V-Type Near-Earth Asteroids: Dynamics, Close Encounters and Impacts With
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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, -
Properties of Cometary Nuclei
Properties of Cometary Nuclei J, Rahe, NASA Headquarters, Washington, DC V. Vanysek, Charles University, Prague, Czech Republic P. R. Weissman Jet Propulsion Laboratory, Pasadena, CA Abstract: Active long- and short-period comets contribute about 20 to 30% of the major impactors on the Earth. Cometary nuclei are irregular bodies, typically a few to ten kilometers in diameter, with masses in the range 10*5 to 10’8 g. The nuclei are composed of an intimate mixture of volatile ices, mostly water ice, and hydrocarbon and silicate grains. The composition is the closest to solar composition of any known bodies in the solar system. The nuclei appear to be weakly bonded agglomerations of smaller icy planetesimals, and material strengths estimated from observed tidal disruption events are fairly low, typically 1& to ld N m-2. Density estimates range between 0.2 and 1.2 g cm-3 but are very poorly determined, if at all. As comets age they develop nonvolatile crusts on their surfaces which eventually render them inactive, similar in appearance to carbonaceous asteroids. However, dormant comets may continue to show sporadic activity and outbursts for some time before they become truly extinct. The source of the long-period comets is the Oort cloud, a vast spherical cloud of perhaps 1012 to 10’3 comets surrounding the solar system and extending to interstellar distances. The likely source of the short-period comets is the Kuiper belt, a ring of perhaps 108 to 1010 remnant icy planetesimals beyond the orbit of Neptune, though some short-period comets may also be long- pcriod comets from the Oort cloud which have been perturbed to short-period orbits. -
Appendix a Recovery of Ejecta Material from Confirmed, Probable
Appendix A Recovery of Ejecta Material from Confirmed, Probable, or Possible Distal Ejecta Layers A.1 Introduction In this appendix we discuss the methods that we have used to recover and study ejecta found in various types of sediment and rock. The processes used to recover ejecta material vary with the degree of lithification. We thus discuss sample processing for unconsolidated, semiconsolidated, and consolidated material separately. The type of sediment or rock is also important as, for example, carbonate sediment or rock is processed differently from siliciclastic sediment or rock. The methods used to take and process samples will also vary according to the objectives of the study and the background of the investigator. We summarize below the methods that we have found useful in our studies of distal impact ejecta layers for those who are just beginning such studies. One of the authors (BPG) was trained as a marine geologist and the other (BMS) as a hard rock geologist. Our approaches to processing and studying impact ejecta differ accordingly. The methods used to recover ejecta from unconsolidated sediments have been successfully employed by BPG for more than 40 years. A.2 Taking and Handling Samples A.2.1 Introduction The size, number, and type of samples will depend on the objective of the study and nature of the sediment/rock, but there a few guidelines that should be followed regardless of the objective or rock type. All outcrops, especially those near industrialized areas or transportation routes (e.g., highways, train tracks) need to be cleaned off (i.e., the surface layer removed) prior to sampling. -
(2000) Forging Asteroid-Meteorite Relationships Through Reflectance
Forging Asteroid-Meteorite Relationships through Reflectance Spectroscopy by Thomas H. Burbine Jr. B.S. Physics Rensselaer Polytechnic Institute, 1988 M.S. Geology and Planetary Science University of Pittsburgh, 1991 SUBMITTED TO THE DEPARTMENT OF EARTH, ATMOSPHERIC, AND PLANETARY SCIENCES IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY IN PLANETARY SCIENCES AT THE MASSACHUSETTS INSTITUTE OF TECHNOLOGY FEBRUARY 2000 © 2000 Massachusetts Institute of Technology. All rights reserved. Signature of Author: Department of Earth, Atmospheric, and Planetary Sciences December 30, 1999 Certified by: Richard P. Binzel Professor of Earth, Atmospheric, and Planetary Sciences Thesis Supervisor Accepted by: Ronald G. Prinn MASSACHUSES INSTMUTE Professor of Earth, Atmospheric, and Planetary Sciences Department Head JA N 0 1 2000 ARCHIVES LIBRARIES I 3 Forging Asteroid-Meteorite Relationships through Reflectance Spectroscopy by Thomas H. Burbine Jr. Submitted to the Department of Earth, Atmospheric, and Planetary Sciences on December 30, 1999 in Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy in Planetary Sciences ABSTRACT Near-infrared spectra (-0.90 to ~1.65 microns) were obtained for 196 main-belt and near-Earth asteroids to determine plausible meteorite parent bodies. These spectra, when coupled with previously obtained visible data, allow for a better determination of asteroid mineralogies. Over half of the observed objects have estimated diameters less than 20 k-m. Many important results were obtained concerning the compositional structure of the asteroid belt. A number of small objects near asteroid 4 Vesta were found to have near-infrared spectra similar to the eucrite and howardite meteorites, which are believed to be derived from Vesta. -
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. -
Proposed 2020 NEA Targets (Med SNR)
Radar Characterization of NEAs: Moderate Resolution Imaging, Astrometry, and a Systematic Survey Anne K. Virkki (Arecibo Observatory, UCF), Patrick A. Taylor (LPI, USRA), Flaviane C.F. Ven- ditti, Sean E. Marshall, Dylan C. Hickson, Luisa F. Zambrano-Marin (Arecibo Observatory, UCF), Edgard G. Rivera-Valent´ın, Sriram S. Bhiravarasu, Betzaida Aponte-Hernandez (LPI, USRA), Michael C. Nolan, Ellen S. Howell (U. Arizona), Tracy M. Becker (SwRI), Jon D. Giorgini, Lance A. M. Benner, Marina Brozovic, Shantanu P. Naidu (JPL), Michael W. Busch (SETI), Jean-Luc Margot, Sanjana Prabhu Desai (UCLA), Agata Rozek˙ (U. Kent), Mary L. Hinkle (UCF), Michael K. Shepard (Bloomsburg U.), and Christopher Magri (U. Maine) Summary We propose the continuation of the long-running project R3035 to physically and dynamically characterize the population of near-Earth asteroids with the Arecibo S-band (2380 MHz; 12.6 cm) planetary radar system. The objectives of project R3035 are to: (1) provide basic characterizations (size, shape, and radar scattering properties) of dozens of objects, (2) report ultra-precise radar astrometry for all detections, and (3) conduct a monthly survey of newly discovered objects around new moon. These observations will be carried out as part of the NASA-funded Arecibo planetary radar program, Grant No. 80NSSC19K0523, to PI Anne Virkki (Arecibo Observatory, University of Central Florida) with Patrick Taylor as Institutional PI at the Lunar and Planetary Institute (Universities Space Research Association). Background Radar is arguably the most powerful Earth-based technique for post-discovery physical and dynamical characterization of near-Earth asteroids (NEAs) and plays a crucial role in the nation’s planetary defense initiatives led through the NASA Planetary Defense Coordination Office. -
Radar Observations of Asteroid 3908 Nyx
Icarus 158, 379–388 (2002) doi:10.1006/icar.2002.6869 Radar Observations of Asteroid 3908 Nyx Lance A. M. Benner and Steven J. Ostro Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California 91109-8099 E-mail: [email protected] R. Scott Hudson School of Electrical Engineering and Computer Science, Washington State University, Pullman, Washington 99164-2752 Keith D. Rosema,1 Raymond F. Jurgens, and Donald K. Yeomans Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California 91109-8099 Donald B. Campbell National Astronomy and Ionosphere Center, Space Sciences Building, Cornell University, Ithaca, New York 14853 and John F. Chandler and Irwin I. Shapiro Harvard–Smithsonian Center for Astrophysics, 60 Garden Street, Cambridge, Massachusets 02138 Received August 30, 2001; revised February 21, 2002 was discovered on August 6, 1980, by H.-E. Schuster at the We report Doppler-only (cw) radar observations of basaltic near- European Southern Observatory in La Silla (Marsden 1980). It Earth asteroid 3908 Nyx obtained at Arecibo and Goldstone in was the subject of an extensive observational campaign at visi- September and October of 1988. The circular polarization ratio of ble, infrared, and radar wavelengths during its approach within 0.75 ± 0.03 exceeds ∼90% of those reported among radar-detected 0.062 AU of Earth in October 1988. Lightcurves obtained in near- Earth asteroids and it implies an extremely rough near-surface 1988 (Drummond and Wisniewski 1990) and in 1996 by Pravec at centimeter-to-decimeter spatial scales. Echo power spectra over and co-workers (in preparation) indicate direct rotation with a narrow longitudinal intervals show a central dip indicative of at 4.426-h period and yield two pole direction solutions that pro- least one significant concavity. -
– Near-Earth Asteroid Mission Concept Study –
ASTEX – Near-Earth Asteroid Mission Concept Study – A. Nathues1, H. Boehnhardt1 , A. W. Harris2, W. Goetz1, C. Jentsch3, Z. Kachri4, S. Schaeff5, N. Schmitz2, F. Weischede6, and A. Wiegand5 1 MPI for Solar System Research, 37191 Katlenburg-Lindau, Germany 2 DLR, Institute for Planetary Research, 12489 Berlin, Germany 3 Astrium GmbH, 88039 Friedrichshafen, Germany 4 LSE Space AG, 82234 Oberpfaffenhofen, Germany 5 Astos Solutions, 78089 Unterkirnach, Germany 6 DLR GSOC, 82234 Weßling, Germany ASTEX Marco Polo Symposium, Paris 18.5.09, A. Nathues - 1 Primary Objectives of the ASTEX Study Identification of the required technologies for an in-situ mission to two near-Earth asteroids. ¾ Selection of realistic mission scenarios ¾ Definition of the strawman payload ¾ Analysis of the requirements and options for the spacecraft bus, the propulsion system, the lander system, and the launcher ASTEX ¾ Definition of the requirements for the mission’s operational ground segment Marco Polo Symposium, Paris 18.5.09, A. Nathues - 2 ASTEX Primary Mission Goals • The mission scenario foresees to visit two NEAs which have different mineralogical compositions: one “primitive'‘ object and one fragment of a differentiated asteroid. • The higher level goal is the provision of information and constraints on the formation and evolution history of our planetary system. • The immediate mission goals are the determination of: – Inner structure of the targets – Physical parameters (size, shape, mass, density, rotation period and spin vector orientation) – Geology, mineralogy, and chemistry ASTEX – Physical surface properties (thermal conductivity, roughness, strength) – Origin and collisional history of asteroids – Link between NEAs and meteorites Marco Polo Symposium, Paris 18.5.09, A. -
The Geological Record of Meteorite Impacts
THE GEOLOGICAL RECORD OF METEORITE IMPACTS Gordon R. Osinski Canadian Space Agency, 6767 Route de l'Aeroport, St-Hubert, QC J3Y 8Y9 Canada, Email: [email protected] ABSTRACT 2. FORMATION OF METEORITE IMPACT STRUCTURES Meteorite impact structures are found on all planetary bodies in the Solar System with a solid The formation of hypervelocity impact craters has surface. On the Moon, Mercury, and much of Mars, been divided, somewhat arbitrarily, into three main impact craters are the dominant landform. On Earth, stages [3] (Fig. 2): (1) contact and compression, (2) 174 impact sites have been recognized, with several excavation, and (3) modification. A further stage of more new craters being discovered each year. The “hydrothermal and chemical alteration” is also terrestrial impact cratering record is critical for our considered as a separate, final stage in the cratering understanding of impacts as it currently provides the process (e.g., [4]), and is also described below. only ground-truth data on which to base interpretations of the cratering record of other planets and moons. In this contribution, I summarize the processes and products of impact cratering and provide and an up-to-date assessment of the geological record of meteorite impacts. 1. INTRODUCTION It is now widely recognized that impact cratering is a ubiquitous geological process that affects all planetary objects with a solid surface (e.g., [1]). One only has to look up on a clear night to see that impact structures are the dominant landform on the Moon. The same can be said of all the rocky and icy bodies in the solar system that have retained portions of their earliest crust. -
CCD Astrometric Observations of 2017 VR12, Camillo and Midas 3
Research in Astronomy and Astrophysics manuscript no. (LATEX: CCD˙astrometric˙observations˙of˙2017˙VR12,Camillo˙and˙Midas.tex; printed on November 19, 2018; 1:37) CCD astrometric observations of 2017 VR12, Camillo and Midas Zhen-Jun Zhang1,2,3, Yi-Gong Zhang1,2,3, Xiang-Ming Chen1,2, Jian-Cheng Wang1,2 and Jie-Su1,2 1 Yunnan Observatories, Chinese Academy of Sciences, Kunming 650216, China; [email protected] 2 Key Laboratory of the Structure and Evolution of Celestial Objects, Chinese Academy of Sciences, Kunming 650216, China 3 University of Chinese Academy of Sciences, Beijing 100049, China Received 20xx month day; accepted 20xx month day Abstract We have observed three near-Earth objects(NEOs), 2017VR12, Camillo, and Midas during the year 2018. The observations were made by the 1-m telescope of Yunnan Observatory over 2 nights. Their precise astrometric positions are derived from 989 CCD observations. The theoretical positions of asteroids are retrieved from the Jet Propulsion Laboratory (JPL) Horizons System and Institut de M´ecanique C´eleste et de Calcul des Eph´em´erides´ (IMCCE). The positions of three asteroids are measured with respect to the stars in Gaia DR2 star catalogue. For 2017 VR12, the mean (O-C) of right ascension and ′′ ′′ declination are -0.090 and -0.623 based on the ephemeris of published JPL, but the mean ′′ ′′ (O-C) are 3.122 and -0.636 based on the ephemeris of published IMCCE. The great differ- ence in declination could be explained by several factors. (1)The degenerated CCD images caused by the high apparent motion speed of the object leads to the reduction of position- ing accuracy. -
Surveillance and Opportunities for Observing Near-Earth Objects
Surveillance and opportunities for observing Near-Earth Objects. Mirel Birlan1;2, Adrian Sonka2;3, Andreea Gornea2, Simon Anghel2, Alin Nedelcu2;1, Francois Colas1, and Pierre Vernazza4 1 Institut de Mecanique Celeste et des Calculs des Ephemerides, CNRS UMR8028, Paris Observatory, PSL Research University, 77 av Denfert Rochereau, 75014 Paris, France 2 Astronomical Institute of Romanian Academy, Str. Cutitul de Argint 5, 040557 Bucharest, Romania 3 Faculty of Physics, University of Bucharest 405-Atomistilor, 077125 Magurele, Ilfov, Romania 4 Aix-Marseille University, CNRS, Laboratoire d’Astrophysique de Marseille, Marseille, France contact e-mail: [email protected] More than 17,000 Near Earth Objects have been discovered so far. Their relatively small diame- ters, between 10 meters to kilometre-size, make them visible from groundbased observations only for their closest approach to Earth. On average this occurs only few times per century. Thus, it is vital to exploit such favourable geometries and to record as much as possible information concerning their dynamics and their physical properties. We will briefly present new results ob- tained using the 1meter telescope of Pic du Midi Observatory and s using the 0.4meter telescope in Bucharest recent results in photometry for Florence, 2012 TC4, and 2018 GE3. The presenta- tion will include also the new spectrograph installed in Pic du Midi and devoted to NEOs, which will cover the spectral interval between 0.5 and 1.6 micron. Recent observations of 3200 Phaethon and 1981 Midas M. Husarik1 and O. V. Ivanova1;2 1 Astronomical Institute of the SAS, 05960 Tatranská Lomnica, Slovakia 2 Main Astronomical Observatory, National Academy of Sciences of Ukraine, Kyiv, 03680 Ukraine contact e-mail: [email protected] We will review recent photometric observations of two asteroids – 3200 Phaethon and 1981 Midas. -
Impact Cratering – Fundamental Process in Geoscience and Planetary Science
Impact cratering – fundamental process in geoscience and planetary science JKPati1 and WUReimold2 1Department of Earth and Planetary Sciences, Nehru Science Centre, University of Allahabad, Allahabad 211 002, India. e-mail: [email protected] 2Museum f. Natural History (Mineralogy), Humboldt-University in Berlin, Invalidenstrasse 43, D-10115 Berlin, Germany. e-mail: [email protected] Impact cratering is a geological process characterized by ultra-fast strain rates, which generates extreme shock pressure and shock temperature conditions on and just below planetary surfaces. Despite initial skepticism, this catastrophic process has now been widely accepted by geoscientists with respect to its importance in terrestrial – indeed, in planetary – evolution. About 170 impact structures have been discovered on Earth so far, and some more structures are considered to be of possible impact origin. One major extinction event, at the Cretaceous–Paleogene boundary, has been firmly linked with catastrophic impact, but whether other important extinction events in Earth history, including the so-called “Mother of All Mass Extinctions” at the Permian–Triassic boundary, were triggered by huge impact catastrophes is still hotly debated and a subject of ongoing research. There is a beneficial side to impact events as well, as some impact structures worldwide have been shown to contain significant (in some cases, world class) ore deposits, including the gold– uranium province of the Witwatersrand basin in South Africa, the enormous Ni and PGE deposits of the Sudbury structure in Canada, as well as important hydrocarbon resources, especially in North America. Impact cratering is not a process of the past, and it is mandatory to improve knowledge of the past-impact record on Earth to better constrain the probability of such events in the future.