Atacamite Cu2cl(OH)3 C 2001-2005 Mineral Data Publishing, Version 1
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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 -
Final Report FAD-2010-0046 TBCC
EUROPEAN COMMISSION JOINT RESEARCH CENTRE Institute for Reference Materials and Measurements European Union Reference Laboratory for Feed Additives JRC.DG.D.6/CvH/PRO/ag/ARES(2011)473276 EURL Evaluation Report on the Analytical Methods submitted in connection with the Application for the Authorisation of Feed Additives according to Regulation (EC) No 1831/2003 Dossier related to: FAD-2010-0046 CRL/100051 Product Name: Tribasic copper chloride (TBCC) Active Substance(s): Di copper chloride tri hydroxide; crystal form atacamite/paratacamite Rapporteur Laboratory: European Union Reference Laboratory for Feed Additives (EURL-FA) Geel, Belgium Report prepared by: Piotr Robouch (EURL-FA) Report revised by: Gerhard Buttinger (EURL-FA) Date: 02/05/2011 Report approved by: Christoph von Holst Date: 02/05/2011 EURL Evaluation Report on “Di copper chloride tri hydroxide” EXECUTIVE SUMMARY In the current application authorisation is sought under articles 4(1) for Di copper chloride tri hydroxide under the category "nutritional additives", functional group 3(b) "compounds of trace elements", according to the classification system of Annex I of Regulation (EC) No 1831/2003. Authorisation is sought for the use of the feed additive for all animal species and categories. Di copper chloride tri hydroxide (Cu2Cl(OH)3, also called tribasic copper chloride – TBCC) is a pure form of crystalline copper (II) chloride hydroxide containing a minimum of 95 % of a defined ratio of the polymorphs atacamite and paratacamite - equivalent to a minimum content of total copper of 58 %. The feed additive is intended to be incorporated into premixtures and feedingstuffs. The Applicant suggested the following maximum levels of total copper in the feedingstuffs ranging from 10 to 170 mg/kg depending on the species of interest. -
Mineral Processing
Mineral Processing Foundations of theory and practice of minerallurgy 1st English edition JAN DRZYMALA, C. Eng., Ph.D., D.Sc. Member of the Polish Mineral Processing Society Wroclaw University of Technology 2007 Translation: J. Drzymala, A. Swatek Reviewer: A. Luszczkiewicz Published as supplied by the author ©Copyright by Jan Drzymala, Wroclaw 2007 Computer typesetting: Danuta Szyszka Cover design: Danuta Szyszka Cover photo: Sebastian Bożek Oficyna Wydawnicza Politechniki Wrocławskiej Wybrzeze Wyspianskiego 27 50-370 Wroclaw Any part of this publication can be used in any form by any means provided that the usage is acknowledged by the citation: Drzymala, J., Mineral Processing, Foundations of theory and practice of minerallurgy, Oficyna Wydawnicza PWr., 2007, www.ig.pwr.wroc.pl/minproc ISBN 978-83-7493-362-9 Contents Introduction ....................................................................................................................9 Part I Introduction to mineral processing .....................................................................13 1. From the Big Bang to mineral processing................................................................14 1.1. The formation of matter ...................................................................................14 1.2. Elementary particles.........................................................................................16 1.3. Molecules .........................................................................................................18 1.4. Solids................................................................................................................19 -
3, Isostructural with Botallackite
American Mineralogist, Volume 101, pages 986–990, 2016 Crystal structure of a new compound, CuZnCl(OH)3, isostructural with botallackite HEXING YANG1,*, ISABEL F. BARTON2, MARCELO B. ANDRADE1, AND ROBERT T. DOWNS1 1Department of Geosciences, University of Arizona, 1040 E. 4th Street, Tucson, Arizona 85721, U.S.A. 2Lowell Institute for Mineral Resources, University of Arizona, Tucson, Arizona 85721, U.S.A. ABSTRACT A new compound, ideally CuZnCl(OH)3, was found on a metallic mining artifact of copper composition at the Rowley mine, Maricopa County, Arizona, U.S.A., and studied with electron microprobe analysis, single-crystal X-ray diffraction, and Raman spectroscopy. It is isostructural with botallackite [Cu2Cl(OH)3] with space group P21/m and unit-cell parameters a = 5.6883(5), b = 3 6.3908(6), c = 5.5248(5) Å, β = 90.832(2)°, V = 200.82(3) Å . The crystal structure of CuZnCl(OH)3, refined to R1 = 0.018, is characterized by brucite-type octahedral sheets made of two distinct and considerably distorted octahedra, M1 and M2, which are coordinated by (5OH + 1Cl) and (4OH + 2Cl), respectively. The octahedral sheets are parallel to (100) and connected by O–H∙∙∙Cl hydrogen bonding. The major structural difference between CuZnCl(OH)3 and botallackite is the complete replacement of Cu2+ in the highly angle-distorted M1 site by non-Jahn-Teller distorting Zn2+. The CuZnCl(OH)3 compound represents the highest Zn content ever documented for the atacamite group of minerals, in conflict with all previous reports that botallackite (like atacamite) is the most 2+ resistant, of all copper hydroxylchloride Cu2Cl(OH)3 polymorphs, to the substitution of Zn for Cu2+, even in the presence of large excess of Zn2+. -
X-Ray Study and Synthesis of Some Copper-Lead Oxychlorides
This dissertation has been 64—7070 microfilmed exactly as received WINCHELL, Jr., Robert Eugene, 1931- X-RAY STUDY AND SYNTHESIS OF SOME COPPER-LEAD OXYCHLORIDES. The Ohio State University, Ph.D., 1963 M ineralogy University Microfilms, Inc., Ann Arbor, Michigan X-RAY STUDY AND SYNTHESIS OF SOME COPPER-LEAD OXYCHLORIDES DISSERTATION Presented in Partial Fulfillment of the Requirements for the Degree Doctor of Philosopher in the Graduate School of the Ohio State University Robert Eugene W inchell, J r ., B. S ., M. S. The Ohio State University 1963 Approved ty Id viser Department of Mineralogy ACKNOWLEDGMENTS The author wishes to acknowledge the assistance, cooperation and encouragement of a great number of people without whom this thesis could not have been completed. The specimens used in the study of these rare oxychlorides were obtained from a number of sources. Dr. C. S. Hurlbut, Jr. supplied samples of a l l the sp ecies from the c o lle c tio n s o f Harvard U n iversity. Dr. Paul E. Desautels provided additional samples of all the minerals except pseudoboleite from the collections of the United States National Museum. Dr. Raymond Hocart, of the University of Paris, supplied several overgrowths of cumengeite on boleite, which had been given to him by G. Friedel, Dr. S. Grolier, of the St. Etienne School of Mines, St. Etienne, France, provided material that had been available to G. Friedel during his study (Friedel, 1906) of boleite, pseudoboleite, and cumengeite. Dr. S. Caillere provided specimens of boleite, cumengeite and pseudoboleite from the collections of the Paris Museum of Natural History. -
Uranium in Situ Leaching
IAEA-TECDOC-720 Uranium in situ leaching Proceedings Technicala of Committee Meeting held in Vienna, 5-8 October 1992 INTERNATIONAL ATOMIC ENERGY AGENC\ /A Y The IAEA doe t normallsno y maintain stock f reportso thin si s series. However, microfiche copies of these reports can be obtained from IIMIS Clearinghouse International Atomic Energy Agency Wagramerstrasse5 P.O. Box 100 A-1400 Vienna, Austria Orders shoul accompaniee db prepaymeny db f Austriao t n Schillings 100,- in the form of a cheque or in the form of IAEA microfiche service coupons which may be ordered separately from the INIS Clearinghouse. Copies of this IAEA-TECDOC may be obtained from: Nuclear Material Fued san l Cycle Technology Section International Atomic Energy Agency Wagramerstrasse 5 P.O. Box 100 A-1400 Vienna, Austria URANIU SITMN I U LEACHING IAEA, VIENNA, 1993 IAEA-TECDOC-720 ISSN 1011-4289 Printe IAEe th AustriAn y i d b a September 1993 FOREWORD The IAEA's latest published estimates show that nuclear power production worldwide will maintain modest growth well into the next century. These estimates indicate that nuclear energy production will gro averagn wo 1.5y eb % 2.5o t year %pe r worldwide ove nex e decadeso rth tw t s i t I . for this reason that despite the continuing depressed uranium market, the question of uranium supply demand an d remain issun sa e that needaddressee b o st monitoredd dan developmentsw Ne . e du , to the recent entry of the Commonwealth of Independent States and China into the uranium market, increase such a need. -
Structures of the Pseudo-Trigonal Polymorphs of Cu2(OH)3Cl
research papers Acta Crystallographica Section B Structural Structures of the pseudo-trigonal polymorphs of Science Cu2(OH)3Cl ISSN 0108-7681 Received 2 February 2009 Thomas Malcherek* and Jochen The crystal structure of Cu2(OH)3Cl has been determined Schlu¨ter using two natural samples with almost ideal stoichiometry. Accepted 14 April 2009 While one of the samples exhibits a twinned clinoatacamite structure, the other sample is characterized by the appearance Mineralogisch-Petrographisches Institut, Univer- of additional weak diffraction maxima at half integer positions sita¨t Hamburg, Grindelallee 48, D-20146 Hamburg, Germany of h and k. Structure refinement was carried out with the space group P11. The relationship between the triclinic phase, clinoatacamite, paratacamite and the herbertsmithite struc- Correspondence e-mail: ture is discussed in terms of symmetry as a function of Cu [email protected] concentration. 1. Introduction Pure Cu2(OH)3Cl so far has been known to occur in the form of the three polymorphs atacamite, botallackite and clino- atacamite. While atacamite is orthorhombic the other two polymorphs are monoclinic. Another, rhombohedral structure type of Cu2(OH)3Cl (paratacamite) has been described by Fleet (1975), but it is now believed that the rhombohedral substructure of paratacamite has to be stabilized by partial substitution of Zn or Ni for Cu (Jambor et al., 1996) at ambient temperature. The Zn end member of such a solid solution, Cu3Zn(OH)6Cl2, has been described as the mineral herbertsmithite (Braithwaite et al., 2004). Recently Clissold et al. (2007) reported the crystal structure of gillardite, the Ni analogue of herbertsmithite. -
Chemistry of Formation of Lanarkite, Pb2oso 4
SHORT COMMUNICATIONS MINERALOGICAL MAGAZINE, DECEMBER 1982, VOL. 46, PP. 499-501 Chemistry of formation of lanarkite, Pb2OSO 4 W E have recently reported (Humphreys et al., 1980; sion which is at odds with the widespread occur- Abdul-Samad et al., 1982) the free energies of rence of the simple sulphate and the extreme rarity formation of a variety of chloride-bearing minerals of the basic salt, and with aqueous synthetic of Pb(II) and Cu(II) together with carbonate procedures for the preparation of the compound and sulphate species of the same metals includ- (Bode and Voss, 1959), which involve reaction of ing leadhillite, Pb,SO4(COa)2(OH)2, caledonite, angtesite in basic solution. PbsCu2CO3(SO4)3(OH)6, and linarite, (Pb,Cu)2 Kellog and Basu (1960) also determined AG~ for SO4(OH)2. By using suitable phase diagrams it has Pb2OSOa(s) at 298.16 K using the method of proved possible to reconstruct, in part, the chemical univariant equilibria in the system Pb-S-O. They history of the development of some complex obtained a value of -1016.4 kJ mol-1 based on secondary mineral assemblages such as those at literature values for PbO(s), PbS(s), PbSO4(s), and the Mammoth-St. Anthony mine, Tiger, Arizona, SO2(g) and another of - 1019.8 kJ mol- 1 based on and the halide and carbonate suite of the Mendip adjusted values for the above compounds. These Hills, Somerset. two results, for which the error was estimated to A celebrated locality for the three sulphate- be about 4.5 kJ mol-1, seem to be considerably bearing minerals above is the Leadhills-Wanlock- more compatible with observed associations than head district of Scotland (Wilson, 1921; Heddle, the earlier values. -
Volborthite Cu3v2o7(OH)2 • 2H2O C 2001-2005 Mineral Data Publishing, Version 1
Volborthite Cu3V2O7(OH)2 • 2H2O c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Monoclinic, pseudohexagonal. Point Group: 2/m. Typically as rosettelike aggregates of scaly crystals, which may have a hexagonal or triangular outline, to 5 mm. Physical Properties: Cleavage: One, perfect. Hardness = 3.5 D(meas.) = 3.5–3.8 D(calc.) = 3.52 Optical Properties: Semitransparent. Color: Dark olive-green, green, yellowish green; green to yellowish green in transmitted light. Luster: Vitreous, oily, resinous, waxy, pearly on the cleavage. Optical Class: Biaxial (–) or biaxial (+). Pleochroism: Faint. Dispersion: r<v,r>v, inclined. α = 1.820–2.01 β = 1.835–2.05 γ = 1.92–2.07 2V(meas.) = 63◦–83◦ Cell Data: Space Group: C2/m. a = 10.610(2) b = 5.866(1) c = 7.208(1) β =95.04(2)◦ Z=2 X-ray Powder Pattern: Monument No. 1 mine, Arizona, USA. 7.16 (10), 2.643 (7), 2.571 (7), 2.389 (7), 4.103 (5), 3.090 (5), 2.998 (5) Chemistry: (1) (2) (1) (2) V2O5 36.65 38.32 CuO 48.79 50.29 SiO2 1.37 H2O [11.49] 11.39 V2O3 1.70 Total [100.00] 100.00 (1) Scrava mine, Italy; by electron microprobe; V2O3 assumed for charge balance, H2Oby 5+ 3+ • • difference; corresponds to Cu2.89V1.90V0.11Si0.11O7(OH)2 2H2O. (2) Cu3V2O7(OH)2 2H2O. Occurrence: An uncommon secondary mineral in the oxidized zone of vanadium-bearing hydrothermal mineral deposits. Association: Brochantite, malachite, atacamite, tangeite, chrysocolla, barite, gypsum. Distribution: In Russia, originally from an unknown locality; later identified at the Sofronovskii copper mine, near Perm, and at Syssersk and Nizhni Tagil, Ural Mountains. -
Clinoailacamite, a NEW POLYMORPH of Gur(Ohl3cl, and ITS Relaflonship to PARATACAMITE and 'ANARAKITE"*
61. Tlrc Catwdian M ineral ogi st Vol. 34, pp.6lJ2 (1996) CLINOAilACAMITE,A NEW POLYMORPHOF Gur(OHl3Cl, AND ITS RELAflONSHIPTO PARATACAMITEAND 'ANARAKITE"* JOHNL. JAMBOR Department of Earth Sciences, University of Waterlao, Waterloo, Ontario N2L 3GI JOHNE. DUTRZAC CANMET,Deparnnent of Naaral ResourcesCananq 555 Booth Street, Ottawa, Ontaria KIA OGj ANDREW C. ROBERTS GeologicalSurvey of Cananq601 Booth Street, Otawa" Owaria KIA 088 JOELD. GRICE ResearchDivisiou CatadianMuseurn of Naure, Ottatva,Ontaria KIP 6P4 JANT. SZYMA(SKI CANMET,Depamnent of NaturalResources Canad4 555 Booth Street, Ottawo" Ontario KIA 0GI ABSTRA T The new mineral clinoatacamiteis a polmorph of Cu2(OII)3C| othen are botallackite (monoclinic), atacamite(ortho- rhornbic),an{ possiblyparatacamite (rhombohedral). Clinoatacanite is monoclinic, spacegroup P21ln,a 6.157(2),b 6.814Q), c 9.104(5) A, p 99.65(4)", which is transformableto a pseudorhombohedralcell approximating that of paxatacamite. Clinoatacamitehas been found in specimensfrom severallocalities, aad coexistswith paratacamitein the holotype specimenof p,aralacamite.The two minerals are not readily distinguishedexcept by optical and X-ray methods:paratacamite is uniaxial negative, whereasclinoatacamite is biaxht negative, 2V@75(5f . Strongestlines of the X-ray powder paltern of clino- aracamireld n A(D@k[)]are 5.47(100)(T0l,0Ll),2.887(40X121J03),2.767(60)81.1),2.742Q0)(0r3,202),2.266(@)Q20), 2.243(50)(004),and L.7M(5Q82a,040). Clinoatacamiteis readily synthesizedand a seriesof experimentswas conductedto promotethe uptakeof Zn and duplicatethe formula of the dubiousmineral "anarakite" (CuZn)2(OI{)3C1.Generally, products with more than about6 mol%o"7iproved to be hexagonal,i.e., nrcranpaatacamite, as did specimensof "anarakite"fron fhe type locality. -
Ramsbeckite (Cu, Zn)15(SO4)4(OH)22 • 6H2O C 2001-2005 Mineral Data Publishing, Version 1 Crystal Data: Monoclinic, Pseudohexagonal
Ramsbeckite (Cu, Zn)15(SO4)4(OH)22 • 6H2O c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Monoclinic, pseudohexagonal. Point Group: 2/m. Crystals are tabular with large {001}, also {210}, {110}, {100}, giving a slightly rounded rhombic outline, to 3 mm. Twinning: Observed, repeated, forming cylindrical aggregates. Physical Properties: Cleavage: On {001}, perfect. Fracture: Conchoidal. Tenacity: Brittle. Hardness = 3.5 D(meas.) = 3.39–3.41 D(calc.) = 3.37 Optical Properties: Transparent to translucent. Color: Green, blue-green. Streak: Pale green. Luster: Vitreous. Optical Class: Biaxial (–). Pleochroism: Weak; X = pale blue-green, emerald-green; Y = Z = blue-green, yellow-green. Orientation: Y = b; X ∧ c =5◦; Z ∧ a =5◦. Absorption: X > Y = Z. α = 1.624–1.669 β = 1.674–1.703 γ = 1.678–1.707 2V(meas.) = 36◦–38◦ 2V(calc.) = 38.0◦ Cell Data: Space Group: P 21/a. a = 16.088–16.110 b = 15.576–15.602 c = 7.102–7.112 β =90.0◦−90.27◦ Z=2 X-ray Powder Pattern: Bastenberg mine, Ramsbeck, Germany. 7.090 (100), 3.549 (25), 1.776 (20), 3.254 (13), 4.400 (12), 3.232 (12), 3.244 (11) Chemistry: (1) (2) (3) SO3 17.4 17.6 17.51 CuO 44.5 43.8 43.49 ZnO 15.8 18.1 22.25 H2O 19.3 [20.5] 16.75 Total 97.0 [100.0] 100.00 (1) Bastenberg mine, Ramsbeck, Germany; SO4 by photometry, CuO, ZnO by AA, H2O by gas 1− chromatography, (OH) computed for charge balance; corresponds to (Cu10.30Zn3.58)Σ=13.88 • (SO4)4.00(OH)19.76 9.84H2O. -
Macphersonite Pb4(SO4)(CO3)2(OH)2 C 2001-2005 Mineral Data Publishing, Version 1
Macphersonite Pb4(SO4)(CO3)2(OH)2 c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Orthorhombic, pseudohexagonal. Point Group: 2/m 2/m 2/m. Crystals are commonly pseudohexagonal, thin to tabular on {010}, to 1 cm. Twinning: Common, lamellar and contact, composition plane {102}. Physical Properties: Cleavage: On {010}, perfect. Fracture: Uneven. Hardness = 2.5–3 D(meas.) = 6.50–6.55 D(calc.) = 6.60–6.65 May exhibit a bright yellow fluorescence under SW and LW UV. Optical Properties: Semitransparent. Color: Colorless, white, very pale amber. Luster: Adamantine to resinous. Optical Class: Biaxial (–). Orientation: X = b; Y = c; Z = a. Dispersion: r> v,moderate. α = 1.87 β = 2.00 γ = 2.01 2V(meas.) = 35◦–36◦ Cell Data: Space Group: P cab. a = 10.383(2) b = 23.050(5) c = 9.242(2) Z = 8 X-ray Powder Pattern: Argentolle mine, France; may show preferred orientation. 3.234 (100), 2.654 (90), 3.274 (50), 2.598 (30), 2.310 (30), 2.182 (30), 2.033 (30) Chemistry: (1) (2) (3) SO3 6.6 7.65 7.42 CO2 8.8 8.47 8.16 CuO 0.1 CdO 0.1 PbO 83.4 83.59 82.75 + H2O 1.3 1.93 1.67 Total 100.3 101.64 100.00 (1) Leadhills, Scotland; by electron microprobe, average of ten analyses, CO2 by evolved gas analysis, H2O by TGA; corresponds to (Pb4.08Cu0.10Cd0.07)Σ=4.25(S0.90O4)(C1.09O3)2(OH)1.58. (2) Argentolle mine, France; corresponds to Pb4.06(S1.03O4)(C1.04O3)2(OH)2.32.