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Solid State Chemistry CHEM-E4155 (5 Cr)
Solid State Chemistry CHEM-E4155 (5 cr) Spring 2019 Antti Karttunen Department of Chemistry and Materials Science Aalto University Course outline • Teacher: Antti Karttunen • Lectures – 16 lectures (Mondays and Tuesdays, 12:15-14:00) – Each lecture includes a set of exercises (a MyCourses Quiz) – We start the exercises together during the lecture (deadline: Sunday 23:59) • Project work – We create content in the Aalto Solid State Chemistry Wiki – Includes both independent and collaborative work (peer review) – Lots of content has been created in the Wiki during 2017-2018. • Grading – Exercises 50% – Project work 50% • Workload (135 h) – Lectures, combined with exercises 32 h – Home problem solving 48 h – Independent project work 55 h 2 Honor code for exercises • The purpose of the exercises is to support your learning • Most of the exercises are graded automatically – Some of the more demaning exercises I will grade manually • It is perfectly OK to discuss the exercises with the other students – In fact, I encourage discussion during the exercise sessions • It is not OK to take answers directly from the other students – This also means that is not OK to give answers directly to the other students • The exercise answers and timestamps are being monitored 3 Mondays: 12.15 – 14.00 Course calendar Tuesdays: 12.15 - 14.00 Week Lect. Date Topic 1: Structure 1 25.2. Structure of crystalline materials. X-ray diffraction. Symmetry. 2 26.2. Structural databases, visualization of crystal structures. 2: Bonding 3 4.3. Bonding in solids. Description of crystal structures. 4 5.3. Band theory. Band structures. 3: Synthesis 5 11.3. -
INTERNATIONAL GEMMOLOGICAL CONFERENCE Nantes - France INTERNATIONAL GEMMOLOGICAL August 2019 CONFERENCE Nantes - France August 2019
IGC 2019 - Nantes IGC 2019 INTERNATIONAL GEMMOLOGICAL CONFERENCE Nantes - France INTERNATIONAL GEMMOLOGICAL August 2019 CONFERENCE Nantes - France www.igc-gemmology.org August 2019 36th IGC 2019 – Nantes, France Introduction 36th International Gemmological Conference IGC August 2019 Nantes, France Dear colleagues of IGC, It is our great pleasure and pride to welcome you to the 36th International Gemmological Conference in Nantes, France. Nantes has progressively gained a reputation in the science of gemmology since Prof. Bernard Lasnier created the Diplôme d’Université de Gemmologie (DUG) in the early 1980s. Several DUGs or PhDs have since made a name for themselves in international gemmology. In addition, the town of Nantes has been on several occasions recognized as a very attractive, green town, with a high quality of life. This regional capital is also an important hub for the industry (e.g. agriculture, aeronautics), education and high-tech. It has only recently developed tourism even if has much to offer, with its historical downtown, the beginning of the Loire river estuary, and the ocean close by. The organizers of 36th International Gemmological Conference wish you a pleasant and rewarding conference Dr. Emmanuel Fritsch, Dr. Nathalie Barreau, Féodor Blumentritt MsC. The organizers of the 36th International Gemmological Conference in Nantes, France From left to right Dr. Emmanuel Fritsch, Dr. Nathalie Barreau, Féodor Blumentritt MsC. 3 36th IGC 2019 – Nantes, France Introduction Organization of the 36th International Gemmological Conference Organizing Committee Dr. Emmanuel Fritsch (University of Nantes) Dr. Nathalie Barreau (IMN-CNRS) Feodor Blumentritt Dr. Jayshree Panjikar (IGC Executive Secretary) IGC Executive Committee Excursions Sophie Joubert, Richou, Cholet Hervé Renoux, Richou, Cholet Guest Programme Sophie Joubert, Richou, Cholet Homepage Dr. -
Properties of Minerals for Processing
2 C h a p t e r Properties of Minerals for Processing 2.1 SAMPLING Sampling is a process of obtaining a small portion from a large quantity of a similar material such that, it truly represents the composition of the whole lot. It is an important step before testing of any material in the laboratory. Sampling of homogeneous materials is easy as compared to heterogeneous materials and hence, has to be conducted carefully. It is so because unlike heterogeneous materials, homogeneous materials have a uniform composition. However, almost all metallurgical materials are heterogeneous in nature. 2.1.1 Sampling of Ores/Minerals The process of sampling is complicated because of the following reasons: (1) A large variety of constituents are present in ores and minerals. (2) There is a large variation in the distribution of these constituents throughout the material. (3) In many cases, weight of the sample may vary from, 0.5 to 5 gm or 10 gm. Small fraction from large quantity like 50 to 250 tonnes are not true representative of the entire lot. The size of the sample required for testing depends on the method of testing and the testing machine which is used. However, sampling may involve three operations, namely, crushing and/or grinding, mixing and finally cutting. These operations may be executed repeatedly wherein the quantity of sample can be reduced to a desired weight. Sampling should be based on the relation between maximum particle size and the amount of sample. The size of ore/mineral particles taken for sampling depends on uniformity of composition, i.e., if the composition is more uniform, smaller particle size of the sample is taken and vice versa. -
Crystal Structure-Crystalline and Non-Crystalline Materials
ASSIGNMENT PRESENTED BY :- SOLOMON JOHN TIRKEY 2020UGCS002 MOHIT RAJ 2020UGCS062 RADHA KUMARI 2020UGCS092 PALLAVI PUSHPAM 2020UGCS122 SUBMITTED TO:- DR. RANJITH PRASAD CRYSTAL STRUCTURE CRYSTALLINE AND NON-CRYSTALLINE MATERIALS . Introduction We see a lot of materials around us on the earth. If we study them , we found few of them having regularity in their structure . These types of materials are crystalline materials or solids. A crystalline material is one in which the atoms are situated in a repeating or periodic array over large atomic distances; that is, long-range order exists, such that upon solidification, the atoms will position themselves in a repetitive three-dimensional pattern, in which each atom is bonded to its nearest-neighbor atoms. X-ray diffraction photograph [or Laue photograph for a single crystal of magnesium. Crystalline solids have well-defined edges and faces, diffract x-rays, and tend to have sharp melting points. What is meant by Crystallography and why to study the structure of crystalline solids? Crystallography is the experimental science of determining the arrangement of atoms in the crystalline solids. The properties of some materials are directly related to their crystal structures. For example, pure and undeformed magnesium and beryllium, having one crystal structure, are much more brittle (i.e., fracture at lower degrees of deformation) than pure and undeformed metals such as gold and silver that have yet another crystal structure. Furthermore, significant property differences exist between crystalline and non-crystalline materials having the same composition. For example, non-crystalline ceramics and polymers normally are optically transparent; the same materials in crystalline (or semi-crystalline) forms tend to be opaque or, at best, translucent. -
A Web-Based Crystallographic Tool for the Construction of Nanoparticles
NATIONAL AND KAPODISTRIAN UNIVERSITY OF ATHENS SCHOOL OF SCIENCE DEPARTMENT OF INFORMATICS AND TELECOMMUNICATION INTERDISCIPLINARY POSTGRADUATE PROGRAM "INFORMATION TECHNOLOGIES IN MEDICINE AND BIOLOGY" MASTER THESIS A web-based crystallographic tool for the construction of nanoparticles Alexios T. Chatzigoulas Supervisor: Dr. Zoe Cournia, Researcher - Assistant Professor Level, Biomedical Research Foundation of the Academy of Athens (BRFAA) ATHENS FEBRUARY 2018 ΔΘΝΗΚΟ ΚΑΗ ΚΑΠΟΓΗΣΡΗΑΚΟ ΠΑΝΔΠΗΣΖΜΗΟ ΑΘΖΝΩΝ ΥΟΛΖ ΘΔΣΗΚΩΝ ΔΠΗΣΖΜΩΝ ΣΜΖΜΑ ΠΛΖΡΟΦΟΡΗΚΖ ΚΑΗ ΣΖΛΔΠΗΚΟΗΝΩΝΗΩΝ ΓΗΑΣΜΖΜΑΣΗΚΟ ΜΔΣΑΠΣΤΥΗΑΚΟ ΠΡΟΓΡΑΜΜΑ "ΣΔΥΝΟΛΟΓΗΔ ΠΛΖΡΟΦΟΡΗΚΖ ΣΖΝ ΗΑΣΡΗΚΖ ΚΑΗ ΣΖ ΒΗΟΛΟΓΗΑ" ΓΗΠΛΧΜΑΣΗΚΖ ΔΡΓΑΗΑ Ένα διαδικηςακό κπςζηαλλογπαθικό επγαλείο για ηεν καηαζηεςή νανοζωμαηιδίων Αλέξιορ Θ. Υαηδεγούλαρ Δπιβλέποςζα: Γπ. Εωή Κούπνια, Δξεπλήηξηα Γ‟, Ίδξπκα Ιαηξνβηνινγηθώλ Δξεπλώλ Αθαδεκίαο Αζελώλ (ΙΙΒΔΑΑ) ΑΘΖΝΑ ΦΔΒΡΟΤΑΡΗΟ 2018 MASTER THESIS A web-based crystallographic tool for the construction of nanoparticles Alexios T. Chatzigoulas S.N.: PIV0155 SUPERVISOR: Dr. Zoe Cournia, Researcher - Assistant Professor Level, Biomedical Research Foundation of the Academy of Athens (BRFAA) EXAMINATION Dr. Zoe Cournia, Researcher - Assistant Professor Level, COMMITTEE: Biomedical Research Foundation of the Academy of Athens (BRFAA) Dr. Ioannis Emiris, Professor Level, National and Kapodistrian University of Athens (NKUA), Department of Informatics and Telecommunications (DIT) Dr. Evangelia Chrysina, Senior Researcher at the Institute of Biology, Medicinal Chemistry and Biotechnology, -
Symmetry-Operations, Point Groups, Space Groups and Crystal Structure
1 Symmetry-operations, point groups, space groups and crystal structure KJ/MV 210 Helmer Fjellvåg, Department of Chemistry, University of Oslo 1994 This compendium replaces chapter 5.3 and 6 in West. Sections not part of the curriculum are enclosed in asterisks (*). It is recommended that the textbooks of West and Jastrzebski are used as supplementary reading material, with special emphasis on illustrative examples. In this compendium illustrative examples (in italics) have been chosen from close packed structures. A few symbols and synonyms are given in Norwegian as information. The compendium contains exercises which will not be explained in the classes. It is recommended to work through the exercises while reading this compendium. Introduction. Condensed phases may be liquids as well as solids. There are fundamental differences between liquids and solids regarding the long-range distribution of atoms. While liquids have long range disorder in a large scale, solids are mainly ordered, i.e. there is regularity in the repetition of structural fragments (atoms and/or groups of atoms) in the 3 dimensional material. Surfaces of solid materials are often somewhat differently organized than the “bulk” (i.e. the inner part of the material). The atomic (structural) arrangement near the surface will often be different from the bulk arrangement due to surface reconstruction in order to minimize the energy loss associated with complete chemical bonding in all actual directions. Liquids are disordered in bulk, but they often have an ordered surface structure. Solids do not need to display systematic long-range order, i.e. to be crystalline. Some phases can be prepared as amorphous materials, e.g. -
Characterization of the Volcanic Rocks of Mount Sinabung, Simacem Village, Karo Regency, Conducted with XRD, SEM-EDX
Journal of Technomaterial Physics Vol. 1, No. 1, 2019 | 1 – 5 JoTP Journal of Technomaterial Physics Characterization of the Volcanic Rocks of Mount Sinabung, Simacem Village, Karo Regency, Conducted With XRD, SEM-EDX Perdinan Sinuhaji1, Awan Maghfirah2 and Sahat M. Nababan3 1,2,3 Department of Physics, Faculty of Mathematics and Natural Science, Universitas Sumatera Utara 20155, Indonesia Abstract. The study of volcanic rocks characterization of Sinabung Volcano erupted on September 15, 2017. The volcanic rocks crystal system was performed with XRD, elemental analysis and microstructure with SEM-EDX. Volcanic rocks contain: Anorthite phase 87,11 (wt%), Triclinic crystal, lattice constant, a = 8.1742 Å, b = 12.844 Å, c = 14.204 Å; Quartz phase 2.26%, Hexagonal crystals, lattice constants, a = 4.799 Å, b = 4.799 Å, c = 5.379 Å; Cristobalite phase 7.72 (wt%), Tetragonal crystals, lattice constants a = 4.970 Å, b = 6.990 Å, c = 6.998 Å; Alunite phase 2.91 (wt%), Hexagonal crystals, lattice constants, a = 6.990 Å, b = 6.990 Å, c = 17.282 Å. Keyword: Volcanic rock, Crystal Structure, Phase, Microstructure Received 1 December 2018 | Revised [3 January 2019] | Accepted [28 February 2019] 1 Introduction Mount Sinabung’s activity aroused after its 400-year slumber. The activity was firstly noticed on August 27th, 2010. Hot clouds, lava, volcanic dust, sand and volcanic rocks were seen bursting out from the bowels of the mountain. Volcanic dust was bursting high and far, reaching tens of kilometers along with sand and volcanic rocks to residential areas. The adverse impacts inflicted to the residents were including the agricultural damage, water pollution, health problems and flight disruption [1]. -
Thermophysical Properties of Kaolin–Zeolite Blends up to 1100 C
crystals Article Thermophysical Properties of Kaolin–Zeolite Blends up to 1100 ◦C Ján Ondruška 1, Tomáš Húlan 1, Ivana Sunitrová 1, Štefan Csáki 2, Grzegorz Łagód 3 , Alena Struhárová 4 and Anton Trník 1,5,* 1 Department of Physics, Faculty of Natural Sciences, Constantine the Philosopher University in Nitra, Tr. A. Hlinku 1, 94974 Nitra, Slovakia; [email protected] (J.O.); [email protected] (T.H.); [email protected] (I.S.) 2 Institute of Plasma Physics, Czech Academy of Sciences, Za Slovankou 3, 18200 Prague, Czech Republic; [email protected] 3 Faculty of Environmental Engineering, Lublin University of Technology, Nadbystrzycka 40B, 20-618 Lublin, Poland; [email protected] 4 Department of Materials Engineering and Physics, Faculty of Civil Engineering, Slovak University of Technology, Radlinskeho 11, 81005 Bratislava, Slovakia; [email protected] 5 Department of Materials Engineering and Chemistry, Faculty of Civil Engineering, Czech Technical University in Prague, Thákurova 7, 16629 Prague, Czech Republic * Correspondence: [email protected]; Tel.: +421-37-6408-616 Abstract: In this study, the thermophysical properties such as the thermal expansion, thermal diffusivity and conductivity, and specific heat capacity of ceramic samples made from kaolin and natural zeolite are investigated up to 1100 ◦C. The samples were prepared from Sedlec kaolin (Czech Republic) and natural zeolite (Nižný Hrabovec, Slovakia). Kaolin was partially replaced with a natural zeolite in the amounts of 10, 20, 30, 40, and 50 mass%. The measurements were performed on cylindrical samples using thermogravimetric analysis, a horizontal pushrod dilatometer, and laser flash apparatus. The results show that zeolite in the samples decreases the values of all studied Citation: Ondruška, J.; Húlan, T.; Sunitrová, I.; Csáki, Š.; Łagód, G.; properties (except thermal expansion), which is positive for bulk density, porosity, thermal diffusivity, Struhárová, A.; Trník, A. -
Raman Evidence for Pressure-Induced Formation of Diamondene
Raman evidence for pressure-induced formation of diamondene The MIT Faculty has made this article openly available. Please share how this access benefits you. Your story matters. Citation Martins, Luiz Gustavo Pimenta et al. “Raman Evidence for Pressure- Induced Formation of Diamondene.” Nature Communications 8, 1 (July 2017) © 2017 The Author(s) As Published http://dx.doi.org/10.1038/S41467-017-00149-8 Publisher Nature Publishing Group Version Final published version Citable link http://hdl.handle.net/1721.1/113640 Terms of Use Creative Commons Attribution 4.0 International License Detailed Terms https://creativecommons.org/licenses/by/4.0/ ARTICLE DOI: 10.1038/s41467-017-00149-8 OPEN Raman evidence for pressure-induced formation of diamondene Luiz Gustavo Pimenta Martins1,7, Matheus J.S. Matos 2, Alexandre R. Paschoal3, Paulo T.C. Freire3, Nadia F. Andrade4, Acrísio L. Aguiar5, Jing Kong6, Bernardo R.A. Neves 1, Alan B. de Oliveira2, Mário S.C. Mazzoni1, Antonio G. Souza Filho3 & Luiz Gustavo Cançado1 Despite the advanced stage of diamond thin-film technology, with applications ranging from superconductivity to biosensing, the realization of a stable and atomically thick two-dimensional diamond material, named here as diamondene, is still forthcoming. Adding to the outstanding properties of its bulk and thin-film counterparts, diamondene is predicted to be a ferromagnetic semiconductor with spin polarized bands. Here, we provide spectro- scopic evidence for the formation of diamondene by performing Raman spectroscopy of double-layer graphene under high pressure. The results are explained in terms of a break- down in the Kohn anomaly associated with the finite size of the remaining graphene sites surrounded by the diamondene matrix. -
Crystal Physics and X Ray Diffraction
CRYSTAL PHYSICS AND X RAY DIFFRACTION US03CPHY22 UNIT - 3 CRYSTAL PHYSICS AND X – RAY DIFFRACTION INTRODUCTION A crystal is a solid composed of atoms or other microscopic particles arranged in an orderly periodic array in three dimensions. It may not be a complete definition, yet it is a true description. The three general types of solids: amorphous, polycrystalline and single crystal are distinguished by the size of ordered regions within the materials. Order in amorphous solids is limited to a few molecular distances. In polycrystalline materials, the solid is made-up of grains which are highly ordered crystalline regions of irregular size and orientation. Single crystals have long-range order. Many important properties of materials are found to depend on the structure of crystals and on the electron states within the crystals. The study of crystal physics aims to interpret the macroscopic properties in terms of properties of the microscopic particles of which the solid is composed. The study of the geometric form and other physical properties of crystalline solids by using x-rays, electron beams and neutron beams constitute the science of crystallography or crystal physics. LATTICE POINTS AND SPACE LATTICE The atomic arrangement in a crystal is called crystal structure. In perfect crystal, there is a regular arrangement of atoms. This periodicity in the arrangement generally varies in different directions. It is very convenient to imagine points in space about which these atoms are located. Such points in space are called lattice points and the totality of such points forms a crystal lattice or space lattice. If all the atoms at the lattice points are identical, the lattice is called a “Bravais lattice”. -
Powder Diffraction Structure Determination and Refinement from Powder Diffraction Data
Berichte aus Arbeitskreisen der DGK Nr. 9 VII. Workshop Powder Diffraction Structure Determination and Refinement from Powder Diffraction Data Robert E. Dinnebier (ed.) Deutsche Gesellschaft für Kristallographie 2000 - ii - Acknowledgement The VII international workshop on powder diffraction, October 4. – 8, 2000 at the Laboratory of Crystallography of the University of Bayreuth (Germany) was organized by the Powder Diffraction Group of the German Society of Crystallogra- phy DGK. We are grateful to the Universität Bayreuth for supplying technical assistance, lecture halls and PC pools free of charge. We are further grateful for financial support from - Deutsche Gesellschaft für Kristallographie (DGK) - Deutsche Mineralogische Gesellschaft (DMG) - International Union of Crystallography (IUCr) - International Centre for Diffraxction Data (ICDD) - Clariant GmbH, Frankfurt - Stoe & Cie, Darmstadt - Bruker AXS, Karlsruhe - Cambridge Crystallographic Data Centre (CCDC), Cambridge - Molecular Simulation Inc. (MSI), Cambridge - Böhringer Ingelheim, Biberach a.d. Riss - Crystal Impact, Bonn - BASF AG, Ludwigshafen - Philips Analytical, Almelo Due to the generous support, it was possible to keep registration costs for this workshop low and to award 15 travel grants to students to cover all local costs at Bayreuth as well as part of their travel costs. - iii - - iv - Preface The complexity of crystal structures which can be solved and/or refined from powder diffraction data has been increasing steadily throughout the last few years. In particular further developments of “traditional” algorithms for structure determination in reciprocal space as well as the application of global optimiza- tion algorithms in direct space have reached a level which for the first time al- lows powder diffraction to be used as an alternative technique to single crystal diffraction for inorganic and small molecule structures. -
Chapter 2: Minerals
503-S1-MSS05_G7NA 8/16/04 2:18 PM Page 28 Minerals Nature’s Beautiful Creation sections Although cut by gemologists to enhance 1 Minerals Lab Crystal Formation their beauty, these gorgeous diamonds formed naturally—deep within Earth. One 2 Mineral Identification requirement for a substance to be a mineral 3 Uses of Minerals is that it must occur in nature. Human- Lab Mineral Identification made diamonds serve their purpose in Virtual Lab How can industry but are not considered minerals. minerals be defined by Science Journal Write two questions you would ask their properties? a gemologist about the minerals that he or she works with. SuperStock 503-S1-MSS05_G7NA 8/16/04 2:18 PM Page 29 Start-Up Activities Minerals Make the following Foldable to help you better understand minerals. Distinguish Rocks from Minerals When examining rocks, you’ll notice that STEP 1 Fold a vertical many of them are made of more than one sheet of note- material. Some rocks are made of many dif- book paper from side to side. ferent crystals of mostly the same mineral. A mineral, however, will appear more like a pure substance and will tend to look the STEP 2 Cut along every third line of only the same throughout. Can you tell a rock from a top layer to form tabs. mineral? 1. Use a magnifying lens to observe a quartz crystal, salt grains, and samples of sandstone, granite, calcite, mica, and schist (SHIHST). STEP 3 Label each tab with a question. 2. Draw a sketch of each sample. 3.