NUCLEAR FUSION Half a Century of Magnetic Con®Nement Fusion Research

Total Page:16

File Type:pdf, Size:1020Kb

NUCLEAR FUSION Half a Century of Magnetic Con®Nement Fusion Research NUCLEAR FUSION Half a Century of Magnetic Con®nement Fusion Research NUCLEAR FUSION Half a Century of Magnetic Con®nement Fusion Research C M Braams and P E Stott Institute of Physics Publishing Bristol andPhiladelphia # IOP Publishing Ltd 2002 All rights reserved. No part of this publication may be reproduced, stored in a retrieval system or transmitted in any form or by any means, electronic, mechanical, photocopying, recording or otherwise, without the prior permission of the publisher. Multiple copying is permitted in accordance with the terms of licences issued by the Copyright Licensing Agency under the terms of its agreement with Universities UK (UUK). British Library Cataloguing-in-Publication Data A catalogue record of this book is available from the British Library. ISBN 0 7503 0705 6 Library of Congress Cataloging-in-Publication Data are available Commissioning Editor: John Navas Production Editor: Simon Laurenson Production Control: Sarah Plenty Cover Design: Fre de rique Swist Marketing: Nicola Newey and Verity Cooke Published by Institute of Physics Publishing, wholly owned by The Institute of Physics, London Institute of Physics Publishing, Dirac House, Temple Back, Bristol BS1 6BE, UK US Oce: Institute of Physics Publishing, The Public Ledger Building, Suite 1035, 150 South Independence Mall West, Philadelphia, PA 19106, USA Typeset by Academic Technical, Bristol Printed in the UK by MPG Books Ltd, Bodmin, Cornwall To Lieke and Olga Thanks for your patience and encouragement Contents Preface xi Prologue xiii 1 The road to Geneva 1 1.1 The scienti®c roots 1 1.1.1 Fusion energy in stars 1 1.1.2 Fusion reactions on Earth 4 1.1.3 The origins of plasma physics 7 1.2 In andout of secrecy 16 1.2.1 Programmes taking shape 16 1.2.2 Looking behindthe curtain 20 1.2.3 The roadto travel 26 2 Geneva 1958 31 2.1 Fast linear pinches or Z-pinches 31 2.2 Steady-state mirror con®nement 35 2.3 Pulsedmirrors andtheta pinches 40 2.4 Stellarators 43 2.5 Toroidal pinches 49 2.6 RF ®elds and other subjects 52 2.7 Looking back at Geneva 53 3 Open systems 56 3.1 Simple mirror machines 56 3.1.1 Mirror loss 57 3.1.2 The quest for burnout 58 3.1.3 MHD stability 61 3.1.4 Velocity-space instabilities in mirror machines 64 3.2 Tandem mirrors 68 3.3 Z-pinch andplasma focus 75 3.4 Theta pinches 80 3.5 Unconventional schemes 84 3.6 The status of open systems 89 vii viii Contents 4 Pulsed toroidal systems and alternative lines 90 4.1 High-beta stellarators 90 4.2 Stabilizedandreversed-®eldpinches 92 4.3 Screw pinches 103 4.4 Field-reversed con®gurations and spheromaks 105 4.5 Internal-ring devices 114 4.6 Unconventional toroidal schemes 120 4.7 Status of alternative toroidal systems 122 5 Stellarators versus tokamaks 124 5.1 Stellarators: Bohm diusion or not? 124 5.2 Tokamaks: from Geneva to Novosibirsk 129 5.3 Diagnosing the plasma 134 5.4 Stellarators trailing tokamaks 143 6 The dash to tokamaks 152 6.1 The tokamak goes abroad152 6.2 Neutral beam heating 157 6.3 Disruptions anddensitylimits 159 6.4 Sawteeth 161 6.5 Passing through purgatory 164 6.6 Hydrogen recycling and refuelling 168 6.7 Divertors 170 6.8 Neoclassical theory 172 6.9 Empirical scalings 176 7 The next generation 179 7.1 New machines 179 7.2 Radio-frequency heating 184 7.3 Non-inductive current drive 187 7.4 The switch to carbon 189 7.5 Beta limits 191 7.6 Con®nement degradation 192 7.7 The H-mode 195 7.8 Attempts to understand con®nement 197 7.9 Transport codes 200 8 The era of the big tokamaks 202 8.1 Building the big tokamaks 202 8.1.1 JETÐthe Joint European Torus 203 8.1.2 TFTRÐthe Tokamak Fusion Test Reactor 206 8.1.3 JT-60 207 8.2 Operation andresults 210 8.2.1 Heating the big tokamaks 210 Contents ix 8.2.2 Keeping clean 212 8.2.3 Pushing to higher performance 214 8.2.4 Real fusion power at last 217 8.2.5 The endof the era 221 8.3 Improving the tokamak 221 8.3.1 Reactor-relevant divertor physics 222 8.3.2 Advanced tokamak scenarios 223 8.3.3 Spherical tokamaks 225 8.4 Towards ignition 227 9 Towards a fusion reactor 230 9.1 First thoughts 230 9.2 Secondthoughts 233 9.3 Pioneering studies 236 9.4 Drawing ®re 240 9.5 Economic andsocial aspects of fusion 244 9.6 Joining forces for the `next step' 247 9.7 ITER 249 9.7.1 The ITER EDA design 250 9.7.2 The physics basis 253 9.7.3 Decision andindecision 255 9.7.4 Back to the drawing board 258 10 Epilogue 261 References 270 Symbols 298 Glossary 301 Index315 Figures The authors gratefully acknowledge the following organizations and individuals for granting permission to reproduce ®gures and illustrations. Copyright in these materials remains with the original publishers: EFDA-JET (®gures 5.4, 6.1, 6.5, 7.2, 8.1, 8.5, 8.6, 9.1 and 9.3), Elsevier Scienti®c (®gures 2.1, 2.2, 2.3, 2.4, 2.7, 3.1, 4.8, 4.11, 4.12, 4.13, 5.3, 6.6a and the ®gure in box 2.4), Euratom-UKAEA Fusion Association Culham (®gures 1.5, 1.8, 2.10 and 8.8), General Atomics (Dr T N Carl- strom for ®gure 5.7), International Atomic Energy Agency (®gures 3.3, 3.5, 3.9, 3.12, 3.13, 4.1, 4.2, 4.3, 4.5, 4.14, 5.2, 5.5, 5.8, 5.10, 6.6b, 6.9 and 7.1), International Ther- monuclear Experimental Reactor (ITER) (®gure 9.4), Japan Atomic Energy Research Institute (®gure 8.3), Lawrence Livermore National Laboratory (®gures 3.4, 3.8, 4.7 and 4.10), Max-Planck-Institut fuÈ r Plasmaphysik, Garching (Dr H Wobig for ®gures 2.8 and 5.9 and Professor F Wagner for ®gures 5.12, 7.3 and 8.7), National Institute for Fusion Science (®gure 5.11), Nature Publishing Group and Dr N J Peacock (®gure 5.6), Oxford University Press and Dr J Wesson (®gures 6.2 and 6.7), Princeton Plasma Physics Laboratory (®gures 5.1, 6.3, 8.2 and 8.4) and Trilateral Euregio Cluster (TEC) (®gure 6.4). Every eort has been made to contact all copyright holders. The authors will be pleased to make good in any future editions any errors or omissions that are brought to their attention. Some ®gures have been redrawn or modi®ed by the authors, in particular ®gures 1.1 and 1.2 after Raeder J et al. 1986 Controlled Nuclear Fusion (Chichester: Wiley); ®gure 1.4 after Alfve n H 1950 Cosmical Electrodynamics (Oxford: Clarendon Press); ®gure 1.9 after Glasstone S and Lovberg R H 1960 Controlled Thermonuclear Reac- tions (Princeton: D van Nostrand); ®gures 2.5 and 2.6 after Rose D J and Clark M 1961 Plasmas and Controlled Fusion (Cambridge: MIT Press); ®gure 3.6 after Kawabe T 1983 Varenna Course on Mirror-Based and Field-Reversed Approaches to Magnetic Fusion 1 43; ®gure 3.7 after Kumazawa R 1983 9th Conf. Plasma Physics and Controlled Nuclear Fusion Research, Baltimore, 1982, Nucl. Fusion Suppl. (Vienna: IAEA) 1 566; ®gure 3.10 after Mather J W and Williams AH 1966 Physics of Fluids 9 2080; ®gure 4.4 after Baker D Aand Quinn W E 1981 The Reversed-Field Pinch, chapter 7 in Fusion 1A ed. E Teller (New York: Academic Press); ®gure 4.9 after Momota H 1992 Fusion Techn. 21 2309; ®gure 6.8 after various sources; ®gure 9.2 after Moir R W 1972 4th Conf. Plasma Physics and Controlled Nuclear Fusion Research, Madison, 1971, Proceedings Series (Vienna: IAEA) 3 315 and 1975 5th Conf. Plasma Physics and Controlled Nuclear Fusion Research, Tokyo, 1974, Proceedings Series (Vienna: IAEA) 3 589. Figures 1.3, 1.6, 1.7, 2.9, 3.2, 3.14, 4.6, 4.15 and those in boxes 2.1, 2.3, 5.2 and 7.2 were produced by the FOM Institute Rijnhuizen, which gladly waives its copyrights. x Preface Physicists who ®rst cast an eye on the problem of the peaceful use of thermo- nuclear energy, aroundthe middleof the twentieth century, soon realizedthat to try something andsee what might happen wouldget them nowhere until they understood more of plasma physics. But although plasmas occur widely in nature, indeed most of the known matter in the universe is in the plasma state, this area of physics hadbeen largely neglected.When relativity andquantum mechanics hadpresentedthemselves in the early years of the twentieth century as the areas where the greatest advances in physics were to be made,the unexploredlandbetween Newtonian mechanics andMaxwellian electromagnetism was simply overlooked. Astronomers and gas discharge physicists were the ®rst to become aware of this omission andto take steps to correct it and, when the thermonuclear problem came up, they were among the ®rst to bring their expertise to bear on the subject. In the course of the 1950s this developedinto a recognizednew branch of physics andas this unfolded, controlled thermonuclear research, or fusion research as it came to be known, evolvedfrom basic to appliedplasma physics. As it turnedout, of all the magnetic ®eldcon®gurations investigatedfor their capability to con®ne a hot plasma, the tokamak became the leading contender, to the point where we can now proceedto the construction of a test reactor and to contemplate the next step: a prototype commercial reactor.
Recommended publications
  • Silica-Rich Deposits and Hydrated Minerals at Gusev Crater, Mars: Vis-NIR Spectral Characterization and Regional Mapping
    Icarus 205 (2010) 375–395 Contents lists available at ScienceDirect Icarus journal homepage: www.elsevier.com/locate/icarus Silica-rich deposits and hydrated minerals at Gusev Crater, Mars: Vis-NIR spectral characterization and regional mapping M.S. Rice a,*, J.F. Bell III a, E.A. Cloutis b, A. Wang c, S.W. Ruff d, M.A. Craig e, D.T. Bailey b, J.R. Johnson f, P.A. de Souza Jr. g, W.H. Farrand h a Department of Astronomy, Cornell University, Ithaca, NY 14853, USA b Department of Geography, University of Winnipeg, 515 Portage Ave., Winnipeg, Man., Canada R3B 2E9 c Department of Earth and Planetary Science and McDonnell Center for Space Science, Washington University, St. Louis, MO 63130, USA d School of Earth and Space Exploration, Arizona State University, Tempe, AZ 85287, USA e Department of Earth Sciences, University of Western Ontario, 1151 Richmond St. Louis, Ont., Canada N6A 5B7 f Astrogeology Team, United States Geological Survey, Flagstaff, AZ 86001, USA g Tasmanian ICT Center, CSIRO, Hobart, Tasmania 7000, Australia h Space Science Institute, 4750 Walnut Street, Suite 205, Boulder, CO 80301, USA article info abstract Article history: The Mars Exploration Rover (MER) Spirit has discovered surprisingly high concentrations of amorphous Received 7 January 2009 silica in soil and nodular outcrops in the Inner Basin of the Columbia Hills. In Pancam multispectral obser- Revised 24 March 2009 vations, we find that an absorption feature at the longest Pancam wavelength (1009 nm) appears to be Accepted 31 March 2009 characteristic of these silica-rich materials; however, spectral analyses of amorphous silica suggest that Available online 8 May 2009 the 1009 nm spectral feature is not a direct reflection of their silica-rich nature.
    [Show full text]
  • The Quest for a Fusion Energy Reactor This Page Intentionally Left Blank the Quest for a Fusion Energy Reactor
    The Quest for a Fusion Energy Reactor This page intentionally left blank The Quest for a Fusion Energy Reactor An Insider’s Account of the INTOR Workshop Weston M. Stacey 1 2010 3 Oxford University Press, Inc., publishes works that further Oxford University’s objective of excellence in research, scholarship, and education. Oxford New York Auckland Cape Town Dar es Salaam Hong Kong Karachi Kuala Lumpur Madrid Melbourne Mexico City Nairobi New Delhi Shanghai Taipei Toronto With offi ces in Argentina Austria Brazil Chile Czech Republic France Greece Guatemala Hungary Italy Japan Poland Portugal Singapore South Korea Switzerland Thailand Turkey Ukraine Vietnam Copyright © 2010 by Oxford University Press, Inc. Published by Oxford University Press, Inc. 198 Madison Avenue, New York, New York 10016 www.oup.com Oxford is a registered trademark of Oxford University Press All rights reserved. No part of this publication may be reproduced, stored in a retrieval system, or transmitted, in any form or by any means, electronic, mechanical, photocopying, recording, or otherwise, without the prior permission of Oxford University Press. Library of Congress Cataloging-in-Publication Data Stacey, Weston M. The quest for a fusion energy reactor : an insider’s account of the INTOR Workshop / Weston M. Stacey. p. cm. Includes bibliographical references and index. ISBN 978-0-19-973384-2 1. Fusion reactors—Design and construction. 2. Engineering test reactors—Design and construction. 3. Tokamaks. 4. Fusion reactors— Research—International coorporation. 5. International Tokamak Reactor Workshop I. Title. TK9204.S62 2010 621.48’4—dc22 2009022620 987654321 Printed in the United States of America on acid-free paper To all of those who contributed to the INTOR Workshop.
    [Show full text]
  • Concepts for a Deuterium-Deuterium Fusion Reactor
    Concepts for a deuterium-deuterium fusion reactor Roberto Onofrio1, 2 1Dipartimento di Fisica e Astronomia “Galileo Galilei”, Universit`adi Padova, Via Marzolo 8, Padova 35131, Italy 2Department of Physics and Astronomy, Dartmouth College, 6127 Wilder Laboratory, Hanover, NH 03755, USA We revisit the assumption that reactors based on deuterium-deuterium (D-D) fusion processes have to be necessarily developed after the successful completion of experiments and demonstrations for deuterium-tritium (D-T) fusion reactors. Two possible mechanisms for enhancing the reactivity are discussed. Hard tails in the energy distribution of the nuclei, through the so-called κ-distribution, allow to boost the number of energetic nuclei available for fusion reactions. At higher temperatures − − than usually considered in D-T plasmas, vacuum polarization effects from real e+e and µ+µ pairs may provide further speed-up due to their contribution to screening of the Coulomb barrier. Furthermore, the energy collection system can benefit from the absence of the lithium blanket, both in simplicity and compactness. The usual thermal cycle can be bypassed with comparable efficiency levels using hadronic calorimetry and third-generation photovoltaic cells, possibly allowing to extend the use of fusion reactors to broader contexts, most notably maritime transport. I. INTRODUCTION high yield scintillating materials and hadronic calorime- try with third-generation photovoltaic cells. This could lead to energy conversion at an initially nearly compara- It is usually assumed that the first commercial fusion ble efficiency with respect to a thermal cycle, with un- reactors will be based on D-T mixtures, and within this known margins for improvement, and within a compact frame a well-defined path has been paved with the ongo- design.
    [Show full text]
  • L-Shell and Energy Dependence of Magnetic Mirror Point of Charged
    Soni et al. Earth, Planets and Space (2020) 72:129 https://doi.org/10.1186/s40623-020-01264-5 FULL PAPER Open Access L-shell and energy dependence of magnetic mirror point of charged particles trapped in Earth’s magnetosphere Pankaj K. Soni* , Bharati Kakad and Amar Kakad Abstract In the Earth’s inner magnetosphere, there exist regions like plasmasphere, ring current, and radiation belts, where the population of charged particles trapped along the magnetic feld lines is more. These particles keep performing gyration, bounce and drift motions until they enter the loss cone and get precipitated to the neutral atmosphere. Theoretically, the mirror point latitude of a particle performing bounce motion is decided only by its equatorial pitch angle. This theoretical manifestation is based on the conservation of the frst adiabatic invariant, which assumes that the magnetic feld varies slowly relative to the gyro-period and gyro-radius. However, the efects of gyro-motion can- not be neglected when gyro-period and gyro-radius are large. In such a scenario, the theoretically estimated mirror point latitudes of electrons are likely to be in agreement with the actual trajectories due to their small gyro-radius. Nevertheless, for protons and other heavier charged particles like oxygen, the gyro-radius is relatively large, and the actual latitude of the mirror point may not be the same as estimated from the theory. In this context, we have carried out test particle simulations and found that the L-shell, energy, and gyro-phase of the particles do afect their mirror points. Our simulations demonstrate that the existing theoretical expression sometimes overestimates or underesti- mates the magnetic mirror point latitude depending on the value of L-shell, energy and gyro-phase due to underlying guiding centre approximation.
    [Show full text]
  • Martian Crater Morphology
    ANALYSIS OF THE DEPTH-DIAMETER RELATIONSHIP OF MARTIAN CRATERS A Capstone Experience Thesis Presented by Jared Howenstine Completion Date: May 2006 Approved By: Professor M. Darby Dyar, Astronomy Professor Christopher Condit, Geology Professor Judith Young, Astronomy Abstract Title: Analysis of the Depth-Diameter Relationship of Martian Craters Author: Jared Howenstine, Astronomy Approved By: Judith Young, Astronomy Approved By: M. Darby Dyar, Astronomy Approved By: Christopher Condit, Geology CE Type: Departmental Honors Project Using a gridded version of maritan topography with the computer program Gridview, this project studied the depth-diameter relationship of martian impact craters. The work encompasses 361 profiles of impacts with diameters larger than 15 kilometers and is a continuation of work that was started at the Lunar and Planetary Institute in Houston, Texas under the guidance of Dr. Walter S. Keifer. Using the most ‘pristine,’ or deepest craters in the data a depth-diameter relationship was determined: d = 0.610D 0.327 , where d is the depth of the crater and D is the diameter of the crater, both in kilometers. This relationship can then be used to estimate the theoretical depth of any impact radius, and therefore can be used to estimate the pristine shape of the crater. With a depth-diameter ratio for a particular crater, the measured depth can then be compared to this theoretical value and an estimate of the amount of material within the crater, or fill, can then be calculated. The data includes 140 named impact craters, 3 basins, and 218 other impacts. The named data encompasses all named impact structures of greater than 100 kilometers in diameter.
    [Show full text]
  • Digital Physics: Science, Technology and Applications
    Prof. Kim Molvig April 20, 2006: 22.012 Fusion Seminar (MIT) DDD-T--TT FusionFusion D +T → α + n +17.6 MeV 3.5MeV 14.1MeV • What is GOOD about this reaction? – Highest specific energy of ALL nuclear reactions – Lowest temperature for sizeable reaction rate • What is BAD about this reaction? – NEUTRONS => activation of confining vessel and resultant radioactivity – Neutron energy must be thermally converted (inefficiently) to electricity – Deuterium must be separated from seawater – Tritium must be bred April 20, 2006: 22.012 Fusion Seminar (MIT) ConsiderConsider AnotherAnother NuclearNuclear ReactionReaction p+11B → 3α + 8.7 MeV • What is GOOD about this reaction? – Aneutronic (No neutrons => no radioactivity!) – Direct electrical conversion of output energy (reactants all charged particles) – Fuels ubiquitous in nature • What is BAD about this reaction? – High Temperatures required (why?) – Difficulty of confinement (technology immature relative to Tokamaks) April 20, 2006: 22.012 Fusion Seminar (MIT) DTDT FusionFusion –– VisualVisualVisual PicturePicture Figure by MIT OCW. April 20, 2006: 22.012 Fusion Seminar (MIT) EnergeticsEnergetics ofofof FusionFusion e2 V ≅ ≅ 400 KeV Coul R + R V D T QM “tunneling” required . Ekin r Empirical fit to data 2 −VNuc ≅ −50 MeV −2 A1 = 45.95, A2 = 50200, A3 =1.368×10 , A4 =1.076, A5 = 409 Coefficients for DT (E in KeV, σ in barns) April 20, 2006: 22.012 Fusion Seminar (MIT) TunnelingTunneling FusionFusion CrossCross SectionSection andand ReactivityReactivity Gamow factor . Compare to DT . April 20, 2006: 22.012 Fusion Seminar (MIT) ReactivityReactivity forfor DTDT FuelFuel 8 ] 6 c e s / 3 m c 6 1 - 0 4 1 x [ ) ν σ ( 2 0 0 50 100 150 200 T1 (KeV) April 20, 2006: 22.012 Fusion Seminar (MIT) Figure by MIT OCW.
    [Show full text]
  • Archons (Commanders) [NOTICE: They Are NOT Anlien Parasites], and Then, in a Mirror Image of the Great Emanations of the Pleroma, Hundreds of Lesser Angels
    A R C H O N S HIDDEN RULERS THROUGH THE AGES A R C H O N S HIDDEN RULERS THROUGH THE AGES WATCH THIS IMPORTANT VIDEO UFOs, Aliens, and the Question of Contact MUST-SEE THE OCCULT REASON FOR PSYCHOPATHY Organic Portals: Aliens and Psychopaths KNOWLEDGE THROUGH GNOSIS Boris Mouravieff - GNOSIS IN THE BEGINNING ...1 The Gnostic core belief was a strong dualism: that the world of matter was deadening and inferior to a remote nonphysical home, to which an interior divine spark in most humans aspired to return after death. This led them to an absorption with the Jewish creation myths in Genesis, which they obsessively reinterpreted to formulate allegorical explanations of how humans ended up trapped in the world of matter. The basic Gnostic story, which varied in details from teacher to teacher, was this: In the beginning there was an unknowable, immaterial, and invisible God, sometimes called the Father of All and sometimes by other names. “He” was neither male nor female, and was composed of an implicitly finite amount of a living nonphysical substance. Surrounding this God was a great empty region called the Pleroma (the fullness). Beyond the Pleroma lay empty space. The God acted to fill the Pleroma through a series of emanations, a squeezing off of small portions of his/its nonphysical energetic divine material. In most accounts there are thirty emanations in fifteen complementary pairs, each getting slightly less of the divine material and therefore being slightly weaker. The emanations are called Aeons (eternities) and are mostly named personifications in Greek of abstract ideas.
    [Show full text]
  • Table of Exposures
    Table of Exposures Dole UT Focal Emulsion Exposure Moon's age Plate Nos. ralio sec. days 08.11.65 2132· f/29 Kodak 0.250 Plole 0.4 15.3 7e/2 08.01.66 2228 f/24 Kodak 0.250 Plate 0.31 17.0 3b, 15e 31.01.66 1947 1/24 Kodak 0.250 Plale 0.3 10.1 5b 02.02.66 1944 f/24 Kodak 0.250 Plote 0.25 12.1 7b, 8b 06.02.66 2326 1/24 Kodak 0.250 Plole 0.2 16.3 14c,16b 05.03.66 2259 1/41 IIford Zenith Plole 0.1 13 .5 lOe/l 27.04.66 2152 1/24 lIford G.30 Plate 0.5 6.9 150 28.04.66 2046 f/30 lIford G.30 Pia Ie 0.8 7.9 10,130 23.05.66 2033 f/24 Kodak 0.250 Plole 0.7 3.4 15e/2 23.05,66 2034 f/24 Kodak 0.250 Plate 0.7 3.4 3e/2,4b 23.05.66 2036 1/24 Kodak 0.250 Plate 0.7 3.4 16e 28.05.66 2122 1/30 IIford G.30 Plole 0.8 8.4 140 29.05.66 2103 1/30 IIford G.30 Plate 0.8 9.4 2e 23.06.66 2109 f/24 lIford G.30 Pia Ie 1.0 5.0 160 06.08.66 0211 f/30 Illord G.30 Pia Ie 0.7 18.9 2b 06.08.66 0215 1/30 IIford G.30 Plale 0.7 18.9 lb, 13b 09.08.66 0315 1/30 IIlord G.30 Plate 1.1 23.8 50,60 09.08.66 03 17 1/30 Ilford G.30 Plate 1.1 23.8 90, 91/2, 11 b, 12e/l 06.
    [Show full text]
  • Crater Geometry and Ejecta Thickness of the Martian Impact Crater Tooting
    Meteoritics & Planetary Science 42, Nr 9, 1615–1625 (2007) Abstract available online at http://meteoritics.org Crater geometry and ejecta thickness of the Martian impact crater Tooting Peter J. MOUGINIS-MARK and Harold GARBEIL Hawai‘i Institute of Geophysics and Planetology, University of Hawai‘i, Honolulu, Hawai‘i 96822, USA (Received 25 October 2006; revision accepted 04 March 2007) Abstract–We use Mars Orbiter Laser Altimeter (MOLA) topographic data and Thermal Emission Imaging System (THEMIS) visible (VIS) images to study the cavity and the ejecta blanket of a very fresh Martian impact crater ~29 km in diameter, with the provisional International Astronomical Union (IAU) name Tooting crater. This crater is very young, as demonstrated by the large depth/ diameter ratio (0.065), impact melt preserved on the walls and floor, an extensive secondary crater field, and only 13 superposed impact craters (all 54 to 234 meters in diameter) on the ~8120 km2 ejecta blanket. Because the pre-impact terrain was essentially flat, we can measure the volume of the crater cavity and ejecta deposits. Tooting crater has a rim height that has >500 m variation around the rim crest and a very large central peak (1052 m high and >9 km wide). Crater cavity volume (i.e., volume below the pre-impact terrain) is ~380 km3 and the volume of materials above the pre-impact terrain is ~425 km3. The ejecta thickness is often very thin (<20 m) throughout much of the ejecta blanket. There is a pronounced asymmetry in the ejecta blanket, suggestive of an oblique impact, which has resulted in up to ~100 m of additional ejecta thickness being deposited down-range compared to the up-range value at the same radial distance from the rim crest.
    [Show full text]
  • March 21–25, 2016
    FORTY-SEVENTH LUNAR AND PLANETARY SCIENCE CONFERENCE PROGRAM OF TECHNICAL SESSIONS MARCH 21–25, 2016 The Woodlands Waterway Marriott Hotel and Convention Center The Woodlands, Texas INSTITUTIONAL SUPPORT Universities Space Research Association Lunar and Planetary Institute National Aeronautics and Space Administration CONFERENCE CO-CHAIRS Stephen Mackwell, Lunar and Planetary Institute Eileen Stansbery, NASA Johnson Space Center PROGRAM COMMITTEE CHAIRS David Draper, NASA Johnson Space Center Walter Kiefer, Lunar and Planetary Institute PROGRAM COMMITTEE P. Doug Archer, NASA Johnson Space Center Nicolas LeCorvec, Lunar and Planetary Institute Katherine Bermingham, University of Maryland Yo Matsubara, Smithsonian Institute Janice Bishop, SETI and NASA Ames Research Center Francis McCubbin, NASA Johnson Space Center Jeremy Boyce, University of California, Los Angeles Andrew Needham, Carnegie Institution of Washington Lisa Danielson, NASA Johnson Space Center Lan-Anh Nguyen, NASA Johnson Space Center Deepak Dhingra, University of Idaho Paul Niles, NASA Johnson Space Center Stephen Elardo, Carnegie Institution of Washington Dorothy Oehler, NASA Johnson Space Center Marc Fries, NASA Johnson Space Center D. Alex Patthoff, Jet Propulsion Laboratory Cyrena Goodrich, Lunar and Planetary Institute Elizabeth Rampe, Aerodyne Industries, Jacobs JETS at John Gruener, NASA Johnson Space Center NASA Johnson Space Center Justin Hagerty, U.S. Geological Survey Carol Raymond, Jet Propulsion Laboratory Lindsay Hays, Jet Propulsion Laboratory Paul Schenk,
    [Show full text]
  • Nicholas Christofilos and the Astron Project in America's Fusion Program
    Elisheva Coleman May 4, 2004 Spring Junior Paper Advisor: Professor Mahoney Greek Fire: Nicholas Christofilos and the Astron Project in America’s Fusion Program This paper represents my own work in accordance with University regulations The author thanks the Program in Plasma Science and Technology and the Princeton Plasma Physics Laboratory for their support. Introduction The second largest building on the Lawrence Livermore National Laboratory’s campus today stands essentially abandoned, used as a warehouse for odds and ends. Concrete, starkly rectangular and nondescript, Building 431 was home for over a decade to the Astron machine, the testing device for a controlled fusion reactor scheme devised by a virtually unknown engineer-turned-physicist named Nicholas C. Christofilos. Building 431 was originally constructed in the late 1940s before the Lawrence laboratory even existed, for the Materials Testing Accelerator (MTA), the first experiment performed at the Livermore site.1 By the time the MTA was retired in 1955, the Livermore lab had grown up around it, a huge, nationally funded institution devoted to four projects: magnetic fusion, diagnostic weapon experiments, the design of thermonuclear weapons, and a basic physics program.2 When the MTA shut down, its building was turned over to the lab’s controlled fusion department. A number of fusion experiments were conducted within its walls, but from the early sixties onward Astron predominated, and in 1968 a major extension was added to the building to accommodate a revamped and enlarged Astron accelerator. As did much material within the national lab infrastructure, the building continued to be recycled. After Astron’s termination in 1973 the extension housed the Experimental Test Accelerator (ETA), a prototype for a huge linear induction accelerator, the type of accelerator first developed for Astron.
    [Show full text]
  • DMAAC – February 1973
    LUNAR TOPOGRAPHIC ORTHOPHOTOMAP (LTO) AND LUNAR ORTHOPHOTMAP (LO) SERIES (Published by DMATC) Lunar Topographic Orthophotmaps and Lunar Orthophotomaps Scale: 1:250,000 Projection: Transverse Mercator Sheet Size: 25.5”x 26.5” The Lunar Topographic Orthophotmaps and Lunar Orthophotomaps Series are the first comprehensive and continuous mapping to be accomplished from Apollo Mission 15-17 mapping photographs. This series is also the first major effort to apply recent advances in orthophotography to lunar mapping. Presently developed maps of this series were designed to support initial lunar scientific investigations primarily employing results of Apollo Mission 15-17 data. Individual maps of this series cover 4 degrees of lunar latitude and 5 degrees of lunar longitude consisting of 1/16 of the area of a 1:1,000,000 scale Lunar Astronautical Chart (LAC) (Section 4.2.1). Their apha-numeric identification (example – LTO38B1) consists of the designator LTO for topographic orthophoto editions or LO for orthophoto editions followed by the LAC number in which they fall, followed by an A, B, C or D designator defining the pertinent LAC quadrant and a 1, 2, 3, or 4 designator defining the specific sub-quadrant actually covered. The following designation (250) identifies the sheets as being at 1:250,000 scale. The LTO editions display 100-meter contours, 50-meter supplemental contours and spot elevations in a red overprint to the base, which is lithographed in black and white. LO editions are identical except that all relief information is omitted and selenographic graticule is restricted to border ticks, presenting an umencumbered view of lunar features imaged by the photographic base.
    [Show full text]