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Transport of Dangerous Goods
ST/SG/AC.10/1/Rev.16 (Vol.I) Recommendations on the TRANSPORT OF DANGEROUS GOODS Model Regulations Volume I Sixteenth revised edition UNITED NATIONS New York and Geneva, 2009 NOTE The designations employed and the presentation of the material in this publication do not imply the expression of any opinion whatsoever on the part of the Secretariat of the United Nations concerning the legal status of any country, territory, city or area, or of its authorities, or concerning the delimitation of its frontiers or boundaries. ST/SG/AC.10/1/Rev.16 (Vol.I) Copyright © United Nations, 2009 All rights reserved. No part of this publication may, for sales purposes, be reproduced, stored in a retrieval system or transmitted in any form or by any means, electronic, electrostatic, magnetic tape, mechanical, photocopying or otherwise, without prior permission in writing from the United Nations. UNITED NATIONS Sales No. E.09.VIII.2 ISBN 978-92-1-139136-7 (complete set of two volumes) ISSN 1014-5753 Volumes I and II not to be sold separately FOREWORD The Recommendations on the Transport of Dangerous Goods are addressed to governments and to the international organizations concerned with safety in the transport of dangerous goods. The first version, prepared by the United Nations Economic and Social Council's Committee of Experts on the Transport of Dangerous Goods, was published in 1956 (ST/ECA/43-E/CN.2/170). In response to developments in technology and the changing needs of users, they have been regularly amended and updated at succeeding sessions of the Committee of Experts pursuant to Resolution 645 G (XXIII) of 26 April 1957 of the Economic and Social Council and subsequent resolutions. -
Alluvial Fans in the Death Valley Region California and Nevada
Alluvial Fans in the Death Valley Region California and Nevada GEOLOGICAL SURVEY PROFESSIONAL PAPER 466 Alluvial Fans in the Death Valley Region California and Nevada By CHARLES S. DENNY GEOLOGICAL SURVEY PROFESSIONAL PAPER 466 A survey and interpretation of some aspects of desert geomorphology UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1965 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director The U.S. Geological Survey Library has cataloged this publications as follows: Denny, Charles Storrow, 1911- Alluvial fans in the Death Valley region, California and Nevada. Washington, U.S. Govt. Print. Off., 1964. iv, 61 p. illus., maps (5 fold. col. in pocket) diagrs., profiles, tables. 30 cm. (U.S. Geological Survey. Professional Paper 466) Bibliography: p. 59. 1. Physical geography California Death Valley region. 2. Physi cal geography Nevada Death Valley region. 3. Sedimentation and deposition. 4. Alluvium. I. Title. II. Title: Death Valley region. (Series) For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C., 20402 CONTENTS Page Page Abstract.. _ ________________ 1 Shadow Mountain fan Continued Introduction. ______________ 2 Origin of the Shadow Mountain fan. 21 Method of study________ 2 Fan east of Alkali Flat- ___-__---.__-_- 25 Definitions and symbols. 6 Fans surrounding hills near Devils Hole_ 25 Geography _________________ 6 Bat Mountain fan___-____-___--___-__ 25 Shadow Mountain fan..______ 7 Fans east of Greenwater Range___ ______ 30 Geology.______________ 9 Fans in Greenwater Valley..-----_____. 32 Death Valley fans.__________--___-__- 32 Geomorpholo gy ______ 9 Characteristics of fans.._______-___-__- 38 Modern washes____. -
Clear-Chlor Lithium - 0040 Product Name: Clear-Chlor Lithium Date: 5/19/2015
SAFETY DATA SHEET Clear-Chlor Lithium - 0040 Product Name: Clear-Chlor Lithium Date: 5/19/2015 1. SECTION 1 IDENTIFICATION Supplier: Phoenix Products Company Distributor: 55 Container Drive Terryville, CT 06786 (860) 589-7502 U.S. PERS Emergency Telephone: 1-800-633-8253 Product Name: Clear-Chlor Lithium Synonyms: Hypochlorous acid, lithium salt; Lithium chlorideoxide; Lithium oxychloride; Hypure L Chemical Name: Lithium Hypochlorite Chemical Formula: ClLiO CAS Number: 13840-33-0 Product Use: Water sanitizer. 2. SECTION 2 HAZARDS IDENTIFICATION Emergency Overview Danger Corrosive Hazard Statement(s) H272: May intensify fire; oxidizer H314: Causes severe skin burns and eye damage H302: Harmful if swallowed H335: May cause respiratory irritation H410: Very toxic to aquatic life with long lasting effects Precautionary Statement(s) P210: Keep away from heat/sparks/open flames/hot surfaces. - No smoking P220: Keep/Store away from clothing/ combustible materials P221: Take any precaution to avoid mixing with combustibles/other chemicals P260: Do not breathe dust. P262: Do not get in eyes, on skin, or on clothing. P270: Do not eat, drink or smoke when using this product P271: Use only outdoors or in a well-ventilated area P273: Avoid release to the environment P280: Wear protective gloves/protective clothing/eye protection/face protection. P284: [In case of inadequate ventilation] wear respiratory protection. P233: Keep container tightly closed. P264: Wash thoroughly after handling. P363: Wash contaminated clothing before reuse P321: Specific treatment (see First Aid Measures on this label). P310: Immediately call a POISON CENTER or doctor/physician P391: Collect spillage P405: Store locked up P403+P233: Store in a well-ventilated place. -
Design, Synthesis and Evaluation of Diphenylamines As MEK5 Inhibitors Suravi Chakrabarty
Duquesne University Duquesne Scholarship Collection Electronic Theses and Dissertations Fall 2014 Design, Synthesis and Evaluation of Diphenylamines as MEK5 Inhibitors Suravi Chakrabarty Follow this and additional works at: https://dsc.duq.edu/etd Recommended Citation Chakrabarty, S. (2014). Design, Synthesis and Evaluation of Diphenylamines as MEK5 Inhibitors (Master's thesis, Duquesne University). Retrieved from https://dsc.duq.edu/etd/388 This Immediate Access is brought to you for free and open access by Duquesne Scholarship Collection. It has been accepted for inclusion in Electronic Theses and Dissertations by an authorized administrator of Duquesne Scholarship Collection. For more information, please contact [email protected]. DESIGN, SYNTHESIS AND EVALUATION OF DIPHENYLAMINES AS MEK5 INHIBITORS A Thesis Submitted to the Graduate School of Pharmaceutical Sciences Duquesne University In partial fulfillment of the requirements for the degree of Master of Science (Medicinal Chemistry) By Suravi Chakrabarty December 2014 Copyright by Suravi Chakrabarty 2014 DESIGN, SYNTHESIS AND EVALUATION OF DIPHENYLAMINES AS MEK5 INHIBITORS By Suravi Chakrabarty Approved August 7, 2014 ________________________________ ________________________________ Patrick Flaherty, Ph.D. Aleem Gangjee, Ph.D., Chair, Thesis Committee Professor of Medicinal Chemistry Associate Professor of Medicinal Mylan School of Pharmacy Chemistry Distinguished Professor Graduate School Pharmaceutical Sciences Graduate School Pharmaceutical Sciences Duquesne University Duquesne -
Washington State Minerals Checklist
Division of Geology and Earth Resources MS 47007; Olympia, WA 98504-7007 Washington State 360-902-1450; 360-902-1785 fax E-mail: [email protected] Website: http://www.dnr.wa.gov/geology Minerals Checklist Note: Mineral names in parentheses are the preferred species names. Compiled by Raymond Lasmanis o Acanthite o Arsenopalladinite o Bustamite o Clinohumite o Enstatite o Harmotome o Actinolite o Arsenopyrite o Bytownite o Clinoptilolite o Epidesmine (Stilbite) o Hastingsite o Adularia o Arsenosulvanite (Plagioclase) o Clinozoisite o Epidote o Hausmannite (Orthoclase) o Arsenpolybasite o Cairngorm (Quartz) o Cobaltite o Epistilbite o Hedenbergite o Aegirine o Astrophyllite o Calamine o Cochromite o Epsomite o Hedleyite o Aenigmatite o Atacamite (Hemimorphite) o Coffinite o Erionite o Hematite o Aeschynite o Atokite o Calaverite o Columbite o Erythrite o Hemimorphite o Agardite-Y o Augite o Calciohilairite (Ferrocolumbite) o Euchroite o Hercynite o Agate (Quartz) o Aurostibite o Calcite, see also o Conichalcite o Euxenite o Hessite o Aguilarite o Austinite Manganocalcite o Connellite o Euxenite-Y o Heulandite o Aktashite o Onyx o Copiapite o o Autunite o Fairchildite Hexahydrite o Alabandite o Caledonite o Copper o o Awaruite o Famatinite Hibschite o Albite o Cancrinite o Copper-zinc o o Axinite group o Fayalite Hillebrandite o Algodonite o Carnelian (Quartz) o Coquandite o o Azurite o Feldspar group Hisingerite o Allanite o Cassiterite o Cordierite o o Barite o Ferberite Hongshiite o Allanite-Ce o Catapleiite o Corrensite o o Bastnäsite -
Reactions of Lithium Nitride with Some Unsaturated Organic Compounds. Perry S
Louisiana State University LSU Digital Commons LSU Historical Dissertations and Theses Graduate School 1963 Reactions of Lithium Nitride With Some Unsaturated Organic Compounds. Perry S. Mason Jr Louisiana State University and Agricultural & Mechanical College Follow this and additional works at: https://digitalcommons.lsu.edu/gradschool_disstheses Recommended Citation Mason, Perry S. Jr, "Reactions of Lithium Nitride With Some Unsaturated Organic Compounds." (1963). LSU Historical Dissertations and Theses. 898. https://digitalcommons.lsu.edu/gradschool_disstheses/898 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 Historical Dissertations and Theses by an authorized administrator of LSU Digital Commons. For more information, please contact [email protected]. This dissertation has been 64—5058 microfilmed exactly as received MASON, Jr., Perry S., 1938- REACTIONS OF LITHIUM NITRIDE WITH SOME UNSATURATED ORGANIC COMPOUNDS. Louisiana State University, Ph.D., 1963 Chemistry, organic University Microfilms, Inc., Ann Arbor, Michigan Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. REACTIONS OF LITHIUM NITRIDE WITH SOME UNSATURATED ORGANIC COMPOUNDS A Dissertation Submitted to the Graduate Faculty of the Louisiana State University and Agricultural and Mechanical College in partial fulfillment of the requireiaents for the degree of Doctor of Philosophy in The Department of Chemistry by Perry S. Mason, Jr. B. S., Harding College, 1959 August, 1963 Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. -
Iron.Rich Amesite from the Lake Asbestos Mine. Black
Canodian Mineralogist Yol.22, pp. 43742 (1984) IRON.RICHAMESITE FROM THE LAKE ASBESTOS MINE. BLACKLAKE. OUEBEC MEHMET YEYZT TANER,* AND ROGER LAURENT DAporternentde Gdologie,Universitd Loval, Qudbec,Qudbec GIK 7P4 ABSTRACT o 90.02(1l)', P W.42(12)',1 89.96(8)'.A notreconnais- sance,c'est la premibrefois qu'on ddcritune am6site riche Iron-rich amesite is found in a metasomatically altered enfer. Elles'ct form€ependant l'altdration hydrothermale granite sheet20 to 40 cm thick emplacedin serpentinite of du granitedans la serpentinite,dans les m€mes conditions the Thetford Mi[es ophiolite complex at the Lake Asbestos debasses pression et temperaturequi ont prdsid6d la for- mine (z16o01'N,11"22' W) ntheQuebec Appalachians.The mation de la rodingite dansle granite et de I'amiante- amesiteis associatedsdth 4lodingife 6semblage(grossu- chrysotiledans la serpentinite. lar + calcite t diopside t clinozoisite) that has replaced the primary minerals of the granite. The Quebec amesite Mots-clds:am6site, rodingite, granite, complexeophio- occurs as subhedral grains 2@ to 6@ pm.in diameter that litique, Thetford Mines, Qu6bec. have a tabular habit. It is optically positive with a small 2V, a 1.612,1 1.630,(t -'o = 0.018).Its structuralfor- INTRoDUc"iloN mula, calculated from electron-microprobe data, is: (Mg1.1Fe6.eA1s.e)(Alo.esil.df Os(OH)r.2. X-ray powder- Amesite is a raxehydrated aluminosilicate of mag- diffraction yield data dvalues that are systematicallygreater nesium in which some ferrous iron usually is found than those of amesitefrom Chester, Massachusetts,prob- replacingmapesium. The extent of this replacement ably becauseof the partial replacement of Mg by Fe. -
Fact Sheet the Conservation of Migratorywhale Sharks SHARK
Memorandum of Understanding on Sharks MOU Species Fact Sheet the Conservation of MigratoryWHALE Sharks SHARK WHALE SHARK REQUIN-BALEINE TIBURÓN BALLENA Fact Sheet Whale Shark Rhincodon typus WHALE SHARK Class: Chondrichthyes Order: Orectolobiforme Family : Rhincodontidae Species: Rhincodon typus 0 Illustration: © Marc Dando Sharks MOU Species Fact Sheet Sharks MOU Species Fact Sheet WHALE SHARK WHALE SHARK © Shark MOU Advisory Committee This fact sheet was produced by the Advisory Committee of the Memorandum of Understanding on the Conservation of Migratory Sharks (Sharks MOU). For further information contact: John Carlson, Ph.D. Research Fish Biologist, NOAA Fisheries Service-Southeast Fisheries Science Center Panama City, 1 [email protected] Sharks MOU Species Fact Sheet WHALE SHARK 1. Biology The Whale Shark (Rhincodon typus) is the world’s largest living fish (<20m), found globally in tropical and warm temperate waters (Rowat and Brooks 2012). Coastal feeding aggregations are known from these filter feeders, where they exploit seasonal productivity of pelagic invertebrates, fish spawning events, and small schooling fishes. Although encounters are rarely associated with surface temperatures below 21°C, Whale Sharks are capable of withstanding temperatures as low as 4.2°C during dives to up to 1,900 m (Colman 1997; Duffy 2002; Afonso et al. 2014; Tyminski et al. 2015). Their reproductive ecology is poorly understood but associated with slow growth and late maturity and therefore a limited reproductive capacity. 2. Distribution Whale Sharks are distributed circum-tropically from approximately 30°N to 35°S with seasonal variations (Rowat and Brooks 2012; Sequeira et al. 2014). Several aggregation sites are distributed over all three ocean basins, with major subpopulations in the Atlantic Ocean and Indo-Pacific (Sequeira et al. -
Bromine Geochemistry of Salar De Uyuni and Deeper Salt Crusts
... .............. * .. ........, ., ;: ... ... ........ .. ........, ., '_.~' . ...: .. ,... ' :, .. , ._... , .-. ,; ..,. _I. ................. .. ; . ... ............ ~ .. .- ............'. ............ .... , . :.. , *.,:.:-' ' .., '. -. - .. 'c..;..,. CHEMICAL /./da 3-4 GEOLOGY lSCL1lDlNri L ISOTOPE GEOSCIEiYCE ELSEVIER Chemical Geology 167 (2000) 373-392 www.elsevier.com/locate/chemgeo Bromine geochemistry of salar de Uyuni and deeper salt crusts, Central Altiplano, Bolivia I FranGois/Risacher a, Bertrand Fritz i E IRD-Centre de Géochiiliie de Ia Siriface, Fralice CNRS 1 rite Blessig, 67084 Strasboiirg Cedex, France Received 15 August 1999; accepted 13 December 1999 Abstract The salar of Uyuni, in the central Bolivian Altiplano, is probably the largest salt pan in the world (10000 km'). A 121 m deep well drilled in the central salar disclosed a complex evaporitic sequence of 12 salt crusts separated by 11 mud layers. In the lower half of the profile, thick halite beds alternate with thin mud layers. The mud layers thicken upwards and show clear lacustrine features. The thickness of the salt beds decreases markedly from the base upward. The bromine content of the halite ranges from 1.3 to 10.4 mg/kg. The halite does not originate from the evaporation of the dilute inflow waters of the Altiplano, which would lead to Br content of tens of mg/kg. The presence of halite of very low Br content (2 mg/kg) in a gypsum diapir strongly suggests that most of the halite deposited at Uyuni originated from the leaching of ancient salt formations associated with the numerous gypsum diapirs of the Altiplano. The deep and thick halite beds were probably deposited in a playa lake, as suggested by their very low and fairly constant Br content (1.6-2.3 mg/kg) and by the abundance of detrital minerals. -
Decontamination of Spas and Wading (Kiddie) Pools Revised – June 2011 Brought to You by the APSP Recreational Water Quality Committee
Fact Sheet Decontamination of Spas and Wading (Kiddie) Pools Revised – June 2011 Brought to you by the APSP Recreational Water Quality Committee I. INTRODUCTION The purpose of the fact sheet is to provide a generic overview of procedures to be used for the decontamination or annual maintenance of spas, hot tubs, swim spas and wading (kiddie) pools. If used for decontamination, the user/operator should check existing local or state regulatory agency guidelines. The following recommendations do not replace existing state or local guidelines. In the absence of regulatory agency guidelines, please refer to CDC Healthy Swimming recommendations. II. SUMMARY OF DECONTAMINATION CHARACTERISTICS 1. Decontaminate water, filter, plumbing 2. Drain, sanitize vessel, filter, plumbing then continue with water and /or filter media replacement and or treatment 3. Complete required documentation in cases involving an Accidental Fecal Release (AFR) accident or suspected bacterial outbreak or when decontamination is part of a general water replacement routine 4. Appropriate Personal Protective Equipment (PPE) should be worn by operators during the decontamination process. See Precautions section for more information. This APSP Fact Sheet has been prepared from the best information available at the time of its publication and represents a consensus of the members of the APSP Recreational Water Quality Committee. The APSP makes no guarantee, and assumes no liability, in connection with any of this information. Moreover, it should not be assumed that every acceptable procedure is included, or that special circumstances may not warrant modified or additional procedures. Appropriate steps should be taken to ensure that the information is current when used. -
Synthetically Important Alkalimetal Utility Amides: Lithium, Sodium, And
Angewandte. Reviews R. E. Mulvey and S. D. Robertson DOI: 10.1002/anie.201301837 Alkali-Metal Amides Synthetically Important Alkali-Metal Utility Amides: Lithium, Sodium, and Potassium Hexamethyldisilazides, Diisopropylamides, and Tetramethylpiperidides Robert E. Mulvey* and Stuart D. Robertson* Keywords: alkali metals · heterometallic compounds · molecular structure · secondary amide · solution state Angewandte Chemie 11470 www.angewandte.org 2013 Wiley-VCH Verlag GmbH & Co. KGaA, Weinheim Angew. Chem. Int. Ed. 2013, 52, 11470 – 11487 Angewandte Alkali-Metal Amides for Synthesis Chemie Most synthetic chemists will have at some point utilized a sterically From the Contents À demanding secondary amide (R2N ). The three most important examples, lithium 1,1,1,3,3,3-hexamethyldisilazide (LiHMDS), 1. Introduction 11471 lithium diisopropylamide (LiDA), and lithium 2,2,6,6-tetramethylpi- 2. Preparation and Uses in peridide (LiTMP)—the “utility amides”—have long been indis- Synthesis 11473 pensible particularly for lithiation (Li-H exchange) reactions. Like organolithium compounds, they exhibit aggregation phenomena and 3. Structures of 1,1,1,3,3,3- strong Lewis acidity, and thus appear in distinct forms depending on Hexamethyldisilazides 11475 the solvents employed. The structural chemistry of these compounds as 4. Structures of Diisopropylamide 11477 well as their sodium and potassium congeners are described in the absence or in the presence of the most synthetically significant donor 5. Structures of 2,2,6,6- solvents tetrahydrofuran (THF) and N,N,N,N-tetramethylethylene- Tetramethylpiperidide 11477 diamine (TMEDA) or closely related solvents. Examples of hetero- 6. Heterometallic Derivatives 11479 alkali-metal amides, an increasingly important composition because of the recent escalation of interest in mixed-metal synergic effects, are also 7. -
Geological Evolution of the Red Sea: Historical Background, Review and Synthesis
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/277310102 Geological Evolution of the Red Sea: Historical Background, Review and Synthesis Chapter · January 2015 DOI: 10.1007/978-3-662-45201-1_3 CITATIONS READS 6 911 1 author: William Bosworth Apache Egypt Companies 70 PUBLICATIONS 2,954 CITATIONS SEE PROFILE Some of the authors of this publication are also working on these related projects: Near and Middle East and Eastern Africa: Tectonics, geodynamics, satellite gravimetry, magnetic (airborne and satellite), paleomagnetic reconstructions, thermics, seismics, seismology, 3D gravity- magnetic field modeling, GPS, different transformations and filtering, advanced integrated examination. View project Neotectonics of the Red Sea rift system View project All content following this page was uploaded by William Bosworth on 28 May 2015. The user has requested enhancement of the downloaded file. All in-text references underlined in blue are added to the original document and are linked to publications on ResearchGate, letting you access and read them immediately. Geological Evolution of the Red Sea: Historical Background, Review, and Synthesis William Bosworth Abstract The Red Sea is part of an extensive rift system that includes from south to north the oceanic Sheba Ridge, the Gulf of Aden, the Afar region, the Red Sea, the Gulf of Aqaba, the Gulf of Suez, and the Cairo basalt province. Historical interest in this area has stemmed from many causes with diverse objectives, but it is best known as a potential model for how continental lithosphere first ruptures and then evolves to oceanic spreading, a key segment of the Wilson cycle and plate tectonics.