Ceramic Materials to Replace Silicon, Because Ceramic Are Tougher, More Refractory and More Inert E.G

Total Page:16

File Type:pdf, Size:1020Kb

Ceramic Materials to Replace Silicon, Because Ceramic Are Tougher, More Refractory and More Inert E.G What are Ceramics? Ceramics are inorganic, non -metallic and crystalline materials that are typically produced using clays and other minerals from the earth or CERAMIC chemically processed powders MATERIALS Ceramics are crystalline and are compounds formed between metall ic MATERIALS and non -metallic elements such as aluminium and oxygen (alumina - Al 2O3 ), silicon and nitrogen (silicon nitride - Si 3N4) and silicon and carbon (silicon carbide -SiC). Glasses are non -metallic, inorganic but amorphous . They are often considered as belonging to ceramics. Characteristics of Ceramics Characteristics of Ceramics Structure of Ceramics Ceramics Metals Polymers Ceramics exhibit ionic, covalent bonding or a combination of the two (like in Al 2O3) Low density High density Very low density High T m Medium to high T m Low Tm Type of bonding strongly influences the crystal structure of cer amics High elastic modulus Medium to high elastic Low elastic modulus Brittle modulus Brittle modulus Ductile and brittle lCeramics crystallise in two main groups: Non -reactive Ductile Goff electrical and Reactive (corrode) thermal insulators Good electrical and 1. Ceramics with simple crystal structure (e.g; SiC, MgO) High hardness and thermal conductors wear resistance 2. Ceramics with complex crystal structures based on silicate SiO 4 (known as silicates) Ceramic Bonding • Bonding: Ionic bonding : metallic ions + nonmetallic ions -- Mostly ionic, some covalent. Cations Anions -- % ionic character increases with difference in electronegativity. Stable structure • Large vs small ionic bond character: Coordination Number: RC/R A CaF 2: large SiC: small RC/R A = 0.155 Adapted from Fig. 2.7, Callister 7e. (Fig. 2.7 is adapted from Linus Pauling, The Nature of the Chemical Bond , 3rd edition, Copyright 1939 and 1940, 3rd edition. Copyright 1960 by Cornell University. 6 Ceramic crystal structure considerations Charge Neutrality The bulk ceramic must remain electrically neutral For example, the compound MgO 2 does not exist Mg +2 & O -2: net charge / molecule = 1(+2) + 2( -2) = -2 must MgO Coordination Number (CN) : The number of atomic or ionic nearest neighbors. Depends on atomic size ratio CN increases as the RC/R A increases CN determines the possible crystal structure, Thus, CN determines the physical properties MgO and FeO Examples of AX type structure MgO and FeO also have the NaCl structure Cs + 2- O rO = 0.140 nm Cl - 2+ Mg rMg = 0.072 nm Rock Salt Structure = Na + Adapted from Fig. = Cl - 12.2, Callister 7e. Each oxygen has 6 neighboring Mg 2+ 10 AX Crystal Structures AX Crystal Structures AX–Type Crystal Structures include NaCl, CsCl, and zinc blende Zinc Blende structure Cesium Chloride structure: Ex: ZnO, ZnS, SiC r + .0 170 Cs = = .0 939 r − .0 181 Cl + - Each Cs has 8 neighboring Cl Adapted from Fig. 12.4, Callister 7e. Adapted from Fig. 12.3, Callister 7e. 11 12 ABX Crystal Structures AX 2 Crystal Structures 3 Fluoride structure • Perovskite • Calcium Fluoride (CaF ) 2 Ex: complex oxide BaTiO • cations in cubic sites 3 • UO 2, ThO 2, ZrO 2, CeO 2 Adapted from Fig. 12.6, Callister 7e. Adapted from Fig. 12.5, Callister 7e. 13 14 Mechanical Properties We know that ceramics are more brittle than metals. ceramics Why? • Consider method of deformation slippage along slip planes Glasses Refractories Cements Eng. Ceramics in ionic solids this slippage is very difficult Clay Products Abrasives too much energy needed to move one anion past another anion Glasses Glass - ceramics Our focus is HERE !!! 15 Engineering ceramics are generally Bioceramics classified into the following: Cutting tools Structural ceramics, Industrial wear parts, bioceramics, cutting tools, engine components Electrical and Electronic ceramics, Capacitors, insulators, substrates, IC packages, piezoelectrics, magnets, superconductors Engine parts Ceramic coatings, Industrial wear parts, cutting tools, engine components Chemical processing & environmental Coating ceramics Filters, membranes, catalysts Silicates Silicate Ceramics Si -O Tetrahedron O 4- Combine SiO 4 tetrahedra by having them share Most common elements on Si corners, edges, or faces earth are Si & O The strong Si-O bond leads to a strong, high melting material Adapted from Fig. (1710ºC) 12.12, Callister 7e. Mg 2SiO 4 Ca 2MgSi 2O7 Cations such as Ca 2+ , Mg 2+ , & Al 3+ act to neutralize & provide ionic bonding 20 Si -O Tetrahedron O Silicate Ceramics O Two most common silicate ceramics are: 2. Silica Glasses Si Silica and silica glasses If the tetrahedra are randomly arranged, a non - crystalline structure, known as Glass is formed. Silica glasses is a dense form of amorphous Silica 1. Silica (SiO ) Silica (SiO 2) silica - Charge imbalance corrected with + If the tetrahedra are arranged in a “counter cations” such as Na regular and ordered manner, a -Borosilicate glass is the pyrex glass crystalline structure is formed. Silica used in labs have 3 different types: quartz, -better temperature stability & less crystobalite and tridymite brittle than sodium glass Amorphous Silica Other oxides may also be incorporated into a • Silica gels - amorphous SiO 2 glassy SiO 2 network in different ways: Si 4+ and O 2- not in well-ordered lattice 1. Network formers: form glassy structures (B O ) Charge balanced by H + (to form 2 3 OH -) at “dangling” bonds 2. Network modifiers: added to terminate (break 2 very high surface area > 200 m /g up) the network (CaO, Na 2O). These are added to silica glass to lower its viscosity (so SiO 2 is quite stable, therefore unreactive that forming is easier) makes good catalyst support 3. Network intermediates: these oxides cannot form glass network but join into the silica network and substitute for Si. Adapted from Fig. 12.11, Callister 7e. 23 Carbon Forms Carbon Forms • Carbon black – amorphous – • layer structure – aromatic layers surface area ca. 1000 m 2/g • Diamond tetrahedral carbon hard – no good slip planes brittle – can cut it Adapted from Fig. large diamonds – jewellery 12.17, Callister 7e. small diamonds often man made - used for cutting tools and polishing Adapted from Fig. 12.15, Callister 7e. weak van der Waal’s forces between layers diamond films hard surface coat – tools, planes slide easily, good lubricant medical devices, etc. 25 26 Carbon Forms Defects in Ceramic Structures • Frenkel Defect • Fullerenes or carbon nanotubes -a cation is out of place. wrap the graphite sheet by curving into ball or tube • Shottky Defect -- a paired set of cation and anion vacancies. Buckminister fullerenes Shottky Like a soccer ball C 60 - also C 70 + others Defect: Adapted from Fig. 12.21, Callister 7e. (Fig. 12.21 is from W.G. Moffatt, G.W. Pearsall, and J. Wulff, The Structure and Properties of Materials , Vol. 1, Structure , John Wiley and Sons, Inc., p. 78.) Frenkel Defect −Q / kT Adapted from Figs. • Equilibrium concentration of defects D 12.18 & 12.19, ~ e Callister 7e. 27 28 Mechanical Properties of Ceramics Mechanical Properties of Ceramics Ceramics have inferior mechanical properties compared to metals, and this Ceramics have excellent compressive strength (used in cement and has limited their applications concrete in foundations for structures and equipment) The main limitation is that ceramics fail in “brittle ” manner with little or no The principles source of fracture in ceramics is surface cracks, porosity, plastic deformation. inclusions and large grains produced during processing. Fracture strength of ceramics are significantly lower than predi cted by Testing ceramics using the usual tensile testing is not possible , so a theory because of the presence of very small cracks in the mater ial (stress transverse bending test is used and a modulus of rupture (MOR) is concentrators). determined. Lack of ductility in ceramics is due to their strong ionic and c ovalent bonds. Strength of ceramics can only be described by statistical method s and it is dependent on specimen size. Transverse rupture Compressive Elastic strength strength modulus Hardness Poisson’s Density Material Symbol (MPa) (MPa) (GPa) (HK) ratio ( n) (kg/m 3) Aluminum Al 2O3 140–240 1000–2900 310–410 2000–3000 0.26 4000–4500 oxide Cubic boron CBN 725 7000 850 4000–5000 — 3480 nitride Diamond — 1400 7000 830–1000 7000–8000 — 3500 Silica, fused SiO 2 — 1300 70 550 0.25 — Silicon SiC 100–750 700–3500 240–480 2100–3000 0.14 3100 carbide Silicon Si 3 N4 480–600 — 300–310 2000–2500 0.24 3300 nitride Titanium TiC 1400–1900 3100–3850 310–410 1800–3200 — 5500–5800 carbide Flexural 3F L Tungsten WC 1030–2600 4100–5900 520–700 1800–2400 — 10,000–15,000 f carbide 2 Rectangular cross section strength, σfs = 2 Partially PSZ 620 — 200 1100 0.30 5800 bd stabilized zirconia 3 Ff L The properties vary widely depending on the condition of the material (crack size) = 3 Circular cross section πR Factors Affecting Strength of Ceramics Failure of ceramics occurs mainly from structural defects; surface cracks, porosity, inclusions and large grains during processing. Toughening Mechanisms of Ceramics Porosity in ceramics acts as stress Fracture strength or toughness of ceramics can be improved only by concentrators: crack forms and propagates mechanisms that influence the crack propagation (ceramics always leading to failure. contain cracks). Once cracks start to propagate, they will continue to grow until fracture occurs. There are various methods used to improve the toughness of Porosity also decrease the cross -sectional ceramics: area over which a load in applied: lower the stress a material can support. 1. Transformation toughening Strength of ceramics is thus determined by many factors: 2. Microcrack induced toughening 1. Chemical composition 2. Microstructure - In dense ceramics materials, no large pores, the flaw is 3. Crack deflection related to grain size. Finer grain size ceramics, smaller flaws size at the boundaries, hence stronger than large grain size. 4. Crack bridging 3. Surface condition 4. Temperature and environment (failure at RT, usually due to larg e flaws).
Recommended publications
  • Crystal Structures
    Crystal Structures Academic Resource Center Crystallinity: Repeating or periodic array over large atomic distances. 3-D pattern in which each atom is bonded to its nearest neighbors Crystal structure: the manner in which atoms, ions, or molecules are spatially arranged. Unit cell: small repeating entity of the atomic structure. The basic building block of the crystal structure. It defines the entire crystal structure with the atom positions within. Lattice: 3D array of points coinciding with atom positions (center of spheres) Metallic Crystal Structures FCC (face centered cubic): Atoms are arranged at the corners and center of each cube face of the cell. FCC continued Close packed Plane: On each face of the cube Atoms are assumed to touch along face diagonals. 4 atoms in one unit cell. a 2R 2 BCC: Body Centered Cubic • Atoms are arranged at the corners of the cube with another atom at the cube center. BCC continued • Close Packed Plane cuts the unit cube in half diagonally • 2 atoms in one unit cell 4R a 3 Hexagonal Close Packed (HCP) • Cell of an HCP lattice is visualized as a top and bottom plane of 7 atoms, forming a regular hexagon around a central atom. In between these planes is a half- hexagon of 3 atoms. • There are two lattice parameters in HCP, a and c, representing the basal and height parameters Volume respectively. 6 atoms per unit cell Coordination number – the number of nearest neighbor atoms or ions surrounding an atom or ion. For FCC and HCP systems, the coordination number is 12. For BCC it’s 8.
    [Show full text]
  • Crystal Structure of a Material Is Way in Which Atoms, Ions, Molecules Are Spatially Arranged in 3-D Space
    Crystalline Structures – The Basics •Crystal structure of a material is way in which atoms, ions, molecules are spatially arranged in 3-D space. •Crystal structure = lattice (unit cell geometry) + basis (atom, ion, or molecule positions placed on lattice points within the unit cell). •A lattice is used in context when describing crystalline structures, means a 3-D array of points in space. Every lattice point must have identical surroundings. •Unit cell: smallest repetitive volume •Each crystal structure is built by stacking which contains the complete lattice unit cells and placing objects (motifs, pattern of a crystal. A unit cell is chosen basis) on the lattice points: to represent the highest level of geometric symmetry of the crystal structure. It’s the basic structural unit or building block of crystal structure. 7 crystal systems in 3-D 14 crystal lattices in 3-D a, b, and c are the lattice constants 1 a, b, g are the interaxial angles Metallic Crystal Structures (the simplest) •Recall, that a) coulombic attraction between delocalized valence electrons and positively charged cores is isotropic (non-directional), b) typically, only one element is present, so all atomic radii are the same, c) nearest neighbor distances tend to be small, and d) electron cloud shields cores from each other. •For these reasons, metallic bonding leads to close packed, dense crystal structures that maximize space filling and coordination number (number of nearest neighbors). •Most elemental metals crystallize in the FCC (face-centered cubic), BCC (body-centered cubic, or HCP (hexagonal close packed) structures: Room temperature crystal structure Crystal structure just before it melts 2 Recall: Simple Cubic (SC) Structure • Rare due to low packing density (only a-Po has this structure) • Close-packed directions are cube edges.
    [Show full text]
  • 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.
    [Show full text]
  • Crystal Structure
    Physics 927 E.Y.Tsymbal Section 1: Crystal Structure A solid is said to be a crystal if atoms are arranged in such a way that their positions are exactly periodic. This concept is illustrated in Fig.1 using a two-dimensional (2D) structure. y T C Fig.1 A B a x 1 A perfect crystal maintains this periodicity in both the x and y directions from -∞ to +∞. As follows from this periodicity, the atoms A, B, C, etc. are equivalent. In other words, for an observer located at any of these atomic sites, the crystal appears exactly the same. The same idea can be expressed by saying that a crystal possesses a translational symmetry. The translational symmetry means that if the crystal is translated by any vector joining two atoms, say T in Fig.1, the crystal appears exactly the same as it did before the translation. In other words the crystal remains invariant under any such translation. The structure of all crystals can be described in terms of a lattice, with a group of atoms attached to every lattice point. For example, in the case of structure shown in Fig.1, if we replace each atom by a geometrical point located at the equilibrium position of that atom, we obtain a crystal lattice. The crystal lattice has the same geometrical properties as the crystal, but it is devoid of any physical contents. There are two classes of lattices: the Bravais and the non-Bravais. In a Bravais lattice all lattice points are equivalent and hence by necessity all atoms in the crystal are of the same kind.
    [Show full text]
  • The American Mineralogist Crystal Structure Database
    American Mineralogist, Volume 88, pages 247–250, 2003 The American Mineralogist crystal structure database ROBERT T. DOWNS* AND MICHELLE HALL-WALLACE Department of Geosciences, University of Arizona, Tucson, Arizona 85721-0077, U.S.A. ABSTRACT A database has been constructed that contains all the crystal structures previously published in the American Mineralogist. The database is called “The American Mineralogist Crystal Structure Database” and is freely accessible from the websites of the Mineralogical Society of America at http://www.minsocam.org/MSA/Crystal_Database.html and the University of Arizona. In addition to the database, a suite of interactive software is provided that can be used to view and manipulate the crystal structures and compute different properties of a crystal such as geometry, diffraction patterns, and procrystal electron densities. The database is set up so that the data can be easily incorporated into other software packages. Included at the website is an evolving set of guides to instruct the user and help with classroom education. INTRODUCTION parameters; (5) incorporating comments from either the origi- The structure of a crystal represents a minimum energy con- nal authors or ourselves when changes are made to the origi- figuration adopted by a collection of atoms at a given tempera- nally published data. Each record in the database consists of a ture and pressure. In principle, all the physical and chemical bibliographic reference, cell parameters, symmetry, atomic properties of any crystalline substance can be computed from positions, displacement parameters, and site occupancies. An knowledge of its crystal structure. The determination of crys- example of a data set is provided in Figure 1.
    [Show full text]
  • Crystal Structures and Symmetries
    Crystal Structures and Symmetries G. Roth This document has been published in Manuel Angst, Thomas Brückel, Dieter Richter, Reiner Zorn (Eds.): Scattering Methods for Condensed Matter Research: Towards Novel Applications at Future Sources Lecture Notes of the 43rd IFF Spring School 2012 Schriften des Forschungszentrums Jülich / Reihe Schlüsseltechnologien / Key Tech- nologies, Vol. 33 JCNS, PGI, ICS, IAS Forschungszentrum Jülich GmbH, JCNS, PGI, ICS, IAS, 2012 ISBN: 978-3-89336-759-7 All rights reserved. B 1 Crystal Structures and Symmetries G. Roth Institute of Crystallography RWTH Aachen University Contents B 1 Crystal Structures and Symmetries ................................................1 1.1 Crystal lattices ...................................................................................2 1.2 Crystallographic coordinate systems ..............................................4 1.3 Symmetry-operations and -elements...............................................7 1.4 Crystallographic point groups and space groups ........................10 1.5 Quasicrystals....................................................................................13 1.6 Application: Structure description of YBa2Cu3O7-δ ....................14 ________________________ Lecture Notes of the 43rd IFF Spring School "Scattering Methods for Condensed Matter Research: Towards Novel Applications at Future Sources" (Forschungszentrum Jülich, 2012). All rights reserved. B1.2 G. Roth Introduction The term “crystal” derives from the Greek κρύσταλλος , which was first
    [Show full text]
  • Crystal Structure and Mechanical Properties of Thbc2
    crystals Article Crystal Structure and Mechanical Properties of ThBC2 Xinchun Zhou and Baobing Zheng * College of Physics and Optoelectronic Technology & Advanced Titanium Alloys and Functional Coatings Cooperative Innovation Center, Baoji University of Arts and Sciences, Baoji 721016, China * Correspondence: [email protected]; Tel.: +86-917-3364-258 Received: 6 July 2019; Accepted: 27 July 2019; Published: 29 July 2019 Abstract: Thorium borocarbide compounds have fascinating physical properties and diverse structures, and hence have stimulated great interest. In this work, we determine the ground state structure of ThBC2 by the unbiased structure prediction method based on first-principles calculations. The dynamical and elastic stabilities of our proposed ThBC2 are verified by the calculations of phonon spectrum and elastic constants. To study the mechanical properties fundamentally, we estimated the elastic anisotropy of ThBC2. The results show that the Young’s and shear moduli possess high degree of anisotropy. The ideal strength calculations reveal that ThBC2 readily collapses upon applied stress due to small ideal strengths. The cleavage fracture probably occurs along the [111] direction while slip may easily appear along the [110] direction on the (111) plane for ThBC2. In addition, we provide an atomic explanation for the different characteristics of the strain–stress curves under different strains. Keywords: ThBC2; crystal structure; anisotropic mechanical properties; ideal strength; first-principles calculations 1. Introduction Due to the potential application in fission fuel, actinoid-metal borocarbides are of great interest, especially thorium borocarbide compounds [1–7]. Thorium borocarbide compounds have diversified stoichiometric proportions with different crystal structures due to the flexible B–C framework.
    [Show full text]
  • 1.1 Silicon Crystal Structure
    EECS143 Microfabrication Technology Professor Ali Javey Introduction to Materials Lecture 1 Evolution of Devices Yesterday’s Transistor (1947) Today’s Transistor (2006) Why “Semiconductors”? • Conductors – e.g Metals • Insulators – e.g. Sand (SiO2 ) • Semiconductors – conductivity between conductors and insulators – Generally crystalline in structure • In recent years, non-crystalline semiconductors have become commercially very important Polycrystalline amorphous crystalline What are semiconductors Elements: Si, Ge, C Binary: GaAs, InSb, SiC, CdSe, etc. Ternary+: AlGaAs, InGaAs, etc. Electrons and Holes in Semiconductors Silicon Crystal Structure • Unit cell of silicon crystal is cubic. • Each Si atom has 4 nearest neighbors. 5.43 Å Silicon Wafers and Crystal Planes z z z • The standard notation for crystal planes is y y y based on the cubic unit cell. x x (100) x (011) (111) • Silicon wafers are usually cut along the (100) plane (100) plane with a flat (011) or notch to help orient flat Si (111) plane the wafer during IC fabrication. Bond Model of Electrons and Holes (Intrinsic Si) Si Si Si • Silicon crystal in a two-dimensional Si Si Si representation. Si Si Si Si Si Si Si Si Si Si Si Si Si Si Si Si Si Si Si Si Si • When an electron breaks loose and becomes a conduction electron, a hole is also created. Dopants in Silicon Si Si Si Si Si Si Si As Si Si B Si Si Si Si Si Si Si N-type Si P-type Si • As (Arsenic), a Group V element, introduces conduction electrons and creates N-type silicon, and is called a donor.
    [Show full text]
  • Preparation, Crystal Structure, Properties, and Electronic Band Structure of Tltase3 Christoph L
    Preparation, Crystal Structure, Properties, and Electronic Band Structure of TlTaSe3 Christoph L. Teskea, Wolfgang Benscha, Diana Beneab, Jan Min´arb, Alexander Perlovb, and Hubert Ebertb a Institut f¨ur Anorganische Chemie, Christian-Albrechts-Universit¨at, Otto-Hahn-Platz 6/7, D-24098 Kiel, Germany b M¨unchen, Department Chemie – Physikalische Chemie, Ludwigs-Maximilians-Universit¨at, Butenandtstraße 11, D-81377 M¨unchen Reprint requests to Dr. C. Teske. Fax: +49 431 880 1520. E-mail: [email protected] Z. Naturforsch. 60b, 858 – 866 (2005); received June 10, 2005 TlTaSe3 was prepared from a fused mixture of Tl4Ta2Se11, Ta and Se in the molar ratio 1:2:1. The compound shows dimorphism with H-TlTaSe3, hexagonal, space group P63/mmc, a = 7.2436(6), c = 5.9736(6) A,˚ c/a = 1.213 and O-TlTaSe3, orthorhombic, space group Pnma, a = 9.554(13), b = 3.6244(6), c = 14.7271(17) A.˚ The crystal structure of H-TlTaSe3 is isotypic to BaVSe3 whereas that of O-TlTaSe3 is closely related to the NH4CdCl3-type. Characteristic features of the structures are: 1 2− ∞[TaSe3 ] chains of regular octahedra sharing faces along [001] for the hexagonal form and columns 1 2− of double edge-sharing octahedra ∞[Ta2Se6 ] running along [010] for O-TlTaSe3. The columns are each separated by Tl+ ions with the coordination number CN = 12 and CN = 8 respectively. The structures are compared and discussed in context with other isotypic structures of chalcogenides. The orthorhombic modification O-TlTaSe3 is a semiconductor while H-TlTaSe3 shows conventional metallic behaviour. The electronic structures of both modifications are discussed on the base of band structure calculations performed within the framework of density functional theory.
    [Show full text]
  • Crystal Structures of Minerals in the Lower Mantle
    6 Crystal Structures of Minerals in the Lower Mantle June K. Wicks and Thomas S. Duffy ABSTRACT The crystal structures of lower mantle minerals are vital components for interpreting geophysical observations of Earth’s deep interior and in understanding the history and composition of this complex and remote region. The expected minerals in the lower mantle have been inferred from high pressure‐temperature experiments on mantle‐relevant compositions augmented by theoretical studies and observations of inclusions in natural diamonds of deep origin. While bridgmanite, ferropericlase, and CaSiO3 perovskite are expected to make up the bulk of the mineralogy in most of the lower mantle, other phases such as SiO2 polymorphs or hydrous silicates and oxides may play an important subsidiary role or may be regionally important. Here we describe the crystal structure of the key minerals expected to be found in the deep mantle and discuss some examples of the relationship between structure and chemical and physical properties of these phases. 6.1. IntrODUCTION properties of lower mantle minerals [Duffy, 2005; Mao and Mao, 2007; Shen and Wang, 2014; Ito, 2015]. Earth’s lower mantle, which spans from 660 km depth The crystal structure is the most fundamental property to the core‐mantle boundary (CMB), encompasses nearly of a mineral and is intimately related to its major physical three quarters of the mass of the bulk silicate Earth (crust and chemical characteristics, including compressibility, and mantle). Our understanding of the mineralogy and density,
    [Show full text]
  • Engineering Materials and Processes Lecture 4 – Crystal Structure of Metals
    Engineering Materials and Processes Lecture 4 – Crystal Structure of Metals Grains after acid etching: Wikipedia Crystal Structure of Metals Reference Text Section Higgins RA & Bolton, 2010. Materials for Engineers and Technicians, Ch 4 5th ed, Butterworth Heinemann Additional Readings Section Sheedy, P. A, 1994. Materials : Their properties, testing and selection Ch 1 Callister, W. Jr. and Rethwisch, D., 2010, Materials Science and Ch 3 Engineering: An Introduction, 8th Ed, Wiley, New York. Engineering Materials and Processes Crystal Structure of Metals Crystals are the lattice structure that metal atoms form when they become solid. In engineering, crystals of metal are called grains. Grains in cast aluminium www.spaceflight.esa.int Engineering Materials and Processes Solid, Liquid, Gas Everything can exist as either solid, liquid or gas. (state). This depends on temperature and pressure. Mercury freezes at -9°C and boils (to form a gas or vapour) at 357°C at 1 atm. Liquid Mercury: Wikipedia At the other end of the scale, tungsten melts at 3410°C and ° Mercury vapour streetlights: theage.com.au boils at 5930 C. Engineering Materials and Processes Classification of Materials by State • Solid: Rigid structure of atoms (or molecules). A regular pattern of atoms is called a crystal (ceramics) or a grain (metals). Random is called amorphous (some plastics). Low temperature all materials freeze (become solid). • Liquid: A liquid is a substance that flows (fluid) but does not compress easily. Solids become liquid when heated to their melting point (fusion) • Gas: A gas is a compressible fluid, that expands to fill its container. At high temperature all materials vapourise to a gas.
    [Show full text]
  • Crystal Structure CRYSTAL STRUCTURES
    Crystal Structure CRYSTAL STRUCTURES Lecture 2 A.H. Harker Physics and Astronomy UCL Lattice and Basis Version: June 6, 2002; Typeset on October 30, 2003,15:28 2 1.4.8 Fourteen Lattices in Three Dimensions Version: June 6, 2002; Typeset on October 30, 2003,15:28 3 System Type Restrictions Triclinic P a =6 b =6 c, α =6 β =6 γ Monoclinic P,C a =6 b =6 c, α = γ = 90◦ =6 β Orthorhmobic P,C,I,F a =6 b =6 c, α = β = γ = 90◦ Tetragonal P,I a = b =6 c, α = β = γ = 90◦ Cubic P,I,F1 a = b = c, α = β = γ = 90◦ Trigonal P a = b = c, α = β = γ < 120◦, =6 90◦ Hexagonal P a = b =6 c, α = β = 90◦, γ = 120◦ No need to learn details except for cubic, basic ideas of hexagonal. Version: June 6, 2002; Typeset on October 30, 2003,15:28 4 1.4.9 Cubic Unit Cells Primitive Unit Cells of cubic system Simple cubic: cube containing one lattice point (or 8 corner points each shared among 8 cubes: 8 × 1 8 = 1). Body centred cubic: 2 points in cubic cell Version: June 6, 2002; Typeset on October 30, 2003,15:28 5 Rhombohedral primitive cell of body centred cubic system. Face centred cubic: 4 points in cubic cell (8 corner points shared 8 1 1 ways, 6 face points shared 2 ways: 8 × 8 + 6 × 2 = 4. Version: June 6, 2002; Typeset on October 30, 2003,15:28 6 Rhombohedral primitive cell of face centred cubic system.
    [Show full text]