On the Winds of Carbon Stars and the Origin of Carbon

Total Page:16

File Type:pdf, Size:1020Kb

On the Winds of Carbon Stars and the Origin of Carbon !"#$" # #% &'' '&&' (""") ISBN 45666446 7 6 8 9 :89;: ; < 8 = 6 6 6 > 7 ? 6 ? 6 = 6 @ 6 6 6 6 = 6 :A6; 6 9 6 A6 6 > 6C = 8 @ 6 8 6 8 D8 ? E 8 @ 89 ! "# !9vvvs6 hqThpr Quvp7$ %VhyhVvr vT@&$ ! ! F =G6 =9G45666446 6: HH 7H J K 6; Oh freddled gruntbuggly, Thy micturations are to me As plurdled gabbleblotchits On a lurgid bee. Groop, I implore thee, my foonting turlingdromes And hooptiosly drangle me with crinkly bindlewurdles, Or I will rend thee in the gobblewarts with my blurglecruncheon See if I don’t. List of Papers This thesis is based on the following papers, which are referred to in the text by their Roman numerals. I L. Mattsson,R.Wahlin&S.Höfner,"Dust Driven Mass Loss from Carbon Stars as Function of Stellar Parameters I. - A Grid of Solar-metallicity Wind Models", submitted to Astronomy & Astrophysics (2009) II L. Mattsson, R. Wahlin, S. Höfner & K. Eriksson, "Intense mass loss from C-rich AGB stars at low metallicity?", published in Astronomy & Astrophysics, 484, L5 (2008) III L. Mattsson &S.Höfner,"Dust Driven Mass Loss from Carbon Stars as Function of Stellar Parameters II. - Effects of Relaxing the Small Particle Approximation", preprint (2009) IV L. Mattsson,S.Höfner&F.Herwig,"Mass Loss Evolution and the For- mation of Detached Shells around TP-AGB Stars", published in Astron- omy & Astrophysics, 470, 339 (2007) V L. Mattsson, F. Herwig, S. Höfner, R. Wahlin, M. Lederer, & B. Paxton, "Effects of Carbon-excess Dependent Mass Loss and Molecular Opaci- ties on Models of C-star Evolution", preprint (2009) VI L. Mattsson,"The Origin of Carbon: Low-mass Stars and an Evolving IMF?", preprint (2009) Reprints were made with permission from the publishers. Contents 1 Introduction ............................................. 9 1.1 SettingtheStage....................................... 9 1.2 EvolutionofLIMStars.................................. 10 1.3 WindsofCarbonStars.................................. 11 1.4 TheCosmicMatterCycle:theOriginofCarbon............. 12 1.5 Carbon-basedLifeintheGalaxy.......................... 13 2 Modelling of Dynamic Atmospheres and Dust Driven Winds . 15 2.1 The Success of Numerical Modelling . ..................... 15 2.2 TheFullSetofEquations................................ 16 2.2.1 RadiationHydrodynamics........................... 16 2.2.2 Selfgravity........................................ 18 2.2.3 Equation of State and other aPrioriAssumptions . 18 2.2.4 RadiativeTransfer.................................. 19 2.2.5 DustFormationandOpacity......................... 21 2.3 MethodofComputation................................ 23 2.3.1 BoundaryConditions............................... 23 2.3.2 InitialConditions.................................. 24 2.3.3 The Modelling Procedure . ..................... 25 3 CarbonStarMassLossasFunctionofStellarParameters......... 27 3.1 TheGridofWindModels................................ 27 3.1.1 GeneralProperties................................. 27 3.1.2 Mass-LossThresholdsandtheCarbonExcess .......... 28 3.2 Metallicity Dependence? . ......................... 32 4 RelaxingtheSmallParticleApproximation..................... 35 4.1 SizeableGrains........................................ 35 4.2 HowBadistheSPA?.................................... 36 4.3 SizeMatters!.......................................... 37 5 StellarStructureandEvolution .............................. 41 5.1 BasicIngredients ...................................... 41 5.1.1 Hydrostatic Equilibrium and Energy Generation ........ 41 5.1.2 EnergyTransport.................................. 42 5.1.3 ConvectionintheMLTPicture....................... 43 5.2 RadiativeTransferandtheRôleofGasOpacities ............ 44 5.3 StellarEvolutioninBrief................................ 45 5.4 Nucleosynthesis....................................... 47 5.4.1 TheTriple-alphaProcess............................ 47 5.4.2 TheCN-cycle ..................................... 47 5.5 EffectsofMassLossandMixing.......................... 49 5.5.1 Carbon Production: Dredge-up and Thermal Pulses . 50 5.5.2 Carbon Destruction: The on-set of HBB and AGB life times 50 6 Mass-LossEvolutionandtheOriginofDetachedShells.......... 51 6.1 AConsequenceofHeliumShellFlashes?................... 51 6.2 Two-windInteraction................................... 52 6.3 PulsationsareCritical .................................. 53 6.4 SoHowDoesDetachedShellsForm?...................... 55 7 ModelsofCarbonStarEvolution............................. 57 7.1 Mass-lossEffectsonC-starEvolution...................... 57 7.2 TheOriginoftheSuperwind............................. 58 7.3 LimitedNucleosynthesis................................ 59 8 GalacticChemicalEvolutionModels.......................... 61 8.1 TheMilkyWayGalaxy.................................. 61 8.1.1 TheGalacticDisc.................................. 61 8.1.2 TheStellarHaloandthe"ThickDisc" ................. 62 8.2 OriginoftheElements.................................. 62 8.3 ModelIngredientsandEquations......................... 63 8.3.1 GalaxyFormation.................................. 64 8.3.2 GalacticDynamics................................. 65 8.3.3 StarFormation.................................... 66 8.3.4 TheInitialMassFunction........................... 66 8.3.5 EvolutionoftheISMandElementalRatios............. 67 8.3.6 SupernovaetypeIa................................. 68 8.4 StellarYields.......................................... 69 9 AnExtensionofthePadoan-NordlundTheoryoftheIMF ........ 71 9.1 AUniversalIMF?....................................... 71 9.2 TurbulentFragmentation ............................... 71 9.3 EnvironmentalVariationsoftheIMF...................... 75 9.4 AlternativeMechanisms ................................ 77 10TheOriginofCarbon ...................................... 79 10.1TheMakingofCarbon.................................. 79 10.2ATop-heavyIMF?...................................... 80 10.3LowMassStarsandanEvolvingIMF? ..................... 82 11ConcludingRemarksandFutureProspects .................... 85 11.1FutureWork .......................................... 85 11.1.1 Subsolar Metallicity . ............................. 85 11.1.2DriftandGrainSizes ............................... 85 11.1.3DetachedShells ................................... 86 11.1.4GalacticChemicalEvolution......................... 86 11.2LifefromaWiderPerspective............................ 86 11.2.1AGalacticHabitableZone?.......................... 86 11.2.2CarbonStarsandCarbon-basedLife.................. 88 ContributionstoIncludedPapers............................... 91 Sammanfattning............................................. 93 Acknowledgements .......................................... 97 Bibliography ................................................ 99 1. Introduction "We are all in the gutter, but some of us are looking at the stars." Oscar Wilde This is a thesis about stars, and to some extent galaxies. More precisely, it is a thesis about the gas, dust and stars that we find in our Galaxy and how it all is evolving. The content may at first glance seem as if it consists of sep- arate parts, but that is not the case. This introductory chapter presents the context of this thesis in an attempt to explain how models of the build-up of heavy elements in the Universe actually connect with models of dynamic stellar atmospheres. 1.1 Setting the Stage There exist many fundamental, unanswered questions in the natural sci- ences, not the least in astrophysics. Such questions are the origin and early evolution of the universe, as well as the formation and evolution of galax- ies. Another question of the same magnitude is the origin of life in the uni- verse (or at least on Earth). Life, as we know it, requires the existence of carbon, nitrogen, oxygen and a few other elements. However, with the ex- ception of hydrogen, helium and a small amount of lithium, all the atomic nuclei in the universe are created in stars, through nuclear reactions (re- ferred to as nucleosynthesis), where light elements are combined into heav- ier elements. These elements have then been expelled from the stars, either through relatively slow mass loss (stellar winds), as in the case of low and intermediate mass stars, or explosively, as in the case of high mass stars. Thus, the interstellar medium (ISM) in a galaxy is continuously enriched in heavy elements as new generations of stars form, evolve and expel their newly synthesised elements. This is what is referred to as the chemical evo- lution of galaxies, which in the strict sense of the word has little to do with chemistry, but rather the build-up of heavy elements over time. These new elements then form molecules and dust in stars and interstellar space and are later incorporated into new generations of stars, planets and eventually life on at least one planet. In this thesis, which is part of a rather ambitious project aiming at a better understanding of the rôle of low- and intermediate-mass (LIM) stars in this "big scheme", results are presented regarding the theoretical modelling of mass-loss from carbon stars and the cosmic origin of atomic carbon
Recommended publications
  • Large Molecules in the Envelope Surrounding IRC+10216
    Mon. Not. R. Astron. Soc. 316, 195±203 (2000) Large molecules in the envelope surrounding IRC110216 T. J. Millar,1 E. Herbst2w and R. P. A. Bettens3 1Department of Physics, UMIST, PO Box 88, Manchester M60 1QD 2Departments of Physics and Astronomy, The Ohio State University, Columbus, OH 43210, USA 3Research School of Chemistry, Australian National University, ACT 0200, Australia Accepted 2000 February 22. Received 2000 February 21; in original form 2000 January 21 ABSTRACT A new chemical model of the circumstellar envelope surrounding the carbon-rich star IRC110216 is developed that includes carbon-containing molecules with up to 23 carbon atoms. The model consists of 3851 reactions involving 407 gas-phase species. Sizeable abundances of a variety of large molecules ± including carbon clusters, unsaturated hydro- carbons and cyanopolyynes ± have been calculated. Negative molecular ions of chemical 2 2 formulae Cn and CnH 7 # n # 23 exist in considerable abundance, with peak concen- trations at distances from the central star somewhat greater than their neutral counterparts. The negative ions might be detected in radio emission, or even in the optical absorption of background field stars. The calculated radial distributions of the carbon-chain CnH radicals are looked at carefully and compared with interferometric observations. Key words: molecular data ± molecular processes ± circumstellar matter ± stars: individual: IRC110216 ± ISM: molecules. synthesis of fullerenes in the laboratory through chains and rings 1 INTRODUCTION is well-known (von Helden, Notts & Bowers 1993; Hunter et al. The possible production of large molecules in assorted astronomi- 1994), the individual reactions have not been elucidated. Bettens cal environments is a problem of considerable interest.
    [Show full text]
  • Organics in the Solar System
    Organics in the Solar System Sun Kwok1,2 1 Laboratory for Space Research, The University of Hong Kong, Hong Kong, China 2 Department of Earth, Ocean, and Atmospheric Sciences, University of British Columbia, Vancouver, B.C., Canada [email protected]; [email protected] ABSTRACT Complex organics are now commonly found in meteorites, comets, asteroids, planetary satellites, and interplanetary dust particles. The chemical composition and possible origin of these organics are presented. Specifically, we discuss the possible link between Solar System organics and the complex organics synthesized during the late stages of stellar evolution. Implications of extraterrestrial organics on the origin of life on Earth and the possibility of existence of primordial organics on Earth are also discussed. Subject headings: meteorites, organics, stellar evolution, origin of life arXiv:1901.04627v1 [astro-ph.EP] 15 Jan 2019 Invited review presented at the International Symposium on Lunar and Planetary Science, accepted for publication in Research in Astronomy and Astrophysics. –2– 1. Introduction In the traditional picture of the Solar System, planets, asteroids, comets and planetary satellites were formed from a well-mixed primordial nebula of chemically and isotopically uniform composition. The primordial solar nebula was believed to be initially composed of only atomic elements synthesized by previous generations of stars, and current Solar System objects later condensed out of this homogeneous gaseous nebula. Gas, ice, metals, and minerals were assumed to be the primarily constituents of planetary bodies (Suess 1965). Although the presence of organics in meteorites was hinted as early as the 19th century (Berzelius 1834), the first definite evidence for the presence of extraterrestrial organic matter in the Solar System was the discovery of paraffins in the Orgueil meteorites (Nagy et al.
    [Show full text]
  • Origin and Evolution of Carbonaceous Presolar Grains in Stellar Environments
    Bernatowicz et al.: Origin and Evolution of Presolar Grains 109 Origin and Evolution of Carbonaceous Presolar Grains in Stellar Environments Thomas J. Bernatowicz Washington University Thomas K. Croat Washington University Tyrone L. Daulton Naval Research Laboratory Laboratory microanalyses of presolar grains provide direct information on the physical and chemical properties of solid condensates that form in the mass outflows from stars. This informa- tion can be used, in conjunction with kinetic models and equilibrium thermodynamics, to draw inferences about condensation sequences, formation intervals, pressures, and temperatures in circumstellar envelopes and in supernova ejecta. We review the results of detailed microana- lytical studies of the presolar graphite, presolar silicon carbide, and nanodiamonds found in primitive meteorites. We illustrate how these investigations, together with astronomical obser- vation and theoretical models, provide detailed information on grain formation and growth that could not be obtained by astronomical observation alone. 1. INTRODUCTION versed the interstellar medium (ISM) prior to their incorpor- ation into the solar nebula, they serve as monitors of physi- In recent years the laboratory study of presolar grains has cal and chemical processing of grains in the ISM (Bernato- emerged as a rich source of astronomical information about wicz et al., 2003). stardust, as well as about the physical and chemical condi- In this review we focus on carbonaceous presolar grains. tions of dust formation in circumstellar
    [Show full text]
  • Implications for Extraterrestrial Hydrocarbon Chemistry: Analysis Of
    The Astrophysical Journal, 889:3 (26pp), 2020 January 20 https://doi.org/10.3847/1538-4357/ab616c © 2020. The American Astronomical Society. All rights reserved. Implications for Extraterrestrial Hydrocarbon Chemistry: Analysis of Acetylene (C2H2) and D2-acetylene (C2D2) Ices Exposed to Ionizing Radiation via Ultraviolet–Visible Spectroscopy, Infrared Spectroscopy, and Reflectron Time-of-flight Mass Spectrometry Matthew J. Abplanalp1,2 and Ralf I. Kaiser1,2 1 W. M. Keck Research Laboratory in Astrochemistry, University of Hawaii at Manoa, Honolulu, HI 96822, USA 2 Department of Chemistry, University of Hawaii at Manoa, Honolulu, HI 96822, USA Received 2019 October 4; revised 2019 December 7; accepted 2019 December 10; published 2020 January 20 Abstract The processing of the simple hydrocarbon ice, acetylene (C2H2/C2D2), via energetic electrons, thus simulating the processes in the track of galactic cosmic-ray particles penetrating solid matter, was carried out in an ultrahigh vacuum surface apparatus. The chemical evolution of the ices was monitored online and in situ utilizing Fourier transform infrared spectroscopy (FTIR) and ultraviolet–visible spectroscopy and, during temperature programmed desorption, via a quadrupole mass spectrometer with an electron impact ionization source (EI-QMS) and a reflectron time-of-flight mass spectrometer utilizing single-photon photoionization (SPI-ReTOF-MS) along with resonance-enhanced multiphoton photoionization (REMPI-ReTOF-MS). The confirmation of previous in situ studies of ethylene ice irradiation
    [Show full text]
  • Origins of Life: Transition from Geochemistry to Biogeochemistry
    December 2016 Volume 12, Number 6 ISSN 1811-5209 Origins of Life: Transition from Geochemistry to Biogeochemistry NITA SAHAI and HUSSEIN KADDOUR, Guest Editors Transition from Geochemistry to Biogeochemistry Staging Life: Warm Seltzer Ocean Incubating Life: Prebiotic Sources Foundation Stones to Life Prebiotic Metal-Organic Catalysts Protometabolism and Early Protocells pub_elements_oct16_1300&icpms_Mise en page 1 13-Sep-16 3:39 PM Page 1 Reproducibility High Resolution igh spatial H Resolution High mass The New Generation Ion Microprobe for Path-breaking Advances in Geoscience U-Pb dating in 91500 zircon, RF-plasma O- source Addressing the growing demand for small scale, high resolution, in situ isotopic measurements at high precision and productivity, CAMECA introduces the IMS 1300-HR³, successor of the internationally acclaimed IMS 1280-HR, and KLEORA which is derived from the IMS 1300-HR³ and is fully optimized for advanced U-Th-Pb mineral dating. • New high brightness RF-plasma ion source greatly improving spatial resolution, reproducibility and throughput • New automated sample loading system with motorized sample height adjustment, significantly increasing analysis precision, ease-of-use and productivity • New UV-light microscope for enhanced optical image resolution (developed by University of Wisconsin, USA) ... and more! Visit www.cameca.com or email [email protected] to request IMS 1300-HR³ and KLEORA product brochures. Laser-Ablation ICP-MS ~ now with CAMECA ~ The Attom ES provides speed and sensitivity optimized for the most demanding LA-ICP-MS applications. Corr. Pb 207-206 - U (238) Recent advances in laser ablation technology have improved signal 2SE error per sample - Pb (206) Combined samples 0.076121 +/- 0.002345 - Pb (207) to background ratios and washout times.
    [Show full text]
  • Lifetimes of Interstellar Dust from Cosmic Ray Exposure Ages of Presolar Silicon Carbide
    Lifetimes of interstellar dust from cosmic ray exposure ages of presolar silicon carbide Philipp R. Hecka,b,c,1, Jennika Greera,b,c, Levke Kööpa,b,c, Reto Trappitschd, Frank Gyngarde,f, Henner Busemanng, Colin Madeng, Janaína N. Ávilah, Andrew M. Davisa,b,c,i, and Rainer Wielerg aRobert A. Pritzker Center for Meteoritics and Polar Studies, The Field Museum of Natural History, Chicago, IL 60605; bChicago Center for Cosmochemistry, The University of Chicago, Chicago, IL 60637; cDepartment of the Geophysical Sciences, The University of Chicago, Chicago, IL 60637; dNuclear and Chemical Sciences Division, Lawrence Livermore National Laboratory, Livermore, CA 94550; ePhysics Department, Washington University, St. Louis, MO 63130; fCenter for NanoImaging, Harvard Medical School, Cambridge, MA 02139; gInstitute of Geochemistry and Petrology, ETH Zürich, 8092 Zürich, Switzerland; hResearch School of Earth Sciences, The Australian National University, Canberra, ACT 2601, Australia; and iEnrico Fermi Institute, The University of Chicago, Chicago, IL 60637 Edited by Mark H. Thiemens, University of California San Diego, La Jolla, CA, and approved December 17, 2019 (received for review March 15, 2019) We determined interstellar cosmic ray exposure ages of 40 large ago. These grains are identified as presolar by their large isotopic presolar silicon carbide grains extracted from the Murchison CM2 anomalies that exclude an origin in the Solar System (13, 14). meteorite. Our ages, based on cosmogenic Ne-21, range from 3.9 ± Presolar stardust grains are the oldest known solid samples 1.6 Ma to ∼3 ± 2 Ga before the start of the Solar System ∼4.6 Ga available for study in the laboratory, represent the small fraction ago.
    [Show full text]
  • Interstellar Dust Within the Life Cycle of the Interstellar Medium K
    EPJ Web of Conferences 18, 03001 (2011) DOI: 10.1051/epjconf/20111803001 C Owned by the authors, published by EDP Sciences, 2011 Interstellar dust within the life cycle of the interstellar medium K. Demyk1,2,a 1Université de Toulouse, UPS-OMP, IRAP, Toulouse, France 2CNRS, IRAP, 9 Av. colonel Roche, BP. 44346, 31028 Toulouse Cedex 4, France Abstract. Cosmic dust is omnipresent in the Universe. Its presence influences the evolution of the astronomical objects which in turn modify its physical and chemical properties. The nature of cosmic dust, its intimate coupling with its environment, constitute a rich field of research based on observations, modelling and experimental work. This review presents the observations of the different components of interstellar dust and discusses their evolution during the life cycle of the interstellar medium. 1. INTRODUCTION Interstellar dust grains are found everywhere in the Universe: in the Solar System, around stars at all evolutionary stages, in interstellar clouds of all kind, in galaxies and in the intergalactic medium. Cosmic dust is intimately mixed with the gas-phase and represents about 1% of the gas (in mass) in our Galaxy. The interstellar extinction and the emission of diffuse interstellar clouds is reproduced by three dust components: a population of large grains, the BGs (Big Grains, ∼10–500 nm) made of silicate and a refractory mantle, a population of carbonaceous nanograins, the VSGs (Very Small Grains, 1–10 nm) and a population of macro-molecules the PAHs (Polycyclic Aromatic Hydrocarbons) [1]. These three components are more or less abundant in the diverse astrophysical environments reflecting the coupling of dust with the environment and its evolution according to the physical and dynamical conditions.
    [Show full text]
  • Appendix A: Scientific Notation
    Appendix A: Scientific Notation Since in astronomy we often have to deal with large numbers, writing a lot of zeros is not only cumbersome, but also inefficient and difficult to count. Scientists use the system of scientific notation, where the number of zeros is short handed to a superscript. For example, 10 has one zero and is written as 101 in scientific notation. Similarly, 100 is 102, 100 is 103. So we have: 103 equals a thousand, 106 equals a million, 109 is called a billion (U.S. usage), and 1012 a trillion. Now the U.S. federal government budget is in the trillions of dollars, ordinary people really cannot grasp the magnitude of the number. In the metric system, the prefix kilo- stands for 1,000, e.g., a kilogram. For a million, the prefix mega- is used, e.g. megaton (1,000,000 or 106 ton). A billion hertz (a unit of frequency) is gigahertz, although I have not heard of the use of a giga-meter. More rarely still is the use of tera (1012). For small numbers, the practice is similar. 0.1 is 10À1, 0.01 is 10À2, and 0.001 is 10À3. The prefix of milli- refers to 10À3, e.g. as in millimeter, whereas a micro- second is 10À6 ¼ 0.000001 s. It is now trendy to talk about nano-technology, which refers to solid-state device with sizes on the scale of 10À9 m, or about 10 times the size of an atom. With this kind of shorthand convenience, one can really go overboard.
    [Show full text]
  • Book of Abstracts
    THE PHYSICS AND CHEMISTRY OF THE INTERSTELLAR MEDIUM Celebrating the first 40 years of Alexander Tielens' contribution to Science Book of Abstracts Palais des Papes - Avignon - France 2-6 September 2019 CONFERENCE PROGRAM Monday 2 September 2019 Time Speaker 10:00 Registration 13:00 Registration & Welcome Coffee 13:30 Welcome Speech C. Ceccarelli Opening Talks 13:40 PhD years H. Habing 13:55 Xander Tielens and his contributions to understanding the D. Hollenbach ISM The Dust Life Cycle 14:20 Review: The dust cycle in galaxies: from stardust to planets R. Waters and back 14:55 The properties of silicates in the interstellar medium S. Zeegers 15:10 3D map of the dust distribution towards the Orion-Eridanus S. Kh. Rezaei superbubble with Gaia DR2 15:25 Invited Talk: Understanding interstellar dust from polariza- F. Boulanger tion observations 15:50 Coffee break 16:20 Review: The life cycle of dust in galaxies M. Meixner 16:55 Dust grain size distribution across the disc of spiral galaxies M. Relano 17:10 Investigating interstellar dust in local group galaxies with G. Clayton new UV extinction curves 17:25 Invited Talk: The PROduction of Dust In GalaxIES C. Kemper (PRODIGIES) 17:50 Unravelling dust nucleation in astrophysical media using a L. Decin self-consistent, non steady-state, non-equilibrium polymer nucleation model for AGB stellar winds 19:00 Dining Cocktail Tuesday 3 September 2019 08:15 Registration PDRs 09:00 Review: The atomic to molecular hydrogen transition: a E. Roueff major step in the understanding of PDRs 09:35 Invited Talk: The Orion Bar: from ALMA images to new J.
    [Show full text]
  • Laboratory Astrophysics: from Observations to Interpretation
    April 14th – 19th 2019 Jesus College Cambridge UK IAU Symposium 350 Laboratory Astrophysics: From Observations to Interpretation Poster design by: D. Benoit, A. Dawes, E. Sciamma-O’Brien & H. Fraser Scientific Organizing Committee: Local Organizing Committee: Farid Salama (Chair) ★ P. Barklem ★ H. Fraser ★ T. Henning H. Fraser (Chair) ★ D. Benoit ★ R Coster ★ A. Dawes ★ S. Gärtner ★ C. Joblin ★ S. Kwok ★ H. Linnartz ★ L. Mashonkina ★ T. Millar ★ D. Heard ★ S. Ioppolo ★ N. Mason ★ A. Meijer★ P. Rimmer ★ ★ O. Shalabiea★ G. Vidali ★ F. Wa n g ★ G. Del-Zanna E. Sciamma-O’Brien ★ F. Salama ★ C. Wa lsh ★ G. Del-Zanna For more information and to contact us: www.astrochemistry.org.uk/IAU_S350 [email protected] @iaus350labastro 2 Abstract Book Scheduley Sunday 14th April . Pg. 2 Monday 15th April . Pg. 3 Tuesday 16th April . Pg. 4 Wednesday 17th April . Pg. 5 Thursday 18th April . Pg. 6 Friday 19th April . Pg. 7 List of Posters . .Pg. 8 Abstracts of Talks . .Pg. 12 Abstracts of Posters . Pg. 83 yPlenary talks (40') are indicated with `P', review talks (30') with `R', and invited talks (15') with `I'. Schedule Sunday 14th April 14:00 - 17:00 REGISTRATION 18:00 - 19:00 WELCOME RECEPTION 19:30 DINNER BAR OPEN UNTIL 23:00 Back to Table of Contents 2 Monday 15th April 09:00 { 10:00 REGISTRATION 09:00 WELCOME by F. Salama (Chair of SOC) SESSION 1 CHAIR: F. Salama 09:15 E. van Dishoeck (P) Laboratory astrophysics: key to understanding the Universe From Diffuse Clouds to Protostars: Outstanding Questions about the Evolution of 10:00 A.
    [Show full text]
  • Six Phases of Cosmic Chemistry
    Six Phases of Cosmic Chemistry Lukasz Lamza The Pontifical University of John Paul II Department of Philosophy, Chair of Philosophy of Nature Kanonicza 9, Rm. 203 31-002 Kraków, Poland e-mail: [email protected] 1. Introduction The steady development of astrophysical and cosmological sciences has led to a growing appreciation of the continuity of cosmic history throughout which all known phenomena come to being. This also includes chemical phenomena and there are numerous theoretical attempts to rewrite chemistry as a “historical” science (Haken 1978; Earley 2004). It seems therefore vital to organize the immense volume of chemical data – from astrophysical nuclear chemistry to biochemistry of living cells – in a consistent and quantitative fashion, one that would help to appreciate the unfolding of chemical phenomena throughout cosmic time. Although numerous specialist reviews exist (e.g. Shaw 2006; Herbst 2001; Hazen et al. 2008) that illustrate the growing appreciation for cosmic chemical history, several issues still need to be solved. First of all, such works discuss only a given subset of cosmic chemistry (astrochemistry, chemistry of life etc.) using the usual tools and languages of these particular disciplines which does not facilitate drawing large-scale conclusions. Second, they discuss the history of chemical structures and not chemical processes – which implicitly leaves out half of the totality chemical phenomena as non-historical. While it may now seem obvious that certain chemical structures such as aromatic hydrocarbons or pyrazines have a certain cosmic “history”, it might cause more controversy to argue that chemical processes such as catalysis or polymerization also have their “histories”.
    [Show full text]
  • The Effect of Aqueous Alteration and Metamorphism in the Survival of Presolar Silicate Grains in Chondrites
    THE EFFECT OF AQUEOUS ALTERATION AND METAMORPHISM IN THE SURVIVAL OF PRESOLAR SILICATE GRAINS IN CHONDRITES Josep Mª Trigo-Rodriguez Institut of Space Sciences (CSIC), Campus UAB, Facultat de Ciències, Torre C5-parell-2ª, 08193 Bellaterra, Barcelona, Spain. E-mail: [email protected] Institut d’Estudis Espacials de Catalunya (IEEC), Edif.. Nexus, c/Gran Capità, 2-4, 08034 Barcelona, Spain and Jürgen Blum Institut fürGeophysik und extraterrestrische Physik, Technische Universität Braunschweig, Mendelssohnstr. 3, 38106 Braunschweig, Germany. E-mail: [email protected] ABSTRACT Relatively small amounts (typically between 2-200 parts per million) of presolar grains have been preserved in the matrices of chondritic meteorites. The measured abundances of the different types of grains are highly variable from one chondrite to another, but are higher in unequilibrated chondrites that have experienced little or no aqueous alteration and/or metamorphic heating than in processed meteorites. A general overview of the abundances measured in presolar grains (particularly the recently identified presolar silicates) contained in primitive chondrites is presented. Here we will focus on the most primitive chondrite groups, as typically the highest measured abundances of presolar grains occur in primitive chondrites that have experienced little thermal metamorphism. Looking at the most aqueously altered chondrite groups, we find a clear pattern of decreasing abundance of presolar silicate grains with increasing level of aqueous alteration. We conclude that the measured abundances of presolar grains in altered chondrites are strongly biased by their peculiar histories. Scales quantifying the intensity of aqueous alteration and shock metamorphism in chondrites could correlate with the content in presolar silicates.
    [Show full text]