Van Flandern's Fission-Explosion Model
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Lurking in the Shadows: Wide-Separation Gas Giants As Tracers of Planet Formation
Lurking in the Shadows: Wide-Separation Gas Giants as Tracers of Planet Formation Thesis by Marta Levesque Bryan In Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy CALIFORNIA INSTITUTE OF TECHNOLOGY Pasadena, California 2018 Defended May 1, 2018 ii © 2018 Marta Levesque Bryan ORCID: [0000-0002-6076-5967] All rights reserved iii ACKNOWLEDGEMENTS First and foremost I would like to thank Heather Knutson, who I had the great privilege of working with as my thesis advisor. Her encouragement, guidance, and perspective helped me navigate many a challenging problem, and my conversations with her were a consistent source of positivity and learning throughout my time at Caltech. I leave graduate school a better scientist and person for having her as a role model. Heather fostered a wonderfully positive and supportive environment for her students, giving us the space to explore and grow - I could not have asked for a better advisor or research experience. I would also like to thank Konstantin Batygin for enthusiastic and illuminating discussions that always left me more excited to explore the result at hand. Thank you as well to Dimitri Mawet for providing both expertise and contagious optimism for some of my latest direct imaging endeavors. Thank you to the rest of my thesis committee, namely Geoff Blake, Evan Kirby, and Chuck Steidel for their support, helpful conversations, and insightful questions. I am grateful to have had the opportunity to collaborate with Brendan Bowler. His talk at Caltech my second year of graduate school introduced me to an unexpected population of massive wide-separation planetary-mass companions, and lead to a long-running collaboration from which several of my thesis projects were born. -
Planet Formation
3. Planet form ation Frontiers of A stronom y W orkshop/S chool Bibliotheca A lexandrina M arch-A pril 2006 Properties of planetary system s • all giant planets in the solar system have a > 5 A U w hile extrasolar giant planets have semi-major axes as small as a = 0.02 A U • planetary orbital angular momentum is close to direction of S un’s spin angular momentum (w ithin 7o) • 3 of 4 terrestrial planets and 3 of 4 giant planets have obliquities (angle betw een spin and orbital angular momentum) < 30o • interplanetary space is virtually empty, except for the asteroid belt and the Kuiper belt • planets account for < 0.2% of mass of solar system but > 98% of angular momentum Properties of planetary system s • orbits of major planets in solar system are nearly circular (eMercury=0.206, ePluto=0.250); orbits of extrasolar planets are not (emedian=0.28) • probability of finding a planet is proportional to mass of metals in the star Properties of planetary system s • planets suffer no close encounters and are spaced fairly n regularly (Bode’s law : an=0.4 + 0.3×2 ) planet semimajor axis (A U ) n an (A U ) Mercury 0.39 −∞ 0.4 V enus 0.72 0 0.7 Earth 1.00 1 1.0 Mars 1.52 2 1.6 asteroids 2.77 (Ceres) 3 2.8 Jupiter 5.20 4 5.2 S aturn 9.56 5 10.0 U ranus 19.29 6 19.6 N eptune 30.27 7 38.8 Pluto 39.68 8 77.2 Properties of planetary system s • planets suffer no close encounters and are spaced fairly n regularly (Bode’s law : an=0.4 + 0.3×2 ) planet semimajor axis (A U ) n an (A U ) Mercury+ 0.39 −∞ 0.4 V enus 0.72 0 0.7 Earth 1.00 1 1.0 *predicted -
Planets of the Solar System
Chapter Planets of the 27 Solar System Chapter OutlineOutline 1 ● Formation of the Solar System The Nebular Hypothesis Formation of the Planets Formation of Solid Earth Formation of Earth’s Atmosphere Formation of Earth’s Oceans 2 ● Models of the Solar System Early Models Kepler’s Laws Newton’s Explanation of Kepler’s Laws 3 ● The Inner Planets Mercury Venus Earth Mars 4 ● The Outer Planets Gas Giants Jupiter Saturn Uranus Neptune Objects Beyond Neptune Why It Matters Exoplanets UnderstandingU d t di theth formationf ti and the characteristics of our solar system and its planets can help scientists plan missions to study planets and solar systems around other stars in the universe. 746 Chapter 27 hhq10sena_psscho.inddq10sena_psscho.indd 774646 PDF 88/15/08/15/08 88:43:46:43:46 AAMM Inquiry Lab Planetary Distances 20 min Turn to Appendix E and find the table entitled Question to Get You Started “Solar System Data.” Use the data from the How would the distance of a planet from the sun “semimajor axis” row of planetary distances to affect the time it takes for the planet to complete devise an appropriate scale to model the distances one orbit? between planets. Then find an indoor or outdoor space that will accommodate the farthest distance. Mark some index cards with the name of each planet, use a measuring tape to measure the distances according to your scale, and place each index card at its correct location. 747 hhq10sena_psscho.inddq10sena_psscho.indd 774747 22/26/09/26/09 111:42:301:42:30 AAMM These reading tools will help you learn the material in this chapter. -
Outer Planets: the Ice Giants
Outer Planets: The Ice Giants A. P. Ingersoll, H. B. Hammel, T. R. Spilker, R. E. Young Exploring Uranus and Neptune satisfies NASA’s objectives, “investigation of the Earth, Moon, Mars and beyond with emphasis on understanding the history of the solar system” and “conduct robotic exploration across the solar system for scientific purposes.” The giant planet story is the story of the solar system (*). Earth and the other small objects are leftovers from the feast of giant planet formation. As they formed, the giant planets may have migrated inward or outward, ejecting some objects from the solar system and swallowing others. The giant planets most likely delivered water and other volatiles, in the form of icy planetesimals, to the inner solar system from the region around Neptune. The “gas giants” Jupiter and Saturn are mostly hydrogen and helium. These planets must have swallowed a portion of the solar nebula intact. The “ice giants” Uranus and Neptune are made primarily of heavier stuff, probably the next most abundant elements in the Sun – oxygen, carbon, nitrogen, and sulfur. For each giant planet the core is the “seed” around which it accreted nebular gas. The ice giants may be more seed than gas. Giant planets are laboratories in which to test our theories about geophysics, plasma physics, meteorology, and even oceanography in a larger context. Their bottomless atmospheres, with 1000 mph winds and 100 year-old storms, teach us about weather on Earth. The giant planets’ enormous magnetic fields and intense radiation belts test our theories of terrestrial and solar electromagnetic phenomena. -
Meteorites and the Origin of the Solar System
Meteorites and the origin of the solar system STEPHEN G. BRUSH University of Maryland, College Park, MD 20742, USA (e-mail: [email protected]) Abstract: During the past two centuries, theories of the origin of the solar system have been strongly influenced by observations and theories about meteorites. I review this history up to about 1985. During the 19th century the hypothesis that planets formed by accretion of small solid particles ('the meteoritic hypothesis') competed with the alternative 'nebular hypothesis' of Laplace, based on condensation from a hot gas. At the beginning of the 20th century Chamberlin and Moulton revived the meteoritic hypothesis as the 'planetesimal hypothesis' and joined it to the assumption that the solar system evolved from the encounter of the Sun with a passing star. Later, the encounter hypothesis was rejected and the planetesimal hypothesis was incorporated into new versions of the nebular hypothesis. In the 1950s, meteorites provided essential data for the establishment by Patterson and others of the pre- sently accepted 4500 Ma age of the Earth and the solar system. Analysis of the Allende meteorite, which fell in 1969, inspired the 'supernova trigger' theory of the origin of the solar system, and furnished useful constraints on theories of planetary formation developed by Urey, Ringwood, Anders and others. Many of these theories assumed condensation from a homogeneous hot gas, an assumption that was challenged by astrophysical calculations. The meteoritic-planetesimal theory of planet formation was developed in Russia by Schmidt and later by Safronov. Wetherill, in the United States, established it as the preferred theory for formation of terrestrial planets. -
Alien Moons Could Bake Dry from Young Gas Giants' Hot Glow 10 March 2014, by Adam Hadhazy
Alien moons could bake dry from young gas giants' hot glow 10 March 2014, by Adam Hadhazy scenarios because they orbit another body besides their star. A new paper by Heller and his colleague Rory Barnes of the University of Washington and the NASA Virtual Planetary Laboratory examines how heat emanating from a freshly formed exoplanet, coupled with irradiation from the solar system's star, can roast the planet's moons. Before the planet cools off sufficiently, its close-orbiting moons could lose all their water, leaving them bone-dry and barren. "An exomoon's habitability is of course constrained by its location in the stellar habitable zone, but it also has a second heat source—its host planet—that has to be accounted for," said Heller, whose paper An Earthlike moon orbiting a gas giant host planet. has been accepted for publication in The Credit: NASA International Journal of Astrobiology. "With regard to this second source, our study shows that at close range, the illumination from young and hot giant planets can render their moons uninhabitable." When we think of where else life might exist in the universe, we tend to focus on planets. But on a Researchers believe moons could serve as suitable grander cosmic scale, moons could prove the more abodes for life just as well as planets. Even moons common life-friendly abode. far beyond the habitable zone, such as Jupiter's Europa and Saturn's Titan, offer tantalizing hints of A single gas giant planet in the not-too-warm, not- potential habitability thanks to the subsurface too-cold habitable zone around its star—where ocean in the former and the intriguing organic Earth and Mars correspondingly reside—could host chemistry of the latter. -
Constructing the Solar System: a Smashing Success
Constructing the Solar System: A Smashing Success A Star is Born Thomas M. Davison Department of the Geophysical Sciences Compton Lecture Series October 6, 2012 T. M. Davison Constructing the Solar System Compton Lectures { Autumn 2012 1 Today's lecture 1 An overview of the Compton Lecture Series 2 A tour of the Solar System 3 Physical properties of the Solar System What can they tell us about the Solar System's formation? 4 How was our star born? The nebula hypothesis of star formation Images courtesy of NASA T. M. Davison Constructing the Solar System Compton Lectures { Autumn 2012 2 Part 1: Introduction to the lecture series Image courtesy of NASA T. M. Davison Constructing the Solar System Compton Lectures { Autumn 2012 3 Constructing the Solar System ... How did the Sun, the planets and the asteroids form? What were their histories like? One process dominates throughout Solar System history: Collisions Growth of asteroids and planets Formation of the Moon Extinction of the dinosaurs After such a violent history, we now have a habitable planet Which you could call: ... A Smashing Success! Images Courtesy of NASA T. M. Davison Constructing the Solar System Compton Lectures { Autumn 2012 4 My day job: Making an impact Computer simulations of collisions between planetesimals Simulations by T. Davison T. M. Davison Constructing the Solar System Compton Lectures { Autumn 2012 5 Compton Lecture Series Schedule 1 10/06/12 A Star is Born 2 10/13/12* Making Planetesimals: the building blocks of planets 3 10/20/12* Guest Lecturer: Mac Cathles 4 10/27/12 Asteroids, Comets and Meteorites: 10/27/12 our eyes in the early Solar System 5 11/03/12 Building the Planets 6 11/10/12 When Asteroids Collide 7 11/17/12 Making Things Hot: The thermal effects of collisions 11/24/12 No lecture: Thanksgiving weekend 8 12/01/12 Constructing the Moon 12/08/12 No lecture: Physics with a Bang! 9 12/15/12 Impact Earth: Chicxulub and other terrestrial impacts T. -
Mixing of the Asteroid Belt Due to the Formation of the Giant Planets
Accretion: Building New Worlds (2017) 2027.pdf MIXING OF THE ASTEROID BELT DUE TO THE FORMATION OF THE GIANT PLANETS. K. A. Kretke1, W. F. Bottke2,3, H. F. Levison2,3, and D. A. Kring4,5, 1SSERVI NPP Fellow ([email protected]), 2Southwest Research Institute, 1050 Walnut St, Suite 300, Boulder, CO 80302, USA, 3ISET, NASA-SSERVI, 4LPI, 3600 Bay Area Blvd, Houston, TX 77058, USA 5CLSE, NASA-SSERVI. Introduction: The asteroid belt is observed to be a evolution of a solar system forming under these condi- mixture of objects with different compositions, with tions. LIPAD is based upon the N-Body integrator volatile-poor asteroids (mostly S-complex) dominant in SWIFT [10] but uses novel algorithms to statistically the inner asteroid belt while volatile-rich (mostly C- follow bodies that are too small and numerous to be han- complex) asteroids dominate the outer asteroid belt. dled in a traditional N-body integrator. This allows us to While this general compositional stratification was orig- model how our system may have evolved starting from inally thought to be an indicator of the primordial tem- pebbles and planetesimals all the way to a mature plan- perature gradient in the protoplanetary disk, there is etary system. growing evidence that that meteorites believed to origi- To test the effect of giant planet formation in the as- nate from those different types of asteroids appear to teroid belt we placed a population planetesimals in outer come from very distinct reservoirs, with distinct iso- Solar System and allow them to accrete pebbles. To topic and elemental signatures [1,2,3]. -
Stanley Keith Runcorn FRS (1922-1995)
Catalogue of the papers and correspondence of Stanley Keith Runcorn FRS (1922-1995) VOLUME 11 Section G: Societies and organisations by Timothy E. Powell and Caroline Thibeaud NCUACS catalogue no. 104/3/02 S.K. Runcorn 124 NCUACS 104/3/02 SECTION G SOCIETIES AND ORGANISATIONS G.1-G.732 G.1 ACADEMIA EUROPAEA G.2-G.6 AMERICAN GEOPHYSICAL UNION G.7-G.11 BRITISH ASSOCIATION FOR THE ADVANCEMENT OF SCIENCE G.12-G.63 COSPAR (COMMITTEE ON SPACE RESEARCH) G.64-G.67 DEPARTMENT OF ENERGY: ENERGY TECHNOLOGY SUPPORT UNIT G.68-G.76 EUROPEAN GEOPHYSICAL SOCIETY G.77 EUROPEAN PLANETARY GEOLOGY CONSORTIUM G.78-G.111 EUROPEAN SCIENCE FOUNDATION G.112-G.1S3 EUROPEAN SPACE AGENCY G.1S4-G.230 INTERNATIONAL ASTRONOMICAL UNION G.231-G.277 INTERNATIONAL UNION OF GEODESY AND GEOPHYSICS G.278 INTERNATIONAL UNION OF GEOLOGICAL SCIENCES G.279-G.294 INTER-UNION COMMISSION FOR STUDIES OF THE MOON G .29S-G .300 JOINT SERVICES WEST-EAST SAHARA EXPEDITION G.301, G.302 LIBERAL PARTY G.303-G.311 LUNAR SCIENCE INSTITUTE S.K. Runcorn 125 NCUACS 104/3/02 Societies and organisations G.312 METEORITICAL SOCIETY G.313 MINERALOLOGICAL SOCIETY G.314-G.319 MINISTRY OF SUPPLY G.320 MUSEUM OF NORTHERN ARIZONA G.321-G.333 NATIONAL AERONAUTICS AND SPACE ADMINISTRATION (NASA) G.334-G.338 NATIONAL SCIENCE FOUNDATION G.339-G.342 NORTH ATLANTIC TREATY ORGANISATION (NATO) G.343 NUFFIELD FOUNDATION G.344-G.365 POI\ITIFICAL ACADEMY OF SCIENCES G.366 PROVINCIAAL UTRECHTS GENOOTSCHAP VAN KUISTEN EN WETENSCHAPPEN G.367-G.386 ROYAL ASTRONOMICAL SOCIETY G.387-G.731 ROYAL SOCIETY G.732 STANDING CONFERENCE OF PROFESSORS OF PHYSICS S.K. -
Allowed Planetary Orbits
RELATIONSHIPS OF PARAMETERS OF PLANETARY ORBITS IN SOLAR---TYPE-TYPE SYSTEMS FACULTY OF SCIENCE, PALACKÝ UNIVERSITY, OLOMOUC RELATIONSHIPS OF PARAMETERS OF PLANETARY ORBITS IN SOLAR-TYPE SYSTEMS DOCTORAL THESIS PAVEL PINTR OLOMOUC 2013 VYJÁD ŘENÍ O PODÍLNICTVÍ Prohlašuji, že všichni auto ři se podíleli stejným dílem na níže uvedených článcích: Pintr P., Pe řinová V.: The Solar System from the quantization viewpoint. Acta Universitatis Palackianae, Physica, 42 - 43 , 2003 - 2004, 195 - 209. Pe řinová V., Lukš A., Pintr P.: Distribution of distances in the Solar System. Chaos, Solitons and Fractals 34 , 2007, 669 - 676. Pintr P., Pe řinová V., Lukš A.: Allowed planetary orbits. Chaos, Solitons and Fractals 36 , 2008, 1273 - 1282. Pe řinová V., Lukš A., Pintr P.: Regularities in systems of planets and moons. In: Solar System: Structure, Formation and Exploration . Editor: Matteo de Rossi, Nova Science Publishers, USA (2012), pp. 153-199. ISBN: 978-1-62100-057-0. Pintr P.: Závislost fotometrických parametr ů hv ězd na orbitálních parametrech exoplanet. Jemná Mechanika a Optika 11 - 12 , 2012, 317 - 319. Pintr P., Pe řinová V., Lukš A.: Areal velocities of planets and their comparison. In : Quantization and Discretization at Large Scales . Editors: Smarandache F., Christianto V., Pintr P., ZIP Publishing, Ohio, USA (2012), pp. 15 - 26. ISBN: 9781599732275. Pintr P., Pe řinová V., Lukš A., Pathak A.: Statistical and regression analyses of detected extrasolar systems. Planetary and Space Science 75 , 2013, 37 - 45. Pintr P., Pe řinová V., Lukš A., Pathak A.: Exoplanet habitability for stellar spectral classes F, G, K and M. 2013, v p říprav ě. -
Dust in Brown Dwarfs and Extrasolar Planets V
A&A 603, A123 (2017) Astronomy DOI: 10.1051/0004-6361/201629696 & c ESO 2017 Astrophysics Dust in brown dwarfs and extrasolar planets V. Cloud formation in carbon- and oxygen-rich environments Ch. Helling, D. Tootill, P. Woitke, and G. Lee Centre for Exoplanet Science, SUPA, School of Physics and Astronomy, University of St. Andrews, North Haugh, St. Andrews, Fife, KY16 9SS, UK e-mail: [email protected] Received 12 September 2016 / Accepted 6 December 2016 ABSTRACT Context. Recent observations indicate potentially carbon-rich (C/O > 1) exoplanet atmospheres. Spectral fitting methods for brown dwarfs and exoplanets have invoked the C/O ratio as additional parameter but carbon-rich cloud formation modeling is a challenge for the models applied. The determination of the habitable zone for exoplanets requires the treatment of cloud formation in chemically different regimes. Aims. We aim to model cloud formation processes for carbon-rich exoplanetary atmospheres. Disk models show that carbon-rich or near-carbon-rich niches may emerge and cool carbon planets may trace these particular stages of planetary evolution. Methods. We extended our kinetic cloud formation model by including carbon seed formation and the formation of C[s], TiC[s], SiC[s], KCl[s], and MgS[s] by gas-surface reactions. We solved a system of dust moment equations and element conservation for a prescribed Drift-Phoenix atmosphere structure to study how a cloud structure would change with changing initial C/O0 = 0:43 ::: 10:0. Results. The seed formation efficiency is lower in carbon-rich atmospheres than in oxygen-rich gases because carbon is a very effective growth species. -
Arthur C. Clarke and Cs Lewis on Moral
Kaufmann, “Riddles in Space” LATCH, Vol. 6, 2013, pp. 55-74 RIDDLES IN SPACE: ARTHUR C. CLARKE AND C.S. LEWIS ON MORAL EXTRAPOLATION By U. Milo Kaufmann University of Illinois, Urbana-Champagne (emeritus) With many matters of prediction science fiction has proved to be prescient. When the genre has been too accurate, as with sundry technological innovations such as the submarine, the prophetic works have tended to lose their interest for the general reader. With another kind of prediction, however, in which utterly novel situations or agents are presented, it is common for perennial moral mysteries to be engaged and, with historic actualization delayed for whatever reasons, it is difficult to be certain just how plausible the projections are. It is not too early to provide some simple definitions and distinctions which will help us in discussing several moral riddles posed when SF masters such as C. S. Lewis and Arthur C. Clarke follow their imaginations into space. 55 Kaufmann, “Riddles in Space” LATCH, Vol. 6, 2013, pp. 55-74 Any one-time student of plane geometry or or statistical graphing will recall that extrapolation is projecting points beyond the line defined by given points. In logic, extrapolation has an analogue in the process of induction, or inducing a general truth from multiple examples. In a legal system we have what is simply described as case law or the resolution of the new challenge by way of precedents. In casuistry, or the disciplines of resolving moral questions, we have the innumerable old volumes common to Scholastic and other writers, dealing in cases of conscience.