British Columbia Coal Industry Overview 2020
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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. -
Coal Studies ELK VALLEY COALFIELD, NORTH HALF (825102, 07, 10, 11) by R
Coal Studies ELK VALLEY COALFIELD, NORTH HALF (825102, 07, 10, 11) By R. J. Morris and D. A. Grieve KEYWORDS: Coalgeology, Elk Valley coalfield, Mount the area is formed by Hmretta andBritt creeks, and is Veits, Mount Tuxford, HenretlaRidge, Bourgeau thrust, coal immediately north of the Fc'rdingRiver operations of Fording rank, Elk River syncline, Alexander Creek syncline. Coal Ltd.(Figure 4-1-1).The northernboundary is the British Columbia - Alberta border. The map area includes INTRODUCTION the upper Elk Valley and a portion of the upper Fording Detailed geological mapping and sampling of the north Valley. half of theElk Valley coalfieldbegan in 1986 and were Most of the area is Crown land and includes three c:od completed in 1987. The end poduct, a preliminary map at a properties. The most southerly comprises the north end ol'tbe scale of 1: IO OOO, will extend available map coverage in the Fording Coal Ltd. Fording River property. Adjacent to the coalfield north from the areas covered by Preliminary Maps north is theElk River property, in which Fording Coal 51 and 60 (Figure 4-l-l),which in turn expanded previous currently holds aSO-per-cent interest. Coal rights to the most coverage in the adjacent Crowsnest coalfield (Preliminary northerly property, formerly known as tlne Vincent option, Maps 24, 27,31 and 42). are reserved to the Crown Work in 1986 (Grieve, 1987) was mainly concentrated in Exploration history of the Weary Ridge - Bleasdell Creek the Weary Ridge ~ Bleasdell Creek area. Themore extensive area was summarized by Grieve (1987). Of the remailing 1987 field program was completed by R.J. -
Proposal for Development of Dry Coking/Coal
Development of Coking/Coal Gasification Concept to Use Indiana Coal for the Production of Metallurgical Coke, Liquid Transportation Fuels, Fertilizer, and Bulk Electric Power Phase II Final Report September 30, 2007 Submitted by Robert Kramer, Ph.D. Director, Energy Efficiency and Reliability Center Purdue University Calumet Table of Contents Page Executive Summary ………………………………………………..…………… 3 List of Figures …………………………………………………………………… 5 List of Tables ……………………………………………………………………. 6 Introduction ……………………………………………………………………… 7 Process Description ……………………………………………………………. 11 Importance to Indiana Coal Use ……………………………………………… 36 Relevance to Previous Studies ………………………………………………. 40 Policy, Scientific and Technical Barriers …………………………………….. 49 Conclusion ………………………………………………………………………. 50 Appendix ………………………………………………………………………… 52 2 Executive Summary Coke is a solid carbon fuel and carbon source produced from coal that is used to melt and reduce iron ore. Although coke is an absolutely essential part of iron making and foundry processes, currently there is a shortfall of 5.5 million tons of coke per year in the United States. The shortfall has resulted in increased imports and drastic increases in coke prices and market volatility. For example, coke delivered FOB to a Chinese port in January 2004 was priced at $60/ton, but rose to $420/ton in March 2004 and in September 2004 was $220/ton. This makes clear the likelihood that prices will remain high. This effort that is the subject of this report has considered the suitability of and potential processes for using Indiana coal for the production of coke in a mine mouth or local coking/gasification-liquefaction process. Such processes involve multiple value streams that reduce technical and economic risk. Initial results indicate that it is possible to use blended coal with up to 40% Indiana coal in a non recovery coke oven to produce pyrolysis gas that can be selectively extracted and used for various purposes including the production of electricity and liquid transportation fuels and possibly fertilizer and hydrogen. -
High Calorific Value Coal Turkish and Global Outlook
High calorific value coal Turkish and global outlook October 2014 2 Executive Summary Despite the fact that coal has notorious perception due to its impacts on the environment, it’s not possible to neglect its share in the global energy supply. Especially, in emerging markets with ever growing energy demand, cost and eligibility advantages bring coal into prominence. When a coal consumption analysis is conducted, it is evident that electricity and heat generation sector maintained its leadership with more than 3.8 billion tonnes in 2012. This situation can be seen in Turkey as well. Installed capacity of imported coal PPs in Turkish Uygar Yörük electricity market has passed 3.9 GW by the end Energy & Resources Industry Leader of the 2013. On account of increasing Turkish Partner electricity demand and economic advantages of imported coal, it wouldn’t be wrong to expect that imported coal PPs will show significant growth. In the first seven months of On the other side, all locations available to 2014, additional installed capacity of 950 MW imported coal power plants are already held connected to the grid. After the natural gas by investors and some of these projects will be investment boom in 2011, Turkish electricity naturally driven out of the competition. market has a new tendency to imported coal power plants. When global coal market is analysed, trends like China’s growing coal demand, shale gas Uncertainties related to natural gas power plants impact on coal prices and carbon policies and unexpected delays in lignite projects lead can be defined as major indicators that have investors to hard coal as a relatively more eligible determining role on coal pricing. -
Memorial to Alexander Rankin Cameron 1927–2000 RUSSELL R
Memorial to Alexander Rankin Cameron 1927–2000 RUSSELL R. DUTCHER Box 128, Carbondale, Illinois 62903-0128 WILLIAM SPACKMAN 170 Rosin Court, Wilmington, North Carolina 28405 As we move forward in our chosen professions, we become acquainted with many colleagues who become friends, professionally and oftentimes socially. By their very nature, geology and closely allied fields attract a large number of individuals who are in their chosen field because of the great satisfaction that stems from learning about Earth and its evolution. In turn, they enjoy imparting their knowledge to others—sometimes in a formal fashion through teaching and in publications, and sometimes through informal discussions, which may be spontaneous in origin. Every once in a while we meet a colleague who displays all of the traits to which everyone aspires. A human being that we just know makes life a little better for all of us, and by their very presence, makes the world a better place. Such a person was Alex Cameron. Alexander Rankin Cameron was born on January 24, 1927, in Toronto, Canada. At an early age Alex and his family moved to Cape Breton Island in the Canadian province of Nova Scotia. He received his bachelor of science degree from St. Francis Xavier University in Antigonish, Nova Scotia, in 1952. He spent the following summer at the Coal Research Laboratory of the Geological Survey of Canada in Sydney, Nova Scotia, under the guidance of Peter A. Hacque- bard. In the fall of 1952, he joined the staff of the Coal Research Section at Pennsylvania State University as a research assistant and graduate student in the Department of Geology and Geo- physics. -
Conodont Biofacies in a Ramp to Basin Setting (Latest Devonian and Earliest Carboniferous) in the Rocky Mountains of Southernmost Canada and Northern Montana
U. S. DEPARTMENT OF THE INTERIOR U. S. GEOLOGICAL SURVEY Conodont biofacies in a ramp to basin setting (latest Devonian and earliest Carboniferous) in the Rocky Mountains of southernmost Canada and northern Montana by Lauret E. Savoy1 and Anita G. Harris 2 Open-File Report 93-184 This report is preliminary and has not been reviewed for conformity with Geological Survey editorial standards or with the North American Stratigraphic Code. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. \ Department of Geology and Geography, Mount Holyoke College, South Hadley, MA 01075 2 U.S. Geological Survey, Reston, VA 22092 1993 TABLE OF CONTENTS ABSTRACT 1 INTRODUCTION 2 LITHOSTRATIGRAPHY AND DEPOSITIONAL SETTING 2 CONODONT BIOSTRATIGRAPHY AND BIOFACIES 8 Palliser Formation 8 Exshaw Formation 13 Banff Formation 13 Correlative units in the Lussier syncline 15 PALEOGEOGRAPfflC SETTING 17 CONCLUSION 23 ACKNOWLEDGMENTS 23 REFERENCES CITED 24 APPENDIX 1 38 FIGURES 1. Index map of sections examined and major structural features of the thrust and fold belt 3 2. Correlation chart of Upper Devonian and Lower Mississippian stratigraphic units. 4 3. Selected microfacies of the Palliser Formation. 5 4. Type section of Exshaw Formation, Jura Creek. 6 5. Lower part of Banff Formation, North Lost Creek. 7 6. Conodont distribution in Palliser and Exshaw formations, Inverted Ridge. 9 7. Conodont distribution in upper Palliser and lower Banff formations, Crowsnest Pass. 11 8. Conodont distribution in upper Palliser, Exshaw, and lower Banff formations, composite Jura Creek - Mount Buller section. 12 9. -
Alaska's High-Rank Coals
ALASKA'S HIGH-RANK COALS A summary of high-rank coal resources in Alaska and their potential for mining and development. First Edition 1990 Revised Edition 1993 Department ofNatura1 Resources DMSION OF GEOLOGICAL & GEOPHYSICAL SURVEYS Fairbanks, Alaska ! Cover photo: North linrb of Wishbone Hill syncline, Mafanusku Valley. (Seefig. 8, p. 7.) STATEOFALASKA Walter J. Hickel, Governor DEPARTMENT OF NATURAL RESOURCES Glenn A. Olds, Commissioner DIVISION OF GEOLOGICAL & GEOPHYSICAL SURVEYS Thomas E. Smith, State Geologist Address mail orders to the Fairbanks office. DGGS publications may be inspected at the following locations. Alaska Division of Geological & Geophysical Surveys 794 University Avenue, Suite 200 Fairbanks, Alaska 99709-3645 Department of Natural Resources Public Information Center 3601 C Street, Suite 200 Anchorage, Alaska 99510 This publication, produced and released by the Division of Geological &Geophysical Surveys, and printed in Delta Junction, Alaska, by Dragon Press at a cost of $2.66 per copy. Publication is required by Alaska Statute 41, "to determine the potential of Alaskan land forproductionofrnetals, minerals, fuels, and geothermal resources; the location and supplies of groundwater and construction materials; the potential geologic hazards to buildings, roads, bridges, and other installations and structures; and shall conduct such other surveys and investigations as will advance knowledge of the geology of Alaska." FOREWORD Although current coal production is limited to subbituminous coals, Alaska produced high rank coals from the MatanuskaJield until 1968. Plans are again under wayfor production from the MatanuskaJield. Deadfall syncline coal, being in close proximity to the Bering Sea, is anofher candidatefor development and is receiving renewed attention. For example, seam K3 of thisfield is ofhigh voIatile A bituminous rank and has a maximum thickness of 17feet, with an average ash content of 9percentand over 10feet of this seam averages less than 4percent ash. -
The Letters F and T Refer to Figures Or Tables Respectively
INDEX The letters f and t refer to figures or tables respectively "A" Marker, 312f, 313f Amherstberg Formation, 664f, 728f, 733,736f, Ashville Formation, 368f, 397, 400f, 412, 416, Abitibi River, 680,683, 706 741f, 765, 796 685 Acadian Orogeny, 686, 725, 727, 727f, 728, Amica-Bear Rock Formation, 544 Asiak Thrust Belt, 60, 82f 767, 771, 807 Amisk lowlands, 604 Askin Group, 259f Active Formation, 128f, 132f, 133, 139, 140f, ammolite see aragonite Assiniboia valley system, 393 145 Amsden Group, 244 Assiniboine Member, 412, 418 Adam Creek, Ont., 693,705f Amundsen Basin, 60, 69, 70f Assiniboine River, 44, 609, 637 Adam Till, 690f, 691, 6911,693 Amundsen Gulf, 476, 477, 478 Athabasca, Alta., 17,18,20f, 387,442,551,552 Adanac Mines, 339 ancestral North America miogeocline, 259f Athabasca Basin, 70f, 494 Adel Mountains, 415 Ancient Innuitian Margin, 51 Athabasca mobile zone see Athabasca Adel Mountains Volcanics, 455 Ancient Wall Complex, 184 polymetamorphic terrane Adirondack Dome, 714, 765 Anderdon Formation, 736f Athabasca oil sands see also oil and gas fields, Adirondack Inlier, 711 Anderdon Member, 664f 19, 21, 22, 386, 392, 507, 553, 606, 607 Adirondack Mountains, 719, 729,743 Anderson Basin, 50f, 52f, 359f, 360, 374, 381, Athabasca Plain, 617f Aftonian Interglacial, 773 382, 398, 399, 400, 401, 417, 477f, 478 Athabasca polymetamorphic terrane, 70f, Aguathuna Formation, 735f, 738f, 743 Anderson Member, 765 71-72,73 Aida Formation, 84,104, 614 Anderson Plain, 38, 106, 116, 122, 146, 325, Athabasca River, 15, 20f, 35, 43, 273f, 287f, Aklak -
Bedrock Geology of Alberta
Alberta Geological Survey Map 600 Legend Bedrock Geology of Alberta Southwestern Plains Southeastern Plains Central Plains Northwestern Plains Northeastern Plains NEOGENE (± PALEOGENE) NEOGENE ND DEL BONITA GRAVELS: pebble gravel with some cobbles; minor thin beds and lenses NH HAND HILLS FORMATION: gravel and sand, locally cemented into conglomerate; gravel of sand; pebbles consist primarily of quartzite and argillite with minor amounts of sandstone, composed of mainly quartzite and sandstone with minor amounts of chert, arkose, and coal; fluvial amygdaloidal basalt, and diabase; age poorly constrained; fluvial PALEOGENE PALEOGENE PALEOGENE (± NEOGENE) PALEOGENE (± NEOGENE) UPLAND GRAVEL: gravel composed of mainly white quartzite cobbles and pebbles with lesser amounts of UPLAND GRAVEL: gravel capping the Clear Hills, Halverson Ridge, and Caribou Mountains; predominantly .C CYPRESS HILLS FORMATION: gravel and sand, locally cemented to conglomerate; mainly quartzite .G .G and sandstone clasts with minor chert and quartz component; fluvial black chert pebbles; sand matrix; minor thin beds and lenses of sand; includes gravel in the Swan Hills area; white quartzite cobbles and pebbles with lesser amounts of black chert pebbles; quartzite boulders occur in the age poorly constrained; fluvial Clear Hills and Halverson Ridge gravels; sand matrix; ages poorly constrained; extents poorly defined; fluvial .PH PORCUPINE HILLS FORMATION: olive-brown mudstone interbedded with fine- to coarse-grained, .R RAVENSCRAG FORMATION: grey to buff mudstone -
Chemical Analyses and Physical Properties of 12 Coal Samples from the Pocahontas Field, Tazewell County, Virginia, and Mcdowell County, West Virginia
Chemical Analyses and Physical Properties of 12 Coal Samples from the Pocahontas Field, Tazewell County, Virginia, and McDowell County, West Virginia GEOLOGICAL SURVEY BULLETIN 1528 Chemical Analyses and Physical Properties of 12 Coal Samples from the Pocahontas Field, Tazewell County, Virginia, and McDowell County, West Virginia By VIRGIL A. TRENT, JACK H. MEDLIN, S. LYNN COLEMAN, and RONALD W. STANTON GEOLOGICAL SURVEY BULLETIN 1528 A discussion of the metamorphic rank, major and minor element content, and physical properties of 12 coal samples from the Pocahontas coal field UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1982 UNITED STATES DEPARTMENT OF THE INTERIOR JAMES G. WATT, Secretary GEOLOGICAL SURVEY Dallas L. Peck, Director Library of Congress Cataloging in Publication Data Main entry under title: Chemical analyses and physical properties of 12 coal samples from the Pocahontas field, Tazewell County, Virginia, and McDowell County, West Virginia. (Geological Survey bulletin ; 1528) Bibliography: p. Supt. of Docs. no.: I 19.3:1528 1. Coal-Virginia-Tazewell County-Analysis. 2. Coal-West Virginia-McDowell County Analysis. I. Trent, Virgil A. II. Series. QE75.B9 vo. 1528 [TP326.U5] 557.3 81-607871 [662.6'224'09755763] AACR2 For sale by the Distribution Branch, U.S. Geological Survey, 604 South Pickett Street, Alexandria, VA 22304 CONTENTS Page A bs tract_________________________________________________________________________________ 1 Introduction_____________________________________________________________________________ -
Stratigraphy, Paleotectonics and Paleoenvironments of the Morrison Formation in the Bighorn Basin of Wyoming and Montana Dibakar Goswami Iowa State University
Iowa State University Capstones, Theses and Retrospective Theses and Dissertations Dissertations 1993 Stratigraphy, paleotectonics and paleoenvironments of the Morrison Formation in the Bighorn Basin of Wyoming and Montana Dibakar Goswami Iowa State University Follow this and additional works at: https://lib.dr.iastate.edu/rtd Part of the Geology Commons Recommended Citation Goswami, Dibakar, "Stratigraphy, paleotectonics and paleoenvironments of the Morrison Formation in the Bighorn Basin of Wyoming and Montana " (1993). Retrospective Theses and Dissertations. 10434. https://lib.dr.iastate.edu/rtd/10434 This Dissertation is brought to you for free and open access by the Iowa State University Capstones, Theses and Dissertations at Iowa State University Digital Repository. It has been accepted for inclusion in Retrospective Theses and Dissertations by an authorized administrator of Iowa State University Digital Repository. For more information, please contact [email protected]. INFORMATION TO USERS This manuscript has been reproduced from the microfilm master. UMI films the text directly from the original or copy submitted. Thus, some thesis and dissertation copies are in typewriter face, while others may be from any type of computer printer. The quality of this reproduction is dependent upon the quality of the copy submitted. Broken or indistinct print, colored or poor quality illustrations and photographs, print bleedthrough, substandard margins, and improper alignment can adversely afiect reproduction. In the unlikely event that the author did not send UMI a complete manuscript and there are missing pages, these will be noted. Also, if unauthorized copyright material had to be removed, a note will indicate the deletion. Oversize materials (e.g., maps, drawings, charts) are reproduced by sectioning the original, beginning at the upper left-hand corner and continuing from left to right in equal sections with small overlaps. -
Oil and Gas Resource Potential of the Kootenay Area of British Columbia
. OIL AND GAS RESOURCE POTENTIAL OF THE KOOTENAY AREA OF BRITISH COLUMBIA by Peter Hannigan, P.J. Lee, K.G. Osadetz and K. Olsen-Heise Petroleum Resources Subdivision Institute of Sedimentary and Petroleum Geology Geological Survey of Canada 3303 - 33 Street N.W. Calgary, Alberta T2L 2A7 April, 1993 TABLE OF CONTENTS SUMMARY 3 INTRODUCTION 5 GEOLOGICAL SETTING AND PLAY PARAMETERS 7 Waterton Colorado Foothills Gas Play 7 Waterton Mannville Foothills Gas Play 8 Waterton Mannville Foothills Oil Play 9 Waterton Rundle/Wabamun Foothills Gas Play 9 Kishenehn Tertiary Graben Gas Play 10 Kishenehn Tertiary Graben Oil Play 12 MacDonald Paleozoic Structural Gas Play 12 Fernie - Elk Valley Mesozoic Structural Gas Play 14 Fernie - Elk Valley Paleozoic Structural Gas Play 15 Rocky Mountain Trench Cenozoic Structural Gas Play 16 Belt - Purcell Structural Oil and Gas Play 17 Belt - Purcell Immature Structural Oil Play 17 Belt - Purcell Immature Structural Gas Play 19 Belt - Purcell Conceptual Structural Oil Play 19 Belt - Purcell Conceptual Structural Gas Play 19 Belt - Purcell Speculative Structural Gas Play 20 Belt - Purcell Speculative Structural Oil Play 20 ASSESSMENT TECHNIQUE 20 RESOURCE APPRAISAL 21 Waterton Colorado Foothills Gas Play 21 Waterton Mannville Foothills Gas Play 22 Waterton Mannville Foothills Oil Play 22 Waterton Rundle/Wabamun Foothills Gas Play 22 Kishenehn Tertiary Graben Gas Play 23 Kishenehn Tertiary Graben Oil Play 23 MacDonald Paleozoic Structural Gas Play 23 Fernie - Elk Valley Mesozoic Structural Gas Play 23 Fernie - Elk Valley Paleozoic Structural Gas Play 24 Rocky Mountain Trench Cenozoic Structural Gas Play 24 Belt - Purcell Immature Structural Oil Play 24 Belt - Purcell Immature Structural Gas Play 25 SUMMARY AND CONCLUSIONS 25 REFERENCES 28 APPENDIX 1: PROBABILITY DISTRIBUTIONS AND RISK FACTORS 44 APPENDIX 2: STATISTICAL OUTPUT 61 FIGURE CAPTIONS 160 SUMMARY There are sixteen exploration hydrocarbon plays identified in the Kootenay area of southeastern British Columbia.