Reaction of Aluminum with Water to Produce Hydrogen
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Recycling of Hazardous Waste from Tertiary Aluminium Industry in A
CORE Metadata, citation and similar papers at core.ac.uk Provided by Digital.CSIC 1 Recycling of hazardous waste from tertiary aluminium 2 industry in a value-added material 3 4 Laura Gonzalo-Delgado1, Aurora López-Delgado1*, Félix Antonio López1, Francisco 5 José Alguacil1 and Sol López-Andrés2 6 7 1Nacional Centre for Metallurgical Research, CSIC. Avda. Gregorio del Amo, 8. 28040. 8 Madrid. Spain. 9 2Dpt. Crystallography and Mineralogy. Fac. of Geology. University Complutense of 10 Madrid. Spain. 11 *Corresponding author e-mail: [email protected] 12 13 Abstract 14 15 The recent European Directive on waste, 2008/98/EC seeks to reduce the 16 exploitation of natural resources through the use of secondary resource management. 17 Thus the main objective of this paper is to explore how a waste could cease to be 18 considered as waste and could be utilized for a specific purpose. In this way, a 19 hazardous waste from the tertiary aluminium industry was studied for its use as a raw 20 material in the synthesis of an added value product, boehmite. This waste is classified as 21 a hazardous residue, principally because in the presence of water or humidity, it releases 22 toxic gases such as hydrogen, ammonia, methane and hydrogen sulphide. The low 23 temperature hydrothermal method developed permits the recovery of 90% of the 24 aluminium content in the residue in the form of a high purity (96%) AlOOH (boehmite). 25 The method of synthesis consists of an initial HCl digestion followed by a gel 26 precipitation. In the first stage a 10% HCl solution is used to yield a 12.63 g.l-1 Al3+ 27 solution. -
Gallium and Germanium Recovery from Domestic Sources
RI 94·19 REPORT OF INVESTIGATIONS/1992 r---------~~======~ PLEASE DO NOT REMOVE FRCJIiI LIBRARY "\ LIBRARY SPOKANE RESEARCH CENTER RECEIVED t\ UG 7 1992 USBOREAtJ.OF 1.j,'NES E. S15't.ON1"OOMERY AVE. ~E. INA 00207 Gallium and Germanium Recovery From Domestic Sources By D. D. Harbuck UNITED STATES DEPARTMENT OF THE INTERIOR BUREAU OF MINES Mission: As the Nation's principal conservation agency, the Department of the Interior has respon sibility for most of our nationally-owned public lands and natural and cultural resources. This includes fostering wise use of our land and water resources, protecting our fish and wildlife, pre serving the environmental and cultural values of our national parks and historical places, and pro viding for the enjoyment of life through outdoor recreation. The Department assesses our energy and mineral resources and works to assure that their development is in the best interests of all our people. The Department also promotes the goals of the Take Pride in America campaign by encouragi,ng stewardship and citizen responsibil ity for the public lands and promoting citizen par ticipation in their care. The Department also has a major responsibility for American Indian reser vation communities and for people who live in Island Territories under U.S. Administration. TIi Report of Investigations 9419 Gallium and Germanium Recovery From Domestic Sources By D. D. Harbuck I ! UNITED STATES DEPARTMENT OF THE INTERIOR Manuel lujan, Jr., Secretary BUREAU OF MINES T S Ary, Director - Library of Congress Cataloging in Publication Data: Harbuck, D. D. (Donna D.) Ga1lium and germanium recovery from domestic sources / by D.D. -
The Periodic Table of Elements
The Periodic Table of Elements 1 2 6 Atomic Number = Number of Protons = Number of Electrons HYDROGENH HELIUMHe 1 Chemical Symbol NON-METALS 4 3 4 C 5 6 7 8 9 10 Li Be CARBON Chemical Name B C N O F Ne LITHIUM BERYLLIUM = Number of Protons + Number of Neutrons* BORON CARBON NITROGEN OXYGEN FLUORINE NEON 7 9 12 Atomic Weight 11 12 14 16 19 20 11 12 13 14 15 16 17 18 SODIUMNa MAGNESIUMMg ALUMINUMAl SILICONSi PHOSPHORUSP SULFURS CHLORINECl ARGONAr 23 24 METALS 27 28 31 32 35 40 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 POTASSIUMK CALCIUMCa SCANDIUMSc TITANIUMTi VANADIUMV CHROMIUMCr MANGANESEMn FeIRON COBALTCo NICKELNi CuCOPPER ZnZINC GALLIUMGa GERMANIUMGe ARSENICAs SELENIUMSe BROMINEBr KRYPTONKr 39 40 45 48 51 52 55 56 59 59 64 65 70 73 75 79 80 84 37 38 39 40 41 42 43 44 45 46 47 48 49 50 51 52 53 54 RUBIDIUMRb STRONTIUMSr YTTRIUMY ZIRCONIUMZr NIOBIUMNb MOLYBDENUMMo TECHNETIUMTc RUTHENIUMRu RHODIUMRh PALLADIUMPd AgSILVER CADMIUMCd INDIUMIn SnTIN ANTIMONYSb TELLURIUMTe IODINEI XeXENON 85 88 89 91 93 96 98 101 103 106 108 112 115 119 122 128 127 131 55 56 72 73 74 75 76 77 78 79 80 81 82 83 84 85 86 CESIUMCs BARIUMBa HAFNIUMHf TANTALUMTa TUNGSTENW RHENIUMRe OSMIUMOs IRIDIUMIr PLATINUMPt AuGOLD MERCURYHg THALLIUMTl PbLEAD BISMUTHBi POLONIUMPo ASTATINEAt RnRADON 133 137 178 181 184 186 190 192 195 197 201 204 207 209 209 210 222 87 88 104 105 106 107 108 109 110 111 112 113 114 115 116 117 118 FRANCIUMFr RADIUMRa RUTHERFORDIUMRf DUBNIUMDb SEABORGIUMSg BOHRIUMBh HASSIUMHs MEITNERIUMMt DARMSTADTIUMDs ROENTGENIUMRg COPERNICIUMCn NIHONIUMNh -
Unit 2 Matter and Chemical Change
TOPIC 5 The Periodic Table By the 1850s, chemists had identified a total of 58 elements, and nobody knew how many more there might be. Chemists attempted to create a classification system that would organize their observations. The various “family” systems were useful for some elements, but most family relationships were not obvious. What else could a classification system be based on? By the 1860s several scientists were trying to sort the known elements according to atomic mass. Atomic mass is the average mass of an atom of an element. According to Dalton’s atomic theory, each element had its own kind of atom with a specific atomic mass, different from the Figure 2.31 Dmitri atomic mass of any other elements. One scientist created a system that Ivanovich Mendeleev was so accurate it is still used today. He was a Russian chemist named was born in Siberia, the Dmitri Mendeleev (1834–1907). youngest of 17 children. Mendeleev Builds a Table Mendeleev made a card for each known element. On each card, he put data similar to the data you see in Figure 2.32. Figure 2.32 The card above shows modern values for silicon, rather than the ones Mendeleev actually used. His values were surprisingly close to modern ones. The atomic mass measurement indicates that silicon is 28.1 times heavier than hydrogen. You can observe other properties of silicon in Figure 2.33. Mendeleev pinned all the cards to the wall, in order of increasing atomic mass. He “played cards” for several Figure 2.33 The element silicon is melted months, arranging the elements in vertical columns and and formed into a crystal. -
The Structure and Vibrational Spectroscopy of Cryolite, Na3alf6 Cite This: RSC Adv., 2020, 10, 25856 Stewart F
RSC Advances PAPER View Article Online View Journal | View Issue The structure and vibrational spectroscopy of cryolite, Na3AlF6 Cite this: RSC Adv., 2020, 10, 25856 Stewart F. Parker, *a Anibal J. Ramirez-Cuesta b and Luke L. Daemenb Cryolite, Na3[AlF6], is essential to commercial aluminium production because alumina is readily soluble in molten cryolite. While the liquid state has been extensively investigated, the spectroscopy of the solid state has been largely ignored. In this paper, we show that the structure at 5 K is the same as that at Received 31st May 2020 room temperature. We use a combination of infrared and Raman spectroscopies together with inelastic Accepted 1st July 2020 neutron scattering (INS) spectroscopy. The use of INS enables access to all of the modes of Na3[AlF6], DOI: 10.1039/d0ra04804f including those that are forbidden to the optical spectroscopies. Our spectral assignments are supported rsc.li/rsc-advances by density functional theory calculations of the complete unit cell. Introduction In view of the technological importance of cryolite, we have Creative Commons Attribution 3.0 Unported Licence. carried out a comprehensive spectroscopic investigation and 1 Cryolite, Na3[AlF6], occurs naturally as a rare mineral. Histori- report new infrared and Raman spectra over extended temper- cally, it was used as a source of aluminium but this has been ature and spectral ranges and the inelastic neutron scattering superseded by bauxite (a mixture of the Al2O3 containing (INS) spectrum. The last of these is observed for the rst time minerals boehmite, diaspore and gibbsite), largely because of and enables access to all of the modes of Na3[AlF6]. -
Clay Minerals Soils to Engineering Technology to Cat Litter
Clay Minerals Soils to Engineering Technology to Cat Litter USC Mineralogy Geol 215a (Anderson) Clay Minerals Clay minerals likely are the most utilized minerals … not just as the soils that grow plants for foods and garment, but a great range of applications, including oil absorbants, iron casting, animal feeds, pottery, china, pharmaceuticals, drilling fluids, waste water treatment, food preparation, paint, and … yes, cat litter! Bentonite workings, WY Clay Minerals There are three main groups of clay minerals: Kaolinite - also includes dickite and nacrite; formed by the decomposition of orthoclase feldspar (e.g. in granite); kaolin is the principal constituent in china clay. Illite - also includes glauconite (a green clay sand) and are the commonest clay minerals; formed by the decomposition of some micas and feldspars; predominant in marine clays and shales. Smectites or montmorillonites - also includes bentonite and vermiculite; formed by the alteration of mafic igneous rocks rich in Ca and Mg; weak linkage by cations (e.g. Na+, Ca++) results in high swelling/shrinking potential Clay Minerals are Phyllosilicates All have layers of Si tetrahedra SEM view of clay and layers of Al, Fe, Mg octahedra, similar to gibbsite or brucite Clay Minerals The kaolinite clays are 1:1 phyllosilicates The montmorillonite and illite clays are 2:1 phyllosilicates 1:1 and 2:1 Clay Minerals Marine Clays Clays mostly form on land but are often transported to the oceans, covering vast regions. Kaolinite Al2Si2O5(OH)2 Kaolinite clays have long been used in the ceramic industry, especially in fine porcelains, because they can be easily molded, have a fine texture, and are white when fired. -
Atomic Weight of Gallium, Weighed Portions of the Pure Metal Were Converted to the Hydroxide, the Sulphate, and the Nitrate, Respectively
- -----.---.--~---------~---------------- U. S. D EPARTMENT OF C OMMERCE N ATIONAL B UREAU OF STANDARDS RESEARCH PAPER RP838 Part of Journal of Research of the J\[ational Bureau of Standards, V olume 15, October 1935 ATOMIC WEIGHT OF GALLI UM By G. E. F. Lundell and James I. Hoffman ABSTRACT In this determination of the atomic weight of gallium, weighed portions of the pure metal were converted to the hydroxide, the sulphate, and the nitrate, respectively. These were then beated until they were changed to the oxide, Ga20 a, which was finally ignited at 1,200 to 1,300° C. By this procedure, the atomic weight is related dir~ctly to that of oxygen. Preliminary tests showed that the metal was free from an appreciable film of oxide and did not contain occluded gases. The highly ignited oxide, obtained through the hydroxide or the sulphate, contained no gases and was not appreciably hygroscopic. The oxide obtained by igniting the nitrate was less satisfactory. To make possible the correction of the weights to the vacuum standard, the density of the oxide was also determined, and found to be 5.95 g/cm3• The value for the atomic weight based on this work is 69.74. CONT E N TS Page I. Introduction ___________ _____ _________________ ____ ___________ ___ 409 II. Preliminary tests ______ ________ ___ _____ ____ ___ _____________ _____ 410 III. Preparation and testing of materials used _________ _________________ 412 1. Metallic gallium _______________________________________ ___ 412 (a) Preparation ___ _________ _____ ____ ______ _____ ____ ___ _ 412 (b) Tests for occluded gases _____________________________ _ 412 (c) Tests for a film of oxide on the surface of the crystals ____ 413 (d) Test for chlorides in the crystals of metallic gallium ______ 414 2. -
Removal of Iron-Bearing Minerals from Gibbsitic Bauxite by Direct Froth Flotation
a Original Article http://dx.doi.org/10.4322/2176-1523.0924 REMOVAL OF IRON-BEARING MINERALS FROM GIBBSITIC BAUXITE BY DIRECT FROTH FLOTATION Felipe de Melo Barbosa 1 Maurício Guimarães Bergerman 2 Daniela Gomes Horta 3 Abstract The refractory bauxite needs to present less than 2.5% of Fe2O3 to be applied in the ceramics industry. The depletion of high Al2O3 grade deposits has stimulated the improvement of bauxite concentration methods in order to remove iron-bearing minerals. The objective of this study was to evaluate the influence of collector dosage, pH and milling time on the gibbsite flotation performance. Firstly, the sample mineralogical composition was determined by means of X-ray diffraction (XRD) and binocular loupe analysis. X-ray fluorescence (XRF) analysis was used to determine the sample chemical composition. Flotation was then accomplished by using hydroxamate as gibbsite collector, sodium silicate as silicate depressant and starch as iron-bearing minerals depressant. The bauxite Fe2O3 content was reduced from 7.66% to 4.81-5.03%. In addition, the flotation performance decreased by diminishing the pH from 9.5 to 8.5 or increasing the pH to 10.5. The milling time influence on the flotation indicates that the presence of slime can significantly affect the gibbsite concentration. Keywords: Bauxite; Gibbsite; Direct flotation; Hydroxamate. REMOÇÃO DE MINERAIS PORTADORES DE FERRO DE BAUXITA GIBSÍTICA POR FLOTAÇÃO DIRETA Resumo As bauxitas refratárias precisam apresentar teores de ferro menores que 2,5% para serem utilizadas na indústria de cerâmica. A exaustão dos depósitos com altos teores de Al2O3 tem estimulado a pesquisa por métodos de concentração de bauxita de forma a remover os minerais portadores de ferro. -
Part 629 – Glossary of Landform and Geologic Terms
Title 430 – National Soil Survey Handbook Part 629 – Glossary of Landform and Geologic Terms Subpart A – General Information 629.0 Definition and Purpose This glossary provides the NCSS soil survey program, soil scientists, and natural resource specialists with landform, geologic, and related terms and their definitions to— (1) Improve soil landscape description with a standard, single source landform and geologic glossary. (2) Enhance geomorphic content and clarity of soil map unit descriptions by use of accurate, defined terms. (3) Establish consistent geomorphic term usage in soil science and the National Cooperative Soil Survey (NCSS). (4) Provide standard geomorphic definitions for databases and soil survey technical publications. (5) Train soil scientists and related professionals in soils as landscape and geomorphic entities. 629.1 Responsibilities This glossary serves as the official NCSS reference for landform, geologic, and related terms. The staff of the National Soil Survey Center, located in Lincoln, NE, is responsible for maintaining and updating this glossary. Soil Science Division staff and NCSS participants are encouraged to propose additions and changes to the glossary for use in pedon descriptions, soil map unit descriptions, and soil survey publications. The Glossary of Geology (GG, 2005) serves as a major source for many glossary terms. The American Geologic Institute (AGI) granted the USDA Natural Resources Conservation Service (formerly the Soil Conservation Service) permission (in letters dated September 11, 1985, and September 22, 1993) to use existing definitions. Sources of, and modifications to, original definitions are explained immediately below. 629.2 Definitions A. Reference Codes Sources from which definitions were taken, whole or in part, are identified by a code (e.g., GG) following each definition. -
The Gallium Melting-Point Standard
TECH NATL INST. OF STAND & AlllDb 312iab /0/Vs Z NBS SPECIAL PUBLICATION 481 U.S. DEPARTMENT OF COMMERCE / National Bureau of Standards Gallium Melting-point Standard NATIONAL BUREAU OF STANDARDS National The Bureau of Standards^ was established by an act of Congress March 3, 1901. The Bureau's overall goal is to strengthen and advance the Nation's science and technology and facilitate their effective application for public benefit. To this end, the Bureau conducts research and provides: (1) a basis for the Nation's physical measurement system, (2) scientific and technological services for industry and government, (3) a technical basis for equity in trade, and (4) technical services to pro- mote public safety. The Bureau consists of the Institute for Basic Standards, the Institute for Materials Research, the Institute for Applied Technology, the Institute for Computer Sciences and Technology, the Office for Information Programs, and the Office of Experimental Technology Incentives Program. THE INSTITUTE FOR BASIC STANDARDS provides the central basis within the United States of a complete and consist- ent system of physical measurement; coordinates that system with measurement systems of other nations; and furnishes essen- tial services leading to accurate and uniform physical measurements throughout the Nation's scientific community, industry, and commerce. The Institute consists of the Office of Measurement Services, and the following center and divisions: Applied Mathematics — Electricity — Mechanics — Heat — Optical Physics — Center for Radiation Research — Lab- oratory Astrophysics- — Cryogenics^ — Electromagnetics"' — Time and Frequency". THE INSTITUTE FOR MATERIALS RESEARCH conducts materials research leading to improved methods of measure- ment, standards, and data on the properties of well-characterized materials needed by industry, commerce, educational insti- tutions, and Government; provides advisory and research services to other Government agencies; and develops, produces, and distributes standard reference materials. -
Bauxite and Aluminum Handbook Commodities and Export Projections Division Economic Analysis and Projectuonsdepartment
I Bauxite and Aluminum Handbook Commodities and Export Projections Division Economic Analysis and ProjectUonsDepartment 3 . February 1981 TABLE OF CONTENTS Page No. I. CHARACTERISTICSOF BAUXITE/ALUMINA/ALUIMINUM.............. 1 A. Introduction .......... 1 B. Definition of Products .......t ........ ......... * 1 C. Uses ....... ..... 2 D. Technology . ... ... 5 II. THE LOCATION OF THE INDUSTRY....................... #...... I A. Production...... ... .. ......................... .. 1 B. Consumption....... ... .. to. 6 C. Trade.................................. 8 III. THE STRUCTURE OF THE INDUSTRY........................ 1 A. Organization ................... .- .. ....... ... 1 B. Marketing .............# ............................ 4 O ZIV.ECONOMIC PARAMETERS FOR MARKET ANALYSIS OF THE BAUXITE-ALUMINUMINDUSTRY ......................................... 1 A. Demand and Supply Elasticities........ ........... 1 B. Price DeterminationMechanisms ....................... 2 V. MARKET PRICES FOR BAUXITE, ALUMINA AND ALUMINUM.......... 1 A. Bauxite................................ .... .*............... 1 B. Alumina .............................................. 7 C. Aluminum,, ........**.............. #.... **.*..................... 7 VI. SPECIAL ISSUES........................................... 1 A. Shipping................... .... .0.0.......................1 B. The InternationalBauxite Association (IBA) .......... 3 C. The Integrated Program for Commodities............... 4 D. United States Government Stockpile................... 5 February1981 -
Hydrothermal Synthesis of Well-Crystallised Boehmite Crystals of Various Shapes
Materials Research, Vol. 12, No. 4, 437-445, 2009 © 2009 Hydrothermal Synthesis of Well-Crystallised Boehmite Crystals of Various Shapes Pérsio de Souza Santosa, Antonio Carlos Vieira Coelhoa*, Helena de Souza Santosb, Pedro Kunihiko Kiyoharab aLaboratório de Matérias-Primas Particuladas e Sólidos Não Metálicos, Departamento de Engenharia Metalúrgica e de Materiais, Escola Politécnica, Universidade de São Paulo – USP, Av. Prof. Luciano Gualberto, Travessa 3, 380, 05508-970 São Paulo - SP, Brazil bLaboratório de Microscopia Eletrônica – LME, Departamento de Física Geral, Instituto de Física – IF, Universidade de São Paulo – USP, CP 66318, 05315-970 São Paulo - SP, Brazil Received: May 26, 2009; Revised: September 10, 2009 Aluminium monohydroxide, also known as aluminium oxyhydroxide (boehmite – AlO[OH]), is water insoluble but crystallises into microcrystals of various shapes. When, by X-ray diffraction, the microcrystals present a basal reflexion (d[020]) of 0.611 nm, the crystalline structure is referred to as “well-crystallised” boehmite. Natural and synthetic crystals of well-crystallised boehmite can have a plate-like shape with either a rhombic or hexagonal profile. Synthetic crystals can also be lath-like or ellipsoid in shape. The purpose of this paper is to present a method of hydrothermal synthesis using a single temperature (200 °C) for preparing plate-like crystals of well- crystallised boehmite with ellipsoid, rhombic, hexagonal, and lath-like profiles by using different precursors. Our observations suggest that all of these shapes are stages of growth of the microcrystals of well-crystallised boehmite along the c-axis direction of the rhombic crystals. Keywords: aluminium hydroxide, boehmite, pseudoboehmite, fibrillar pseudoboehmite 1.