Metallofullerene and Fullerene Formation from Condensing Carbon Gas Under Conditions of Stellar Outflows and Implication to Stardust

Total Page:16

File Type:pdf, Size:1020Kb

Metallofullerene and Fullerene Formation from Condensing Carbon Gas Under Conditions of Stellar Outflows and Implication to Stardust Metallofullerene and fullerene formation from condensing carbon gas under conditions of stellar outflows and implication to stardust Paul W. Dunka,b,1, Jean-Joseph Adjizianc, Nathan K. Kaiserb, John P. Quinnb, Gregory T. Blakneyb, Christopher P. Ewelsc,1, Alan G. Marshalla,b,1, and Harold W. Krotoa,1 aDepartment of Chemistry and Biochemistry, Florida State University, Tallahassee, FL 32306; bIon Cyclotron Resonance Program, National High Magnetic Field Laboratory, Florida State University, Tallahassee, FL 32310; and cInstitut des Matériaux Jean Rouxel, Centre National de la Recherche Scientifique, Unité Mixte de Recherche 6502, Université de Nantes, BP 32229 Nantes, France Contributed by Harold W. Kroto, August 29, 2013 (sent for review June 13, 2013) Carbonaceous presolar grains of supernovae origin have long confirmed to exist in circumstellar and interstellar environments. been isolated and are determined to be the carrier of anomalous C60 and C70 were first unequivocally detected in a planetary 22Ne in ancient meteorites. That exotic 22Ne is, in fact, the decay nebula in 2010, which was thought to be hydrogen deficient (11). isotope of relatively short-lived 22Na formed by explosive nucleo- Thereafter, Buckminsterfullerene was detected in hydrogen- synthesis, and therefore, a selective and rapid Na physical trapping rich [including the least H-deficient R Coronae Borealis stars] mechanism must take place during carbon condensation in super- (12, 13) and oxygen-rich environments (14), as well as the ISM nova ejecta. Elucidation of the processes that trap Na and produce (15) and a protoplanetary nebula (16). Moreover, fullerenes large carbon molecules should yield insight into carbon stardust have been detected in a host of other circumstellar and in- enrichment and formation. Herein, we demonstrate that Na effec- terstellar sources, with new reports of cosmic fullerene de- tection constantly emerging. tively nucleates formation of Na@C60 and other metallofullerenes during carbon condensation under highly energetic conditions in Fullerenes have recently been experimentally shown to self- assemble in condensing carbon through a closed network growth oxygen- and hydrogen-rich environments. Thus, fundamental car- ASTRONOMY (CNG) mechanism (17, 18), in which small fullerenes form ini- bon chemistry that leads to trapping of Na is revealed, and should tially and then progress into larger species, such as C60, by in- be directly applicable to gas-phase chemistry involving stellar envi- corporation of atomic and diatomic carbon into growing cages. ronments, such as supernova ejecta. The results indicate that, in That process resolves how fullerenes form spontaneously under addition to empty fullerenes, metallofullerenes should be constit- highly energetic conditions from carbon vapor, as well as how uents of stellar/circumstellar and interstellar space. In addition, C60 forms as the most abundant species. The CNG mechanism gas-phase reactions of fullerenes with polycyclic aromatic hydro- for fullerene formation should occur in condensing carbon vapor carbons are investigated to probe “build-up” and formation of of stellar ejecta; although, formation by photochemical pro- carbon stardust, and provide insight into fullerene astrochemistry. cessing of existing carbonaceous materials, such as hydrogenated amorphous carbon (HACs), polycyclic aromatic hydrocarbons ne of the most profound findings in cosmochemistry has (PAHs), or PAH-like structures, could also be important for- Obeen the isolation and study of presolar grains recovered mation routes (12, 19, 20). Indeed, such photochemical pro- from carbonaceous chondrites, which are ancient meteorites (1– cessing could work in tandem with CNG formation to produce 3). A particularly striking example is the micrometer-sized low- density graphite grains of supernovae origin (1, 4). This discovery Significance was due to identification of noble gas isotopic anomalies iden- tified by mass spectrometry; upon stepwise heating of bulk samples We experimentally study the processes that result in fullerene 22 of carbonaceous chondrite, highly enriched Ne is released (3, 4). formation in oxygen- and hydrogen-rich carbon gas. Metal- 22 That observation led to the possibility that exotic Ne was a decay lofullerenes are found to form as readily as empty cages and 22 product of the extinct nuclide Na, produced from a supernova thus, like fullerenes, should be important constituents of (cir- 22 explosion (5). Subsequently, Ne was used as a guide to pinpoint cum)stellar/interstellar space. Element trapping by metal- the tiny carbonaceous grains embedded within the bulk meteorite, lofullerene formation is shown to be selective and rapid, which and the supernovae origin was further confirmed by other isotopic can explain long-standing astrophysical puzzles such as the “cosmic fingerprints” (2–4). Thus, these particular carbonaceous anomalous element enrichment of stardust. Infrared spectro- grains represent a direct chemical sample from a supernova. scopic signatures are simulated to provide an observational Despite many detailed experiments on presolar carbonaceous test for metallofullerenes in space. Further, energetic reactions 22 grains, the mechanism whereby Na is selectively trapped to between larger polycyclic aromatic hydrocarbons (PAHs) and enrich stardust remains a puzzle. The carbon chemistry of su- fullerenes are established form stable classes of complex mol- pernova ejecta, in part, determines the composition of carbon ecules that hold high astrochemical importance. Bottom-up stardust. Supernovae-originating dust is ejected into the in- fullerene growth is also demonstrated to result from PAH terstellar medium (ISM), directly impacting interstellar chemis- processing, another potentially important extraterrestrial for- try and subsequent stellar evolution. Furthermore, dust is mation mechanism. ubiquitous in the universe, and recent observational studies – suggest that supernovae are major dust contributors (6 8). Author contributions: P.W.D., C.P.E., A.G.M., and H.W.K. designed research; P.W.D. and Therefore, study of the gas-phase chemical processes that can J.-J.A. performed research; N.K.K., J.P.Q., and G.T.B. contributed new reagents/analytic operate under conditions of stellar outflows should provide in- tools; P.W.D., J.-J.A., C.P.E., A.G.M., and H.W.K. analyzed data; and P.W.D., J.-J.A., C.P.E., sight into a broad range of phenomena, including stellar and A.G.M., and H.W.K. wrote the paper. interstellar chemistry, distribution of carbon in the universe, and The authors declare no conflict of interest. supernova mixing. 1To whom correspondence may be addressed. E-mail: [email protected], chris.ewels@ Fullerenes have been principal astronomic molecular targets cnrs-imn.fr, [email protected], or [email protected]. since the discovery of Buckminsterfullerene, C60 (9, 10). The This article contains supporting information online at www.pnas.org/lookup/suppl/doi:10. closed-caged molecules, however, have only recently been 1073/pnas.1315928110/-/DCSupplemental. www.pnas.org/cgi/doi/10.1073/pnas.1315928110 PNAS Early Edition | 1of6 Downloaded by guest on September 29, 2021 C60 and other larger fullerenes in lower-energy conditions, out- spectrometer provides ultrahigh resolution and high mass accu- side of stellar environments. We note that because energetic racy, and overcomes that experimental challenge (22, 25). barriers are low or nonexistent for incorporation of C and C2 To probe the ability of Na to nucleate metallofullerene for- into closed cages and carbon catalyzed bond rearrangements mation in carbon plasma, a Na-doped carbon rod (1.0 atom % − (17), CNG formation should also be possible in circumstellar Na) was subjected to laser ablation (∼35 mJ∙cm 2 fluence or environments, such as planetary nebula. 5 mJ per pulse) under a 10-psi He flow. Because 22Na is not Many investigations into the astronomical origin of these hol- available for experimental study, 23Na is used. Both isotopes low caged molecules are currently under way. By contrast, little exhibit the same essential chemical reactivity and kinetics, and consideration has been given to endohedral metallofullerenes, thus 23Na can be used to accurately elucidate interaction of 22Na which are cages that encapsulate metals and other elements, as with carbon plasma. Fig. 1 shows the cluster cations generated relevant astrochemical species. Understanding how large carbon under conditions that yield empty-caged fullerenes. The empty- molecules can form in the hostile environments of stellar out- caged species are observed, as expected, but an entire family of flows is a central issue that should offer valuable information on carbon clusters containing a single Na atom is also present. the origin and cosmic role of fullerenes. Critical insight into Na@C60 forms as the most abundant species, followed by Na@C70. that problem can be achieved by study of the key processes All Na@C2n are unequivocally resolved from the “overlapping” and resulting molecular products formed through carbon con- empty cages. For example, as shown in Fig. 1, Na@C60 is clearly densation reactions in high-energy oxygen- and hydrogen-rich resolved from empty cage C62,definitively showing that Na@C60 environments. spontaneously forms in condensing carbon. Fragmentation ex- Herein, we explore carbon condensation and interaction with periments unambiguously confirm that Na@C60 and all other Na under highly energetic conditions by use of a pulsed super- Na@C2n cluster
Recommended publications
  • Minutes of the IUPAC Chemical Nomenclature and Structure Representation Division (VIII) Committee Meeting Boston, MA, USA, August 18, 2002
    Minutes of the IUPAC Chemical Nomenclature and Structure Representation Division (VIII) Committee Meeting Boston, MA, USA, August 18, 2002 Members Present: Dr Stephen Heller, Prof Herbert Kaesz, Prof Dr Alexander Lawson, Prof G. Jeffrey Leigh, Dr Alan McNaught (President), Dr. Gerard Moss, Prof Bruce Novak, Dr Warren Powell (Secretary), Dr William Town, Dr Antony Williams Members Absent: Dr. Michael Dennis, Prof Michael Hess National representatives Present: Prof Roberto de Barros Faria (Brazil) The second meeting of the Division Committee of the IUPAC Division of Chemical Nomenclature and Structure Representation held in the Great Republic Room of the Westin Hotel in Boston, Massachusetts, USA was convened by President Alan McNaught at 9:00 a.m. on Sunday, August 18, 2002. 1.0 President McNaught welcomed the members to this meeting in Boston and offered a special welcome to the National Representative from Brazil, Prof Roberto de Barros Faria. He also noted that Dr Michael Dennis and Prof Michael Hess were unable to be with us. Each of the attendees introduced himself and provided a brief bit of background information. Housekeeping details regarding breaks and lunch were announced and an invitation to a reception from the U. S. National Committee for IUPAC on Tuesday, August 20 was noted. 2.0 The agenda as circulated was approved with the addition of a report from Dr Moss on the activity on his website. 3.0 The minutes of the Division Committee Meeting in Cambridge, UK, January 25, 2002 as posted on the Webboard (http://www.rsc.org/IUPAC8/attachments/MinutesDivCommJan2002.rtf and http://www.rsc.org/IUPAC8/attachments/MinutesDivCommJan2002.pdf) were approved with the following corrections: 3.1 The name Dr Gerard Moss should be added to the members present listing.
    [Show full text]
  • Polycyclic Aromatic Hydrocarbon Structure Index
    NIST Special Publication 922 Polycyclic Aromatic Hydrocarbon Structure Index Lane C. Sander and Stephen A. Wise Chemical Science and Technology Laboratory National Institute of Standards and Technology Gaithersburg, MD 20899-0001 December 1997 revised August 2020 U.S. Department of Commerce William M. Daley, Secretary Technology Administration Gary R. Bachula, Acting Under Secretary for Technology National Institute of Standards and Technology Raymond G. Kammer, Director Polycyclic Aromatic Hydrocarbon Structure Index Lane C. Sander and Stephen A. Wise Chemical Science and Technology Laboratory National Institute of Standards and Technology Gaithersburg, MD 20899 This tabulation is presented as an aid in the identification of the chemical structures of polycyclic aromatic hydrocarbons (PAHs). The Structure Index consists of two parts: (1) a cross index of named PAHs listed in alphabetical order, and (2) chemical structures including ring numbering, name(s), Chemical Abstract Service (CAS) Registry numbers, chemical formulas, molecular weights, and length-to-breadth ratios (L/B) and shape descriptors of PAHs listed in order of increasing molecular weight. Where possible, synonyms (including those employing alternate and/or obsolete naming conventions) have been included. Synonyms used in the Structure Index were compiled from a variety of sources including “Polynuclear Aromatic Hydrocarbons Nomenclature Guide,” by Loening, et al. [1], “Analytical Chemistry of Polycyclic Aromatic Compounds,” by Lee et al. [2], “Calculated Molecular Properties of Polycyclic Aromatic Hydrocarbons,” by Hites and Simonsick [3], “Handbook of Polycyclic Hydrocarbons,” by J. R. Dias [4], “The Ring Index,” by Patterson and Capell [5], “CAS 12th Collective Index,” [6] and “Aldrich Structure Index” [7]. In this publication the IUPAC preferred name is shown in large or bold type.
    [Show full text]
  • Temperature-Induced Oligomerization of Polycyclic Aromatic Hydrocarbons
    www.nature.com/scientificreports OPEN Temperature-induced oligomerization of polycyclic aromatic hydrocarbons at ambient Received: 7 June 2017 Accepted: 10 July 2017 and high pressures Published: xx xx xxxx Artem D. Chanyshev 1,2, Konstantin D. Litasov1,2, Yoshihiro Furukawa3, Konstantin A. Kokh1,2 & Anton F. Shatskiy1,2 Temperature-induced oligomerization of polycyclic aromatic hydrocarbons (PAHs) was found at 500–773 K and ambient and high (3.5 GPa) pressures. The most intensive oligomerization at 1 bar and 3.5 GPa occurs at 740–823 K. PAH carbonization at high pressure is the fnal stage of oligomerization and occurs as a result of sequential oligomerization and polymerization of the starting material, caused by overlapping of π-orbitals, a decrease of intermolecular distances, and fnally the dehydrogenation and polycondensation of benzene rings. Being important for building blocks of life, PAHs and their oligomers can be formed in the interior of the terrestrial planets with radii less than 2270 km. High-pressure transformations of polycyclic aromatic hydrocarbons (PAHs) and benzene become extremely important due to wide applications for example in graphene- and graphene-based nanotechnology1–3, synthesis of organic superconductors4, 5, petroleum geoscience, origin of organic molecules in Universe and origin of life. In particular, PAHs were found in many space objects: meteorites6–8, cometary comae9, interstellar clouds and planetary nebulas10–12. Although the prevalent hypothesis for the formation of these PAHs is irradiation-driven polymerization of smaller hydrocarbons13, alternative explanation could be shock fragmentation of carbonaceous solid material11. PAH-bearing carbonaceous material could contribute to the delivery of extraterrestrial organic materials to the prebiotic Earth during the period of heavy bombardment of the inner Solar System from 4.5 to 3.8 Ga ago14–16.
    [Show full text]
  • Nanostructural Origin of Blue Fluorescence in the Mineral Karpatite
    Potticary, J. , Jensen, T. T., & Hall, S. R. (2017). Nanostructural origin of blue fluorescence in the mineral karpatite. Scientific Reports, 7(1), [9867]. https://doi.org/10.1038/s41598-017-10261-w Publisher's PDF, also known as Version of record License (if available): CC BY Link to published version (if available): 10.1038/s41598-017-10261-w Link to publication record in Explore Bristol Research PDF-document This is the final published version of the article (version of record). It first appeared online via Nature at https://www.nature.com/articles/s41598-017-10261-w. Please refer to any applicable terms of use of the publisher. University of Bristol - Explore Bristol Research General rights This document is made available in accordance with publisher policies. Please cite only the published version using the reference above. Full terms of use are available: http://www.bristol.ac.uk/red/research-policy/pure/user-guides/ebr-terms/ www.nature.com/scientificreports OPEN Nanostructural origin of blue fuorescence in the mineral karpatite Received: 9 June 2017 Jason Potticary 1,2, Torsten T. Jensen 1,3 & Simon R. Hall1 Accepted: 7 August 2017 The colour of crystals is a function of their atomic structure. In the case of organic crystals, it is the Published: xx xx xxxx spatial relationships between molecules that determine the colour, so the same molecules in the same arrangement should produce crystals of the same colour, regardless of whether they arise geologically or synthetically. There is a naturally-occurring organic crystal known as karpatite which is prized for its beautiful blue fuorescence under ultra-violet illumination.
    [Show full text]
  • Fluoranthene
    ) , "- United States Office of Water EPA 440/5-80-049 Environmental Protection Regulations and Standards October 1980 Agency Criteria and Standards Division Washington DC 20460 aEPA Ambient Water Quality Criteria for Fluoranthene ... AMBIENT WATER QUALITY CRITERIA FOR FLUORANTHENE Prepared By U.S. ENVIRONMENTAL PROTECTION AGENCY Office of Water Regulations and Standards Criteria and Standards Division Washington, D.C. Office of Research and Development Environmental Criteria and Assessment Office Cincinnati, Ohio Carcinogen Assessment Group Washington, D.C. Environmental Research Laboratories Corvalis, Oregon Duluth, Minnesota Gulf Breeze, Florida Narragansett, Rhode Island - -J i DISCLAIMER This report has been reviewed by the Environmental Criteria and Assessment Office, U.S. Environmental Protection Agency, and approved for publication. Mention of trade names or commercial products does not constitute endorsement or recommendation for use. AVAILABILITY NOTICE This document is available to the public through the National Technical Information Service, (NTIS), Springfield, Virginia 22161. ii FOREWORD Section 304 (a) (1) of the Clean Water Act of 1977 (P.L. 95-217), requires the Administrator of the Environmental Protection Agency to publish criteria for water quality accurately reflecting the latest scientific knowledge on the kind and extent of all identifiable effects on health and we 1fare wh ich may be expected from the presence of pollutants in any body of water, including ground water. Proposed water quality criteria for the 65 toxic pollutants listed under section 307 (a) (1) of the Cl ean Water Act were deve loped and a not ice of their availability was published for public comment on March 15, 1979 (44 FR 15926), July 25, 1979 (44 FR 43660), and October 1, 1979 (44 FR 56628).
    [Show full text]
  • Measurements of Polycyclic Aromatic Hydrocarbons and Genotoxicity in Soot Deposited at a Toll Plaza Near Durban, South Africa
    RESEARCH ARTICLE S.J. Godefroy, B.S. Martincigh and L.F. Salter, 61 S. Afr. J. Chem., 2005, 58, 61–66, <http://journals.sabinet.co.za/sajchem/>. Measurements of Polycyclic Aromatic Hydrocarbons and Genotoxicity in Soot Deposited at a Toll Plaza near Durban, South Africa Susan J. Godefroy, Bice S. Martincigh* and Leo F. Salter‡ School of Chemistry, University of KwaZulu-Natal, Howard College Campus, Durban, 4041 South Africa. Received 18 October 2004; revised and accepted 30 March 2005 ABSTRACT This research was designed to examine the presence of polycyclic aromatic hydrocarbons (PAHs) in soot deposited at the Mariannhill toll plaza situated on the N3 highway in KwaZulu-Natal, South Africa. Samples were collected from the toll plaza either by scraping the toll booth walls and surrounding areas, or by wiping the surfaces with cotton wool swabs. The organic component was separated by ultrasonic extraction into dichloromethane and analysed for PAHs by reverse phase high performance liquid chromatography with both fluorescence and ultraviolet detection. The genotoxicity was investigated by means of two bacterial assays: the Ames test and the SOS Chromotest. A number of PAHs were identified and genotoxic activity was observed in both of the assays. KEYWORDS Polycyclic aromatic hydrocarbons, toll plaza, genotoxicity. 1. Introduction mutagenicity.8–10 Since a toll plaza is an area of high traffic Polycyclic aromatic hydrocarbons (PAHs) are ubiquitous density, it is an ideal location for an investigation into the environmental pollutants that are of health concern because of build-up of particles emitted by vehicles, and for a study of the their mutagenic and carcinogenic properties.
    [Show full text]
  • From the Picacho Peak Area, San Benito County, California: Evidences for the Hydrothermal Formation
    American Mineralogist, Volume 92, pages 1262–1269, 2007 Crystal-chemical and carbon-isotopic characteristics of karpatite (C24H12) from the Picacho Peak Area, San Benito County, California: Evidences for the hydrothermal formation TAKUYA ECHIGO,1,* MITSUYOSHI KIMATA,1 AND TERUYUKI MARUOKA2 1Earth Evolution Sciences, Life and Environmental Sciences, University of Tsukuba, Tennoudai 1-1-1, Tsukuba 305-8572, Japan 2Integrative Environmental Sciences, Life and Environmental Sciences, University of Tsukuba, Tennoudai 1-1-1, Tsukuba 305-8572, Japan ABSTRACT Karpatite from the Picacho Peak Area, San Benito County, California, has been characterized as an exceptionally pure crystal of coronene (C24H12) by infrared absorption analysis, Raman scattering analysis, and differential thermal analysis. Furthermore, the crystal structure of karpatite was deter- mined using a single-crystal X-ray diffraction method for the Þ rst time. The mineral crystallizes in the monoclinic system, space group P21/a, with unit-cell dimensions of a = 16.094(9), b = 4.690(3), c = 10.049(8) Å, β = 110.79(2)°, V = 709.9(8) Å3, and Z = 2. The structure was solved and Þ nally reÞ ned to R1 = 3.44% and wR2 = 2.65%, respectively. The coronene molecules in the crystal structure of karpatite are all isolated and the intermolecular distances correspond to van der Waals interactions. The coronene molecules have the high degree of aromaticity and no overcrowded hydrogen atoms, both of which avoid a mixing of other polycyclic aromatic hydrocarbons (PAHs) in karpatite. The corrugated arrangement of coronene molecules constituting karpatite prevents intercalation reactions, accounting for the exceptional purity of this mineral. The isotopic composition of carbon was measured, using an elemental analyzer-isotopic ratio mass spectrometer (EA/IRMS).
    [Show full text]
  • Identification of Polycyclic Aromatic Hydrocarbons in the Supercritical
    Louisiana State University LSU Digital Commons LSU Doctoral Dissertations Graduate School 2008 Identification of Polycyclic Aromatic Hydrocarbons in the Supercritical Pyrolysis Products of Synthetic Jet Fuel S-8 and Methylcyclohexane Jorge Oswaldo Ona Ruales Louisiana State University and Agricultural and Mechanical College, [email protected] Follow this and additional works at: https://digitalcommons.lsu.edu/gradschool_dissertations Part of the Chemical Engineering Commons Recommended Citation Ona Ruales, Jorge Oswaldo, "Identification of Polycyclic Aromatic Hydrocarbons in the Supercritical Pyrolysis Products of Synthetic Jet Fuel S-8 and Methylcyclohexane" (2008). LSU Doctoral Dissertations. 2092. https://digitalcommons.lsu.edu/gradschool_dissertations/2092 This Dissertation is brought to you for free and open access by the Graduate School at LSU Digital Commons. It has been accepted for inclusion in LSU Doctoral Dissertations by an authorized graduate school editor of LSU Digital Commons. For more information, please [email protected]. IDENTIFICATION OF POLYCYCLIC AROMATIC HYDROCARBONS IN THE SUPERCRITICAL PYROLYSIS PRODUCTS OF SYNTHETIC JET FUEL S-8 AND METHYLCYCLOHEXANE A Dissertation Submitted to the Graduate Faculty of the Louisiana State University and Agricultural and Mechanical College in partial fulfillment of the requirements for the degree of Doctor of Philosophy in The Department of Chemical Engineering by Jorge Oswaldo Oña Ruales Ingeniero Quimico, Universidad Central del Ecuador – Quito, 2000 May, 2008 ACKNOWLEDGEMENTS I would like to thank the following: My advisor, Prof. Mary Julia Wornat, for her wise guidance during the last six years, for introduce me to the world of polycyclic aromatic hydrocarbons, and for showing me how to transform my observations into words and the words into scientific papers.
    [Show full text]
  • PAH Volatilization Following Application of Coal-Tar-Based Pavement Sealant
    Atmospheric Environment 51 (2012) 108e115 Contents lists available at SciVerse ScienceDirect Atmospheric Environment journal homepage: www.elsevier.com/locate/atmosenv PAH volatilization following application of coal-tar-based pavement sealant Peter C. Van Metre a,*, Michael S. Majewski b, Barbara J. Mahler a, William T. Foreman c, Christopher L. Braun a, Jennifer T. Wilson a, Teresa L. Burbank c a U.S. Geological Survey, 1505 Ferguson Lane, Austin, TX, United States b U.S. Geological Survey, Sacramento, CA, United States c U.S. Geological Survey, Denver, CO, United States article info abstract Article history: Coal-tar-based pavement sealants, a major source of PAHs to urban water bodies, have recently been Received 12 November 2011 identified as a source of volatile PAHs to the atmosphere. We tracked the volatilization of PAHs for 1 year Received in revised form after application of a coal-tar-based pavement sealant by measuring gas-phase PAH concentrations above 13 January 2012 the pavement surface and solid-phase PAH concentrations in sealant scraped from the surface. Gas-phase Accepted 16 January 2012 concentrations at two heights (0.03 and 1.28 m) and wind speed were used to estimate volatilization flux. The sum of the concentrations of eight frequently detected PAHs (SPAH8) in the 0.03-m sample 1.6 h Keywords: À after application (297,000 ng m 3) was about 5000 times greater than that previously reported for the PAHs À3 Emissions same height above unsealed parking lots (66 ng m ). Flux at 1.6 h after application was estimated at m À2 À1 m À2 À1 Atmosphere 45,000 gm h and decreased rapidly during the 45 days after application to 160 gm h .
    [Show full text]
  • Complex Polycyclic Aromatic Hydrocarbons from Coal Tar on Agilent J&W Select PAH
    Complex polycyclic aromatic hydrocarbons from coal tar on Agilent J&W Select PAH Application Note Author Introduction John Oostdijk Coal tar is a brown or black liquid of high viscosity, which smells of naphthalene Agilent Technologies, Inc. and aromatic hydrocarbons and is obtained from the destructive distillation of coal. Formerly, coal tar was obtained as a by-product in manufacturing coal gas. It is now produced in making coke for steel making. The crude tar contains a large number of organic compounds, such as benzene, naphthalene, methylbenzene and phenols, which can be obtained by distillation. The residue is pitch. At one time coal tar was the major source of organic chemicals, most of which are now derived from petroleum and natural gas. Coal tar pitch is mainly used as a binding agent in the production of carbon electrodes, anodes and Søderberg electrodes, for example, by the aluminium industry. It is also used as a binding agent for refractories, clay pigeons, active carbon, coal briquetting, road construction and roofing. Furthermore, small quantities are used for heavy-duty corrosion protection. The standard coal tar reference material (SRM 1597a, NIST) is a natural, combustion-related mixture of polycyclic aromatic hydrocarbons (PAHs), isolated from a medium crude coke-oven tar and dissolved in toluene. However, PAHs can be difficult to analyze because some of them have the same mass. This makes their separation with GC/MS problematic, and so column selectivity and an optimized oven program are necessary to resolve these PAHs. In this application note, a coal tar sample was analyzed using an optimized oven program for the Select PAH column.
    [Show full text]
  • Polycyclic Aromatic Hydrocarbons and Associated Occupational Exposures Charles William Jameson
    part 1 . PART 1 concordance between cancer in humans and in experimental CHAPTER 7 animals chapter 7. Polycyclic aromatic hydrocarbons and associated occupational exposures Charles William Jameson Properties of PAHs this makes them more readily uptake or degradation, which means available for biological uptake and that their persistence in the environ- Most polycyclic aromatic hydrocar- degradation (Mackay and Callcott, ment is increased (Johnsen et al., bons (PAHs) with potential biolog- 1998; Choi et al., 2010). Furthermore, 2005; Haritash and Kaushik, 2009). ical activity have been determined two- to four-ring PAHs volatilize The properties that influence the to have a molecular structure that sufficiently to appear in the atmo- biological activity of PAHs include ranges in size from two to six fused sphere predominantly in gaseous their vapour pressure, their adsorp- aromatic rings (IARC, 2010). The form, although the physical state of tion on surfaces of solid carrier par- physicochemical properties of four-ring PAHs can depend on tem- ticles, their absorption into liquid these PAHs that are critical to their perature (Atkinson and Arey, 1994; carriers, their lipid–water partition biological activity vary greatly, be- Srogi, 2007). coefficient in tissues, and their limits cause their molecular weights cover In contrast, PAHs with five or of solubility in the lipid and aqueous a vast range. more rings have low solubility in wa- phases of tissues. These properties Aqueous solubility of PAHs de- ter and low volatility. They therefore are linked with the metabolic activa- creases approximately logarith- occur predominantly in solid form, tion of PAHs, as well as their deposi- mically with increasing molecular bound to particulates in polluted air, tion and disposition.
    [Show full text]
  • PAH) in Urban Background Soil
    Examination of the Sources of Polycyclic Aromatic Hydrocarbon (PAH) in Urban Background Soil Examination of the Sources of Polycyclic Aromatic Hydrocarbon (PAH) in Urban Background Soil 1015558 Interim Report, December 2008 EPRI Project Manager J. Lingle ELECTRIC POWER RESEARCH INSTITUTE 3420 Hillview Avenue, Palo Alto, California 94304-1338 ▪ PO Box 10412, Palo Alto, California 94303-0813 ▪ USA 800.313.3774 ▪ 650.855.2121 ▪ [email protected] ▪ www.epri.com DISCLAIMER OF WARRANTIES AND LIMITATION OF LIABILITIES THIS DOCUMENT WAS PREPARED BY THE ORGANIZATION(S) NAMED BELOW AS AN ACCOUNT OF WORK SPONSORED OR COSPONSORED BY THE ELECTRIC POWER RESEARCH INSTITUTE, INC. (EPRI). NEITHER EPRI, ANY MEMBER OF EPRI, ANY COSPONSOR, THE ORGANIZATION(S) BELOW, NOR ANY PERSON ACTING ON BEHALF OF ANY OF THEM: (A) MAKES ANY WARRANTY OR REPRESENTATION WHATSOEVER, EXPRESS OR IMPLIED, (I) WITH RESPECT TO THE USE OF ANY INFORMATION, APPARATUS, METHOD, PROCESS, OR SIMILAR ITEM DISCLOSED IN THIS DOCUMENT, INCLUDING MERCHANTABILITY AND FITNESS FOR A PARTICULAR PURPOSE, OR (II) THAT SUCH USE DOES NOT INFRINGE ON OR INTERFERE WITH PRIVATELY OWNED RIGHTS, INCLUDING ANY PARTY'S INTELLECTUAL PROPERTY, OR (III) THAT THIS DOCUMENT IS SUITABLE TO ANY PARTICULAR USER'S CIRCUMSTANCE; OR (B) ASSUMES RESPONSIBILITY FOR ANY DAMAGES OR OTHER LIABILITY WHATSOEVER (INCLUDING ANY CONSEQUENTIAL DAMAGES, EVEN IF EPRI OR ANY EPRI REPRESENTATIVE HAS BEEN ADVISED OF THE POSSIBILITY OF SUCH DAMAGES) RESULTING FROM YOUR SELECTION OR USE OF THIS DOCUMENT OR ANY INFORMATION, APPARATUS, METHOD, PROCESS, OR SIMILAR ITEM DISCLOSED IN THIS DOCUMENT. ORGANIZATION(S) THAT PREPARED THIS DOCUMENT Meta Environmental NOTE For further information about EPRI, call the EPRI Customer Assistance Center at 800.313.3774 or e-mail [email protected].
    [Show full text]