B. Grobéty. Mineralogy and Cristallography Mineralogy: study of naturally occuring crystalline solids = minerals Cristallography: study of crystalline.

Slides:



Advertisements
Similar presentations
Chapter 12 Additional Analytical Methods. Analytical Methods Technique Type Technique application Subdivisions Specific application DescriptionDestruction.
Advertisements

Acero 2000 PHYSICAL METALLURGY AND THERMAL PROCESSING OF STEEL
Solid-State Microstructures
TEM in geological science polymorphism, polytypism, polysomatism F. Nieto Dto. de Mineralogía y Petrología Instituto Ándaluz de Ciencias de la Tierra Universidad.
Ductile deformational processes
What is diffraction? Diffraction – the spreading out of waves as they encounter a barrier.
Minerals. Essential Points 1.Chemical elements form in stars 2.Atoms bond by sharing electrons 3.Minerals are classified by their chemistry 4.Minerals.
Chapter 2.2. Definition of a Mineral  Naturally occurring- which means minerals are not a man-made substance.  Solid at normal temps on the Earth’s.
©2010 John Wiley & Sons, Inc. M P Groover, Principles of Modern Manufacturing 4/e SI Version THE NATURE OF MATERIALS 1.Atomic Structure and the Elements.
Yat Li Department of Chemistry & Biochemistry University of California, Santa Cruz CHEM 146C_Experiment #3 Identification of Crystal Structures by Powder.
Crystals and Symmetry. Why Is Symmetry Important? Identification of Materials Prediction of Atomic Structure Relation to Physical Properties –Optical.
Minerals Modified from a PowerPoint presentation prepared by J. Crelling, Southern Illinois University.
X-ray Diffraction (XRD) and Forensic Geology X-ray diffraction pattern for goethite X-ray diffractometer (XRD) laboratory.
Earth Materials.
17-plane groups When the three symmetry elements, mirrors, rotation axis and glide planes are shown on the five nets, 17-plane groups are derived.
Mineral assembly Most minerals will deal with ionic bonds between cations and anions (or anionic subunits which are themselves mostly covalent but do.
Crystal Chem  Crystallography Chemistry behind minerals and how they are assembled –Bonding properties and ideas governing how atoms go together –Mineral.
Introduction to Mineralogy Mineralogy is a mixture of: Mineralogy is a mixture of: New concepts – much of it from chemistry and physics with a geologic.
Introduction to Minerals. Earth Materials Mineral: –Naturally occurring –Solid substance –Orderly crystalline structure –Definite chemical composition.
Lecture 8 (10/09/2006) Crystallography Part 1: Symmetry Operations
EARTH MATERIALS 2.07 Professor Peter Doyle
Minerals.
Pamela Burnley, UNLV Wendy Panero, OSU Integrating Mineral Physics into Geoscience Curricula.
Elementary Crystallography for X-ray Diffraction
Minerals Chapter 3 Sec. 1 & 2.
Post-crystallization process Changes in structure and/or composition following crystallization Changes in structure and/or composition following crystallization.
ESS 材料熱力學 3 Units (Thermodynamics of Materials)
Mineral Stability What controls when and where a particular mineral forms? Commonly referred to as “Rock cycle” Rock cycle: Mineralogical changes that.
Chapter 2: Earth Materials
Earth Science Notes MINERALS. Definition of a Mineral A mineral is a naturally occurring, inorganic, homogeneous solid with a definite chemical composition.
MINERALS Chapter 3. Section 1 What is it? 1. Naturally occurring- formed by processes on or outside Earth with NO input from humans 2. Inorganic- Not.
The Changing Earth Chapter Thirteen: Formation of Rocks 13.1 The Composition of Rocks 13.2 Igneous Rocks 13.3 How Rocks Change.
MINERALS!. Earth’s Geosphere Densest part of planet’s materials; solid at surface temperatures; includes rocks and minerals Accounts for ___% of Earth’s.
Earth Science Daily Challenge, 11/12 Minerals crystals can be tiny or very large. What kinds of things might control how big a given crystal grows?
Solid state physics Dr. Abeer Kamal Abd El-Aziz 1.
GEOL 3010 Mineralogy Fall, 2009 Introduction. Logistics Joseph R. Smyth Office: 340 Benson Office Hours Wed-Fri
Earth Science Tarbuck/Lutgens.
Earth Materials Minerals: The Crystalline State Minerals and Mineralogy Mineral Chemistry Atomic Structure of Minerals Minerals as indicators of the environment.
Introduction to Mineralogy Dr. Tark Hamilton Chapter 4: Lecture 11 The Chemical Basis of Minerals (Closest Packing & Valency) Camosun College GEOS 250.
Lecture Outlines Physical Geology, 14/e Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display. Plummer, Carlson &
Rocks and Minerals. Rocks Rocks are any solid mass of mineral or mineral-like matter occurring naturally as part of our planet Types of Rocks 1.Igneous.
Growth II Twinning, defects, and polymorphism Jon Price.
Chapter 4, Section 3 Crystal Chemistry Monday, December 14, 2009 Pages
Chapter 1 Introduction. Content Definition of crystal and mineral Definition of crystal and mineral What is mineralogy? What is mineralogy? Major directions.
قسم الهندسة الميكانيكية Mechanical Engineering Department, King Saud University, P.O. Box 800, Riyadh 11421, Saudi Arabia Department of Mechanical Engineering.
PHY1039 Properties of Matter Crystallography, Lattice Planes, Miller Indices, and X-ray Diffraction (See on-line resource: )
Differentiate between physical and chemical changes and properties.[CHE.4A] October 2014Secondary Science - Chemistry.
AIM: What characteristics are used to identify rocks and what are the three main groups of rocks? OBJ: Given notes and activity sheet SWBAT explain the.
Review of Foldable Notes
EBB 512 – Phase Diagram and Equilibria Lecture 1.
Minerals Geology 101, Fall Mineral Definition: “A naturally-occurring homogenous inorganic solid substance with a definite chemical composition.
Minerals.
CHAPTER 16 Solids and Liquids 16.2 The Microstructure of Solids.
Ductile Deformation Processes Chapter 9 in Van der Pluijm and Marshak.
Unit II Rocks and Minerals. Earth’s Interior Our Earth consists of four main layers.
1 Basic of thermodynamic by Dr. Srimala room 2.07 Albert Einstein.
PHS 460 X-ray crystallography and structural analyses 3 units (3 hrs/week) G.A. Adebayo, Department of Physics, UNAAB, Nigeria.
Crystal Defects Steel spheres:
Petrology and mineralogy
Introduction to Minerals
Minerals Geology 115.
SPS1. Obtain, evaluate, and communicate information from the Periodic Table to explain the relative properties of elements based on patterns of atomic.
Minerals.
Solid state physics Lecturer: Prof. Wu mingzai
THE NATURE OF MATERIALS
Earth’s Materials and Processes-Part 6 Minerals
Minerals.
Crystals and Symmetry.
Mon. April 28 Do Now: Define constructive and destructive.
Crystal Chem  Crystallography
Presentation transcript:

B. Grobéty

Mineralogy and Cristallography Mineralogy: study of naturally occuring crystalline solids = minerals Cristallography: study of crystalline solids Both deal with:- macroscopic geometry (morphology) of crystals - microscopic build up of crystals - chemical properties of crystal - physical properties of crystals Gem quality grossular garnet Polyhedral representation of the garnet structure Optical absorption spectrum of a grossular garnet

References The course will be presented mainly with help of powerpoint presentations, available under Moodle. Textbooks A. Putnis An Introduction to Mineral Sciences Cambridge University Press, 1992 ISBN: C. Klein Mineral Science John Wiley and Sons Ltd, 2002 ISBN: Moodle adress:

Course organisation Teacher: Bernard Grobéty Office No Tel Schedule and location: Lecture: Monday Auditoire 2ème étage

Why is Mineralogy/Crystallography important? - Earth, interior planets: Vol% solid, consisting of minerals - Processes affecting the Earth’s surface and interior depend on the properties of the solid constituents elements used by mankind are extracted from minerals - The properties of minerals (and all other materials) depend, among others, on the microscopic build- up (= crystal structures) of the constituent phases. - Important technologies used by modern society is based on specific poperties of solids: - Information technology: optical properties of ruby, piezoelectric properties of quartz (laser telephone, electronic devices). - Computer: electrical properties of silicium and siliciumdioxide (= quartz) (processsors), magnetic properties of ferrites (memory) - Energy production: radioactive properties of uraniumoxide - Biology:structure and function of biological molecules (proteins, enzymes etc.) are obtained from “solidified” versions of these molecules

Content of part I (WS) 1.Introduction 2.Symmetry - Symmetry in daily life and art - Symmetry operations - Point groups 3. Crystal morphology - Morphology, habitus - Crystal axes - Miller indices - Forms - Zones 4. Stereographic Projection 5. Point groups - Monoclinic point groups - Tetragonal point groups - Cubic point groups 6.Ionic bonds - Atom models - Ionization - Ionic bonding 7.Paulings model - Coordination - Pauling rules - Halite, fluorite and perovskite structures 8. Periodic patterns - Translations, unit cell - Glide mirrors - Plane groups 9. Space groups - Glide mirrors - Screw axes - Space groups - Hermann-Maugin notation - Halite and andalusite structure 10.Energetics of minerals - Enthalpy - Entropy - Gibbs Free energy 11.Point defects and diffusion - Point defects - Diffusion - Solid solutions

12. Analytical methods - Diffraction techniques - Spectroscopic methods - Electronmicroscopy 13. Color of minerals - Color - Crystal field splitting - Color of ruby - Electron transfer 14. Radioactivity - Alpha decay - Spontaneous fission - Metamictization - Fission tracks - Decay law 15. Line and planar defects - Edge and screw dislocation - Line defects and deformation - Twinning - Stacking faults - Antiphase boundaries Content of part II (SS) 16. Polytypism and polysomatism - Phyllosilicate structures - Inosilicate structures - Mica polytypes - Biopyriboles 17. Mineral reactions - Displacive phase transitions - Reconstructive phase transitions - Order - disorder transitions - Exsolution - Heterogeneous reactions

Minerals are the "elementary" components of rocks igneous, polymineralic rock granite marblethin section: marble is made up of calcite crystals thin section: granite is made of different minerals metamorphic, monomineralic rock

Mineralogy/Crystallography: Related Fields Mineralogical/crystallographic information is needed in: PetrographyPetrologyExperimental PetrologySedimentpetrography GeologySedimentologyStratigraphy Paleontology Solid state chemistry, physicsSpectroscopyProtein crystallography Material science: Metallurgy, Ceramics Special fields in Mineralogy: Ore Mineralogy Biomineralogy Mineralsystematics Mineralphysics:Optical Mineralogy Mineral Spectroscopy High pressure and temperature (mineral) physics Technical (Applied) Mineralogy Refractory Materials

Stability Field (T, P, fO 2, pH 2 O, pCO 2, etc.) A Happy Stable Mineral! Chemical composition (what elements are present) Crystal structure (how they are arranged) Phase transformation! (change in structure and/or change in way elements are distributed in structure) Change in physical properties (e.g. change in elastic properties changes speed of seismic waves) Microstructure (records history of phase transformations - use to work out what conditions rock has experienced) Principles of mineral behaviour Physical and chemical properties: mechanincal, optical,electrical etc. behavior