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14 Title: Coal Review of Hydrocarbon Emissions Related to Tar Pitch
AP42 Section 7.1 Related: 14 Title: Review of Hydrocarbon Emissions Related to Coal Tar Pitch. Includes pitch vapor pressure data and Antoine's coefficients. EF Bart, et al. Allied Chemical Corporation 1980 I ._ ,.. ?i e!,/..'. r'.:.. ,,T.<,ili -:*., $0 ,i .# 1 .... i;.'.,.,: _..:, '">,U<>j. .. .. REVIEW OF HYDROCMSON EMISSIONS RELATED TO COAL TAR PITCH E. F. Bart, S. A. Visnic, P. A. Cerria Allied Chemical Corporation Morristown, New Jersey 07960 Sumnary Coal tar pitch is used primarily as a binder in the manufacture of carbon electrodes for the aluminum and steel industries. The pitch repre- sents the main product from the continuous, high-temperature distillation of coke oven tar. The pitch is produced and generally handled as a liquid at high temperatures, thus resulting in a potential for hydrocarbon emissions during its handling. An ever-increasing need for control of hydrocarbon emissions has resulted for process and storage equipment since amendments were made in 1977 to the Clean Air Act. Within the next several years, most industries will be faced with requirements for the installation of air pollution con- trol equipment. This paper deals with the types of emissions and methods used in quantifying and controlling emissions from coal tar pitch storage equipment. To better understand the nature of coal tar pitch, a brief description is given of its origin, chemistry and physical properties. Coal Tar Distillation Coal tar pitch is the residue from the distillation of coal tar and represents from 30% to 60% of the tar. It is a complex, bituminous sub- stance and has been estimated to contain about 5,000 compounds. -
Organic Data Validation Report Soil Samples Collected June 4,1997 Brodhead Creek, Stroudsburg, Pa
ENVIRONMENTAL RESEARCH AND CONSULTING, INC. 112 COMMONS COURT CHADDS FORD, PA 19317 ORGANIC DATA VALIDATION REPORT SOIL SAMPLES COLLECTED JUNE 4,1997 BRODHEAD CREEK, STROUDSBURG, PA JULY 1997 ACRES INTERNATIONAL CORPORATION 140 John James Audubon Parkway Amherst, New York 14228-1 1 80 AR302871* TABLE OF CONTENTS 1 NARRATIVE ........................................................... 1 2 OVERVIEW ............................................................ 1 3 SUMMARY ........................................................... 1 4 MAJORPROBLEMS .................................................... 1 5 MINOR PROBLEMS .................................................... 2 8 NOTES ......................................................."........ 2 7 REPORT CONTENT .................................................... 2 8 ATTACHMENTS ......".......'.......................................... 3 APPENDICES APPENDIX A - GLOSSARY OF DATA QUALIFIER CODES APPENDIX B - DATA SUMMARY FORMS^ APPENDIX C- RESULTS AS REPORTED BY THE LABORATORY FOR ALL TARGET COMPOUNDS APPENDIX D - REVIEWED AND ACCEPTED TENTATIVELY IDENTIFIED COMPOUNDS APPENDIX E - SUPPORT DOCUMENTATION AR302875 1 NARRATIVE Date: July 28,1997 Subject Organic Data Validation for Sample Delivery Group (SDG) #BRH01 Brodhead Creek • Stroudsburg, Pennsylvania From: James R. Stachowski. Environmental Specialist Acres International Corporation To: Harold M. Brundage III Environmental Research and Consulting, Inc. 2 OVERVIEW This report pertains to data validation of fifteen (15) soil samples from the -
ORGANIC CHEMISTRY- I (Nature of Title Bonding and Stereochemistry) Module No
Subject Chemistry Paper No. and Paper 1: ORGANIC CHEMISTRY- I (Nature of Title Bonding and Stereochemistry) Module No. and Module 8: Aromaticity of fused rings Title Module Tag CHE_P1_M8 CHEMISTRY PAPER 1: ORGANIC CHEMISTRY- I(Nature of Bonding and Stereochemistry) MODULE 8: Aromaticity of fused rings TABLE OF CONTENT 1. Learning Outcomes 2. Introduction 3. Classification of fused ring systems 4. Aromaticity in fused ring systems 4.1. Aromaticity of some benzenoid fused systems 4.1.1. Naphthalene 4.1.2. Anthracene 4.1.3. Phenanthrene 4.1.4. Resonance energy of fused ring systems 4.2. Aromaticity of some non-benzenoid fused systems 4.2.1. Azulenes 4.2.2. Oxaazulenaones 5. Other fused ring systems 5.1. Phenalene 5.2. Benzo cyclobutadiene 5.3. Ferrocene 6. Summary CHEMISTRY PAPER 1: ORGANIC CHEMISTRY- I(Nature of Bonding and Stereochemistry) MODULE 8: Aromaticity of fused rings 1. Learning Outcomes After studying this module, you shall be able to: Learn about the fused rings Understand that how fused rings are classified Learn about the aromaticity of the fused rings Understand aromaticity in the benzenoid and non-benzenoid fused ring systems Learn about some other special cases 2. Introduction As you are already aware that the aromatic compounds apparently contain alternate double and single bonds in a cyclic structure and resemble benzene in chemical behavior. Up till now we have discussed the aromaticity in monocyclic rings. In this module, we shall discuss about the aromaticity of fused rings. So, before starting with the aromaticity of fused rings first we should know what fused rings are. -
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. -
The Study of the Absoiption Spectra of the Hydrocarbons Isolated from the Products of the Action of Alunzinium Chloride on Nup12tkccle.R~E
View Article Online / Journal Homepage / Table of Contents for this issue ABSORPTION SPECTRA OF HYDROCARBONS. 1319 Published on 01 January 1908. Downloaded by University of California - San Diego 12/04/2016 06:21:24. CXXV1.-The Study of the Absoiption Spectra of the Hydrocarbons isolated from the Products of the Action of Alunzinium Chloride on Nup12tkccle.r~e. By ANNIEHOMER, Fellow of Newnham College, and JOHNEDWARD PURVIS, M.A. FROMthe products of the action of aluminium chloride on naphthalene, besides PP-dinaphthyl previously isolated by Friedel and Crafts from the same reaction, there have been isolated three new hydrocarbons which have been described in detail by one of us (Homer, Trans., 1907, 9 1, 1103). The substances isolated were : (.i) CI4Hl6, a homologue of naphthalene, either tetramethyl- or 4s2 View Article Online 1320 HOMER AND PURVIS: THE STUDY OF THE diethyl-naphthalene, more probably the former ; (ii) CZ0Hl4, /3@-dinaphthyl; (iii) c26H22, a substance supposed to be a homologue of dinaphthanthracene, C,,H14 ; and (iv) C40H26, probably tetra- naph t h yl. @B-Dinaphthylis formed by the condensation of two naphthalene molecules. It was thought that the hydrocarbon C,,HZ6 was formed by the condensation of either two PP-dinaphthgl or four naphthalene molecules, more probably by the former, as an increase in the time allowed for the action of aluminium chloride on naphthalene, or a rise in the temperature at which the reaction was conducted, caused a decrease in the amount of the hydrocarbon aad an increase in the amount of the hydrocarbon C,,H,, produced. It was suggested that the substance C261322was a homologue of dinaphthanthracene, CZ2Hl4,and its formation from alkylnaphthalenes, which are also formed during the reaction, was given as follows : The intense fluorescence of the substance suggested the presence of an anthracenoid linking, In the method of formation thus proposed, hydrogen would be eliminated from a /3-methyl group of trimethylnaphthalene. -
Ecological Assessment of a Coastal Shallow Lagoon in Lagos, Nigeria: a Bio-Indicator Approach
March JASEM ISSN 1119-8362 Full-text Available Online at J. Appl. Sci. Environ. Manage. , 2011 All rights reserved www.bioline.org.br/ja Vol. 15 (1) 41 - 46 Ecological assessment of a coastal shallow lagoon in Lagos, Nigeria: A bio-indicator approach *BALOGUN, K J; LADIGBOLU, I A; ARIYO, A A Nigerian Institute for Oceanography and Marine Research, P.M.B. 12729, Victoria Island, Lagos, Nigeria ABSTRACT: Benthic macro-invertebrates of the Northern axis of metropolitan segment of Lagos Lagoon sediments, Nigeria were investigated for six months (April – September, 2010). The study was aimed at using benthic macro-invertebrates to assess the water quality of this part of the Lagoon. A total of ten taxa belonging to three major animal phyla from a total of 2,672 individuals were encountered. The dominant taxa throughout the study and stations were Pachymelania aurita, Aloidis trigona, and Neritina glabrata. Station A (Ikorodu port) had seven taxa, station B (Ibese) had five while stations C (Ofin) and D (Oreta) had eight taxa each. Stations A(Ikorodu port), B(Ibese), C(Ofin) and D(Oreta) accounted for 8.19%, 0.94%, 79.83% and 11.04% respectively in all the individuals collected. Gastropoda was highest and accounted for 54.83% of all individuals collected from all stations contributing 2.58% at station A and 0.49%, 48.39% and 3.37% respectively at stations B, C and D, while Polychaeta had the least (0.97%) with station A, B, C and D constituted 0.82%, 0.04%, 0.04% and 0.07% respectively. Sediment type of the study areas was predominantly muddy sand. -
The Ecology and Natural Food Components of Pachymelania Aurita MÜLLER (Gastropoda: Melaniidae) in a Coastal Lagoon
Report and Opinion. 2009; 1(5) Uwadiae, et al. Ecology and Natural Food of P.aurita The ecology and natural food components of Pachymelania aurita MÜLLER (Gastropoda: Melaniidae) in a Coastal lagoon *Uwadiae RE, *Edokpayi CA and **Egonmwan RI *Department of Marine sciences, University of Lagos, Akoka , Yaba, Lagos, Nigeria. **Department of Zoology, University of Lagos, Akoka , Yaba, Lagos, Nigeria. Email: [email protected]. Tel: +2348063145723 Abstract: The ecology and natural food of Pachymelania aurita MỨLLER in a coastal Nigerian lagoon are reported. Ecological parameters were investigated by monthly sample collection from September, 2004 to August, 2006. Natural food components were identified by microscopic examination of the feacal matter. The abundance of the P. aurita was related to salinity, total organic content (TOC) and grain size of sediment at the study stations. Greater densities of P. aurita occurred at stations with relatively higher salinity (>1.77‰), low TOC (<10%), high sand (>60%) and low mud (<30%) contents. A range of 0.01 – 19.72‰ for water salinity was observed during this study, while sediment sand and mud recorded ranges of 65.8-92.8% and 7.8-29.4% respectively. The TOC of sediment ranged between 2.05 and 98.5%. Sediments at the study stations were predominantly sand intermixed with varied proportions of mud and varied rapidly within relatively short distances along the study stretch. A total of 6,869 individuals were recorded during the study, with wet and dry season contributions of 3,693 and 3,176 individuals respectively. Population of P. aurita was highest (490 individuals) in the month of January, 2005, while the lowest (230 individuals) was recorded in October, 2005. -
Gas Phase Formation of Phenalene Via 10Π-Aromatic, Resonantly Stabilized Free Radical Intermediates
Gas Phase Formation of Phenalene via 10π-Aromatic, Resonantly Stabilized Free Radical Intermediates Long Zhao1, Ralf I. Kaiser1* 1 Department of Chemistry, University of Hawaii at Manoa, Honolulu, Hawaii, 96822 (USA) Wenchao Lu2, Musahid Ahmed2* 2 Chemical Sciences Division, Lawrence Berkeley National Laboratory, Berkeley, CA 94720 (USA) Artem D. Oleinikov 3,4, Valeriy N. Azyazov3,4 3Department of Physics, Samara National Research University, Samara 443086 (Russian Federation) 4Lebedev Physical Institute, Samara 443011 (Russian Federation) Alexander M. Mebel3,5* A. Hasan Howlader,5 Stanislaw F. Wnuk5 5Department of Chemistry and Biochemistry, Florida International University, Miami, FL 33199 (USA) * Corresponding author: Ralf I. Kaiser <[email protected]> Musahid Ahmed <[email protected]> Alexander M. Mebel <[email protected]> 1 Abstract: For the last decades, the Hydrogen-Abstraction/aCetylene-Addition (HACA) mechanism has been fundamental in aiding our understanding of the source of polycyclic aromatic hydrocarbons (PAHs) in combustion processes and in circumstellar envelopes of carbon rich stars. However, the reaction mechanisms driving high temperature molecular mass growth beyond triphenylene (C18H12) along with the link between PAHs and graphene-type nanostructures as identified in carbonaceous meteorites such as in Murchison and Allende has remained elusive. By • exploring the reaction of the 1-naphthyl radical ([C10H7] ) with methylacetylene (CH3CCH) and allene (H2CCCH2) under conditions prevalent in carbon-rich circumstellar environments and combustion systems, we provide compelling evidence on a facile formation of 1H-phenalene (C13H10) – the central molecular building block of graphene-type nanostructures. Beyond PAHs, molecular mass growth processes from 1H-phenalene via ring-annulation through C3 molecular building blocks may ultimately lead to two-dimensional structures such as graphene nano flakes and after condensation of multiple layers to graphitized carbon. -
Gastropod Fauna of the Cameroonian Coasts
Helgol Mar Res (1999) 53:129–140 © Springer-Verlag and AWI 1999 ORIGINAL ARTICLE Klaus Bandel · Thorsten Kowalke Gastropod fauna of the Cameroonian coasts Received: 15 January 1999 / Accepted: 26 July 1999 Abstract Eighteen species of gastropods were encoun- flats become exposed. During high tide, most of the tered living near and within the large coastal swamps, mangrove is flooded up to the point where the influence mangrove forests, intertidal flats and the rocky shore of of salty water ends, and the flora is that of a freshwater the Cameroonian coast of the Atlantic Ocean. These re- regime. present members of the subclasses Neritimorpha, With the influence of brackish water, the number of Caenogastropoda, and Heterostropha. Within the Neriti- individuals of gastropod fauna increases as well as the morpha, representatives of the genera Nerita, Neritina, number of species, and changes in composition occur. and Neritilia could be distinguished by their radula Upstream of Douala harbour and on the flats that lead anatomy and ecology. Within the Caenogastropoda, rep- to the mangrove forest next to Douala airport the beach resentatives of the families Potamididae with Tympano- is covered with much driftwood and rubbish that lies on tonos and Planaxidae with Angiola are characterized by the landward side of the mangrove forest. Here, Me- their early ontogeny and ecology. The Pachymelaniidae lampus liberianus and Neritina rubricata are found as are recognized as an independent group and are intro- well as the Pachymelania fusca variety with granulated duced as a new family within the Cerithioidea. Littorini- sculpture that closely resembles Melanoides tubercu- morpha with Littorina, Assiminea and Potamopyrgus lata in shell shape. -
Drmno Lignite Field (Kostolac Basin, Serbia): Origin and Palaeoenvironmental Implications from Petrological and Organic Geochemi
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Faculty of Chemistry Repository - Cherry J. Serb. Chem. Soc. 77 (8) 1109–1127 (2012) UDC 553.96.:550.86:547(497.11–92) JSCS–4338 Original scientific paper Drmno lignite field (Kostolac Basin, Serbia): origin and palaeoenvironmental implications from petrological and organic geochemical studies KSENIJA STOJANOVIĆ1*#, DRAGANA ŽIVOTIĆ2, ALEKSANDRA ŠAJNOVIĆ3, OLGA CVETKOVIĆ3#, HANS PETER NYTOFT4 and GEORG SCHEEDER5 1University of Belgrade, Faculty of Chemistry, Studentski trg 12–16, 11000 Belgrade, Serbia, 2University of Belgrade, Faculty of Mining and Geology, Djušina 7, 11000 Belgrade, Serbia, 3University of Belgrade, Centre of Chemistry, ICTM, Studentski trg 12–16, 11000 Belgrade; Serbia, 4Geological Survey of Denmark and Greenland, Øster Voldgade 10, DK-1350 Copenhagen, Denmark and 5Federal Institute for Geosciences and Natural Resources, Steveledge 2, 30655 Hanover, Germany (Received 26 November 2011, revised 17 February 2012) Abstract: The objective of the study was to determine the origin and to recon- struct the geological evolution of lignites from the Drmno field (Kostolac Ba- sin, Serbia). For this purpose, petrological and organic geochemical analyses were used. Coal from the Drmno field is typical humic coal. Peat-forming vegetation dominated by decay of resistant gymnosperm (coniferous) plants, followed by prokaryotic organisms and angiosperms. The coal forming plants belonged to the gymnosperm families Taxodiaceae, Podocarpaceae, Cupres- saceae, Araucariaceae, Phyllocladaceae and Pinaceae. Peatification was rea- lised in a neutral to slightly acidic, fresh water environment. Considering that the organic matter of the Drmno lignites was deposited at the same time, in a relatively constant climate, it could be supposed that climate probably had only a small impact on peatification. -
Absence of Photoemission from the Fermi Level in Potassium Intercalated Picene and Coronene films: Structure, Polaron Or Correlation Physics?
Absence of photoemission from the Fermi level in potassium intercalated picene and coronene films: structure, polaron or correlation physics? Benjamin Mahns,1 Friedrich Roth,1 and Martin Knupfer1 IFW Dresden, P.O. Box 270116, D-01171 Dresden, Germany (Dated: 13 September 2018) The electronic structure of potassium intercalated picene and coronene films has been studied using photoemission spectroscopy. Picene has additionally been intercalated using sodium. Upon alkali metal addition core level as well as valence band pho- toemission data signal a filling of previously unoccupied states of the two molecular materials due to charge transfer from potassium. In contrast to the observation of superconductivity in Kxpicene and Kxcoronene (x ∼ 3), none of the films studied shows emission from the Fermi level, i. e. we find no indication for a metallic ground state. Several reasons for this observation are discussed. arXiv:1203.4728v1 [cond-mat.supr-con] 21 Mar 2012 1 I. INTRODUCTION Superconductivity always has attracted a large number of researchers since this phe- nomenon harbors challenges and prospects both under fundamental and applied points of view. Very recently, it has been discovered that some molecular crystal consisting of poly- cyclic aromatic hydrocarbons demonstrate superconductivity upon alkali metal addition. Furthermore, these compounds are characterized by rather high transition temperatures into 1 2 the superconducting state, for instance K3picene (Tc=18 K) and K3coronene (Tc=15 K) . Most recently, superconductivity with a transition temperature of 33 K has been reported 3 for K3dibenzopentacene . These doped aromatic hydrocarbons thus represent a class of or- ganic superconductors with transition temperatures only slightly below that of the famous 4{8 alkali metal doped fullerenes with Tc's up to 40 K . -
Determination of Molecular Signatures of Natural and Thermogenic Products in Tropospheric Aerosols - Input and Transport
AN ABSTRACT OF THE THESIS OF Laurel J. Standley for the degree of Doctor of Philosophy in Oceanography presented on June 12, 1987. Title: Determination of Molecular Signatures of Natural and Thermogenic Products in Tropospheric Aerosols - Input and Transport Redacted for Privacy Abstract approved: Bernd R.Y. Simoneit A cheniotaxonomic study of natural compounds and their thermally altered products in rural and smoke aerosols within Oregon is pre- sented. Correlation with source vegetation provided information on the formation of aerosols and their transport. Distributions and concentrations of straight-chain homologous series such as n- alkanes, n-alkanoic acids, n-alkan-2-ones, n-alkanols and n-alkanals were analyzed in rural aerosols, aerosols produced by prescribed burning and residential wood combustion, and extracts of source vegetation. Cyclic di- and triterpenoids were also examined. The latter components provided more definitive correlations between source vegetation and aerosols. Results included: (1) an increase in Cmax in regions of warmer climate; (2) possible correlation of aerosols with source vegetation 100 km to the east; (3) the tracing of input from combustion of various fuels such as pine, oak and alder in aerosols produced by residential wood combustion; and (4) preliminary results that demonstrate a potentially large input of thermally altered diterpenoids via direct deposition rather than diagenesis of unaltered sedimentary diterpenoids. CCopyright by Laurel J. Standley June 12, 1987 All rights reserved DETERMINATION OF MOLECULAR SIGNATURES OF NATURAL AND THERMOGENIC PRODUCTS IN TROPOSPHERIC AEROSOLS - INPUT AND TRANSPORT by Laurel 3. Standley A THESIS submitted to Oregon State University in partial fulfillment of the requirements for the degree of Doctor of Philosophy Completed June 12, 1987 Commencement June, 1988 APPROVED: Redacted for Privacy Dr.