The Moon Race and the Dark Sides of Lunar Crater Naming
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Pos(Westerbork)002 Historical Introduction Historical S 4.0 International License (CC BY-NC-ND 4.0)
Historical Introduction PoS(Westerbork)002 Richard Strom ASTRON Oude Hoogeveensedijk 4, 7991 PD Dwingeloo, The Netherlands E-mail: [email protected] 50 Years Westerbork Radio Observatory, A Continuing Journey to Discoveries and Innovations Richard Strom, Arnold van Ardenne, Steve Torchinsky (eds) Published with permission of the Netherlands Institute for Radio Astronomy (ASTRON) under the terms of the Creative CommonsAttribution-NonCommercial-NoDerivatives 4.0 International License (CC BY-NC-ND 4.0). Chapter 1 Historical introduction Richard Strom* rom the English longbows at the battle of Crécy (1346) to Winston Chur- chill’s world war I mobilized cannon (its true identity hidden behind the Fpseudonym “[water] tank”), warfare has always pushed technological innovation to new fronts. The second world war (WWII) was no exception. It gave us technology ranging from the dynamo-powered flashlight (a Philips invention) to jet engines, and space-capable rockets (Germany’s V2), not to mention (in a completely different realm) the mass production of Penicillin. In fact, it could be argued that WWII inventions marked the inception of the modern technological era1. In the field of electronics, the war led to innovations such as radio navigation, aircraft landing systems, and radar. It was these developments which were to * ASTRON, Univer- sity of Amsterdam, have a revolutionary impact on astronomy, initially in Britain, Australia and the The Netherlands United States. But the story begins in the US, with the electronics of the 1920s and ‘30s. Figure 1. Karl G. Jansky (c. 1933) Around 1930, there was increasing interest in the use of radio frequencies for communication. One of the main players, the Bell Telephone Laboratories in New Jersey, asked their research engineer, Karl Jansky (Figure 1), to investigate the inter- ference environment in the “short-wave” band around 20 MHz. -
Marcel Minnaert, Astrofysicus 1893-1970
Marcel Minnaert, astrofysicus 1893-1970 De rok van het universum Leo Molenaar bron Leo Molenaar, Marcel Minnaert, astrofysicus 1893-1970. De rok van het universum. Balans, Amsterdam / Van Halewyck, Leuven 2003 Zie voor verantwoording: http://www.dbnl.org/tekst/mole016marc01_01/colofon.htm © 2007 dbnl / Leo Molenaar 4 In deze tijd heeft wat men altijd noemde Schoonheid, schoonheid haar gezicht verbrand Zij troost niet meer de mensen Zij troost de larven de reptielen de ratten Maar de mens verschrikt zij En treft hem met het besef Een broodkruimel te zijn op de rok van het universum (Uit Lucebert, ik tracht op poëtische wijze, Verzamelde gedichten, Amsterdam 2002, pag. 52) Leo Molenaar, Marcel Minnaert, astrofysicus 1893-1970 7 Proloog Marcel Minnaert (1893-1970): Erflater van de Groot-Nederlandse beschaving Er zijn heel wat mensen voor wie de naam van Minnaert nog een dierbare klank heeft. Dat geldt in ieder geval voor leraren in de natuurwetenschap die houden van waarnemingen in de vrije natuur. Mijn eerste kennismaking met hem had dan ook plaats via de Minnaert: zo heten de drie delen van De Natuurkunde van 't Vrije Veld die ik omstreeks 1970 heb aangeschaft. De eerste druk van dit boek verscheen eind jaren dertig. In de jaren negentig kwamen van het eerste deel van Minnaerts trilogie, Licht en kleur in het landschap, nieuw geïllustreerde uitgaven in het Engels en Duits op de markt naast de herdruk van de Minnaert in het Nederlands. Het is dan ook een uniek boek. Minnaert had vijfentwintig jaar lang natuurverschijnselen geobserveerd, daar aantekeningen van gemaakt en onderzoek gedaan naar de fysische verklaringen. -
Four-Dimensional B-Spline Algorithm for Mars Crater Reconstruction
FOUR-DIMENSIONAL B-SPLINE ALGORITHM FOR MARS CRATER RECONSTRUCTION Maged Marghany and Shattri Mansor Geospatial Information Science Research Centre, Faculty of Engineering University Putra Malaysia 43400 UPM, Serdang, Selangor Email :[email protected] KEY WORDS: Mars, Crater, High Resolution Stereo Camera (HRSC), Four-dimensional, B-spline. ABSTRACT: The main contribution of this work is to simulate 4-D of Mars carters. In doing so, 3-D data of High Resolution Stereo Camera (HRSC) was aquired and then 4-D spline algorithm implemented to sequences of HRSC data with different fram of times. The study shows that B-spline can determine the 4-D crater surface with deep ice covers which could indicate for the existence of water. In conclusion, integration between 4-D B-spline algorithm and High Resolution Stereo Camera can be excellent 4-D visualization tool. 1. INTRODUCTION A carter is most visual feature which exists in Mars surface. Crater can be created by two cosmic bodies crashed each other, for instance, a meteorite striking a planet. It can be also formed by volcanic occupation. The different sort of carter is subsidence crater, which is occurred from an underground due to nuclear explosion. A crater-like pattern shaped by erosion which is known as Machtesh. Furthermore, a relief crater triggered by a phreatic outburst or explosion is defined as a maar crater. Therefore, Mars is a terrestrial planet which contains of minerals. These minerals are containing silicon and oxygen, metals, and other elements which naturally form rock. The Mars surface is mostly created from tholeiitic basalt. With these regards, the Mars is required standard procedures to understand its complicated nature and characteristics formation. -
Anton Pannekoek: Ways of Viewing Science and Society
STUDIES IN THE HISTORY OF KNOWLEDGE Tai, Van der Steen & Van Dongen (eds) Dongen & Van Steen der Van Tai, Edited by Chaokang Tai, Bart van der Steen, and Jeroen van Dongen Anton Pannekoek: Ways of Viewing Science and Society Ways of Viewing ScienceWays and Society Anton Pannekoek: Anton Pannekoek: Ways of Viewing Science and Society Studies in the History of Knowledge This book series publishes leading volumes that study the history of knowledge in its cultural context. It aspires to offer accounts that cut across disciplinary and geographical boundaries, while being sensitive to how institutional circumstances and different scales of time shape the making of knowledge. Series Editors Klaas van Berkel, University of Groningen Jeroen van Dongen, University of Amsterdam Anton Pannekoek: Ways of Viewing Science and Society Edited by Chaokang Tai, Bart van der Steen, and Jeroen van Dongen Amsterdam University Press Cover illustration: (Background) Fisheye lens photo of the Zeiss Planetarium Projector of Artis Amsterdam Royal Zoo in action. (Foreground) Fisheye lens photo of a portrait of Anton Pannekoek displayed in the common room of the Anton Pannekoek Institute for Astronomy. Source: Jeronimo Voss Cover design: Coördesign, Leiden Lay-out: Crius Group, Hulshout isbn 978 94 6298 434 9 e-isbn 978 90 4853 500 2 (pdf) doi 10.5117/9789462984349 nur 686 Creative Commons License CC BY NC ND (http://creativecommons.org/licenses/by-nc-nd/3.0) The authors / Amsterdam University Press B.V., Amsterdam 2019 Some rights reserved. Without limiting the rights under copyright reserved above, any part of this book may be reproduced, stored in or introduced into a retrieval system, or transmitted, in any form or by any means (electronic, mechanical, photocopying, recording or otherwise). -
Wetenschap Van Gene Zijde Geschiedenis Van De Nederlandse Parapsychologie in De Twintigste Eeuw
WETENSCHAP VAN GENE ZIJDE GESCHIEDENIS VAN DE NEDERLANDSE PARAPSYCHOLOGIE IN DE TWINTIGSTE EEUW SCIENCE FROM BEYOND HISTORY OF DUTCH PARAPSYCHOLOGY IN THE TWENTIETH CENTURY (WITH A SUMMARY IN ENGLISH) PROEFSCHRIFT TER VERKRIJGING VAN DE GRAAD VAN DOCTOR AAN DE UNIVERSITEIT UTRECHT OP GEZAG VAN DE RECTOR MAGNIFICUS, PROF.DR. G.J. VAN DER ZWAAN, INGEVOLGE HET BESLUIT VAN HET COLLEGE VOOR PROMOTIES IN HET OPENBAAR TE VERDEDIGEN OP DONDERDAG 18 FEBRUARI 2016 DES MIDDAGS TE 4.15 UUR DOOR INGRID ELS KLOOSTERMAN GEBOREN OP 21 OKTOBER 1983 TE FRANEKER PROMOTOREN: PROF. DR. W. KOOPS PROF. DR. J. VIJSELAAR COPROMOTOR: DR. J. BOS INHOUD OVERZICHT INTERVIEWS EN ARCHIEVEN 8 1 INTRODUCTIE 11 2 DE NATUUR GOOCHELT NIET: POGINGEN TOT PSYCHISCH ONDERZOEK 1888-1914 EEN MISLUKTE SEANCE 41 POGINGEN TOT PSYCHISCH ONDERZOEK 45 FREDERIK VAN EEDEN ALS OVERTUIGD SPIRITIST 48 HENRI DE FREMERY ALS KRITISCH SPIRITIST 63 CONCLUSIES 80 3 VERBORGEN KRACHTEN: VERENIGINGEN VOOR PSYCHISCH ONDERZOEK 1915-1925 TELEPATHIE VAN TONEEL NAAR LABORATORIUM 83 VERENIGINGEN VOOR PSYCHISCH ONDERZOEK 86 EEN VERENIGING VOOR TOEGEPAST MAGNETISME 89 DE STUDIEVEREENIGING VOOR PSYCHICAL RESEARCH 101 CONCLUSIES 122 4 DE BOVENNATUUR IN DE PRAKTIJK: ACADEMISCHE VERBINTENISSEN 1928-1940 DE STRIJD OM DE PARAPSYCHOLOGIE 125 ACADEMISCHE VERBINTENISSEN 128 DE EERSTE PRIVAATDOCENTEN 131 WETENSCHAPPELIJK TIJDSCHRIFT EN LABORATORIUM 143 CONCLUSIES 161 5 EEN BIJZONDERE PERSOONLIJKHEID: ACADEMISCHE INBEDDING IN UTRECHT 1940-1959 EEN INTERNATIONALE CONFERENTIE 163 ACADEMISCHE INBEDDING IN UTRECHT 167 -
Water on the Moon, III. Volatiles & Activity
Water on The Moon, III. Volatiles & Activity Arlin Crotts (Columbia University) For centuries some scientists have argued that there is activity on the Moon (or water, as recounted in Parts I & II), while others have thought the Moon is simply a dead, inactive world. [1] The question comes in several forms: is there a detectable atmosphere? Does the surface of the Moon change? What causes interior seismic activity? From a more modern viewpoint, we now know that as much carbon monoxide as water was excavated during the LCROSS impact, as detailed in Part I, and a comparable amount of other volatiles were found. At one time the Moon outgassed prodigious amounts of water and hydrogen in volcanic fire fountains, but released similar amounts of volatile sulfur (or SO2), and presumably large amounts of carbon dioxide or monoxide, if theory is to be believed. So water on the Moon is associated with other gases. Astronomers have agreed for centuries that there is no firm evidence for “weather” on the Moon visible from Earth, and little evidence of thick atmosphere. [2] How would one detect the Moon’s atmosphere from Earth? An obvious means is atmospheric refraction. As you watch the Sun set, its image is displaced by Earth’s atmospheric refraction at the horizon from the position it would have if there were no atmosphere, by roughly 0.6 degree (a bit more than the Sun’s angular diameter). On the Moon, any atmosphere would cause an analogous effect for a star passing behind the Moon during an occultation (multiplied by two since the light travels both into and out of the lunar atmosphere). -
Project Note Weston Solutions, Inc
PROJECT NOTE WESTON SOLUTIONS, INC. To: Canadian Radium & Uranium Corp. Site File Date: June 5, 2014 W.O. No.: 20405.012.013.2222.00 From: Denise Breen, Weston Solutions, Inc. Subject: Determination of Significant Lead Concentrations in Sediment Samples References 1. New York State Department of Environmental Conservation. Technical Guidance for Screening Contaminated Sediments. March 1998. [45 pages] 2. U.S. Environmental Protection Agency (EPA) Office of Emergency Response. Establishing an Observed Release – Quick Reference Fact Sheet. Federal Register, Volume 55, No. 241. September 1995. [7 pages] 3. International Union of Pure and Applied Chemistry, Inorganic Chemistry Division Commission on Atomic Weights and Isotopic Abundances. Atomic Weights of Elements: Review 2000. 2003. [120 pages] WESTON personnel collected six sediment samples (including one environmental duplicate sample) from five locations along the surface water pathway of the Canadian Radium & Uranium Corp. (CRU) site in May 2014. The sediment samples were analyzed for Target Analyte List (TAL) Metals and Stable Lead Isotopes. 1. TAL Lead Interpretation: In order to quantify the significance for Lead, Thallium and Mercury the following was performed: 1. WESTON personnel tabulated all available TAL Metal data from the May 2014 Sediment Sampling event. 2. For each analyte of concern (Lead, Thallium, and Mercury), the highest background concentration was selected and then multiplied by three. This is the criteria to find the significance of site attributable release as per Hazard Ranking System guidelines. 3. One analytical lead result (2222-SD04) of 520 mg/kg (J) was qualified with an unknown bias. In accordance with US EPA document “Using Data to Document an Observed Release and Observed Contamination”, 2222-SD03 lead concentration was adjusted by dividing by the factor value for lead of 1.44 to equal 361 mg/kg. -
Asymmetric Terracing of Lunar Highland Craters: Influence of Pre-Impact Topography and Structure
Proc. L~lnorPli~nel. Sci. Corrf. /Of11 (1979), p. 2597-2607 Printed in the United States of America Asymmetric terracing of lunar highland craters: Influence of pre-impact topography and structure Ann W. Gifford and Ted A. Maxwell Center for Earth and Planetary Studies, National Air and Space Museum, Smithsonian Institition, Washington, DC 20560 Abstract-The effects of variable pre-impact topography and substrate on slumping and terrace for- mation have been studied on a group of 30 craters in the lunar highlands. These craters are charac- terized by a distinct upper slump block and are all situated on the rim of a larger, older crater or a degraded rim segment. Wide, isolated terraces occur where the rim of the younger crater coincides with a rim segment of the older crater. The craters are all located in Nectarianlpre-Nectarian highland units, and range in age from Imbrian to Copernican. A proposed model for formation of slump blocks in these craters includes the existence of layers with different competence in an overturned rim of the pre-existing crater. Such layering could have resulted from overturning of more coherent layers during formation of the Nectarian and pre-Nec- tarian craters. A combination of material and topographic effects is therefore responsible for terrace formation. Similar terrain effects may be present on other planets and should be considered when interpreting crater statistics in relation to morphology. INTRODUCTION Slumping, terracing or wall failure is an important process in formation and mod- ification of lunar craters. The process of slumping has been investigated by both geometrical (Cintala et a1 ., 1977) and theoretical models (Melosh, 1977; Melosh and McKinnon, 1979); however, these studies are dependent on morphologic constraints imposed by the geologic setting of the craters. -
Appendix I Lunar and Martian Nomenclature
APPENDIX I LUNAR AND MARTIAN NOMENCLATURE LUNAR AND MARTIAN NOMENCLATURE A large number of names of craters and other features on the Moon and Mars, were accepted by the IAU General Assemblies X (Moscow, 1958), XI (Berkeley, 1961), XII (Hamburg, 1964), XIV (Brighton, 1970), and XV (Sydney, 1973). The names were suggested by the appropriate IAU Commissions (16 and 17). In particular the Lunar names accepted at the XIVth and XVth General Assemblies were recommended by the 'Working Group on Lunar Nomenclature' under the Chairmanship of Dr D. H. Menzel. The Martian names were suggested by the 'Working Group on Martian Nomenclature' under the Chairmanship of Dr G. de Vaucouleurs. At the XVth General Assembly a new 'Working Group on Planetary System Nomenclature' was formed (Chairman: Dr P. M. Millman) comprising various Task Groups, one for each particular subject. For further references see: [AU Trans. X, 259-263, 1960; XIB, 236-238, 1962; Xlffi, 203-204, 1966; xnffi, 99-105, 1968; XIVB, 63, 129, 139, 1971; Space Sci. Rev. 12, 136-186, 1971. Because at the recent General Assemblies some small changes, or corrections, were made, the complete list of Lunar and Martian Topographic Features is published here. Table 1 Lunar Craters Abbe 58S,174E Balboa 19N,83W Abbot 6N,55E Baldet 54S, 151W Abel 34S,85E Balmer 20S,70E Abul Wafa 2N,ll7E Banachiewicz 5N,80E Adams 32S,69E Banting 26N,16E Aitken 17S,173E Barbier 248, 158E AI-Biruni 18N,93E Barnard 30S,86E Alden 24S, lllE Barringer 29S,151W Aldrin I.4N,22.1E Bartels 24N,90W Alekhin 68S,131W Becquerei -
From Zone Plates to Microcalorimeter: 50 Years of Cosmic X-Ray Spectroscopy at SRON
From zone plates to microcalorimeter: 50 years of cosmic X-ray spectroscopy at SRON Johan Bleeker University of Utrecht/SRON, the Netherlands The grass-roots at Utrecht (1) Christophorus Buys Ballot: - 1853: Sonnenborgh Observatory Meteorology and Astronomy - 1877: New Physics Laboratory Mainly: teaching - → : optical spectroscopy (Julius, Moll, Ornstein) - 1896 : Heliostat spectrograph for Fraunhofer lines in Solar spectrum - 1923 : concept of equivalent line width W(Minnaert) - 1929 : formulation of curve of growth W=f(N) (Minnaert, Unsöld) The grass roots at Utrecht (2): Atlas of the solar spectrum: Marcel Minnaert 1936: ~ 100 photographic plates taken at Mount Wilson Observatory 1940: Utrecht Photometric Atlas of the solar spectrum (Minnaert et al) 1952: Solar atmosphere temperature model (de Jager 1952) 1966: Solar abundances from The Solar Spectrum (Moore et al ) To shorter wavelengths: X-ray spectroscopy • 1961: Start Space research in Utrecht • First target: X-ray spectroscopy of the sun Mid 1960’s: Monochromatic XUV-images of the Sun X-ray lense employing diffraction: Fresnel zone plate Zone partition of spherical wavefront → block even/odd zones th Radius n zone: , with N = nmax= large → Focal length(5nm): ΔrN=1μm rN=1mm, f=40cm Mid 1960s: Q-monochromatic XUV-images of the Sun X-ray lense employing diffraction: Fresnel zone plate Manufacturing: RQ: transparent zones completely open, width 1-2 μm → radial support - First successful trials with electron optical imaging, FOV limitations - Interferogram of two coherent spherical wave fronts: Photolithography Sun in Si X at 5.1 nm 1967: Successful sun stabilized Aerobee rocket experiment 4 Zone plates of 50 metallic rings f = 40 cm, outer diam. -
Moore Et Al., 1977
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 98, NO. E2, PAGES 3413-3429, FEBRUARY 25, 1993 SOIL TEXTURE AND GRANULOMETRY AT THE SURFACE OF MARS Audouin Dollfus and Marc Deschamps Observatoire de Paris, Meudon, France James R. Zimbelman Center for Earth and Planetary Sciences, National Air and Space Museum Smithsonian Institution, Washington, D. C. The physical behavior of the Martian surface soil has been characterized remotely by both photopolarimetry and radiometry. The degree of linear polarization defines a coefficient b which is related to the top surface soil texture and is calibrated in terms of grain size, or as a fraction of the area exhibiting uncovered clean rocks. This coefficient b was recorded with the instrument VPM (Visual Polarimeter Mars) on board Soviet orbiter MARS 5 in 1974. The radiometric thermal inertia coefficient I is essentially a measurement of the soil compaction, or an effective average particle size in the soil texture, through the few decimeters below the top surface sensed by polarimetry. The instrument IBTM (Infra Bed Thermal Mapper) was used on board the Viking spacecraft between 1976 and 1982. The polarimetric scans raked a strip covering two contrasting regions, the dark-hued Mare Erythraeum and the light-hued Thaumasia. Over these wide areas, several smaller typical terrains were characterized by the three parameters A (albedo), b (related to top surface grain size) and I (underlaying compaction or block size). The large dark region Erythraeum is characterized everywhere by a uniform polarization response, despite the large geomorphological diversity of the surface. The values of A and b indicate a ubiquitous coating or mantling with small dark grains of albedo 12.7%, with a radius of 10 to 20 urn. -
Annual Progress Report
? ASTRDGEOLOGIC ANNUAL PROGRESS REPORT July 1, 1964 to c July 1, 1965 xov&iiib&r1365 This preliminary report is distributed without editorial and technical review for conformity with official standards and nomenclature. It should not be quoted without permission. This report concerns work done on behalf of the National Aeronautics and Space Administration. DEPARTMENT OF THE INTERIOR UNITED STATES GEOIX)(;ICAL SURVEY 6 F DISTRIBUTION No. of Copies National Aeronautics and Space Administration Washington, D.C. ......................... -20 U.S. Geological Survey ...................... .10 A'~elsoii, Dr. P. E., Oirector Geophysical Laboratory Carnegie Institution Washington, D.C. .......................... 1 Allen, Mr. H. J. Ames Research Center Moffett Field, California. ..................... 1 Babcock, Dr. H. W., Director Mt. Wilson and Palomar Observatories Mount Wilson, California ...................... 1 Beattie, Mr. D. A. National Aeronautics and Space Administration Washington, D.C. ......................... .1 Brown, Professor Harrison Division of Geological Sciences California Institute of Technology Pasadena, California ........................ 1 Bryson, Mr. R. P. National Aeronautics and Space Administration Washington, D.C. .......................... 2 Cannell, Mr. W. D. Aeronautical Chart and Information Center Lowell Observatory Flagstaff, Arizona ......................... 1 Carder, Mr. R. W. Aeronautical Chart and Information Center Second and Arsenal Streets St. Louis, Missouri. ........................ 1 Chapman, 'Dr. D.