Cesium from Pollucite by Aluminum Reduction
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Cesstibtantite Cs(Sb3+
3+ Cesstibtantite Cs(Sb , Na)Ta2(O, OH, F)7 c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Cubic. Point Group: 4/m 32/m. As cubo-octahedral crystals; granular, to 3 mm. Physical Properties: Fracture: Uneven. Tenacity: Brittle. Hardness = ∼5 VHN = 670– 780 (100 g load). D(meas.) = 6.4–6.6 D(calc.) = 6.49 Fluoresces yellow-orange to orange under LW UV; weak yellowish cathodoluminescence. Optical Properties: Transparent; may be opaque except in thinnest fragments. Color: Colorless to gray, yellow-orange, black. Luster: Adamantine to vitreous. Optical Class: Isotropic. n = > 1.8 R: (480) 13.8, (551) 13.6, (589) 13.6, (656) 13.0 Cell Data: Space Group: Fd3m. a = 10.496–10.515 Z = 8 X-ray Powder Pattern: Kola Peninsula, Russia. 3.04 (10), 1.860 (10), 1.587 (10), 1.012 (10), 3.17 (9), 1.370 (9), 1.017 (9) Chemistry: (1) (2) (3) (1) (2) (3) Nb2O5 2.3 2.8 1.2 CaO 0.1 0.6 Ta2O5 72.0 70.8 72.5 Na2O 1.3 1.7 2.4 Bi2O3 0.7 0.3 0.6 K2O 0.0 0.05 Sb2O3 13.6 14.2 9.7 Cs2O 7.3 7.4 5.4 SnO 0.1 H2O [1.5] [1.2] PbO 1.6 0.8 5.3 Total 98.9 [99.5] [99.0] (1) Kola Peninsula, Russia; by electron microprobe, average of five analyses; (OH)1− confirmed by IR. (2) Do.; by electron microprobe, H2O calculated from structural considerations; corresponds to [Cs0.31(OH, F)0.69]Σ=1.00(Sb0.57Na0.31Pb0.02Bi0.01)Σ=0.91(Ta1.88Nb0.12)Σ=2.00 [O5.69(OH, F)0.31]Σ=6.00. -
Synthesis of Alum from Aluminum
Synthesis of Alum from Aluminum Taken from Central Oregon College Chemistry Manual OBJECTIVES: To carry out a series of reactions to transform a piece of aluminum foil into crystals of alum and to gain familiarity with using stoichiometry to determine the yield for the reaction. SAFETY AND DISPOSAL: Strong acids and bases are corrosive and should be handled with care. Immediately wipe up any spills and wash hands with plenty of soap and water. Work in the mini-hoods whenever possible to avoid breathing in fumes. All solutions can be disposed of down the sink with running water. The alum can be safely disposed of in the trash but has a number of uses and can be used for other laboratories, place alum crystals into the designated container. INTRODUCTION: Aluminum is a material that you may have had some experience with and paid little attention to, but has some very interesting characteristics. Here are some fun facts about aluminum metal: 1. Aluminum is the third most abundant element in the earth's crust. 2. The supply of aluminum ore is not inexhaustible. 3. The winning, or extraction of the metallic form an impure ionic source, of aluminum from aluminum ore is very costly from an energy point of view. 4. The above point explains why Napoleon III used aluminum dinnerware for his state dinners. Lesser guests were served on plates of gold or silver. 5. The process of obtaining pure metallic aluminum from aluminum oxide in a reasonably energy efficient manner, which made it possible for aluminum to be the inexpensive metal we know today, was developed in a home laboratory shortly after the chemist finished his undergraduate degree. -
A Review of Rare-Element (Li-Cs-Ta) Pegmatite Exploration Techniques for the Superior Province, Canada, and Large Worldwide Tantalum Deposits
Exploration and Mining Geology, Vol. 14, Nos. 1-4, pp. 1-30, 2005 © 2006 Canadian Institute of Mining, Metallurgy and Petroleum. All rights reserved. Printed in Canada. 0964-1823/00 $17.00 + .00 A Review of Rare-Element (Li-Cs-Ta) Pegmatite Exploration Techniques for the Superior Province, Canada, and Large Worldwide Tantalum Deposits JULIE B. SELWAY, FREDERICK W. BREAKS Precambrian Geoscience Section, Ontario Geological Survey 933 Ramsey Lake Road, Sudbury, ON P3E 6B5 ANDREW G. TINDLE Department of Earch Sciences, Open University Milton Keynes, Buckinghamshire, UK MK7 6AA (Received February 16, 2004; accepted September 20, 2004) Abstract — Rare-element pegmatites may host several economic commodities, such as tantalum (Ta- oxide minerals), tin (cassiterite), lithium (ceramic-grade spodumene and petalite), and cesium (pollucite). Key geological features that are common to pegmatites in the Superior province of Ontario and Manitoba, Canada, and in other large tantalum deposits worldwide, can be used in exploration. An exploration project for rare-element pegmatites should begin with an examination of a regional geology map. Rare-element pegmatites occur along large regional-scale faults in greenschist and amphibolite facies metamorphic terranes. They are typically hosted by mafic metavolcanic or metasedimentary rocks, and are located near peraluminous granite plutons (A/CNK > 1.0). Once a peraluminous granite pluton has been identified, then the next step is to determine if the pluton is barren or fertile. Fertile granites have elevated rare element contents, Mg/Li ratio < 10, and Nb/Ta ratio < 8. They commonly contain blocky K-feldspar and green muscovite. Key fractionation indicators can be plotted on a map of the fertile granite pluton to determine the fractionation direction: presence of tourmaline, beryl, and ferrocolumbite; Mn content in garnet; Rb content in bulk K-feldspar; and Mg/Li and Nb/Ta ratios in bulk granite samples. -
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ON POLLUCITE W. E. RrcnMoNDAND F. A. GoNvnn, H araard.U niversi.ty, C ambrid.ge, M ass' 1. POLLUCITE AND PETALITE FROM GREENWOOD,MAINE Introduction Several years ago in the course of feldspar mining at a quarry at the base of Noyes Mountain in Greenwood, Maine, a mineral supposed to be spodumene was found in quantity and about eight tons of it were taken to the grinding mill at West Paris, Maine. There it lay in a bin for a year or more before it was examined by the late W. D' Nevel of Andover, Maine, who identified the mineral as petalite. He sorted out the petalite and the rejects were sacked and retained until the summer of t937. On a visit to the mill that year Richmond selected a quantity of petalite for the Harvard Mineralogical Museum and also carried away some of the waste reject material for examination. This proved, after a delay of months, to contain glassy crystals of pollucite. The effort to securemore of this mineral was unsuccessful,however, sinceon returning to the mill it was found that the lot had been sent through the grinder. Occurrence.The specimensstudied are clearly replacementsof petalite by pollucite and quartz. The pollucite is for the most part massive granular but preserves the laminated structure peculiar to the petalite with which it is associated.Some layers are composed of quartz grains, and elsewhere there are fractures showing indistinct faces of pollucite crystals. In a few cavities in massivepollucite the walls are covered with small crystals of pollucite, the first to be reported from an American locality. -
AM30 616.Pdf
QUANTITATIVE SPECTROCHEMICAL EXAMINATION OF THE MINOR CONSTITUENTS IN POLLUCITE L. H. AHnnNs, Go o er n m ent M etallur gicaI L abor at or y, W itw ater sr an d U niner s ity, J ohonnesburg, South AJrica. Cor.rrnNrs Introduction. 616 Brief outline of analytical principles. 617 Quantitative analysis of pollucite samples. 618 Discussion: (1) Rubidium and thallium. 619 Quantitative analysis of a lepidolite sample.. 619 (2) Gallium. 620 (3) Lithium. 620 Radioactive disintegration of rubidium. 621 Acknowledgments... 622 References. 622 ABSTRACT Details are given of a quantitative spectrochemical analysis for Tl, Rb, Li, Ga, and K, in two samples of poilucite, one from Karibib, South West Africa, and the other from near Norway, Maine, U.S.A., and the presence of these elements (excluding potassium) within the pollucite lattice is discussed. The ratio, Rb/Tl, is approximately 50 (Karibib) and 180 (Maine). Both ratios are within the limits of 40 and 440 found in 42 analyses of various Rb- and Tl-containing minerals, chiefly South AIrican, data on which will be published later. Although the former ratio (50) is considerably lower than the mean ratio of the 42 analyses (150) it is worth noting that the mean Rb/TI ratio for two samples of lepidolite from the same locality was found to be almost identical (70), providing further evidence that Rb and TI enter different crystal lattices with equal facility. The presence of a trace of strontium is discussed, and a radioactive origin, involving the transition RbE?-51s2, is suggested. h.rrnooucttoN Recently, a sample of pollucite from K.aribib, South West Africa, was examined at the Union Geological Survey, South Africa, by Nel.l This investigation included a qualitative spectrochemicalanalysis by Dr. -
New Family of Silicate Phases with the Pollucite Structure
Zeitschrift fUr Kristallographie 175, 1-7 (1986) @ by R. Oldenbourg Verlag, Miinchen 1986 New family of silicate phases with the pollucite structure Leticia M. Torres-Martinez and A. R. West University of Aberdeen, Department of Chemistry, Meston Walk, Old Aberdeen AB9 2UE, Scotland, United Kingdom Received: April 10, 1984; in final form: February 14, 1986 Pollucite structure I RbzMgSis012 type Abstract. A new family of silicate phases, CszMSi5012: M = Be, Mg, Fe, Co, Ni, Zn, Cd; RbzMSi5012: M = Mg, Fe, (Co, Zn) has been prepared with the cubic pollucite structure, a in the range 13.3 to 13.8 A, space group Ia3d, Z = 8. The structure of one, RbzMgSi5012' has been refined to R = 10.8% using X-ray powder data. The structures are built of a 3D, [MSi50u]z- framework containing large, 12-coordinated cavities for the alkali cations. These structures are unusual in that a wide range of divalent cations have partially replaced Si4+ in the silicate anion framework. Introduction Pollucite, CsAISiz06, is a framework alumino silicate containing large, 12- coordinated cavities suitable for occupation by Cs+ ions (Strunz, 1936; Naray-Szabo, 1938; Newnham, 1967). The unit cell is cubic with space group Ia3d, Z = 16. Similar alumino-silicate frameworks are present in analcite, NaAISiz06 . HzO and leucite, KAISiz06 (Taylor, 1938; Beattie, 1954; Knowles et aI., 1965; Wyart, 1941; Deer et aI., 1963; Wyckoff, 1968), although leucite is tetragonal below 6050 (Wyart, 1941; Deer et aI., 1963; Wyckoff, 1968). Structural studies on these phases are complicated by the occurrence of twinning in tetragonalleucite (Mazzi et aI., 1976) and by Si, Al disorder in the alumino silicate framework. -
Paper Number: 2059
Paper Number: 2059 New Geochronological, Isotopic and Fluid Inclusion Study Constraints on the Formation of the World-class Bikita LCT Pegmatite Deposit Dittrich, T.1, Seifert, T.1, Richter, L.1, Hagemann, S.2, Lüders, V.3, Schulz, B.1, Pfänder, J.A.4 and Gerdes, A.5 1Division of Economic Geology and Petrology, TU Bergakademie Freiberg/Germany [email protected] freiberg.de 2University of Western Australia, Centre for Exploration Targeting, Crawley/Australia 3Helmholtz Centre Potsdam, GFZ German Research Centre for Geosciences, Potsdam/Germany 4ArgonLab Freiberg, Department of Geology, TU Bergakademie Freiberg/Germany 5Institute for Geosciences, Goethe University, Frankfurt am Main/Germany ___________________________________________________________________________________________ The increasing demand for metals such as Li and Ta used by high technology applications (e.g., renewable energies, electronics) led to increasing exploration activities on lithium-cesium-tantalum (LCT) pegmatite deposits worldwide. LCT pegmatites are interpreted to be linked to granitic systems and represent the geochemically most enriched, highest fractionated portions of initially granitic melts and thus can host economic quantities of various metals (i.e., Li, Cs, Ta, Nb, Sn, Rb, Be). However, many economic LCT pegmatite deposits (e.g., Tanco/Canada, Greenbushes, Wodgina/Western Australia) are situated in greenstone belt successions on Archean Cratons making those prospective exploration areas [1]. The Bikita LCT pegmatite deposit located in the Zimbabwe Craton represents a typical example of Archean LCT pegmatites. The pegmatites are hosted by metavolcanic rocks of the Masvingo greenstone belt [2] and represent the highest evolved portions of a 20 km long NE-SW striking pegmatite field. The Bikita pegmatite is currently mined for Li (petalite) and Cs (pollucite). -
The Crystal Structure and Chemical Composition of Pollucite
Zeitschrift fUr Kristallographie, Bd. 129, S. 280-302 (1969) The crystal structure and chemical composition of pollucite By RICHARD M. BEGER * (Received May 20, 1968) Crystallographic Laboratory, Massachusetts Institute of Technology Cambridge, Massachusetts Auszug Die Struktur des Pollucits von Rumford, Maine, wurde aus 213, mit einem Diffraktometer gemessenen Interferenzen bestimmt und bis R = 0,050 fiir aIle Interferenzen verfeinert. Raumgruppe ist Ia3d, Gitterkonstante a = 13,69 A. Das Strukturgeriist ist das gleiche wie beim Analcim. Die gro13en Hohlriiume sind von Caesiumatomen und Wassermolekiilen besetzt. Die Natriumatome befinden sich wie beim Analcim in der Punktlage 24c, [t to]. Sie sind jedoch in groJ3eren, von Wassermolekiilen begrenzten Gruppen nach Zufall angesam- melt. Die allgemeine Zusammensetzung des Pollucits liiJ3t sich durch eine y Formel von der Art CsxNayAlx+ySi4s-x-y096 . (16-x) H20 mit 2y :> 16 - x :> ausdriicken. Abstract The structure of pollucite from Rumford, Maine has been determined and refined. The space group is Ia3d with cell edge a = 13.69 A. The structure was investigated using 213 independent reflection intensities measured on a single crystal diffractometer. Pollucite has the analcime framework with the cesium atoms occupying the large voids in the framework, as initially suggested by NARAY-SZABO. The water molecules occupy the large voids of this same set which are not occupied by the cesium atoms. The sodium atoms are located in equipoint 24c, at t t 0, in the positions between the water molecules. The water molecules and the sodium atoms occupy the same positions as they do in analcime, but they occur only in randomly distributed clusters of atoms whose outer members are restricted to water molecules. -
Compositional Heterogeneity of Pollucite from High Grade Dyke
681 Conodian Mineralogist Yol. 30, pp. 687.697(1992) COMPOSITIONALHETEROGENEITY OF POLLUCITEFROM HIGH GRADEDYKE" MASKWA LAKE. SOUTHEASTERNMANITOBA DAVID K. TEERTSTRA,PETRTERNY AND RON CHAPMAN Department of Geological Sciences,University of Manitoba, Winnipeg, Manitobo R3T 2N2 AssrRACT Primary pollucite from the High Grade Dyke pegmatite of the Maskwa Lake group in southeastern Manitoba occurs with spodumene,microcline, quartz, elbaite, albite, and lepidolite. Pollucite is replaced en masseby microcline and lepidolite + quartz, veined by a sequenceof spodumene, lepidolite, late spodumeneand adularia, and replaced at a late stage by clay minerals. The primary homogeneouspollucite has locally evolved to a mosaic of Na-enriched and Cs-enricheddomains 20-3@ pm across,cross-cut by l- to l57m veinletsof quartz-containingCs-rich pollucite rimmed by Na-rich pollucite. This homogeneouspollucite has an average composition of Na6.1a9Ca6.9l6cs0.58l Rbo.043Ab.B60Si2.153O6per anhydrous subcell. The primary homogeneouspollucite has 2.45 < Si/Al < 2.55 and a molar proportion of the pollucite end-memberCRK = (Cs + Rb + K) x l@/(cation sum) between76 and 81, in contrast with the Cs-enrichedblebs (2.10 < Si/Al 12.N,82 < CRK < 90), Na-enrichedblebs Q30 < Si/Al < 2.50,74 < CRK < 80),veinletsofCs-richpollucite(2.@ < Si/Al < 2.40,84 < cRK < 92)andtheirNa-richrims (2.50 < Si/Al < 2.90, 58 < CRK < 78). Na contentsand Si,/Al are highestadjacent to the margin of the Cs-rich veinlet, and decreaseover 30-70 pm into homogeneouspollucite. The above sequenceindicates re-equilibration of primary pollucite at decreasingtemperature into a two-phase subsolvus assemblageof Cs- and Na-rich compositions. An overall positive correlation of Al contents with CRK is noted throughout the homogeneouspollucite, the blebby domains, and veinlets plus their rims. -
Uilitgd States Patent [19] [11] Patent Number: 4,647,386 Jamison [45] Date of Patent: Mar
UIlItGd States Patent [19] [11] Patent Number: 4,647,386 Jamison [45] Date of Patent: Mar. 3, 1987 [54] INTERCALATED TRANSITION METAL Attorney, Agent, or Firm-—Robert E. Harris BASED SOLID LUBRICATING COMPOSITION AND METHOD OF SO [57] ABSTRACT , FORMING A solid lubricating composition and method for form ing such a composition are disclosed. The composition [76] Inventor: Warren E. Jamison, 528 Parkview Ave., Golden, Colo. 80401 is formed by intercalating a transition metal that has been chemically reacted with chalcogen to form a lay [21] App]. No.: 538,137 ered structure. The transition metal is selected from [22] Filed: Oct. 3, 1983 niobium, tantalum, tungsten and/or an alloy including one or more, and the transition metal is chemically [51] Int. Cl.4 ......................................... .. C10M 125/22 combined with chalcogen selected from sulfur, sele [52] US. Cl. ...................... .. 252/25; 423/561 R nium and/or a combination which can also include [5 8] Field of Search ..................... .. 252/25; 423/561 R tellurium to form a layered transition metal dischal [56] References Cited cogenide prior to intercalation with a metal, preferably U.S. PATENT DOCUMENTS a coinage metal. The effect of intercalation is to expand the crystal lattice to create a composition having excel 3,573,204 3/1971 Van Wyk ............................ .. 252/12 Thompson 252/12 lent lubricating characteristics the performance of 3,763,043 10/1973 which is not adversely effected by operation in a high 3,769,210 10/1973 Cais et a1. ........ .. 252/25 4,040,917 8/1977 Whittingham . .. 204/36 temperature environment. 4,094,893 6/ 1978 Dines ................................. -
BERYLLONITE and OTHER PHOSPHATES from NEWRY, MAINE Cuanr,As Par-Acnn Anp Eenr V. Shennon the Dunton Tourmaline Mine in the Town
392 THE AMERICAN MINERALOGIST BERYLLONITE AND OTHER PHOSPHATES FROM NEWRY, MAINE Cuanr,as Par-acnn aNp Eenr V. SheNNoN The Dunton tourmaline mine in the town of Newry, Maine, was operated about twenty years ago in a search for gem tourmaline- The locality is described briefly by Bastinr and was widely known becauseof the large tourmalines found there with green center and pink border zone, tightly frozen in the pegmatite ledge-matter' Little gem tourmaline was found and the mine was soon aban- doned. This ledge and others near it was reopenedin the summers of 1926 and. 1927 under the superintendence of W. D. Nevel of Andover, Maine, in search for pollucite in commercial quanti- ties.2 The search was successful but mining has now ceased' Mr. Nevel saved with great care all unusual minerals found in opening these ledges and from him a very full suite has been secured for the Harvard Mineralogical Museum. On a later occasionit is hoped to give a full account of the paragenesisof this lithium pegmatite. In this paper it is intended to describe only three rare phosphates found there of which analyses have been made for the author by Dr. E. V. Shannon. Bonvr-r-ontre. Beryllonite was first describedby E. S' Dana and H. L. Wellssfrom Stoneham, Maine. Their material consisted of isolated crystals found by Sumner Andrews in the talus slope of a cliff together with other typical pegmatite minerals' Only one or two specimens showed the new mineral attached to any other substance and one of these, a smoky quartz crystal with a beryllonite crystal partly imbedded in it, is in the Harvard Mineralogical Museum. -
Synergy of Alum and Chlorine Dioxide for Curbing Disinfection Byproduct Formation Potential at Central Arkansas Water Corey W
University of Arkansas, Fayetteville ScholarWorks@UARK Theses and Dissertations 5-2012 Synergy of Alum and Chlorine Dioxide for Curbing Disinfection Byproduct Formation Potential at Central Arkansas Water Corey W. Granderson University of Arkansas, Fayetteville Follow this and additional works at: http://scholarworks.uark.edu/etd Part of the Environmental Engineering Commons, and the Water Resource Management Commons Recommended Citation Granderson, Corey W., "Synergy of Alum and Chlorine Dioxide for Curbing Disinfection Byproduct Formation Potential at Central Arkansas Water" (2012). Theses and Dissertations. 310. http://scholarworks.uark.edu/etd/310 This Thesis is brought to you for free and open access by ScholarWorks@UARK. It has been accepted for inclusion in Theses and Dissertations by an authorized administrator of ScholarWorks@UARK. For more information, please contact [email protected], [email protected]. SYNERGY OF ALUM AND CHLORINE DIOXIDE FOR CURBING DISINFECTION BYPRODUCT FORMATION POTENTIAL AT CENTRAL ARKANSAS WATER SYNERGY OF ALUM AND CHLORINE DIOXIDE FOR CURBING DISINFECTION BYPRODUCT FORMATION POTENTIAL AT CENTRAL ARKANSAS WATER A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Civil Engineering By Corey W. Granderson University of Arkansas Bachelor of Science in Civil Engineering, 2008 May 2012 University of Arkansas Abstract Central Arkansas Water (CAW), the water utility for Little Rock, AR, draws their source water from Lake Maumelle and Lake Winona. To curb disinfection byproduct (DBP) formation, CAW has begun retrofitting their two plants to use chlorine dioxide as an alternative primary disinfectant followed by free chlorine secondary disinfection in the distribution system. In this study, fluorescence parallel factor (PARAFAC) analysis was combined with free chlorine simulated distribution system (SDS) tests and DBP formation potential (DBPFP) tests to study the benefit of chlorine dioxide primary disinfection (CDPD) with alum coagulation.