Dalmat Carbonization and Energy System
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Studies in Organic Geochemistry"
A Thesis entitled "STUDIES IN ORGANIC GEOCHEMISTRY" submitted to the UNIVERSITY OF GLASGOW in part fulfilment of the requirements for admittance to the degree of DOCTOR OF PHILOSOPHY in the Faculty of Science by JAMES RANKIN MAXWELL, B.Sc. Chemistry Department April, 1967 ProQuest Number: 11011805 All rights reserved INFORMATION TO ALL USERS The quality of this reproduction is dependent upon the quality of the copy submitted. In the unlikely event that the author did not send a com plete manuscript and there are missing pages, these will be noted. Also, if material had to be removed, a note will indicate the deletion. uest ProQuest 11011805 Published by ProQuest LLC(2018). Copyright of the Dissertation is held by the Author. All rights reserved. This work is protected against unauthorized copying under Title 17, United States C ode Microform Edition © ProQuest LLC. ProQuest LLC. 789 East Eisenhower Parkway P.O. Box 1346 Ann Arbor, Ml 48106- 1346 To t:vv rorontn , v/if^ and dna^ktor, I wish to express my gratitude to Drs. G.Eglinton and J.D, Loudon for their close interest and guidance throughout the work of this thesis. My appreciation is also due to Dr. A.G, Douglas, whose assistance at all times proved to he invaluable. I would also like to thank Miss F. Greene and Miss T.Devit for technical assistance, my colleagues of the Organic Geochemistry Unit and Dr. A, McCormick for their advice and help, Mr, J.M.L. Cameron and his staff for the micro-analyses, Mrs. F. Lawrie and Miss A. -
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. -
Origin and Resources of World Oil Shale Deposits - John R
COAL, OIL SHALE, NATURAL BITUMEN, HEAVY OIL AND PEAT – Vol. II - Origin and Resources of World Oil Shale Deposits - John R. Dyni ORIGIN AND RESOURCES OF WORLD OIL SHALE DEPOSITS John R. Dyni US Geological Survey, Denver, USA Keywords: Algae, Alum Shale, Australia, bacteria, bitumen, bituminite, Botryococcus, Brazil, Canada, cannel coal, China, depositional environments, destructive distillation, Devonian oil shale, Estonia, Fischer assay, Fushun deposit, Green River Formation, hydroretorting, Iratí Formation, Israel, Jordan, kukersite, lamosite, Maoming deposit, marinite, metals, mineralogy, oil shale, origin of oil shale, types of oil shale, organic matter, retort, Russia, solid hydrocarbons, sulfate reduction, Sweden, tasmanite, Tasmanites, thermal maturity, torbanite, uranium, world resources. Contents 1. Introduction 2. Definition of Oil Shale 3. Origin of Organic Matter 4. Oil Shale Types 5. Thermal Maturity 6. Recoverable Resources 7. Determining the Grade of Oil Shale 8. Resource Evaluation 9. Descriptions of Selected Deposits 9.1 Australia 9.2 Brazil 9.2.1 Paraiba Valley 9.2.2 Irati Formation 9.3 Canada 9.4 China 9.4.1 Fushun 9.4.2 Maoming 9.5 Estonia 9.6 Israel 9.7 Jordan 9.8 Russia 9.9 SwedenUNESCO – EOLSS 9.10 United States 9.10.1 Green RiverSAMPLE Formation CHAPTERS 9.10.2 Eastern Devonian Oil Shale 10. World Resources 11. Future of Oil Shale Acknowledgments Glossary Bibliography Biographical Sketch Summary ©Encyclopedia of Life Support Systems (EOLSS) COAL, OIL SHALE, NATURAL BITUMEN, HEAVY OIL AND PEAT – Vol. II - Origin and Resources of World Oil Shale Deposits - John R. Dyni Oil shale is a fine-grained organic-rich sedimentary rock that can produce substantial amounts of oil and combustible gas upon destructive distillation. -
Mineralogy and Organic Petrology of Oil Shales in the Sangkarewang Formation, Ombilin Basin, West Sumatra, Indonesia
Mineralogy and Organic Petrology of Oil Shales in The Sangkarewang Formation, Ombilin Basin, West Sumatra, Indonesia Fatimah Student no: 3008511 SCHOOL OF BIOLOGICAL EARTH AND ENVIRONMENTAL SCIENCES UNIVERSITY OF NEW SOUTH WALES 2009 ABSTRACT The Ombilin Basin, which lies in Sumatra Island, is one of the Tertiary basins in Indonesia. This basin contains a wide variety of rock units, from pre-Tertiary to Quaternary in age. Significant oil shale deposits occur in the Sangkarewang Formation which was deposited during Paleocene-Eocene time. Several analyses have been carried out namely, XRD, XRF, carbon and sulphur determination, thin section petrology, polished section petrology as well as Fischer assay. These were intended to determine the inorganic and organic constituents of the Sangkarewang oil shale. Inorganic constituents of the Sangkarewang oil shale consist mainly of quartz, feldspar, carbonates and a range of clay minerals, together in some cases with minor proportions of sulphides, evaporites and zeolites. The organic matter in the oil shales of the sequence is dominated by liptinite macerals, particularly alginite (mainly lamalginite) and sporinite. Cutinite also occurs in some samples, along with resinite and traces of bituminite. The dominance of lamalginite in the liptinite components suggests that the material can be described as a lamosite. Samples from the Sangkarewang Formation have vitrinite reflectance values ranging between 0.37% and 0.55%. These are markedly lower than the vitrinite reflectance for coal from the overlying Sawahlunto Formation (0.68%), possibly due to suppression associated with the abundant liptinite in the oil shales. Fischer assay data on outcrop samples indicate that the oil yield is related to the organic carbon content. -
KIER's 5-BARREL STILL 'A Venerable Industrial Relic" W
KIER'S 5-BARREL STILL 'A Venerable Industrial Relic" W. K. Cadman okof toclax,today, completely 5Ulroun6e<1surrounded byox petroleum and2n6 en- joying the many services derived from it, may look upon this „„ ~ People ~*~^*.-.~n rt « n *..~ natural«*#>4-«««.r*1 mineral~~.^«-..rw~.r>1 resource as something4.U.'«» new. However,TLT^ the4-i*A record shows that petroleum, in its various forms, belongs to a group of minerals that have excited the curiosity and the interest of mankind from a time even before the dawn of written human history. In this group are found gold and copper, whose first use antedates the earliest records of civilization; the more common metals, such as iron, tin, and bronze, all known to man prior to 3500 B.C. Petroleum has been found in many widely separated places throughout the globe. It has appeared in the form of heavy tar or pitch deposited in sedimentary formations or on the surface of the earth, or found flowing from cracks or crevices in rocks, as oil springs or seeps. Ithas attracted mankind by its smell, its strange oiliness, and by the ease with which it burns. On the basis of use, the long history of petroleum can be logi- cally and conveniently divided into two main periods, namely: the Crude Petroleum Era, and the Refined Petroleum Era. The Crude Petroleum Era includes a segment of time perhaps as long as 8000 years, and is constantly being projected further into the past by research, especially in the field of archeology. On the other hand, the Refined Era, in comparison, is just an infant, whose present age is but five years past the century mark. -
Structural Characterization of Organic Matter in Oil Shales Using Multiple Nuclear Magnetic Resonance Spectroscopic Techniques
Old Dominion University ODU Digital Commons Chemistry & Biochemistry Theses & Dissertations Chemistry & Biochemistry Summer 8-2020 Structural Characterization of Organic Matter in Oil Shales Using Multiple Nuclear Magnetic Resonance Spectroscopic Techniques Wenying Chu Old Dominion University, [email protected] Follow this and additional works at: https://digitalcommons.odu.edu/chemistry_etds Part of the Analytical Chemistry Commons, and the Geochemistry Commons Recommended Citation Chu, Wenying. "Structural Characterization of Organic Matter in Oil Shales Using Multiple Nuclear Magnetic Resonance Spectroscopic Techniques" (2020). Doctor of Philosophy (PhD), Dissertation, Chemistry & Biochemistry, Old Dominion University, DOI: 10.25777/1bq4-6j64 https://digitalcommons.odu.edu/chemistry_etds/51 This Dissertation is brought to you for free and open access by the Chemistry & Biochemistry at ODU Digital Commons. It has been accepted for inclusion in Chemistry & Biochemistry Theses & Dissertations by an authorized administrator of ODU Digital Commons. For more information, please contact [email protected]. STRUCTURAL CHARACTERIZATION OF ORGANIC MATTER IN OIL SHALES USING MULTIPLE NUCLEAR MAGNETIC RESONANCE SPECTROSCOPIC TECHNIQUES by Wenying Chu B.S. June 2008, Huazhong Agricultural University, China A Dissertation Submitted to the Faculty of Old Dominion University in Partial Fulfillment of the Requirements for the Degree of DOCTOR OF PHILOSOPHY CHEMISTRY OLD DOMINION UNIVERSITY August 2020 Approved by: Jingdong Mao (Director) Guijun Wang (Member) John R. Donat (Member) Lesley H. Greene (Member) Shizhi Qian (Member) ABSTRACT STRUCTURAL CHARACTERIZATION OF ORGANIC MATTER IN OIL SHALES USING MULTIPLE NUCLEAR MAGNETIC RESONANCE SPECTROSCOPIC TECHNIQUES Wenying Chu Old Dominion University, 2020 Director: Dr. Jingdong Mao Oil shale is a promising source of hydrocarbon fuel that is distributed throughout the world. -
Developing a Rare and Valuable Torbanite Resource in Central Queensland &
ASX ANNOUNCEMENT 06 NOVEMBER 2020 GREENVALE MINING LTD INVESTOR WEBINAR • Greenvale Mining Ltd to present at Resources Rising Stars 2020 Investor Conference • Presentation scheduled for Wednesday 11th November 2020 at 8:10AM WST / 11:10AM AEDT Greenvale Mining Ltd (ASX: GRV) is pleased to advise it will present an investor briefing at the Resources Rising Stars 2020 Investor Forum on 11th November 2020. The Company invites investors to view a live streamed video presentation with Executive Director, Neil Biddle, with the opportunity to submit questions for Mr. Biddle to answer following the presentation. Investors can register online to watch the presentation via the following link: https://www.bigmarker.com/series/Resources-Rising-Stars-2020-Investor- Conference/series_summit More information can be found at: https://www.resourcesrisingstars.com.au/events/rrs-two-day-investor-webinar A copy of the Presentation to be made on 11 November 2020 is enclosed. This presentation has been approved by the Board for release. Alan Boys Company Secretary Greenvale Mining Limited I ABN 54 000 743 555 130 Stirling Highway, North Fremantle WA 6159 I Locked Bag 4, North Fremantle WA 6159 t:+61 2 8046 2799 | e: [email protected] | www.greenvalemining.com RRS Conference Gold Coast November 10-11 2020 DEVELOPING A RARE AND VALUABLE TORBANITE RESOURCE IN CENTRAL QUEENSLAND & EXPLORING FOR LARGE SCALE IOCG DEPOSITS IN THE BARKLEY TABLELAND NORTHERN TERRITORY PRESENTED BY: NEIL BIDDLE (EXECUTIVE DIRECTOR) DISCLAIMER This document and all other information (whether in writing or otherwise) which may be made available or part thereof does not: 1. Contain all information that investors and their professional advisers would require to make an informed assessment of the following: a) a) assets and liabilities, financial position and performance, profits and losses and prospects of the Company; and b) b) rights and liabilities attaching to the Company's securities. -
A TECHNICAL STUDY of TRANSVAAL TORBANITE .* by S
V o l . 27. No. 208. F e b r u a r y 1941. A TECHNICAL STUDY OF TRANSVAAL TORBANITE .* By S. L. N eppe, B.Sc.(Eng.), A.I.C., A.M.Inst.Pet. S e c tio n A. Introduction. T h e author has taken the opportunity of carrying out a survey of Trans vaal torbanite in a more systematized manner than has hitherto been attempted. Fortunately access to the requisite number of samples of varying character was readily available from the vast deposits of the South African Torbanite Mining and Refining Co., Ltd. There are two main classes of Transvaal torbanite which have been con sidered by the author—viz., the richer-quality torbanite as generally obtained from the Troye or Carlis’ Adits, and the poorer class as mostly obtained from the Giesecke Adit of the well-known Ermelo deposits. This differentiation is necessary in order to emphasize the wide variation in the composition of torbanites. Table III (Section B—Experimental), giving analyses of a large number of samples of varying composition, has been compiled with a view to classi fication according to “ fuel ratio ” —i.e., ratio of organic volatiles to fixed carbon. Generally speaking, the grade of torbanite is related to its ash content. Three classes of mineral matter may be included in the ash value of the torbanite :— (а) Inherent mineral matter which is so intimately mixed with the torbanite as to preclude its separation by ordinary means. (б) Adventitious mineral matter, such as pyrites, nodules, shale, etc., which is deposited and mixed with the torbanite in such a way that its separation by ordinary means is quite feasible. -
Geology and Resources of Some World Oil Shale Deposits 195 of the World
Oil Shale, 2003, Vol. 20, No. 3 ISSN 0208-189X pp. 193-252 © 2003 Estonian Academy Publishers GEOLOGY AND RESOURCES OF SOME WORLD OIL-SHALE DEPOSITS* J. R. DYNI** U.S. Geological Survey Box 25046, Mail Stop 939 Denver Federal Center, Colorado 80225 Oil-shale deposits are found in many parts of the world. They range in age from Cambrian to Tertiary and were formed in a variety of marine, continen- tal, and lacustine depositional environments. The largest known deposit is the Green River oil shale in western United States. It contains an estimated 215 billion tons of in-place shale oil (1.5 trillion U.S. barrels). Total resources of a selected group of oil-shale deposits in 33 countries is estimated at 411 billion tons of in-place shale oil which is equivalent to 2.9 trillion U.S. barrels of shale oil. This figure is very conservative because several deposits mentioned herein have not been explored sufficiently to make accurate estimates and other deposits were not included in this survey. Introduction Oil shale is commonly defined as a fine-grained sedimentary rock containing organic matter that will yield substantial amounts of oil and combustible gas upon destructive distillation. Underlying most definitions of oil shale is its potential for the economic recovery of energy including shale oil, combusti- ble gas, heat, and byproducts. A deposit of oil shale having economic poten- tial is usually one that is at or near enough to the surface to be developed by open-cast or conventional underground mining or by in situ methods. -
Geology and Resources of Some World Oil-Shale Deposits
Geology and Resources of Some World Oil-Shale Deposits Scientific Investigations Report 2005–5294 U.S. Department of the Interior U.S. Geological Survey Cover. Left: New Paraho Co. experimental oil shale retort in the Piceance Creek Basin a few miles west of Rifle, Colorado. Top right: Photo of large specimen of Green River oil shale interbedded with gray layers of volcanic tuff from the Mahogany zone in the Piceance Creek Basin, Colorado. This specimen is on display at the museum of the Geological Survey of Japan. Bottom right: Block diagram of the oil shale resources in the Mahogany zone in about 1,100 square miles in the eastern part of the Uinta Basin, Utah. The vertical scale is in thousands of barrels of in-place shale oil per acre and the horizontal scales are in UTM coordinates. Illustration published as figure 17 in U.S. Geological Survey Open-File Report 91-0285. Geology and Resources of Some World Oil-Shale Deposits By John R. Dyni Scientific Investigations Report 2005–5294 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior Dirk Kempthorne, Secretary U.S. Geological Survey P. Patrick Leahy, Acting Director U.S. Geological Survey, Reston, Virginia: 2006 Posted onlline June 2006 Version 1.0 This publication is only available online at: World Wide Web: http://www.usgs.gov/sir/2006/5294 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 Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. -
Classification of Torbanite and Cannel Coal. I. Insights from Petrographic Analysis of Density Fractions. International Journal of Coal Geology 38:161-202
Montclair State University Montclair State University Digital Commons Department of Earth and Environmental Studies Faculty Scholarship and Creative Works Department of Earth and Environmental Studies 1999 Classification of orbaniteT and Cannel Coal. I. Insights from Petrographic Analysis of Density Fractions. Zhiwen Han Southern Illinois University Carbondale Michael A. Kruge Montclair State University, [email protected] John C. Crelling Southern Illinois University Carbondale David F. Bensley Southern Illinois University Carbondale Follow this and additional works at: https://digitalcommons.montclair.edu/earth-environ-studies-facpubs Part of the Geochemistry Commons, Geology Commons, Paleontology Commons, and the Sedimentology Commons MSU Digital Commons Citation Han, Zhiwen; Kruge, Michael A.; Crelling, John C.; and Bensley, David F., "Classification of orbaniteT and Cannel Coal. I. Insights from Petrographic Analysis of Density Fractions." (1999). Department of Earth and Environmental Studies Faculty Scholarship and Creative Works. 633. https://digitalcommons.montclair.edu/earth-environ-studies-facpubs/633 This Article is brought to you for free and open access by the Department of Earth and Environmental Studies at Montclair State University Digital Commons. It has been accepted for inclusion in Department of Earth and Environmental Studies Faculty Scholarship and Creative Works by an authorized administrator of Montclair State University Digital Commons. For more information, please contact [email protected]. PREPRINT: Han Z., Kruge M. A., Crelling J. C., and Bensley D. F. (1999) Classification of torbanite and cannel coal. I. Insights from petrographic analysis of density fractions. International Journal of Coal Geology 38:161-202. https://doi.org/10.1016/S0166-5162(98)00013-5 Classification of torbanite and cannel coal. -
Industrial Revolution Days Agricultural Revolution
Pre- industrial revolution days Farming was the first main occupation of majority of the people People lived closed to their food sources All commodities were local. Production of goods was for use rather than profit. Weapons which kill few people at once. Life expectancy – 35 years. Travel and communication between far off places extremely slow. The industrial revolution begins in Britain In 17th century Britain, the beginnings of an agricultural revolution would eventually lead to an industrial revolution, changing the country – and the world – forever. Agricultural Revolution The Agricultural Revolution was a period of technological improvement and increased crop productivity that occurred during the 18th and early 19th centuries in Europe. Historians have often labelled the first Agricultural Revolution (which took place around 10,000 B.C.) as the period of transition from a hunting-and-gathering society to one based on stationary farming. During the 18th century, another Agricultural Revolution took place when European agriculture shifted from the techniques of the past. New patterns of crop rotation and livestock utilization paved the way for better crop yields, a greater diversity of wheat and vegetables and the ability to support more livestock. These changes impacted society as the population became better nourished and healthier. The Enclosure Acts, passed in Great Britain, allowed wealthy lords to purchase public fields and push out small-scale farmers, causing a migration of men looking for wage labour in cities. The Agricultural Revolution began in Great Britain around the turn of the 18th century. Several major events, which will be discussed in more detail later, include: 1.