Mercury Bichloride Iatrogenic Poisoning
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Mercury--Quicksilver
scueu« No. 12 Mineral Technology Series No 6 University of Arizona Bulletin Mercury---Quicksilver By P. E. JOSEPH SECOND ISSUE NOVEMBER, 1916. Entered as second class matter November 2:1, 191~, at the postoftice at Tucson, Arizona. under the Act ot August 24, 1912. Issued weekb". September to Ya)·. PUBLISHED BY THE University of Arizona Bureau of Mines CHARLES F. WILLIS, Director TUCSON, ARIZONA 1916-17 BIBLIOGRAPHY Bancroft, Howland. Notes on the occurrence of cinnabar in central western Arizona. U. S. G. S. Bull. 430, pp. 151-153, 1910. Becker, G. F. Geology of- the quicksilver deposits of the Pacific slope, with atlas. Mon. 13, p. 486, 1888. Only the atlas in stock. Quicksilver Ore Deposits; Mineral Resources U. S. for 1892, pp. 139-168, 1893. Christy, S. B. Quicksilver reduction at New Almaden, Cal. Min- eral Resources U. S. for 1883-1884, pp. 603-636, 1885. Hillebrand, W. F., and Schaller, W. T. Mercury miner-als from Terlingua, Tex. U. S. G. S. Bull. 405, pp. 174, 1909. McCaskey, H. D. Quicksilver in 1912; Mineral Resources U. S. for 1912, Pt. 1, pp. 931-948, 1913. Quicksilver in 1913-Production and Resources; Mineral Resources U. S. for 1913, Pt. 1, pp. 197-212, 1914. Melville, W. H., and Lindgren, Waldemar. Contributions to the mineralogy of the Pacific coast. U. S. G. S. Bull. 61, 30 pp., 1890. Parker, E. W. Quicksilver; Twenty-first Ann. Rept. U. S. G. S., Pt. 6, pp. 273-283, 1901. University of Arizona Bulletin BULLETIN No. 12 SECOND ISSUE, NOVEMBER, 1916 MERCURY-QUICKSILVER By P. -
Mercury and Mercury Compounds
United States Office of Air Quality EPA-454/R-97-012 Environmental Protection Planning And Standards Agency Research Triangle Park, NC 27711 December 1997 AIR EPA LOCATING AND ESTIMATING AIR EMISSIONS FROM SOURCES OF MERCURY AND MERCURY COMPOUNDS L & E EPA-454/R-97-012 Locating And Estimating Air Emissions From Sources of Mercury and Mercury Compounds Office of Air Quality Planning and Standards Office of Air and Radiation U.S. Environmental Protection Agency Research Triangle Park, NC 27711 December 1997 This report has been reviewed by the Office of Air Quality Planning and Standards, U.S. Environmental Protection Agency, and has been approved for publication. Mention of trade names and commercial products does not constitute endorsement or recommendation for use. EPA-454/R-97-012 TABLE OF CONTENTS Section Page EXECUTIVE SUMMARY ................................................ xi 1.0 PURPOSE OF DOCUMENT .............................................. 1-1 2.0 OVERVIEW OF DOCUMENT CONTENTS ................................. 2-1 3.0 BACKGROUND ........................................................ 3-1 3.1 NATURE OF THE POLLUTANT ..................................... 3-1 3.2 OVERVIEW OF PRODUCTION, USE, AND EMISSIONS ................. 3-1 3.2.1 Production .................................................. 3-1 3.2.2 End-Use .................................................... 3-3 3.2.3 Emissions ................................................... 3-6 4.0 EMISSIONS FROM MERCURY PRODUCTION ............................. 4-1 4.1 PRIMARY MERCURY -
The Elements.Pdf
A Periodic Table of the Elements at Los Alamos National Laboratory Los Alamos National Laboratory's Chemistry Division Presents Periodic Table of the Elements A Resource for Elementary, Middle School, and High School Students Click an element for more information: Group** Period 1 18 IA VIIIA 1A 8A 1 2 13 14 15 16 17 2 1 H IIA IIIA IVA VA VIAVIIA He 1.008 2A 3A 4A 5A 6A 7A 4.003 3 4 5 6 7 8 9 10 2 Li Be B C N O F Ne 6.941 9.012 10.81 12.01 14.01 16.00 19.00 20.18 11 12 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 3 Na Mg IIIB IVB VB VIB VIIB ------- VIII IB IIB Al Si P S Cl Ar 22.99 24.31 3B 4B 5B 6B 7B ------- 1B 2B 26.98 28.09 30.97 32.07 35.45 39.95 ------- 8 ------- 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 4 K Ca Sc Ti V Cr Mn Fe Co Ni Cu Zn Ga Ge As Se Br Kr 39.10 40.08 44.96 47.88 50.94 52.00 54.94 55.85 58.47 58.69 63.55 65.39 69.72 72.59 74.92 78.96 79.90 83.80 37 38 39 40 41 42 43 44 45 46 47 48 49 50 51 52 53 54 5 Rb Sr Y Zr NbMo Tc Ru Rh PdAgCd In Sn Sb Te I Xe 85.47 87.62 88.91 91.22 92.91 95.94 (98) 101.1 102.9 106.4 107.9 112.4 114.8 118.7 121.8 127.6 126.9 131.3 55 56 57 72 73 74 75 76 77 78 79 80 81 82 83 84 85 86 6 Cs Ba La* Hf Ta W Re Os Ir Pt AuHg Tl Pb Bi Po At Rn 132.9 137.3 138.9 178.5 180.9 183.9 186.2 190.2 190.2 195.1 197.0 200.5 204.4 207.2 209.0 (210) (210) (222) 87 88 89 104 105 106 107 108 109 110 111 112 114 116 118 7 Fr Ra Ac~RfDb Sg Bh Hs Mt --- --- --- --- --- --- (223) (226) (227) (257) (260) (263) (262) (265) (266) () () () () () () http://pearl1.lanl.gov/periodic/ (1 of 3) [5/17/2001 4:06:20 PM] A Periodic Table of the Elements at Los Alamos National Laboratory 58 59 60 61 62 63 64 65 66 67 68 69 70 71 Lanthanide Series* Ce Pr NdPmSm Eu Gd TbDyHo Er TmYbLu 140.1 140.9 144.2 (147) 150.4 152.0 157.3 158.9 162.5 164.9 167.3 168.9 173.0 175.0 90 91 92 93 94 95 96 97 98 99 100 101 102 103 Actinide Series~ Th Pa U Np Pu AmCmBk Cf Es FmMdNo Lr 232.0 (231) (238) (237) (242) (243) (247) (247) (249) (254) (253) (256) (254) (257) ** Groups are noted by 3 notation conventions. -
Kleinite Hg2n(Cl, SO4)• Nh2o
Kleinite Hg2N(Cl, SO4) • nH2O c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Hexagonal or triclinic. Point Group: 6/m 2/m 2/m. Crystals short prismatic to equant, to 3 mm, showing prominent {1010}, {2021}, and {0001}. Physical Properties: Cleavage: {0001}, uneven; {1010}, imperfect. Tenacity: Brittle. Hardness = 3.5–4 D(meas.) = 7.9–8.0 D(calc.) = [7.87] Optical Properties: Transparent to translucent. Color: Pale yellow, canary-yellow to orange, may be zoned, yellow cores with reddish orange rims; tenebrescent, deepening in color in daylight, the original color restored in darkness; yellow to colorless in transmitted light. Streak: Sulfur-yellow. Luster: Adamantine to greasy. Optical Class: Biaxial (–); uniaxial (+) ≥ 130 ◦C; isotropic ≥∼190 ◦C. Dispersion: r< v,very strong. ω = 2.19 = 2.21 α = 2.16 β = 2.18 γ = 2.18 2V(meas.) = Small to 80◦. Cell Data: Space Group: C6/mmc. a = 13.56 c = 11.13 Z = [18] X-ray Powder Pattern: Terlingua, Texas, USA. 2.914 (10), 2.615 (10), 3.884 (6), 2.013 (6), 1.434 (4), 1.242 (4), 5.228 (2) Chemistry: (1) Hg 85.86 N 2.57 Cl 7.30 H2O 1.03 SO4 3.10 Total 99.86 (1) Terlingua, Texas, USA; averages of numerous partial analyses, corresponds to Hg2.00N0.86 • [Cl0.96(SO4)0.15]Σ=1.11 0.53H2O. Occurrence: In hydrothermal mercury deposits. Association: Terlinguaite, gypsum, barite, calcite, other mercury minerals (Terlingua, Texas, USA); mosesite, calomel, montroydite (McDermitt mine, Nevada, USA). Distribution: In the USA, from Terlingua, Brewster Co., Texas; the New Idria district, San Benito Co., California; and in the McDermitt and Cordero mercury mines, Opalite district, Humboldt Co., Nevada. -
Synthesis and Reactivity of Group 12 Β-Diketiminate Coordination Complexes
Synthesis and Reactivity of Group 12 β-Diketiminate Coordination Complexes By Dylan Webb A thesis Submitted to Victoria University of Wellington in fulfilment of the requirements for the degree of Masters of Science In Chemistry Victoria University of Wellington 2016 Abstract The variable β-diketiminate ligand poses as a suitable chemical environment to explore unknown reactivity and functionality of metal centres. Variants on the β-diketiminate ligand can provide appropriate steric and electronic stabilization to synthesize a range of β-diketiminate group 12 metal complexes. This project aimed to explore various β-diketiminate ligands as appropriate ancillary ligands to derivatise group 12 element complexes and investigate their reactivity. i A β-diketiminato-mercury(II) chloride, [o-C6H4{C(CH3)=N-2,6- Pr2C6H3}{NH(2,6- i i Pr2C6H3)}]HgCl, was synthesized by addition of [o-C6H4{C(CH3)=N-2,6- Pr2C6H3}{NH(2,6- i Pr2C6H3)}]Li to mercury dichloride. Attempts to derivatise the β-diketiminato-mercury(II) chloride using salt metathesis reactions were unsuccessful with only β-diketiminate ligand degradation products being observed in the 1H NMR. i A β-diketiminato-cadmium chloride, [CH{(CH3)CN-2,6- Pr2C6H3}2]CdCl, was derivatized to a i β-diketiminato-cadmium phosphanide, [CH{(CH3)CN-2,6- Pr2C6H3}2]Cd P(C6H11)2, via a lithium dicyclohexyl phosphanide and a novel β-diketiminato-cadmium hydride, [CH{(CH3)CN-2,6- i Pr2C6H3}2]CdH, via Super Hydride. Initial reactivity studies of the novel cadmium hydride with various carbodiimides yielded a β-diketiminato-homonuclear cadmium-cadmium i dimer, [CH{(CH3)CN-2,6- Pr2C6H3}2Cd]2, which formed via catalytic reduction of the cadmium hydride. -
The Mercury Minerals from Terlingua, Texas: Kleinite, Terlinguaite, Eglestonite, Montroydite, Calomel, Mercury.' \V 12
THE MERCURY MINERALS FROM TERLINGUA, TEXAS: KLEINITE, TERLINGUAITE, EGLESTONITE, MONTROYDITE, CALOMEL, MERCURY.' \V 12. HILLEI~RASI)ATI) \V, '? SCHAI.LF::K. In the late fall of 1905 the senior author received for identification from hlr. H. W. Turner, at that time connected with oiie of the mining companies of Terlingua, Texas, specinieiis of two minerals from the well known Terlingua mercury field in Brewster county. Cue of these proved to be the unidentified mineral referred to as So. j by Professor A. J. Moses in his paper' 011 new mercury iniuerals from that district, iianiely terlinguaite, eglestonite and montroydite, the last of these being mercuric oxide, the others oxyclilorides. Preliminary tests having shom~ that So. j belonged to the so-called ii~ercury-niiiiiioniuiii compounds, hitherto unknown in nature, a lirief announcenieiit' of this fact was made in order to secure the field for as full an in~estigatioii of this unique mineral and its associates :is the matt-rial on liaiid and to be ob- tained might permit. This work lias been conducted at intervals during the past eighteen months, and is yet iiicoinplete with reference to the new mineral. It has, however, extended over so long a time and the chances for obtain- ing more perfect material than that already available are so slight, that it is deemed inadvisable to longer delay publication of tlie results ob- tained. The full details of the work herein suniiiiarized nil1 be found in a bulletin of the C. S. Geological Survey, tlie appearance of wliicli will unfortunately be delayed still longer, chiefly on accomit of the plates that are to illustrate it and the unavoidable delays attending publication. -
Neiman Thesis Final Version
UCLA UCLA Electronic Theses and Dissertations Title Cinnabar Alteration in Archaeological Wall Paintings: An Experimental and Theoretical Approach Permalink https://escholarship.org/uc/item/8f1260dn Author Neiman, Madeleine Publication Date 2014 Peer reviewed|Thesis/dissertation eScholarship.org Powered by the California Digital Library University of California UNIVERSITY OF CALIFORNIA Los Angeles Cinnabar Alteration in Archaeological Wall Paintings: An Experimental and Theoretical Approach A thesis submitted in partial satisfaction of the requirements for the degree Master of Arts in Conservation of Archaeological and Ethnographic Materials by Madeleine Kegelman Neiman 2014 ABSTRACT OF THE THESIS Cinnabar Alteration in Archaeological Wall Paintings: An Experimental and Theoretical Approach by Madeleine Kegelman Neiman Master of Arts in Conservation of Archaeological and Ethnographic Materials University of California, Los Angeles, 2014 Professor Ioanna Kakoulli, Chair The red mineral pigment mercuric sulfide (HgS) was commonly employed in Roman wall paintings. Fresco artists of the period favored this pigment for its striking red color. Upon excavation and exposure to air and light, however, cinnabar pigmented surfaces recovered from archaeological contexts often proved unstable. Mural paintings colored with cinnabar that have been exposed in the open air frequently demonstrate a disfiguring, irreversible darkening of the surface. Traditionally, scholars have attributed this alteration to a light-induced phase change from red α-cinnabar to black β-cinnabar (meta-cinnabar) (Gettens et al. 1972). While this transformation has not been totally excluded, the prevailing view among conservation scientists is that chlorine plays a key role in the darkening process (Spring and Grout 2002, Keune and Boon 2005, Cotte et al. 2006, Cotte et al. -
Elemental Mercury and Inorganic Mercury Compounds : Human Health Aspects
This report contains the collective views of an international group of experts and does not necessarily represent the decisions or the stated policy of the United Nations Environment Programme, the International Labour Organization, or the World Health Organization. Concise International Chemical Assessment Document 50 ELEMENTAL MERCURY AND INORGANIC MERCURY COMPOUNDS: HUMAN HEALTH ASPECTS Please note that the pagination and layout of this web version are not identical to the printed CICAD First draft prepared by Dr J.F. Risher, Agency for Toxic Substances and Disease Registry (ATSDR), Atlanta, Georgia, USA Published under the joint sponsorship of the United Nations Environment Programme, the International Labour Organization, and the World Health Organization, and produced within the framework of the Inter-Organization Programme for the Sound Management of Chemicals. World Health Organization Geneva, 2003 The International Programme on Chemical Safety (IPCS), established in 1980, is a joint venture of the United Nations Environment Programme (UNEP), the International Labour Organiza- tion (ILO), and the World Health Organization (WHO). The overall objectives of the IPCS are to establish the scientific basis for assessment of the risk to human health and the environment from exposure to chemicals, through international peer review processes, as a prerequisite for the promo- tion of chemical safety, and to provide technical assistance in strengthening national capacities for the sound management of chemicals. The Inter-Organization Programme for the Sound Management of Chemicals (IOMC) was established in 1995 by UNEP, ILO, the Food and Agriculture Organization of the United Nations, WHO, the United Nations Industrial Development Organization, the United Nations Institute for Training and Research, and the Organisation for Economic Co-operation and Development (Partici- pating Organizations), following recommendations made by the 1992 UN Conference on Environ- ment and Development to strengthen cooperation and increase coordination in the field of chemical safety. -
Isotopic Variability of Mercury in Ore, Mine-Waste Calcine, and Leachates of Mine-Waste Calcine from Areas Mined for Mercury
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by PubMed Central Environ. Sci. Technol. 2009, 43, 7331–7336 Cinnabar (hexagonal, HgS) is the dominant Hg-bearing Isotopic Variability of Mercury in ore mineral in Hg mines worldwide, although minor ore Ore, Mine-Waste Calcine, and minerals such as elemental Hg (Hg0), metacinnabar, (iso- metric HgS, metastable relative to cinnabar), calomel (Hg2Cl2), · Leachates of Mine-Waste Calcine kleinite (Hg2N(Cl,SO4) n(H2O)), montroydite (HgO), and terlinguaite (Hg+Hg2+ClO)) are found in some deposits from Areas Mined for Mercury (7-10). Extraction of Hg during mining is generally carried out in a retort or a rotary furnace where Hg ore is heated to 0 ,† ‡ 600-700 °C, which converts cinnabar to elemental Hg , the SARAH J. STETSON,* JOHN E. GRAY, - RICHARD B. WANTY,‡ AND final Hg product that is sold commercially (6, 9, 11 13). DONALD L. MACALADY† Retorting of Hg-bearing ore is known to be an incomplete process, and as a result, calcine found at most Hg mines Colorado School of Mines, Department of Chemistry and 0 Geochemistry, 1500 Illinois St, Golden, Colorado 80401, contains unconverted cinnabar, elemental Hg , metacinna- and U.S. Geological Survey. P.O. Box 25046, bar, and other ionic Hg byproduct compounds formed during Denver, Colorado 80225 ore retorting (5, 7). One consequence of Hg mining is that considerable calcine is generated during ore processing and this calcine is typically discarded on the surface at mined Received March 5, 2009. Revised manuscript received June sites. Even after many years of inactivity, Hg mining areas 17, 2009. -
Mercury (Hg) Mineral Evolution: a Mineralogical Record of Supercontinent Assembly, Changing Ocean Geochemistry, and the Emerging Terrestrial Biosphere
American Mineralogist, Volume 97, pages 1013–1042, 2012 Mercury (Hg) mineral evolution: A mineralogical record of supercontinent assembly, changing ocean geochemistry, and the emerging terrestrial biosphere ROBERT M. HAZEN,1,* JOSHUA GOLDEN,2 ROBERT T. DOWNS,2 GRETHE HYSTAD,3 EDWARD S. GREW,4 DAVID AZZOLINI,5 AND DIMITRI A. SVERJENSKY1,5 1Geophysical Laboratory, Carnegie Institution, 5251 Broad Branch Road NW, Washington, D.C. 20015, U.S.A. 2Department of Geosciences, University of Arizona, 1040 East 4th Street, Tucson, Arizona 85721-0077, U.S.A. 3Department of Mathematics, University of Arizona, Tucson, Arizona 85721-0089, U.S.A. 4Department of Earth Sciences, University of Maine, Orono, Maine 04469, U.S.A. 5Department of Earth and Planetary Sciences, Johns Hopkins University, Baltimore, Maryland 21218, U.S.A. ABSTRACT Analyses of the temporal and geographic distribution of earliest recorded appearances of the 88 IMA-approved mercury minerals plus two potentially valid species exemplify principles of mineral evolution. Metacinnabar (HgS) and native Hg are the only two species reported from meteorites, specifically, the primitive H3 Tieschitz chondrite with an age of 4550 Ma. Since the first terrestrial appearance of cinnabar more than 3 billion years ago, mercury minerals have been present continu- ously at or near Earth’s surface. Mercury mineral evolution is characterized by episodic deposition and diversification, perhaps associated with the supercontinent cycle. We observe statistically significant increases in the number of reported Hg mineral localities and new Hg species at ~2.8–2.6, ~1.9–1.8, and ~0.43–0.25 Ga— intervals that correlate with episodes of presumed supercontinent assembly and associated orogenies of Kenorland (Superia), Columbia (Nuna), and Pangea, respectively. -
Calomel Hgcl C 2001-2005 Mineral Data Publishing, Version 1
Calomel HgCl c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Tetragonal. Point Group: 4/m 2/m 2/m. Of variable and complex habit; crystals commonly tabular on {001}, prismatic k [001], equant pyramidal, to 1 cm; in drusy crusts, earthy, massive. Twinning: On {112}, contact and penetration twins, may be repeated. Physical Properties: Cleavage: Good on {110}, uneven; imperfect on {011}. Fracture: Conchoidal. Tenacity: Sectile, plastic. Hardness = 1.5 D(meas.) = 7.15 D(calc.) = 7.23 Fluoresces brick-red under UV. Optical Properties: Transparent to translucent. Color: Colorless, white, ash-gray, yellowish gray, brown, color deepening on exposure to light; colorless in transmitted light. Streak: Pale yellowish white. Luster: Adamantine. Optical Class: Uniaxial (+). Pleochroism: Weak. Absorption: E > O. ω = 1.973 = 2.656 Cell Data: Space Group: I4/mmm (synthetic). a = 4.4795(5) c = 10.9054(9) Z = 4 X-ray Powder Pattern: Synthetic. 3.170 (100), 4.15 (75), 2.067 (40), 2.727 (30), 1.962 (30), 1.970 (16), 2.824 (12) Chemistry: Analyses of natural material are not available. Polymorphism & Series: Forms a series with kuzminite. Occurrence: An uncommon secondary mineral formed through the alteration of other mercury minerals. Association: Mercury, amalgam, cinnabar, mercurian tetrahedrite, eglestonite, terlinguaite, montroydite, kleinite, moschelite, kadyrelite, kuzminite, chursinite, kelyanite, calcite, “limonite”, clay minerals. Distribution: From Moschellandsberg [ck?? Landsberg, near Obermoschel??], Rhineland- Palatinate, Germany [TL]. At Alva, Serbia. Large crystals from Almad´en,Ciudad Real Province, Spain. Found near Montpellier, H´erault,France. In England, at the Chatsworth mine, Grassington Moor, Yorkshire. From the Kadyrel deposit, Tuva, Siberia, Russia. -
Understanding of Chemical Reactions Involved in Pigment Discoloration, in Particular in Mercury Sulfide (Hgs) Blackening Marie Radepont
Understanding of chemical reactions involved in pigment discoloration, in particular in mercury sulfide (HgS) blackening Marie Radepont To cite this version: Marie Radepont. Understanding of chemical reactions involved in pigment discoloration, in particular in mercury sulfide (HgS) blackening. Analytical chemistry. Université Pierre et Marie Curie -Paris VI, 2013. English. tel-00805147v1 HAL Id: tel-00805147 https://tel.archives-ouvertes.fr/tel-00805147v1 Submitted on 28 Mar 2013 (v1), last revised 28 Dec 2014 (v2) HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Universiteit Antwerpen LAMS UMR 8220 CNRS Université Pierre et Marie Curie City Campus UPMC Site « Le Raphaël » 4 place Jussieu Prinsstraat 13 3 rue Galilée 75005 Paris Cedex 05 2000 Antwerpen 94200 Ivry-sur-Seine FRANCE BELGIUM FRANCE Understanding of chemical reactions involved in pigment discoloration, in particular in mercury sulfide (HgS) blackening PhD defended by Marie RADEPONT Antwerp, 2013 To obtain the degree of: Doctor in de wetenschappen: chemie (Universiteit Antwerpen) D U P Mrie Curie (Ecole doctorale ED397 Physique et chimie des matériaux) Promoters : Prof. Koen JANSSENS Dr. Marine COTTE Professor of Analytical Chemistry Beamline scientist University of Antwerp, Belgium ESRF, Grenoble, France CNRS Researcher LAMS UMR8220, Ivry-sur-Seine, France Composition of the jury : Dr.