The Search for Other Solar Systems
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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. -
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. -
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. -
A 4565 Myr Old Andesite from an Extinct Chondritic Protoplanet
A 4565 Myr old andesite from an extinct chondritic protoplanet. Jean-Alix Barrata*, Marc Chaussidonb, Akira Yamaguchic, Pierre Beckd, Johan Villeneuvee, David J. Byrnee, Michael W. Broadleye, Bernard Martye a Univ Brest, Institut Universitaire Européen de la Mer (IUEM), UMR 6539, Place Nicolas Copernic, F- 29280 Plouzané, France ;b Université de Paris, Institut de pHysique du globe de Paris, CNRS, F-75005 Paris;c National Institute of Polar ResearcH, Tokyo, 190-8518, Japan ;dUniversite Grenoble Alpes, CNRS, Institut de Planetologie et d’Astrophysique de Grenoble (IPAG), Saint-Martin d’Heres, France;e Université de Lorraine, CNRS, CRPG, F-54000 Nancy, France. *Corresponding autHor Jean-Alix Barrat Email: [email protected] Abstract The age of iron meteorites implies that accretion of protoplanets began during the first millions of years of the solar system. Due to the Heat generated by 26Al decay, many early protoplanets were fully differentiated, with an igneous crust produced during the cooling of a magma ocean, and the segregation at depth of a metallic core. The formation and nature of the primordial crust generated during the early stages of melting is poorly understood, due in part to the scarcity of available samples. The newly discovered meteorite Erg CHecH 002 (EC 002) originates from one sucH primitive igneous crust, and has an andesite bulk composition. It derives from the partial melting of a non-carbonaceous chondritic reservoir, witH no depletion in alkalis relative to the sun’s photosphere, and at a high melting rate of around 25%. Moreover, EC 002 is to date, the oldest known piece of an igneous crust witH a 26Al-26Mg crystallization age of 4565.0 Myr. -
Origin of Water Ice in the Solar System 309
Lunine: Origin of Water Ice in the Solar System 309 Origin of Water Ice in the Solar System Jonathan I. Lunine Lunar and Planetary Laboratory The origin and early distribution of water ice and more volatile compounds in the outer solar system is considered. The origin of water ice during planetary formation is at least twofold: It condenses beyond a certain distance from the proto-Sun — no more than 5 AU but perhaps as close as 2 AU — and it falls in from the surrounding molecular cloud. Because some of the infalling water ice is not sublimated in the ambient disk, complete mixing between these two sources was not achieved, and at least two populations of icy planetesimals may have been present in the protoplanetary disk. Added to this is a third reservoir of water ice planetesimals representing material chemically processed and then condensed in satellite-forming disks around giant planets. Water of hydration in silicates inward of the condensation front might be a sepa- rate source, if the hydration occurred directly from the nebular disk and not later in the parent bodies. The differences among these reservoirs of icy planetesimals ought to be reflected in diverse composition and abundance of trapped or condensed species more volatile than the water ice matrix, although radial mixing may have erased most of the differences. Possible sources of water for Earth are diverse, and include Mars-sized hydrated bodies in the asteroid belt, smaller “asteroidal” bodies, water adsorbed into dry silicate grains in the nebula, and comets. These different sources may be distinguished by their deuterium-to-hydrogen ratio, and by pre- dictions on the relative amounts of water (and isotopic compositional differences) between Earth and Mars. -
Abstracts of Extreme Solar Systems 4 (Reykjavik, Iceland)
Abstracts of Extreme Solar Systems 4 (Reykjavik, Iceland) American Astronomical Society August, 2019 100 — New Discoveries scope (JWST), as well as other large ground-based and space-based telescopes coming online in the next 100.01 — Review of TESS’s First Year Survey and two decades. Future Plans The status of the TESS mission as it completes its first year of survey operations in July 2019 will bere- George Ricker1 viewed. The opportunities enabled by TESS’s unique 1 Kavli Institute, MIT (Cambridge, Massachusetts, United States) lunar-resonant orbit for an extended mission lasting more than a decade will also be presented. Successfully launched in April 2018, NASA’s Tran- siting Exoplanet Survey Satellite (TESS) is well on its way to discovering thousands of exoplanets in orbit 100.02 — The Gemini Planet Imager Exoplanet Sur- around the brightest stars in the sky. During its ini- vey: Giant Planet and Brown Dwarf Demographics tial two-year survey mission, TESS will monitor more from 10-100 AU than 200,000 bright stars in the solar neighborhood at Eric Nielsen1; Robert De Rosa1; Bruce Macintosh1; a two minute cadence for drops in brightness caused Jason Wang2; Jean-Baptiste Ruffio1; Eugene Chiang3; by planetary transits. This first-ever spaceborne all- Mark Marley4; Didier Saumon5; Dmitry Savransky6; sky transit survey is identifying planets ranging in Daniel Fabrycky7; Quinn Konopacky8; Jennifer size from Earth-sized to gas giants, orbiting a wide Patience9; Vanessa Bailey10 variety of host stars, from cool M dwarfs to hot O/B 1 KIPAC, Stanford University (Stanford, California, United States) giants. 2 Jet Propulsion Laboratory, California Institute of Technology TESS stars are typically 30–100 times brighter than (Pasadena, California, United States) those surveyed by the Kepler satellite; thus, TESS 3 Astronomy, California Institute of Technology (Pasadena, Califor- planets are proving far easier to characterize with nia, United States) follow-up observations than those from prior mis- 4 Astronomy, U.C. -
Formation and Evolution of Planetary Systems
Specialist Topics in Astrophysics: Lecture 2 Formation and Evolution of Planetary Systems Ken Rice ([email protected]) FormationFormation ofof PlanetaryPlanetary SystemsSystems Lecture 2: Main topics • Solar System characteristics • Origin of the Solar System • Building the planets Most theories of planet formation have been carried out in the context of explaining our Solar System • Any theory must first explain the data/observables OriginOrigin ofof ourour SolarSolar SystemSystem To have a successful theory we must explain the following: • Planets revolve in mostly circular orbits in same direction as the Sun spins OriginOrigin ofof ourour SolarSolar SystemSystem • Planetary orbits nearly lie in a single plane (except Pluto [no longer a planet!!] and Mercury), close to the Sun’s equator • Planets are well spaced, and their orbits do not cross or come close to crossing (except Neptune/Pluto) OriginOrigin ofof ourour SolarSolar SystemSystem • All planets (probably) formed at roughly the same time • Meteorites suggest inner portions of the Solar System were heated to ~1500 K during meteorite/planet formation period OriginOrigin ofof ourour SolarSolar SystemSystem • Planet composition varies in a systematic way throughout the Solar System Terrestrial planets are rocky Outer planets are gaseous OriginOrigin ofof ourour SolarSolar SystemSystem • Jupiter/Saturn are dominated by H and He; Neptune/ Uranus have much less H and He (mainly ices, methane, carbon dioxide and ammonia) OriginOrigin ofof OurOur SolarSolar SystemSystem • Planetary satellites -
How Do You Find an Exoplanet?
October 27, 2015 Time: 09:41am chapter1.tex © Copyright, Princeton University Press. No part of this book may be distributed, posted, or reproduced in any form by digital or mechanical means without prior written permission of the publisher. 1 INTRODUCTION For as long as there been humans we have searched for our place in the cosmos. — Carl Sagan, 1980 1.1 My Brief History I am an astronomer, and as such my professional interest is focused on the study of light emitted by objects in the sky. However, unlike many astronomers, my interest in the night sky didn’t begin until later in my life, well into my college education. I don’t have childhood memories of stargazing, I never thought to ask for a telescope for Christmas, I didn’t have a moon-phase calendar on my wall, and I never owned a single book about astronomy until I was twenty-one years old. As a child, my closest approach to the subject of astronomy was a poster of the Space Shuttle that hung next to my bed, but my interest was piqued more by the intricate mechanical details of the spacecraft rather than where it traveled. Looking back, I suppose the primary reason for my ignorance of astronomy was because I grew up in a metropolitan area, in the North County of St. Louis, Missouri. The skies are often cloudy in the winter when the nights are longest, the evenings are bright with light For general queries, contact [email protected] October 27, 2015 Time: 09:41am chapter1.tex © Copyright, Princeton University Press. -
The Tessmann Planetarium Guide to Exoplanets
The Tessmann Planetarium Guide to Exoplanets REVISED SPRING 2020 That is the big question we all have: Are we alone in the universe? Exoplanets confirm the suspicion that planets are not rare. -Neil deGrasse Tyson What is an Exoplanet? WHAT IS AN EXOPLANET? Before 1990, we had not yet discovered any planets outside of our solar system. We did not have the methods to discover these types of planets. But in the three decades since then, we have discovered at least 4158 confirmed planets outside of our system – and the count seems to be increasing almost every day. We call these worlds exoplanets. These worlds have been discovered with the help of new and powerful telescopes, on Earth and in space, including the Hubble Space Telescope (HST). The Kepler Spacecraft (artist’s conception, below) and the Transiting Exoplanet Survey Satellite (TESS) were specifically designed to hunt for new planets. Kepler discovered 2662 planets during its search. TESS has discovered 46 planets so far and has found over 1800 planet candidates. In Some Factoids: particular, TESS is looking for smaller, rocky exoplanets of nearby, bright stars. An earth-sized planet, TOI 700d, was discovered by TESS in January 2020. This planet is in its star’s Goldilocks or habitable zone. The planet is about 100 light years away, in the constellation of Dorado. According to NASA, we have discovered 4158 exoplanets in 3081 planetary systems. 696 systems have more than one planet. NASA recognizes another 5220 unconfirmed candidates for exoplanets. In 2020, a student at the University of British Columbia, named Michelle Kunimoto, discovered 17 new exoplanets, one of which is in the habitable zone of a star. -
Exoplanet Atmosphere Measurements from Direct Imaging
Exoplanet Atmosphere Measurements from Direct Imaging Beth A. Biller and Mickael¨ Bonnefoy Abstract In the last decade, about a dozen giant exoplanets have been directly im- aged in the IR as companions to young stars. With photometry and spectroscopy of these planets in hand from new extreme coronagraphic instruments such as SPHERE at VLT and GPI at Gemini, we are beginning to characterize and classify the at- mospheres of these objects. Initially, it was assumed that young planets would be similar to field brown dwarfs, more massive objects that nonetheless share sim- ilar effective temperatures and compositions. Surprisingly, young planets appear considerably redder than field brown dwarfs, likely a result of their low surface gravities and indicating much different atmospheric structures. Preliminarily, young free-floating planets appear to be as or more variable than field brown dwarfs, due to rotational modulation of inhomogeneous surface features. Eventually, such inho- mogeneity will allow the top of atmosphere structure of these objects to be mapped via Doppler imaging on extremely large telescopes. Direct imaging spectroscopy of giant exoplanets now is a prelude for the study of habitable zone planets. Even- tual direct imaging spectroscopy of a large sample of habitable zone planets with future telescopes such as LUVOIR will be necessary to identify multiple biosigna- tures and establish habitability for Earth-mass exoplanets in the habitable zones of nearby stars. Introduction Since 1995, more than 3000 exoplanets have been discovered, mostly via indirect means, ushering in a completely new field of astronomy. In the last decade, about a dozen planets have been directly imaged, including archetypical systems such as arXiv:1807.05136v1 [astro-ph.EP] 13 Jul 2018 Beth A. -
Thoughts on the Nebular Theory of Our Planetary System Formation
Thoughts on the Nebular Theory of our Planetary System Formation Thierry De Mees e-mail: thierrydemees (at) telenet.be The Nebular Hypothesis For the protoplanetary disk, a large number of hypotheses follow subsequently to explain how the small dust would be The hypothesis of a Solar Nebula, also known as the Kant- clumping and form planets. Laplace hypothesis, is currently the most accepted explanation I enumerate here some of the keywords and key phrases that for the origin of the Solar System. are usually needed to explain that evolution: turbulence, viscosi- The theory was invented by Emanuel Swedenborg in 1734. ty, transport of the mass, gas drifting outwards, growth of both Immanuel Kant extended Swedenborg's theory further in 1755. the protostar and of the disk radius, mixing of materials, coagula- He thought that if nebulae and gas clouds rotate slowly, they tion, gravitational instability, migration to another orbit, frag- would slowly contract and flatten under their own gravitational mentation into clumps, some will collapse, stochastic growth, force, and eventually the central star and planets of the solar sys- nearly circular orbits, more eccentric orbits, oligarchic growth tem would be formed. A similar model was proposed in 1796 by stage, natural growth restriction, natural sphere of influence, Pierre-Simon Laplace. frost line, by the Solar wind all the gas from the protoplanetary According to the hypothesis a planetary system like the Solar disk is blown away, collisions between protoplanets, the System begins as a large, approximately spherical cloud of very protoplanets disrupt each other's orbits with their gravity, cold interstellar gas.