Synthesis and Molecular Transport Studies in Zeolites and Nanoporous Membranes
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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 -
Marinellite, a New Feldspathoid of the Cancrinite-Sodalite Group
Eur. J. Mineral. 2003, 15, 1019–1027 Marinellite, a new feldspathoid of the cancrinite-sodalite group ELENA BONACCORSI* and PAOLO ORLANDI Dipartimento di Scienze della Terra, Universita` di Pisa, Via S. Maria 53, I-56126 Pisa, Italy * Corresponding author, e-mail: [email protected] Abstract: Marinellite, [(Na,K)42Ca6](Si36Al36O144)(SO4)8Cl2·6H2O, cell parameters a = 12.880(2) Å, c = 31.761(6) Å, is a new feldspathoid belonging to the cancrinite-sodalite group. The crystal structure of a twinned crystal was preliminary refined in space group P31c, but space group P62c could also be possible. It was found near Sacrofano, Latium, Italy, associated with giuseppettite, sanidine, nepheline, haüyne, biotite, and kalsilite. It is anhedral, transparent, colourless with vitreous lustre, white streak and Mohs’ hardness of 5.5. The mineral does not fluoresce, is brittle, has conchoidal fracture, and presents poor cleavage on {001}. Dmeas is 3 3 2.405(5) g/cm , Dcalc is 2.40 g/cm . Optically, marinellite is uniaxial positive, non-pleochroic, = 1.495(1), = 1.497(1). The strongest five reflections in the X-ray powder diffraction pattern are [d in Å (I) (hkl)]: 3.725 (100) (214), 3.513 (80) (215), 4.20 (42) (210), 3.089 (40) (217), 2.150 (40) (330). The electron microprobe analysis gives K2O 7.94, Na2O 14.95, CaO 5.14, Al2O3 27.80, SiO2 32.73, SO3 9.84, Cl 0.87, (H2O 0.93), sum 100.20 wt %, less O = Cl 0.20, (total 100.00 wt %); H2O calculated by difference. The corresponding empirical formula, based on 72 (Si + Al), is (Na31.86K11.13Ca6.06) =49.05(Si35.98Al36.02)S=72O144.60(SO4)8.12Cl1.62·3.41H2O. -
26 May 2021 Aperto
AperTO - Archivio Istituzionale Open Access dell'Università di Torino The crystal structure of sacrofanite, the 74 Å phase of the cancrinite–sodalite supergroup This is the author's manuscript Original Citation: Availability: This version is available http://hdl.handle.net/2318/90838 since Published version: DOI:10.1016/j.micromeso.2011.06.033 Terms of use: Open Access Anyone can freely access the full text of works made available as "Open Access". Works made available under a Creative Commons license can be used according to the terms and conditions of said license. Use of all other works requires consent of the right holder (author or publisher) if not exempted from copyright protection by the applicable law. (Article begins on next page) 05 October 2021 This Accepted Author Manuscript (AAM) is copyrighted and published by Elsevier. It is posted here by agreement between Elsevier and the University of Turin. Changes resulting from the publishing process - such as editing, corrections, structural formatting, and other quality control mechanisms - may not be reflected in this version of the text. The definitive version of the text was subsequently published in MICROPOROUS AND MESOPOROUS MATERIALS, 147, 2012, 10.1016/j.micromeso.2011.06.033. You may download, copy and otherwise use the AAM for non-commercial purposes provided that your license is limited by the following restrictions: (1) You may use this AAM for non-commercial purposes only under the terms of the CC-BY-NC-ND license. (2) The integrity of the work and identification of the author, copyright owner, and publisher must be preserved in any copy. -
Information Clearance Review and Release Approval
INFORMATION CLEARANCE REVIEW AND RELEASE APPROVAL Part I: Background Information Title: TEST RESULTS FOR CAUSTIC DEMAND MEASUREMENTS Information Category: ON TANK 241-AX-101 AND TANK 241-AX-103 ARCHIVE SAMPLES 0 Abstract 0 Journal Article 0 Summary 0 Internet 0 Visual Aid 0 Software Publish to OSTI? 0 Yes □ No 0 Full Paper 0 Report 0 Other Yes NA Trademark/Copyright “Right to Use” Information or Permission Documentation O 0 Document Number: WRPS-1602862 Revision 0 Date: July 2016 Author: Doll, Stephanie R Part II: External/Public Presentation Information Conference Name: Sponsoring Organization(s): WRPS Date of Conference: Conference Location: Will Material be Handed Out? □ Yes 0 No Will Information be Published? □ Yes 0 No ^formatinstuctfons/guidance^1106 Part III: WRPS Document Originator Checklist Description Yes N/A Print/Sign/Date Information Product meets requirements in TFC-BSM-AD-C-01? o 0 Document Release Criteria in TFC-ENG-DESIGN-C-25 completed? 0 (Attach checklist) o If product contains pictures, safety review completed? 0 o Lindberg, Chandy IDMS Data File att. Part IV: WRPS Internal Review Function Organization Date Print Name/Signature/Date Subject Matter Expert WRPS 10/04/2016 Doll, Stephanie R IDMS Data File att. Responsible Manager WRPS 08/08/2016 Cooke, Gary A IDMS Data File att. Other: Part V: IRM Clearance Services Review Description Yes No Print Name/Signature Document Contains Classified Information? o H If Answer is “Yes,” ADC Approval Required Print Name/Signature/Date Document Contains Information Restricted by DOE Operational o 0 Reviewer Signature: Security Guidelines? Print Name/Signature/Date Document is Subject to Release Restrictions? o H Document contains: If theanswer is “Yes, ” please mark category at right and describe 0 Applied Technology 0 Protected CRADA limitation or responsible organization below: 0 Personal/Private 0 Export Controlled 0 Proprietary 0 Procurement - Sensitive 0 Patentable Info. -
Crystal Chemistry of Cancrinite-Group Minerals with an Ab-Type Framework: a Review and New Data
1151 The Canadian Mineralogist Vol. 49, pp. 1151-1164 (2011) DOI : 10.3749/canmin.49.5.1151 CRYSTAL CHEMISTRY OF CANCRINITE-GROUP MINERALS WITH AN AB-TYPE FRAMEWORK: A REVIEW AND NEW DATA. II. IR SPECTROSCOPY AND ITS CRYSTAL-CHEMICAL IMPLICATIONS NIKITA V. CHUKANOV§ Institute of Problems of Chemical Physics, 142432 Chernogolovka, Moscow Oblast, Russia IGOR V. PEKOV, LYUDMILA V. OLYSYCH, NATALIA V. ZUBKOVA AND MARINA F. VIGASINA Faculty of Geology, Moscow State University, Leninskie Gory, 119992 Moscow, Russia ABSTRACT We present a comparative analysis of powder infrared spectra of cancrinite-group minerals with the simplest framework, of AB type, from the viewpoint of crystal-chemical characteristics of extra-framework components. We provide IR spectra for typical samples of cancrinite, cancrisilite, kyanoxalite, hydroxycancrinite, depmeierite, vishnevite, pitiglianoite, balliranoite, davyne and quadridavyne, as well as the most unusual varieties of cancrinite-subgroup minerals (Ca-deficient cancrinite, H2O-free cancrinite, intermediate members of the series cancrinite – hydroxycancrinite, cancrinite–cancrisilite, cancrinite– kyanoxalite, K-rich vishnevite, S2-bearing balliranoite). Samples with solved crystal structures are used as reference patterns. Empirical trends and relationships between some parameters of IR spectra, compositional characteristics and unit-cell dimensions 2– are obtained. The effect of Ca content on stretching vibrations of CO3 is explained in the context of the cluster approach. The existence of a hydrous variety of quadridavyne is demonstrated. Keywords: cancrinite, cancrisilite, kyanoxalite, hydroxycancrinite, depmeierite, vishnevite, pitiglianoite, balliranoite, davyne, quadridavyne, cancrinite group, infrared spectrum, crystal chemistry. SOMMAIRE Nous présentons une analyse comparative des spectres infrarouges obtenus à partir de poudres de minéraux du groupe de la cancrinite ayant la charpente la plus simple, de type AB, du point de vue des caractéristiques cristallochimiques des composantes externes à la charpente. -
Geology of Greenland Survey Bulletin 190, 25-33
List of all minerals identified in the Ilímaussaq alkaline complex, South Greenland Ole V. Petersen About 220 minerals have been described from the Ilímaussaq alkaline complex. A list of all minerals, for which proper documentation exists, is presented with formulae and references to original publications. The Ilímaussaq alkaline complex is the type locality for 27 minerals including important rock-forming minerals such as aenigmatite, arfvedsonite, eudialyte, poly- lithionite, rinkite and sodalite. Nine minerals, chalcothallite, karupmøllerite-Ca, kvanefjeldite, nabesite, nacareniobsite-(Ce), naujakasite, rohaite, semenovite and sorensenite appear to be unique to the Ilímaussaq complex. Geological Museum, University of Copenhagen, Øster Voldgade 5–7, DK-1350 Copenhagen K, Denmark. E-mail: [email protected] Keywords: agpaite, Ilímaussaq, mineral inventory, minerals type locality The agpaitic complexes Ilímaussaq (South Greenland), world. Most of the minerals for which Ilímaussaq is Khibina and Lovozero (Kola Peninsula, Russia), and the type locality have later been found in other com- Mont Saint-Hilaire (Quebec, Canada) are among the plexes of agpaitic rocks. areas in the world which are richest in rare minerals. Two minerals were described simultaneously from About 700 minerals have been found in these com- Ilímaussaq and the Kola Peninsula, tugtupite and vi- plexes which hold the type localities for about 200 tusite. Tugtupite was published from the Lovozero minerals. complex by Semenov & Bykova (1960) under the name About 220 minerals have been found in the Ilímaus- beryllosodalite and from Ilímaussaq by Sørensen (1960) saq complex of which 27 have their type localities under the preliminary name beryllium sodalite which within the complex. In comparison Khibina and Lov- was changed to tugtupite in later publications (Søren- ozero hold the type localities for 127 minerals (Pekov sen 1962, 1963). -
Italian Type Minerals / Marco E
THE AUTHORS This book describes one by one all the 264 mi- neral species first discovered in Italy, from 1546 Marco E. Ciriotti was born in Calosso (Asti) in 1945. up to the end of 2008. Moreover, 28 minerals He is an amateur mineralogist-crystallographer, a discovered elsewhere and named after Italian “grouper”, and a systematic collector. He gradua- individuals and institutions are included in a pa- ted in Natural Sciences but pursued his career in the rallel section. Both chapters are alphabetically industrial business until 2000 when, being General TALIAN YPE INERALS I T M arranged. The two catalogues are preceded by Manager, he retired. Then time had come to finally devote himself to his a short presentation which includes some bits of main interest and passion: mineral collecting and information about how the volume is organized related studies. He was the promoter and is now the and subdivided, besides providing some other President of the AMI (Italian Micromineralogical As- more general news. For each mineral all basic sociation), Associate Editor of Micro (the AMI maga- data (chemical formula, space group symmetry, zine), and fellow of many organizations and mine- type locality, general appearance of the species, ralogical associations. He is the author of papers on main geologic occurrences, curiosities, referen- topological, structural and general mineralogy, and of a mineral classification. He was awarded the “Mi- ces, etc.) are included in a full page, together cromounters’ Hall of Fame” 2008 prize. Etymology, with one or more high quality colour photogra- geoanthropology, music, and modern ballet are his phs from both private and museum collections, other keen interests. -
Combined Single-Crystal X-Ray and Neutron Powder Diffraction Structure
American Mineralogist, Volume 95, pages 519–526, 2010 Combined single-crystal X-ray and neutron powder diffraction structure analysis exemplified through full structure determinations of framework and layer beryllate minerals JENNIFER A. ARMSTRONG ,1 HENRIK FRIIS,2 ALEX A NDR A LIEB ,1,* ADRI A N A. FINC H ,2 A ND MA RK T. WELLER 1,† 1School of Chemistry, University of Southampton, Highfield, Southampton, Hampshire SO17 1BJ, U.K. 2School of Geography and Geosciences, Irvine Building, University of St. Andrews, North Street, St. Andrews, Fife KY16 9AL, U.K. ABSTR A CT Structural analysis, using neutron powder diffraction (NPD) data on small quantities (<300 mg) and in combination with single-crystal X-ray diffraction (SXD) data, has been employed to determine accurately the position of hydrogen and other light atoms in three rare beryllate minerals, namely bavenite, leifite/IMA 2007-017, and nabesite. For bavenite, leifite/IMA 2007-017, and nabesite, sig- nificant differences in the distribution of H, as compared to the literature using SXD analysis alone, have been found. The benefits of NPD data, even with small quantities of H-containing materials, and, more generally, in applying a combined SXD-NPD method to structure analysis of minerals are discussed, with reference to the quality of the crystallographic information obtained. Keywords: Hydrogen, beryllium, minerals, powder neutron diffraction INTRODUCTION lower cation charge, Be2+ vs. Si4+. Thus, a bridging or terminal Information on crystal structure of minerals, including the O forming part of a Beϕ4 tetrahedron is under-bonded compared localization of light atoms such as H and Be, is of considerable to the equivalent Siφ4 unit leading to the prevalence of Be-OH importance because it allows a better understanding of the min- and Be-F in beryllate minerals (Hawthorne and Huminicki eral behavior under natural conditions. -
GEUS No 190.Pmd
G E O L O G Y O F G R E E N L A N D S U R V E Y B U L L E T I N 1 9 0 · 2 0 0 1 The Ilímaussaq alkaline complex, South Greenland: status of mineralogical research with new results Edited by Henning Sørensen Contributions to the mineralogy of Ilímaussaq, no. 100 Anniversary volume with list of minerals GEOLOGICAL SURVEY OF DENMARK AND GREENLAND MINISTRY OF THE ENVIRONMENT 1 Geology of Greenland Survey Bulletin 190 Keywords Agpaite, alkaline, crystallography, Gardar province, geochemistry, hyper-agpaite, Ilímaussaq, mineralogy, nepheline syenite, peral- kaline, Mesoproterozoic, rare-element minerals, South Greenland. Cover Igneous layering in kakortokites in the southern part of the Ilímaussaq alkaline complex, South Greenland. The central part of the photograph shows the uppermost part of the layered kakortokite series and the overlying transitional kakortokites and aegirine lujavrite on Laksefjeld (680 m), the dark mountain in the left middle ground of the photograph. The cliff facing the lake in the right middle ground shows the kakortokite layers + 4 to + 9. The kakortokite in the cliff on the opposite side of the lake is rich in xenoliths of roof rocks of augite syenite and naujaite making the layering less distinct. On the skyline is the mountain ridge Killavaat (‘the comb’), the highest peak 1216 m, which is made up of Proterozoic granite which was baked and hardened at the contact to the intrusive complex. The lake (987 m) in the foreground is intensely blue and clear because it is practically devoid of life. -
1) Parodi, G.C., Della Ventura, G. (1987) Steacyite from the Rouma Isle (Los Island, Republic of Guinea)
PUBLICATIONS IN PEER REVIEWED JOURNALS 1) Parodi, G.C., Della Ventura, G. (1987) Steacyite from the Rouma Isle (Los Island, Republic of Guinea). Neues Jahrbuch für Mineralogie, Mon., 5, 233-239. 2) Della Ventura, G., Maras, A., Parodi, G.C. (1987) Nonmetamict U-rich ekanite from Pitigliano (Tuscany, Italy). Rendiconti Accademia dei Lincei, s.8, 80, 585-592. 3) Robert, J.L., Della Ventura, G. e Thauvin, J.-L. (1989) The infrared OH-stretching region of synthetic richterites in the system Na2O-K2O-CaO-MgO-SiO2-H2O-HF. European Journal of Mineralogy, 1, 203-211. 4) Parodi, G. C., Della Ventura, G., Lorand, J.-P. (1989) Mineralogy and petrology of an unusual osumilite + vanadium-rich pseudobrookite assemblage in a ejectum from the Vico Volcanic Complex (Latium, Italy). American Mineralogist, 74, 1278-1284. 5) Della Ventura, G., Robert, J.-L. (1990) Synthesis, XRD and FT-IR studies of strontium richterites. European Journal of Mineralogy, 2, 171-175. 6) Della Ventura, G., Parodi, G.C., Mottana, A. (1990) New Rare Earth Minerals in the Sanidinitic ejecta within Pyroclastic rocks of the Roman Potassic Province. Rendiconti Accademia dei Lincei, s. 9, 1, 159- 163. 7) Mottana, A., Paris, E., Della Ventura, G., Robert, J.-L. (1990) Spectroscopic evidence for tetrahedrally-coordinated titanium in richteritic amphiboles. Rendiconti Accademia dei Lincei, s. 9, 1, 387-392. 8) Mottana, A., Della Ventura, G., Parodi, G.C., Guidi, G. (1990) A calcian member of the ganophyllite group in the manganiferous metacherts of Molinello mine, Liguria, Italy. Rendiconti Accademia dei Lincei, s. 9, 1, 313-317. 9) Della Ventura, G., Robert, J.-L., Bény, J.-M. -
Vishnevite (Na; Ca; K)6(Si; Al)12O24[(SO4); (CO3); Cl2]2 4 ² Nh2o ¡ C 2001 Mineral Data Publishing, Version 1.2 ° Crystal Data: Hexagonal
Vishnevite (Na; Ca; K)6(Si; Al)12O24[(SO4); (CO3); Cl2]2 4 ² nH2O ¡ c 2001 Mineral Data Publishing, version 1.2 ° Crystal Data: Hexagonal. Point Group: 6: As prismatic crystals and irregular granular masses. Physical Properties: Cleavage: Perfect on 1010 , poor on 0001 . Hardness = 5{6 D(meas.) = 2.32{2.42 D(calc.) = 2.37 f g f g Optical Properties: Transparent to translucent. Color: Pale lilac, light blue to dark gray. Optical Class: Uniaxial ({). ! = 1.490{1.507 ² = 1.488{1.495 Cell Data: Space Group: P 63: a = 12.685(6) c = 5.179(1) Z = 1 X-ray Powder Pattern: Russia. 3.273 (100), 3.695 (88), 2.769 (65), 4.742 (50), 2.649 (28), 2.101 (27), 6.4 (25) Chemistry: (1) (2) (1) (2) SiO2 37.24 34.76 K2O 4.89 1.29 + Al2O3 29.64 30.81 H2O 2.30 CaO 0.52 3.87 H2O¡ 0.20 SrO 0.32 CO2 1.90 Na2O 20.08 18.90 SO3 6.97 5.93 Total [99.34] 100.28 (1) Vishnevy Mountains, Russia; by electron microprobe, original total given as 99.35%; corresponds to (Na6:47K1:04Ca0:09)§=7:60(Si6:19Al5:81)§=12:00O24(SO4)0:87: (2) Allt a' Mhuillin, Scotland; corresponds to (Na6:19Ca0:70K0:28Sr0:03)§=7:20(Si5:87Al6:13)§=12:00O23:71 [(SO4)0:75(CO3)0:44]§=1:19 ² 1:41H2O: Mineral Group: Cancrinite group. Occurrence: In poikilitic aegirine-nepheline-sodalite syenites and associated pegmatites. Association: Aegirine, nepheline, cancrinite, sodalite, scolecite. Distribution: From the Kurochkin Valley, Vishnevy-Ilmen Mountains, Southern Ural Mountains; on Mts. -
An Introduction to the Rock-Forming Minerals
Downloaded from http://pubs.geoscienceworld.org/books/book/chapter-pdf/3751723/9780903056434_frontmatter.pdf by guest on 28 September 2021 An Introduction to the Rock-Forming Minerals Third Edition W. A. DEER{, FRS Emeritus Professor of Mineralogy & Petrology, University of Cambridge R. A. HOWIE{ Emeritus Professor of Mineralogy, University of London J. ZUSSMAN Emeritus Professor of Geology, University of Manchester { Sadly, Professors Deer and Howie died while this edition was in preparation The Mineralogical Society London Downloaded from http://pubs.geoscienceworld.org/books/book/chapter-pdf/3751723/9780903056434_frontmatter.pdf by guest on 28 September 2021 The Mineralogical Society First published 1966 Second edition 1992 Third edition 2013 # W. A. Deer, R. A. Howie and J. Zussman 1966 Second edition # W. A. Deer, R. A. Howie and J. Zussman 1992 This edition # W. A. Deer, R. A. Howie and J. Zussman 2013 All rights reserved; no part of this publication may be reproduced, stored in a retrieval system, or transmitted in any form or by any means, electronic, mechanical, photocopying, recording, or otherwise without either the prior written permission of the Publishers or a licence permitting restricted copying in the United Kingdom issued by the Copyright Licensing Agency Ltd, 90 Tottenham Court Road, London W1P 9HE. First published 1966 Second edition 1992 Third edition 2013 British Library Cataloguing in Publication Data Deer, W. A. An introduction to the rock-forming minerals. – 3rd ed. I. Title II. Howie, R. A. III. Zussman, J. 549 ISBN 978-0903056-33-5 Library of Congress Cataloging-in-Publication Data Deer, W. A. (William Alexander) An introduction to the rock-forming minerals/W.