Origin and Resources of World Oil Shale Deposits - John R
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Coal and Oil: the Dark Monarchs of Global Energy – Understanding Supply and Extraction Patterns and Their Importance for Futur
nam et ipsa scientia potestas est List of Papers This thesis is based on the following papers, which are referred to in the text by their Roman numerals. I Höök, M., Aleklett, K. (2008) A decline rate study of Norwe- gian oil production. Energy Policy, 36(11):4262–4271 II Höök, M., Söderbergh, B., Jakobsson, K., Aleklett, K. (2009) The evolution of giant oil field production behaviour. Natural Resources Research, 18(1):39–56 III Höök, M., Hirsch, R., Aleklett, K. (2009) Giant oil field decline rates and their influence on world oil production. Energy Pol- icy, 37(6):2262–2272 IV Jakobsson, K., Söderbergh, B., Höök, M., Aleklett, K. (2009) How reasonable are oil production scenarios from public agen- cies? Energy Policy, 37(11):4809–4818 V Höök M, Söderbergh, B., Aleklett, K. (2009) Future Danish oil and gas export. Energy, 34(11):1826–1834 VI Aleklett K., Höök, M., Jakobsson, K., Lardelli, M., Snowden, S., Söderbergh, B. (2010) The Peak of the Oil Age - analyzing the world oil production Reference Scenario in World Energy Outlook 2008. Energy Policy, 38(3):1398–1414 VII Höök M, Tang, X., Pang, X., Aleklett K. (2010) Development journey and outlook for the Chinese giant oilfields. Petroleum Development and Exploration, 37(2):237–249 VIII Höök, M., Aleklett, K. (2009) Historical trends in American coal production and a possible future outlook. International Journal of Coal Geology, 78(3):201–216 IX Höök, M., Aleklett, K. (2010) Trends in U.S. recoverable coal supply estimates and future production outlooks. Natural Re- sources Research, 19(3):189–208 X Höök, M., Zittel, W., Schindler, J., Aleklett, K. -
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 -
Oil Shale and Tar Sands
Fundamentals of Materials for Energy and Environmental Sustainability Editors David S. Ginley and David Cahen Oil shale and tar sands James W. Bunger 11 JWBA, Inc., Energy Technology and Engineering, Salt Lake City, UT, USA 11.1 Focus 11.2 Synopsis Tar sands and oil shale are “uncon- Oil shale and tar sands occur in dozens of countries around the world. With in-place ventional” oil resources. Unconven- resources totaling at least 4 trillion barrels (bbl), they exceed the world's remaining tional oil resources are characterized petroleum reserves, which are probably less than 2 trillion bbl. As petroleum becomes by their solid, or near-solid, state harder to produce, oil shale and tar sands are finding economic and thermodynamic under reservoir conditions, which parity with petroleum. Thermodynamic parity, e.g., similarity in the energy cost requires new, and sometimes of producing energy, is a key indicator of economic competitiveness. unproven, technology for their Oil is being produced on a large commercial scale by Canada from tar sands, recovery. For tar sands the hydrocar- and to a lesser extent by Venezuela. The USA now imports well over 2 million barrels bon is a highly viscous bitumen; for of oil per day from Canada, the majority of which is produced from tar sands. oil shale, it is a solid hydrocarbon Production of oil from oil shale is occurring in Estonia, China, and Brazil albeit on called “kerogen.” Unconventional smaller scales. Importantly, the USA is the largest holder of oil-shale resources. oil resources are found in greater For that reason alone, and because of the growing need for imports in the USA, quantities than conventional petrol- oil shale will receive greater development attention as petroleum supplies dwindle. -
Bedrock Geology Glossary from the Roadside Geology of Minnesota, Richard W
Minnesota Bedrock Geology Glossary From the Roadside Geology of Minnesota, Richard W. Ojakangas Sedimentary Rock Types in Minnesota Rocks that formed from the consolidation of loose sediment Conglomerate: A coarse-grained sedimentary rock composed of pebbles, cobbles, or boul- ders set in a fine-grained matrix of silt and sand. Dolostone: A sedimentary rock composed of the mineral dolomite, a calcium magnesium car- bonate. Graywacke: A sedimentary rock made primarily of mud and sand, often deposited by turbidi- ty currents. Iron-formation: A thinly bedded sedimentary rock containing more than 15 percent iron. Limestone: A sedimentary rock composed of calcium carbonate. Mudstone: A sedimentary rock composed of mud. Sandstone: A sedimentary rock made primarily of sand. Shale: A deposit of clay, silt, or mud solidified into more or less a solid rock. Siltstone: A sedimentary rock made primarily of sand. Igneous and Volcanic Rock Types in Minnesota Rocks that solidified from cooling of molten magma Basalt: A black or dark grey volcanic rock that consists mainly of microscopic crystals of pla- gioclase feldspar, pyroxene, and perhaps olivine. Diorite: A plutonic igneous rock intermediate in composition between granite and gabbro. Gabbro: A dark igneous rock consisting mainly of plagioclase and pyroxene in crystals large enough to see with a simple magnifier. Gabbro has the same composition as basalt but contains much larger mineral grains because it cooled at depth over a longer period of time. Granite: An igneous rock composed mostly of orthoclase feldspar and quartz in grains large enough to see without using a magnifier. Most granites also contain mica and amphibole Rhyolite: A felsic (light-colored) volcanic rock, the extrusive equivalent of granite. -
Chemical and Physical Structural Studies on Two Inertinite-Rich Lump
CHEMICAL AND PHYSICAL STRUCTURAL STUDIES ON TWO INERTINITE-RICH LUMP COALS. Nandi Malumbazo A thesis submitted in fulfilment of the requirements for the degree of Doctor of Philoso- phy in the School of Chemical and Metallurgical Engineering at the University of the Witwatersrand. Johannesburg, 2011 DECLARATION I, Nandi Malumbazo, declare that the thesis entitled: “CHEMICAL AND PHYSICAL STRUCTURAL STUDIES ON TWO INER- TINITE-RICH LUMP COALS” is my own work and that all sources I have used or quoted have been indicated and ac- knowledged by means of references. Signature: ……………………………………………………………….. Date:………………………………………………………………………… Page i ABSTRACT ABSTRACT Two Highveld inertinite-rich lump coals were utilized as feed coal samples in order to study their physical, chemical structural and petrographic variations during heat treat- ment in a packed-bed reactor unit combustor. The two feed lump coals were selected as it is claimed that Coal B converts at a slower rate in a commercial coal conversion process when compared to Coal A. The reason for this requires detailed investigation. Chemical structural variations were determined by proximate and coal char CO2 reactiv- ity analysis. Physical structural variations were determined by FTIR, BET adsorption methods, XRD and 13C Solid state NMR analysis. Carbon particle type analysis was con- ducted to determine the petrographic constituents of the reactor generated samples, their maceral associations (microlithotype), and char morphology. This analysis was undertaken with the intention of tracking the carbon conversion and char formation and consumption behaviour of the two coal samples within the reactor. Proximate analysis revealed that Coal A released 10 % more of its volatile matter through the reactor compared to Coal B. -
Evaluating the Extent to Which Wildfire History Can Be Interpreted From
International Journal of Coal Geology 89 (2012) 13–25 Contents lists available at ScienceDirect International Journal of Coal Geology journal homepage: www.elsevier.com/locate/ijcoalgeo Evaluating the extent to which wildfire history can be interpreted from inertinite distribution in coal pillars: An example from the Late Permian, Kuznetsk Basin, Russia V. Hudspith a,⁎, A.C. Scott a, M.E. Collinson a, N. Pronina b, T. Beeley c a Department of Earth Sciences, Royal Holloway University of London, Egham, Surrey TW20 0EX, UK b Geology Department, Moscow State University, Vorobyovy Gory, 119992 Moscow, Russia c Fuels and Combustion, RWE Npower, Windmill Hill Business Park, Whitehill Way, Swindon, Wiltshire SN5 6PB, UK article info abstract Article history: Inertinite (charcoal) distributions in two randomly sampled in situ coal pillars (seams 78 and 88) from the Late Received 15 January 2011 Permian Kuznetsk Basin, Siberia, were analysed using petrographic techniques to determine palaeowildfire Received in revised form 25 July 2011 histories (fire occurrence, type and return interval). In situ coal pillars are judged to be essential for this type of Accepted 29 July 2011 research as they retain information on the original inertinite distribution and maceral clast size ranges which Available online 4 August 2011 can never be obtained from the crushed coals typically used for petrographic analysis. The seams represent an ombrotrophic mire (seam 78) and mire with mire lake (seam 88) depositional Keywords: fi Coal petrography settings but both environments show the same pattern of re history. Charcoal is present in all lithotype Charcoal units in both pillars. Both pillars contain episodic charcoal horizons representing local surface fires within the Mire peat-forming environment, interspersed with frequent regional background fire events (as shown by small Fire return interval scattered inertinite). -
The Destructive Distillation of Pine Sawdust
Scholars' Mine Bachelors Theses Student Theses and Dissertations 1903 The destructive distillation of pine sawdust Frederick Hauenstein Herbert Arno Roesler Follow this and additional works at: https://scholarsmine.mst.edu/bachelors_theses Part of the Mining Engineering Commons Department: Mining Engineering Recommended Citation Hauenstein, Frederick and Roesler, Herbert Arno, "The destructive distillation of pine sawdust" (1903). Bachelors Theses. 238. https://scholarsmine.mst.edu/bachelors_theses/238 This Thesis - Open Access is brought to you for free and open access by Scholars' Mine. It has been accepted for inclusion in Bachelors Theses by an authorized administrator of Scholars' Mine. 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]. FOR THE - ttl ~d IN SUBJECT, ••The Destructive Distillation of P ine Sawdust:• F . HAUENSTEIN AND H . A. ROESLER. CLASS OF 1903. DISTILLATION In pine of the South, the operation of m.ills to immense quanti waste , such and sawdust.. The sawdust especially, is no practical in vast am,ounte; very difficult to the camp .. s :ls to util the be of commercial .. folloWing extraction turpentine .. of the acid th soda and treat- products .. t .. the t.he turpentine to in cells between , or by tissues to alcohol, a soap which a commercial t this would us too the rd:- hydrochloric was through supposition being that it d form & pinene hydro- which produced~ But instead the hydrochl , a dark unl<:nown compound was The fourth experiment, however, brought out a number of possibilities, a few of Which have been worked up. -
Secure Fuels from Domestic Resources ______Profiles of Companies Engaged in Domestic Oil Shale and Tar Sands Resource and Technology Development
5th Edition Secure Fuels from Domestic Resources ______________________________________________________________________________ Profiles of Companies Engaged in Domestic Oil Shale and Tar Sands Resource and Technology Development Prepared by INTEK, Inc. For the U.S. Department of Energy • Office of Petroleum Reserves Naval Petroleum and Oil Shale Reserves Fifth Edition: September 2011 Note to Readers Regarding the Revised Edition (September 2011) This report was originally prepared for the U.S. Department of Energy in June 2007. The report and its contents have since been revised and updated to reflect changes and progress that have occurred in the domestic oil shale and tar sands industries since the first release and to include profiles of additional companies engaged in oil shale and tar sands resource and technology development. Each of the companies profiled in the original report has been extended the opportunity to update its profile to reflect progress, current activities and future plans. Acknowledgements This report was prepared by INTEK, Inc. for the U.S. Department of Energy, Office of Petroleum Reserves, Naval Petroleum and Oil Shale Reserves (DOE/NPOSR) as a part of the AOC Petroleum Support Services, LLC (AOC- PSS) Contract Number DE-FE0000175 (Task 30). Mr. Khosrow Biglarbigi of INTEK, Inc. served as the Project Manager. AOC-PSS and INTEK, Inc. wish to acknowledge the efforts of representatives of the companies that provided information, drafted revised or reviewed company profiles, or addressed technical issues associated with their companies, technologies, and project efforts. Special recognition is also due to those who directly performed the work on this report. Mr. Peter M. Crawford, Director at INTEK, Inc., served as the principal author of the report. -
Hardwood-Distillation Industry
HARDWOOD-DISTILLATION INDUSTRY No. 738 Revised February 1956 41. /0111111 110 111111111111111111 t I 1, UNITED STATES DEPARTMENT OF AGRICULTURE FOREST PRODUCTS LABORATORY FOREST SERVICE MADISON 5, WISCONSIN. In Cooperation with the University of Wisconsin 1 HARDWOOD-DISTILLATION INDUSTRY— By EDWARD BEGLINGER, Chemical Engineer 2 Forest Products Laboratory, — Forest Service U. S. Department of Agriculture The major portion of wood distillation products in the United States is obtained from forest and mill residues, chiefly beech, birch, maple, oak, and ash. Marketing of the natural byproducts recovered has been concerned traditionally with outlets for acetic acid, methanol, and charcoal. Large and lower cost production of acetic acid and methanol from other sources has severely curtailed markets formerly available to the distillation in- dustry, and has in turn created operational conditions generally unfavor- able to many of the smaller and more marginal plants. Increased demand for charcoal, which is recovered in the largest amount as a plant product, now provides a compensating factor for more favorable plant operation. The present hardwood-distillation industry includes six byproduct-recovery plants. With the exception of one smaller plant manufacturing primarily a specialty product, all have modern facilities for direct byproduct re- covery. Changing economic conditions during the past 25 years, including such factors as progressively increasing raw material, equipment, and labor costs, and lack of adequate markets for methanol and acetic acid, have caused the number of plants to be reduced from about 50 in the mid- thirties to the 6 now operating. In addition to this group, a few oven plants formerly practicing full recovery have retained the carbonizing equipment and produce only charcoal. -
A) Conglomerate B) Dolostone C) Siltstone D) Shale 1. Which
1. Which sedimentary rock would be composed of 7. Which process could lead most directly to the particles ranging in size from 0.0004 centimeter to formation of a sedimentary rock? 0.006 centimeter? A) metamorphism of unmelted material A) conglomerate B) dolostone B) slow solidification of molten material C) siltstone D) shale C) sudden upwelling of lava at a mid-ocean ridge 2. Which sedimentary rock could form as a result of D) precipitation of minerals from evaporating evaporation? water A) conglomerate B) sandstone 8. Base your answer to the following question on the C) shale D) limestone diagram below. 3. Limestone is a sedimentary rock which may form as a result of A) melting B) recrystallization C) metamorphism D) biologic processes 4. The dot below is a true scale drawing of the smallest particle found in a sample of cemented sedimentary rock. Which sedimentary rock is shown in the diagram? What is this sedimentary rock? A) conglomerate B) sandstone C) siltstone D) shale A) conglomerate B) sandstone C) siltstone D) shale 9. Which statement about the formation of a rock is best supported by the rock cycle? 5. Which sequence of events occurs in the formation of a sedimentary rock? A) Magma must be weathered before it can change to metamorphic rock. A) B) Sediment must be compacted and cemented before it can change to sedimentary rock. B) C) Sedimentary rock must melt before it can change to metamorphic rock. C) D) Metamorphic rock must melt before it can change to sedimentary rock. D) 6. Which sedimentary rock formed from the compaction and cementation of fragments of the skeletons and shells of sea organisms? A) shale B) gypsum C) limestone D) conglomerate Base your answers to questions 10 and 11 on the diagram below, which is a geologic cross section of an area where a river has exposed a 300-meter cliff of sedimentary rock layers. -
Shale Oil Combustion
INIS-mf—1 5509 University of Jordan J09600040 Faculty of Graduate Studies f’'r*dit.i(c Department of Engineering Mnthrm.'Ucs nncl Physical Science: SHALE OIL COMBUSTION 13 Y MOHAMMED AW WAD ALI AL-DABJJAS SUPERVISOR Dr. MOHAMMED II AMD AN AND Dr. V. II. KHRA1SIIA Submitted in partial fulfillment of Hie requirements for the degree of master of science in mechanical engineering. Faculty of Graduate Studies, University of Jordan. Amman , Jordan May , 1002 tr** POUR QUALITY I ORIGINAL 8 Ns OS u We regret that some of the pages in this report may not be up to the proper legibility standards, even though the best possible copy was used for scanning The Examining CommiU.ee considers this thesis satisfactory and acceptable for Ui award of the Degree of Master of Science in Mechanical Engineering in MAY, 1992. Dr. Mohammed Hamdan Chairman of Conrfhittee Mechanical Engineering Department University of Jordan Dr. Y. II. Khraisha Chemical Engineering Department University of Jordan Dr. S. A. Saved Member of Committee Chemical Engineering Department University of Jordan Dr. M. Ham mad Member of Committee Mechanical Engineering Department University of Jordan Dr. Ali Badran Member of Committee Mechanical Engineering Department University of Jordan To my mother and father I Acknowledgements H. is of my pleasure to express my gratitude to all people who helped me in completing the present work. Special thanks are indebted to my supervisors Dr. M. Hamdan and Dr. Y. Khraisha, whom without their support, encouragement and advice, my work could have been infinitely more difficult . Also special thanks are indebted to my family, especially my father and my mother for their advice and encouragement . -
OPEC in a Shale Oil World
OPEC in a Shale Oil World Mohamed Ramady • Wael Mahdi OPEC in a Shale Oil World Where to Next? Mohamed Ramady Wael Mahdi Department of Finance and Economics Regus, Building 12, Level 4 Trust Tower Visiting Associate Professor OPEC & Middle East Energy King Fahd University of Petroleum Correspondent Bloomberg News and Minerals Manama , Bahrain Dhahran , Saudi Arabia ISBN 978-3-319-22370-4 ISBN 978-3-319-22371-1 (eBook) DOI 10.1007/978-3-319-22371-1 Library of Congress Control Number: 2015946616 Springer Cham Heidelberg New York Dordrecht London © Springer International Publishing Switzerland 2015 This work is subject to copyright. All rights are reserved by the Publisher, whether the whole or part of the material is concerned, specifi cally the rights of translation, reprinting, reuse of illustrations, recitation, broadcasting, reproduction on microfi lms or in any other physical way, and transmission or information storage and retrieval, electronic adaptation, computer software, or by similar or dissimilar methodology now known or hereafter developed. The use of general descriptive names, registered names, trademarks, service marks, etc. in this publication does not imply, even in the absence of a specifi c statement, that such names are exempt from the relevant protective laws and regulations and therefore free for general use. The publisher, the authors and the editors are safe to assume that the advice and information in this book are believed to be true and accurate at the date of publication. Neither the publisher nor the authors or the editors give a warranty, express or implied, with respect to the material contained herein or for any errors or omissions that may have been made.