Emissions of Hazardous Air Pollutants from Coal-Fired Power Plants
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Petrographic and Vitrinite Reflectance Analyses of a Suite of High Volatile Bituminous Coal Samples from the United States and Venezuela
Petrographic and vitrinite reflectance analyses of a suite of high volatile bituminous coal samples from the United States and Venezuela Open-File Report 2008-1230 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior Dirk A. Kempthorne, Secretary U.S. Geological Survey Mark D. Myers, Director U.S. Geological Survey, Reston, Virginia 2008 For product and ordering information: World Wide Web: http://www.usgs.gov/pubprod Telephone: 1-888-ASK-USGS For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment: World Wide Web: http://www.usgs.gov Telephone: 1-888-ASK-USGS Suggested citation: Hackley, P.C., Kolak, J.J., 2008, Petrographic and vitrinite reflectance analyses of a suite of high volatile bituminous coal samples from the United States and Venezuela: U.S. Geological Survey Open-File Report 2008-1230, 36 p., http://pubs.usgs.gov/of/2008/1230. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted material contained within this report. ii Contents Introduction ........................................................................................................................................................................1 Methods ..............................................................................................................................................................................1 -
Middle School - Round 14A
MIDDLE SCHOOL - ROUND 14A TOSS-UP 1) Earth and Space – Short Answer What is the term for sediment with a particle size less than 2 microns? ANSWER: CLAY BONUS 1) Earth and Space – Multiple Choice Which of the following correctly describes the typical progression from dead organic matter to coal? W) Peat, lignite, bituminous [bih-TOOM-in-us], anthracite [AN-thrah-site] X) Lignite, peat, bituminous, anthracite Y) Lignite, bituminous, peat, anthracite Z) Peat, bituminous, anthracite, lignite ANSWER: W) PEAT, LIGNITE, BITUMINOUS, AND ANTHRACITE ~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ TOSS-UP 2) Physical Science – Short Answer Chlorine has an atomic mass of 35.45. Given that chlorine has two naturally-occurring isotopes, chlorine-35 and chlorine-37, then, to the nearest whole number, what percentage of chlorine atoms have a mass number of 35.45? ANSWER: ZERO BONUS 2) Physical Science – Short Answer To the nearest gram, what is the mass of two moles of carbon dioxide? ANSWER: 88 Middle School - Round 14A Page 1 TOSS-UP 3) Math – Short Answer What is the slope of a line perpendicular to the line with equation 7x – 4y = –28? ANSWER: –4/7 BONUS 3) Math – Short Answer A fence is built along the perimeter of a 200-foot-by-300-foot rectangular field. Posts are placed at the four corners and every 5 feet thereafter. How many posts are required? ANSWER: 200 ~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ TOSS-UP 4) Life Science – Short Answer In eukaryotes [YOO-care-ee-oats], DNA and histones are organized into what structures? ANSWER: CHROMOSOMES BONUS 4) Life Science – Short Answer What type of microscopy [my-CRAW-scah-pee] involves the use of a laser, photomultiplier detector, and a pinhole that ensures elimination of out-of-plane light emitted by the sample? ANSWER: CONFOCAL Middle School - Round 14A Page 2 TOSS-UP 5) Energy – Short Answer Researchers at the Joint BioEnergy Institute are studying ionic liquids as a solvent to break down cellulose before biofuel production. -
Anthracite Coal 13
Rock and Mineral 10-Specimen Kit Companion Book Presented by This mineral kit was also made possible through the generosity of the mining companies who supplied the minerals. If you have any questions or comments about this kit please contact the SME Pittsburgh Section Chair at www.smepittsburgh.org. For more information about mining, visit the following web site: www.smepittsburgh.org BSA’s www.scouting.org - search “Mining in Society” SME’s www.mineralseducationcoalition.org/ Updated July 2016 © SME Pittsburgh Section The SME Pittsburgh Section thanks the companies, mines, and individuals who provided mineral samples and donated time or services that made these mineral kits possible. Alpha Natural Resources, Inc. CONSOL Energy, Inc. Coolspring Stone Supply John T. Boyd Company Morton Salt Murray Energy Corporation Newmont Mining Corporation Reed Gold Mine (State of North Carolina) Steelhead Specialty Minerals United States Gypsum Company US Steel Corporation United Taconite (Cliffs Natural Resources, Inc.) CONTENTS INTRODUCTION 3 MINERAL IDENTIFICATION 5 FUELS 10 Bituminous Coal 12 Anthracite Coal 13 BASE METAL ORES 14 Iron Ore 15 Copper Ore 16 PRECIOUS METALS 17 Gold Ore 18 ROCKS AND INDUSTRIAL MINERALS 19 Gypsum 21 Limestone 22 Marble 23 Salt 24 Zeolite 25 Note: many of the images reproduced here are from Wikipedia which allows non commercial use or from the Minerals Education Coalition web site http://www.mineralseducationcoalition.org/minerals. INTRODUCTION The effect rocks and minerals have on our daily lives is not always obvious, but this book will help explain how essential they really are. If you don’t think you come in contact with minerals every day, think about these facts below and see if you change your mind. -
Coal Characteristics
CCTR Indiana Center for Coal Technology Research COAL CHARACTERISTICS CCTR Basic Facts File # 8 Brian H. Bowen, Marty W. Irwin The Energy Center at Discovery Park Purdue University CCTR, Potter Center, 500 Central Drive West Lafayette, IN 47907-2022 http://www.purdue.edu/dp/energy/CCTR/ Email: [email protected] October 2008 1 Indiana Center for Coal Technology Research CCTR COAL FORMATION As geological processes apply pressure to peat over time, it is transformed successively into different types of coal Source: Kentucky Geological Survey http://images.google.com/imgres?imgurl=http://www.uky.edu/KGS/coal/images/peatcoal.gif&imgrefurl=http://www.uky.edu/KGS/coal/coalform.htm&h=354&w=579&sz= 20&hl=en&start=5&um=1&tbnid=NavOy9_5HD07pM:&tbnh=82&tbnw=134&prev=/images%3Fq%3Dcoal%2Bphotos%26svnum%3D10%26um%3D1%26hl%3Den%26sa%3DX 2 Indiana Center for Coal Technology Research CCTR COAL ANALYSIS Elemental analysis of coal gives empirical formulas such as: C137H97O9NS for Bituminous Coal C240H90O4NS for high-grade Anthracite Coal is divided into 4 ranks: (1) Anthracite (2) Bituminous (3) Sub-bituminous (4) Lignite Source: http://cc.msnscache.com/cache.aspx?q=4929705428518&lang=en-US&mkt=en-US&FORM=CVRE8 3 Indiana Center for Coal Technology Research CCTR BITUMINOUS COAL Bituminous Coal: Great pressure results in the creation of bituminous, or “soft” coal. This is the type most commonly used for electric power generation in the U.S. It has a higher heating value than either lignite or sub-bituminous, but less than that of anthracite. Bituminous coal -
On the Fundamental Difference Between Coal Rank and Coal Type
International Journal of Coal Geology 118 (2013) 58–87 Contents lists available at ScienceDirect International Journal of Coal Geology journal homepage: www.elsevier.com/locate/ijcoalgeo Review article On the fundamental difference between coal rank and coal type Jennifer M.K. O'Keefe a,⁎, Achim Bechtel b,KimonChristanisc, Shifeng Dai d, William A. DiMichele e, Cortland F. Eble f,JoanS.Esterleg, Maria Mastalerz h,AnneL.Raymondi, Bruno V. Valentim j,NicolaJ.Wagnerk, Colin R. Ward l, James C. Hower m a Department of Earth and Space Sciences, Morehead State University, Morehead, KY 40351, USA b Department of Applied Geosciences and Geophysics, Montan Universität, Leoben, Austria c Department of Geology, University of Patras, 265.04 Rio-Patras, Greece d State Key Laboratory of Coal Resources and Safe Mining, China University of Mining and Technology, Beijing 100083, China e Department of Paleobiology, Smithsonian Institution, Washington, DC 20013-7012, USA f Kentucky Geological Survey, University of Kentucky, Lexington, KY 40506, USA g School of Earth Sciences, The University of Queensland, QLD 4072, Australia h Indiana Geological Survey, Indiana University, 611 North Walnut Grove, Bloomington, IN 47405-2208, USA i Department of Geology and Geophysics, College Station, TX 77843, USA j Department of Geosciences, Environment and Spatial Planning, Faculty of Sciences, University of Porto and Geology Centre of the University of Porto, Rua Campo Alegre 687, 4169-007 Porto, Portugal k School Chemical & Metallurgical Engineering, University of Witwatersrand, 2050, WITS, South Africa l School of Biological, Earth and Environmental Sciences, University of New South Wales, Sydney, Australia m University of Kentucky, Center for Applied Energy Research, 2540 Research Park Drive, Lexington, KY 40511, USA article info abstract Article history: This article addresses the fundamental difference between coal rank and coal type. -
Iea Statistics
IEA STATISTICS COAL INFORMATION Corrigendum Please note that despite our best efforts to ensure quality control, errors have slipped into the Coal Information 2015. New pages from IV.435 to IV.444 (Plus, “Achevé d’imprimer” changed to “second edition, October 2015”) See next pages 2015 Secure Sustainable Together COAL INFORMATION (2015 edition) PART IV - IV.435 COUNTRY NOTES In many cases, data submitted by Member countries to Greenhouse and Energy Reporting (NGER) data as the secretariat do not conform to the standard report- the main energy consumption data source for the ing methodology or have other particular characteris- Australian Energy Statistics. As a result, there are tics. Information set out below will assist readers to breaks in the time series for many data between 2002 interpret data for particular countries and aid in the and 2003. The revisions have also introduced some comparison of data among countries. methodological problems. The national statistics appear The notes given below refer to data for the years 1960 to have problems identifying inputs and outputs to cer- to 2013 and may also refer to 2014p preliminary data tain transformation processes such as gas works plants, as well as the information on CD-ROM and the on- electricity plants and CHP plants. Energy industry own line data service. In general, more detailed notes are use and inputs to the transformation processes are available for data since 1990. sometimes not reported separately in the correct cate- gories. More detail is given in the notes below. Data for anthracite, coking coal, other bituminous coal, sub-bituminous coal and lignite are available separately For the 2002 data, the Australian administration began from 1978. -
Maceral Types and Quality of Coal in the Tuli Coalfield: a Case
applied sciences Article Maceral Types and Quality of Coal in the Tuli Coalfield: A Case Study of Coal in the Madzaringwe Formation in the Vele Colliery, Limpopo Province, South Africa Elelwani Denge * and Christopher Baiyegunhi Department of Geology and Mining, University of Limpopo, Private Bag X1106, Sovenga 0727, South Africa; [email protected] * Correspondence: [email protected] Featured Application: Authors are encouraged to provide a concise description of the specific application or a potential application of the work. This section is not mandatory. Abstract: The Madzaringwe Formation in the Vele colliery is one of the coal-bearing Late Palaeozoic units of the Karoo Supergroup, consisting of shale with thin coal seams and sandstones. Maceral group analysis was conducted on seven representative coal samples collected from three existing boreholes—OV125149, OV125156, and OV125160—in the Vele colliery to determine the coal rank and other intrinsic characteristics of the coal. The petrographic characterization revealed that vitrinite is the dominant maceral group in the coals, representing up to 81–92 vol.% (mmf) of the total sample. Collotellinite is the dominant vitrinite maceral, with a total count varying between 52.4 vol.% (mmf) and 74.9 vol.% (mmf), followed by corpogelinite, collodetrinite, tellinite, and pseudovitrinite with a Citation: Denge, E.; Baiyegunhi, C. count ranging between 0.8 and 19.4 vol.% (mmf), 1.5 and 17.5 vol.% (mmf), 0.8 and 6.5 vol.% (mmf) Maceral Types and Quality of Coal in the Tuli Coalfield: A Case Study of and 0.3 and 5.9 vol.% (mmf), respectively. The dominance of collotellinite gives a clear indication Coal in the Madzaringwe Formation that the coals are derived from the parenchymatous and woody tissues of roots, stems, and leaves. -
C) an Introduction to Coal Quality
Chapter C The National Coal Resource Assessment An Introduction to Coal Quality Overview By Stanley P. Schweinfurth1 Click here to return to Volume Table of Contents Chapter C of The National Coal Resource Assessment Overview Edited by Brenda S. Pierce and Kristin O. Dennen U.S. Geological Survey Professional Paper 1625–F 1U.S. Geological Survey, Reston, Virginia 20192 This report, although in the USGS Professional Paper series, is available only on CD–ROM U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior KEN SALAZAR, Secretary U.S. Geological Survey Suzette M. Kimball, Acting Director U.S. Geological Survey, Reston, Virginia: 2009 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment, visit http://www.usgs.gov or call 1-888-ASK-USGS For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod To order this and other USGS information products, visit http://store.usgs.gov Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted materials contained within this report. Suggested citation: Schweinfurth, S.P., 2009, An introduction to coal quality, in Pierce, B.S., and Dennen, K.O., eds., The National Coal Resource Assessment Overview: U.S. Geological Survey Professional Paper 1625–F, Chapter C, 16 p. -
Anthracite Anthracite – an Overview
ANTHRACITE ANTHRACITE – AN OVERVIEW Anthracite is a high-rank coal, representing a coal that has been subjected to the highest grade of metamorphism. Anthracite is shiny black, hard and brittle and has the highest fixed-carbon content. Due to its low volatile matter, anthracite's combustion process is slow. Most anthracites have low-moisture content and their heating value is up to 8,200 kcal/kg. Anthracite combusts with hot, clean flame, containing low content of sulfur and volatiles. Due to these characteristics, anthracite is often used in specialized industrial uses that require smokeless fuels. 2 CLASSIFICATION OF COAL 3 ANTHRACITE – AN OVERVIEW Anthracite has a history of use A small amount of impurities in blast furnaces for iron smelting; and a high percentage of carbon however, it lacks the pore space of makes anthracite coal the most metallurgical coke, which advantageous for combustion, as eventually replaced anthracite. it gives the maximum amount of Nonetheless, anthracite is a unique energy. high-tech raw material characterized by the maximum carbon content. In various grades In its calorific value, UHQ of coal, this parameter can range anthracite surpasses all other from 50 pct in brown coal (lignite), grades of coal – 8,200 kcal/kg to 95 pct of ultra high quality compared to 7,000 kcal/kg of anthracite coal (UHQ). The higher natural gas. Coal Anthracite is the the carbon content in coal, the hardest of all coals and practically smaller the volume of various does not sinter. impurities, such as nitrogen, hydrogen, ash, and so on. 4 USES OF UHQ ANTHRACITE Anthracites can be used in various spheres of human activity, like industrial production (metal smelting, power generation, chemical – filtering sugar to make it white and as catalyst support, soda ash, and pharmaceutical industry as a material absorbents in the production of medicines, etc.). -
Bituminous Coal and Lignite Surface Mining 1997 Issued October 1999
Bituminous Coal and Lignite Surface Mining 1997 Issued October 1999 EC97N-2121A 1997 Economic Census Mining Industry Series U.S. Department of Commerce Economics and Statistics Administration U.S. CENSUS BUREAU ACKNOWLEDGMENTS The staff of the Manufacturing and Con- The Geography Division staff developed struction Division prepared this report. geographic coding procedures and associ- Judy M. Dodds, Assistant Chief for Cen- ated computer programs. sus and Related Programs, was respon- The Economic Statistical Methods and Pro- sible for the overall planning, manage- gramming Division, Charles P. Pautler ment, and coordination. Patricia L. Jr., Chief, developed and coordinated the Horning, Chief, Construction and Miner- computer processing systems. Martin S. als Branch, assisted by M. Susan Bucci Harahush, Assistant Chief for Quinquen- and Susan L. DiCola, Section Chiefs, per- nial Programs, assisted by Barbara Lam- formed the planning and implementation. bert and Christina Arledge were respon- Richard Hough, Christopher D. sible for design and implementation of the Perrien, John F. Roehl, Eva J. Snapp, computer systems. Gary T. Sheridan, and Sarah B. Teichner provided primary Chief, Manufacturing and Construction staff assistance. Branch, Lori A. Guido and Roy A. Smith, Brian Greenberg, Assistant Chief for Section Chiefs, supervised the preparation Research and Methodology Programs, of the computer programs. assisted by Stacey Cole, Chief, Manufac- turing Programs Methodology Branch, and Computer Services Division, Debra Will- Robert Struble, Section Chief, provided iams, Chief, performed the computer pro- the mathematical and statistical tech- cessing. niques as well as the coverage operations. The staff of the Administrative and Cus- Jeffrey Dalzell and Cathy Ritenour pro- tomer Services Division, Walter C. -
The Pennsylvania Anthracite District – a Frontier Area for the Development
Milici, R.C., 2004, The Pennsylvania Anthracite District – a frontier area for the development of coalbed methane?, in Warwick, P.D., ed., Selected presentations on coal-bed gas in the eastern United States, U.S. Geological Survey Open-File Report 2004-1273, p. 37-59. The Pennsylvania Anthracite District – a Frontier Area for the Development of 1 Coalbed Methane? By Robert C. Milici2 Abstract3 The anthracite region of eastern Pennsylvania consists of four major coal fields that are within the folded and faulted Appalachians, in the Valley and Ridge and Appalachian Plateaus physiographic provinces. These are, from south to north, the Southern Anthracite field, the Western Middle Anthracite field, the Eastern Middle Anthracite field, and the Northern Anthracite field. Rank of the coal ranges from semi-anthracite to anthracite. In general, the anthracite fields consist of Pennsylvanian strata that are complexly folded, faulted, and preserved in structural synclines within older Paleozoic strata. Published gas-in-place (GIP) data for Pennsylvania anthracite range from 6.4 SCF/ton (0.2 cc/g) for the Orchard coal bed to a high of 691.2 SCF/ton (21.6 cc/g) from a sample of the Peach Mountain coal bed that was collected in the Southern Anthracite field at a depth of 685 feet. This is the largest GIP value that the U.S. Bureau of Mines (USBM) (Diamond et al, 1986) reported for coalbed methane (CBM) nationwide. Of the 11 CBM analyses reported for the Southern Field by USBM, seven exceed 396 SCF/ton (12.4 cc/g) (average of 11 samples: 325.8 SCF/ton [10.2 cc/g]). -
Heats of Combustion of Anthracite Cokes and of Artificial and Natural Graphites 1
1 U. S. DEPARTMENT OF COMMERCE NATIONAL BUREAU OF STANDARDS RESEARCH PAPER RP1139 Part of Journal of Research of the National Bureau of Standards, Volume 21 : October 1938 HEATS OF COMBUSTION OF ANTHRACITE COKES AND OF ARTIFICIAL AND NATURAL GRAPHITES 1 By Phillip H. Dewey 2 and D. Roberts Harper, 3d 3 ABSTRACT There have been determined the heats of combustion of 30 samples of anthracite coke of known different temperatures of preparation (900° to 1,300° C) , hydrogen contents (0.08 to 0.78 percent), and adsorptive capacities (0.13 t o 37.5 cma of gaseous CO2 pel' gram of solid carbon), in order to study the effect of these proper ties on the energy content of the material. Data were also obtained on the heats of combustion of two samples of pure ash-free artifi cial graphite and four different samples of natural graphite. The heats evolved, expressed in international kilojoul es, for the combustion of 1 mole of solid carbon to form CO2, at 25.0° C and a pressure of 1 atmosphere, without the production of external work, are as follows : Art ificial graphit.e No. 0, 393.39 ± 0.17; artificial graphite No. I, 393.25 ± 0.15; Ticonderoga natural graphite, 393.32 ± 0.1l; Buckingham nat ural graphite, 393.35 ±0.13; Baffin Island natural graphite, 393.37 ± 0.26; and hydrogen-free anthracite coke, 403.03 ±0.29 (obtained by linear extrapolation to zero hydrogen content of the data on the hydrogen-containing cokes). CONTENTS Page I. Introduction __ _________ ____ ______ ____ ______ __________________ _ 457 II.