Meteoroid Stream Formation Due to the Extraction of Space Resources from Asteroids
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Mining Outer Space: Who Owns the Asteroids?
G THE B IN EN V C R H E S A N 8 8 D 8 B 1 AR SINCE WWW. NYLJ.COM VOLUME 254—NO. 19 WEDNESDAY, JULY 29, 2015 Outside Counsel Expert Analysis Mining Outer Space: Who Owns the Asteroids? ver the last two years, U.S. outer space. Most relate to navigation and business and policy makers By space flight—reflecting the aspirations have focused afresh on the Timothy G. (and limits) of the era. Two, however, commercial possibilities of the Nelson are potentially relevant: Article I of the asteroids—the solar system’s OST states that “[t]he exploration and use Ominor planetary objects. Most of these of outer space, including the moon and are located between Mars and Jupiter, other celestial bodies, shall be carried out while some are closer to Earth. Some The ‘Law’ of Space for the benefit and in the interests of all have large deposits of precious metals countries, irrespective of their degree of and other potentially valuable substanc- Until the Sputnik launch in the 1950s, economic or scientific development, and es.1 In the last few years, some private few steps had been taken in defining the shall be the province of all mankind.”8 operators have announced plans to mine legal rules relating to outer space. Indeed, Article II states that “[o]uter space, includ- them commercially, a concept that, until the only circumstance in which “owner- ing the moon and other celestial bodies, now, has been exclusively the realm of ship of space minerals” was relevant was is not subject to national appropriation science fiction.2 if someone was fortunate (or unfortunate) by claim of sovereignty, by means of use In apparent response to these initiatives, or occupation, or by any other means.”9 the House of Representatives recently The legal status of mining in Together, these articles mean that passed the “Space Resource Exploration space cannot be subdivided into national and Utilization Act of 2015,” H.R. -
Meteors, Meteoroids, and Meteorites by Cindy Grigg
Meteors, Meteoroids, and Meteorites By Cindy Grigg 1 Have you ever seen a falling star? You really saw a meteor. A meteor is a bright streak of light we see in the sky. It only lasts for a few seconds. People often call meteors shooting stars or falling stars because they look like stars falling from the sky. People sometimes call the brightest meteors fireballs. While it is in space, it is called a meteoroid. Meteoroids that reach the Earth are called meteorites. 2 A meteor appears when a chunk of metallic or stony matter called a meteoroid enters the Earth's atmosphere from outer space. Air friction heats the meteoroid so that it glows. It creates a shining trail of gases and melted meteoroid particles. Most meteoroids burn up before reaching the Earth. Some leave a trail that lasts several seconds. Millions of meteors occur in the Earth's atmosphere every day. Most meteoroids that cause meteors are about the size of a pebble. 3 Meteoroids travel around the sun in different orbits and at different speeds. The fastest ones move at about 26 miles per second. The Earth travels at about 18 miles per second. So when meteoroids meet the Earth's atmosphere head-on, the combined speed may reach about 44 miles per second, or 264 miles per hour! 4 The Earth meets a number of clusters of tiny meteoroids at certain times every year. At these times, the sky seems filled with a shower of sparks. These clusters have orbits like comets and are believed to be pieces of comets. -
The Solar System
5 The Solar System R. Lynne Jones, Steven R. Chesley, Paul A. Abell, Michael E. Brown, Josef Durech,ˇ Yanga R. Fern´andez,Alan W. Harris, Matt J. Holman, Zeljkoˇ Ivezi´c,R. Jedicke, Mikko Kaasalainen, Nathan A. Kaib, Zoran Kneˇzevi´c,Andrea Milani, Alex Parker, Stephen T. Ridgway, David E. Trilling, Bojan Vrˇsnak LSST will provide huge advances in our knowledge of millions of astronomical objects “close to home’”– the small bodies in our Solar System. Previous studies of these small bodies have led to dramatic changes in our understanding of the process of planet formation and evolution, and the relationship between our Solar System and other systems. Beyond providing asteroid targets for space missions or igniting popular interest in observing a new comet or learning about a new distant icy dwarf planet, these small bodies also serve as large populations of “test particles,” recording the dynamical history of the giant planets, revealing the nature of the Solar System impactor population over time, and illustrating the size distributions of planetesimals, which were the building blocks of planets. In this chapter, a brief introduction to the different populations of small bodies in the Solar System (§ 5.1) is followed by a summary of the number of objects of each population that LSST is expected to find (§ 5.2). Some of the Solar System science that LSST will address is presented through the rest of the chapter, starting with the insights into planetary formation and evolution gained through the small body population orbital distributions (§ 5.3). The effects of collisional evolution in the Main Belt and Kuiper Belt are discussed in the next two sections, along with the implications for the determination of the size distribution in the Main Belt (§ 5.4) and possibilities for identifying wide binaries and understanding the environment in the early outer Solar System in § 5.5. -
Meteor Showers' Activity and Forecasting
Meteoroids 2007 – Barcelona, June 11-15 About the cover: The recent fall of the Villalbeto de la Peña meteorite on January 4, 2004 (Spain) is one of the best documented in history for which atmospheric and orbital trajectory, strewn field area, and recovery circumstances have been described in detail. Photometric and seismic measurements together with radioisotopic analysis of several recovered specimens suggest an original mass of about 760 kg. About fifty specimens were recovered from a strewn field of nearly 100 km2. Villalbeto de la Peña is a moderately shocked (S4) equilibrated ordinary chondrite (L6) with a cosmic-ray-exposure age of 48±5 Ma. The chemistry and mineralogy of this genuine meteorite has been characterized in detail by bulk chemical analysis, electron microprobe, electron microscopy, magnetism, porosimetry, X-ray diffraction, infrared, Raman, and 57Mössbauer spectroscopies. The picture of the fireball was taken by M.M. Ruiz and was awarded by the contest organized by the Spanish Fireball Network (SPMN) for the best photograph of the event. The Moon is also visible for comparison. The picture of the meteorite was taken as it was found by the SPMN recovery team few days after the fall. 2 Meteoroids 2007 – Barcelona, June 11-15 FINAL PROGRAM Monday, June 11 Auditorium conference room 9h00-9h50 Reception 9h50-10h00 Opening event Session 1: Observational Techniques and Meteor Detection Programs Morning session Session chairs: J. Borovicka and W. Edwards 10h00-10h30 Pavel Spurny (Ondrejov Observatory, Czech Republic) et al. “Fireball observations in Central Europe and Western Australia – instruments, methods and results” (invited) 10h30-10h45 Josep M. -
19. Near-Earth Objects Chelyabinsk Meteor: 2013 ~0.5 Megaton Airburst ~1500 People Injured
Astronomy 241: Foundations of Astrophysics I 19. Near-Earth Objects Chelyabinsk Meteor: 2013 ~0.5 megaton airburst ~1500 people injured (C) Don Davis Asteroids 101 — B612 Foundation Great Daylight Fireball: 1972 Earthgrazer: The Great Daylight Fireball of 1972 Tunguska Meteor: 1908 Asteroid or comet: D ~ 40 m ~10 megaton airburst ~40 km destruction radius The Tunguska Impact Tunguska: The Largest Recent Impact Event Barringer Crater: ~50 ky BP M-type asteroid: D ~ 50 m ~10 megaton impact 1.2 km crater diameter Meteor Crater — Wikipedia Chicxulub Crater: ~65 My BP Asteroid: D ~ 10 km 180 km crater diameter Chicxulub Crater— Wikipedia Comets and Meteor Showers Comets shed dust and debris which slowly spread out as they move along the comet’s orbit. If the Earth encounters one of these trails, we get a Breakup of a Comet meteor shower. Meteor Stream Perseid Meteor Shower Raining Perseids Major Meteor Showers Forty Thousand Meteor Origins Across the Sky Known Potentially-Hazardous Objects Near-Earth object — Wikipedia Near-Earth object — Wikipedia Origin of Near-Earth Objects (NEOs) ! WHAM Mars Some fragments wind up on orbits which are resonant with Jupiter. Their orbits grow more elliptical, finally entering the inner solar system. Wikipedia: Asteroid belt Asteroid Families Many asteroids are members of families; they have similar orbits and compositions (indicated by colors). Asteroid Belt Populations Inner belt asteroids (left) and families (right). Origin of Key Stages in the Evolution of the Asteroid Vesta Processed Family Members Crust Surface Magnesium-Sliicate Lavas Meteorites Mantle (Olivine) Iron-Nickle Core Stony Irons? As smaller bodies in the early Solar System Heavier elements sink to the Occasional impacts with other bodies fall together, the asteroid agglomerates. -
Sun Passes by Zubenelgenubi
The Wilderness Above Aileen O’Donoghue St. Lawrence University & Adirondack Public Observatory FOR 3/5/13 Comet Pan-STARRS The closing of the Isthmus of Panama, cutting off the equatorial flow between the Atlantic and Pacific oceans, was just about complete five million years ago when, in the far reaches of the solar system, 50,000 times farther from the sun than Earth, two hill-sized hulks of rock, dust and volatile ices had a close encounter. The gravitational tug sent one of them plunging toward the distant sun appearing slightly dimmer than Venus does to us. It has taken all these years for that hulk, now Comet Pan-STARRS, to plunge to the inner solar system. It was just inside the orbit of Saturn and very faint on June 6, 2011 when it was discovered by the Panoramic Survey Telescope and Rapid Response (Pan-STARRS) facility in Hawaii. In March of 2012, J.J. Gonzalez of Leon, Spain was the first amateur astronomer to spot it. It became visible with binoculars in January of this year and had formed a tail by February that southern hemisphere observers have imaged. Today, Comet Pan-STARRS will pass closest to the Earth at a distance a little greater than that to the sun. However, it is not yet visible from our latitude. On Thursday we may be able to spot it very low on the western horizon about ½ an hour after sunset. As the diagram shows, it will rise away from the horizon through the next couple weeks and gradually fade. On Sunday, the first day of Daylight Saving Time, it will make its closest approach to the sun at about 28 million miles. -
8 Asteroid–Meteoroid Complexes
“9781108426718c08” — 2019/5/13 — 16:33 — page 187 — #1 8 Asteroid–Meteoroid Complexes Toshihiro Kasuga and David Jewitt 8.1 Introduction Jenniskens, 2011)1 and asteroid 3200 Phaethon are probably the best-known examples (Whipple, 1983). In such cases, it Physical disintegration of asteroids and comets leads to the appears unlikely that ice sublimation drives the expulsion of production of orbit-hugging debris streams. In many cases, the solid matter, raising following general question: what produces mechanisms underlying disintegration are uncharacterized, or the meteoroid streams? Suggested alternative triggers include even unknown. Therefore, considerable scientific interest lies in thermal stress, rotational instability and collisions (impacts) tracing the physical and dynamical properties of the asteroid- by secondary bodies (Jewitt, 2012; Jewitt et al., 2015). Any meteoroid complexes backwards in time, in order to learn how of these, if sufficiently violent or prolonged, could lead to the they form. production of a debris trail that would, if it crossed Earth’s orbit, Small solar system bodies offer the opportunity to understand be classified as a meteoroid stream or an “Asteroid-Meteoroid the origin and evolution of the planetary system. They include Complex”, comprising streams and several macroscopic, split the comets and asteroids, as well as the mostly unseen objects fragments (Jones, 1986; Voloshchuk and Kashcheev, 1986; in the much more distant Kuiper belt and Oort cloud reservoirs. Ceplecha et al., 1998). Observationally, asteroids and comets are distinguished princi- The dynamics of stream members and their parent objects pally by their optical morphologies, with asteroids appearing may differ, and dynamical associations are not always obvious. -
Planetary Defense Final Report I
Team Project - Planetary Defense Final Report i Team Project - Planetary Defense Final Report ii Team Project - Planetary Defense Cover designed by: Tihomir Dimitrov Images courtesy of: Earth Image - NASA US Geological Survey Detection Image - ESA's Optical Ground Station Laser Tags ISS Deflection Image - IEEE Space Based Lasers Collaboration Image - United Nations General Assembly Building Outreach Image - Dreamstime teacher with students in classroom Evacuation Image - Libyan City of Syrte destroyed in 2011 Shield Image - Silver metal shield PNG image The cover page was designed to include a visual representation of the roadmap for a robust Planetary Defense Program that includes five elements: detection, deflection, global collaboration, outreach, and evacuation. The shield represents the idea of defending our planet, giving confidence to the general public that the Planetary Defense elements are reliable. The orbit represents the comet threat and how it is handled by the shield, which represents the READI Project. The curved lines used in the background give a sense of flow representing the continuation and further development for Planetary Defense programs after this team project, as we would like for everyone to be involved and take action in this noble task of protecting Earth. The 2015 Space Studies Program of the International Space University was hosted by the Ohio University, Athens, Ohio, USA. While all care has been taken in the preparation of this report, ISU does not take any responsibility for the accuracy of its content. -
Meteors Ebook, Epub
METEORS PDF, EPUB, EBOOK Melissa Stewart | 32 pages | 01 Jun 2015 | National Geographic Kids | 9781426319433 | English | London, United Kingdom Meteors PDF Book These particles might affect climate, both by scattering electromagnetic radiation and by catalyzing chemical reactions in the upper atmosphere. This year, with a 60 percent illuminated moon rising near pm local summer time, one could easily dismiss the probably of seeing anything extraordinary from this source. Oxford Dictionary of Astronomy. Early Earth experienced many large meteor impacts that caused extensive destruction. At this time, the moon is located near the sun and is invisible at night. Stony meteoroids without these features are called " achondrites ", which are typically formed from extraterrestrial igneous activity; they contain little or no extraterrestrial iron. Meteorites are bits of the solar system that have fallen to the Earth. What's Up - January More than 1, people were injured in the blast, mostly due to broken glass. They have three main classifications: iron, stone, and stony-iron. If a meteor survives its transit of the atmosphere to come to rest on the Earth's surface, the resulting object is called a meteorite. Photographing a meteor shower can be an exercise in patience, but with these tips — and some good fortune — you might be rewarded with a great photo. Meteor radars can measure atmospheric density and winds by measuring the decay rate and Doppler shift of a meteor trail. When a meteor comes hurtling toward Earth, the high-pressure air in front of it seeps into its pores Meteorite Impacts in History. Another rare phenomenon is a meteor procession , where the meteor breaks up into several fireballs traveling nearly parallel to the surface of Earth. -
The Chant Meteor Procession of 1913 – Towards a Descriptive Model
American Journal of Astronomy and Astrophysics 2018; 6(2): 31-38 http://www.sciencepublishinggroup.com/j/ajaa doi: 10.11648/j.ajaa.20180602.11 ISSN: 2376-4678 (Print); ISSN: 2376-4686 (Online) The Chant Meteor Procession of 1913 – Towards a Descriptive Model Martin Beech 1, 2, Mark Comte 2 1Campion College at the University of Regina, Saskatchewan, Canada 2Department of Physics, The University of Regina, Saskatchewan, Canada Email address: To cite this article: Martin Beech, Mark Comte. The Chant Meteor Procession of 1913 – Towards a Descriptive Model . American Journal of Astronomy and Astrophysics . Vol. 6, No. 2, 2018, pp. 31-38. doi: 10.11648/j.ajaa.20180602.11 Received : April 5, 2018; Accepted : April 19, 2018; Published : June 28, 2018 Abstract: From an observational standpoint the Chant Meteor Procession of 9 February, 1913 is particularly remarkable, being especially noted for its long ground track of at least 15,000 km, and for the slow motion and near parallel to the horizon paths adopted by the meteors. The circumstances surrounding the Procession are re-considered here in terms of the successive entry of multiple meteoroid clusters. These clusters are in turn considered to be derived from a temporarily captured Earth orbiting object that has undergone disaggregation. It is suggested that the general observational accounts of the Procession can be explained through the sequential entry of multiple meteoroid clusters that moved through the Earth’s atmosphere on grazing-incident trajectories. It is further suggested that the parent object to the Procession, prior to its breakup, may have been no more than 3 to 4-m across. -
China Lake Astronomical Society Members and Friends of CLAS
Volume 57 No. 08 July 31, 2020 NEXT MEETING 7:30 p.m., Monday, Aug 03, 2020 Maturango Museum, 100 East Las Flores Avenue, Ridgecrest, California. PROGRAM FOR THE Aug 03, 2020 7:30 PM MEETING For our first meeting since March Keith Weisz (Vice President) will have a program on work he has been doing regarding “The Earthquake”. Because of family events he may not be able to do it and that is where our membership comes in. Most of you have been watching or photographing Comet Neowise and if possible could you please send in images you may have acquired and talk about your experiences. In addition we would like to have some input on what we might want to do for club activities in the future. Please send your images to [email protected] George Hodgkinson is inviting you to a scheduled Zoom meeting. Topic: China Lake Astronomical Society Time: Aug 3, 2020 7:30 PM Pacific Time (US and Canada) Join Zoom Meeting https://us02web.zoom.us/j/86928105798?pwd=RlVSNVhTd1dTeVhEQlpEeWxJSVhlUT09 Meeting ID: 869 2810 5798 Passcode: 852674 One tap mobile +14086380968,,86928105798#,,,,,,0#,,852674# US (San Jose) +16699006833,,86928105798#,,,,,,0#,,852674# US (San Jose) Dial by your location +1 408 638 0968 US (San Jose) +1 669 900 6833 US (San Jose) +1 253 215 8782 US (Tacoma) +1 346 248 7799 US (Houston) +1 301 715 8592 US (Germantown) +1 312 626 6799 US (Chicago) +1 646 876 9923 US (New York) Meeting ID: 869 2810 5798 Passcode: 852674 Find your local number: https://us02web.zoom.us/u/kLkhsd2Pj This picture was taken by our past CLAS President David Gregg. -
Rising from Ashes Or Dying Flash? Mega Outburst of Small Comet 289P/Blanpain in 2013∗
Draft version June 18, 2019 Typeset using LATEX default style in AASTeX62 Rising from Ashes or Dying Flash? Mega Outburst of Small Comet 289P/Blanpain in 2013∗ Quanzhi Ye (叶泉志)1, 2 and David L. Clark3, 4, 5 1Division of Physics, Mathematics and Astronomy, California Institute of Technology, Pasadena, CA 91125, U.S.A. 2Infrared Processing and Analysis Center, California Institute of Technology, Pasadena, CA 91125, U.S.A. 3Department of Earth Sciences, University of Western Ontario, London, Ontario, N6A 5B7, Canada 4Department of Physics and Astronomy, University of Western Ontario, London, Ontario, N6A 3K7, Canada 5Centre for Planetary Science and Exploration, University of Western Ontario, London, Ontario, N6A 5B7, Canada (Received {; Revised {; Accepted {) Submitted to ApJL ABSTRACT Jupiter-family comet 289P/Blanpain was first discovered in 1819 and was then lost for 200 years, only to be rediscovered in 2003 as a small, weakly active comet. The comet is associated∼ with the Phoenicids, an otherwise minor meteor shower that produced significant outbursts in 1956 and 2014. The shower points to the existence of significant mass-loss events of P/Blanpain in recent history. P/Blanpain was recovered during an apparent large outburst in 2013 July at an appreciable heliocentric distance of 3.9 au, with brightness increase of 9 mag, making it one of the largest comet outbursts ever observed. Here we present an analysis of archival data taken by several telescopes. We find that the 2013 outburst has produced 108 kg of dust, which accounts for a modest fraction ( 1%) of the mass of P/Blanpain's nucleus as measured∼ in 2004.