Factors Influencing Methyl Iodide Production in the Ocean and Its Flux to the Atmosphere

Total Page:16

File Type:pdf, Size:1020Kb

Factors Influencing Methyl Iodide Production in the Ocean and Its Flux to the Atmosphere Factors influencing methyl iodide production in the ocean and its flux to the atmosphere Dissertation zur Erlangung des Doktorgrades der Mathematisch-Naturwissenschaftlichen Fakultät der Christian-Albrechts-Universität zu Kiel vorgelegt von Uwe Richter Kiel 2003 1 Referent: Prof. Dr. D.W.R. Wallace Korreferent: Prof. Dr. A. Körtzinger Tag der mündlichen Prüfung: 5.2.2004 Zum Druck genehmigt: 15.3.2004 gez. Prof. Dr. Wulf Depmeier 2 Table of contents Abstract ................................................................................................................6 Zusammenfassung ...............................................................................................7 1. Introduction .....................................................................................................8 1.1 Natural halocarbons ....................................................................................8 1.2 Methyl iodide in the atmosphere................................................................10 1.2.1 Sources for the atmosphere....................................................................................... 10 1.2.2 Sinks in the atmosphere............................................................................................ 12 1.3 Methyl iodide in the ocean .........................................................................13 1.3.1 Sources for the ocean................................................................................................ 14 1.3.2 Oceanic sinks............................................................................................................ 15 1.4 Goal of the present study............................................................................16 2. Data collecting methods................................................................................17 2.1 Cruise tracks...............................................................................................17 2.2 Methods for halocarbon measurements.....................................................18 2.3 Equilibrator................................................................................................20 2.4 Traps...........................................................................................................23 2.4.1 Traps for removing water ......................................................................................... 23 2.4.2 Traps for concentration of analytes .......................................................................... 23 2.5 Gas chromatographic system.....................................................................25 2.6 Water samples ............................................................................................27 2.7 Air samples .................................................................................................28 2.8 Standards....................................................................................................28 3 2.9 Water vapour correction ............................................................................30 2.10 Chlorophyll measurements.......................................................................31 3. Underway data...............................................................................................32 3.1 Air samples .................................................................................................32 3.2 Surface water samples................................................................................34 3.2.1 Henry’s law constant ................................................................................................ 34 3.2.2 Surface water concentrations.................................................................................... 35 3.3 Flux calculations ........................................................................................36 3.3.1 Transfer velocity....................................................................................................... 38 3.3.2 Schmidt number........................................................................................................ 40 3.3.3 Wind speed corrections ............................................................................................ 42 3.3.4 Concentration anomaly............................................................................................. 43 3.3.5 Methyl iodide flux calculations ................................................................................ 43 3.4 Discussion of the underway data ...............................................................48 4. Incubation experiments ................................................................................57 4.1 Introduction................................................................................................57 4.2 Methods ......................................................................................................59 4.2.1 Incubation flasks....................................................................................................... 59 4.2.2 Experimental protocol .............................................................................................. 61 4.3 Results.........................................................................................................63 4.4 Discussion...................................................................................................72 4.4.1 Freshwater controls................................................................................................... 76 4.4.2 Production rates ........................................................................................................ 77 5. Discussion.......................................................................................................82 5.1 Flux calculations ........................................................................................82 5.1.1 Proxies for methyl iodide?........................................................................................ 83 5.1.2 Global ocean atmosphere flux .................................................................................. 86 4 5.2 Global budget of methyl iodide..................................................................90 5.2.1 Sources and sinks of oceanic methyl iodide ............................................................. 92 5.3 Future research ..........................................................................................97 5.4 Conclusions ................................................................................................98 6. Literature .......................................................................................................99 Abbreviations and symbols ............................................................................111 List of figures ...................................................................................................114 List of tables.....................................................................................................115 5 Abstract Methyl iodide is an atmospheric trace gas and a major source of atmospheric iodine. Recent estimates of methyl iodide sources and sinks indicate that anthropogenic sources are neglectible. The major source of atmospheric methyl iodide are emissions from the ocean. The production pathways of methyl iodide in the ocean are, however, poorly understood. The known oceanic sources can only account for about 10 % of the ocean-atmosphere flux, whereas the sources for the remaining 90 % are not known. In this work a measuring system, consisting of an equilibrator connected to a 2-dimensional gas chromatograph, equipped with two electron capture detectors, was developed. This system was used on four cruises in the tropical and North Atlantic to measure the seawater concentrations and the atmospheric dry gas mole fractions of methyl iodide, and the ocean- atmosphere flux was calculated. A mean flux of ~22 nmol m-2 d-1 was calculated from all cruises. A global annual flux of 2.89 Gmol a-1 was estimated using this flux. The limiting factor for the methyl iodide flux seems to be the production in the ocean, because the measured fluxes were relatively uniform and independent from observed changes in the surface water concentrations and wind speeds. Incubation experiments were done in the tropical Atlantic to test the hypothesis that methyl iodide is produced in the surface water by a photochemical pathway, instead direct biological production by phytoplankton or bacteria. During the experiments untreated, filtered and poisoned seawater was incubated at ambient water temperature, either in the sunlight or in the dark. The production of methyl iodide observed in all incubations kept in the sunlight was five times higher than the production from incubations kept in the dark. No significant difference was observed between untreated, filtered and poisoned samples. This strongly indicates a photochemical production with no direct influence by biota. The mean photochemical production rate from all incubations was 0.12 nmol m-3 h-1. A layer of 14 m with this production rate is needed to balance the methyl iodide sinks from the halogen exchange reaction with chloride in the mixed layer and the flux to the atmosphere, based on model calculations. The global photochemical production of methyl iodide was estimated to be 5.3 Gmol a-1, using the measured production rate and a the calculated layer depth of 14 m. From these results the photochemical production of methyl
Recommended publications
  • WO 2015/095882 Al 25 June 2015 (25.06.2015) W P O P C T
    (12) INTERNATIONAL APPLICATION PUBLISHED UNDER THE PATENT COOPERATION TREATY (PCT) (19) World Intellectual Property Organization International Bureau (10) International Publication Number (43) International Publication Date WO 2015/095882 Al 25 June 2015 (25.06.2015) W P O P C T (51) International Patent Classification: (81) Designated States (unless otherwise indicated, for every C12Q 1/68 (2006.0 1) C12Q 1/70 (2006.0 1) kind of national protection available): AE, AG, AL, AM, AO, AT, AU, AZ, BA, BB, BG, BH, BN, BR, BW, BY, (21) International Application Number: BZ, CA, CH, CL, CN, CO, CR, CU, CZ, DE, DK, DM, PCT/US20 14/07 1963 DO, DZ, EC, EE, EG, ES, FI, GB, GD, GE, GH, GM, GT, (22) International Filing Date: HN, HR, HU, ID, IL, IN, IR, IS, JP, KE, KG, KN, KP, KR, 22 December 2014 (22. 12.2014) KZ, LA, LC, LK, LR, LS, LU, LY, MA, MD, ME, MG, MK, MN, MW, MX, MY, MZ, NA, NG, NI, NO, NZ, OM, (25) Filing Language: English PA, PE, PG, PH, PL, PT, QA, RO, RS, RU, RW, SA, SC, (26) Publication Language: English SD, SE, SG, SK, SL, SM, ST, SV, SY, TH, TJ, TM, TN, TR, TT, TZ, UA, UG, US, UZ, VC, VN, ZA, ZM, ZW. (30) Priority Data: 61/ 19,663 20 December 201 3 (20. 12.20 13) US (84) Designated States (unless otherwise indicated, for every kind of regional protection available): ARIPO (BW, GH, (71) Applicant: THE REGENTS OF THE UNIVERSITY GM, KE, LR, LS, MW, MZ, NA, RW, SD, SL, ST, SZ, OF CALIFORNIA [US/US]; 1111 Franklin Street, TZ, UG, ZM, ZW), Eurasian (AM, AZ, BY, KG, KZ, RU, Twelfth Floor, Oakland, CA 94607-5200 (US).
    [Show full text]
  • Reactive Chlorine Compounds in the Atmosphere
    CHAPTER 1 Reactive Bromine Compounds O.N.Singh 1 · P.Fabian 2 1 Department of Applied Physics, Institute of Technology, Banaras Hindu University, Varanasi- 221 005, India. E-mail: [email protected] 2 University of Munich, Lehrstuhl für Bioklimatologie und Immissionsforschung, Am Hochanger 13, D-85354 Freising-Weihenstephan, Germany. E-mail: [email protected] Bromine, a minor constituent in the Earth’s atmosphere – with its 50-fold higher efficiency of ozone destruction compared to chlorine – contributes significantly to the ozone hole formation and wintertime stratospheric ozone depletion over northern mid and high latitudes.In addition ozone episodes observed in the Arctic during polar sunrise are solely due to atmospheric bromine.CH3Br, CH2Br2 and CHBr3 are the major brominated gases in the atmosphere, of which CH3Br being most abundant, contributes about 50% and CH2Br2 around 7 to 10% of the total organic stratospheric bromine.Bromocarbons with shorter lifetimes like CHBr3 ,CH2BrCl, CHBr2Cl, CHBrCl2 and CH2BrI decompose before reaching the stratosphere, and are responsible for the ozone episodes.But for 3CHBr, which has also significant anthropogenic sources, all the aforementioned bromocarbons are mostly of marine origin.Halons (H-1211, H-1301, H-2402, H-1202) are solely anthropogenic and are far more stable.They decompose only after reaching the stratosphere.It is estimated that 39% of the stratospheric organic bromine (ª 7 pptv) loading is due to these halons.Increa- ses are being still registered in the atmospheric abundance of halons in spite of production restrictions.Though extensively investigated,the existing knowledge with regard to the pro- duction and degradation of atmospheric bromine gases, is not commensurate with its importance.
    [Show full text]
  • Welcome to the 18Th Radiochemical Conference. the Conference Is Held
    Czech Chem. Soc. Symp. Ser. 16, 49-257 (2018) RadChem 2018 elcome to the 18th Radiochemical Conference. The conference is held in Mariánské Lázne,ˇ the second largest W Czech spa and the largest and most beautiful city – garden in the Czech Republic. RadChem 2018 aims at maintaining the more than 55 year tradition of radiochemical conferences (the 1st Radiochemical Conference was held in 1961), dealing with all aspects of nuclear- and radiochemistry, organised in the Czech Republic (or formerly in Czechoslovakia). We strive to continue in the tradition of organising a fruitful and well attended platform for contacts between experts working in both basic and applied research in all aspects of nuclear- and radiochemistry. More than 300 scientists from 36 countries registered for the conference. The verbal sessions, where more than 170 plenary, invited and contributed presentations are scheduled to be presented, will be complemented by the corre- sponding poster sessions. Selected “hot topics” in nuclear- and radiochemistry will be covered in six plenary opening lectures delivered by invited recognized experts. These talks will include laureate lectures by winners of two pres- tigious medals – Ioannes Marcus Marci Medal awarded by the Ioannes Marcus Marci Spectroscopic Society (won by Dr. Peter Bode) and Vladimír Majer Medal awarded by the Czech Chemical Society (won by Prof. Jukka K. Lehto). In conjunction with the technical programme, an exhibition covering technologies, equipment, technical and management services in areas pertaining to the theme of the conference will be held. The extensive social programme is expected to provide an opportunity for informal contacts and discussions among the participants.
    [Show full text]
  • UV Photodissociation Dynamics of Chi2cl and Its Role As a Photolytic Precursor for a Chlorinated Criegee Intermediate
    This is a repository copy of UV Photodissociation Dynamics of CHI2Cl and its Role as a Photolytic Precursor for a Chlorinated Criegee Intermediate. White Rose Research Online URL for this paper: http://eprints.whiterose.ac.uk/124025/ Version: Accepted Version Article: Kapnas, K.M., Toulson, B.W., Foreman, E.S. et al. (3 more authors) (2017) UV Photodissociation Dynamics of CHI2Cl and its Role as a Photolytic Precursor for a Chlorinated Criegee Intermediate. Physical Chemistry Chemical Physics. ISSN 1463-9076 https://doi.org/10.1039/C7CP06532A Reuse Items deposited in White Rose Research Online are protected by copyright, with all rights reserved unless indicated otherwise. They may be downloaded and/or printed for private study, or other acts as permitted by national copyright laws. The publisher or other rights holders may allow further reproduction and re-use of the full text version. This is indicated by the licence information on the White Rose Research Online record for the item. Takedown If you consider content in White Rose Research Online to be in breach of UK law, please notify us by emailing [email protected] including the URL of the record and the reason for the withdrawal request. [email protected] https://eprints.whiterose.ac.uk/ UV Photodissociation Dynamics of CHI2Cl and its Role as a Photolytic Precursor for a Chlorinated Criegee Intermediate Kara M. Kapnas, Benjamin W. Toulson,1 Elizabeth S. Foreman,2 Sarah A. Block, and Craig Murray3 Department of Chemistry, University of California, Irvine, Irvine CA 92697, USA J. Grant Hill4 Department of Chemistry, University of Sheffield, Sheffield S3 7HF, UK 1 Current address: Chemical Sciences Division, Lawrence Berkeley National Laboratory, Berkeley, California 94720, USA.
    [Show full text]
  • Recent Discoveries on the Structure of Iodine(Iii) Reagents and Their Use in Cross-Nucleophile Coupling
    Chemical Science View Article Online PERSPECTIVE View Journal | View Issue Recent discoveries on the structure of iodine(III) reagents and their use in cross-nucleophile Cite this: Chem. Sci.,2021,12,853 All publication charges for this article coupling have been paid for by the Royal Society of Chemistry Adriano Bauer and Nuno Maulide * Received 11th June 2020 This perspective article discusses structural features of iodine(III) compounds as a prelude to presenting their Accepted 15th December 2020 use as umpolung reagents, in particular as pertains to their ability to promote the selective coupling of two DOI: 10.1039/d0sc03266b nucleophilic species via 2eÀ oxidation. rsc.li/chemical-science Introduction Reactions which follow a redox umpolung approach (Scheme1d)canbetermed“cross-nucleophile couplings” in One of the cornerstones of modern organic synthesis was set analogy to the term “cross-electrophile couplings” which with the advent of retrosynthetic analysis as a powerful refers on the use of two electrophilic species in combination Creative Commons Attribution 3.0 Unported Licence. systematic tool for planning a synthetic route.1 Its introduction with a reductant.38 made it increasingly more evident, that 1,3- or 1,5-heteroatom- substituted carbon frameworks are usually easily accessible General aspects of the chemistry of because their synthons adhere to what is referred to as natural polarity (Scheme 1a). On the other hand, 1,2- or 1,4-heteroatom- organoiodine compounds substituted organic molecules present challenges resulting The chemical properties of iodine are determined by its from the need that one of the synthons reacts with inversed relatively low electronegativity and its high polarizability polarity (i.e.
    [Show full text]
  • (12) Patent Application Publication (10) Pub. No.: US 2011/0052503 A1 Almen Et Al
    US 2011 0052503A1 (19) United States (12) Patent Application Publication (10) Pub. No.: US 2011/0052503 A1 Almen et al. (43) Pub. Date: Mar. 3, 2011 (54) BIODEGRADABLE CONTRASTAGENTS (30) Foreign Application Priority Data (75) Inventors: Torsten Almen, Lund (SE); Bjarne Dec. 21, 2007 (GB) ................................... O725070.7 Brudeli, Lund (SE); Fred Kjelson, Lund (SE); Jo Klaveness, Lund Publication Classification (SE); Jian-Sheng Wang, Lund (SE) (51) Int. Cl. (73) Assignee: OPHARMA TECHNOLOGIES g 19 :08: AB, Lund (SE) (52) U.S. Cl. .......................................... 424/9.4; 252/478 (21) Appl. No.: 12/808,318 (57) ABSTRACT (22) PCT Filed: Dec. 22, 2008 The present invention provides a radio-opaque composition (86). PCT No.: PCT/GB2O08/OO.4268 comprising a cleavable, preferably enzymatically-cleavable, derivative of a physiologically tolerable organoiodine com S371 (c)(1), pound and a non-acrylic polymer wherein said derivative is (2), (4) Date: Nov. 8, 2010 incorporated in said non-acrylic polymer. Patent Application Publication Mar. 3, 2011 Sheet 1 of 5 US 2011/0052503 A1 Degradation of IHA to lohexol -0-lohexol -u HA Day2 Day3 Degradation Time --PLLA --PLLA+2%HA aris-PLLA -5%HA -(-PLLA10%IHA-K-PLLA-15%IHA-O-PLLA+20%IHA Fig. 2 Patent Application Publication Mar. 3, 2011 Sheet 2 of 5 US 2011/0052503 A1 PLLA PLLA2%IHA PLLA+5%IHA PLLAH10%IHA PLLA-15%IHA PLLA20%IHA Sample ODay 0 Day 10 Day 50 Day 81 Day 10 Fig. 3 Patent Application Publication Mar. 3, 2011 Sheet 3 of 5 US 2011/0052503 A1 Patent Application Publication Mar. 3, 2011 Sheet 4 of 5 US 2011/0052503 A1 Patent Application Publication Mar.
    [Show full text]
  • Practical Lab Manual of Pharmaceutical Organic Chemistry - I
    Practical Lab Manual of Pharmaceutical Organic Chemistry - I As Per PCI Syllabus B. Pharm 2nd Semester Dr. Shivendra Kumar Dwivedi M. Pharm (Pharmaceutical Chemsitry), Ph.D. Assoc. Professor University of Pharmacy, Oriental University, Indore (MP) IP Innovative Publication Pvt. Ltd. Dedicated Affectionately to my Father Mr. Ramkhelawan Dwivedi, he is also a great teacher in a sky and my Mother Mrs. Phool Kumari Dwivedi. Shivendra Kumar Dwivedi About the Author Dr. Shivendra Kumar Dwivedi, M. Pharm (Pharmaceutical Chemistry), Ph.D., presently working as an Assoc. Professor in University Institute of Pharmacy, Oriental University, Indore (M.P). He has 10 years of experience in academics and research. He is also the author of some of the other books for UG and PG in Pharmaceutical Chemistry and Practical manual. He has published more than 30 research papers in a different versatile International and National journals. Acknowledgement I am indebted to all my family members particularly to my wife Mrs. Namrata Dwivedi, my daughter Shravi Dwivedi who have always remained my source of inspiration and encouragement. I am grateful to Dr. Neetesh Jain, Principal, UIP, Oriental University, Indore (M.P.) for every step to encourage to publish the book. I am also grateful to Dr. Mahavir Chached, Principal, OCPR, Oriental University, Indore (M.P.) and Dr. Rakesh Patel, Principal & Professor, School of Pharmacy, APJ Abdul Kalam University, Indore (M.P.) for giving guidance to publish the book. Note for the Students If you are a student, you will probably appreciate our effort to present you the book “Practical Lab manual of Pharmaceutical Organic Chemistry - I, which covers all practicals in the 2nd semester in organic chemistry - I.
    [Show full text]
  • Hypervalent Iodine Compounds: Reagents of the Future
    The Free Internet Journal Review for Organic Chemistry Archive for Arkivoc 2020, part iv, 1-11 Organic Chemistry Hypervalent iodine compounds: reagents of the future Viktor V. Zhdankin Department of Chemistry and Biochemistry, University of Minnesota Duluth, Duluth, Minnesota 55 812, USA Email: [email protected] Received 01-01-2020 Accepted 01-26-2020 Published on line 01-31-2020 Abstract This short introductory review provides a brief summary of history and recent developments in the field of hypervalent iodine chemistry in connection with the 7th International Conference on Hypervalent Iodine Chemistry (ICHIC-2021, Moscow, 27th June to 1st July, 2021). Hypervalent iodine reagents and catalysts are intensively used in modern organic chemistry as mild, environmentally safe, and economical alternative to heavy metal reagents. General features and applications of hypervalent iodine compounds are overviewed. Keywords: Iodine, hypervalent iodine, iodonium, oxidation DOI: https://doi.org/10.24820/ark.5550190.p011.145 Page 1 ©AUTHOR(S) Arkivoc 2020, iv, 1-11 Zhdankin, V. V. Table of Contents 1. Introduction 2. Brief history of Organohypervalent Iodine Chemistry 3. General Classification of Hypervalent Iodine Compounds 4. Recent Developments and Future Perspectives 5. Conclusions 6. Acknowledgements References 1. Introduction Iodine is an essential element closely linked to our daily life.1 In the human body, iodine is present in the thyroid gland in the form of thyroxine, a metabolism-regulating hormone. In natural organic compounds, iodine occurs exclusively in the monovalent state. However, it can form a myriad of polycoordinated compounds in different oxidation states. In modern literature, polyvalent compounds of iodine are commonly named as “hypervalent” iodine compounds, which reflects the special [3c-4e] hypervalent bonding present in these molecules.2-5 Structural features and reactivity pattern of hypervalent iodine compounds in many aspects are similar to the derivatives of heavy transition metals.
    [Show full text]
  • Applications of Hypervalent Iodine Reagents in Organic Synthesis: the Development of Iodonium Metathesis Reaction and Effort Towards Himandrine
    APPLICATIONS OF HYPERVALENT IODINE REAGENTS IN ORGANIC SYNTHESIS: THE DEVELOPMENT OF IODONIUM METATHESIS REACTION AND EFFORT TOWARDS HIMANDRINE by Takahito Kasahara A THESIS SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY in THE FACULTY OF GRADUATE AND POSTDOCTORAL STUDIES (Chemistry) THE UNIVERSITY OF BRITISH COLUMBIA (Vancouver) October 2015 © Takahito Kasahara, 2015 Abstract This thesis discloses two different applications of hypervalent iodine(III) reagents in organic synthesis. In the first part, a novel reactivity of diaryliodonium triflates towards aryl iodides will be discussed. The new mode of reactivity allows various diaryliodonium triflates to be accessed, simply by heating a mixture of electron deficient diaryliodonium triflate with a moderately electron rich aryliodide. In the second part of the thesis, the use of (diacetoxyiodo)benzene in oxidative amidation in the context of total synthesis will be made. ii Preface The thesis is written by, and is based on experiments conducted by Kasahara, T. Professor Ciufolini, M. A. provided the overall synthetic strategy and tactic, helpful suggestions, and thorough editing of the thesis. The research reported in Chapter 1 has been published in: Kasahara,T.; Jang, Y. J.; Racicot, L.; Panagopoulos, D.; Liang, S. H.; Ciufolini M. A. Angew. Chem. Int. Ed. 2014, 53, 9637. Professor Ciufolini, M. A. wrote the manuscript, Kasahara, T. and Racicot, L. wrote the supporting information. The data shown in Table 1.1 and 1.2 are based on experiments performed by Racicot, L. The results shown in Scheme 1.15 are based on experiments peformed by Jang, Y. J. Semi-empirical calculations (HyperChem) shown in Figure 1.6 was performed by Professor Ciufolini, M.
    [Show full text]
  • Download Article (PDF)
    Main Group Metal Chemistry Vol. 25, No. 10, 2002 (POLYFLUOROORGANO)HALOBORANES AND (POLYFLUOROORGANO)FLUOROBORATE SALTS: PREPARATION, NMR SPECTRA AND REACTIVITY Vadim V. Bardin1 and Hermann-Josef Frohn2 * 1 Ν. N. Vorozhtsov Novosibirsk Institute of Organic Chemistry SB RAS, 630090 Novosibirsk, Russia 2 Institute of Chemistry, Inorganic Chemistry, Gerhard-Mercator-Universität Duisburg, Lotharstr. 1, D-47048 Duisburg, Germany <[email protected]> ABSTRACT New developments concerning the preparation and reactivity of (polyfluoroorgano)haloboranes RFBX2, (RF)2BX (X = F, CI, Br), some of their adducts (RF)NBX,. · Base (n = 1 - 3), and their related fluoroborate salts Μ [(RF)nBF4.„] were reviewed. Significant 'B and F NMR spectroscopic patterns of all three classes were described. CONTENTS 1. Introduction 2. Preparation of (polyfluoroorgano)haloboranes RFBX2 and (RF)2BX (X = F, CI, Br) 2.1. From (polyfluoroorgano)metallic precursors 2.2. From other (polyfluoroorgano)boron compounds 2.3. By various procedures 3. Preparation of (polyfluoroorgano)fluoroborate salts Μ [(RF)nBF4_n] 4. The NMR spectra of (polyfluoroorgano)haloboranes, their complexes with bases and (polyfluoroorgano)fluoroborate salts 5. "The reactivity of (polyfluoroorgano)haloboranes 5.1. Thermal stability 5.2. Reactions with bases and nucleophiles 5.3. Reactions with anhydrous HF 5.4. Conversion of(RF)„BX3.n into (RF)nBF3_n (X = CI, Br) 5.5. Reactions of (polyfluoroorgano)haloboranes with hypervalent fluorine-element-fluorine bonds in xenon fluorides, bromine trifluoride, and organoiodine difluorides 5.6. Reactions of (polyfluoroorgano)haloboranes with selected organoelement compounds. 6. The reactivity of (polyfluoroorgano)fluoroborate salts 7. Conclusions 8. References 1. INTRODUCTION (Organo)dihaloboranes RBX2 and di(organo)haloboranes R2BX (X = F, CI, Br, I) are well-established compounds and their preparations and reactivities were reviewed in fundamental monographs [1, 2].
    [Show full text]
  • 1 Halogen-Specific Total Organic Halogen Analysis
    1 Halogen-Specific Total Organic Halogen Analysis: Assessment by Recovery of Total 2 Bromine 3 4 Markus Langsa1,3, Sebastien Allard1, Ina Kristiana1, Anna Heitz2 and Cynthia A. Joll1* 5 6 1. Curtin Water Quality Research Centre, Department of Chemistry, Curtin University, 7 Perth Western Australia 6102, Australia. E-mail: [email protected] 8 2. Department of Civil Engineering, Curtin University, Perth Western Australia 6102, 9 Australia 10 3. Jurusan Kimia, Fakultas Matematika dan Ilmu Pengetahuan Alam, Universitas Papua, 11 Manokwari Papua Barat 98314, Indonesia 12 13 *Corresponding Author. E-mail: [email protected]. Phone: +61 8 9266 7229. Postal 14 address: Curtin Water Quality Research Centre, GPO Box U1987, Perth WA 6845, Australia. 15 16 Abstract: Determination of halogen-specific total organic halogen (TOX) is vital for 17 studies of disinfection of waters containing bromide, since total organic bromine (TOBr) is 18 likely to be more problematic than total organic chlorine. Here, we present further halogen- 19 specific TOX method optimisation and validation, focusing on measurement of TOBr. The 20 optimised halogen-specific TOX method was validated based on the recovery of model 21 compounds covering different classes of disinfection by-products (haloacetic acids, 22 haloacetonitriles, halophenols and halogenated benzenes) and the recovery of total bromine 23 (mass balance of TOBr and bromide concentrations) during disinfection of waters containing 24 dissolved organic matter and bromide. The validation of a halogen-specific TOX method 25 based on the mass balance of total bromine has not previously been reported. Very good 26 recoveries of organic halogen from all model compounds were obtained, indicating high or 27 complete conversion of all organic halogen in the model compound solution through to halide 28 in the absorber solution for ion chromatography analysis.
    [Show full text]
  • Czech Chemical Society Ch Al Ty
    CzechCzech www.spektroskopie.cz ABOUT US ChemicalChemical Ioannes Marcus Marci Spectroscopic Society (IMMSS) is a non-profit organization of scientific, educational and professional technical workers in spectroscopy, eventually legal entities engaged in scientific or application activities in this field, all associated in joint activities with the aims of promoting and fostering advancement in the field of spectroscopy. IMMSS has SocietySociety currently ca 110 members . Its history dates back to 1949 (Czechoslovak Spectroscopic Society). The Society is named after Ioannes Marcus Marci (1595-1667), a distinguished doctor, physicist and mathematician of the renaissance and rector of Charles University in Prague. Marci is sometimes denoted as a first spectroscopist in history and foreshadower of Newton since he had dealt with light refraction well before him, studied and explained the nature of the phenomenon of the rainbow. ACTIVITIES AWARDS IMMSS bulletin – published quarterly Ioannes Marcus Marci medal SymposiumSymposiumSymposiumSymposium (co)organization of conferences and workshops o awarded to eminent foreign and domestic scientists in recognition of their outstanding o national level: workshops/conferences in different fields of spectroscopy. The biggest one is the annual achievements in some of the spectroscopic Summer school of mass spectrometry (>200 participants). disciplines o international level: Czech-Slovak Spectroscopic Conference (biennial) o Ioannes Marcus Marci medal laureates SeriesSeriesSeriesSeries European Symposium on Atomic Spectrometry (ESAS) 2014 include five Nobel prize winners: Euro-Mediterranean Symposium on Laser-Induced Breakdown Spectroscopy (EMSLIBS) 2019 2222 prof. Eric Allin Cornell organization of competitons prof. Dr. Theodor W. Hänsch prof. Ahmed H. Zewail o The Young Authors’ Best Paper in Spectroscopy Competition – annualy in two categories: as the best dissertation in the field; as the best spectrosopic paper(s) published of author below Sir Harold W.
    [Show full text]