The Leiden Atomic and Molecular Database (LAMDA): Current Status, Recent Updates, and Future Plans
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Phosphine and Ammonia Photochemistry in Jupiter's
40th Lunar and Planetary Science Conference (2009) 1201.pdf PHOSPHINE AND AMMONIA PHOTOCHEMISTRY IN JUPITER’S TROPOSPHERE. C. Visscher1, A. D. Sperier2, J. I. Moses1, and T.C. Keane3. 1Lunar and Planetary Institute, USRA, 3600 Bay Area Blvd., Houston, TX 77058-1113 2Baylor University, Waco, TX 76798, 3Department of Chemistry and Physics, The Sage Colleges, Troy, NY 12180, ([email protected], [email protected]) Introduction: The last comprehensive photo- tions involving the amino radical (NH2) play a larger chemical model for Jupiter’s troposphere was pre- role. We note that this is the first photochemical sented by Edgington et al. [1,2], based upon the work model to include P2H as an intermediate species in PH3 of Atreya et al. [3] and Kaye and Strobel [4-6]. Since photolysis. The equivalent N2Hx species are believed these early studies, numerous laboratory experiments to be important in the combustion chemistry of nitro- have led to an improvement in our understanding of gen compounds [15]. PH3, NH3-PH3, and NH3-C2H2 photochemistry [7-13]. Furthermore, recent Galileo, Cassini, and Earth-based observations have better defined the abundance of key atmospheric constituents as a function of altitude and latitude in Jupiter’s troposphere. These new results provide an opportunity to test and improve theoretical models of Jovian atmospheric chemistry. We have therefore developed a photochemical model for Jupi- ter’s troposphere considering the updated experimental and observational constraints. Using the Caltech/JPL KINETICS code [14] for our photochemical models, our basic approach is two- fold. The validity of our selected chemical reaction list is first tested by simulating the laboratory experiments of PH3, NH3-PH3, and NH3-C2H2 photolysis with pho- tochemical “box” models. -
The Primordial Earth: Hadean and Archean Eons
5th International Symposium on Strong Electromagnetic Fields and Neutron Stars 10 –13 of May, 2017 -Varadero, Cuba HABITABILITY OF THE MILKY WAY REVISITED Rolando Cárdenas and Rosmery Nodarse-Zulueta e-mail: [email protected] Planetary Science Laboratory Universidad Central “Marta Abreu” de Las Villas, Santa Clara, Cuba Abstract • The discoveries of the last three decades on deep sea and deep crust of planet Earth show that life can thrive in many places where solar radiation does not reach, using chemosynthesis instead of photosynthesis for primary production. • Underground life is relatively well protected from hazardous ionizing cosmic radiation, so above mentioned discoveries reopen the habitability budget of the Milky Way, turning potentially habitable even planetary bodies without atmosphere. • Considering this, in this work the habitability potential of the Milky Way is reconsidered. Energy Sources for Primary Habitability: - Photosynthesis: Electromagnetic Waves, mostly in the range 400-700 nm. Dominant in planetary surface. - Chemosynthesis: Energy released by redox chemical reactions. Dominant in deep sea and crust. Circumstellar Habitable Zone https://en.wikipedia.org/wiki/Circumstellar_habitable_zone. Accessed on 2017.04.28 Liquid water at surface: biased towards surface (photosynthetic) life Chemosynthesis: More common than previously thought… - Any redox process giving at least 20 kJ/mol of free energy can support microbial metabolism. The following gives 794 kJ/mol: Pohlman, J.: The biogeochemistry of anchialine caves: -
HI Balmer Jump Temperatures for Extragalactic HII Regions in the CHAOS Galaxies
HI Balmer Jump Temperatures for Extragalactic HII Regions in the CHAOS Galaxies A Senior Thesis Presented in Partial Fulfillment of the Requirements for Graduation with Research Distinction in Astronomy in the Undergraduate Colleges of The Ohio State University By Ness Mayker The Ohio State University April 2019 Project Advisors: Danielle A. Berg, Richard W. Pogge Table of Contents Chapter 1: Introduction ............................... 3 1.1 Measuring Nebular Abundances . 8 1.2 The Balmer Continuum . 13 Chapter 2: Balmer Jump Temperature in the CHAOS galaxies .... 16 2.1 Data . 16 2.1.1 The CHAOS Survey . 16 2.1.2 CHAOS Balmer Jump Sample . 17 2.2 Balmer Jump Temperature Determinations . 20 2.2.1 Balmer Continuum Significance . 20 2.2.2 Balmer Continuum Measurements . 21 + 2.2.3 Te(H ) Calculations . 23 2.2.4 Photoionization Models . 24 2.3 Results . 26 2.3.1 Te Te Relationships . 26 − 2.3.2 Discussion . 28 Chapter 3: Conclusions and Future Work ................... 32 1 Abstract By understanding the observed proportions of the elements found across galaxies astronomers can learn about the evolution of life and the universe. Historically, there have been consistent discrepancies found between the two main methods used to measure gas-phase elemental abundances: collisionally excited lines and optical recombination lines in H II regions (ionized nebulae around young star-forming regions). The origin of the discrepancy is thought to hinge primarily on the strong temperature dependence of the collisionally excited emission lines of metal ions, principally Oxygen, Nitrogen, and Sulfur. This problem is exacerbated by the difficulty of measuring ionic temperatures from these species. -
1.1 Questions Chapter 1
i 1.1 Questions Chapter 1 Question 1.5 Question 1.5 What is H I? And H II and H III? Do these spectra have spectral lines? What is the 21 cm line associated with? Does Fe XII have spectral lines? If so, in which wavelength region? H I = the spectrum of neutral hydrogen (proton + electron). H II = the spectrum of ionized hydrogen (H+, free proton). H III does not exist. H I contains the Lyman-, Balmer-, Paschen-, Pfundt- etc. series, see Figure 1.4 H II does not have spectral lines, there is no bound electron that can do bb transi- tions. The 21 cm line is part of the H I spectrum but is not part of a series of bb transitions of the electron; this transition is a flip of the spin of the electron in the ground state. The energy difference between these two spin states is ∆Espin = 6 × 10−6 eV. Fe XII is the spectrum of Fe11+. This spectrum contains lines because the twelfth, thirteenth electron, etc. still can make bb transitions. These inner-shell electrons are strongly bound, therefore the ∆Emn is large and the spectral lines have short wavelengths. Figure 8.11 shows an example of the emission line of Fe XII at 195 A.˚ Question 1.6 Question 1.6 Compare the observed wavelengths of the Na I D lines in Figure 1.2 and the Lyα line in Figure 1.3 with those of the associated bb transitions in the relevant term diagrams (see Appendix). What is your conclusion? Figure 1.3 shows a large number of spectral lines with λ < 3530 A:˚ the Lyα forest. -
SIDE GROUP ADDITION to the POLYCYCLIC AROMATIC HYDROCARBON CORONENE by PROTON IRRADIATION in COSMIC ICE ANALOGS Max P
The Astrophysical Journal, 582:L25–L29, 2003 January 1 ᭧ 2003. The American Astronomical Society. All rights reserved. Printed in U.S.A. SIDE GROUP ADDITION TO THE POLYCYCLIC AROMATIC HYDROCARBON CORONENE BY PROTON IRRADIATION IN COSMIC ICE ANALOGS Max P. Bernstein,1,2 Marla H. Moore,3 Jamie E. Elsila,4 Scott A. Sandford,2 Louis J. Allamandola,2 and Richard N. Zare4 Received 2002 July 23; accepted 2002 November 5; published 2002 December 6 ABSTRACT ∼ Ices at 15 K consisting of the polycyclic aromatic hydrocarbon coronene (C24H12) condensed either with H2O, CO2, or CO in the ratio of 1 : 100 or greater have been subjected to MeV proton bombardment from a Van de Graaff generator. The resulting reaction products have been examined by infrared transmission- reflection-transmission spectroscopy and by microprobe laser-desorption laser-ionization mass spectrometry. Just as in the case of UV photolysis, oxygen atoms are added to coronene, yielding, in the case of H2O ices, the addition of one or more alcohol (i OH) and ketone (1CuO) side chains to the coronene scaffolding. There are, however, significant differences between the products formed by proton irradiation and the products formed by UV photolysis of coronene containing CO and CO2 ices. The formation of a coronene carboxylic i acid ( COOH) by proton irradiation is facile in solid CO but not in CO2, the reverse of what was previously observed for UV photolysis under otherwise identical conditions. This work presents evidence that cosmic- ray irradiation of interstellar or cometary ices should have contributed to the formation of aromatics bearing ketone and carboxylic acid functional groups in primitive meteorites and interplanetary dust particles. -
NIPPON SHOKUBAI Company Profile
COMPANY PROFILE Osaka Office Kogin Bldg., 4-1-1 Koraibashi, Chuo-ku, Osaka 541-0043, Japan TEL +81-6-6223-9111 FAX +81-6-6201-3716 Tokyo Office Hibiya Dai Bldg., 1-2-2 Uchisaiwai-cho, Chiyoda-ku, Tokyo 100-0011, Japan TEL +81-3-3506-7475 FAX +81-3-3506-7598 https://www.shokubai.co.jp/en/ 2021.6.2000 Nippon Shokubai Group Mission Management Commitment We are deeply dedicated to humanity and the innate human values of sincerity We conduct all of our corporate and honesty. We respect the unique traits and worldview of each individual, embracing diversity and working to promote mutual understanding and trust. activities based upon a deep We recognize that it is the human spirit and point of view that shape our respect for humanity. understanding of management and our actions. A deep respect for humanity is Providing affluence and comfort to people and society, the foundation for all of our corporate activities. with our unique technology We aim at coexisting with We work to create sustainable societies. We believe it is our corporate social society, and working in responsibility to develop positive relationships with all of our stakeholders, as harmony with the environment. well as with the global environment. We pursue technologies We deliver new value that benefits people and society and are dedicated to working as a unified team to develop technology that will open the door to Corporate Credo that will create the future. the future. Safety takes priority over production. By working to expand our business worldwide, we aim to realize our We act on the global stage. -
Cosmic-Ray Soil Water Monitoring: the Development, Status & Potential of the COSMOS- India Network Ross Morrison, J
Cosmic-ray soil water monitoring: the development, status & potential of the COSMOS- India network Ross Morrison, J. G. Evans, S. S. Angadi, L. Ball, T. Chakraborty, H. Cooper, M. Fry, G. Geet, M. Goswami, N. Ganeshi, O. Hitt, S. Jain, M. Krishnan, R. Krishnan, A. Kumar, M. Mujumdar, M. Nema, G. Rees, M. Sekhar, O. Swain, R. Thayyen, S. Tripathi, D. Upadhyaya & A. Jenkins COSMOS-India: outline o Background & rationale o Basics of measurement principle o COSMOS-India network & sites o Selected results o Future work COSMOS-India: objectives o Collaborative development of soil moisture (SM) network in India using cosmic ray (COSMOS) sensors o Deliver high temporal frequency SM observations at the intermediate spatial scale in near real-time o Development of national COSMOS-India data system & near real time data portal o Integrate with Earth Observation datasets for validated SM maps of India o Empower many other applications… Acknowledgment: other COSMOS networks cosmos.hwr.arizona.edu cosmos.ceh.ac.uk Why measure soil moisture (SM)? o Controls exchanges of energy & mass between land surface & atmosphere o Hydrology: controls evapotranspiration, partitioning between runoff & infiltration, groundwater recharge o Meteorology: partitioning solar energy into sensible, latent & soil heat fluxes, surface-boundary layer interactions o Plant growth & soil biogeochemistry https://www2.ucar.edu/atmosnews/people/aiguo-dai https://nevada.usgs.gov/water/et/measured.htm Applications of soil moisture data SM observation techniques o Challenge: SM observations at spatial & temporal resolution relevant Measuringto applications soil (e.g.moisture gridded models, content field scale) o Point scale: high temporal resolution & low cost o Issues - spatial heterogeneity & sensor placement (e.g. -
H2CS) and Its Thiohydroxycarbene Isomer (HCSH
A chemical dynamics study on the gas phase formation of thioformaldehyde (H2CS) and its thiohydroxycarbene isomer (HCSH) Srinivas Doddipatlaa, Chao Hea, Ralf I. Kaisera,1, Yuheng Luoa, Rui Suna,1, Galiya R. Galimovab, Alexander M. Mebelb,1, and Tom J. Millarc,1 aDepartment of Chemistry, University of Hawai’iatManoa, Honolulu, HI 96822; bDepartment of Chemistry and Biochemistry, Florida International University, Miami, FL 33199; and cSchool of Mathematics and Physics, Queen’s University Belfast, Belfast BT7 1NN, Northern Ireland, United Kingdom Edited by Stephen J. Benkovic, The Pennsylvania State University, University Park, PA, and approved August 4, 2020 (received for review March 13, 2020) Complex organosulfur molecules are ubiquitous in interstellar molecular sulfur dioxide (SO2) (21) and sulfur (S8) (22). The second phase clouds, but their fundamental formation mechanisms have remained commences with the formation of the central protostars. Tempera- largely elusive. These processes are of critical importance in initiating a tures increase up to 300 K, and sublimation of the (sulfur-bearing) series of elementary chemical reactions, leading eventually to organo- molecules from the grains takes over (20). The subsequent gas-phase sulfur molecules—among them potential precursors to iron-sulfide chemistry exploits complex reaction networks of ion–molecule and grains and to astrobiologically important molecules, such as the amino neutral–neutral reactions (17) with models postulating that the very acid cysteine. Here, we reveal through laboratory experiments, first sulfur–carbon bonds are formed via reactions involving methyl electronic-structure theory, quasi-classical trajectory studies, and astro- radicals (CH3)andcarbene(CH2) with atomic sulfur (S) leading to chemical modeling that the organosulfur chemistry can be initiated in carbonyl monosulfide and thioformaldehyde, respectively (18). -
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. -
E R U P T I V E S T a R S S P E C T R O S C O
Erupti ve stars spectroscopy Catacl ys mics, Sy mbi otics, Novae, Supernovae ARAS Eruptive Stars Information letter n° 14 #2015‐02 28‐02‐2015 Observations of February 2015 Contents News Two novae discovered in february Novae p. 2‐8 Nova Sco 2015 = PNV J17032620‐3504140 Nova Cyg 2014 Nova Cen 2013 Ungoing observations 2015 February 11.837 UT at mag 8.1 Nova Del 2013 rsising in the morning sky by Tadashi Kojima Nova Sco 2015 Nova Sgr 2015 Spectra obtained by C. Buil Nova Sgr 2015 = PNV J18142514‐2554343 Symbiotics p. 9‐22 2015 February 12.840 at mag 11.2 by Hideo Nishimura, Survey of V694 Mon Koichi Nishiyama CH Cygni campaign : fisrt spectrum of the new season the 1th of and Fujio Kabashima march ( see next issue) Cataclysmics p. 23‐27 SS Aur in outburst : a complete coverage of the outburst in February by P. Somgogyi and J. Guarro U Gem outburst late February Notes from Steve shore : p. 28‐31 Recent publications about eruptive stars p. 32‐34 ARAS Spectroscopy Extra : Cat’s eye nebula spectroscopy, 150 years after Huggins, ARAS Web page by Olivier Thizy http://www.astrosurf.com/aras/ p. 35 ‐ 47 ARAS Forum http://www.spectro‐aras.com/forum/ ARAS list https://groups.yahoo.com/neo/groups/sp Acknowledgements : ectro‐l/info V band light curves from AAVSO photometric data base ARAS preliminary data base http://www.astrosurf.com/aras/Aras_Data Authors : Base/DataBase.htm F. Teyssier, S. Shore, A. Skopal, P. Somogyi, D. Boyd, J. Edlin, J. Guarro, ARAS BeAM Franck Boubault http://arasbeam.free.fr/?lang=en ARAS Eruptive Stars Information Letter -
Phosphine Safety Data Sheet (180KB)
Phosphine Safety Data Sheet P-4643 This SDS conforms to U.S. Code of Federal Regulations 29 CFR 1910.1200, Hazard Communication. Date of issue: 01/01/1980 Revision date: 08/31/2018 Supersedes: 10/24/2016 SECTION: 1. Product and company identification 1.1. Product identifier Product form : Substance Substance name : Phosphine CAS-No. : 7803-51-2 Formula : PH3 Other means of identification : Hydrogen phosphide, Phosphorous hydride, Phosphorous trihydride, Phosphorated hydrogen 1.2. Relevant identified uses of the substance or mixture and uses advised against Use of the substance/mixture : Industrial use; Use as directed. 1.3. Details of the supplier of the safety data sheet Praxair, Inc. 10 Riverview Drive Danbury, CT 06810-6268 - USA T 1-800-772-9247 (1-800-PRAXAIR) - F 1-716-879-2146 www.praxair.com 1.4. Emergency telephone number Emergency number : Onsite Emergency: 1-800-645-4633 CHEMTREC, 24hr/day 7days/week — Within USA: 1-800-424-9300, Outside USA: 001-703-527-3887 (collect calls accepted, Contract 17729) SECTION 2: Hazard identification 2.1. Classification of the substance or mixture GHS-US classification Pyr. Gas H250 Flam. Gas 1 H220 Press. Gas (Liq.) H280 Acute Tox. 1 (Inhalation:gas) H330 Skin Corr. 1B H314 Eye Dam. 1 H318 Aquatic Acute 1 H400 2.2. Label elements GHS-US labeling Hazard pictograms (GHS-US) : GHS02 GHS04 GHS05 GHS06 GHS09 Signal word (GHS-US) : Danger Hazard statements (GHS-US) : H220 - EXTREMELY FLAMMABLE GAS H250 - CATCHES FIRE SPONTANEOUSLY IF EXPOSED TO AIR H280 - CONTAINS GAS UNDER PRESSURE; MAY EXPLODE IF HEATED H314 - Causes severe skin burns and eye damage H330 - FATAL IF INHALED H400 - VERY TOXIC TO AQUATIC LIFE CGA-HG04 - MAY FORM EXPLOSIVE MIXTURES WITH AIR CGA-HG11 - SYMPTOMS MAY BE DELAYED Precautionary statements (GHS-US) : P202 - Do not handle until all safety precautions have been read and understood. -
Ijmp.Jor.Br V
INDEPENDENT JOURNAL OF MANAGEMENT & PRODUCTION (IJM&P) http://www.ijmp.jor.br v. 10, n. 8, Special Edition Seng 2019 ISSN: 2236-269X DOI: 10.14807/ijmp.v10i8.1046 A NEW HYPOTHESIS ABOUT THE NUCLEAR HYDROGEN STRUCTURE Relly Victoria Virgil Petrescu IFToMM, Romania E-mail: [email protected] Raffaella Aversa University of Naples, Italy E-mail: [email protected] Antonio Apicella University of Naples, Italy E-mail: [email protected] Taher M. Abu-Lebdeh North Carolina A and T State Univesity, United States E-mail: [email protected] Florian Ion Tiberiu Petrescu IFToMM, Romania E-mail: [email protected] Submission: 5/3/2019 Accept: 5/20/2019 ABSTRACT In other papers already presented on the structure and dimensions of elemental hydrogen, the elementary particle dynamics was taken into account in order to be able to determine the size of the hydrogen. This new work, one comes back with a new dynamic hypothesis designed to fundamentally change again the dynamic particle size due to the impulse influence of the particle. Until now it has been assumed that the impulse of an elementary particle is equal to the mass of the particle multiplied by its velocity, but in reality, the impulse definition is different, which is derived from the translational kinetic energy in a rapport of its velocity. This produces an additional condensation of matter in its elemental form. Keywords: Particle structure; Impulse; Condensed matter. [http://creativecommons.org/licenses/by/3.0/us/] Licensed under a Creative Commons Attribution 3.0 United States License 1749 INDEPENDENT JOURNAL OF MANAGEMENT & PRODUCTION (IJM&P) http://www.ijmp.jor.br v.