Planetary Science Division May 6, 2008 1 Outline • FY09 Presidents Budget • Venus exploration opportunities: – Plans for next New Frontiers – Plans for next Discovery – Plans for SALMON – R&A opportunities 2 BUDGET BY SCIENCE THEME 3 Planetary Division 4 Planetary Division 5 What Changed, What’s the Same What Changed: • Initiated an Outer Planets Flagship (OPF) study activity joint with ESA/JAXA. • Lunar Science Research augmented to include a series of small lunar spacecraft. • Augments and enhances R&A to return more results from Planetary missions. • Discovery Program: Includes the recently selected MoOs (EPOXI and Stardust-NExT), adds Aspera-3 2nd extension (ESA/Mars Express), and selected GRAIL. • Preserves critical ISP work FY08 thru FY10, but deletes outyear activities in favor of more critical R&A and RPS enhancements. • Completes the Advanced Stirling RPS development and prepares for flight demonstration. • Mars Scout 2011 delayed to 2013 due to conflict of interest discovered during proposal evaluation. • Direction to the Mars Program to study Mars Sample Return (MSR) as a next decade goal • Expands US participation on the ESA/ExoMars mission by funding the potential selection of BOTH candidate U.S. instruments and EDL support. What’s the Same: • Discovery Program: MESSENGER, Dawn, Mars Express/Aspera-3, Chandraayn/MMM • New Frontiers Program: Juno and New Horizons • Mars Program: Odyssey, MER, MRO, Phoenix, MSL • Research
    [Show full text]
  • Navigation of the Twin GRAIL Spacecraft Into Science Formation at the Moon †
    Navigation of the Twin GRAIL Spacecraft into Science Formation at the Moon † P.G. Antreasian 1, R.S. Bhat 2, S.B. Broschart 3, M.K. Chung 4, K.E. Criddle 3, T.D. Goodson 5, S.J. Hatch 6, D.C. Jefferson 3, E.L. Lau 3, S. Mohan 3, J.S. Parker 2, R.B. Roncoli 7, M.S. Ryne 3, T.H. Sweetser 5, T.H. You 8, B.T. Young 2 Jet Propulsion Laboratory, California Institute of Technology 4800 Oak Grove Drive, Pasadena, CA 91109-8099 Abstract On February 29, 2012 the twin NASA Gravity Recovery And Interior Laboratory (GRAIL) spacecraft, Ebb and Flow, achieved precise synchronized formation for collecting highly sensitive lunar gravity data. This was accomplished after performing a total of 27 maneuvers between the two spacecraft (13 on Ebb, 14 on Flow) over six months. Each 300 kg GRAIL spacecraft independently flew a 3.8-month, low-energy trajectory to reach the Moon after separation from the launch vehicle on September 10, 2011. Accurate performance of the Delta-II 7920H 10C launch vehicle led to the cancellation of the first of five planned Trajectory Correction Maneuvers (TCMs) on each spacecraft to target the required lunar orbit insertion conditions. Each GRAIL Trans-Lunar Cruise (TLC) trajectory shown in Figure 1 was optimized using 3 TCMs (TCMs 2-4). The last maneuvers, TCM-A5, B5, which were planned to clean up trajectory errors 8 days from lunar orbit insertion were cancelled due to good performance of the earlier TCMs. The Lunar Orbit Insertion (LOI) maneuvers executed on New Year’s Eve (Dec 31, 2011) and New Year’s Day (Jan 1, 2012), respectively for Ebb, and Flow.
    [Show full text]
  • Wrinkle Ridges and Ancient Rifts Bordering Procellarum and Frigoris Identified in Grail Gravity Data
    49th Lunar and Planetary Science Conference 2018 (LPI Contrib. No. 2083) 2044.pdf WRINKLE RIDGES AND ANCIENT RIFTS BORDERING PROCELLARUM AND FRIGORIS IDENTIFIED IN GRAIL GRAVITY DATA. T. R. Watters1, D.R. DeFelice1, 2, 1Center for Earth and Planetary Studies, National Air and Space Museum, Smithsonian Institution, Washington, DC 20560, USA ([email protected]); 2Department of Geology and Astronomy, West Chester University, West Chester, PA 19383, USA. Introduction: The recent and current stress state of the over and parallel- ing the bordering rifts may express Moon is dominantly contractional. This is evident from structural control by these buried features. a vast population of globally distributed lobate thrust Wrinkle Ridges of Procellarum and Frigoris: The dis- fault scarps revealed in images returned from the Lunar tribution of wrinkle ridges mapped using LROC mosaics Reconnaissance Orbiter Camera (LROC) [1-3]. The pe- and stereo derived topography indicates a direct spatial riod of dominant global contraction appears to date back correlation with segments of the narrow linear Bouguer as far as ~3.6 Gyr when large-scale mare basin-related and gradient anomalies (Fig. 1). A large number of the extension appears to have ceased [4-7], marking a stage wrinkle ridges that occur outside the mascon basins are in the Moon's thermal history at which interior cooling spatially associated with the anomalies. The hypothesis resulted in a shift from net expansion to net contraction that co-located wrinkle ridges have been controlled by [8, 9]. During the last stages of this period of net expan- subsurface structures related to buried border rifts can be sion, starting at ~3.9–4.0 b.y., the mare basalts were em- tested by examing the displacement-length (D/L) of placed [10].
    [Show full text]
  • The Symbolism of the Holy Grail
    University of Richmond UR Scholarship Repository Honors Theses Student Research 1962 The symbolism of the Holy Grail : a comparative analysis of the Grail in Perceval ou Le Conte del Graal by Chretien de Troyes and Parzival by Wolfram von Eschenbach Karin Elizabeth Nordenhaug Follow this and additional works at: https://scholarship.richmond.edu/honors-theses Part of the English Language and Literature Commons Recommended Citation Nordenhaug, Karin Elizabeth, "The symbolism of the Holy Grail : a comparative analysis of the Grail in Perceval ou Le Conte del Graal by Chretien de Troyes and Parzival by Wolfram von Eschenbach" (1962). Honors Theses. 1077. https://scholarship.richmond.edu/honors-theses/1077 This Thesis is brought to you for free and open access by the Student Research at UR Scholarship Repository. It has been accepted for inclusion in Honors Theses by an authorized administrator of UR Scholarship Repository. For more information, please contact [email protected]. UNIVERSITY OF RICHMOND LIBRARIES ~lllllllllllllllllllllllllllllllllllllllllllllllllllllllllllll3 3082 01028 5079 r THE SYMBOLISM OF THE HOLY GRAIL A COMPARATIVE ANALYSIS OF THE GRAIL In PERCEVAL ou LE CONTE del GRAAL by CHRETIEN de TROYES and PARZIVAL by WOLFRAM von ESCHENBACH by Karin Elizabeth Nordenhaug A Thesis prepared for Professor Wright In partial fulfillment of the requirements of the Honors Program And in candidacy for the degree of Bachelor of Arts Westhampton College University of Richmond, Va. May 1962 P R E F A C E If I may venture to make a bold comparison, I have often felt like Sir Perceval while writing this thesis. Like. him, I set out on a quest for the Holy Grail.
    [Show full text]
  • Juno Math: Exploring Jupiter's Gravitational Field
    Juno Math: Exploring Jupiter’s Gravitational Field All objects in the universe produce a gravitational force, and in our solar system, the second largest source of gravity after the sun is the magnificent planet Jupiter! Since Sir Isaac Newton first described the mathematics of gravity through his Law of Universal Gravitation and his detailed mathematical description of motion, astronomers have been able to use this theory to make some seemingly miraculous discoveries. For example, they can follow the minute changes in the way a satellite is accelerated as it orbits a planet to deduce how matter is distributed inside the planet. They can also determine the mass of the entire planet itself! This set of activities will show you how these marvels of astrophysics are performed using Jupiter as an example! The Mass of a Planet. In 1600, Johannes Kepler noticed from very careful studies of the planets, that they obeyed Three Golden Rules. First, they all orbited along paths that were similar to ellipses. Second, as they traveled along the orbit, they swept out equal areas in equal times. But the most exciting discovery was that there was a relationship between the square of the orbit period and the cube of the orbit distance; called Kepler’s Third Law of Planetary Motion. It can be written as T2 = C x A3 where T is the period in seconds, A is the distance (actually the semi-major axis of the elliptical orbit) in meters, and C is a constant. Problem 1 - For Jupiter, the orbit period of Juno is 13.97 days and its semi-major axis is 1.39 million km.
    [Show full text]
  • Water Organics and Mobile Elements in the Lunar Regolith V4 3
    CONSTRAINTS ON TRANSPORT AND EMPLACEMENT MECHANISMS OF LABILE FRACTIONS IN LUNAR COLD TRAPS. D. Rickman1 and L. Gertsch2, 1NASA (Earth Science Office/MSFC/NASA, 320 Spark- man Drive, Huntsville, AL 35805, [email protected]), 2Missouri University of Science and Technology (Rock Mechanics & Explosives Research Center, 1006 Kingshighway, Rolla, MO 65401, [email protected]). Introduction: Sustaining the scientific exploration For this discussion we assume that concentrations of the Solar System will require a significant propor- of labile molecules on the Moon are geographically tion of the necessary fuels and propellants, as well as limited to polar-region cold traps. other bulk commodities, to be produced from local raw General Constraints: Several constraints on the materials [1]. The viability of mineral production de- transport and/or concentration mechanisms in lunar pends on the ability to locate and characterize minea- cold trap environments should be studied. ble deposits of the necessary feedstocks. This requires, Species Applicability. First, the mechanisms must, among other things, a workable understanding of the singularly or together, work for all labiles detected. mechanisms by which such deposits form, which is the Further, they should be able to explain observed rela- subject of Economic Geology. tive abundances. Until better data arise, e.g. from on- Background: Current understanding of the distri- site sampling, we assume that all species listed above bution, abundance, and mechanisms of transport and are present in the lunar cold traps. emplacement of lunar volatiles are very problematic Relative Ages. Cabeus Crater formed after the lu- [2], a point brought out by most authors discussing nar crust stabilized.
    [Show full text]
  • Methods and Tools for the Certification of GALILEO Localisation for Railway Applications
    Methods and Tools for the Certification of GALILEO Localisation for Railway Applications Jan Poliak1, Juliette Marais2, Frank Hänsel1, Uwe Becker1, Eckehard Schnieder1 1Institute for Traffic Safety and Automation Engineering (iVA), Technical University of Braunschweig, 2Transport Electronics and Signal Processing laboratory, French National Institute for Transport and Safety Research (INRETS-LEOST) Abstract Positioning information is used in many railway typical applications: for track, fleet or wagon management as well as for level crossings and many others. Today, this function is provided by track side equipments. However, in the context of European harmonisation but also for saving costs (in particular to help low density traffic lines survive) GNSS (Global Navigation Satellite Systems) seems to fulfil some of the railway localisation requirements – or at least can be one of the bricks of a localisation system. In order to introduce this technology, many applications have been developed over the last few years in this sector and supported by European Commission and national programs. They integrate and use available as well as innovative technologies with the main focus on satellite based positioning (GPS and EGNOS already available, GLONASS and Galileo under re- deployment and development). But this introduction will not be possible without any validation of the performances. The basic idea that will be developed in this paper consists of developing generic reference measurement platforms for the evaluation and validation of applications in the transportation sector. The upcoming European satellite based localisation system Galileo will provide five different services with different performances and characteristics that will be suitable for different ranges of applications. These services will be: Open Services, Safety of Life Services, Commercial Services, Public Regulated Service and Rescue Service.
    [Show full text]