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This Is the Author Version Published As: QUT Digital Repository
QUT Digital Repository: http://eprints.qut.edu.au/ This is the author version published as: Frost, Ray L. and Bahfenne, Silmarilly (2010) A Review of the Vibrational Spectroscopic Studies of Arsenite, Antimonite, and Antimonate Minerals. Applied Spectroscopy Reviews: an international journal of principles, methods, and applications, 45(2). pp. 101-129. Copyright Taylor & Francis 1 A Review of the Vibrational Spectroscopic Studies of Arsenite, Antimonite, and 2 Antimonate Minerals 3 4 Silmarilly Bahfenne and Ray L. Frost 5 6 Inorganic Materials Research program, School of Physical and Chemical Sciences, Queensland 7 University of Technology, GPO Box 2434, Brisbane Queensland 4001, Australia 8 9 Abstract 10 11 This review focuses on the vibrational spectroscopy of the compounds and minerals 12 containing the arsenite, antimonite and antimonate anions. The review collects and 13 correlates the published data. 14 15 Key words: Arsenite, antimonite, antimonate, infrared spectroscopy, Raman 16 spectroscopy 17 18 1 19 Arsenite, Antimonite and Antimonate Minerals 20 21 Introduction 22 23 Arsenic and antimony are found throughout the earth’s crust as a variety of minerals, although 24 not particularly abundant. It has been estimated that there are 2 grams of arsenic and 0.2 grams 25 of antimony in every tonne of crustal rocks [1]. Many arsenic-bearing minerals associated with 26 sulphides have been identified, such as arsenopyrite FeAsS, orpiment As2S3, and realgar α- 27 As4S4. When these ores are oxidised, As2O3 is obtained as a by-product. Antimony also 28 occurs with sulphur, Sb2S3 being the principal source. Many oxides have also been identified; 3+ 5+ 29 valentinite Sb2O3 and cervantite Sb Sb O4. -
Authority Review for the Former Staten Island Warehouse
-. -“” i\lf 2’-L THE AEROSPACE CORPORATION Suite 4000, 955 L’Enfant P.!aza, S. W., Washington, D. C. 20024, Telephone: (202) 488-6000 7117-03.85.eav.15 20 August 1985 bee: A. Wallo F. Hoch (w/o) Mr. Arthur Whitman F. Newman (w/o) Division of Remedial Action Projects, NE-24 R. Johnson (w/o) U.S. Department of Energy Germantown, Maryland 20545 Dear Mr. Whitman: AUTHORITY REVIEW FOR THE FORMER STATEN ISLAND WAREHOUSE Aerospace has completed the analysis of the available documentation related to the former Staten Island Warehouse. The attachment is sub- mitted for your review to determine whether DOE has authority to pursue remedial action at the site under FUSRAP. As indicated in the summary of the attached analysis, it would appear that, except for export controls imposed by the State Department, the ore stored in the former Staten Island Warehouse was not under the control of the U.S. Government. The Manhattan District only purchased a portion of the U308 content of the ore, while African Metals Corpora- tion retained ownership of the radium and other precious metals that remained in the ore after processing. Further, the U.S. Government did not take custody of the ore until delivered by lighter free alongside ship to the Lehigh Valley Railroad at the Dean Mill Plant of the Archer- Daniels-Midland Company. As a result, it does not appear that DOE has authority under the Atomic Energy Act to take remedial actions, if needed, at this site. Based upon your review and final authority determination, Aerospace will prepare an elimination package to document the status of the site as it is turned over to the EPA for remedial action. -
GRAESERITE, Featisasol3(OH), a NEW MINERAL SPECIES of the DERBYLITE GROUP from the MONTE LEONE NAPPE, BINNTAL REGION, WESTERN AL
1083 The Canadian Mineralogist Vol.36, pp. 1083-1088(1998) GRAESERITE,FeaTisAsOl3(OH), A NEWMINERAL SPECIES OF THE DERBYLITE GROUP FROM THE MONTELEONE NAPPE, BINNTAL REGION, WESTERN ALPS, SWITZERLAND MICHAEL S. KRZEMNICKII Mineralagisch-Petrographischzs Instint, Universitiit Ba$eI, Bemoullistr. 30, CH-4056 Basel, Switzerl.and ERIC REUSSERI Iwtitut fiir Mincralogie und Petrographie, ETH-7zntram, Sonneggstr. 5, CH-8092 Zurich SwitzerLanl AssrRAcr Graeserite, ideally Fe4t3AsOl3(OH), is a new mineral species of the derbylite gloup, which includes derbylite, tomichite, a"ndhemloite. It is found in needle-shapedcrystals, elongate along the c axis. Graeserils i5 6sn6alinig, spacegtoup AXm, with the cell paramelersa 7 .184(2), b 14.289(6),c 5.006(2) A, p 105.17(2)",V 495.9(2) At, z=2, D,a.. =!.56 g/cm3.The VHNxgis_52L (Mohs hardness -595). The strongest five lines of the X-ray powder-diffraction pattern [d in An)(hkD] are: 2.681(100)@31), 2.846(80X131), 1.583(50X351), 3.117 (30)(220), nd 2.029(30)(122). Graeserite is black and metallic, with a black streak; it displays a conchoidal fracture. Pleochroism, bireflectance a"ndinternal reflections were not observed. The measured values of reflecrance in air are compared with those of other members of the derbylite group. Electron-microprobe analyses gave TiO2 40.89, Fe2O333.64, FeO"6" 3.94, PbO 5.00, As2O3 13.51,Sb2O3 1.43, and H2O"a" 1.30, loral 99.80 wt.7o. The empirical formula, based on 13 atoms of oxygen and one hydroxyl group, is (Fe3*z.qrFe2*o.gsTlos+Pbo.rs)>r.grTi3(As3*s.9aSb3*e.m)>r.orOrg(OH). -
Hallencup TSV 04 Feucht Jg. 2010
Hallencup TSV 04 Feucht Jg. 2010 Presenter: TSV 04 Feucht Date: 18.01.2020 Event Location: Wilhelm-Baum-Turnhalle, Schulstr. 28, 90337 Feucht Start: 10:00 Match Duration in Group Phase: 10 minutes Match Duration in Final Phase: 10 minutes Placement Mode: Points - Head-to-Head Record - Goal Difference - Amount of Goals Participants Group A Group B Live Results 1 TSV Burgthann 5 1. FC Reichenschwand 2 1. FC Schnaittach 6 SpVgg Sittenbachtal 3 Tuspo Nürnberg 7 TSV Winkelhaid 4 SG Schwarzenlohe 8 TSV 04 Feucht Preliminary Round No. Start Gr Match Result Group A 1 10:00 A Tuspo Nürnberg SG Schwarzenlohe 0 : 3 Pl Participant G GD Pts 2 10:12 A TSV Burgthann 1. FC Schnaittach 0 : 1 1. SG Schwarzenlohe 7 : 2 5 9 3 10:24 B 1. FC Reichenschwand SpVgg Sittenbachtal 0 : 1 2. 1. FC Schnaittach 4 : 3 1 6 4 10:36 B TSV Winkelhaid TSV 04 Feucht 1 : 0 3. TSV Burgthann 3 : 4 -1 3 5 10:48 A 1. FC Schnaittach Tuspo Nürnberg 2 : 1 4. Tuspo Nürnberg 2 : 7 -5 0 6 11:00 A SG Schwarzenlohe TSV Burgthann 2 : 1 7 11:12 B SpVgg Sittenbachtal TSV Winkelhaid 1 : 1 Group B 8 11:24 B TSV 04 Feucht 1. FC Reichenschwand 0 : 1 Pl Participant G GD Pts 9 11:36 A TSV Burgthann Tuspo Nürnberg 2 : 1 1. TSV Winkelhaid 3 : 1 2 7 10 11:48 A SG Schwarzenlohe 1. FC Schnaittach 2 : 1 2. SpVgg Sittenbachtal 2 : 4 -2 4 11 12:00 B 1. -
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 -
Junior Ranger Book Is for All Ages
National Park Service Manhattan Project U.S. Department of the Interior National Historical Park NM, TN, WA Manhattan Project National Historical Park JUNIORat Hanford, RANGERWashington Turn the page to accept this mission Welcome friends! My name is Atom U235 Fission. I will be your guide as we explore the Hanford site of the Manhattan JR JR RANGER Manhattan a Project N Project National Historical Park G SITE, WA ER together. This project was So big it changed the world! How to earn points This junior ranger book is for all ages. You may find some activities harder than others. That’s okay. You choose what activities to complete by earning enough points for your age. 4 points —— ages 6-8 Points needed 6 points —— ages 9-11 to earn a badge 8 points —— ages 12-14 10 points —— ages 15 and older ACTIVITIES POINT VALUE YOUR POINTS Complete activities in 1 activity = the Junior Ranger Book. 1 pt Join a docent tour or 1 pt ranger program. Total: Watch a park film. 1 pt Download the park’s app. Learn about our other locations. 1 pt This QR code will take you to the free National Park Service app. Once you have the app, search for the Manhattan Project to explore the entire park including sites in New Mexico, Tennessee, and Washington. WHEN FINISHED: Return your book to the visitor center and be sworn in as an official junior ranger. PARENTS: Participate with your aspiring junior ranger to learn about this park as a family. NEED MORE TIME? Mail your book to Manhattan Project National Historical Park, 2000 Logston Blvd. -
Iidentilica2tion and Occurrence of Uranium and Vanadium Identification and Occurrence of Uranium and Vanadium Minerals from the Colorado Plateaus
IIdentilica2tion and occurrence of uranium and Vanadium Identification and Occurrence of Uranium and Vanadium Minerals From the Colorado Plateaus c By A. D. WEEKS and M. E. THOMPSON A CONTRIBUTION TO THE GEOLOGY OF URANIUM GEOLOGICAL S U R V E Y BULL E TIN 1009-B For jeld geologists and others having few laboratory facilities.- This report concerns work done on behalf of the U. S. Atomic Energy Commission and is published with the permission of the Commission. UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1954 UNITED STATES DEPARTMENT OF THE- INTERIOR FRED A. SEATON, Secretary GEOLOGICAL SURVEY Thomas B. Nolan. Director Reprint, 1957 For sale by the Superintendent of Documents, U. S. Government Printing Ofice Washington 25, D. C. - Price 25 cents (paper cover) CONTENTS Page 13 13 13 14 14 14 15 15 15 15 16 16 17 17 17 18 18 19 20 21 21 22 23 24 25 25 26 27 28 29 29 30 30 31 32 33 33 34 35 36 37 38 39 , 40 41 42 42 1v CONTENTS Page 46 47 48 49 50 50 51 52 53 54 54 55 56 56 57 58 58 59 62 TABLES TABLE1. Optical properties of uranium minerals ______________________ 44 2. List of mine and mining district names showing county and State________________________________________---------- 60 IDENTIFICATION AND OCCURRENCE OF URANIUM AND VANADIUM MINERALS FROM THE COLORADO PLATEAUS By A. D. WEEKSand M. E. THOMPSON ABSTRACT This report, designed to make available to field geologists and others informa- tion obtained in recent investigations by the Geological Survey on identification and occurrence of uranium minerals of the Colorado Plateaus, contains descrip- tions of the physical properties, X-ray data, and in some instances results of chem- ical and spectrographic analysis of 48 uranium arid vanadium minerals. -
Geochemistry, Mineralogy and Microbiology of Cobalt in Mining-Affected Environments
minerals Article Geochemistry, Mineralogy and Microbiology of Cobalt in Mining-Affected Environments Gabriel Ziwa 1,2,*, Rich Crane 1,2 and Karen A. Hudson-Edwards 1,2 1 Environment and Sustainability Institute, University of Exeter, Penryn TR10 9FE, UK; [email protected] (R.C.); [email protected] (K.A.H.-E.) 2 Camborne School of Mines, University of Exeter, Penryn TR10 9FE, UK * Correspondence: [email protected] Abstract: Cobalt is recognised by the European Commission as a “Critical Raw Material” due to its irreplaceable functionality in many types of modern technology, combined with its current high-risk status associated with its supply. Despite such importance, there remain major knowledge gaps with regard to the geochemistry, mineralogy, and microbiology of cobalt-bearing environments, particu- larly those associated with ore deposits and subsequent mining operations. In such environments, high concentrations of Co (up to 34,400 mg/L in mine water, 14,165 mg/kg in tailings, 21,134 mg/kg in soils, and 18,434 mg/kg in stream sediments) have been documented. Co is contained in ore and mine waste in a wide variety of primary (e.g., cobaltite, carrolite, and erythrite) and secondary (e.g., erythrite, heterogenite) minerals. When exposed to low pH conditions, a number of such minerals are 2+ known to undergo dissolution, typically forming Co (aq). At circumneutral pH, such aqueous Co can then become immobilised by co-precipitation and/or sorption onto Fe and Mn(oxyhydr)oxides. This paper brings together contemporary knowledge on such Co cycling across different mining environments. -
Tavistock 632381 (STD (022) ORDERING INFORMATION RICHARD W. 8ARSTOW Drakewalls House, Drakewalls, Gunnislake, Cornwall, England
I RIC HARD W. 8ARSTOW Dr akewalls House , Drakewalls , Gunni sl ake , Cornwall , England. TEL. ~O .: Tavistock 632381 ( STD (022 ) V.A.T.No. : 132-7852- 67 ORDERI NG INFORMA TION Mail orders are prom ptly filled and despatched on a 7- day examination basis , subj ect to a pproval. Immedi at e refund guar anteed on r eturn of the specimen(s) in good condition. Please quote the name and numbe r of the s pecimen( s ) r equired and enclose P.o ./Cheque with or der. All prices are inclusive of V.A.T. No charge is ma de f or postage and packing , except for overseas customers and postage ov er 75p. We r es erve the ri ght to make slight substitutions , if necessary , unless advised to the contrary. Special r equests a,!d "wants lists" are welcome . We hope t hat we may be of some service to you , and assure you of our best attention at all t i mes. APRIL 1980 1. AESCH YN ITE. Va l Nalps , Graubunden, Switzerland. Sharp micro crystals impl anted on g1i1eiss matrix . ~xi " £1. 50p 2. AGARDITE. Gou Skour , J bel Sarhrp , Morocco. Specimen A: Apple- green s~a l l fibrous tufts and masses scattered ov er large well formed Azurite crystal s which are mostly r eplaced by gr een Ma l achite - the crystal s ranging in size up to f" , and intergrown on a limonitic matrix. 1-~'x1 fx1 ~ " , @9.oo . Specimen B: Apple- green crystal tuf t s scatter ed ov er limonitic matrix with a little crystal lised Azurite . -
Refinement of the Crystal Structure of Ushkovite from Nevados De Palermo, República Argentina
929 The Canadian Mineralogist Vol. 40, pp. 929-937 (2002) REFINEMENT OF THE CRYSTAL STRUCTURE OF USHKOVITE FROM NEVADOS DE PALERMO, REPÚBLICA ARGENTINA MIGUEL A. GALLISKI§ AND FRANK C. HAWTHORNE¶ Department of Geological Sciences, University of Manitoba, Winnipeg, Manitoba R3T 2N2, Canada ABSTRACT The crystal structure of ushkovite, triclinic, a 5.3468(4), b 10.592(1), c 7.2251(7) Å, ␣ 108.278(7),  111.739(7), ␥ 71.626(7)°, V 351.55(6) Å3, Z = 2, space group P¯1, has been refined to an R index of 2.3% for 1781 observed reflections measured with MoK␣ X-radiation. The crystal used to collect the X-ray-diffraction data was subsequently analyzed with an electron microprobe, 2+ 3+ to give the formula (Mg0.97 Mn 0.01) (H2O)4 [(Fe 1.99 Al0.03) (PO4) (OH) (H2O)2]2 (H2O)2, with the (OH) and (H2O) groups assigned from bond-valence analysis of the refined structure. Ushkovite is isostructural with laueite. Chains of corner-sharing 3+ 3+ {Fe O2 (OH)2 (H2O)2} octahedra extend along the c axis and are decorated by (PO4) tetrahedra to form [Fe 2 O4 (PO4)2 (OH)2 3+ (H2O)2] chains. These chains link via sharing between octahedron and tetrahedron corners to form slabs of composition [Fe 2 (PO4)2 (OH)2 (H2O)2] that are linked by {Mg O2 (H2O)4} octahedra. Keywords: ushkovite, crystal-structure refinement, electron-microprobe analysis. SOMMAIRE Nous avons affiné la structure cristaline de l’ushkovite, triclinique, a 5.3468(4), b 10.592(1), c 7.2251(7) Å, ␣ 108.278(7),  111.739(7), ␥ 71.626(7)°, V 351.55(6) Å3, Z = 2, groupe spatial P¯1, jusqu’à un résidu R de 2.3% en utilisant 1781 réflexions observées mesurées avec rayonnement MoK␣. -
New Mineral Names*,†
American Mineralogist, Volume 106, pages 1360–1364, 2021 New Mineral Names*,† Dmitriy I. Belakovskiy1, and Yulia Uvarova2 1Fersman Mineralogical Museum, Russian Academy of Sciences, Leninskiy Prospekt 18 korp. 2, Moscow 119071, Russia 2CSIRO Mineral Resources, ARRC, 26 Dick Perry Avenue, Kensington, Western Australia 6151, Australia In this issue This New Mineral Names has entries for 11 new species, including 7 minerals of jahnsite group: jahnsite- (NaMnMg), jahnsite-(NaMnMn), jahnsite-(CaMnZn), jahnsite-(MnMnFe), jahnsite-(MnMnMg), jahnsite- (MnMnZn), and whiteite-(MnMnMg); lasnierite, manganflurlite (with a new data for flurlite), tewite, and wumuite. Lasnierite* the LA-ICP-MS analysis, but their concentrations were below detec- B. Rondeau, B. Devouard, D. Jacob, P. Roussel, N. Stephant, C. Boulet, tion limits. The empirical formula is (Ca0.59Sr0.37)Ʃ0.96(Mg1.42Fe0.54)Ʃ1.96 V. Mollé, M. Corre, E. Fritsch, C. Ferraris, and G.C. Parodi (2019) Al0.87(P2.99Si0.01)Ʃ3.00(O11.41F0.59)Ʃ12 based on 12 (O+F) pfu. The strongest lines of the calculated powder X-ray diffraction pattern are [dcalc Å (I%calc; Lasnierite, (Ca,Sr)(Mg,Fe)2Al(PO4)3, a new phosphate accompany- ing lazulite from Mt. Ibity, Madagascar: an example of structural hkl)]: 4.421 (83; 040), 3.802 (63, 131), 3.706 (100; 022), 3.305 (99; 141), characterization from dynamic refinement of precession electron 2.890 (90; 211), 2.781 (69; 221), 2.772 (67; 061), 2.601 (97; 023). It diffraction data on submicrometer sample. European Journal of was not possible to perform powder nor single-crystal X-ray diffraction Mineralogy, 31(2), 379–388. -
CSU Nominiert Kreistagsliste
Kreisverband Nürnberger Land Artikel vom 16.10.2019 CSU Nürnberger Land Eine tolle Mischung aus erfahrenen Kommunalpolitikern und neuen Kandidaten Cornelia Trinkl (vorne, Bildmitte) führt die Liste der CSU an. Die Röthenbacherin will Landrätin werden. Außerdem möchten die Christsozialen wieder stärkste Fraktion im Kreistag werden. 19 Frauen und 51 Männer kandidieren bei der Wahl im Frühjahr 2020 Mit großer Geschlossenheit hat der CSU-Kreisverband Nürnberger Land die Kandidatinnen und Kandidaten für die Kreistagswahlen am 15. März 2020 nominiert. „Die CSU im Nürnberger Land präsentiert mit dieser Liste ein starkes Team und ein tolles Angebot für die Kreistagswahl“ so CSU-Kreisvorsitzender und Landtagsabgeordneter Norbert Dünkel. „Vom Landwirt bis zur Abgeordneten, von der Pflegefachfrau bis zum Bankkaufmann bietet die CSU mit dieser Mannschaft ein breites Spektrum an Kandidaten mit viel Erfahrung und breitem Engagement bei Feuerwehr, Sanitätsdiensten, THW, Sozialverbänden, Sport und Kultur.“ Die Kandidatin für das Amt der Landrätin Cornelia Trinkl freut sich ebenfalls über das Ihr zur Seite gestellte Team: „Eine tolle Mischung aus erfahrenen Kommunalpolitikern und neuen Kandidaten, die sich aus allen Städten und Gemeinden im Landkreis Nürnberger Land einbringen ist ein großer Gewinn.“ Als Ziel formulierte sie klar, dass die CSU auch nach der Kommunalwahl 2020 wieder die stärkste Fraktion im Kreistag stellen wolle und weiter konstruktiv für die Menschen im Nürnberger Land arbeiten möchte, da auch in Zukunft viele Herausforderungen auf die Kreispolitik zukommen. „Im Dreiklang von Innovation, Nachhaltigkeit und Stabilität wollen wir auch zukünftig Ansprechpartner und Impulsgeber sein, zuhören, zusammenarbeiten und zupacken für das Nürnberger Land!“ so die Vorsitzende der CSU-Kreistagsfraktion Cornelia Trinkl. Im Internet firmiert die Kreistagsliste der CSU unter #teamtrinkl2020.