Coal Mine Methane: a Review of Capture and Utilization Practices with Benefits to Mining Safety and to Greenhouse Gas Reduction
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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 -
Masterarbeit
MASTERARBEIT Titel der Masterarbeit Late Cretaceous Volcaniclastic Rocks in the Pontides (NW Turkey) verfasst von Katharina Böhm BSc angestrebter akademischer Grad Master of Science (M.Sc.) Wien, 2015 Studienkennzahl lt. Studienblatt: A 066 815 Studienrichtung lt. Studienblatt: Erdwissenschaften Betreuerin / Betreuer: Ao. Univ.-Prof. Dr. Michael Wagreich Declaration ”I hereby declare that this master’s thesis was authored by myself independently, without use of other sources than indicated. I have explicitly cited all material which has been quoted either literally or by content from the used sources. Further this work was neither submitted in Austria nor abroad for any degree or examination.” Contents Declaration2 1. Introduction8 1.1. Project.................................. 9 1.1.1. Goals............................... 9 1.2. Geographical setting.......................... 10 1.3. Geological setting............................ 12 1.3.1. The Pontides........................... 14 1.3.2. The Pontides in the Cretaceous................ 18 1.3.3. Correlation with relative ages.................. 24 2. Nomenclature 28 3. Methods 29 3.1. ICP-ES and ICP-MS........................... 29 3.2. PXRD.................................. 29 3.3. Heavy mineral extraction........................ 30 4. Results 31 4.1. Mineralogy................................ 31 4.1.1. Powder X-Ray diffraction.................... 31 4.1.2. Thin sections.......................... 33 4.1.3. Mineral Extraction: Dating of minerals............. 34 4.2. Geochemistry.............................. 36 5. Interpretation of the geochemical results 37 5.1. Mobility of elements........................... 37 5.2. Alteration of minerals.......................... 39 5.3. Determining the rock type........................ 41 3 5.4. Discriminating volcanic series..................... 48 5.5. Revealing the tectonic setting...................... 52 5.6. Plotting geochemical element patterns................. 60 5.7. Summary of the geochemical classification.............. 62 6. -
Vitrinite Recycling: Diagnostic Criteria and Reflectance Changes During Weathering and Reburial
Vitrinite recycling: diagnostic criteria and reflectance changes during weathering and reburial. Pierre Nzoussi - Mbassani, Yoann Copard, Jean-Robert Disnar To cite this version: Pierre Nzoussi - Mbassani, Yoann Copard, Jean-Robert Disnar. Vitrinite recycling: diagnostic criteria and reflectance changes during weathering and reburial.. International Journal of Coal Geology, Elsevier, 2005, 61, pp.223-239. 10.1016/j.coal.2004.08.002. hal-00023485 HAL Id: hal-00023485 https://hal-insu.archives-ouvertes.fr/hal-00023485 Submitted on 23 May 2006 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Vitrinite recycling: diagnostic criteria and reflectance changes during weathering and reburial P. Nzoussi-Mbassani, Y. Copard and J.R. Disnar Institut des Sciences de la Terre d'Orléans (ISTO- UMR 6113 du CNRS, Université d'Orléans, Bâtiment de Géosciences, 45067 Orléans cedex 2, France Keywords: Recycled vitrinite; Autochthonous vitrinite; Vitrinite reflectance; Senegalese basin; Ardèche margin; Weathering Abstract The aim of this study was first to review or even identify reliable diagnostic criteria to distinguish recycled and autochthonous vitrinite particles and, second, to examine and try to explain the impact of weathering and reburial on optical changes (reflectance) of recycled material. -
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. -
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. -
Article Discusses the Mechanical Properties of Processes
Adv. Geosci., 45, 73–83, 2018 https://doi.org/10.5194/adgeo-45-73-2018 © Author(s) 2018. This work is distributed under the Creative Commons Attribution 4.0 License. Nanoindentation study of macerals in coals from the Ukrainian Donets Basin Sanja Vranjes1,2, David Misch1, Thomas Schöberl3, Daniel Kiener2, Doris Gross1, and Reinhard F. Sachsenhofer1 1Department Applied Geosciences and Geophysics, Montanuniversitaet Leoben, Leoben, 8700, Austria 2Department Materials Physics, Montanuniversitaet Leoben, Leoben, 8700, Austria 3Erich Schmid Institute of Materials Science, Austrian Academy of Sciences, Leoben, 8700, Austria Correspondence: Sanja Vranjes ([email protected]) Received: 29 May 2018 – Accepted: 26 July 2018 – Published: 7 August 2018 Abstract. This article discusses the mechanical properties of processes. Moreover, it is considered a substantial source macerals in Carboniferous coals from the Ukrainian Donets for methane which not only represents a mining hazard Basin, covering a maturity range from 0.62 to 1.47 %Rr (vit- but can also be utilized by modern unconventional produc- rinite reflectance). The inherent inhomogeneity of geological tion techniques (e.g. coal bed methane; CBM). However, samples requires characterization at the micro-/nanoscale, the producibility of coal bed methane depends on mechan- and hence material parameters, such as hardness H and re- ical properties and fracture behaviour of the hosting coals. duced elastic modulus Er, were obtained from twelve coal Coals are constituted by distinct organic components referred specimens via nanoindentation tests. Different material prop- to as macerals (vitrinite, liptinite, inertinite), and obtaining erties and maturity trends were acquired for the individual the mechanical properties of individual maceral particles is maceral groups (vitrinite, inertinite, liptinite). -
Extractable Organic Material in Fault Zones As a Tool to 2 Investigate Frictional Stress 3 Pratigya J
1 Extractable organic material in fault zones as a tool to 2 investigate frictional stress 3 Pratigya J. Polissar1*, Heather M. Savage2, Emily E. Brodsky3 4 1Lamont-Doherty Earth Observatory of Columbia University, Division of Biology and Paleo 5 Environment, 61 Rt. 9W, Palisades NY, 10964. [email protected], 845-365-8400 6 (office), 845-365-8150 (fax) 7 2Lamont-Doherty Earth Observatory of Columbia University, Division of Seismology, Geology 8 and Tectonophysics, 61 Rt. 9W, Palisades NY, 10964. [email protected], 845-365- 9 8720 (office) 10 3Department of Earth and Planetary Sciences, University of California, Santa Cruz, 1156 High 11 St., Santa Cruz, CA 95060. [email protected], 831-459-1854 (office) 12 *corresponding author 13 Abstract 14 The detection of a frictional heating signature is an attractive, but elusive, way to measure 15 frictional stress on exhumed faults with no evidence of melting. We present a new 16 paleothermometer for fault zones that utilizes the thermal maturity of extractable organic 17 material to determine the maximum frictional heating experienced by the fault. Because there 18 are no retrograde reactions in these organic systems, maximum heating is preserved. We 19 investigate the Punchbowl Fault, an ancient strand of the San Andreas Fault in southern 20 California. According to the methylphenanthrene index for thermal maturity, there is no 21 differential heating between the fault and off-fault samples, indicating that the fault did not get 22 hotter than the surrounding rock during slip. Additionally, the thermal maturity of the rocks falls 23 within the range of heating expected from the bounds on burial depth and time. -
Multi-Phase Tectonic Movements and Their Controls on Coalbed Methane: a Case Study of No
energies Article Multi-Phase Tectonic Movements and Their Controls on Coalbed Methane: A Case Study of No. 9 Coal Seam from Eastern Yunnan, SW China Ming Li 1,2, Bo Jiang 1,2,* , Qi Miao 2,3, Geoff Wang 4, Zhenjiang You 4 and Fengjuan Lan 1,2 1 Key Laboratory of Coalbed Methane Resources and Reservoir Formation Process, Ministry of Education (China University of Mining and Technology), Xuzhou 221116, China; [email protected] (M.L.); [email protected] (F.L.) 2 School of Resources and Earth Science, China University of Mining and Technology, Xuzhou 221116, China; [email protected] 3 No. 198 Coalfield Geology Prospecting Team of Yunnan Province, Kunming 650208, China 4 School of Chemical Engineering, The University of Queensland, Brisbane, QLD 4072, Australia; [email protected] (G.W.); [email protected] (Z.Y.) * Correspondence: [email protected]; Tel.: +86-139-5135-9055 Received: 22 October 2020; Accepted: 16 November 2020; Published: 17 November 2020 Abstract: Multi-phase tectonic movements and complex geological structures limit the exploration and hotspot prediction of coalbed methane (CBM) in structurally complex areas. This scientific problem is still not fully understood, particularly in the Bumu region, Southwest China. The present paper analyses the occurrence characteristics and distribution of CBM based on the comprehensive analysis of CBM data. In combination with the analysis of the regional tectonics setting, geological structure features and tectonic evolution. The control action of multi-phase tectonic movements on CBM occurrence are further discussed. Results show that the Indosinian local deformation, Yanshanian intense deformation, and Himalayan secondary derived deformation formed the current tectonic framework of Enhong synclinorium. -
First Report of Myalinid Bivalves in the Lower Carboniferous of the Hakkari Basin, SE Turkey: Paleoecologic and Paleogeographic Implications
Turkish Journal of Earth Sciences Turkish J Earth Sci (2021) 30: 313-321 http://journals.tubitak.gov.tr/earth/ © TÜBİTAK Research Article doi:10.3906/yer-2010-20 First report of myalinid bivalves in the Lower Carboniferous of the Hakkari Basin, SE Turkey: paleoecologic and paleogeographic implications İzzet HOŞGÖR* Çalık Petrol (Oil and Gas Exploration and Production Company), Ankara, Turkey Received: 28.10.2020 Accepted/Published Online: 22.02.2021 Final Version: 17.05.2021 Abstract: Knowledge of the Late Paleozoic sedimentary history of the northern Gondwana shelf is advanced by new data from the Şort Dere section (Hakkari Basin). Early Carboniferous myalinid bivalves from the Middle East are reported here for the first time. The pre-Permian basement of the Hakkari Basin consists of a Lower Carboniferous sedimentary sequence including the Köprülü and Belek formations. The Köprülü Formation has yielded rich assemblages of vertebrates and invertebrates. Hitherto myalinid bivalves were unknown from this formation; this paper reports the discovery of small and poorly calcified myaliniform shells from two thin beds in the middle part of the Köprülü Formation of the Şort Dere section in the Zap Valley. The morphological characteristics of the specimens, especially the umbonal region with the numerous rounded wrinkles, suggest that it probably belongs to an undescribed species of Selenimyalina Newell, 1942. Based on this record, the state of the art of warm-water myalinid taxa in the Paleotethyan Realm is shortly discussed with a focus on the pteriomorph bivalve faunas within a global scenario for both paleobiogeography and patterns of Gondwana-Laurussia faunal exchange. The new occurrence is one of the most important pteriomorph bivalve records ever made in Southeast Turkey, helping to assist paleogeographic reconstructions of the Paleotethyan paleocontinents. -
The Effect of Substituting Fractions of Imported Coking Coals with Coke Oven Tar on Coal Blend, Carbonization, and Coke Properties by S.S
The effect of substituting fractions of imported coking coals with coke oven tar on coal blend, carbonization, and coke properties by S.S. Makgato*, and R.M.S. Falcon* in the Waterberg (Jeffrey, 2005). In order to produce coke of sufficient strength and quality, the South African iron and steel industries Synopsis import coking coals from countries such as the In this study, coke oven tar additions over a range of 0–8 wt.% were USA, New Zealand, and Australia, to mention evaluated as a possible substitute for imported coal fractions. The just a few. The properties of these imported coke oven tar used was collected from tar decanters in the by- coals are shown in Tables I to IV. products section of the coking plant. The moisture content in the tar Table I shows the origin and properties of varied depending on the residence time and water carryover from the the coking coals, and Table II shows their coke oven tar separators to the storage tanks. Moisture contents of 1 wt.%, 3 wt.%, and 6 wt.% were investigated in order to evaluate the corresponding ultimate analysis and sulphur. effect on coal blend, carbonization, and coke properties. At 6 wt.% Table III shows that poor-coking high- and moisture content with 6 wt.% coke oven tar, although the coke low- volatile coals have low fluidity and a quality improved the yield showed a 4% decrease. On the other hand, narrow plastic range. The thermoplastic 1 wt.% moisture content with coke oven tar of 6 wt.%, increased the properties of coals depend on their rank, but yield by 1% and the coke quality improved.