Provisional Guidance on Use of Chemical Categories
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1 the Volumetric Determination of Hydroxylamine
VOLUMETRIC DETERMINATION OF HYDROXYLAMINE. I363 [CONTRIBUTION FROM THE CHEMICAL LABORATORYOF THE UNIVERSITY OF CALIFORNIA.1 THE VOLUMETRIC DETERMINATION OF HYDROXYLAMINE. BY WILLIAMC. BRAY,MIBUM E. SIMPSONAND ANNA A. MACKENZIE. Received July 17, 1919 In the present investigation 3 volumetric methods of determining hydroxylamine in aqueous solution have been studied : The titanous salt method,' in which the hydroxylamine is reduced by excess titanous salt in acid solution with exclusion of air, and the excess titrated with permanganate. 2NH20H + Ti2(S04)3 = (NH4)2S04 + 4TiOS04 + HzS04. (I) The ferric salt method,2 in which the hydroxylamine is oxidized in an acid solution by excess of a ferric salt, the mixture is boiled and the fer- rous salt formed titrated with permanganate. 2NH20H + 2Fe@04)3 = N2O + 4FeS04 + 2H2S04 + H20. (2) The iodine method,3 in which the hydroxylamine is oxidized by iodine in a neutral solution, e. g., in the presence of disodium phosphate. 2NH20H + 212 = N2O + 4HI + H2O (3) or 2NH20H + 213- = N20 + 61- + 4H+ + HzO. Our first experiments, with the iodine method, yielded irregular results which could not be interpreted until the concentration of the hydroxyl- amine solution was accurately determined. An examination of the literature showed a rather unsatisfactory state of affairs. The advocates of the ferric sulfate method furnish evidence that it is perfectly reliable, but Leuba4 gives detailed experimental data to prove the contrary, and Adams5 states that he could not obtain reproducible results with it. The investigators who have used the iodine method consider it to be fairly satisfactory, but some of them state that it is not very accurate, and Rupp and Maeder6 have recently concluded that correct results are obtained only by a compensation of errors. -
Landolt-Börnstein Indexes of Organic Compounds Subvolumes A-I by V
Landolt-Börnstein Indexes of Organic Compounds Subvolumes A-I By V. Vill, C. Bauhofer, G. Peters, H. Sajus, P. Weigner, LCI-Publisher and Chemistry Department of the University of Hamburg All printed index material has been used to build up the comprehensive Scidex database index developed by LCI Publisher GmbH, Hamburg For further information please visit www.lci-publisher.com From this database a CD-ROM and two online versions were derived. The first is attached to each of the printed subvolumes and the latter are offered for free use at the following addresses: Scidex Database online with graphical structure search on http://lb.chemie.uni-hamburg.de/ Or the easy to use html version on http://lb.chemie.uni-hamburg.de/static/ Landolt-Börnstein Numerical Data and Functional Relationships in Science and Technology New Series / Editor in Chief: W. Martienssen Index of Organic Compounds Subvolume A Compounds with 1 to 7 Carbon Atoms Editor: V. Vill Authors: V. Vill, G. Peters, H. Sajus 1 3 ISBN 3-540-66203-0 Springer-Verlag Berlin Heidelberg New York Library of Congress Cataloging in Publication Data Zahlenwerte und Funktionen aus Naturwissenschaften und Technik, Neue Serie Editor in Chief: W. Martienssen Index of Organic Compounds A: Editor: V. Vill At head of title: Landolt-Börnstein. Added t.p.: Numerical data and functional relationships in science and technology. Tables chiefly in English. Intended to supersede the Physikalisch-chemische Tabellen by H. Landolt and R. Börnstein of which the 6th ed. began publication in 1950 under title: Zahlenwerte und Funktionen aus Physik, Chemie, Astronomie, Geophysik und Technik. -
Polymetallic Mineralization in Ediacaran Sediments in the Żarki-Kotowice Area, Poland
MINERALOGIA, 43, No 3-4: 199-212 (2012) DOI: 10.2478/v10002-012-0008-0 www.Mineralogia.pl MINERALOGICAL SOCIETY OF POLAND POLSKIE TOWARZYSTWO MINERALOGICZNE __________________________________________________________________________________________________________________________ Original paper Polymetallic mineralization in Ediacaran sediments in the Żarki-Kotowice area, Poland Łukasz KARWOWSKI1*, Marek MARKOWIAK2 1University of Silesia, Faculty of Earth Sciences, ul. Będzińska 60, 41-200 Sosnowiec, Poland; e-mail: [email protected] 2Polish Geological Institute - Research and Development Unit, Upper Silesian Branch, ul. Królowej Jadwigi 1, 41-200 Sosnowiec, Poland; e-mail: [email protected] * Corresponding author Received: September 5, 2012 Received in revised form: February 20, 2013 Accepted: March 17, 2013 Available online: March 30, 2013 Abstract. In one small mineral vein in core from borehole 144-Ż in the Żarki-Kotowice area, almost all of the ore minerals known from related deposits in the vicinity occur. Some of the minerals in the vein described in this paper, namely, nickeline, hessite, native silver and minerals of the cobaltite-gersdorffite group, have not previously been reported from elsewhere in the Kraków-Lubliniec tectonic zone. The identified minerals are chalcopyrite, pyrite, marcasite, sphalerite, Co-rich pyrite, tennantite, tetrahedrite, bornite, galena, magnetite, hematite, cassiterite, pyrrhotite, wolframite (ferberite), scheelite, molybdenite, nickeline, minerals of the cobaltite- gersdorffite group, carrollite, hessite and native silver. Moreover, native bismuth, bismuthinite, a Cu- and Ag-rich sulfosalt of Bi (cuprobismutite) and Ni-rich pyrite also occur in the vein. We suggest that, the ore mineralization from the borehole probably reflects post-magmatic hydrothermal activity related to an unseen granitic intrusion located under the Mesozoic sediments in the Żarki-Pilica area. -
A Fundamental Evaluation of the Atmospheric Pre-Leaching Section of the Nickel-Copper Matte Treatment Process
A FUNDAMENTAL EVALUATION OF THE ATMOSPHERIC PRE-LEACHING SECTION OF THE NICKEL-COPPER MATTE TREATMENT PROCESS by RODRICK MULENGA LAMYA Dissertation presented for the Degree of DOCTOR OF PHILOSOPHY (Extractive Metallurgical Engineering) in the Department of Process Engineering at the University of Stellenbosch, South Africa Promoter Prof. L. Lorenzen STELLENBOSCH March 2007 DECLARATION I the undersigned, hereby declare that the work contained in this dissertation is my own original work and that I have not previously in its entirety or in part submitted it at any university for a degree. Signature: ............................................... Date: ....................................................... Copyright © 2007 Stellenbosch University All rights reserved i SYNOPSIS Nickel-Copper sulphide ores are the most important Platinum Group Metal bearing ores. The South African deposits are exceptionally rich in the platinum group metals (PGMs) and production of the PGMs is the primary purpose of treating these ores. The methods used in the recovery of the PGMs from the nickel-copper ores generally consists of ore concentration by physical techniques, pyrometallurgical concentration and hydrometallurgical extraction of the base metals followed by the PGMs. Pyrometallurgical concentration produces Ni-Cu matte, which is treated by hydrometallurgical processes to recover the nickel, copper, cobalt and the precious metals. In this study, the leaching behaviour of a Ni–Cu matte in CuSO4–H2SO4 solution during the repulping (pre-leach) stage at Impala Platinum Refineries was studied. The repulping stage is basically a non–oxidative atmospheric leach stage, in which nickel, iron and cobalt are partially dissolved, while the copper is precipitated. To understand the nature of the leaching process during this stage of the base metal refining operation, the effects of variations in the key process variables such as temperature, stirring rate, particle size, pulp density, residence time, initial copper and acid concentrations were investigated. -
Structures and Reaction Mechanisms of Organocuprate Clusters in Organic Chemistry
REVIEWS Wherefore Art Thou Copper? Structures and Reaction Mechanisms of Organocuprate Clusters in Organic Chemistry Eiichi Nakamura* and Seiji Mori Organocopper reagents provide the principles. This review will summarize example of molecular recognition and most general synthetic tools in organic first the general structural features of supramolecular chemistry, which chemistry for nucleophilic delivery of organocopper compounds and the pre- chemists have long exploited without hard carbanions to electrophilic car- vious mechanistic arguments, and then knowing it. Reasoning about the bon centers. A number of structural describe the most recent mechanistic uniqueness of the copper atom among and mechanistic studies have been pictures obtained through high-level neighboring metal elements in the reported and have led to a wide variety quantum mechanical calculations for periodic table will be presented. of mechanistic proposals, some of three typical organocuprate reactions, which might even be contradictory to carbocupration, conjugate addition, Keywords: catalysis ´ conjugate addi- others. With the recent advent of and SN2 alkylation. The unified view tions ´ copper ´ density functional physical and theoretical methodolo- on the nucleophilic reactivities of met- calculations ´ supramolecular chemis- gies, the accumulated knowledge on al organocuprate clusters thus ob- try organocopper chemistry is being put tained has indicated that organocup- together into a few major mechanistic rate chemistry represents an intricate 1. Introduction 1 R Cu X The desire to learn about the nature of elements has been R or R1 R and will remain a main concern of chemists. In this review, we R Cu will consider what properties of copper make organocopper R1 chemistry so useful in organic chemistry. -
Nickeline Nias C 2001-2005 Mineral Data Publishing, Version 1
Nickeline NiAs c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Hexagonal. Point Group: 6/m 2/m 2/m. Commonly in granular aggregates, reniform masses with radial structure, and reticulated and arborescent growths. Rarely as distorted, horizontally striated, {1011} terminated crystals, to 1.5 cm. Twinning: On {1011} producing fourlings; possibly on {3141}. Physical Properties: Fracture: Conchoidal. Tenacity: Brittle. Hardness = 5–5.5 VHN = n.d. D(meas.) = 7.784 D(calc.) = 7.834 Optical Properties: Opaque. Color: Pale copper-red, tarnishes gray to blackish; white with strong yellowish pink hue in reflected light. Streak: Pale brownish black. Luster: Metallic. Pleochroism: Strong; whitish, yellow-pink to pale brownish pink. Anisotropism: Very strong, pale greenish yellow to slate-gray in air. R1–R2: (400) 39.2–45.4, (420) 38.0–44.2, (440) 36.8–43.5, (460) 36.2–43.2, (480) 37.2–44.3, (500) 39.6–46.4, (520) 42.3–48.6, (540) 45.3–50.7, (560) 48.2–52.8, (580) 51.0–54.8, (600) 53.7–56.7, (620) 55.9–58.4, (640) 57.8–59.9, (660) 59.4–61.3, (680) 61.0–62.5, (700) 62.2–63.6 Cell Data: Space Group: P 63/mmc. a = 3.621(1) c = 5.042(1) Z = 2 X-ray Powder Pattern: Unknown locality. 2.66 (100), 1.961 (90), 1.811 (80), 1.071 (40), 1.328 (30), 1.033 (30), 0.821 (30) Chemistry: (1) (2) Ni 43.2 43.93 Co 0.4 Fe 0.2 As 55.9 56.07 Sb 0.1 S 0.1 Total 99.9 100.00 (1) J´achymov, Czech Republic; by electron microprobe, corresponds to (Ni0.98Co0.01 Fe0.01)Σ=1.00As1.00. -
APPENDIX G Acid Dissociation Constants
harxxxxx_App-G.qxd 3/8/10 1:34 PM Page AP11 APPENDIX G Acid Dissociation Constants § ϭ 0.1 M 0 ؍ (Ionic strength ( † ‡ † Name Structure* pKa Ka pKa ϫ Ϫ5 Acetic acid CH3CO2H 4.756 1.75 10 4.56 (ethanoic acid) N ϩ H3 ϫ Ϫ3 Alanine CHCH3 2.344 (CO2H) 4.53 10 2.33 ϫ Ϫ10 9.868 (NH3) 1.36 10 9.71 CO2H ϩ Ϫ5 Aminobenzene NH3 4.601 2.51 ϫ 10 4.64 (aniline) ϪO SNϩ Ϫ4 4-Aminobenzenesulfonic acid 3 H3 3.232 5.86 ϫ 10 3.01 (sulfanilic acid) ϩ NH3 ϫ Ϫ3 2-Aminobenzoic acid 2.08 (CO2H) 8.3 10 2.01 ϫ Ϫ5 (anthranilic acid) 4.96 (NH3) 1.10 10 4.78 CO2H ϩ 2-Aminoethanethiol HSCH2CH2NH3 —— 8.21 (SH) (2-mercaptoethylamine) —— 10.73 (NH3) ϩ ϫ Ϫ10 2-Aminoethanol HOCH2CH2NH3 9.498 3.18 10 9.52 (ethanolamine) O H ϫ Ϫ5 4.70 (NH3) (20°) 2.0 10 4.74 2-Aminophenol Ϫ 9.97 (OH) (20°) 1.05 ϫ 10 10 9.87 ϩ NH3 ϩ ϫ Ϫ10 Ammonia NH4 9.245 5.69 10 9.26 N ϩ H3 N ϩ H2 ϫ Ϫ2 1.823 (CO2H) 1.50 10 2.03 CHCH CH CH NHC ϫ Ϫ9 Arginine 2 2 2 8.991 (NH3) 1.02 10 9.00 NH —— (NH2) —— (12.1) CO2H 2 O Ϫ 2.24 5.8 ϫ 10 3 2.15 Ϫ Arsenic acid HO As OH 6.96 1.10 ϫ 10 7 6.65 Ϫ (hydrogen arsenate) (11.50) 3.2 ϫ 10 12 (11.18) OH ϫ Ϫ10 Arsenious acid As(OH)3 9.29 5.1 10 9.14 (hydrogen arsenite) N ϩ O H3 Asparagine CHCH2CNH2 —— —— 2.16 (CO2H) —— —— 8.73 (NH3) CO2H *Each acid is written in its protonated form. -
The Gersdorffite-Bismuthinite-Native Gold Association and the Skarn
minerals Article The Gersdorffite-Bismuthinite-Native Gold Association and the Skarn-Porphyry Mineralization in the Kamariza Mining District, Lavrion, Greece † Panagiotis Voudouris 1,* , Constantinos Mavrogonatos 1 , Branko Rieck 2, Uwe Kolitsch 2,3, Paul G. Spry 4 , Christophe Scheffer 5, Alexandre Tarantola 6 , Olivier Vanderhaeghe 7, Emmanouil Galanos 1, Vasilios Melfos 8 , Stefanos Zaimis 9, Konstantinos Soukis 1 and Adonis Photiades 10 1 Department of Geology & Geoenvironment, National and Kapodistrian University of Athens, 15784 Athens, Greece; [email protected] (C.M.); [email protected] (E.G.); [email protected] (K.S.) 2 Institut für Mineralogie und Kristallographie, Universität Wien, 1090 Wien, Austria; [email protected] 3 Mineralogisch-Petrographische Abteilung, Naturhistorisches Museum, 1010 Wien, Austria; [email protected] 4 Department of Geological and Atmospheric Sciences, Iowa State University, Ames, IA 50011, USA; [email protected] 5 Département de Géologie et de Génie Géologique, Université Laval, Québec, QC G1V 0A6, Canada; [email protected] 6 Université de Lorraine, CNRS, GeoRessources UMR 7359, Faculté des Sciences et Technologies, F-54506 Vandoeuvre-lès-Nancy, France; [email protected] 7 Université de Toulouse, Géosciences Environnement Toulouse (GET), UMR 5563 CNRS, F-31400 Toulouse, France; [email protected] 8 Department of Mineralogy-Petrology-Economic Geology, Faculty of Geology, Aristotle University of Thessaloniki, 54124 Thessaloniki, Greece; [email protected] 9 Institut für Mineralogie, TU Bergakademie Freiberg, 09599 Freiberg, Germany; [email protected] 10 Institute of Geology and Mineral Exploration (I.G.M.E.), 13677 Acharnae, Greece; [email protected] * Correspondence: [email protected]; Tel.: +30-210-7274129 † The paper is an extended version of our paper published in 1st International Electronic Conference on Mineral Science. -
Mechanistic Considerations on the Hydrodechlorination Process of Polychloroarenes
Chapter 3 Mechanistic Considerations on the Hydrodechlorination Process of Polychloroarenes YoshiharuYoshiharu Mitoma, Mitoma, Yumi KatayamaYumi Katayama andand CristianCristian Simion Simion Additional information is available at the end of the chapter http://dx.doi.org/10.5772/intechopen.79083 Abstract Defunctionalization of organochlorines through reductive dechlorination (also known as hydrodechlorination—replacement of chlorine atoms by hydrogen—is one of the main methodologies used in the detoxification of these harmful compounds. Most of the pub- lished papers on this particular matter focused on specific reagents, reaction conditions, and mainly result efficiency. Some of the authors were also concerned with reaction -path ways (e.g., the order in which chlorine atoms were removed from a polychlorinated aro- matic substrate—polychlorinated biphenyls, PCBs; polychlorinated dibenzo-p-dioxins, PCDDs; or polychlorinated dibenzofurans, PCDFs). However, the papers that dealt with the investigation of reaction mechanism were rather scarce. This chapter presents the advances made by researchers in understanding, from a mechanistic point of view, the hydrodechlorination process, along with our own assumptions. In doing so, it would be easier to predict the behavior of such compounds in a specific environment, showing more clearly the scope and limitations of each process, depending on the reaction condi- tions and reagents. Keywords: hydrodechlorination, reaction mechanism, metal/hydrogen donor 1. Introduction Most chlorinated and especially polychlorinated arenes (such as polychloro-dibenzo-p-diox- ins 1, polychloro-dibenzofurans 2, or polychlorobiphenyls 3) are persistent organic pollutants (POPs) that are harmful to both man and the environment [1–5]. © 2016 The Author(s). Licensee InTech. This chapter is distributed under the terms of the Creative Commons © 2018 The Author(s). -
A Comparative Study of Nickel Sulphide Deposits Within the Area of the Canadian Shield
Wilfrid Laurier University Scholars Commons @ Laurier Theses and Dissertations (Comprehensive) 1970 A Comparative Study of Nickel Sulphide Deposits Within the Area of the Canadian Shield Robert G. Kreiner Wilfrid Laurier University Follow this and additional works at: https://scholars.wlu.ca/etd Part of the Geology Commons, and the Physical and Environmental Geography Commons Recommended Citation Kreiner, Robert G., "A Comparative Study of Nickel Sulphide Deposits Within the Area of the Canadian Shield" (1970). Theses and Dissertations (Comprehensive). 1528. https://scholars.wlu.ca/etd/1528 This Thesis is brought to you for free and open access by Scholars Commons @ Laurier. It has been accepted for inclusion in Theses and Dissertations (Comprehensive) by an authorized administrator of Scholars Commons @ Laurier. For more information, please contact [email protected]. A COMPARATIVE STUDY OF NICKEL SULPHIDE DEPOSITS WITHIN THE AREA OF THE CANADIAN SHIELD BY Robert G. Kreiner Submitted in partial fulfillment of the requirements for theM.A. Degree in Geography Faculty of Graduate Studies Waterloo Lutheran University Waterloo, Ontario 1970 Property ii i,\j Library Waterloo University College UMI Number: EC56498 All rights reserved INFORMATION TO ALL USERS The quality of this reproduction is dependent on the quality of the copy submitted. In the unlikely event that the author did not send a complete manuscript and there are missing pages, these will be noted. Also, if material had to be removed, a note will indicate the deletion. UMI EC56498 Copyright 2012 by ProQuest LLC. All rights reserved. This edition of the work is protected against unauthorized copying under Title 17, United States Code. -
Why Nature Chose Selenium Hans J
Reviews pubs.acs.org/acschemicalbiology Why Nature Chose Selenium Hans J. Reich*, ‡ and Robert J. Hondal*,† † University of Vermont, Department of Biochemistry, 89 Beaumont Ave, Given Laboratory, Room B413, Burlington, Vermont 05405, United States ‡ University of WisconsinMadison, Department of Chemistry, 1101 University Avenue, Madison, Wisconsin 53706, United States ABSTRACT: The authors were asked by the Editors of ACS Chemical Biology to write an article titled “Why Nature Chose Selenium” for the occasion of the upcoming bicentennial of the discovery of selenium by the Swedish chemist Jöns Jacob Berzelius in 1817 and styled after the famous work of Frank Westheimer on the biological chemistry of phosphate [Westheimer, F. H. (1987) Why Nature Chose Phosphates, Science 235, 1173−1178]. This work gives a history of the important discoveries of the biological processes that selenium participates in, and a point-by-point comparison of the chemistry of selenium with the atom it replaces in biology, sulfur. This analysis shows that redox chemistry is the largest chemical difference between the two chalcogens. This difference is very large for both one-electron and two-electron redox reactions. Much of this difference is due to the inability of selenium to form π bonds of all types. The outer valence electrons of selenium are also more loosely held than those of sulfur. As a result, selenium is a better nucleophile and will react with reactive oxygen species faster than sulfur, but the resulting lack of π-bond character in the Se−O bond means that the Se-oxide can be much more readily reduced in comparison to S-oxides. -
Neutral, Cationic and Anionic Organonickel and -Palladium Complexes Supported by Cite This: Dalton Trans., 2020, 49, 322 Iminophosphine/Phosphinoenaminato Ligands†‡
Dalton Transactions View Article Online PAPER View Journal | View Issue Neutral, cationic and anionic organonickel and -palladium complexes supported by Cite this: Dalton Trans., 2020, 49, 322 iminophosphine/phosphinoenaminato ligands†‡ Tomás G. Santiago, Carmen Urbaneja, Eleuterio Álvarez, Elena Ávila, Pilar Palma and Juan Cámpora * We report a series of organometallic nickel and palladium complexes containing iminophosphine ligands R2PCH2C(Ph) = N-Dipp (Dipp = 2,6-diisopropylphenyl; R = iPr, La; R = Ph, Lb; and R = o-C6H4OMe, Lc), synthesized by ligand exchange or oxidative addition reactions, and we investigate the capacity of such ligands to undergo reversible deprotonation to the corresponding phosphinoenaminato species. In the attempted ligand exchange reaction of the nickel bis(trimethylsilyl)methyl precursor [Ni(CH2SiMe3)2Py2] with Lb, the iminophosphine acts as a weak acid rather than a neutral ligand, cleaving one of the Ni–C bonds, to afford the phosphinoenaminato complex [Ni(CH2SiMe3)(L’b)(Py)] (L’b = conjugate base of Lb). Creative Commons Attribution-NonCommercial 3.0 Unported Licence. + We disclose a general method for the syntheses of complexes [Ni(CH2SiMe3)(L)(Py)] (L = La, Lb or Lc), and demonstrate that iminophosphine deprotonation is a general feature and occurs reversibly in the coordination sphere of the metal. By studying proton exchange reactions of the cation [Ni(CH2SiMe3)(Lb) (Py)]+ with bases of different strength we show that the conjugate phosphinoenaminato ligand in Received 17th October 2019, [Ni(CH2SiMe3)(L’b)(Py)] is a base with strength comparable to DBU in THF. The acyl group in the function- Accepted 19th November 2019 alized aryl complex [Ni(p-C6H4COCH3)(Br)(La)] does not interfere in the iminophosphine deprotonation with DOI: 10.1039/c9dt04062e − + NaH.