Crystal Structure Transformations in Inorganic Sulfates, Phosphates, Perchlorates, and Chromates Based on the Literature up to 1974
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Supramolecular Materials
This is a repository copy of Supramolecular Materials. White Rose Research Online URL for this paper: https://eprints.whiterose.ac.uk/115714/ Version: Accepted Version Article: Amabilino, David, Smith, David Kelham orcid.org/0000-0002-9881-2714 and Steed, Jon (2017) Supramolecular Materials. Chemical Society Reviews. pp. 2404-2420. ISSN 0306- 0012 https://doi.org/10.1039/c7cs00163k Reuse Items deposited in White Rose Research Online are protected by copyright, with all rights reserved unless indicated otherwise. They may be downloaded and/or printed for private study, or other acts as permitted by national copyright laws. The publisher or other rights holders may allow further reproduction and re-use of the full text version. This is indicated by the licence information on the White Rose Research Online record for the item. Takedown If you consider content in White Rose Research Online to be in breach of UK law, please notify us by emailing [email protected] including the URL of the record and the reason for the withdrawal request. [email protected] https://eprints.whiterose.ac.uk/ CREATED USING THE RSC ARTICLE TEMPLATE (VER. 3.0) - SEE WWW.RSC.ORG/ELECTRONICFILES FOR DETAILS ARTICLE TYPE www.rsc.org/xxxxxx | XXXXXXXX Supramolecular Materials David B. Amabilino,a David K. Smith b and Jonathan W. Steed c Received (in XXX, XXX) 1st January 2017, Accepted 1st January 2017 First published on the web 1st January 2017 5 DOI: 10.1039/b000000x Molecular material properties depend upon the contacts between and the arrangement of the component parts, and therefore supramolecular chemistry has developed a highly important role in this area. -
Observation of Quadrupole Helix Chirality and Its Domain Structure in Dyfe3(BO3)4
ARTICLES PUBLISHED ONLINE: 6 APRIL 2014 | DOI: 10.1038/NMAT3942 Observation of quadrupole helix chirality and its domain structure in DyFe3(BO3)4 T. Usui1, Y. Tanaka2, H. Nakajima1, M. Taguchi2, A. Chainani2, M. Oura2, S. Shin2, N. Katayama3, H. Sawa3, Y. Wakabayashi1 and T. Kimura1* Resonant X-ray diraction (RXD) uses X-rays in the vicinity of a specific atomic absorption edge and is a powerful technique for studying symmetry breaking by motifs of various multipole moments, such as electric monopoles (charge), magnetic dipoles (spin) and electric quadrupoles (orbital). Using circularly polarized X-rays, this technique has been developed to verify symmetry breaking eects arising from chirality, the asymmetry of an object upon its mirroring. Chirality plays a crucial role in the emergence of functionalities such as optical rotatory power and multiferroicity. Here we apply spatially resolved RXD to reveal the helix chirality of Dy 4f electric quadrupole orientations and its domain structure in DyFe3(BO3)4, which shows a reversible phase transition into an enantiomorphic space-group pair. The present study provides evidence for a helix chiral motif of quadrupole moments developed in crystallographic helix chirality. t is well known that chirality often plays a critical role in various detect not only crystallographic helix handedness but also the disciplines, such as biology, organic chemistry and particle chirality ascribed to the periodic motif of multipole moments, such Iphysics1,2. In contrast, chirality in solid-state physics, which as magnetic dipoles and electric quadrupoles12–14. In the case of is largely concerned with crystals possessing periodic arrays of magnetic dipoles, the handedness of a `helical magnetic structure' atoms, has attracted less attention. -
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 -
SYMMETRY of PHOSPHOSIDERITE Duncelc Mcconnbr.L, The
SYMMETRY OF PHOSPHOSIDERITE DuNcelc McCoNNBr.l, The Uniaersity of Teras, Austin, Teras INrnooucuoN Prior to the description of crystals lrom Sardinia by M. de Angelis (l) in 1926, phosphosiderite was supposed to exhibit the external sym- metry of a substance belonging to the orthorhombic holohedral class. This mineral had been investigated by H. Laubmann and H. Steinmetz (2) as well as the authors who originally described the mineral, W. Bruhns and K. Busz (3). More recently phosphosideritehas been de- scribedfrom Kirunavara, Sweden,by R. Koechlin (4). De Angelis demonstrated that the symmetry is monoclinic on the basis of three difierent types of evidence: (1) The etch figures on the basal pinakoid do not exhibit planar symmetry with respect to a plane normal to the o axis, nor axial sym- metry with respect to the c axis (Fig. 4). (2) The goniometric measurementscannot be reconciled with ortho- rhombic axes of reference,but are quite amenable to monoclinic axes wittr B:89"24t. Certain prominent faces are not repeated as required by orthorhombic symmetry. (3) The optical data are not consistent with orthorhombic symmetry, becauseX Ac> J-3". Before the appearanceof the work by De Angelis, W. T. Schaller (5) had pointed out the marked similarity between the compositions,crystal habits and axial ratios of phosphosiderite and metavariscite [formerly called variscite (6)] and he had suggestedthe possibility of an isodimor- phous series: Octahedral Habit Tabular Habit Scorodite Strengite Phosphosiderite Variscite Metavariscite P. Kokkoros (7) has recently shown that scorodite and strengite are isostructural and the writer has found that variscite produces a powder diffraction pattern sufficiently similar to indicate that it also belongs to this group. -
38Th RMS Program Notes
E.fu\wsoil 'og PROGRAM Thursday Evening, April 14, 2011 PM 4:00-6:00 Cocktails and Snacks – Hospitality Suite 400 (4th Floor) 6:00-7:45 Dinner – Baxter’s 8:00-9:15 THE GUALTERONI COLLECTION: A TIME CAPSULE FROM A CENTURY AGO – Dr. Renato Pagano In 1950, the honorary curator of the Museum of Natural History in Genoa first introduced Dr. Renato Pagano to mineral collecting as a Boy Scout. He has never looked back. He holds a doctorate in electrical engineering and had a distinguished career as an Italian industrialist. His passion for minerals has produced a collection of more than 13,000 specimens, with both systematic and aesthetic subcollections. His wife Adriana shares his passion for minerals and is his partner in collecting and curating. An excellent profile of Renato, Adriana, and their many collections appeared earlier this year in Mineralogical Record (42:41-52). Tonight Dr. Pagano will talk about an historic mineral collection assembled between 1861 and 1908 and recently acquired intact by the Museum of Natural History of Milan. We most warmly welcome Dr. Renato Pagano back to the speakers’ podium. 9:15 Cocktails and snacks in the Hospitality Suite on the 4th floor will be available throughout the rest of the evening. Dealers’ rooms will be open at this time. All of the dealers are located on the 4th floor. Friday Morning, April 15, 2011 AM 9:00 Announcements 9:15-10:15 CRACKING THE CODE OF PHLOGOPITE DEPOSITS IN QUÉBEC (PARKER MINE), MADAGASCAR (AMPANDANDRAVA) AND RUSSIA (KOVDOR) – Dr. Robert F. Martin Robert François Martin is an emeritus professor of geology at McGill University in Montreal. -
The Use of Raman Spectroscopy in the Characterization of Variscite Provenance: the Gavà Case
Chapitre III : Apport des méthodes d’analyses à l’étude de la diffusion des productions The use of Raman spectroscopy in the characterization of variscite provenance: the Gavà case Joan Carlos Melgarejo, Laia Arqués, Cristina Villanova-de-Benavent, Tariq Jahwari, Lisard Torró, Josep Bosch Argilagós, Montgarri Castillo-Oliver, Marc Campeny, Sandra Amores, Aleu Andreazini, Saleh Lehbib, Antoni Camprubí Abstract. The Gavà phosphate deposit, mined during the Neolithic, was produced by weathering processes affecting primary apatite beds. It exhibits a neat vertical zoning, related to chemical gradients during weathering. Strengite, yellowish Al-rich strengite and ferroan variscite are found at the top, pale- green variscite at the intermediate levels, and green variscite in depth. Fe values are very low in the greenish samples, as well as Cr and V. Raman spectrums of the Gavà variscite show differences with samples from other occurrences worldwide. Moreover, some spectral differences can also be observed in the Raman spectra of variscite coming from different depths in the deposit. Raman spectroscopy can be an efficient tool to discriminate not only samples from different geographical localities, but also from its original position in a given deposit. Key-words: variscite, Raman, microprobe, veins, supergene. Résumé. Le gîte de phosphates de Gavà, exploité au Néolithique, s’est formé par des processus de météorisation qui auraient affecté des strates primaires d’apatite. Ce gîte a une zonation chimique verticale, qui aurait été produite par des gradations chimiques lors de la météorisation. La partie haute du gîte contient de la strengite, de l’Al-strengite et de la Fe-variscite jaunâtres ; les niveaux intermédiaires contiennent de la variscite verdâtre et les niveaux plus profonds, de la variscite verte. -
NEW MINERALS It Is Proposed Hereafter to Indicate In.A General Way the Classification of All New Minerals Recoided in This Department
JOURNAL MINERALOGICAL SOCIETY OF AMENICA 63 Dr. Kunz then spoke of the various city localities and the minerals found therein. He stated that the East Side, from 37 to 110 St., probably afforded the most specimens. The various tunnels and their minerals were spoken of. Capt. Miller called attention to the fine collection of Brooklyn Drift Minerals and Rocks in the collection of the Long Island Historical Society. Ife abo mentioned the occurrence of monazite and xenotime crystals, on the Speedway,Harlem River. Dr. Kunz emphasizedthe irnportance of complete records being kept of all finds. Tnou,q,s L Mrr,r,nn, SecretaryPro, Tem. NEW MINERALS It is proposed hereafter to indicate in.a general way the classification of all new minerals recoided in this department. Subdivision will be first into "families," of which nine may be recognized,as listed in the January number (Am. Min.6 (1), 12,1921). Eachfamilywillbe separatedinto "subfamilies " based on special features of composition. This arrangement is tentative and open to modification, and criticism of it will be welcome, [Eo.] FAMILY 2. SULFIDES, ETC. SosreMrr,v 3. Doust,u suLFrDEs oF METALSAND sEMr-METAr,s. I'LTRABASITE V. Rosrcxf and J. Srnnse-Btinu. Ultrabasit, ein neues Mineral aus Freiberg in Sachsen. (Ultrabasite, a new mineral from Freiberg, Saxony). Rozpr.Eeslcd Ako,il. Prag,25, No. 45, 1916;Z. Krgst. Min., 55,43H39, 1920, Neun: From its extremely basic chemical composition. Pnrsrcar, Pnopnnrrus Color black, somewhat grayish; luster metallic; streak black; cleavage none; fracture scaly, with somewhat greasy luster on the surface. H. : 5; sp. gr. -
New Mineral Names*
American Mineralogist, Volume 75, pages 240-246, 1990 NEW MINERAL NAMES* JOHN L. JAMBOR CANMET, 555 Booth Street, Ottawa, Ontario KIA OGI, Canada EDWARD S. GREW Department of Geological Sciences, University of Maine, Orono, Maine 04469, U.S.A. Baiyuneboite-(Ce) the formula for cordylite-(Ce) requires revision such that Pigqiu Fu, Xlanze Su (1987) Baiyuneboite-A new min- cordylite-(Ce) and baiyuneboite-(Ce) may be identical. The eral. Acta Mineralogica Sinica, 7, 289-297 (in Chinese, Chairman therefore withdrew the approval and asked that English abstract). the authors withhold publication of their description of Pingqiu Fu, Youhua Kong, Guohong Gong, Meicheng baiyuneboite-(Ce) until the matter could be resolved. The Shao, Jinzi Qian (1987) The crystal structure of bai- request, unfortunately, was ignored. J.L.J. yuneboite-(Ce). Acta Mineralogica Sinica, 7, 298-304 (in Chinese, English abstract). Diaoyudaoite* Electron-microprobe analyses of ten grains, whose va- lidity was checked by single-crystal X-ray methods prior Shunxi Shen, Lirong Chen, Anchun Li, Tailu Dong, Qiu- to analysis, gave an average ofNa20 4.73, CaO 1.04, BaO huo Huang, Wenqiang Xu (1986) Diaoyudaoite-A new 20.38, Ce20, 24.21, La20, 10.92, Pr20, 0.62, Nd20, 10.04, mineral. Acta Mineralogica Sinica, 6, 224-227 (in Gd20, 0.13, F 2.50, C02 (by gas chromatography) 24.64, Chinese, English abstract). o == F 1.05, sum 98.16 wt%, corresponding to Nal.OS- The average of 13 electron-microprobe analyses gave (BaO.94CaO.I,)n07( Ce I.OSLao.4sN do.42Pr 0.0'Gdo.OI)"1.99F 0.9'C,.97- Na20 4.54, AI20, 93.00, Cr20, 1.95, MgO 0.10, CaO 0.10, 012.07'ideally NaBaCe2F(CO')4' The mineral occurs as yel- SiOz 0.23, K20 0.12, sum 100.04 wt%, corresponding to low, irregular grains 0.3 to 3 mm in size, frequently as (N ao.87Ko.ozMgo.02CaO.01)ro.92(AllO.84CrO.lsSio.02)"'1.01 0,7, ide- thin hexagonal tablets. -
Strengite.Pdf
3+ Strengite Fe PO4 • 2H2O c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Orthorhombic. Point Group: 2/m 2/m 2/m. Crystals are variable in habit, may be dominated by {111}, lathlike along [001], or elongated along [100] or [010], to 5 cm, with many forms. Generally radial fibrous, as botryoidal or spherical aggregates and crusts. Twinning: Rarely on {201}. Physical Properties: Cleavage: On {010}, good; on {001}, poor. Hardness = 3.5 D(meas.) = 2.84–2.87 D(calc.) = 2.84 Optical Properties: Transparent to translucent. Color: Purple, violet, pink, peach-blossom- red, carmine, greenish white; may be nearly colorless. Streak: White. Luster: Vitreous. Optical Class: Biaxial (+). Orientation: X = a; Y = c; Z = b. Dispersion: r< v,strong. α = 1.697–1.708 β = 1.708–1.719 γ = 1.741–1.745 2V(meas.) = Moderate to small. Cell Data: Space Group: P cab. a = 10.122(1) b = 9.886(1) c = 8.7233(7) Z = 8 X-ray Powder Pattern: The Kreuzberg, Germany. (ICDD 33–667). 3.114 (100), 4.383 (85), 5.509 (60), 2.546 (50), 3.996 (45), 3.002 (45), 2.949 (45) Chemistry: (1) (2) P2O5 38.24 37.99 Fe2O3 43.40 42.73 H2O 18.89 19.28 Total 100.53 100.00 • (1) Pleystein, Germany. (2) FePO4 2H2O. Polymorphism & Series: Dimorphous with phosphosiderite, forms a series with variscite. Mineral Group: Variscite group. Occurrence: A late secondary mineral in complex granite pegmatites; in “limonite” iron ores and gossans; with magnetite iron ores; rarely a cave mineral. Association: Beraunite, hur´eaulite,dufr´enite,bermanite, stewartite, cacoxenite, rockbridgeite, vivianite, apatite, leucophosphite, phosphosiderite. -
Fall ¥ Pages 17-32
The Role of Electrochemical Power Sources in Modern Health Care by Curtis F. Holmes t has been more than forty years since the first implantable pacemaker was implanted into an animal. Two years later, in 1960, the first successful pace- maker was implanted into a human. This event ushered in an era of battery- powered biomedical devices that have played an increasingly important role in health care.1 I Today a variety of battery powered implantable devices are routinely implanted into patients to treat ailments ranging from irregular heartbeat to pain and epilepsy. Moreover, a wide variety of battery powered external devices are used to administer drugs, treat ailments, and monitor bodily functions. Battery powered devices thus play a very important role in the treatment of disease. This paper will discuss some of the more common applications of batteries in medical devices. The Cardiac Pacemaker In the 1950s it became common to treat a patient suffering from bradycardia with an external pacemaker which applied electrical shocks through the skin. The first units were powered by normal line power. The treatment was painful and patient mobility was severely restricted. Later a battery-powered hand-held device was developed by Earl Bakken and was used with myocardial leads, which eliminated much of the discomfort caused by the earlier line-powered units. The invention of the transistor in the 1950s provided the possibility of creating an implantable battery-powered pacemaker. Great- batch and Chardack in the U.S. and Sennig in Sweden were both pursuing this goal.2 The Greatbatch/Chardack team succeeded in pro- ducing a device powered by zinc/mercuric oxide cells. -
Phase Behavior of Ag2cro4 Under Compression
Article pubs.acs.org/JPCC Phase Behavior of Ag2CrO4 under Compression: Structural, Vibrational, and Optical Properties † ‡ † † † § ∥ David Santamaría-Perez,́ *, , Enrico Bandiello, Daniel Errandonea, Javier Ruiz-Fuertes, , Oscar Gomis, ⊥ ⊥ # # Juan Angel Sans, Francisco Javier Manjon,́ Placidá Rodríguez-Hernandez,́ and Alfonso Muñoz † Departamento de Física Aplicada-ICMUV, MALTA Consolider Team, Universidad de Valencia, C/Dr. Moliner 50, Burjassot, 46100 Valencia, Spain ‡ Departamento de Química Física I, Universidad Complutense de Madrid, MALTA Consolider Team, Avenida Complutense s/n, 28040 Madrid, Spain § Lyman Laboratory of Physics, Harvard University, Cambridge, Massachusetts 02138, United States of America ∥ Centro de Tecnologías Físicas: Acustica,́ Materiales y Astrofísica, MALTA Consolider Team, Universitat Politecnicà de Valencia,̀ 46022 Valencia,̀ Spain ⊥ Instituto de Diseño para la Fabricacioń y Produccioń Automatizada, MALTA Consolider Team, Universitat Politecnicà de Valencia,̀ 46022 Valencia,̀ Spain # Departamento de Física Fundamental II, Instituto de Materiales y Nanotecnología, MALTA Consolider Team, Universidad de La Laguna, 38205 Tenerife, Spain ABSTRACT: We have performed an experimental study of the crystal structure, lattice dynamics, and optical properties of silver chromate (Ag2CrO4) at ambient temperature and high pressures. In particular, the crystal structure, Raman-active phonons, and electronic band gap have been accurately determined. When the initial orthorhombic Pnma Ag2CrO4 structure (phase I) is compressed up to 4.5 GPa, a previously undetected phase (phase II) has been observed with a 0.95% volume collapse. The structure of phase II can be indexed to a similar orthorhombic cell as phase I, and the transition can be considered to be an isostructural transition. This collapse is mainly due to the drastic contraction of the a axis (1.3%). -
Minerals from the Cioclovina Cave, Romania: a Review
Studia Universitatis Babeş-Bolyai, Geologia, 2007, 52 (2), 3 - 10 High-temperature and “exotic” minerals from the Cioclovina Cave, Romania: a review Bogdan P. ONAC1,2 *, Herta S. EFFENBERGER3 & Radu C. BREBAN4 1 Department of Geology, University of South Florida, 4202 E. Fowler Ave., SCA 528, Tampa, FL 33620, USA 2 Department of Mineralogy, „Babeş-Bolyai“ University, Kogălniceanu 1, 400084 Cluj Napoca, Romania „Emil Racoviţă“ Institute of Speleology, Clinicilor 5, 400006 Cluj Napoca, Romania 3 Institut für Mineralogie und Kristallographie, Universität Wien, Althanstraße 14, 1090 Wien, Austria 4 SpeleoClub “Proteus”, Aleea Pescarilor, Bl. 30/47, Deva, Hunedoara, Romania Received November 2006; accepted February 2007 Available online 17 August 2007 ABSTRACT. This paper reports on the identification of four rare minerals in the phosphate deposit in Cioclovina Cave, Romania. Berlinite, AlPO4 and hydroxylellestadite, Ca5[(Si,P,S)O4]3(OH,F,Cl) are minerals that can form only at high temperatures, and would not be expected in a sedimentary environment. In this study we review the characteristics of berlinite and hydroxylellestadite from a heated sedimentary sequence in Cioclovina Cave (Romania) and refine their structure from single-crystal X-ray data. Two other minerals, churchite-(Y), YPO4⋅2H2O and foggite, CaAl(PO4)(OH)2⋅H2O are, for the first time, described from a cave environment. The minerals were documented by means of single-crystal X-ray investigations, X-ray powder diffraction, and electron-microprobe (EMPA) analyses. In addition, laboratory synthesis of berlinite was conducted and vibrational spectroscopy data were collected for hydroxylellestadite and churchite-(Y). Based on these investigations, we suggest that locally the heavily compacted phosphate-bearing clay sediments underwent a natural heating process.