A Dearth of Small Particles in the Transiting Material Around the White Dwarf WD 1145+017
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. -
197 3Apj. . .186.1107S the Astrophysical Journal, 186:1107
The Astrophysical Journal, 186:1107-1125, 1973 December 15 .186.1107S . © 1973. The American Astronomical Society. All rights reserved. Printed in U.S.A. 3ApJ. 197 PHASE EQUILIBRIA IN MOLECULAR HYDROGEN-HELIUM MIXTURES AT HIGH PRESSURES* W. B. Streett Science Research Laboratory, U.S. Military Academy, West Point, New York Received 1973 June 11 ABSTRACT Experiments on phase behavior in hydrogen-helium mixtures have been carried out at pressures up to 9.3 kilobars, at temperatures from 26° to 100° K. Two distinct fluid phases are shown to exist at supercritical temperatures and high pressures. Both the trend of the experimental results and an analysis based on the van der Waals theory of mixtures suggest that this fluid-fluid phase separation persists at temperatures and pressures beyond the range of these experiments, perhaps even to the limits of stability of the molecular phases. The results confirm earlier predictions concerning the form of the hydrogen-helium phase diagram in the region of pressure-induced solidification of the molecular phases at supercritical temperatures. The implications of this phase diagram for planetary interiors are discussed. Subject headings: gas dynamics — interiors, planetary — molecules I. INTRODUCTION The properties of hydrogen-helium mixtures are of interest for several reasons. From a theoretical standpoint, they are of interest because they are composed of the two elements with the simplest atomic and molecular structures, and would seem to be among the mixtures most amenable to a theoretical treatment based on first principles. However, it is fair to say that a satisfactory theory of dense mixtures of molecular hydrogen and helium has yet to be developed. -
Effects of Helium Phase Separation on the Evolution of Extrasolar Giant Planets
Accepted to ApJ, February, 2004 A Preprint typeset using L TEX style emulateapj v. 11/12/01 EFFECTS OF HELIUM PHASE SEPARATION ON THE EVOLUTION OF EXTRASOLAR GIANT PLANETS Jonathan J. Fortney1, W. B. Hubbard1 Accepted to ApJ, February, 2004 ABSTRACT We build on recent new evolutionary models of Jupiter and Saturn and here extend our calculations to investigate the evolution of extrasolar giant planets of mass 0.15 to 3.0 MJ. Our inhomogeneous thermal history models show that the possible phase separation of helium from liquid metallic hydrogen in the deep interiors of these planets can lead to luminosities ∼ 2 times greater than have been predicted by homogeneous models. For our chosen phase diagram this phase separation will begin to affect the planets’ evolution at ∼ 700 Myr for a 0.15 MJ object and ∼ 10 Gyr for a 3.0 MJ object. We show how phase separation affects the luminosity, effective temperature, radii, and atmospheric helium mass fraction as a function of age for planets of various masses, with and without heavy element cores, and with and without the effect of modest stellar irradiation. This phase separation process will likely not affect giant planets within a few AU of their parent star, as these planets will cool to their equilibrium temperatures, determined by stellar heating, before the onset of phase separation. We discuss the detectability of these objects and the likelihood that the energy provided by helium phase separation can change the timescales for formation and settling of ammonia clouds by several Gyr. We discuss how correctly incorporating stellar irradiation into giant planet atmosphere and albedo modeling may lead to a consistent evolutionary history for Jupiter and Saturn. -
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. -
Habitable Environments in Late Stellar Evolution
Habitable Environments in Late Stellar Evolution Conditions for Abiogenesis in the Planetary Systems of White Dwarfs Author: Dewy Peters Supervisor: Prof. dr. F.F.S. van der Tak A thesis submitted in fulfillment of the requirements for the degree BSc in Astronomy Faculty of Science and Engineering University of Groningen The Netherlands March 2021 Abstract With very high potential transit-depths and an absence of stellar flare activity, the planets of White Dwarfs (WDs) are some of the most promising in the search for detectable life. Whilst planets with Earth-like masses and radii have yet to be detected around WDs, there is considerable evidence from spectroscopic and photometric observations that both terrestrial and gas-giant planets are capable of surviving post-main sequence evolution and migrating into the WD phase. WDs are also capable of hosting stable Habitable Zones outside orbital distances at which Earth-mass plan- ets would be disintegrated by tidal forces. Whilst transition- ing to the WD Phase, a main-sequence star has to progress along the Asymptotic Giant Branch (AGB), whereby orbit- ing planets would be subjected to atmospheric erosion by its harsh stellar winds. As a trade-off, the Circumstellar En- velope (CSE) of an AGB star is found to be rich in organics and some of the simple molecules from which more complex prebiotic molecules such as amino acids and simple sugars can be synthesised. It is found that planets with initial or- bital distances equivalent to those of Saturn and the Kuiper Belt would be capable of accreting a mass between 1 and 20 times that of the Earth’s atmosphere from the CSE and as a result, could obtain much of the material necessary to sustain life after the AGB and also experience minimal at- mospheric erosion. -
Part 1: the 1.7 and 3.9 Earth Radii Rule
Hi this is Steve Nerlich from Cheap Astronomy www.cheapastro.com and this is What are exoplanets made of? Part 1: The 1.7 and 3.9 earth Radii rule. As of August 2016, the current count of confirmed exoplanets is up around 3,400 in 2,617 systems – with 590 of those systems confirmed to be multiplanet systems. And the latest thinking is that if you want to understand what exoplanets are made of you need to appreciate the physical limits of planet-hood, which are defined by the boundaries of 1.7 and 3.9 Earth radii . Consider that the make-up of an exoplanet is largely determined by the elemental make up of its protoplanetary disk. While most material in the Universe is hydrogen and helium – these are both tenuous gases. In order to generate enough gravity to hang on to them, you need a lot of mass to start with. So, if you’re Earth, or anything up to 1.7 times the radius of Earth – you’ve got no hope of hanging onto more than a few traces of elemental hydrogen and helium. Indeed, any exoplanet that’s less than 1.7 Earth radii has to be primarily composed of non-volatiles – that is, things that don’t evaporate or blow away easily – to have any chance of gravitationally holding together. A non-volatile exoplanet might be made of rock – which for our Solar System is a primarily silicon/oxygen based mineral matrix, but as we’ll hear, small sub-1.7 Earth radii exoplanets could be made of a whole range of other non-volatile materials. -
Shallow Ultraviolet Transits of WD 1145+017
Shallow Ultraviolet Transits of WD 1145+017 Item Type Article Authors Xu, Siyi; Hallakoun, Na’ama; Gary, Bruce; Dalba, Paul A.; Debes, John; Dufour, Patrick; Fortin-Archambault, Maude; Fukui, Akihiko; Jura, Michael A.; Klein, Beth; Kusakabe, Nobuhiko; Muirhead, Philip S.; Narita, Norio; Steele, Amy; Su, Kate Y. L.; Vanderburg, Andrew; Watanabe, Noriharu; Zhan, Zhuchang; Zuckerman, Ben Citation Siyi Xu et al 2019 AJ 157 255 DOI 10.3847/1538-3881/ab1b36 Publisher IOP PUBLISHING LTD Journal ASTRONOMICAL JOURNAL Rights Copyright © 2019. The American Astronomical Society. All rights reserved. Download date 09/10/2021 04:17:12 Item License http://rightsstatements.org/vocab/InC/1.0/ Version Final published version Link to Item http://hdl.handle.net/10150/634682 The Astronomical Journal, 157:255 (12pp), 2019 June https://doi.org/10.3847/1538-3881/ab1b36 © 2019. The American Astronomical Society. All rights reserved. Shallow Ultraviolet Transits of WD 1145+017 Siyi Xu (许偲艺)1 ,Na’ama Hallakoun2 , Bruce Gary3 , Paul A. Dalba4 , John Debes5 , Patrick Dufour6, Maude Fortin-Archambault6, Akihiko Fukui7,8 , Michael A. Jura9,21, Beth Klein9 , Nobuhiko Kusakabe10, Philip S. Muirhead11 , Norio Narita (成田憲保)8,10,12,13,14 , Amy Steele15, Kate Y. L. Su16 , Andrew Vanderburg17 , Noriharu Watanabe18,19, Zhuchang Zhan (詹筑畅)20 , and Ben Zuckerman9 1 Gemini Observatory, 670 N. A’ohoku Place, Hilo, HI 96720, USA; [email protected] 2 School of Physics and Astronomy, Tel-Aviv University, Tel-Aviv 6997801, Israel 3 Hereford Arizona Observatory, Hereford, AZ 85615, USA -
NASA Data Used to Discover Eighth Planet Circling Distant Star
Journal of Aircraft and Spacecraft Technology Review NASA Data Used to Discover Eighth Planet Circling Distant Star 1 2 2 1 Relly Victoria Petrescu, Raffaella Aversa, Antonio Apicella and Florian Ion Tiberiu Petrescu 1ARoTMM-IFToMM, Bucharest Polytechnic University, Bucharest, (CE), Romania 2Department of Architecture and Industrial Design, Advanced Material Lab, Second University of Naples, 81031 Aversa (CE), Italy Article history Abstract: Discovering the origins of life and colonizing extraterrestrial planets Received: 09-01-2018 are two of the greatest ambitions that the international scientific community has Revised: 13-01-2018 today. Today, NASA is more prepared than ever to embark on an Accepted: 18-01-2018 unprecedented race to conquer other worlds. The Kepler mission, named after Johannes Kepler, the German astronomer of the 16th-17th centuries, was Corresponding Author: Florian Ion Tiberiu Petrescu scheduled to begin on March 7, 2009. In this mission, Space Agency released ARoTMM-IFToMM, space from the Cape Canaveral Air Force Base, Florida, a Delta II rocket that Bucharest Polytechnic will carry the Kepler space probe. It will try to identify Earth-like planets that University, Bucharest, (CE), orbitate stars similar to the Sun in a warm area of space, with liquid water and Romania oxygen, that is, heavenly bodies that have all the conditions of life formation E-mail: [email protected] and maintenance. Kepler is looking for a new Earth. Kepler is a critical component of NASA's efforts to identify and study planets with Earth-like eco- conditions. The results of the Kepler space photometer will prove to be extremely important in understanding the frequency of Earth-sized planets in our galaxy. -
The Kepler Revolution Observations and Satellite Inferences of the Kepler Space Telescope Will Soon Run out of Fuel and End Its Mission
VOL. 99 • NO. 10 • OCT 2018 Models That Forecast Wildfires Recording the Roar of a Hurricane Earth & Space Science News How Much Snow Is in the World? The Honors and Recognition Committee is pleased to announce the recipients of this year’s Union Medals, Awards, and Prizes honors.agu.org Earth & Space Science News Contents OCTOBER 2018 PROJECT UPDATE VOLUME 99, ISSUE 10 20 Seismic Sensors Record a Hurricane’s Roar Newly installed infrasound sensors at a Global Seismographic Network station on Puerto Rico recorded the sounds of Hurricane Maria passing overhead. PROJECT UPDATE 26 How Can We Find Out How Much Snow Is in the World? In Colorado forests, NASA scientists and a multinational team of researchers test the limits of satellite remote sensing for measuring the water content of snow. 30 OPINION Global Water Clarity: COVER 14 Continuing a Century- Long Monitoring An approach that combines field The Kepler Revolution observations and satellite inferences of The Kepler Space Telescope will soon run out of fuel and end its mission. Here are nine Secchi depth could transform how we assess fundamental discoveries about planets aided by Kepler, one for each year since its water clarity across the globe and pinpoint launch. key changes over the past century. Earth & Space Science News Eos.org // 1 Contents DEPARTMENTS Senior Vice President, Marketing, Communications, and Digital Media Dana Davis Rehm: AGU, Washington, D. C., USA; [email protected] Editors Christina M. S. Cohen Wendy S. Gordon Carol A. Stein California Institute Ecologia Consulting, Department of Earth and of Technology, Pasadena, Austin, Texas, USA; Environmental Sciences, Calif., USA; wendy@ecologiaconsulting University of Illinois at cohen@srl .caltech.edu .com Chicago, Chicago, Ill., José D. -
Fifth Giant Ex-Planet of the Solar System: Characteristics and Remnants
Fifth giant ex-planet of the Solar System: characteristics and remnants Yury I. Rogozin* Abstract In recent years it has coming to light that the early outer Solar System likely might have somewhat more planets than today. However, to date there is unknown what a former giant planet might in fact have represented and where its orbit may certainly have located. Using the originally suggested relations, we have found the reasonable orbital and physical characteristics of the icy giant ex-planet, which in the past may have orbited the Sun about in the halfway between Saturn and Uranus. Validity of the results obtained here is supported by a feasibility of these relations to other objects of the outer Solar System. A possible linkage between the fifth giant ex-planet and the puzzling objects of the outer Solar System such as the Saturn’s rings and the irregular moons Triton and Phoebe existing today is briefly discussed. Keywords: planets and satellites; individuals: fifth giant ex-planet, Saturn´s rings, Triton, Phoebe 1 Introduction According to the existing ideas of the formation of the Solar System its planetary structure is held unchanged during about 4.5 billion years. Such a static situation of the things had been embodied, particularly, in offered in 1766 Titius-Bode’s rule of the orbital distances for known at that time the seven planets from Mercury to Uranus. As it is known, the conformity to this rule for planets Neptune and Pluto discovered subsequently has appeared much worse than for before known seven planets. However, the essential departures of the real orbital distances from this rule for these two planets so far have not obtained any explained justifying within the framework of such conservative insights into a structure of the Solar System. -
FINAL TECHNICAL REPORT NEIL W. ASHCROFT PROFESSOR of PHYSICS August 1972 To
N.A.S.A. ASTROPHYSICAL MATERIALS SCIENCE: THEORY FINAL TECHNICAL REPORT NEIL W. ASHCROFT PROFESSOR OF PHYSICS August 1972 to September 1978 -' Laboratory of Atomic and ' Solid State Physics Cornell University, Ithaca, N.Y. 14853 (NASA-CR-157782) ASTROPHYSICAL MATERIALS N79-10978 SCIENCE: THEORY Final Technical Report, Aug. 1972- Sep. 1978 (Cornell Univ., Ithaca, N. Y.) 19,2 p HC A09/MF A01 CSCL 03B Unclas G3/9O 36040 GRANT NUMBER NGR-33-010-188 ASTROPHYSICAL MATERIALS SCIENCE: THEORY PROJECT SUMMARY: 1972-1978 Since the initial award of Grant NGR-33-010-188 in summer of 1972, the aim of the project "Astrophysical Materials Science: Theory" has been to develop analytic methods to better our understanding of common astrophysical materials particularly those subjected to extreme physical conditions. The program has been administered in the past by the staff of the Lewis Research Center, National Aeronautics and Space Administration, Cleveland, Ohio. Beginning Oct. 1, 1978 the project will be administered by N.A.S.A. Washington, re-appearing under the same title as NSG-7487. This document briefly summarises the research discoveries and work carried out over the last six or so years. Hydrogen and helium constitute by far the most abundant of the elements and it is no accident that the research has focussed heavily on these elements in their condensed forms, both as pure substances and in mixtures. It will be seen below,that the research has combined the fundamental with the pragmatic. The proper and complete under standing of materials of astrophysical interest requires a deep appreciation of their physical properties, especially when taken into the unusual ranges of extreme conditions. -
Analysis of Exoplanetary Transit Light Curves Joshua Adam Carter
Analysis of Exoplanetary Transit Light Curves by Joshua Adam Carter B.S., Physics, University of North Carolina at Chapel Hill, 2004 B.S., Mathematics, University of North Carolina at Chapel Hill, 2004 Submitted to the Department of Physics in partial fulfillment of the requirements for the degree oft MASSACHUSETTS INSTITUTE Doctor of Philosophy at the MASSACHUSETTS INSTITUTE OF TECHNOLOGY ARCHIVES September 2009 © Massachusetts Institute of Technology 2009. All rights reserved. Author ................ .............. Department of Physics 31, 2009 7A .August Certified by....... Joshua N. Winn Assistant Professor of Physics Class of 1942 Career Development Professor Thesis Supervisor A Accepted by ............................ TlW rs J. Greytak Lester Wolfe Professor of Physics Associate Department Head for Education Analysis of Exoplanetary Transit Light Curves by Joshua Adam Carter Submitted to the Department of Physics on August 31, 2009, in partial fulfillment of the requirements for the degree of Doctor of Philosophy Abstract This Thesis considers the scenario in which an extra-solar planet (exoplanet) passes in front of its star relative to our observing perspective. In this event, the light curve measured for the host star features a systematic drop in flux occurring once every orbital period as the exoplanet covers a portion of the stellar disk. This exoplanetary transit light curve provides a wealth of information about both the planet and star. In this Thesis we consider the transit light curve as a tool for characterizing the exoplanet. The Thesis can divided into two parts. In the first part, comprised of the second and third chapters, I assess what ob- servables describing the exoplanet (and host) may be measured, how well they can be measured, and what effect systematics in the light curve can have on our estimation of these parameters.