Proceedings of the Symposium on the Study of the Sun and Interplanetary Medium in Three Dimensions
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From: "MESSENGER, SCOTT R
The Starting Materials In: Meteorites and the Early Solar System II S. Messenger Johnson Space Center S. Sandford Ames Research Center D. Brownlee University of Washington Combined information from observations of interstellar clouds and star forming regions and studies of primitive solar system materials give a first order picture of the starting materials for the solar system’s construction. At the earliest stages, the presolar dust cloud was comprised of stardust, refractory organic matter, ices, and simple gas phase molecules. The nature of the starting materials changed dramatically together with the evolving solar system. Increasing temperatures and densities in the disk drove molecular evolution to increasingly complex organic matter. High temperature processes in the inner nebula erased most traces of presolar materials, and some fraction of this material is likely to have been transported to the outermost, quiescent portions of the disk. Interplanetary dust particles thought to be samples of Kuiper Belt objects probably contain the least altered materials, but also contain significant amounts of solar system materials processed at high temperatures. These processed materials may have been transported from the inner, warmer portions of the disk early in the active accretion phase. 1. Introduction A principal constraint on the formation of the Solar System was the population of starting materials available for its construction. Information on what these starting materials may have been is largely derived from two approaches, namely (i) the examination of other nascent stellar systems and the dense cloud environments in which they form, and (ii) the study of minimally altered examples of these starting materials that have survived in ancient Solar System materials. -
Asteroidal Dust 423
Dermott et al.: Asteroidal Dust 423 Asteroidal Dust Stanley F. Dermott University of Florida Daniel D. Durda Southwest Research Institute Keith Grogan NASA Goddard Space Flight Center Thomas J. J. Kehoe University of Florida There is good evidence that the high-speed, porous, anhydrous chondritic interplanetary dust particles (IDPs) collected in Earth’s stratosphere originated from short-period comets. How- ever, by considering the structure of the solar-system dust bands discovered by IRAS, we are able to show that asteroidal collisions are probably the dominant source of particles in the zodiacal cloud. It follows that a significant and probably the dominant fraction of the IDPs collected in Earth’s stratosphere also originated from asteroids. IDPs are the most primitive particles in the inner solar system and represent a class of material quite different from that in our meteorite collections. The structure, mineralogy, and high C content of IDPs dictate that they cannot have originated from the grinding down of known meteorite types. We argue that the asteroidal IDPs were probably formed as a result of prolonged mechanical mixing in the deep regoliths of asteroidal rubble piles in the outer main belt. 1. INTRODUCTION information on the nature of the particles in the preplanetary solar nebula (Bradley, 1999). Observations of microcraters In our collections on Earth, we have an abundance of on the Long Duration Exposure Facility (LDEF) confirmed meteorite samples from three major sources of extraterres- that each year Earth accretes 3 × 107 kg of dust particles, a trial material: the asteroid belt, the Moon, and Mars. Some mass influx ~100× greater than the influx associated with of the source bodies of these meteorites have experienced the much larger meteorites that have masses between 100 g major physical, chemical, and mineralogical changes since and 1000 kg. -
Urea, Glycolic Acid, and Glycerol in an Organic Residue Produced by Ultraviolet Irradiation of Interstellar=Pre-Cometary Ice Analogs
ASTROBIOLOGY Volume 10, Number 2, 2010 ª Mary Ann Liebert, Inc. DOI: 10.1089=ast.2009.0358 Urea, Glycolic Acid, and Glycerol in an Organic Residue Produced by Ultraviolet Irradiation of Interstellar=Pre-Cometary Ice Analogs Michel Nuevo,1,2 Jan Hendrik Bredeho¨ft,3 Uwe J. Meierhenrich,4 Louis d’Hendecourt,1 and Wolfram H.-P. Thiemann3 Abstract More than 50 stable organic molecules have been detected in the interstellar medium (ISM), from ground-based and onboard-satellite astronomical observations, in the gas and solid phases. Some of these organics may be prebiotic compounds that were delivered to early Earth by comets and meteorites and may have triggered the first chemical reactions involved in the origin of life. Ultraviolet irradiation of ices simulating photoprocesses of cold solid matter in astrophysical environments have shown that photochemistry can lead to the formation of amino acids and related compounds. In this work, we experimentally searched for other organic molecules of prebiotic interest, namely, oxidized acid labile compounds. In a setup that simulates conditions relevant to the ISM and Solar System icy bodies such as comets, a condensed CH3OH:NH3 ¼ 1:1 ice mixture was UV irradiated at *80 K. The molecular constituents of the nonvolatile organic residue that remained at room temperature were separated by capillary gas chromatography and identified by mass spectrometry. Urea, glycolic acid, and glycerol were detected in this residue, as well as hydroxyacetamide, glycerolic acid, and glycerol amide. These organics are interesting target molecules to be searched for in space. Finally, tentative mechanisms of formation for these compounds under interstellar=pre-cometary conditions are proposed. -
The Analysis of Interplanetary Dust Particles
WORKSHOP ON THE ANALYSIS OF INTERPLANETARY DUST PARTICLES LPI Technical Report Number 94-02 Lunar and Planetary Institute 3600 Bay Area Boulevard Houston TX 77058-1113 LPIITR--94-02 WORKSHOP ON THE ANALYSIS OF INTERPLANETARY DUST PARTICLES Edited by M. Zolensky Held at Lunar and Planetary Institute May 15-17, 1993 Sponsored by Lunar and Planetary Institute Lunar and Planetary Institute 3600 Bay Area Boulevard Houston TX 77058-1113 LPI Technical Report Number 94-02 LPIITR--94-02 Compiled in 1994 by LUNAR AND PLANETARY INSTITUTE The Institute is operated by the University Space Research Association under Contract No. NASW-4574 with the National Aeronautics and Space Administration. Material in this volume may be copied without restraint for library, abstract service, education, or personal research purposes; however, republication of any paper or portion thereof requires the written permission of the authors as well as the appropriate acknowledgment of this publication. This report may be cited as M. Zolensky, ed. (1994) Workshop on the Analysis ofInterplanetary Dust Particles. LPI Tech. Rpt. 94-02, Lunar and Planetary Institute, Houston. 62 pp. This report is distributed by ORDER DEPARTMENT Lunar and Planetary Institute 3600 Bay Area Boulevard Houston TX 77058-1113 Mail order requestors will be invoiced for the cost of shipping and handling. Cover. Backscattered electron image of a hydrated, chondritic interplanetary dust particle, measuring 17).1m across. LPT Technical Report 94-02 iii Program Saturday, May 15, 1993 7:30-8:30 a.m. Registration and Continental Breakfast 8:30 a.m.-5:00 p.m. INVITED PRESENTATIONS AND DISCUSSION TOPICS An Overview ofthe Origin and Role ofDust in the Early Solar System D. -
Annual Report 2017 - 2018 Annual Report 2017 - 2018 Citizens’ Charter of Department of Space
GSAT-17 Satellites Images icro M sat ries Satellit Se e -2 at s to r a C 0 SAT-1 4 G 9 -C V L S P III-D1 -Mk LV GS INS -1 C Asia Satell uth ite o (G S S A T - 09 9 LV-F ) GS ries Sat Se ellit t-2 e sa to 8 r -C3 a LV C PS Annual Report 2017 - 2018 Annual Report 2017 - 2018 Citizens’ Charter of Department Of Space Department Of Space (DOS) has the primary responsibility of promoting the development of space science, technology and applications towards achieving self-reliance and facilitating in all round development of the nation. With this basic objective, DOS has evolved the following programmes: • Indian National Satellite (INSAT) programme for telecommunication, television broadcasting, meteorology, developmental education, societal applications such as telemedicine, tele-education, tele-advisories and similar such services • Indian Remote Sensing (IRS) satellite programme for the management of natural resources and various developmental projects across the country using space based imagery • Indigenous capability for the design and development of satellite and associated technologies for communications, navigation, remote sensing and space sciences • Design and development of launch vehicles for access to space and orbiting INSAT / GSAT, IRS and IRNSS satellites and space science missions • Research and development in space sciences and technologies as well as application programmes for national development The Department Of Space is committed to: • Carrying out research and development in satellite and launch vehicle technology with a goal to achieve total self reliance • Provide national space infrastructure for telecommunications and broadcasting needs of the country • Provide satellite services required for weather forecasting, monitoring, etc. -
Small Satellite Launchers
SMALL SATELLITE LAUNCHERS NewSpace Index 2020/04/20 Current status and time from development start to the first successful or planned orbital launch NEWSPACE.IM Northrop Grumman Pegasus 1990 Scorpius Space Launch Demi-Sprite ? Makeyev OKB Shtil 1998 Interorbital Systems NEPTUNE N1 ? SpaceX Falcon 1e 2008 Interstellar Technologies Zero 2021 MT Aerospace MTA, WARR, Daneo ? Rocket Lab Electron 2017 Nammo North Star 2020 CTA VLM 2020 Acrux Montenegro ? Frontier Astronautics ? ? Earth to Sky ? 2021 Zero 2 Infinity Bloostar ? CASIC / ExPace Kuaizhou-1A (Fei Tian 1) 2017 SpaceLS Prometheus-1 ? MISHAAL Aerospace M-OV ? CONAE Tronador II 2020 TLON Space Aventura I ? Rocketcrafters Intrepid-1 2020 ARCA Space Haas 2CA ? Aerojet Rocketdyne SPARK / Super Strypi 2015 Generation Orbit GoLauncher 2 ? PLD Space Miura 5 (Arion 2) 2021 Swiss Space Systems SOAR 2018 Heliaq ALV-2 ? Gilmour Space Eris-S 2021 Roketsan UFS 2023 Independence-X DNLV 2021 Beyond Earth ? ? Bagaveev Corporation Bagaveev ? Open Space Orbital Neutrino I ? LIA Aerospace Procyon 2026 JAXA SS-520-4 2017 Swedish Space Corporation Rainbow 2021 SpinLaunch ? 2022 Pipeline2Space ? ? Perigee Blue Whale 2020 Link Space New Line 1 2021 Lin Industrial Taymyr-1A ? Leaf Space Primo ? Firefly 2020 Exos Aerospace Jaguar ? Cubecab Cab-3A 2022 Celestia Aerospace Space Arrow CM ? bluShift Aerospace Red Dwarf 2022 Black Arrow Black Arrow 2 ? Tranquility Aerospace Devon Two ? Masterra Space MINSAT-2000 2021 LEO Launcher & Logistics ? ? ISRO SSLV (PSLV Light) 2020 Wagner Industries Konshu ? VSAT ? ? VALT -
Production of Cosmic Dust by Hydrous and Anhydrous Asteroids: Implications for the Production of Interplanetary Dust Particles and Micrometeorites
40th Lunar and Planetary Science Conference (2009) 1164.pdf PRODUCTION OF COSMIC DUST BY HYDROUS AND ANHYDROUS ASTEROIDS: IMPLICATIONS FOR THE PRODUCTION OF INTERPLANETARY DUST PARTICLES AND MICROMETEORITES. G. J. Flynn 1, D. D. Durda 2, M. A. Minnick 3, and M. Strait 3. 1Dept. of Physics, SUNY-Plattsburgh, 101 Broad St., Platts- burgh, NY 12901 ([email protected]), 2Southwest Research Institute, 1050 Walnut St., Suite 300, Boul- der, CO, 80302. 3Department of Chemistry, Alma College, Alma, MI 48801 Introduction: In our Solar System the asteroid Measurements: We have performed disruption ex- belt is compositionally zoned, with the asteroids simi- periments on four hydrous meteorite targets, Murchi- lar in reflection spectrum to the carbonaceopus meteor- son and three CM2 meteorites recovered from the Ant- ites dominating the outer-half of the main belt. In the arctic. The projectiles in these experiments were 1/8 th outer-half of the main belt about one-half of the carbo- inch diameter aluminum spheres fired at the meteorite naceous asteroids are hydrous, based on their infrared targets at speeds comparable to the collision velocities spectra [1]. The asteroids in the inner-half of the main in the main-belt. belt are predominantly anhydrous. Thus, about one- Each meteorite target was surrounded by “passive quarter of the main belt asteroids are hydrous. detectors” that included three thicknesses of aluminum Because dust particles from the main-belt asteroids foil to monitor the size of the small debris from the generally encounter the Earth with lower relative ve- distrption. The foil hole diameters were measured, and locities than dust from comets [2], asteroidal dust ex- converted to impacting particle diameters using the periences much less severe atmospheric entry heating calibration data of Hörz et al. -
ASTRONAUTICS and AERONAUTICS, 1977 a Chronology
NASA SP--4022 ASTRONAUTICS AND AERONAUTICS, 1977 A Chronology Eleanor H. Ritchie ' The NASA History Series Scientific and Technical Information Branch 1986 National Aeronautics and Space Administration Washington, DC Four spacecraft launched by NASA in 1977: left to right, top, ESA’s Geos 1 and NASA’s Heao 1; bottom, ESA’s Isee 2 on NASA’s Isee 1, and Italy’s Wo. (NASA 77-H-157,77-H-56, 77-H-642, 77-H-484) Contents Preface ...................................................... v January ..................................................... 1 February .................................................... 21 March ...................................................... 47 April ....................................................... 61 May ........................................................ 77 June ...................................................... 101 July ....................................................... 127 August .................................................... 143 September ................................................. 165 October ................................................... 185 November ................................................. 201 December .................................................. 217 Appendixes A . Satellites, Space Probes, and Manned Space Flights, 1977 .......237 B .Major NASA Launches, 1977 ............................... 261 C. Manned Space Flights, 1977 ................................ 265 D . NASA Sounding Rocket Launches, 1977 ..................... 267 E . Abbreviations of References -
NSS North Houston Space Society
NSS North Houston Space Society Space News December 12, 2020 Greg Stanley Lunar news from China “Chang’e flies to the Moon” • Lunar news Credit: Nguyen Manh, via Pinterest Chang’e (“Chang the beautiful”) Chinese Moon goddess, namesake of Chinese Lunar Exploration Program Ming Dynasty, circa 1500 Chinese lunar sample return Credit: NAOC (Chang’e 5) Overview • Return 2 kg (4.4 lbs) of lunar rock & dirt to Earth Orbiter and return capsule • First return of lunar materials since 1976 (Russia’s Luna 24) • Structured like an Apollo mission, except completely robotic • Target area: “Ocean of Storms” • Volcanic mound 1.21 billion years old, vs. Apollo samples 3.1 – 4.4 billion years old • China’s 3rd soft landing on the Moon • First takeoff of a spacecraft from large planetary body since 1976 (Russia’s Luna 24) • First robotic docking between 2 craft orbiting the moon • Launch mass: about 18,100 lbs Ascender Lander Orbiter with all components enroute Credit: Junior Miranda Credit: NAOC Chinese lunar sample return mission (Chang’e 5) Milestones • Launched Nov 23 • Entered Moon orbit Nov. 28 • Lander/ascender detached to begin descent to Moon’s surface Nov 30 • Landed on Moon Dec 1 • Samples taken, sealed in a storage device in ascender • Drilled samples up to 2 meters (6.6 feet); also scooped samples from surface • Solar powered only – had to complete mission in 2 days before lunar night • Ascender launched from Moon Dec 3; 6 minutes to orbit • Ascender docked with Earth return craft Dec 5 • Samples transferred from ascender to orbiter • Orbiter -
Espinsights the Global Space Activity Monitor
ESPInsights The Global Space Activity Monitor Issue 6 April-June 2020 CONTENTS FOCUS ..................................................................................................................... 6 The Crew Dragon mission to the ISS and the Commercial Crew Program ..................................... 6 SPACE POLICY AND PROGRAMMES .................................................................................... 7 EUROPE ................................................................................................................. 7 COVID-19 and the European space sector ....................................................................... 7 Space technologies for European defence ...................................................................... 7 ESA Earth Observation Missions ................................................................................... 8 Thales Alenia Space among HLS competitors ................................................................... 8 Advancements for the European Service Module ............................................................... 9 Airbus for the Martian Sample Fetch Rover ..................................................................... 9 New appointments in ESA, GSA and Eurospace ................................................................ 10 Italy introduces Platino, regions launch Mirror Copernicus .................................................. 10 DLR new research observatory .................................................................................. -
Liquid Water on Mars
Report, Planetary Sciences Unit (AST80015), Swinburne Astronomy Online Preprint typeset using LATEX style emulateapj v. 12/16/11 LIQUID WATER ON MARS M. Usatov1 Report, Planetary Sciences Unit (AST80015), Swinburne Astronomy Online ABSTRACT Geomorphological, mineralogical and other evidence of the conditions favoring the existence of water on Mars in liquid phase is reviewed. This includes signatures of past and, possibly, present aqueous environments, such as the northern ocean, lacustrine environments, sedimentary and thermokarst landforms, glacial activity and water erosion features. Reviewed also are hydrous weathering processes, observed on surface remotely and also via analysis of Martian meteorites. Chemistry of Martian water is discussed: the triple point, salts and brines, as well as undercooled liquid interfacial and solid-state greenhouse effect melted waters that may still be present on Mars. Current understanding of the evolution of Martian hydrosphere over geological timescales is presented from early period to the present time, along with the discussion of alternative interpretations and possibilities of dry and wet Mars extremes. 1. INTRODUCTION morphological and mineralogical evidence of aqueous en- The presence of water on Earth, as seen from space, vironments available in the past and, possibly, present can be implied from the observations of low-albedo fea- time is presented in x3 which will be correlated with the tures, like seas and oceans, fluvial features on its sur- current understanding of the evolution of Martian hy- face, atmospheric phenomena, polar ice caps, and the drosphere at x4. Alternative (dry) interpretations of the snow cover exhibiting seasonal variations, not to mention evidence are discussed in x5. spectroscopy. -
The Planet Earth-I)
Geology (The Planet Earth-I) UNIT-1 The Planet Earth-I 1. ORIGIN OF THE SOLAR SYSTEM AND EARTH The Solar System The Solar System is made up of all the planets that orbit our Sun. In addition to planets, the Solar System also consists of moons, comets, asteroids, minor planets, and dust and gas. Everything in the Solar System orbits or revolves around the Sun. The Sun contains around 98% of all the material in the Solar System. The larger an object is, the more gravity it has. Because the Sun is so large, its powerful gravity attracts all the other objects in the Solar System towards it. At the same time, these objects, which are moving very rapidly, try to fly away from the Sun, outward into the emptiness of outer space. The result of the planets trying to fly away, at the same time that the Sun is trying to pull them inward is that they become trapped half-way in between. Balanced between flying towards the Sun, and escaping into space, they spend eternity orbiting around their parent star. Our solar system consists of an average star we call the Sun, the planets Mercury, Venus, Earth, Mars, Jupiter, Saturn, Uranus, Neptune, and Pluto. It includes: the satellites of the planets; numerous comets, asteroids, and meteoroids; and the interplanetary medium. The Sun is the richest source of electromagnetic energy (mostly in the form of heat and light) in the solar system. The Sun's nearest known stellar neighbor is a red dwarf star called Proxima Centaury, at a distance of 4.3 light years away.