Symmetry Relationships Between Crystal Structures: Applications Of
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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. -
Quartz Crystal Division of Seiko Instruments Inc
(1) Quartz Crystal Division of Seiko Instruments Inc. and affiliates, which is responsible for manufacturing the products described in this catalogue, holds ISO 9001 and ISO 14001 certification. (2) SII Crystal Technology Inc. Tochigi site holds IATF 16949 certification. Quartz Crystal Product Catalogue Electronic Components Sales Head Office 1-8, Nakase, Mihamaku, Chiba-shi, Chiba 261-8507, Japan Telephone:+81-43-211-1207 Facsimile:+81-43-211-8030 E-mail:[email protected] <Manufacturer> SII Crystal Technology Inc. 1110, Hirai-cho, Tochigi-shi, Tochigi 328-0054, Japan Released in February 2019 No.QTC2019EJ-02C1604 Creating Time - Optimizing Time - Enriching Time Seiko Instruments Inc. (SII), founded in 1937 as a member of the Seiko Group specializing in the manufacture of watches, has leveraged its core competency in high precision watches to create a wide range of new products and technologies. Over the years SII has developed high-precision processed parts and machine tools that pride themselves on their sub-micron processing capability, quartz crystals that came about as a result of our quartz watch R&D, and electronic components such as micro batteries. Optimizing our extensive experience and expertise, we have since diversified into such new fields as compact, lightweight, exceedingly quiet thermal printers, and inkjet printheads, a key component in wide format inkjet printers for corporate use. SII, in the years to come, will maintain an uncompromised dedication to its time-honored technologies and innovations of craftsmanship, miniaturization, and efficiency that meet the needs of our changing society and enrich the lives of those around us. SEIKO HOLDINGS GROUP 1881 1917 1983 1997 2007 K. -
WHAT IS...A Quasicrystal?, Volume 53, Number 8
?WHAT IS... a Quasicrystal? Marjorie Senechal The long answer is: no one is sure. But the short an- diagrams? The set of vertices of a Penrose tiling does— swer is straightforward: a quasicrystal is a crystal that was known before Shechtman’s discovery. But with forbidden symmetry. Forbidden, that is, by “The what other objects do, and how can we tell? The ques- Crystallographic Restriction”, a theorem that confines tion was wide open at that time, and I thought it un- the rotational symmetries of translation lattices in two- wise to replace one inadequate definition (the lattice) and three-dimensional Euclidean space to orders 2, 3, with another. That the commission still retains this 4, and 6. This bedrock of theoretical solid-state sci- definition today suggests the difficulty of the ques- ence—the impossibility of five-fold symmetry in crys- tion we deliberately but implicitly posed. By now a tals can be traced, in the mineralogical literature, back great many kinds of aperiodic crystals have been to 1801—crumbled in 1984 when Dany Shechtman, a grown in laboratories around the world; most of them materials scientist working at what is now the National are metals, alloys of two or three kinds of atoms—bi- Institute of Standards and Technology, synthesized nary or ternary metallic phases. None of their struc- aluminium-manganese crystals with icosahedral sym- tures has been “solved”. (For a survey of current re- metry. The term “quasicrystal”, hastily coined to label search on real aperiodic crystals see, for example, the such theretofore unthinkable objects, suggests the website of the international conference ICQ9, confusions that Shechtman’s discovery sowed. -
Bubble Raft Model for a Paraboloidal Crystal
Syracuse University SURFACE Physics College of Arts and Sciences 9-17-2007 Bubble Raft Model for a Paraboloidal Crystal Mark Bowick Department of Physics, Syracuse University, Syracuse, NY Luca Giomi Syracuse University Homin Shin Syracuse University Creighton K. Thomas Syracuse University Follow this and additional works at: https://surface.syr.edu/phy Part of the Physics Commons Recommended Citation Bowick, Mark; Giomi, Luca; Shin, Homin; and Thomas, Creighton K., "Bubble Raft Model for a Paraboloidal Crystal" (2007). Physics. 144. https://surface.syr.edu/phy/144 This Article is brought to you for free and open access by the College of Arts and Sciences at SURFACE. It has been accepted for inclusion in Physics by an authorized administrator of SURFACE. For more information, please contact [email protected]. Bubble Raft Model for a Paraboloidal Crystal Mark J. Bowick, Luca Giomi, Homin Shin, and Creighton K. Thomas Department of Physics, Syracuse University, Syracuse New York, 13244-1130 We investigate crystalline order on a two-dimensional paraboloid of revolution by assembling a single layer of millimeter-sized soap bubbles on the surface of a rotating liquid, thus extending the classic work of Bragg and Nye on planar soap bubble rafts. Topological constraints require crystalline configurations to contain a certain minimum number of topological defects such as disclinations or grain boundary scars whose structure is analyzed as a function of the aspect ratio of the paraboloid. We find the defect structure to agree with theoretical predictions and propose a mechanism for scar nucleation in the presence of large Gaussian curvature. Soft materials such as amphiphilic membranes, diblock any triangulation of M reads copolymers and colloidal emulsions can form ordered structures with a wide range of complex geometries and Q = X(6 ci)+ X (4 ci)=6χ , (1) − − topologies. -
Washington State Minerals Checklist
Division of Geology and Earth Resources MS 47007; Olympia, WA 98504-7007 Washington State 360-902-1450; 360-902-1785 fax E-mail: [email protected] Website: http://www.dnr.wa.gov/geology Minerals Checklist Note: Mineral names in parentheses are the preferred species names. Compiled by Raymond Lasmanis o Acanthite o Arsenopalladinite o Bustamite o Clinohumite o Enstatite o Harmotome o Actinolite o Arsenopyrite o Bytownite o Clinoptilolite o Epidesmine (Stilbite) o Hastingsite o Adularia o Arsenosulvanite (Plagioclase) o Clinozoisite o Epidote o Hausmannite (Orthoclase) o Arsenpolybasite o Cairngorm (Quartz) o Cobaltite o Epistilbite o Hedenbergite o Aegirine o Astrophyllite o Calamine o Cochromite o Epsomite o Hedleyite o Aenigmatite o Atacamite (Hemimorphite) o Coffinite o Erionite o Hematite o Aeschynite o Atokite o Calaverite o Columbite o Erythrite o Hemimorphite o Agardite-Y o Augite o Calciohilairite (Ferrocolumbite) o Euchroite o Hercynite o Agate (Quartz) o Aurostibite o Calcite, see also o Conichalcite o Euxenite o Hessite o Aguilarite o Austinite Manganocalcite o Connellite o Euxenite-Y o Heulandite o Aktashite o Onyx o Copiapite o o Autunite o Fairchildite Hexahydrite o Alabandite o Caledonite o Copper o o Awaruite o Famatinite Hibschite o Albite o Cancrinite o Copper-zinc o o Axinite group o Fayalite Hillebrandite o Algodonite o Carnelian (Quartz) o Coquandite o o Azurite o Feldspar group Hisingerite o Allanite o Cassiterite o Cordierite o o Barite o Ferberite Hongshiite o Allanite-Ce o Catapleiite o Corrensite o o Bastnäsite -
Crystal Structures and Symmetry 1 Crystal Structures and Symmetry
PHYS 624: Crystal Structures and Symmetry 1 Crystal Structures and Symmetry Introduction to Solid State Physics http://www.physics.udel.edu/∼bnikolic/teaching/phys624/phys624.html PHYS 624: Crystal Structures and Symmetry 2 Translational Invariance • The translationally invariant nature of the periodic solid and the fact that the core electrons are very tightly bound at each site (so we may ignore their dynamics) makes approximate solutions to many-body problem ≈ 1021 atoms/cm3 (essentially, a thermodynamic limit) possible. Figure 1: The simplest model of a solid is a periodic array of valance orbitals embedded in a matrix of atomic cores. Solving the problem in one of the irreducible elements of the periodic solid (e.g., one of the spheres in the Figure), is often equivalent to solving the whole system. PHYS 624: Crystal Structures and Symmetry 3 From atomic orbitals to solid-state bands • If two orbitals are far apart, each orbital has a Hamiltonian H0 = εn, where n is the orbital occupancy ⇐ Ignoring the effects of electronic corre- lations (which would contribute terms proportional to n↑n↓). + +++ ... = Band E Figure 2: If we bring many orbitals into proximity so that they may exchange electrons (hybridize), then a band is formed centered around the location of the isolated orbital, and with width proportional to the strength of the hybridization PHYS 624: Crystal Structures and Symmetry 4 From atomic orbitals to solid-state bands • Real Life: Solids are composed of elements with multiple orbitals that produce multiple bonds. Now imagine what happens if we have several orbitals on each site (ie s,p, etc.), as we reduce the separation between the orbitals and increase their overlap, these bonds increase in width and may eventually overlap, forming bands. -
Crystal Symmetry Groups
X-Ray and Neutron Crystallography rational numbers is a group under Crystal Symmetry Groups multiplication, and both it and the integer group already discussed are examples of infinite groups because they each contain an infinite number of elements. ymmetry plays an important role between the integers obey the rules of In the case of a symmetry group, in crystallography. The ways in group theory: an element is the operation needed to which atoms and molecules are ● There must be defined a procedure for produce one object from another. For arrangeds within a unit cell and unit cells example, a mirror operation takes an combining two elements of the group repeat within a crystal are governed by to form a third. For the integers one object in one location and produces symmetry rules. In ordinary life our can choose the addition operation so another of the opposite hand located first perception of symmetry is what that a + b = c is the operation to be such that the mirror doing the operation is known as mirror symmetry. Our performed and u, b, and c are always is equidistant between them (Fig. 1). bodies have, to a good approximation, elements of the group. These manipulations are usually called mirror symmetry in which our right side ● There exists an element of the group, symmetry operations. They are com- is matched by our left as if a mirror called the identity element and de- bined by applying them to an object se- passed along the central axis of our noted f, that combines with any other bodies. -
Quasicrystals a New Kind of Symmetry Sandra Nair First, Definitions
Quasicrystals A new kind of symmetry Sandra Nair First, definitions ● A lattice is a poset in which every element has a unique infimum and supremum. For example, the set of natural numbers with the notion of ordering by magnitude (1<2). For our purposes, we can think of an array of atoms/molecules with a clear sense of assignment. ● A Bravais lattice is a discrete infinite array of points generated by linear integer combinations of 3 independent primitive vectors: {n1a1 + n2a2 + n3a3 | n1, n2, n3 ∈ Z}. ● Crystal structures = info of lattice points + info of the basis (primitive) vectors. ● Upto isomorphism of point groups (group of isometries leaving at least 1 fixed point), 14 different Bravais lattice structures possible in 3D. Now, crystals... ● Loosely speaking, crystals are molecular arrangements built out of multiple unit cells of one (or more) Bravais lattice structures. ● Crystallographic restriction theorem: The rotational symmetries of a discrete lattice are limited to 2-, 3-, 4-, and 6-fold. ● This leads us to propose a “functional” definition: A crystal is a material that has a discrete diffraction pattern, displaying rotational symmetries of orders 2, 3, 4 and 6. ● Note: Order 5 is a strictly forbidden symmetry → important for us. Tessellations aka tilings Now that we have diffraction patterns to work with, we consider the question of whether a lattice structure tiles or tessellates the plane. This is where the order of the symmetry plays a role. The crystals are special, as they display translational symmetries. As such, the tiling of their lattice structures (which we could see thanks to diffraction patterns) are periodic- they repeat at regular intervals. -
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]. -
Nickeline Nias C 2001-2005 Mineral Data Publishing, Version 1
Nickeline NiAs c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Hexagonal. Point Group: 6/m 2/m 2/m. Commonly in granular aggregates, reniform masses with radial structure, and reticulated and arborescent growths. Rarely as distorted, horizontally striated, {1011} terminated crystals, to 1.5 cm. Twinning: On {1011} producing fourlings; possibly on {3141}. Physical Properties: Fracture: Conchoidal. Tenacity: Brittle. Hardness = 5–5.5 VHN = n.d. D(meas.) = 7.784 D(calc.) = 7.834 Optical Properties: Opaque. Color: Pale copper-red, tarnishes gray to blackish; white with strong yellowish pink hue in reflected light. Streak: Pale brownish black. Luster: Metallic. Pleochroism: Strong; whitish, yellow-pink to pale brownish pink. Anisotropism: Very strong, pale greenish yellow to slate-gray in air. R1–R2: (400) 39.2–45.4, (420) 38.0–44.2, (440) 36.8–43.5, (460) 36.2–43.2, (480) 37.2–44.3, (500) 39.6–46.4, (520) 42.3–48.6, (540) 45.3–50.7, (560) 48.2–52.8, (580) 51.0–54.8, (600) 53.7–56.7, (620) 55.9–58.4, (640) 57.8–59.9, (660) 59.4–61.3, (680) 61.0–62.5, (700) 62.2–63.6 Cell Data: Space Group: P 63/mmc. a = 3.621(1) c = 5.042(1) Z = 2 X-ray Powder Pattern: Unknown locality. 2.66 (100), 1.961 (90), 1.811 (80), 1.071 (40), 1.328 (30), 1.033 (30), 0.821 (30) Chemistry: (1) (2) Ni 43.2 43.93 Co 0.4 Fe 0.2 As 55.9 56.07 Sb 0.1 S 0.1 Total 99.9 100.00 (1) J´achymov, Czech Republic; by electron microprobe, corresponds to (Ni0.98Co0.01 Fe0.01)Σ=1.00As1.00. -
Multidisciplinary Design Project Engineering Dictionary Version 0.0.2
Multidisciplinary Design Project Engineering Dictionary Version 0.0.2 February 15, 2006 . DRAFT Cambridge-MIT Institute Multidisciplinary Design Project This Dictionary/Glossary of Engineering terms has been compiled to compliment the work developed as part of the Multi-disciplinary Design Project (MDP), which is a programme to develop teaching material and kits to aid the running of mechtronics projects in Universities and Schools. The project is being carried out with support from the Cambridge-MIT Institute undergraduate teaching programe. For more information about the project please visit the MDP website at http://www-mdp.eng.cam.ac.uk or contact Dr. Peter Long Prof. Alex Slocum Cambridge University Engineering Department Massachusetts Institute of Technology Trumpington Street, 77 Massachusetts Ave. Cambridge. Cambridge MA 02139-4307 CB2 1PZ. USA e-mail: [email protected] e-mail: [email protected] tel: +44 (0) 1223 332779 tel: +1 617 253 0012 For information about the CMI initiative please see Cambridge-MIT Institute website :- http://www.cambridge-mit.org CMI CMI, University of Cambridge Massachusetts Institute of Technology 10 Miller’s Yard, 77 Massachusetts Ave. Mill Lane, Cambridge MA 02139-4307 Cambridge. CB2 1RQ. USA tel: +44 (0) 1223 327207 tel. +1 617 253 7732 fax: +44 (0) 1223 765891 fax. +1 617 258 8539 . DRAFT 2 CMI-MDP Programme 1 Introduction This dictionary/glossary has not been developed as a definative work but as a useful reference book for engi- neering students to search when looking for the meaning of a word/phrase. It has been compiled from a number of existing glossaries together with a number of local additions. -
Cobalt Mineral Ecology
American Mineralogist, Volume 102, pages 108–116, 2017 Cobalt mineral ecology ROBERT M. HAZEN1,*, GRETHE HYSTAD2, JOSHUA J. GOLDEN3, DANIEL R. HUMMER1, CHAO LIU1, ROBERT T. DOWNS3, SHAUNNA M. MORRISON3, JOLYON RALPH4, AND EDWARD S. GREW5 1Geophysical Laboratory, Carnegie Institution, 5251 Broad Branch Road NW, Washington, D.C. 20015, U.S.A. 2Department of Mathematics, Computer Science, and Statistics, Purdue University Northwest, Hammond, Indiana 46323, U.S.A. 3Department of Geosciences, University of Arizona, 1040 East 4th Street, Tucson, Arizona 85721-0077, U.S.A. 4Mindat.org, 128 Mullards Close, Mitcham, Surrey CR4 4FD, U.K. 5School of Earth and Climate Sciences, University of Maine, Orono, Maine 04469, U.S.A. ABSTRACT Minerals containing cobalt as an essential element display systematic trends in their diversity and distribution. We employ data for 66 approved Co mineral species (as tabulated by the official mineral list of the International Mineralogical Association, http://rruff.info/ima, as of 1 March 2016), represent- ing 3554 mineral species-locality pairs (www.mindat.org and other sources, as of 1 March 2016). We find that cobalt-containing mineral species, for which 20% are known at only one locality and more than half are known from five or fewer localities, conform to a Large Number of Rare Events (LNRE) distribution. Our model predicts that at least 81 Co minerals exist in Earth’s crust today, indicating that at least 15 species have yet to be discovered—a minimum estimate because it assumes that new minerals will be found only using the same methods as in the past. Numerous additional cobalt miner- als likely await discovery using micro-analytical methods.