An Assessment of Oil Shale Technologies (Part 6 Of
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Oil Shale in Jordan 1 2.1
MINISTRY OF ENERGY AND MINERAL RESOURCES Mineral Status and Future Opportunity OIL SHALE Prepared By Dr Jamal Alali Geo. Abdelfattah Abu Salah Dr. Suha M. Yasin Geo. Wasfi Al Omari Edited By Geo. Julia Sahawneh Geo. Marwan Madanat 2014 Oil Shale Ministry of Energy and Mineral Resources, 2014 CONTENTS List of Contents I List of Figures II List of Tables II 1. Introduction 1 2. Geology of Oil Shale in Jordan 1 2.1. Origin and Definition 1 2.2. Mineralogy and Chemistry of Oil Shale 2 2.3. Uses and Industrial Applications of Oil Shale 3 3. Oil Shale Deposits 3 3.1. El-Lajjun Deposit 4 3.2. Sultani Oil Shale Deposit 6 3.3. Attarat Umm Ghudran Oil Shale Deposit 8 3.4. Wadi Maghar Oil Shale Deposit 9 3.5. Khan Az Zabib Deposit 10 3.6. Jurf Ed Darawish Deposit 11 3.7. Siwaqa Deposit 11 3.8. El Hasa Deposit 12 3.9. Eth Thamad/ Madaba Area 4. Summary of Previous Technical Activities 12 5. Mining Aspects 14 5.1. Overburden 14 5.2. Ore Body of the Oil Shale 14 5.3. Reserves 14 5.4. Mining Method 15 6. Oil shale Technologies and Exploitation Worldwide 17 6.1. Crude Oil Production 17 6.2. Power Generation 18 7. Investment Opportunities and Outlook 19 7.1. Crude Oil Production 20 7.2. Direct Combustion 20 8. References 23 I Oil Shale Ministry of Energy and Mineral Resources, 2014 List of Figures Figure (1): Location map of the major oil shale deposits. 5 Figure (2): Oil Shale outcrop in El-Lajjun deposit. -
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. -
New Permian Fauna from Tropical Gondwana
ARTICLE Received 18 Jun 2015 | Accepted 18 Sep 2015 | Published 5 Nov 2015 DOI: 10.1038/ncomms9676 OPEN New Permian fauna from tropical Gondwana Juan C. Cisneros1,2, Claudia Marsicano3, Kenneth D. Angielczyk4, Roger M. H. Smith5,6, Martha Richter7, Jo¨rg Fro¨bisch8,9, Christian F. Kammerer8 & Rudyard W. Sadleir4,10 Terrestrial vertebrates are first known to colonize high-latitude regions during the middle Permian (Guadalupian) about 270 million years ago, following the Pennsylvanian Gondwanan continental glaciation. However, despite over 150 years of study in these areas, the bio- geographic origins of these rich communities of land-dwelling vertebrates remain obscure. Here we report on a new early Permian continental tetrapod fauna from South America in tropical Western Gondwana that sheds new light on patterns of tetrapod distribution. Northeastern Brazil hosted an extensive lacustrine system inhabited by a unique community of temnospondyl amphibians and reptiles that considerably expand the known temporal and geographic ranges of key subgroups. Our findings demonstrate that tetrapod groups common in later Permian and Triassic temperate communities were already present in tropical Gondwana by the early Permian (Cisuralian). This new fauna constitutes a new biogeographic province with North American affinities and clearly demonstrates that tetrapod dispersal into Gondwana was already underway at the beginning of the Permian. 1 Centro de Cieˆncias da Natureza, Universidade Federal do Piauı´, 64049-550 Teresina, Brazil. 2 Programa de Po´s-Graduac¸a˜o em Geocieˆncias, Departamento de Geologia, Universidade Federal de Pernambuco, 50740-533 Recife, Brazil. 3 Departamento de Cs. Geologicas, FCEN, Universidad de Buenos Aires, IDEAN- CONICET, C1428EHA Ciudad Auto´noma de Buenos Aires, Argentina. -
Organic-Rich Shale of the United States and World Land Areas Organic-Rich Shale of the United States and World Land Areas
GEOLOGICAL SURVEY CIRCULAR 523 Organic-Rich Shale of the United States and World Land Areas Organic-Rich Shale of the United States and World Land Areas By Donald C. Duncan and Vernon E. Swanson Geological Survey Circular 523 Washington 7965 United States Department of the Interior STEWART L. UDALL, Secretary Geological Survey William T. Pecora, Director REPRINTED 1966 Free on application to the U.S. Geological Survey, Washington, D.C. 20242 CONTENTS Page Page Abstract----- _ ____________ _ ____ 1 Shale oil resources Continued Introduction- ______________ _ _____ 1 North America Continued Acknowledgments __ ____________ _ 2 United States Continued Previous summaries______________ 2 Shale associated with coal ______ 14 Definitions _______________________ 2 Other shale deposits _ ______ 15 Organic -rich shale _____________ 2 Total shale oil resources.---- 16 Oil shale __ ____ __ ___ __ 3 Other areas in North America ____ 16 Other terms ___________________ 3 Africa-___--__-_-_----_--_----_--- 17 Types of deposits_________________ 4 Total shale oil resources of Potential energy, oil, or gas yield of Africa _______________________ 17 the organic matter in shale ______ 4 Asia _________ _ _____ ___ 19 Status of the shale industry ________ 5 China __________________ _ 19 World production _______________ 5 Israel, Jordan, and Syria _________ 19 Byproducts ____________________ 5 Siberia _________________________ 20 Activities in the United States ____ 5 Thailand and Burma-_____________ 20 Classification of resources ________ 5 Turkey ________ _____ -
Unusual Isotopic Composition of Carbonates from the Irati Formation, Brazil
WAGNER FERRARESI DE GIOVANI 1 ENEAS SALATI F <--entro de Energia Nuclear na Agricultura, ESALQ-USP, Piracicaba, Brazil ONILDO J. MARINI Departmento de Geocièncias, Universidade de Brasilia, Brasilia, Brazil IRVING FRIEDMAN U.S. Geological Survey, Denver, Colorado 80225 Unusual Isotopic Composition of Carbonates from the Irati Formation, Brazil ABSTRACT easily identifiable lithology makes it a good were collected at the town of Sao Mateus do marker horizon. The formation was as- Sul. Near this outcrop, 5 more samples (Fig. Samples of dolomite and limestone from signed by MacGregor (in Mendes, 1967, p. 1, loc. II; Table 3, SMS samples) of the the Permian Irati Formation collected in the 139) to the Permian, in his study of the fossil intermediate zone were collected. Paraná Basin, southern Brazil, have been reptile Mesosaurus brasiliensis. Nine samples were collected from the analyzed for 8Cia and SO18. The 8C'3 ranges Carbon and oxygen isotopic composi- state of Santa Catarina: 5 from Papanduva from +18.3°/oo to -17.4°/oo PDB, while the tions have been used to differentiate (Fig. 1, loc. Ill; Table 4, P samples) and 4 SO18 ranges from -2.6°/oo to -12.5°/oo limestones deposited in marine environ- from Correia Pinto (Fig. 1, loc. IV; Table 4, PDB. In some quarries where the exposures ments from those originating from fresh CP samples). are especially good, a large variation in 8C13 water. For example, Clayton and Degens From the state of Rio Grande do Sul, 5 can be found. The lower, dense gray (1959) have shown that in 30 samples of samples were collected in Pantano Grande dolomite has light carbon ( —17to +2.6%o), limestone (mainly Pennsylvanian) the 8C13 (Table 5), in an outcrop of very poor quality, whereas the overlying intermediate zone of differs for samples from the two environ- containing clayey soil formed by decomposi- interbedded organic-rich shale and black ments. -
HISTORY of WESTERN OIL SHALE HISTORY of WESTERN OIL SHALE
/ _... i';C4 - SHELF , Historyof Western Oil Shale Paul L. Russell . " The Center for Professional Advancement Paul Russell received his degree from the University of Arizona. After working for Industry for five years, he began his involvement with oil shale in 1948 when he joined the U.S. Bureau of Mines and was assigned to Rifle, Colorado, to work at Anvil Points. During the middle fifties, he was assigned to the Atomic Energy Com mission to study the extraction of ura nium from the Chattanooga Shales in Tennessee. He became Research Director of the U.S. Bureau ofMines in 1967 and served in this capacity until he retired in 1979. During these years his involvement with oil shale intensified. Currently, he is an engineering consultant. ISBN: 0-86563-000-3 ,._-------_._.. V.D.ALLRED 6016 SOUTH BANNOCK LI7TLETON. COLO. 80120 ....~ ...........~..... This compelling history spans 65 years of western oil shale development from its begin ning to the present day. These were the years in which most of the present-day retorting pro cesses were invented and devel oped,leading to present studies of in-situ retorting, and to the resumption of leasing of fed eral oil shale lands. The many excellent illustra tions and contemporary photo graphs in themselves provide a pictorial record of an era when the United States was "wild over oil"-an era when Gov ernment estimates of billions of barrels of oil in western oil shales were used to advan tage for questionable-if not fraudulent-stock promotions designed to raise capital for development, or to fatten the promoters' pockets. -
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. -
IV. Northern South America EIA/ARI World Shale Gas and Shale Oil Resource Assessment
IV. Northern South America EIA/ARI World Shale Gas and Shale Oil Resource Assessment IV. NORTHERN SOUTH AMERICA SUMMARY Northern South America has prospective shale gas and shale oil potential within marine- deposited Cretaceous shale formations in three main basins: the Middle Magdalena Valley and Llanos basins of Colombia, and the Maracaibo/Catatumbo basins of Venezuela and Colombia, Figure IV-1. The organic-rich Cretaceous shales (La Luna, Capacho, and Gacheta) sourced much of the conventional gas and oil produced in Colombia and western Venezuela, and are similar in age to the Eagle Ford and Niobrara shale plays in the USA. Ecopetrol, ConocoPhillips, ExxonMobil, Shell, and others have initiated shale exploration in Colombia. Colombia’s petroleum fiscal regime is considered attractive to foreign investment. Figure IV-1: Prospective Shale Basins of Northern South America Source: ARI 2013 May 17, 2013 IV-1 IV. Northern South America EIA/ARI World Shale Gas and Shale Oil Resource Assessment For the current EIA/ARI assessment, the Maracaibo-Catatumbo Basin was re-evaluated while new shale resource assessments were undertaken on the Middle Magdalena Valley and Llanos basins. Technically recoverable resources (TRR) of shale gas and shale oil in northern South America are estimated at approximately 222 Tcf and 20.2 billion bbl, Tables IV-1 and IV- 2. Colombia accounts for 6.8 billion barrels and 55 Tcf of risked TRR, while western Venezuela has 13.4 billion barrels and 167 Tcf. Eastern Venezuela may have additional potential but was not assessed due to lack of data. Colombia’s first publicly disclosed shale well logged 230 ft of over-pressured La Luna shale with average 14% porosity. -
Analyzing of Formation Evaluation of the Unconventional Upper-Safa Formation, Western Desert, Egypt
Petroleum & Petrochemical Engineering Journal ISSN: 2578-4846 Analyzing of Formation Evaluation of the Unconventional Upper-Safa Formation, Western Desert, Egypt Fathy Omran MA1,2,* and Hassane T2 Research Article 1Norwegian University of Science and Technology, Norway Volume 2 Issue 7 Received Date: September 14, 2018 2The British University in Egypt (BUE), Cairo, Egypt Published Date: November 05, 2018 *Corresponding author: Mohamed Ahmed Fathy Omran, Norwegian University of DOI: 10.23880/ppej-16000175 Science and Technology, Norway, Tel: +4746217833; Email: [email protected]. Abstract Unconventional reservoirs can add huge amounts of additional energy to our world resources bases like organic shale in terms of Shale gas, shale oil, tight gas and coal-bed methane. These reservoirs can transform the world global energy market through advances in reservoir characterization, drilling, and completion technologies. Reservoir characterization and properties have great influences on the exploration and development processes, it is not through a single discipline that can provide a fulfill description of the reservoir characteristics especially for unconventional reservoirs. Moreover, unconventional sources can be defined by their difference of intrinsic of their geological sittings, origins, and tapping mechanisms, thus having different methodologies for exploration, production, and development methods. Therefore, it is very important to well express and identify the necessary parameters for unconventional characterization of these reservoirs for defining reservoir rock and fluid properties in terms of total organic carbon content, gas adsorption, level of maturity, grains surface roughness, original fluids in place, and etc. Hence there are many developed correlations and methods to get these parameters that can define each one of them, but most of them are not correlated with each other. -
U.S. Fossil Fuel Resources: Terminology, Reporting, and Summary
U.S. Fossil Fuel Resources: Terminology, Reporting, and Summary Carl E. Behrens Specialist in Energy Policy Michael Ratner Specialist in Energy Policy Carol Glover Information Research Specialist December 28, 2011 Congressional Research Service 7-5700 www.crs.gov R40872 CRS Report for Congress Prepared for Members and Committees of Congress U.S. Fossil Fuel Resources: Terminology, Reporting, and Summary Summary Discussions of U.S. and global energy supply refer to oil, natural gas, and coal using several terms that may be unfamiliar to some. The terms used to describe different types of fossil fuels have technically precise definitions, and misunderstanding or misuse of these terms may lead to errors and confusion in estimating energy available or making comparisons among fuels, regions, or nations. Fossil fuels are categorized, classified, and named using a number of variables. Naturally occurring deposits of any material, whether it is fossil fuels, gold, or timber, comprise a broad spectrum of concentration, quality, and accessibility (geologic, technical, and cultural). Terminology is adopted to reflect those characteristics. For oil and natural gas, a major distinction in measuring quantities of energy commodities is made between proved reserves and undiscovered resources. Proved reserves are those amounts of oil, natural gas, or coal that have been discovered and defined, typically by drilling wells or other exploratory measures, and which can be economically recovered. In the United States, proved reserves are typically measured by private companies, who report their findings to the Energy Information Administration, and also to the Securities and Exchange Commission because they are considered capital assets. In addition to the volumes of proved reserves are deposits of oil and gas that have not yet been discovered, which are called undiscovered resources. -
The Permian Tiaraju Bivalve Assemblage
DOI: 10.1590/2317‑4889201720170013 ARTICLE The Permian Tiaraju bivalve assemblage, Passa Dois Group, southern Brazil: biostratigraphic and paleobiogeographic significance Assembleia de bivalves permianos de Tiaraju, Grupo Passa Dois, sul do Brasil: significado bioestratigráfico e paleobiogeográfico Marcello Guimarães Simões1*, Juliana Machado David2, Luiz Eduardo Anelli2, Carla Klein3, Suzana Aparecida Matos1, Vitor Bonatto Guerrini4, Lucas Veríssimo Warren4 ABSTRACT: Permian bivalves of the Paraná Basin evolved in a large RESUMO: Bivalves permianos da Bacia do Paraná evoluíram em inland sea, under conditions of extreme isolation and environmental um imenso mar interior, sob condições de extremo isolamento e estresse stress. Although known since 1918, its evolutionary history is still obs‑ ambiental. Embora conhecidos desde 1918, a história evolutiva desses cure due to the incomplete and biased information on faunal com‑ bivalves é ainda obscurecida pelo conhecimento incompleto e enviesado position and stratigraphic distribution of various assemblages. Hence, sobre a composição faunística e a distribuição estratigráfica de várias the description of the Tiaraju assemblage, the only known bivalve oc‑ assembleias. Portanto, a descrição da assembleia de Tiaraju, a única currence in the Passa Dois Group from the southernmost Brazil, adds conhecida no Grupo Passa Dois do sul do Brasil, contribui com novas new key information on the composition, biocorrelation and age of informações‑chave sobre a composição, biocorrelação e idade dessa this unique molluscan fauna. Terraia falconeri, Cowperesia emerita, Hol‑ fauna de moluscos únicos. Terraia falconeri, Cowperesia emerita, dhausiella elongata, and Terraia altissima were recorded and described. Holdhausiella elongata e Terraia altissima foram registradas e descritas. T. falconeri is the commonest species, followed by C. -
Tooth Microstructure of the Early Permian Aquatic Predator Stereosternum Tumidum
Tooth microstructure of the Early Permian aquatic predator Stereosternum tumidum FLÁVIO A. PRETTO, SÉRGIO F. CABREIRA, and CESAR L. SCHULTZ Pretto, F.A., Cabreira, S.F., and Schultz, C.L. 2014. Tooth microstructure of the Early Permian aquatic predator Stereosternum tumidum. Acta Palaeontologica Polonica 59 (1): 125–133. A histological investigation of the feeding apparatus of a Stereosternum specimen revealed a great number of adaptations in the structure and insertion of teeth, to deal with breakage risks. The tooth wall is composed of different layers of dentine, varying in orientation and composition. This mixed arrangement may have increased tooth resistance to lateral tension. The tooth insertion also involves more than one mechanism. The teeth are located inside shallow tooth sockets and are held in place by a tripartite periodontium (composed of alveolar bone, cementum and possibly soft periodontal tissue) and accessory structures, here termed anchorage trabeculae (mainly composed of cementum). Fully grown teeth are ankylosed to the bottom of the tooth socket. The recognition of alveolar bone and cementum (and the possible pres- ence of a soft periodontal ligament) reinforces the idea that these tissues were widespread among Amniota, not being exclusive to mammals and archosaurs. The adaptations identified here reinforce the hypothesis that Stereosternum was an active aquatic predator. Key words: Amniota, Mesosauridae, Stereosternum tumidum, histology, tripartite periodontium, Permian. Flávio A. Pretto [[email protected]] and Cesar L. Schultz [[email protected]], Universidade Federal do Rio Grande do Sul, Instituto de Geociências, Setor de Paleovertebrados, Av. Bento Gonçalves, 9500 – Bloco J, Pré- dio 43127, Campus do Vale, Agronomia−Porto Alegre, Rio Grande do Sul, Brazil, CEP 91540-000; Sérgio F.