X-Ray Study and Synthesis of Some Copper-Lead Oxychlorides

Total Page:16

File Type:pdf, Size:1020Kb

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. Dr. P. G. Embrey furnished type percylite from the material described by Brooke (1850) and d ia b o leite and ch loroxip h ite from the Mendip H ills. The specimens furnished by Dr. Embrey were supplied from the collections of the British Museum of History. Mr. Karl Schwartzwalder made available to the author certain facilities of the AC Spark Plug Division of the General Motors Corporation. The author is also indebted to Dr. William Shulhof of i i the AC Spark Plug Division for his cooperation during the use of these facilities. Thanks are also due Dr. Charles Sclar and Dr. George Cocks of Battelle Memorial Institute who made certain equipment available for use in this study. Dr. Reynolds M. Denning of the University of Michigan was also kind enough to provide the use of equipment in the Department of Geology and Mineralogy. Financial assistance which made it possible for the author to devote full time to the research involved in the thesis was provided through the William J. McCaughey Fellowship and the author wishes to thank the contributors to this fellowship for their assistance. The author wishes also to thank the faculty in the Department of Mineralogy for their direct and indirect assistance and encouragement in the course of this study. Most particularly he wishes to thank Dr. Henry £. Wenden, his adviser, for assistance and encouragement during this investigation. Lastly, the author wishes to thank his wife Grace for her encouragement and perserverance, since this dissertation could never have been completed without them. iii CONTENTS Page ACKNOWLEDGMENTS i i LIST OF TABLES v i LIST OF ILLUSTRATIONS v i i i INTRODUCTION 1 I . HISTORICAL SURVEY 2 I I . SCOPE OF THE INVESTIGATION 19 I I I . EXPERIMENTAL METHODS 21 Specimens X-ray Analysis Heating Stage C rystallographic Measurements Specific Gravity Measurements Synthesis MLcrochemical Tests IV. CUMENGEITE...................................................................................... 29 H isto r ic a l Summary Results of Present Study V. PSEUDOBOLEITE................................................................................ 77 H isto r ic a l Summary Results of Present Study VI. BOLEITE ............................................................................................. llJi H isto r ic a l Summary Results of Present Study V II. THE BOLEITE PROBLEM..................................................................... 166 iv CONTENTS (Continued) Page V III. FERCYLITE.............................................................................................. 173 H isto r ic a l Summary Results of Present Study IX. EPITAXY IN THE BOLEITE G R O U P ............................................... 185 X. DIABCLEITE........................................................................................ 192 H isto r ic a l Summary Results of Present Study XI. C HLOROXIP HI T E ................................................................................. 20U H isto r ic a l Summary Results of Present Study X II. SYNTHESIS.............................................................................................. 209 Introduction Experimental Procedure R esults X III. SUMMARY AND CONCLUSIONS............................................................. 222 BIBLIOGRAPHY AND REFERENCES ......................................... 229 AUTOBIOGRAPHY................................. 233 v LIST OF TABLES Table Page 1. Minerals of the boleite group .............................................. 8 2 . The b o le ite g r o u p .................................................................. ........ 11 3. Angle table for cumengeite .................................................... 3U U. Indices of refraction for cumengeite (Hadding, 1919) • 36 5. X-ray powder data for cumengeite ....................................... hi 6. Comparison of x-ray parameters according to the setting of Friedel (1906) ................................................................. 53 7. Crystallographic data for cum engeite ......................... Sh 8. Presence criteria for cumengeite ....................................... 55 9. Specific gravity values for cumengeite ...................................... 68 10. Chemical analyses for cumengeite ................................................ 69 11. X-ray data for cum engeite .................................................... 73 12. X-ray powder data for pseudoboleite ................................ 91 13. Crystallographic data for pseudoboleite ..... 103 lU. Presence criteria for pseudoboleite . 10U 15. Cleavage observed in boleite try Hadding (1919) . • 126 16. Thermal cycle for b o le ite .............................................................. l 5 l 17. X-ray powder data for b o leite ...................................................... 1$6 18. X-ray and microchemical examination of percylite speci­ mens .................................................................................................... 183 19. Comparison of parameters for members of the boleite group determined in this stu d y ....................................... 189 v i LIST OF TABLES (Continued) Table Page 20. X-ray powder data fo r d i a b o l e i t e .............................. 19U 21. Comparison of cell dimensions for diaboleite . 198 22. Forrailas and reagents used in synthesis experiments . 211 23. Summary of diffusion experiments ........................................ 215 2J4. Summary of evaporation exp erim ents ....................... 216 25. Summary of pyrex tube experiments .............................. 217 26. Summary of pot bomb experim ents .............................. 220 v i i IIST OF ILLUSTRATIONS Figure Page 1. Morphology of natural cumengeite (Hadding, 1919) . , U2 2. Morphology of natural cumengeite U2 3. Powder diffraction pattern of natural cumengeite (Sainte- Etienne 2750) ................................................................................ U5 U. Powder d iffr a c tio n pattern of natural cumengeite (USNM 9U6U0) ............................................................................................. , 16 5. Powder diffraction pattern of natural cumengeite from an overgrowth of cumengeite on boleite (Hocart specimen) ...................................................................................... 16 6. Powder diffraction pattern of natural cumengeite from an overgrowth of cumengeite on boleite (OSU collections) ..................................................... .... U5 7. Diagramatic representation of the space group FTnmm . 57 8. Diagramatic representation of the twinned space group FU/m 2/m 2/m developed from ty twinning across (110) or rotation of 90° about 001 ....................................... 57 9. Diagramatic representation of the space group FU/m 2/m 2/m........................................................................................ 61 10. Diagramatic representation of the twinned space group FU/m 2/m 2/m developed from P^/m 2/ m 2/m an n-glide in (001) ......................................................................... 61 11. Disordered form of AuCu^ (after Cullity, 1956) . * 65 12. Ordered form of AuCu^ (after Cullity, 1956) . 65 13 • Morphology of sy n th etic cumengeite ....... 71 lii. Morphology of synthetic cumengeite 71 15. Powder diffraction pattern of natural cumengeite from an overgrowth of cumengeite on boleite (Hocart s p e c i m e n ) .................................................................. 7U v i i i LIST OF ILLUSTRATIONS (Continued) Figure Page 16. Powder diffraction pattern of aynthetic cumengeite obtained try alow diffusion at 25>°C. from stoichio­ metric proportions for pseudoboleite ...... 7k 17 . Powder d iffr a c tio n pattern o f sy n th etic cumengeite obtained in a sealed glass tube at 170°C. from stoichiometric proportions for cumengeite • . 7U 18. Powder diffraction pattern of synthetic cumengeite obtained in a
Recommended publications
  • Paralaurionite Pbcl(OH) C 2001-2005 Mineral Data Publishing, Version 1
    Paralaurionite PbCl(OH) c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Monoclinic. Point Group: 2/m. Crystals are thin to thick tabular k{100}, or elongated along [001], to 3 cm; {100} is usually dominant, but may show many other forms. Twinning: Almost all crystals are twinned by contact on {100}. Physical Properties: Cleavage: {001}, perfect. Tenacity: Flexible, due to twin gliding, but not elastic. Hardness = Soft. D(meas.) = 6.05–6.15 D(calc.) = 6.28 Optical Properties: Transparent to translucent. Color: Colorless, white, pale greenish, yellowish, yellow-orange, rarely violet; colorless in transmitted light. Luster: Subadamantine. Optical Class: Biaxial (–). Pleochroism: Noted in violet material. Orientation: Y = b; Z ∧ c =25◦. Dispersion: r< v,strong. Absorption: Y > X = Z. α = 2.05(1) β = 2.15(1) γ = 2.20(1) 2V(meas.) = Medium to large. Cell Data: Space Group: C2/m. a = 10.865(4) b = 4.006(2) c = 7.233(3) β = 117.24(4)◦ Z=4 X-ray Powder Pattern: Laurium, Greece. 5.14 (10), 3.21 (10), 2.51 (9), 2.98 (7), 3.49 (6), 2.44 (6), 2.01 (6) Chemistry: (1) (2) (3) Pb 78.1 77.75 79.80 O [3.6] 6.00 3.08 Cl 14.9 12.84 13.65 H2O 3.4 3.51 3.47 insol. 0.09 Total [100.0] 100.19 100.00 (1) Laurium, Greece. (2) Tiger, Arizona, USA. (3) PbCl(OH). Polymorphism & Series: Dimorphous with laurionite. Occurrence: A secondary mineral formed through alteration of lead-bearing slag by sea water or in hydrothermal polymetallic mineral deposits.
    [Show full text]
  • 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
    [Show full text]
  • 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
    [Show full text]
  • 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.
    [Show full text]
  • The Crystal Structure of Boleit+A Mineral Containing Silver Atom Clusters
    JOURNAL OF SOLID STATE CHEMISTRY 6,86-92 (1973) The Crystal Structure of Boleit+A Mineral Containing Silver Atom Clusters ROLAND C. ROUSE Department of Geology and Mineralogy,* The University of Michigan, Ann Arbor, Michigan 48104 Received March IO,1972 The mineral boleite, Pb26Ag,Cu~,CI,1(OH)1s, is cubic, space group Pm3m, with u = 15.29 A. Lead and silver atoms form a distorted body-centered array leading to octahedral groupings of these atoms. The silver atoms and their coordinating chlorines form Ag&18C16 groups similar to those in the metal cluster compounds MoCI, and WCL. Lead and conoer atoms are in distorted square antiprismatic and tetragonal bipyramidal coordination, r&ectively. - - Introduction gradually from blue to green, while the bire- Boleite is a lead copper oxychloride mineral fringent rim and the quasi-isotropic core merged which occurs as deep blue crystals of cubic form. into an apparently homogeneous, isotropic These cubes are zoned and consist of an optically phase. Upon cooling, the blue color returned but isotropic or quasi-isotropic core and a bire- the isotropy persisted. From these and other fringent outer rim of complex structure. The cube observations Winchell proposed that boleite faces are sometimes occupied by epitaxial undergoes an inversion from a pseudocubic form overgrowths of the related speciespseudoboleite to a cubic one with increasing temperature. and cumengite. Boleite has been studied in detail by Mallard and Cumenge (I), Friedel (2), and Symmetry and Composition Hocart (3). They all considered the birefringent To determine the true symmetry of boleite, material to be tetragonal and untwinned and the isotropic cleavage fragments were examined by isotropic core to be pseudocubic due to twinning.
    [Show full text]
  • Thirty-Fourth List of New Mineral Names
    MINERALOGICAL MAGAZINE, DECEMBER 1986, VOL. 50, PP. 741-61 Thirty-fourth list of new mineral names E. E. FEJER Department of Mineralogy, British Museum (Natural History), Cromwell Road, London SW7 5BD THE present list contains 181 entries. Of these 148 are Alacranite. V. I. Popova, V. A. Popov, A. Clark, valid species, most of which have been approved by the V. O. Polyakov, and S. E. Borisovskii, 1986. Zap. IMA Commission on New Minerals and Mineral Names, 115, 360. First found at Alacran, Pampa Larga, 17 are misspellings or erroneous transliterations, 9 are Chile by A. H. Clark in 1970 (rejected by IMA names published without IMA approval, 4 are variety because of insufficient data), then in 1980 at the names, 2 are spelling corrections, and one is a name applied to gem material. As in previous lists, contractions caldera of Uzon volcano, Kamchatka, USSR, as are used for the names of frequently cited journals and yellowish orange equant crystals up to 0.5 ram, other publications are abbreviated in italic. sometimes flattened on {100} with {100}, {111}, {ill}, and {110} faces, adamantine to greasy Abhurite. J. J. Matzko, H. T. Evans Jr., M. E. Mrose, lustre, poor {100} cleavage, brittle, H 1 Mono- and P. Aruscavage, 1985. C.M. 23, 233. At a clinic, P2/c, a 9.89(2), b 9.73(2), c 9.13(1) A, depth c.35 m, in an arm of the Red Sea, known as fl 101.84(5) ~ Z = 2; Dobs. 3.43(5), D~alr 3.43; Sharm Abhur, c.30 km north of Jiddah, Saudi reflectances and microhardness given.
    [Show full text]
  • Journal of the Russell Society, Vol 4 No 2
    JOURNAL OF THE RUSSELL SOCIETY The journal of British Isles topographical mineralogy EDITOR: George Ryba.:k. 42 Bell Road. Sitlingbourn.:. Kent ME 10 4EB. L.K. JOURNAL MANAGER: Rex Cook. '13 Halifax Road . Nelson, Lancashire BB9 OEQ , U.K. EDITORrAL BOARD: F.B. Atkins. Oxford, U. K. R.J. King, Tewkesbury. U.K. R.E. Bevins. Cardiff, U. K. A. Livingstone, Edinburgh, U.K. R.S.W. Brai thwaite. Manchester. U.K. I.R. Plimer, Parkvill.:. Australia T.F. Bridges. Ovington. U.K. R.E. Starkey, Brom,grove, U.K S.c. Chamberlain. Syracuse. U. S.A. R.F. Symes. London, U.K. N.J. Forley. Keyworth. U.K. P.A. Williams. Kingswood. Australia R.A. Howie. Matlock. U.K. B. Young. Newcastle, U.K. Aims and Scope: The lournal publishes articles and reviews by both amateur and profe,sional mineralogists dealing with all a,pecI, of mineralogy. Contributions concerning the topographical mineralogy of the British Isles arc particularly welcome. Not~s for contributors can be found at the back of the Journal. Subscription rates: The Journal is free to members of the Russell Society. Subsc ription rates for two issues tiS. Enquiries should be made to the Journal Manager at the above address. Back copies of the Journal may also be ordered through the Journal Ma nager. Advertising: Details of advertising rates may be obtained from the Journal Manager. Published by The Russell Society. Registered charity No. 803308. Copyright The Russell Society 1993 . ISSN 0263 7839 FRONT COVER: Strontianite, Strontian mines, Highland Region, Scotland. 100 mm x 55 mm.
    [Show full text]
  • A Specific Gravity Index for Minerats
    A SPECIFICGRAVITY INDEX FOR MINERATS c. A. MURSKyI ern R. M. THOMPSON, Un'fuersityof Bri.ti,sh Col,umb,in,Voncouver, Canad,a This work was undertaken in order to provide a practical, and as far as possible,a complete list of specific gravities of minerals. An accurate speciflc cravity determination can usually be made quickly and this information when combined with other physical properties commonly leads to rapid mineral identification. Early complete but now outdated specific gravity lists are those of Miers given in his mineralogy textbook (1902),and Spencer(M,i,n. Mag.,2!, pp. 382-865,I}ZZ). A more recent list by Hurlbut (Dana's Manuatr of M,i,neral,ogy,LgE2) is incomplete and others are limited to rock forming minerals,Trdger (Tabel,l,enntr-optischen Best'i,mmungd,er geste,i,nsb.ildend,en M,ineral,e, 1952) and Morey (Encycto- ped,iaof Cherni,cal,Technol,ogy, Vol. 12, 19b4). In his mineral identification tables, smith (rd,entifi,cati,onand. qual,itatioe cherai,cal,anal,ys'i,s of mineral,s,second edition, New york, 19bB) groups minerals on the basis of specificgravity but in each of the twelve groups the minerals are listed in order of decreasinghardness. The present work should not be regarded as an index of all known minerals as the specificgravities of many minerals are unknown or known only approximately and are omitted from the current list. The list, in order of increasing specific gravity, includes all minerals without regard to other physical properties or to chemical composition. The designation I or II after the name indicates that the mineral falls in the classesof minerals describedin Dana Systemof M'ineralogyEdition 7, volume I (Native elements, sulphides, oxides, etc.) or II (Halides, carbonates, etc.) (L944 and 1951).
    [Show full text]
  • 31 May 2013 2013-024 Yeomanite
    Title Yeomanite, Pb2O(OH)Cl, a new chain-structured Pb oxychloride from Merehead Quarry, Somerset, England Authors Turner, RW; Siidra, OI; Rumsey, MS; Polekhovsky, YS; Kretser, YL; Krivovichev, SV; Spratt, J; Stanley, Christopher Date Submitted 2016-04-04 2013-024 YEOMANITE CONFIDENTIAL INFORMATION DEADLINE: 31 MAY 2013 2013-024 YEOMANITE Pb2O(OH)Cl Orthorhombic Space group: Pnma a = 6.585(10) b = 3.855(6) c = 17.26(1) Å V = 438(1) Å3 Z = 4 R.W. Turner1*, O.I. Siidra2, M.S. Rumsey3, Y.S. Polekhovsky4, S.V. Krivovichev2, Y.L. Kretser5, C.J. Stanley3, and J. Spratt3 1The Drey, Allington Track, Allington, Salisbury SP4 0DD, Wiltshire, UK 2Department of Crystallography, Geological Faculty, St Petersburg State University, University Embankment 7/9, St Petersburg 199034, Russia 3Department of Earth Sciences, Natural History Museum, Cromwell Road, London SW7 5BD, UK 4Department of Mineral Deposits, St Petersburg State University, University Embankment 7/9, 199034 St Petersburg, Russia 5V.G. Khlopin Radium Institute, Roentgen Street 1, 197101 St Petersburg, Russia *E-mail: [email protected] OCCURRENCE The mineral occurs in the Torr Works (Merehead) Quarry, East Cranmore, Somerset, UK. Yeomanite is associated with mendipite, as a cavity filling in manganese oxide pods. Other oxyhalide minerals that are found hosted in mendipite include diaboleite, chloroxiphite and paralaurionite. Secondary Pb and Cu minerals, including mimetite, wulfenite, cerussite, hydrocerussite, malachite, and crednerite also occur in the same environment. Gangue minerals associated with mineralised manganese pods include aragonite, calcite and barite. Undifferentiated pod-forming Mn oxides are typically a mixture of manganite and pyrolusite, associated with Fe oxyhydroxides such as goethite (Turner, 2006).
    [Show full text]
  • The Substituted Basic Cu(II) Chloride Phase Transformations
    European Mineralogical Conference Vol. 1, EMC2012-61-1, 2012 European Mineralogical Conference 2012 © Author(s) 2012 The substituted basic Cu(II) chloride phase transformations M. Sciberras (1), P. Leverett (1), P.A Williams (1), T. Malcherek (2), and J. Schlueter (2) (1) School of Science and Health, University of Western Sydney, Sydney, Australia ([email protected]), (2) Mineralogisch-Petrographisches Institut, Universität Hamburg, Hamburg, Germany ([email protected]) The known polymorphs of composition Cu2Cl(OH)3 are botallackite (P 21/m), atacamite (Pnma), clinoatacamite (P 21/n), anatacamite (P 1) and paratacamite (R3). Paratacamite was originally described by Smith (1906) as having the composition Cu2Cl(OH)3, but it is now accepted that the rhombohedral structure is stabilised by the presence of some essential Zn or Ni (Jambor et al., 1996). The structure of paratacamite was determined by Fleet (1975) assuming the nominal formula Cu2Cl(OH)3 and exhibits a pronounced sub-cell with a’ = 1/2a, c’ = c, space group R3m. It is now known that this R3mstructure is that of herbertsmithite and gillardite, Cu3MCl2(OH)6, M = Zn, Ni, respectively (Braithwaite et al., 2004; Clissold et al., 2007). A series a compositionally related phase transformations are known to occur in this group as Cu is replaced by Zn or Ni. It is suggested that the order of phase transformations follow the series, P 1 ! P 21/n ! R3 ! R3m (Malcherek and Schlüter, 1999). This series of potential transformations was explored by Raman spectroscopy for materials of composition Cu4−xMxCl2(OH)6 where M = Zn or Ni, between Cu3:90M0:10Cl2(OH)6 to Cu3:08M0:92Cl2(OH)6.
    [Show full text]
  • Mendipite Pb3o2cl2 C 2001-2005 Mineral Data Publishing, Version 1
    Mendipite Pb3O2Cl2 c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Orthorhombic. Point Group: 222. In columnar or fibrous aggregates, and cleavable masses, to 12 cm. Physical Properties: Cleavage: {010}, perfect; {100} and {010}, less perfect. Fracture: Conchoidal to uneven. Hardness = 2.5 D(meas.) = 7.240 D(calc.) = 7.22 Optical Properties: Translucent, rarely transparent. Color: Colorless to white, brownish cream, gray, tinged yellow, pink, red, or blue; nearly colorless in transmitted light. Streak: White. Luster: Pearly to silky on cleavages; resinous to adamantine on fractures. Optical Class: Biaxial (+). Orientation: X = a; Y = b; Z = c. Dispersion: r< v,very strong. α = 2.24(2) β = 2.27(2) γ = 2.31(2) 2V(meas.) = ∼90◦ Cell Data: Space Group: P 212121. a = 9.52 b = 11.95 c = 5.87 Z = 4 X-ray Powder Pattern: L˚angban,Sweden. 2.78 (10), 2.64 (9), 3.04 (8), 3.51 (7), 7.40 (6), 3.78 (6), 3.08 (6) Chemistry: (1) (2) (3) Pb 85.87 85.69 85.79 O 4.53 [4.44] 4.42 Cl 9.35 9.87 9.79 Total 99.75 [100.00] 100.00 (1) Mendip Hills, England; corresponds to Pb3.14Cl2O2.15. (2) Kunibert mine, near Brilon, Germany. (3) Pb3O2Cl2. Occurrence: In nodules in manganese oxide ores (Somerset, England). Association: Hydrocerussite, cerussite, malachite, pyromorphite, calcite, chloroxiphite, diaboleite, parkinsonite (Somerset, England). Distribution: In England, from the Higher Pitts Farm, the Priddy Hill Farm, the Wesley mine, and near Churchill, Mendip Hills, and in the Merehead quarry, near Shepton Mallet, Somerset.
    [Show full text]
  • Matlockite Pbfcl C 2001-2005 Mineral Data Publishing, Version 1
    Matlockite PbFCl c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Tetragonal. Point Group: 4/m 2/m 2/m. Tabular crystals, to 5 cm, flattened on {001}, with {110}, {011}, and {111} modifications, may be equant, rounded. In subparallel aggregates, rosettelike, radiating, hemispherical; lamellar, cleavable massive. Physical Properties: Cleavage: {001}, perfect. Fracture: Uneven to subconchoidal. Tenacity: Brittle. Hardness = 2.5–3 D(meas.) = 7.12 D(calc.) = 7.16 Optical Properties: Transparent. Color: Colorless, pale yellow, amber-yellow, yellow-orange; colorless in transmitted light. Luster: Adamantine, pearly on {001}. Optical Class: Uniaxial (–); rarely biaxial due to strain. ω = 2.145 = 2.006 2V(meas.) = Small. Cell Data: Space Group: P 4/nmm (synthetic). a = 4.1104(2) c = 7.2325(5) Z = 2 X-ray Powder Pattern: Synthetic. 3.574 (100), 2.906 (45), 3.617 (40), 2.265 (40), 2.715 (35), 1.781 (25), 2.055 (20) Chemistry: (1) (2) (3) Pb 79.55 78.92 79.19 F 7.11 7.25 7.26 Cl 13.44 13.57 13.55 Total 100.10 [99.74] 100.00 (1) Cromford, England. (2) Tiger, Arizona, USA; original total given as 99.67%. (3) PbFCl. Occurrence: In the oxide zone of some lead-bearing mineral deposits. Association: Phosgenite, anglesite, cerussite, galena, sphalerite, barite, fluorite (Cromford, England); diaboleite, boleite, caledonite, leadhillite (Tiger, Arizona, USA). Distribution: Large crystals from the Bage and Wallclose mines, about 2.5 km south of Matlock, Derbyshire, England. In slag, at Laurium, Greece. In slag, along Baratti Beach and one km north of Campiglia, Tuscany, Italy.
    [Show full text]