(704) Interamnia from Its Occultations and Lightcurves
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ESO's VLT Sphere and DAMIT
ESO’s VLT Sphere and DAMIT ESO’s VLT SPHERE (using adaptive optics) and Joseph Durech (DAMIT) have a program to observe asteroids and collect light curve data to develop rotating 3D models with respect to time. Up till now, due to the limitations of modelling software, only convex profiles were produced. The aim is to reconstruct reliable nonconvex models of about 40 asteroids. Below is a list of targets that will be observed by SPHERE, for which detailed nonconvex shapes will be constructed. Special request by Joseph Durech: “If some of these asteroids have in next let's say two years some favourable occultations, it would be nice to combine the occultation chords with AO and light curves to improve the models.” 2 Pallas, 7 Iris, 8 Flora, 10 Hygiea, 11 Parthenope, 13 Egeria, 15 Eunomia, 16 Psyche, 18 Melpomene, 19 Fortuna, 20 Massalia, 22 Kalliope, 24 Themis, 29 Amphitrite, 31 Euphrosyne, 40 Harmonia, 41 Daphne, 51 Nemausa, 52 Europa, 59 Elpis, 65 Cybele, 87 Sylvia, 88 Thisbe, 89 Julia, 96 Aegle, 105 Artemis, 128 Nemesis, 145 Adeona, 187 Lamberta, 211 Isolda, 324 Bamberga, 354 Eleonora, 451 Patientia, 476 Hedwig, 511 Davida, 532 Herculina, 596 Scheila, 704 Interamnia Occultation Event: Asteroid 10 Hygiea – Sun 26th Feb 16h37m UT The magnitude 11 asteroid 10 Hygiea is expected to occult the magnitude 12.5 star 2UCAC 21608371 on Sunday 26th Feb 16h37m UT (= Mon 3:37am). Magnitude drop of 0.24 will require video. DAMIT asteroid model of 10 Hygiea - Astronomy Institute of the Charles University: Josef Ďurech, Vojtěch Sidorin Hygiea is the fourth-largest asteroid (largest is Ceres ~ 945kms) in the Solar System by volume and mass, and it is located in the asteroid belt about 400 million kms away. -
Asteroid Family Ages. 2015. Icarus 257, 275-289
Icarus 257 (2015) 275–289 Contents lists available at ScienceDirect Icarus journal homepage: www.elsevier.com/locate/icarus Asteroid family ages ⇑ Federica Spoto a,c, , Andrea Milani a, Zoran Knezˇevic´ b a Dipartimento di Matematica, Università di Pisa, Largo Pontecorvo 5, 56127 Pisa, Italy b Astronomical Observatory, Volgina 7, 11060 Belgrade 38, Serbia c SpaceDyS srl, Via Mario Giuntini 63, 56023 Navacchio di Cascina, Italy article info abstract Article history: A new family classification, based on a catalog of proper elements with 384,000 numbered asteroids Received 6 December 2014 and on new methods is available. For the 45 dynamical families with >250 members identified in this Revised 27 April 2015 classification, we present an attempt to obtain statistically significant ages: we succeeded in computing Accepted 30 April 2015 ages for 37 collisional families. Available online 14 May 2015 We used a rigorous method, including a least squares fit of the two sides of a V-shape plot in the proper semimajor axis, inverse diameter plane to determine the corresponding slopes, an advanced error model Keywords: for the uncertainties of asteroid diameters, an iterative outlier rejection scheme and quality control. The Asteroids best available Yarkovsky measurement was used to estimate a calibration of the Yarkovsky effect for each Asteroids, dynamics Impact processes family. The results are presented separately for the families originated in fragmentation or cratering events, for the young, compact families and for the truncated, one-sided families. For all the computed ages the corresponding uncertainties are provided, and the results are discussed and compared with the literature. The ages of several families have been estimated for the first time, in other cases the accu- racy has been improved. -
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, -
Surface Composition of Icy Asteroids and the Special Case of Ceres
Surface composition of icy asteroids and the special case of Ceres P. Vernazza (Laboratoire d’Astrophysique de Marseille) March 15, 2017 SOFIA Tele-Talk Examples of asteroids with Compositional links between asteroids and meteorites meteoritic analogues Falls Mass in the asteroid belt 6.2% 9.6% 80.0% 8.4% 1.9% 1.0% 1.1% 0.4% 2.5% 0.1% 1.5% 7.0% 4.6% 3.3% Total Total ~98% ~30% Vernazza & Beck 2016 ~2/3 of the mass of the asteroid belt seems absent from our meteorite collections 6 asteroid types, representing ~2/3 of the main belt mass (DeMeo & Carry 2013), are presently unconnected to meteorites. Asteroid spectral properties (DeMeo et al. 2009) Metamorphosed CI/CM chondrites as analogues of most B, C, Cb, Cg types? (1) Metamorphosed CI/CM chondrites as analogues of most B, C, Cb, Cg types? (2) This is very unlikely because: a) Metamorphosed CI/CM chondrites represent 0.2% of the falls whereas B, C, Cb and Cg type represent ~50% of the mass of the belt b) Metamorphosed CI/CM chondrites possess a significantly higher density (2.5-3 g/cm3) than those asteroid types (0.8-1.5 g/cm3) c) Metamorphosed CI/CM chondrites possess different spectral properties in the mid-infrared with respect to those asteroid types Why are most B, C, Cb, Cg, P and D types unsampled by our meteorite collections? The lack of samples for these objects within our collections may stem from the fact that they are volatile-rich as implied by their low density (0.8-2 g/cm3) and their comet-like activity in some cases. -
Small Vehicle Asteroid Mission Concept
The “Bering” Small Vehicle Asteroid Mission Concept The “Bering” Small Vehicle Asteroid Mission Concept. Rene Michelsen1, Anja Andersen2, Henning Haack3, John L. Jørgensen4, Maurizio Betto4, Peter S. Jørgensen4, 1Astronomical Observatory, University of Copenhagen, Juliane Maries Vej 30, 2100 Copenhagen Denmark, Phone: +45 3532 5929, Fax: +45 3532 5989, e-mail: [email protected] 2Nordita, Blegdamsvej 17, 2100 Copenhagen, Denmark, Phone: +45 3532 5501, Fax: +45 3538 9157, e-mail: [email protected]. 3Geological Museum, University of Copenhagen, Øster Voldgade 5-7, 1350 Copenhagen K, Denmark Phone: +45 3532 2367, Fax: +45 3532 2325, e-mail: [email protected] 4Ørsted*DTU, MIS, Building 327, Technical University of Denmark, 2800 Lyngby, Denmark, Phone +45 4525 3438, Fax: +45 4588 7133, e-mail: [email protected], mbe@…, psj@… Abstract The study of the Asteroids is traditionally performed by means of large Earth based telescopes, by which orbital elements and spectral properties are acquired. Space borne research, has so far been limited to a few occasional flybys and a couple of dedicated flights to a single selected target. While the telescope based research offers precise orbital information, it is limited to the brighter, larger objects, and taxonomy as well as morphology resolution is limited. Conversely, dedicated missions offers detailed surface mapping in radar, visual and prompt gamma, but only for a few selected targets. The dilemma obviously being the resolution vs. distance and the statistics vs. delta-V requirements. Using advanced instrumentation and onboard autonomy, we have developed a space mission concept whose goal is to map the flux, size and taxonomy distributions of the Asteroids. -
In Pursuit of the GENUINE CHRISTIAN IMAGE
In Pursuit of THE GENUINE CHRISTIAN IMAGE Erland Forsberg as a Lutheran Producer of Icons in the Fields of Culture and Religion Juha Malmisalo Academic dissertation To be publicly discussed, by permission of the Faculty of Theology of the University of Helsinki, in Auditorium XII in the Main Building of the University, on May 14, 2005, at 10 am. Helsinki 2005 1 In Pursuit of THE GENUINE CHRISTIAN IMAGE Erland Forsberg as a Lutheran Producer of Icons in the Fields of Culture and Religion Juha Malmisalo Helsinki 2005 2 ISBN 952-91-8539-1 (nid.) ISBN 952-10-2414-3 (PDF) University Printing House Helsinki 2005 3 Contents Abbreviations .......................................................................................................... 4 Abstract ................................................................................................................... 6 Preface ..................................................................................................................... 7 1. Encountering Peripheral Cultural Phenomena ......................................... 9 1.1. Forsberg’s Icon Painting in Art Sociological Analysis: Conceptual Issues and Selected Perspectives ............................................................ 9 1.2. An Adaptation of Bourdieu’s Theory of Cultural Fields .......................... 18 1.3. The Pictorial Source Material: Questions of Accessibility and Method .. 23 2. Attempts at a Field-Constitution ................................................................ 30 2.1. Educational, Social, and -
New Double Stars from Asteroidal Occultations, 1971 - 2008
Vol. 6 No. 1 January 1, 2010 Journal of Double Star Observations Page 88 New Double Stars from Asteroidal Occultations, 1971 - 2008 Dave Herald, Canberra, Australia International Occultation Timing Association (IOTA) Robert Boyle, Carlisle, Pennsylvania, USA Dickinson College David Dunham, Greenbelt, Maryland, USA; Toshio Hirose, Tokyo, Japan; Paul Maley, Houston, Texas, USA; Bradley Timerson, Newark, New York, USA International Occultation Timing Association (IOTA) Tim Farris, Gallatin, Tennessee, USA Volunteer State Community College Eric Frappa and Jean Lecacheux, Paris, France Observatoire de Paris Tsutomu Hayamizu, Kagoshima, Japan Sendai Space Hall Marek Kozubal, Brookline, Massachusetts, USA Clay Center Richard Nolthenius, Aptos, California, USA Cabrillo College and IOTA Lewis C. Roberts, Jr., Pasadena, California, USA California Institute of Technology/Jet Propulsion Laboratory David Tholen, Honolulu, Hawaii, USA University of Hawaii E-mail: [email protected] Abstract: Observations of occultations by asteroids and planetary moons can detect double stars with separations in the range of about 0.3” to 0.001”. This paper lists all double stars detected in asteroidal occultations up to the end of 2008. It also provides a general explanation of the observational method and analysis. The incidence of double stars with a separation in the range 0.001” to 0.1” with a magnitude difference less than 2 is estimated to be about 1%. Vol. 6 No. 1 January 1, 2010 Journal of Double Star Observations Page 89 New Double Stars from Asteroidal Occultations, 1971 - 2008 tions. More detail about the method of analysis is set Introduction out in the Appendix. Asteroids and planetary moons will naturally oc- cult many stars as they move through the sky. -
Aqueous Alteration on Main Belt Primitive Asteroids: Results from Visible Spectroscopy1
Aqueous alteration on main belt primitive asteroids: results from visible spectroscopy1 S. Fornasier1,2, C. Lantz1,2, M.A. Barucci1, M. Lazzarin3 1 LESIA, Observatoire de Paris, CNRS, UPMC Univ Paris 06, Univ. Paris Diderot, 5 Place J. Janssen, 92195 Meudon Pricipal Cedex, France 2 Univ. Paris Diderot, Sorbonne Paris Cit´e, 4 rue Elsa Morante, 75205 Paris Cedex 13 3 Department of Physics and Astronomy of the University of Padova, Via Marzolo 8 35131 Padova, Italy Submitted to Icarus: November 2013, accepted on 28 January 2014 e-mail: [email protected]; fax: +33145077144; phone: +33145077746 Manuscript pages: 38; Figures: 13 ; Tables: 5 Running head: Aqueous alteration on primitive asteroids Send correspondence to: Sonia Fornasier LESIA-Observatoire de Paris arXiv:1402.0175v1 [astro-ph.EP] 2 Feb 2014 Batiment 17 5, Place Jules Janssen 92195 Meudon Cedex France e-mail: [email protected] 1Based on observations carried out at the European Southern Observatory (ESO), La Silla, Chile, ESO proposals 062.S-0173 and 064.S-0205 (PI M. Lazzarin) Preprint submitted to Elsevier September 27, 2018 fax: +33145077144 phone: +33145077746 2 Aqueous alteration on main belt primitive asteroids: results from visible spectroscopy1 S. Fornasier1,2, C. Lantz1,2, M.A. Barucci1, M. Lazzarin3 Abstract This work focuses on the study of the aqueous alteration process which acted in the main belt and produced hydrated minerals on the altered asteroids. Hydrated minerals have been found mainly on Mars surface, on main belt primitive asteroids and possibly also on few TNOs. These materials have been produced by hydration of pristine anhydrous silicates during the aqueous alteration process, that, to be active, needed the presence of liquid water under low temperature conditions (below 320 K) to chemically alter the minerals. -
Sciences, Is the Discovery of Twenty-Two Minor Planets Commonly Known As the Watson Asteriods
ASTRONOMY: A. O. LEUSCHNER 67 ADMISSIONS TO SICK REPORT-Concluded UNITED STATES NUMBERS opFr White Colored INTERNA- TIONAL CLASSIFICA- Mean strength..................................................... 545,518 13,150 TIONT Causes of admission to sick report Ratio perstrength1000 of mean 00-02, 07,15, 16,24- 27,29- 31,49, 57,58, 60,61, Traumatisms, others ............................... 9.14 10.04 63-65, 70-72, 74,76- 78,82- 84,97- 99 80 Sunstroke.. 0.04 0.08 Total for diseases................................. 882.51 1064.41 Total for external causes.. 91.69 90.42 Grand total................... ................ 974.19 1154.83 PERTURBATIONS AND TABLES OF THE MINOR PLANETS DISCOVERED BY JAMES C. WATSON BY ARMIN 0. LEUSCHNER BERKELEY ASTRONOMICAL DEPARTMENT, UNIVERSITY OF CALIFORNIA Read before the Academy, April 16, 1916 Among the many important contributions to Astronomical Science by James C. Watson, one of the original members of the National Academy of Sciences, is the discovery of twenty-two minor planets commonly known as the Watson asteriods. The first of these, (79) Eurynome, was discovered at Ann Arbor on September 14, 1863, and the last, (179) Klytaemnestra, on November 11, 1877, three years before his death. By his will a fund was bequeathed in trust to the National Academy of Sciences for the purpose of promoting astronomical research. One of the objects specifically designated was the construction of tables of the perturbations of the minor planets dis- covered by the testator. From the beginning Prof. Simon Newcomb was a Downloaded by guest on September 30, 2021 68 ASTRONOMY: A. O. LEUSCHNER member of the board of Watson Trustees; later he became chairman of the board, and remained in that capacity on the board until his death in 1908, being succeeded by Prof. -
Precise Astrometry and Diameters of Asteroids from Occultations – a Data-Set of Observations and Their Interpretation
MNRAS 000,1–22 (2020) Preprint 14 October 2020 Compiled using MNRAS LATEX style file v3.0 Precise astrometry and diameters of asteroids from occultations – a data-set of observations and their interpretation David Herald 1¢, David Gault2, Robert Anderson3, David Dunham4, Eric Frappa5, Tsutomu Hayamizu6, Steve Kerr7, Kazuhisa Miyashita8, John Moore9, Hristo Pavlov10, Steve Preston11, John Talbot12, Brad Timerson (deceased)13 1Trans Tasman Occultation Alliance, [email protected] 2Trans Tasman Occultation Alliance, [email protected] 3International Occultation Timing Association, [email protected] 4International Occultation Timing Association, [email protected] 5Euraster, [email protected] 6Japanese Occultation Information Network, [email protected] 7Trans Tasman Occultation Alliance, [email protected] 8Japanese Occultation Information Network, [email protected] 9International Occultation Timing Association, [email protected] 10International Occultation Timing Association – European Section, [email protected] 11International Occultation Timing Association, [email protected] 12Trans Tasman Occultation Alliance, [email protected] 13International Occultation Timing Association, deceased Accepted XXX. Received YYY; in original form ZZZ ABSTRACT Occultations of stars by asteroids have been observed since 1961, increasing from a very small number to now over 500 annually. We have created and regularly maintain a growing data-set of more than 5,000 observed asteroidal occultations. The data-set includes: the raw observations; astrometry at the 1 mas level based on centre of mass or figure (not illumination); where possible the asteroid’s diameter to 5 km or better, and fits to shape models; the separation and diameters of asteroidal satellites; and double star discoveries with typical separations being in the tens of mas or less. -
Hydrated Minerals on Asteroids: the Astronomical Record
Hydrated Minerals on Asteroids: The Astronomical Record A. S. Rivkin, E. S. Howell, F. Vilas, and L. A. Lebofsky March 28, 2002 Corresponding Author: Andrew Rivkin MIT 54-418 77 Massachusetts Ave. Cambridge MA, 02139 [email protected] 1 1 Abstract Knowledge of the hydrated mineral inventory on the asteroids is important for deducing the origin of Earth’s water, interpreting the meteorite record, and unraveling the processes occurring during the earliest times in solar system history. Reflectance spectroscopy shows absorption features in both the 0.6-0.8 and 2.5-3.5 pm regions, which are diagnostic of or associated with hydrated minerals. Observations in those regions show that hydrated minerals are common in the mid-asteroid belt, and can be found in unex- pected spectral groupings, as well. Asteroid groups formerly associated with mineralogies assumed to have high temperature formation, such as MAand E-class asteroids, have been observed to have hydration features in their reflectance spectra. Some asteroids have apparently been heated to several hundred degrees Celsius, enough to destroy some fraction of their phyllosili- cates. Others have rotational variation suggesting that heating was uneven. We summarize this work, and present the astronomical evidence for water- and hydroxyl-bearing minerals on asteroids. 2 Introduction Extraterrestrial water and water-bearing minerals are of great importance both for understanding the formation and evolution of the solar system and for supporting future human activities in space. The presence of water is thought to be one of the necessary conditions for the formation of life as 2 we know it. -
Iso and Asteroids
r bulletin 108 Figure 1. Asteroid Ida and its moon Dactyl in enhanced colour. This colour picture is made from images taken by the Galileo spacecraft just before its closest approach to asteroid 243 Ida on 28 August 1993. The moon Dactyl is visible to the right of the asteroid. The colour is ‘enhanced’ in the sense that the CCD camera is sensitive to near-infrared wavelengths of light beyond human vision; a ‘natural’ colour picture of this asteroid would appear mostly grey. Shadings in the image indicate changes in illumination angle on the many steep slopes of this irregular body, as well as subtle colour variations due to differences in the physical state and composition of the soil (regolith). There are brighter areas, appearing bluish in the picture, around craters on the upper left end of Ida, around the small bright crater near the centre of the asteroid, and near the upper right-hand edge (the limb). This is a combination of more reflected blue light and greater absorption of near-infrared light, suggesting a difference Figure 2. This image mosaic of asteroid 253 Mathilde is in the abundance or constructed from four images acquired by the NEAR spacecraft composition of iron-bearing on 27 June 1997. The part of the asteroid shown is about 59 km minerals in these areas. Ida’s by 47 km. Details as small as 380 m can be discerned. The moon also has a deeper near- surface exhibits many large craters, including the deeply infrared absorption and a shadowed one at the centre, which is estimated to be more than different colour in the violet than any 10 km deep.