The Element Six Cvd Diamond Handbook
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Graphene – Diamond Nanomaterials: a Status Quo Review
Preprints (www.preprints.org) | NOT PEER-REVIEWED | Posted: 29 July 2021 doi:10.20944/preprints202107.0647.v1 Article Graphene – diamond nanomaterials: a status quo review 1 Jana Vejpravová ,* 1 Department of Condensed Matter Physics, Faculty of Mathematics and Physics, Charles University, Ke Karlovu 5, 121 16 Prague 2, Czech Republic. * Correspondence: JV, [email protected] Abstract: Carbon nanomaterials with a different character of the chemical bond – graphene (sp2) and nanodiamond (sp3) are the building bricks for a new class of all-carbon hybrid nanomaterials, where the two different carbon networks with the sp3 and sp2 hybridization coexist, interact and even transform into one another. The unique electronic, mechanical, and chemical properties of the two border nanoallotropes of carbon ensure the immense application potential and versatility of these all-carbon graphene – diamond nanomaterials. The review gives an overview of the current state of the art of graphene – diamond nanomaterials, including their composites, heterojunctions, and other hybrids for sensing, electronic, energy storage, and other applications. Also, the graphene- to-diamond and diamond-to-graphene transformations at the nanoscale, essential for innovative fabrication, and stability and chemical reactivity assessment are discussed based on extensive theo- retical, computational, and experimental studies. Keywords: graphene; diamond; nanodiamond; diamane; graphene-diamond nanomaterials; all car- bon materials; electrochemistry; mechanochemistry; sensor; supercapacitor; -
Symposium on Agate and Cryptocrystalline Quartz
Symposium on Agate and Cryptocrystalline Quartz September 10 – 13, 2005 Golden, Colorado Sponsored by Friends of Mineralogy, Colorado Chapter; Colorado School of Mines Geology Museum; and U.S. Geological Survey 2 Cover Photos {top left} Fortification agate, Hinsdale County, Colorado, collection of the Geology Museum, Colorado School of Mines. Coloration of alternating concentric bands is due to infiltration of Fe with groundwater into the porous chalcedony layers, leaving the impermeable chalcedony bands uncolored (white): ground water was introduced via the symmetric fractures, evidenced by darker brown hues along the orthogonal lines. Specimen about 4 inches across; photo Dan Kile. {lower left} Photomicrograph showing, in crossed-polarized light, a rhyolite thunder egg shell (lower left) a fibrous phase of silica, opal-CTLS (appearing as a layer of tan fibers bordering the rhyolite cavity wall), and spherulitic and radiating fibrous forms of chalcedony. Field of view approximately 4.8 mm high; photo Dan Kile. {center right} Photomicrograph of the same field of view, but with a 1 λ (first-order red) waveplate inserted to illustrate the length-fast nature of the chalcedony (yellow-orange) and the length-slow character of the opal CTLS (blue). Field of view about 4.8 mm high; photo Dan Kile. Copyright of articles and photographs is retained by authors and Friends of Mineralogy, Colorado Chapter; reproduction by electronic or other means without permission is prohibited 3 Symposium on Agate and Cryptocrystalline Quartz Program and Abstracts September 10 – 13, 2005 Editors Daniel Kile Thomas Michalski Peter Modreski Held at Green Center, Colorado School of Mines Golden, Colorado Sponsored by Friends of Mineralogy, Colorado Chapter Colorado School of Mines Geology Museum U.S. -
Compilation of Reported Sapphire Occurrences in Montana
Report of Investigation 23 Compilation of Reported Sapphire Occurrences in Montana Richard B. Berg 2015 Cover photo by Richard Berg. Sapphires (very pale green and colorless) concentrated by panning. The small red grains are garnets, commonly found with sapphires in western Montana, and the black sand is mainly magnetite. Compilation of Reported Sapphire Occurrences, RI 23 Compilation of Reported Sapphire Occurrences in Montana Richard B. Berg Montana Bureau of Mines and Geology MBMG Report of Investigation 23 2015 i Compilation of Reported Sapphire Occurrences, RI 23 TABLE OF CONTENTS Introduction ............................................................................................................................1 Descriptions of Occurrences ..................................................................................................7 Selected Bibliography of Articles on Montana Sapphires ................................................... 75 General Montana ............................................................................................................75 Yogo ................................................................................................................................ 75 Southwestern Montana Alluvial Deposits........................................................................ 76 Specifi cally Rock Creek sapphire district ........................................................................ 76 Specifi cally Dry Cottonwood Creek deposit and the Butte area .................................... -
X-Ray Topographic Investigation of Diamond Anvils for High Pressure Generation - Correlation Between Defects and Early Failure
X-ray topographic investigation of diamond anvils for high pressure generation - Correlation between defects and early failure Dewaele A. and Loubeyre P. CEA/DPTA, BP12, 91680 Bruyères le Châtel The diamond anvil cell technique revolutionized high pressure physics some 25 years ago. This device takes advantage of the unusual mechanical properties of the diamond. A metallic gasket with a hole in it to confine the sample is compressed between two diamond anvils. This device allows the generation of pressures that reach 300 GPa (3 millions times atmospheric pressure), pressure at which the diamond exhibits large elastic strain [1]. The pressure reached in diamond anvil cells is very often limited by the failure of a diamond anvil. In order to prevent this phenomenon, anvils are selected on the basis of their chemical purity, and their internal strains. However, the chemical purity does not guarantee the resistance of diamond anvils under high pressure operation. In particular, when the diamonds are used in contact with H2 or Helium samples, species which diffuse in diamond. Unfortunately, helium is known to be the best pressure transmitting medium, and is often loaded for that use in diamonds anvil cells [2]. A better understanding of early breakdown of diamond anvils and an a priori diagnostic of their resistance would thus constitute a major improvement for high pressure techniques. X-ray topography helps to establish this anvils quality diagnostic, because this method evidences intrinsic crystallographic defects of the anvils. These defects are likely to influence the mechanical properties of the anvil [3]. However, the liability of x-ray topography diagnostic had to be proven. -
Ecological Comparison of Synthetic Versus Mined Diamonds
Ecological Comparison of Synthetic versus Mined Diamonds Saleem H. Ali Working Paper, Institute for Environmental Diplomacy and Security University of Vermont, January, 2011 http://www.uvm.edu/ieds Abstract The energy usage and emissions in mined versus lab-created diamonds was evaluated, based on industrial data, since these two factors are often a general indicator of environmental impact that can be useful in product comparisons. Depending on the process and the location of the mine, the data can be highly divergent and cannot be used as a singular measure of environmental impact. There is a need to develop life cycle analysis techniques from industrial ecology to conduct a detailed comparison of synthetic versus mined stones. Introduction Synthetic diamonds have come of age, and the year 2010 will be remembered as a landmark year in this regard since for the first time labs of the Gemological Institute of America (GIA) in New York were able to grade a gem quality near-colorless synthetic diamond (formed by chemical vapor deposition) , greater than 1 carat. The history of synthetic diamonds at the industrial level, goes back to patents for super-abrasives at General Electric can be traced back to several decades (Hazen, 1996). However, gem quality synthetic diamonds have only risen to prominence in the last decade with the rise of a few key companies who are taking on this growing market in concert with boutique jewelry brands. As jewelers consider environmental social responsibility more seriously in marketing their gemstone products, energy usage in mined versus lab-created gems can be an important factor in determining comparative environmental impact. -
OF SYNTHETIC DIAMONDS. Introduction
PI ^ AU9817130 IONOLUMINESCENCE (IL) OF SYNTHETIC DIAMONDS. A. A. Bettiol, K. W. Nugent, D. N. Jamieson and S. Prawer School of Physics, Microanalytical Research Centre, University of Melbourne, Parkville, 3052, AUSTRALIA. Introduction The optical properties of natural and synthetic diamonds have been extensively characterized in the past by absorption and luminescence. The use of such techniques as cathodoluminescence, photoluminescence, photoluminescence excitation and electron spin and paramagnetic resonance has resulted in the identification of many impurity and defect related optical centres in diamond [1-2]. Of the impurities found in diamond, nitrogen is by far the most abundant and hence responsible for most of the optical properties [3]. The development of diamond synthesis methods has resulted in the discovery of a number of a new optically active impurities and defects which are introduced during the growth process. These include Si, O, Ni and B [1-2]. In this study we identify a number of defect and impurity related centres in two commercially produced synthetic diamond samples by using the novel technique of ionoluminescence (IL) [4]. The first sample characterized is a Norton polycrystalline diamond detector. Signal produced in any charged particle detector is degraded if recombination of the electrons and holes occurs before the charge can be swept out by the electric field in the detector. In diamonds where the radiative recombination cross-section can be quite high, signal degradation can occur depending on the optical centres present and their lifetimes. Recombination centres with lifetimes much longer than the sweep out time will potentially saturate hence only cause a degradation of signal. -
DIAMOND Natural Colorless Type Iab Diamond with Silicon-Vacancy
Editors Thomas M. Moses | Shane F. McClure DIAMOND logical and spectroscopic features con- Natural Colorless Type IaB firmed the diamond’s natural origin, – Diamond with Silicon-Vacancy despite the occurrence of [Si-V] emis- Defect Center sions. No treatment was detected. Examination of this stone indicated The silicon-vacancy defect, or [Si-V]–, that the [Si-V]– defect can occur, albeit is one of the most important features rarely, in multiple types of natural dia- in identifying CVD synthetic dia- monds. Therefore, all properties should monds. It can be effectively detected be carefully examined in reaching a using laser photoluminescence tech- conclusion when [Si-V]– is present. nology to reveal sharp doublet emis- sions at 736.6 and 736.9 nm. This Carmen “Wai Kar” Lo defect is extremely rare in natural dia- monds (C.M. Breeding and W. Wang, “Occurrence of the Si-V defect center Figure 1. Emissions from the Screening of Small Yellow Melee for in natural colorless gem diamonds,” silicon-vacancy defect at 736.6 and Treatment and Synthetics Diamond and Related Materials, Vol. 736.9 nm were detected in this Diamond treatment and synthesis 17, No. 7–10, pp. 1335–1344) and has 0.40 ct type IaB natural diamond. have undergone significant develop- been detected in very few natural type ments in the last decade. During this IIa and IaAB diamonds over the past showed blue fluorescence with natural time, the trade has grown increasingly several years. diamond growth patterns. These gemo- concerned about the mixing of treated Recently, a 0.40 ct round brilliant diamond with D color and VS2 clarity (figure 1) was submitted to the Hong Figure 2. -
On Palaeozoic–Mesozoic Brittle Normal Faults Along the SW Barents Sea Margin: Fault Processes and Implications for Basement Permeability and Margin Evolution
research-articleResearch ArticleXXX10.1144/jgs2014-018K. Indrevær et al.Brittle Faults on the SW Barents Sea Margin 2014 Downloaded from http://jgs.lyellcollection.org/ by guest on October 9, 2021 Journal of the Geological Society, London. http://dx.doi.org/10.1144/jgs2014-018 Published Online First © 2014 The Authors On Palaeozoic–Mesozoic brittle normal faults along the SW Barents Sea margin: fault processes and implications for basement permeability and margin evolution KJETIL INDREVÆR1,2*, HOLGER STUNITZ1 & STEFFEN G. BERGH1 1Department of Geology, University of Tromsø, N-9037 Tromsø, Norway 2DONG E&P Norge AS, Roald Amundsens Plass 1, N-9257 Tromsø, Norway *Corresponding author (e-mail: [email protected]) Abstract: Palaeozoic–Mesozoic brittle normal faults onshore along the SW Barents Sea passive margin off northern Norway give valuable insight into fault and fluid flow processes from the lower brittle crust. Micro- structural evidence suggests that Late Permian–Early Triassic faulting took place during multiple phases, with initial fault movement at minimum P–T conditions of c. 300 °C and c. 240 MPa (c. 10 km depth), followed by later fault movement at minimum P–T conditions of c. 275 °C and c. 220 MPa (c. 8.5 km depth). The study shows that pore pressures locally reached lithostatic levels (240 MPa) during faulting and that faulting came to a halt during early (deep) stages of rifting along the margin. Fault permeability has been controlled by heal- ing and precipitation processes through time, which have sealed off the core zone and eventually the damage zones after faulting. A minimum average exhumation rate of c. -
De Beers Natural Versus Synthetic Diamond Verification Instruments
DE BEERSNATURAL VERSUS By Christopher M.Welbourn, Martin Cooper, and Paul M,Spear Twoinstruments have been developed at he subject of cuttable-quality synthetic diamonds De Beers DTC Research Centre, has been receiving much attention in the gem trade Maidenhead, to distinguish synthetic dia- recently. Yellow to yellow-brown synthetic diamonds grown monds from natural diamonds. The in Russia have been offered for sde at a number of recent DiainondSureTMenables the rapid exami- gem and jewelry trade shows (Shor and Weldon, 1996; nation of large numbers of polished dia- monds, both loose and set in jewehy. Reinitz, 1996; Johnson and Koivula, 1996))and a small num- Automatically and with high sensitivity, ber of synthetic diamonds have been submitted to gem grad- this instrument detects the presence of the ing laboratories for identification reports (Fryer, 1987; 415 nm optical absorption line, which is Reinitz, 1996; Moses et al., 1993a and b; Emms, 1994; found in the vast majority of natural dia- Kammerling et al., 1993, 1995; Kammerling and McClure, monds but not in synthetic diamonds. 1995). Particular concern was expressed following recent Those stones in which this line is detected announcements of the production and planned marketing of are "passed" by the instrument, and those near-colorless synthetic diamonds (Koivula et al., 1994; in which it is not detected are "referredfor "Upfront," 1995). further tests." The DiamondViewTRfpro- Synthetic diamonds of cuttable size and quality, and the duces a fluorescence image of the surface of technology to produce them, are not new. In 1971, researchers a polished diamond, from which the growth structure of the stone may be deter- at the General Electric Company published the results of mined. -
Non-Stoichiometric Magnesium Aluminate Spinel
NON-STOICHIOMETRIC MAGNESIUM ALUMINATE SPINEL: MICROSTRUCTURE EVOLUTION AND ITS EFFECT ON PROPERTIES by J. Aaron Miller A thesis submitted to the Faculty and the Board of Trustees of the Colorado School of Mines in partial fulfillment of the requirements for the degree of Doctor of Philosophy (Materials Science). Golden, Colorado Date _________________________ Signed: __________________________________ J. Aaron Miller Signed: __________________________________ Ivar E. Reimanis Thesis Advisor Golden, Colorado Date _________________________ Signed: _________________________ Dr. Angus Rockett Professor and Head Department of Metallurgical and Materials Engineering ii ABSTRACT Magnesium aluminate spinel is a material of interest for transparent armor applications. Owing to its unique combination of transparency to large portions of the electromagnetic spectrum and mechanical robustness, spinel is among the front runners for applications including transparent armor windows for military vehicles and space craft windows, missile radomes, and infrared windows. However, failure in such applications may lead to severe outcomes, creating motivation to further improve the mechanical reliability of the materials used. In this thesis, potential toughening mechanisms that utilize unique control over the evolution of second phase particles are explored. Al-rich spinel (MgO•nAl2O3) with a composition of n = 2 is investigated. First, it is demonstrated that precipitation of second phase Al2O3 from single phase spinel can be achieved by modifying the densification -
Large Man-Made Diamond Single Crystals: Manufacture, Properties and Application
Large man-made diamond single crystals: manufacture, properties and application Dr. Sergey A.Terentjev , the head of Department of Single Crystal Growth. Technological Institute for Superhard and Novel Carbon Materials ( ТISN СМ ) E-mail: Diamond is a material possessing a unique complex of physical and chemical properties which potentially allow using it, besides traditional application in the processing industry, in Hi- Tech branches also. Such use of diamond restrains by insufficient quantity of natural perfect raw material of so-called "device" quality. Single crystals of diamond grown up in laboratory conditions differ from natural, first of all, in high reproducibility of physical properties (impurities level, an optical transparency, heat conductivity, specific electric resistance, etc.). Creation of technologies for cultivation a high purity «nitrogen free» (IIa type) and semi- conductor (IIb type) large diamond single crystals, which are extremely rare among natural diamonds and very expensive, is of the great interest and simultaneously of the greatest difficulty. Technologies for manufacture of both IIa and IIb diamond single crystals 0.5 to 5.0 carat in weight (characteristic size 3÷8 mm) from solvent/catalyst melt of transitive metals at high static pressures and temperatures (based on a temperature gradient growth technique) have been developed by Dr. Terentiev’s research team some years ago and successfully introduced in industrial department of ТISN СМ . Man-made IIa type single crystals are characterized by an optical transparency in a less than 25 µm wave lengths region and have fundamental absorption edge at 225 nanometers. Their thermal conductivity reaches 2000 Wt/m• К. Nitrogen concentration (a basic impurity element) level does not exceed 2 рр m (usually less than 1 рр m). -
Methods Used to Identifying Minerals
METHODS USED TO IDENTIFYING MINERALS More than 4,000 minerals are known to man, and they are identified by their physical and chemical properties. The physical properties of minerals are determined by the atomic structure and crystal chemistry of the minerals. The most common physical properties are crystal form, color, hardness, cleavage, and specific gravity. CRYSTALS One of the best ways to identify a mineral is by examining its crystal form (external shape). A crystal is defined as a homogenous solid possessing a three-dimensional internal order defined by the lattice structure. Crystals developed under favorable conditions often exhibit characteristic geometric forms (which are outward expressions of the internal arrangements of atoms), crystal class, and cleavage. Large, well- developed crystals are not common because of unfavorable growth conditions, but small crystals recognizable with a hand lens or microscope are common. Minerals that show no external crystal form but possess an internal crystalline structure are said to be massive. A few minerals, such as limonite and opal, have no orderly arrangement of atoms and are said to be amorphous. Crystals are divided into six major classes based on their geometric form: isometric, tetragonal, hexagonal, orthorhombic, monoclinic, and triclinic. The hexagonal system also has a rhombohedral subdivision, which applies mainly to carbonates. CLEAVAGE AND FRACTURE After minerals are formed, they have a tendency to split or break along definite planes of weakness. This property is called cleavage. These planes of weakness are closely related to the internal structure of the mineral, and are usually, but not always, parallel to crystal faces or possible crystal faces.