Structural Characterization Studies on Semiconducting Znsnn2 Films Using Synchrotron X-Ray Diffraction
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Laser Raman Spectroscopy As a Technique for Identification Of
ARTICLE IN PRESS CHEMGE-15589; No of Pages 13 Chemical Geology xxx (2008) xxx–xxx Contents lists available at ScienceDirect Chemical Geology journal homepage: www.elsevier.com/locate/chemgeo Laser Raman spectroscopy as a technique for identification of seafloor hydrothermal and cold seep minerals Sheri N. White ⁎ Department of Applied Ocean Physics and Engineering, Woods Hole Oceanographic Institution, Woods Hole, MA 02536, USA article info abstract Article history: In situ sensors capable of real-time measurements and analyses in the deep ocean are necessary to fulfill the Received 8 August 2008 potential created by the development of autonomous, deep-sea platforms such as autonomous and remotely Received in revised form 8 November 2008 operated vehicles, and cabled observatories. Laser Raman spectroscopy (a type of vibrational spectroscopy) is an Accepted 10 November 2008 optical technique that is capable of in situ molecular identification of minerals in the deep ocean. The goals of this Available online xxxx work are to determine the characteristic spectral bands and relative Raman scattering strength of hydrothermally- Editor: R.L. Rudnick and cold seep-relevant minerals, and to determine how the quality of the spectra are affected by changes in excitation wavelength and sampling optics. The information learned from this work will lead to the development Keywords: of new, smaller sea-going Raman instruments that are optimized to analyze minerals in the deep ocean. Raman spectroscopy Many minerals of interest at seafloor hydrothermal and cold seep sites are Raman active, such as elemental sulfur, Mineralogy carbonates, sulfates and sulfides. Elemental S8 sulfur is a strong Raman scatterer with dominant bands at ∼219 and Hydrothermal vents 472 Δcm−1. -
Both Pestle and Mortar Should Be Sent to a Commercial Heat Treating House to Be Carburized to a Depth of at Least $ Inch and Hardened to 62-64 Rockwell C
NOTES AND NEWS 165 Both pestle and mortar should be sent to a commercial heat treating house to be carburized to a depth of at least $ inch and hardened to 62-64 Rockwell C. It is not necessaryto harden the sleeve although it may be cyanided. After heat treating the mortar is chucked in the lathe and the diameter of the projection is ground with a tool post grinder to a tight, but re- movable, fi.t to the sleeve. The face of the projection should be ground true to the side at the same chucking. The pestle is also chucked and the diameter of the grinding end reduced about .005 inch, or a working fit in the sleeve.The face of the pestle should also be ground true with the side. A NEW LOCALITY FOR GREENOCKITE CRYSTALS IN BOLIVIA FnBoBnrco Aur,rnr,o, C ochabambo, Bol'ivia. Greenockite is a rare mineral in the Bolivian tin deposits' It has been describedonly from Llallagua by S. Gordon (1). The mineral forms coat- ings of minute red crystals, resembling vanadinite in colour, upon quartz' marcasite, cassiteriteand on the wall rock, almost always associatedwith wavellite. The crystals are exceedinglyminute, rarely measuring as much as 0.1 mm. They vary greatly in habit from pyramidal to thick tabular and prismatic. Cyclic twins are common. Gordon ascribesthe formation of the mineral to supergenesolutions. The source of the cadmium may have been from the wurtzite or sphalerite which has relaced pyrrhotite. 166 NOTESAND NEWS Recently I found a secondoccurrence of greenockite in Bolivia, which is remarkable for the larger size and the rich red colour of the crystals. -
Se2 Nanoparticles for Screen Printing Application
nanomaterials Article Large-Scale Synthesis of Semiconducting Cu(In,Ga)Se2 Nanoparticles for Screen Printing Application Bruna F. Gonçalves 1,2,3 , Alec P. LaGrow 1 , Sergey Pyrlin 2, Bryan Owens-Baird 4,5 , Gabriela Botelho 3 , Luis S. A. Marques 2, Marta M. D. Ramos 2, Kirill Kovnir 4,5 , Senentxu Lanceros-Mendez 2,6,7 and Yury V. Kolen’ko 1,* 1 International Iberian Nanotechnology Laboratory, 4715-330 Braga, Portugal; [email protected] (B.F.G.); [email protected] (A.P.L.) 2 Center of Physics, University of Minho, 4710-057 Braga, Portugal; pyrlinsv@fisica.uminho.pt (S.P.); lsam@fisica.uminho.pt (L.S.A.M.); marta@fisica.uminho.pt (M.M.D.R.); [email protected] (S.L.-M.) 3 Center of Chemistry, University of Minho, 4710-057 Braga, Portugal; [email protected] 4 Department of Chemistry, Iowa State University, Ames, IA 50011, USA; [email protected] (B.O.-B.); [email protected] (K.K.) 5 Ames Laboratory, U.S. Department of Energy, Ames, IA 50011, USA 6 BCMaterials, Basque Center for Materials, Applications and Nanostructures, UPV/EHU Science Park, 48940 Leioa, Spain 7 Ikerbasque, Basque Foundation for Science, 48009 Bilbao, Spain * Correspondence: [email protected] Citation: Gonçalves, B.F.; LaGrow, A.P.; Pyrlin, S.; Owens-Baird, B.; Abstract: During the last few decades, the interest over chalcopyrite and related photovoltaics has Botelho, G.; Marques, L.S.A.; Ramos, been growing due the outstanding structural and electrical properties of the thin-film Cu(In,Ga)Se2 M.M.D.; Kovnir, K.; photoabsorber. -
Dicke Superradiance in Solids [Invited]
C80 Vol. 33, No. 7 / July 2016 / Journal of the Optical Society of America B Review Dicke superradiance in solids [Invited] 1 1 2 1 2 KANKAN CONG, QI ZHANG, YONGRUI WANG, G. TIMOTHY NOE II, ALEXEY BELYANIN, AND 1,3,4, JUNICHIRO KONO * 1Department of Electrical and Computer Engineering, Rice University, Houston, Texas 77005, USA 2Department of Physics and Astronomy, Texas A&M University, College Station, Texas 77843, USA 3Department of Physics and Astronomy, Rice University, Houston, Texas 77005, USA 4Department of Materials Science and NanoEngineering, Rice University, Houston, Texas 77005, USA *Corresponding author: [email protected] Received 18 February 2016; revised 7 April 2016; accepted 7 April 2016; posted 8 April 2016 (Doc. ID 259437); published 13 May 2016 Recent advances in optical studies of condensed matter systems have led to the emergence of a variety of phenomena that have conventionally been studied in the realm of quantum optics. These studies have not only deepened our understanding of light–matter interactions but have also introduced aspects of many-body corre- lations inherent in optical processes in condensed matter systems. This paper is concerned with the phenomenon of superradiance (SR), a profound quantum optical process originally predicted by Dicke in 1954. The basic concept of SR applies to a general N body system, where constituent oscillating dipoles couple together through interaction with a common light field and accelerate the radiative decay of the whole system. Hence, the term SR ubiquitously appears in order to describe radiative coupling of an arbitrary number of oscillators in many situations in modern science of both classical and quantum description. -
Alphabetical List
LIST L - MINERALS - ALPHABETICAL LIST Specific mineral Group name Specific mineral Group name acanthite sulfides asbolite oxides accessory minerals astrophyllite chain silicates actinolite clinoamphibole atacamite chlorides adamite arsenates augite clinopyroxene adularia alkali feldspar austinite arsenates aegirine clinopyroxene autunite phosphates aegirine-augite clinopyroxene awaruite alloys aenigmatite aenigmatite group axinite group sorosilicates aeschynite niobates azurite carbonates agate silica minerals babingtonite rhodonite group aikinite sulfides baddeleyite oxides akaganeite oxides barbosalite phosphates akermanite melilite group barite sulfates alabandite sulfides barium feldspar feldspar group alabaster barium silicates silicates albite plagioclase barylite sorosilicates alexandrite oxides bassanite sulfates allanite epidote group bastnaesite carbonates and fluorides alloclasite sulfides bavenite chain silicates allophane clay minerals bayerite oxides almandine garnet group beidellite clay minerals alpha quartz silica minerals beraunite phosphates alstonite carbonates berndtite sulfides altaite tellurides berryite sulfosalts alum sulfates berthierine serpentine group aluminum hydroxides oxides bertrandite sorosilicates aluminum oxides oxides beryl ring silicates alumohydrocalcite carbonates betafite niobates and tantalates alunite sulfates betekhtinite sulfides amazonite alkali feldspar beudantite arsenates and sulfates amber organic minerals bideauxite chlorides and fluorides amblygonite phosphates biotite mica group amethyst -
Minerals Found in Michigan Listed by County
Michigan Minerals Listed by Mineral Name Based on MI DEQ GSD Bulletin 6 “Mineralogy of Michigan” Actinolite, Dickinson, Gogebic, Gratiot, and Anthonyite, Houghton County Marquette counties Anthophyllite, Dickinson, and Marquette counties Aegirinaugite, Marquette County Antigorite, Dickinson, and Marquette counties Aegirine, Marquette County Apatite, Baraga, Dickinson, Houghton, Iron, Albite, Dickinson, Gratiot, Houghton, Keweenaw, Kalkaska, Keweenaw, Marquette, and Monroe and Marquette counties counties Algodonite, Baraga, Houghton, Keweenaw, and Aphrosiderite, Gogebic, Iron, and Marquette Ontonagon counties counties Allanite, Gogebic, Iron, and Marquette counties Apophyllite, Houghton, and Keweenaw counties Almandite, Dickinson, Keweenaw, and Marquette Aragonite, Gogebic, Iron, Jackson, Marquette, and counties Monroe counties Alunite, Iron County Arsenopyrite, Marquette, and Menominee counties Analcite, Houghton, Keweenaw, and Ontonagon counties Atacamite, Houghton, Keweenaw, and Ontonagon counties Anatase, Gratiot, Houghton, Keweenaw, Marquette, and Ontonagon counties Augite, Dickinson, Genesee, Gratiot, Houghton, Iron, Keweenaw, Marquette, and Ontonagon counties Andalusite, Iron, and Marquette counties Awarurite, Marquette County Andesine, Keweenaw County Axinite, Gogebic, and Marquette counties Andradite, Dickinson County Azurite, Dickinson, Keweenaw, Marquette, and Anglesite, Marquette County Ontonagon counties Anhydrite, Bay, Berrien, Gratiot, Houghton, Babingtonite, Keweenaw County Isabella, Kalamazoo, Kent, Keweenaw, Macomb, Manistee, -
A Comprehensive Review of Zno Materials and Devices Ü
Virginia Commonwealth University VCU Scholars Compass Electrical and Computer Engineering Publications Dept. of Electrical and Computer Engineering 2005 A comprehensive review of ZnO materials and devices Ü. Özgür Virginia Commonwealth University, [email protected] Ya. I. Alivov Virginia Commonwealth University C. Liu Virginia Commonwealth University See next page for additional authors Follow this and additional works at: http://scholarscompass.vcu.edu/egre_pubs Part of the Electrical and Computer Engineering Commons Ozgur, U., Alivov, Y. I., Liu, C., et al. A comprehensive review of ZnO materials and devices. Journal of Applied Physics 98, 041301 (2005). Copyright © 2005 AIP Publishing LLC. Downloaded from http://scholarscompass.vcu.edu/egre_pubs/174 This Article is brought to you for free and open access by the Dept. of Electrical and Computer Engineering at VCU Scholars Compass. It has been accepted for inclusion in Electrical and Computer Engineering Publications by an authorized administrator of VCU Scholars Compass. For more information, please contact [email protected]. Authors Ü. Özgür, Ya. I. Alivov, C. Liu, A. Teke, M. A. Reshchikov, S. Doğan, Vitaliy Avrutin, S.-J. Cho, and H. Morkoç This article is available at VCU Scholars Compass: http://scholarscompass.vcu.edu/egre_pubs/174 JOURNAL OF APPLIED PHYSICS 98, 041301 ͑2005͒ APPLIED PHYSICS REVIEWS A comprehensive review of ZnO materials and devices ͒ ͒ ͒ Ü. Özgür,a Ya. I. Alivov, C. Liu, A. Teke,b M. A. Reshchikov, S. Doğan,c V. Avrutin, ͒ S.-J. Cho, and H. Morkoçd Department of Electrical Engineering and Physics Department, Virginia Commonwealth University, Richmond, Virginia 23284-3072 ͑Received 2 February 2005; accepted 13 June 2005; published online 30 August 2005͒ The semiconductor ZnO has gained substantial interest in the research community in part because of its large exciton binding energy ͑60 meV͒ which could lead to lasing action based on exciton recombination even above room temperature. -
Primary Minerals of the Jáchymov Ore District
Journal of the Czech Geological Society 48/34(2003) 19 Primary minerals of the Jáchymov ore district Primární minerály jáchymovského rudního revíru (237 figs, 160 tabs) PETR ONDRU1 FRANTIEK VESELOVSKÝ1 ANANDA GABAOVÁ1 JAN HLOUEK2 VLADIMÍR REIN3 IVAN VAVØÍN1 ROMAN SKÁLA1 JIØÍ SEJKORA4 MILAN DRÁBEK1 1 Czech Geological Survey, Klárov 3, CZ-118 21 Prague 1 2 U Roháèových kasáren 24, CZ-100 00 Prague 10 3 Institute of Rock Structure and Mechanics, V Holeovièkách 41, CZ-182 09, Prague 8 4 National Museum, Václavské námìstí 68, CZ-115 79, Prague 1 One hundred and seventeen primary mineral species are described and/or referenced. Approximately seventy primary minerals were known from the district before the present study. All known reliable data on the individual minerals from Jáchymov are presented. New and more complete X-ray powder diffraction data for argentopyrite, sternbergite, and an unusual (Co,Fe)-rammelsbergite are presented. The follow- ing chapters describe some unknown minerals, erroneously quoted minerals and imperfectly identified minerals. The present work increases the number of all identified, described and/or referenced minerals in the Jáchymov ore district to 384. Key words: primary minerals, XRD, microprobe, unit-cell parameters, Jáchymov. History of mineralogical research of the Jáchymov Chemical analyses ore district Polished sections were first studied under the micro- A systematic study of Jáchymov minerals commenced scope for the identification of minerals and definition early after World War II, during the period of 19471950. of their relations. Suitable sections were selected for This work was aimed at supporting uranium exploitation. electron microprobe (EMP) study and analyses, and in- However, due to the general political situation and the teresting domains were marked. -
Some Chemical Problems in Geology
Scholars' Mine Masters Theses Student Theses and Dissertations 1916 Some chemical problems in geology Reginald Scott Dean Follow this and additional works at: https://scholarsmine.mst.edu/masters_theses Part of the Physical Sciences and Mathematics Commons Department: Recommended Citation Dean, Reginald Scott, "Some chemical problems in geology" (1916). Masters Theses. 4650. https://scholarsmine.mst.edu/masters_theses/4650 This thesis is brought to you by Scholars' Mine, a service of the Missouri S&T Library and Learning Resources. This work is protected by U. S. Copyright Law. Unauthorized use including reproduction for redistribution requires the permission of the copyright holder. For more information, please contact [email protected]. SOME CHEMICAL PROBLEMS IN GEOLOGY BY REGINALD SCOTT DEAl A THESIS subm! tted to the faculty of the SCHOOL OF MIRES liD METALLURGY OF THE UNIVERSI!Y OF MISSOURI in partial ful~111.8nt of the work required for the Degree o~ MASTER OF SCIENCE Rolla, Mo. 1916 Approved bY __~:r.w....""...;.:.:..uI· .. c?tt6~~vLJjoUll:iWl~~(' ___ Professor of Chemistr,r. TABLE OF CONTENTS. Introduotion. The Nature and Formation of Iron Disulfide. Bibliography. The Nature of Iron Disulfide. The Formation of Iron Disulfide in Nature. ~actor8 Controlling the Formation of Maroasite or Pyrite. The Natural ~erric Oxides. BIbliography • The Nature of a Gel. Natural Ferric OxIdes. The Reduotion of Sulfates to Sulfides. Relations of Pyrite to Maroasite and Sphalerite to Wurtzite. (Some Chemical Problems in Geology) INTRODUCTION. This thesis is in the main a oompi1ation of the views held at this institution in regard to the prob lems disoussed as interpreted by the author. -
A New Zincian Greenockite Occurrence in the Saishitang Cu Skarn Deposit, Qinghai Province, Northwest China
minerals Article A New Zincian Greenockite Occurrence in the Saishitang Cu Skarn Deposit, Qinghai Province, Northwest China Jianping Liu and Shugen Zhang * Key Laboratory of Metallogenic Prediction of Non-Ferrous Metals and Geological Environment Monitor (Central South University), Ministry of Education, Changsha 410083, China; [email protected] * Correspondence: [email protected]; Tel.: +86-731-888-30616 Received: 15 June 2017; Accepted: 26 July 2017; Published: 28 July 2017 Abstract: Zn-Cd-S series minerals not only comprise industrial resources for Zn and Cd, but are also significant mineralogical indicators for hydrothermal ore-forming processes. Due to its unique formation conditions and rare occurrence, our understanding of the formation of zincian greenockite in natural systems is limited. Zincian greenockite was discovered during mineralogical studies in the Saishitang Cu skarn deposit, Qinghai Province, Northwest China. This provided an ideal opportunity to assess the occurrence and formation of zincian greenockite in skarn-type deposits. Ore minerals were observed using reflected-light microscopy, and the zincian greenockite was further analyzed using electron-probe microanalysis (EPMA) and X-ray diffraction (XRD). The zincian greenockite occurs in the bornite–chalcopyrite ores and is composed of subhedral to anhedral grains approximately 50 × 150 µm2 to 200 × 300 µm2 in size, replaces the bornite, and is replaced by native silver. Two phases (I and II) were identified based on back-scattered electron images, X-ray element-distributions maps, and EPMA data. The textural relationship indicated that Phase I was replaced by Phase II. Phase I contained high Zn (14.6 to 21.7 mol % ZnS) and low Cd (72.4 to 82.2 mol % CdS), while Phase II contained low Zn (5.6 to 9.1 mol % ZnS) and high Cd (85.4 to 89.9 mol % CdS). -
Sulfide Sulfate Chimneys on the East Pacific Rise
Canadian Mineralogist Yol.26, pp. 487-504(1988) SULFIDE_SULFATECHIMNEYS ON THE EAST PACIFICRISE, 11o AND 13oN LAflTUDES. PARTt: MtNERALOcy AND PARAGENESTS URSULAM. GRAHAM, GREGGJ. BLUTHaNo HIRoSHI oHMoTo Department of Geosciences,The Pennsylvonia State University, University Park, Pennsylvania 16802,U.S.A. ASSTRACT speciesfor FeS2,but also recrystallization and replacernent of earlier minerals in warmer conditions. Hydrothermal fluids up to -350.C emerge . o from vent sitesar I I and I3"N latitudes,East pacific Rise. Varia_ Keywords: chimneys, hydrothermal, sulfides, sulfates, tions in the morphology, zoning and mtneralogyof 27 chim_ mineralogy, zoning, paragenesis.East Pacific Rise. neys from I I vent sites can be representedby three active a1{ ge eltinctdogged chimney. Microscopii observation SoMMAIRE of 127 polished sections of these four chimneys has rev_ ealedfour types eachofmarcasite, pyrite and wurtzite, and Des fluides hydrothermaux atteignant une temp6rature lwg.types of sphalerite, which are distinct in their crystal d'environ 350oCsont 6mis des€vents aux latitudes llo et habits. Th€ consistency in the parageneticsequ.n.. und io l3oN, le long de la ride Est-Pacifique.Les variations en the spatial distribution with respect to the exterior chim_ morphologie, zonation et mindralogiede 27 chemin6espro- ney wall of theseFe and Zn sulfides, as well as anhydrite, venant de I I sites sont bien repr6sentdespar trois chemi- cialcopyrite and bornite in these four chimneys ,r,ggot, ndesactives et une €teinte qui est engorgdede d6p6ts. Un all chimneys tha-t in the ll vent sites ,epresent sililar examen par microscopie de 127 sections prdlevdesde ces hydrothermal processes.The variation among the chimneys quatre chemindesr6vble la prdsencede quatre g6n6ralions reflects simply the difference in the maturity (ongevity of de marcasite, pyrite et wurtzite, et deux de sphal6rite, dis- vgnting) preservation and of a complete liaeirty ctrlmney, tingudespar leur habitus. -
Coupled Substitutions of Minor and Trace Elements in Co-Existing Sphalerite and Wurtzite
minerals Article Coupled Substitutions of Minor and Trace Elements in Co-Existing Sphalerite and Wurtzite Allan Pring 1,*, Benjamin Wade 2, Aoife McFadden 2,3, Claire E. Lenehan 1 and Nigel J. Cook 4 1 College of Science and Engineering, Flinders University, Adelaide 5001, South Australia, Australia; claire.lenehan@flinders.edu.au 2 Adelaide Microscopy, The University of Adelaide, Adelaide 5005, South Australia, Australia; [email protected] (B.W.); [email protected] (A.M.) 3 Flinders Microscopy, Flinders University, Adelaide 5001, South Australia, Australia 4 School of Chemical Engineering and Advanced Materials, The University of Adelaide, Adelaide 5005, South Australia, Australia; [email protected] * Correspondence: allan.pring@flinders.edu.au; Tel.: +618-8201-5570 Received: 28 November 2019; Accepted: 6 February 2020; Published: 9 February 2020 Abstract: The nature of couple substitutions of minor and trace element chemistry of expitaxial intergrowths of wurtzite and sphalerite are reported. EPMA and laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS) analyses display significant differences in the bulk chemistries of the two epitaxial intergrowth samples studied. The sample from the Animas-Chocaya Mine complex of Bolivia is Fe-rich with mean Fe levels of 4.8 wt% for wurztite-2H and 2.3 wt% for the sphalerite component, while the sample from Merelani Hills, Tanzania, is Mn-rich with mean Mn levels in wurztite-4H of 9.1 wt% and for the sphalerite component 7.9 wt% In both samples studied the wurtzite polytype is dominant over sphalerite. LA-ICP-MS line scans across the boundaries between the wurtzite and sphalerite domains within the two samples show significant variation in the trace element chemistries both between and within the two coexisting polytypes.