The Role of Tetrahedral Building Blocks in Low-Dimensional Oxohalide Materials
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Mixite Bicu6(Aso4)3(OH)6 • 3H2O C 2001-2005 Mineral Data Publishing, Version 1 Crystal Data: Hexagonal
Mixite BiCu6(AsO4)3(OH)6 • 3H2O c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Hexagonal. Point Group: 6/m. As acicular crystals, elongated along [0001], commonly in mats, radial fibrous aggregates, or cross-fiber veinlets. Physical Properties: Hardness = 3–4 D(meas.) = 3.79–3.83 D(calc.) = [4.04] Optical Properties: Transparent to translucent. Color: Blue-green to emerald-green, pale green, white; pale green to colorless in transmitted light. Streak: Pale bluish green. Luster: Vitreous, silky in aggregates. Optical Class: Uniaxial (+). Pleochroism: O = colorless; E = bright green. Absorption: E > O. ω = 1.743–1.749 = 1.810–1.830 Cell Data: Space Group: P 63/m. a = 13.646(2) c = 5.920(1) Z = 2 X-ray Powder Pattern: Anton mine, Germany. 12.03 (10), 2.46 (9), 3.57 (8), 2.95 (7), 2.86 (6), 2.70 (6), 2.57 (6) Chemistry: (1) (2) (3) P2O5 1.05 0.06 As2O5 29.51 28.79 29.64 SiO2 0.42 Fe2O3 0.97 Bi2O3 12.25 11.18 20.03 FeO 1.52 CuO 44.23 43.89 41.04 ZnO 2.70 CaO 0.83 0.26 H2O 11.06 11.04 9.29 Total 100.45 99.31 100.00 • (1) J´achymov, Czech Republic. (2) Tintic district, Utah, USA. (3) BiCu6(AsO4)3(OH)6 3H2O. Mineral Group: Mixite group. Occurrence: An uncommon secondary mineral in the oxidized zone of copper deposits. Association: Bismutite, smaltite, bismuth, atelestite, erythrite, malachite, barite. Distribution: From the Geister vein, Werner mine, J´achymov (Joachimsthal), Czech Republic. -
Final Program
1 General Information SCOPE OF THE CONFERENCE The 11th Joint MMM/Intermag Conference is sponsored jointly by the American Institute of Physics (PCI) and the Magnetics Society of the IEEE, in cooperation with The American Physical Society. Members of the inter- national scientific and engineering communities interested in recent devel- opments in fundamental and applied magnetism are invited to attend the Conference and contribute to its technical sessions. Sessions will include invited and contributed papers, oral and poster presentations and invited symposia. This Conference provides an outstanding opportunity for partici- pants to meet their colleagues and discuss new, advanced and controversial developments. WASHINGTON, DC The 2010 Joint Conference will be held in the nation’s capital. The city wel- comes 15 million visitors each year of which 1.2 million are international. There are more than 100 restaurants located in the downtown area alone, and the city has been called “one of the most exciting restaurant cities on the East Coast” by Travel & Leisure. To obtain an in-depth and current view of what to see and do while you are here, visit the official website at: http://www.washington.org. Here you will find information on how to trav- el to the Marriott Washington Wardman Park from any of the three local air- ports; you can check on the weather in mid-January, and can request a free Visitors Guide prior to making your trip. VISA REQUIREMENTS The US has updated its visa policies to increase security, so it may take you 3-6 months to apply for and receive your visa. -
Petersite, a REE and Phosphate Analog of Mixite
American Mineralogist, Volume 67, pages 1039-142, l9E2 Petersite,a REE and phosphateanalog of mixite DoNer-o R. PBecon Department of Geological Sciences University of Michigan Ann Arbor, Michigan 48109 nNn PBIB J. DUNN Department of Mineral Sciences Smithsonian Institution Washington, D.C.20560 Abstract The new mineral petersite (Y,REE,Ca)Cuo@Oa)I(OH)6.3H2O)occurs as a supergene mineral at the traprock quarry at Laurel Hill in Secaucus,New Jersey. It occurs in a brecciatedand mineralizedhornfels near a diabasecontact, in associationwith opal and malachite.Prismatic crystals less than 0. I mm in lengthwith forms {1010}and {0001}occur as radiatingsprays. It is optically uniaxial, positive,with or : 1.666(4) and e: 1.747(4). The measureddensity is 3.41g/cm3. Petersite is hexagonal,probable space group PQlm or P63,with a : 13.288(5)c : 5.877(5)4,V : 898.6(8)43,and Z:2.The strongestlines in the powderdiffraction pattern are: (d, intensity,index) I1.6, 100,100; 4.36, 50, 210;3.49,40, 2ll;2.877,40, 400;2.433, 60,212. The nameis in honorof Thomasand JosephPeters. Introduction under catalog # NMNH 148973at the Smithsonian Institution. The new mineral describedherein was sent to us for examinationby Mr. ThomasPeters of the Pater- Morphology son Museum,who had obtainedit from Mr. Nicho- Petersiteoccurs as prismatic hexagonalcrystals las Facciolla, who found it in early 1981. Mr. of simplemorphology. The only forms presentare Peters'examination by SEM techniquessuggested the prism {1010}, and the pinacoid {0001}. The a hexagonal morphology for the mineral and our crystals are usually euhedral and occur in radiating subsequentX-ray diffraction study showedit to be clustersand sprayswhich are somewhatisolated on hexagonaland isostructural with members of the the matrix (Fig. -
Water Splitting by Heterogeneous Catalysis
!"#$ #"%"" &' () * ( +# ,% - . ( (.( ( . %/ .0! 1 ( % 2 3 . 4 . 5 % . . % . . . . . . 3 % !# 3 ( 3 ( 3 ( 3 %/. . - % . (. 6 7 % ( 2!0! . (/ (3 . 7 % ( ( 3 % . 3 ( %/ . 8 9 3 8 % ( :;0 9 . <= 3 9 . % ( . ( 3 > % !"#$ ?@@ %% @ A B ?? ? ? #;C#C# ,8D$CD#$$D$":D! ,8D$CD#$$D$";"C ! " # $ (#" D# WATER SPLITTING BY HETEROGENEOUS CATALYSIS Henrik Svengren Water splitting by heterogeneous catalysis Henrik Svengren ©Henrik Svengren, Stockholm University 2017 ISBN print 978-91-7797-039-2 ISBN PDF 978-91-7797-040-8 Printed in Sweden by Universitetsservice US-AB, Stockholm 2017 Distributed by the Department of Materials and Environmental Chemistry To my beloved family Cover image + Heterogeneous catalysis of water oxidation according to 2H2O ĺ O2 + 4H on CoSbO4/CoSb2O6, investigated in Paper II. The figure is composed of SEM- and TEM images, structural drawings, reactant- and product molecules. i Examination Faculty opponent Docent Tomas Edvinsson Solid State Physics Department of Engineering Sciences Uppsala University, -
A Review of the Structural Architecture of Tellurium Oxycompounds
Mineralogical Magazine, May 2016, Vol. 80(3), pp. 415–545 REVIEW OPEN ACCESS A review of the structural architecture of tellurium oxycompounds 1 2,* 3 A. G. CHRISTY ,S.J.MILLS AND A. R. KAMPF 1 Research School of Earth Sciences and Department of Applied Mathematics, Research School of Physics and Engineering, Australian National University, Canberra, ACT 2601, Australia 2 Geosciences, Museum Victoria, GPO Box 666, Melbourne, Victoria 3001, Australia 3 Mineral Sciences Department, Natural History Museum of Los Angeles County, 900 Exposition Boulevard, Los Angeles, CA 90007, USA [Received 24 November 2015; Accepted 23 February 2016; Associate Editor: Mark Welch] ABSTRACT Relative to its extremely low abundance in the Earth’s crust, tellurium is the most mineralogically diverse chemical element, with over 160 mineral species known that contain essential Te, many of them with unique crystal structures. We review the crystal structures of 703 tellurium oxysalts for which good refinements exist, including 55 that are known to occur as minerals. The dataset is restricted to compounds where oxygen is the only ligand that is strongly bound to Te, but most of the Periodic Table is represented in the compounds that are reviewed. The dataset contains 375 structures that contain only Te4+ cations and 302 with only Te6+, with 26 of the compounds containing Te in both valence states. Te6+ was almost exclusively in rather regular octahedral coordination by oxygen ligands, with only two instances each of 4- and 5-coordination. Conversely, the lone-pair cation Te4+ displayed irregular coordination, with a broad range of coordination numbers and bond distances. -
02-Newsl7tabs 27..32
Mineralogical Magazine, February 2011, Vol. 75(1), pp. 27À31 CNMNC Newsletter IMA Commission on New Minerals, Nomenclature and Classification (CNMNC) NEWSLETTER 7 New minerals and nomenclature modifications approved in 2010 1 2 3 P. A. WILLIAMS (Chairman, CNMNC), F. HATERT (Vice-Chairman, CNMNC), M. PASERO (Vice-Chairman, 4 CNMNC) AND S. J. MILLS (Secretary, CNMNC) 1 School of Natural Sciences, University of Western Sydney, Locked Bag 1797, Penrith South DC, NSW 1797, Australia À [email protected] 2 Laboratoire de Mine´ralogie, Universite´ de Lie`ge, B-4000 Lie`ge, Belgium À [email protected] 3 Dipartimento di Scienze della Terra, Universita` degli Studi di Pisa, Via Santa Maria 53, I-56126 Pisa, Italy À [email protected] 4 Department of Earth and Ocean Sciences, University of British Columbia, Vancouver BC, Canada V6T 1Z4 À [email protected] The information given here is provided by the IMA Commission on New Minerals, Nomenclature and Classification for comparative purposes and as a service to mineralogists working on new species. Each mineral is described in the following format: NEW MINERAL PROPOSALS APPROVED IN NOVEMBER 2 010 Mineral name, if the authors agree on its IMA No. 2010-044 release prior to the full description appearing Titanium in press Ti Chemical formula Orebody 31, Luobusa mining district, in Qusong Type locality County, Tibet (29º5’N 92º5’E) Full authorship of proposal Fang Qing-Song, Shi Ni-Cheng, Li Guo-Wu*, E-mail address of corresponding author Bai Wen-Ji, Yang Jing-Sui, Xiong Ming, Rong Relationship to other -
Preparation and Spectral Properties of Oxomolybdenum(V) Complexes. Harry Edmond Pence II Louisiana State University and Agricultural & Mechanical College
Louisiana State University LSU Digital Commons LSU Historical Dissertations and Theses Graduate School 1968 Preparation and Spectral Properties of Oxomolybdenum(v) Complexes. Harry Edmond Pence II Louisiana State University and Agricultural & Mechanical College Follow this and additional works at: https://digitalcommons.lsu.edu/gradschool_disstheses Recommended Citation Pence, Harry Edmond II, "Preparation and Spectral Properties of Oxomolybdenum(v) Complexes." (1968). LSU Historical Dissertations and Theses. 1411. https://digitalcommons.lsu.edu/gradschool_disstheses/1411 This Dissertation is brought to you for free and open access by the Graduate School at LSU Digital Commons. It has been accepted for inclusion in LSU Historical Dissertations and Theses by an authorized administrator of LSU Digital Commons. For more information, please contact [email protected]. This dissertation has been microfilmed exactly as received 68-10,753 PENCE n , Harry Edmond, 1937- PREPARATION AND SPECTRAL PROPERTIES OF OXOMOLYBDENUM(V) COMPLEXES. Louisiana State University and Agricultural and Mechanical College, Ph.D., 1968 Chemistry, inorganic University Microfilms, Inc., Ann Arbor, Michigan PREPARATION AND SPECTRAL PROPERTIES OF OXOMOLYBDENUM ( V) COMPLEXES A Dissertation Submitted to the Graduate Faculty of the Louisiana State University and Agricultural and Mechanical College in partial fulfillment of the requirements for the degree of Doctor of Philosophy in The Department of Chemistry by Harry Edmond Pence II B.S., Bethany College, Bethany, W.Va., 1958 M.S., West Virginia University, Morgantown, W.Va., 1962 February, 1968 To Ginn ACKNOWLEDGMENTS The final creation of this dissertation has been assisted by many different individuals and it is appropriate to attempt to indicate some of these contributors and offer the sincere thanks of the author,, The most important component of this assistance has been the continual encouragement offered by parents and family. -
Ucri, 100554 Preprint
UCRI, 100554 PREPRINT x CHEMICAL THERMODYNAMICS OF TECHNETIUM 0 r0 0 0m 0 Joseph A.' Rard z C w1 m This paper was prepared for inclusion in the book CHEMICAL THERMODYNAMICS OF TECHNETIUM (to' be published by the Nuclear Energy Agency, Paris, France) February 1989 This is a preprint of a paper intended for publication in a journal or proceedings. Since changes may be made before publication, this preprint is made available with the understanding that it will not be cited or reproduced without the permission of the author. - DISCILAIMER This document was prepared as an account of work sponsored by asnagency of the United States Government Neither the United States Government nor the University of California nor any of their employees. makes any warranty, express or implieid, or assumes any legal liability or responsibility for the accuracy completeness, or useful- ness of any Information, apparatus. product, or process disclosed. or represents that Its use would not Iafringe privately owned rights. Reference hereln to any specific commercial products, process, or service by trade name. trademark. manufacturer, or otherwise. does not necessarily constitute or Imply its endorsement. recommendation, or favoring by the United States Government or the University of California. The views and opinions of authors expressed hereb do not necessarily state or reflect those of the United States Government or the University of California, and shall not be used for advertising or product endorsement purposes. -W This manuscript by JA Rard is to be part of a book entitled "CHEMICAL THERMODYNAMICS OF TECHNETIUM". It will be published by the Nuclear Energy Agency Data Bank at Saclay, France. -
Agardite-(Y), Cu 6Y(Aso4)3(OH)6Á3H2O a = 13.5059 (5) a T = 293 K C = 5.8903 (2) A˚ 0.10 Â 0.02 Â 0.02 Mm
inorganic compounds Acta Crystallographica Section E Experimental Structure Reports Crystal data Online ˚ 3 Cu5.70(Y0.69Ca0.31)[(As0.83P0.17)O4]3- V = 930.50 (6) A ISSN 1600-5368 (OH)6Á3H2O Z =2 Mr = 985.85 Mo K radiation À1 Hexagonal, P63=m = 13.13 mm 2+ ˚ Agardite-(Y), Cu 6Y(AsO4)3(OH)6Á3H2O a = 13.5059 (5) A T = 293 K c = 5.8903 (2) A˚ 0.10 Â 0.02 Â 0.02 mm a b Shaunna M. Morrison, * Kenneth J. Domanik, Marcus J. Data collection a a Origlieri and Robert T. Downs Bruker APEXII CCD 20461 measured reflections diffractometer 786 independent reflections aDepartment of Geosciences, University of Arizona, 1040 E. 4th Street, Tucson, Absorption correction: multi-scan 674 reflections with I >2(I) Arizona 85721-0077, USA, and bLunar and Planetary Laboratory, University of (SADABS; Bruker, 2004) Rint = 0.048 Arizona, 1629 E. University Blvd., Tucson, AZ. 85721-0092, USA Tmin = 0.353, Tmax = 0.779 Correspondence e-mail: [email protected] Refinement Received 24 July 2013; accepted 21 August 2013 R[F 2 >2(F 2)] = 0.032 1 restraint wR(F 2) = 0.086 H-atom parameters not refined ˚ À3 Key indicators: single-crystal X-ray study; T = 293 K; mean () = 0.000 A˚; H-atom S = 1.14 Ámax = 2.34 e A ˚ À3 completeness 0%; disorder in main residue; R factor = 0.032; wR factor = 0.086; 786 reflections Ámin = À0.79 e A data-to-parameter ratio = 13.1. 60 parameters 2+ Agardite-(Y), with a refined formula of Cu 5.70(Y0.69Ca0.31)- Data collection: APEX2 (Bruker, 2004); cell refinement: SAINT 2+ [(As0.83P0.17)O4]3(OH)6Á3H2O [ideally Cu 6Y(AsO4)3(OH)6Á- (Bruker, 2004); data reduction: SAINT; program(s) used to solve structure: SHELXS97 (Sheldrick, 2008); program(s) used to refine 3H2O, hexacopper(II) yttrium tris(arsenate) hexahydroxide trihydrate], belongs to the mixite mineral group which is structure: SHELXL97 (Sheldrick, 2008); molecular graphics: Xtal- characterized by the general formula Cu2+ A(TO ) (OH) Á- Draw (Downs & Hall-Wallace, 2003); software used to prepare 6 4 3 6 material for publication: publCIF (Westrip, 2010). -
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). -
Occurrence and Crystal Structure of Calciopetersite from Monte Beni (Firenzuola, Florence, Tuscany, Italy)
Atti Soc. tosc. Sci. nat., Mem., Serie A, 116 (2011) pagg. 17-22, figg. 2, tabb. 4; doi: 10.2424/ASTSN.M.2011.03 C. Biagioni (*), E. Bonaccorsi (*), P. Orlandi (*) OCCURRENCE AND CRystal structure OF CALCIOPETERSITE from MONTE BENI (FIRENzUOLA, FLORENCE, TUSCANy, Italy) Abstract - The mixite group includes several hexagonal Introduction phosphates and arsenates, characterized by the general chem- ical formula MCu6(XO4)3(OH)6⋅3H2O. A phosphate belong- The mixite group is formed by a series of hexagonal ing to this group has been identified on samples collected at phosphates and arsenates, having the general chemical the Fantoni quarry (Monte Beni, Firenzuola, Florence), as formula MCu6(XO4)3(OH)6⋅3H2O. M is represented by tufts of acicular crystals with hexagonal section, blue-green 3+ 3+ 3+ 3+ 2+ 2+ 5+ 5+ in color, associated with chrysocolla. Semi-quantitative REE , y , Al , Bi , Ca , or Pb ; X can be As or P . chemical data point to a dominance of Ca over y, indicat- Up to now, only two natural phosphates have been ing that these samples could be classified as calciopetersite. described: petersite-(y) and calciopetersite. Petersite- The crystal structure of this mineral has been solved and (y), ideally yCu6(PO4)3(OH)6⋅3H2O, was described refined using intensity data collected through synchrotron by Peacor & Dunn (1982) and was found in very radiation, due to the extremely small size of the single crys- few localities world-wide; calciopetersite, ideally tals. Calciopetersite is hexagonal, space group P6 /m, cell 3 CaCu6(PO4)2(PO3OH)(OH)6⋅3H2O, is rarer than the parameters a 13.206(2), c 5.824(3) Å. -
Analyses of Rocks and Minerals
DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, DIRECTOR BULLETIN 419 ANALYSES OF ROCKS AND MINERALS FEOM THE LABORATORY OF THE UNITED STATES GEOLOGICAL SURVEY \ 1880 TO 1908 TABULATED BY F. W. CLARKE, CHIEF CHEMIST WASHINGTON GOVERNMENT PRINTING OFFICE 1910 CONTENTS. Page. Introduction.............................................................. 1 The average composition of rocks. ..'.....< .................................. 4 Analyses of igneous and crystalline rocks................................... 13 Maine. .................................................................... 13 1. Rocks from Aroostook County..... ^..................'........... 13 2. Miscellaneous rocks............................................. 14 New Hampshire....................................................... 15 Vermont............................................................... 15 1. Rocks of Mount Ascutney........................................ 15 2. Miscellaneous rocks.................:........................... 17 Massachusetts....:..............................................:..... .18 1. Magnesian rocks.............. ; .................................. 18 2. Amphibolite................................................... 19 3. Miscellaneous rocks............................................. 21 Connecticut............................................................ 24 New York............................................................. 26 1. Rocks of the Adirondack region................................... 26 2.