Coalbed Methane, a Fossil Fuel Resource with the Potential for Zero Greenhouse Gas Emissions – the Alberta, Canada Program 1996 -2009: a Summary
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The Hydrology of Coalbed Methane Reservoirs and the Interplay of Gas, Water, and Coal in CBM Production
University of Colorado Law School Colorado Law Scholarly Commons Coalbed Methane Development in the Intermountain West (April 4-5) 2002 4-4-2002 The Hydrology of Coalbed Methane Reservoirs and the Interplay of Gas, Water, and Coal in CBM Production Leslie Nogaret Follow this and additional works at: https://scholar.law.colorado.edu/coalbed-methane-development- intermountain-west Part of the Geotechnical Engineering Commons, Hydraulic Engineering Commons, Hydrology Commons, Natural Resources Management and Policy Commons, Oil, Gas, and Energy Commons, Science and Technology Law Commons, and the Water Resource Management Commons Citation Information Nogaret, Leslie, "The Hydrology of Coalbed Methane Reservoirs and the Interplay of Gas, Water, and Coal in CBM Production" (2002). Coalbed Methane Development in the Intermountain West (April 4-5). https://scholar.law.colorado.edu/coalbed-methane-development-intermountain-west/9 Reproduced with permission of the Getches-Wilkinson Center for Natural Resources, Energy, and the Environment (formerly the Natural Resources Law Center) at the University of Colorado Law School. Leslie Nogaret, The Hydrology of Coalbed Methane Reservoirs and the Interplay of Gas, Water, and Coal in CBM Production, in COALBED METHANE DEVELOPMENT IN THE INTERMOUNTAIN WEST (Natural Res. Law Ctr., Univ. of Colo. Sch. of Law 2002). Reproduced with permission of the Getches-Wilkinson Center for Natural Resources, Energy, and the Environment (formerly the Natural Resources Law Center) at the University of Colorado Law School. References Lyons, W.S., 2002, Seismic Assists Geologic Interpretation and Development Program in the Ferron Bowles, J., 2001, Phillips’ CBM Outlook, A.G. Edwards, Coalbed Methane Play, presentation to the Rocky March 14, 2001, Coal Bed Methane Energy Mountain Section of SEPM, February 26, 2002. -
T U R G a Y E R T E K I N, B.Sc, M.Sc., Ph.D
T U R G A Y E R T E K I N, B.Sc, M.Sc., Ph.D. ● P E N N S T A T E U N I V E R S I T Y ● U N I V E R S I T Y P A R K , P A 1 6 8 7 0 ● ● (8 14 ) 8 6 5 - 6 0 8 2 ● Professor Emeritus Petroleum and Natural Gas Engineering E DUC A T I ON Middle East Technical University, Ankara, Turkey, B.Sc., 1969, Petroleum Engineering Middle East Technical University, Ankara, Turkey, M.Sc., 1971, Petroleum Engineering Pennsylvania State University, University Park, USA, Ph.D., 1978, Petroleum and Natural Gas Engineering A C A D E M IC A N D A D M INIST R A T IVE P O S ITION S July 2017 to present Professor Emeritus of Petroleum and Natural Gas Engineering The Pennsylvania State University July 2013 to July 2017 Head, John and Willie Leone Family Department of Energy and Mineral Engineering, the George E. Trimble Chair in Earth and Mineral Sciences, the Pennsylvania State University May 2013 to May 2014 Co-Director, Institute of Natural Gas Research (INGaR), Pennsylvania State University July 2001 to Present Professor of Petroleum and Natural Gas Engineering and George E. Trimble Chair in Earth and Mineral Sciences, Pennsylvania State University July 1998 to June 2001 Associate Head, Department of Energy and Geo-Environmental Engineering July 1987 to Present Professor of Petroleum and Natural Gas Engineering, Pennsylvania State University July 1984 to January 2015 Chairman of Petroleum and Natural Gas Engineering, Pennsylvania State University July 1983 to July 1984 Associate Professor of Petroleum and Natural Gas Engineering, Pennsylvania State University -
(12) United States Patent (10) Patent No.: US 8,505,620 B2 Zupanick (45) Date of Patent: *Aug
US00850562OB2 (12) United States Patent (10) Patent No.: US 8,505,620 B2 Zupanick (45) Date of Patent: *Aug. 13, 2013 (54) METHOD AND SYSTEM FOR ACCESSING (58) Field of Classification Search SUBTERRANEAN DEPOSTS FROM THE USPC .............................................. 166/50, 52, 245 SURFACE AND TOOLS THEREFOR See application file for complete search history. (75) Inventor: Joseph A. Zupanick, Beckley, WV (US) (56) References Cited (73) Assignee: Vitruvian Exploration, LLC, Houston, U.S. PATENT DOCUMENTS TX (US) 54,144 A 4, 1866 Hamar 274,740 A 3/1883 Douglass (*) Notice: Subject to any disclaimer, the term of this (Continued) patent is extended or adjusted under 35 U.S.C. 154(b) by 0 days. FOREIGN PATENT DOCUMENTS AU 85,49964 A 11, 1986 This patent is Subject to a terminal dis CA 2210866 1, 1998 claimer. (Continued) (21) Appl. No.: 11/982,249 OTHER PUBLICATIONS (22) Filed: Oct. 31, 2007 McCray, Arthur, et al., “Oil Well Drilling Technology.” University of Oklahoma Press, 1959, Title Page, Copyright Page and pp. 315-319 (65) Prior Publication Data (7 pages). US 2008/OO60806A1 Mar. 13, 2008 (Continued) Primary Examiner — John Kreck Related U.S. Application Data (74) Attorney, Agent, or Firm — Fish & Richardson P.C. (60) Continuation of application No. 10/630,345, filed on Jul. 29, 2003, which is a continuation-in-part of (57) ABSTRACT According to one embodiment, a system for accessing a Sub (Continued) terranean Zone from the surface includes a well bore extend ing from the Surface to the Subterranean Zone, and a well bore (51) Int. C. pattern connected to the junction and operable to drain fluid E2IB 43/00 (2006.01) from a region of the Subterranean Zone to the junction. -
Histology and Ontogeny of Pachyrhinosaurus Nasal Bosses By
Histology and Ontogeny of Pachyrhinosaurus Nasal Bosses by Elizabeth Kruk A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Systematics and Evolution Department of Biological Sciences University of Alberta © Elizabeth Kruk, 2015 Abstract Pachyrhinosaurus is a peculiar ceratopsian known only from Upper Cretaceous strata of Alberta and the North Slope of Alaska. The genus consists of three described species Pachyrhinosaurus canadensis, Pachyrhinosaurus lakustai, and Pachyrhinosaurus perotorum that are distinguishable by cranial characteristics, including parietal horn shape and orientation, absence/presence of a rostral comb, median parietal bar horns, and profile of the nasal boss. A fourth species of Pachyrhinosaurus is described herein and placed into its phylogenetic context within Centrosaurinae. This new species forms a polytomy at the crown with Pachyrhinosaurus canadensis and Pachyrhinosaurus perotorum, with Pachyrhinosaurus lakustai falling basal to that polytomy. The diagnostic features of this new species are an apomorphic, laterally curved Process 3 horns and a thick longitudinal ridge separating the supraorbital bosses. Another focus is investigating the ontogeny of Pachyrhinosaurus nasal bosses in a histological context. Previously, little work has been done on cranial histology in ceratopsians, focusing instead on potential integumentary structures, the parietals of Triceratops, and how surface texture relates to underlying histological structures. An ontogenetic series is established for the nasal bosses of Pachyrhinosaurus at both relative (subadult versus adult) and fine scale (Stages 1-5). It was demonstrated that histology alone can indicate relative ontogenetic level, but not stages of a finer scale. Through Pachyrhinosaurus ontogeny the nasal boss undergoes increased vascularity and secondary remodeling with a reduction in osteocyte lacunar density. -
Chapter L—Coal-Bed Methane Gas-In-Place Resource Estimates
Chapter L National Coal Resource Coal-Bed Methane Gas-In-Place Resource Assessment Estimates Using Sorption Isotherms and Burial History Reconstruction: An Example from the Ferron Sandstone Member Click here to return to Disc 1 Volume Table of Contents of the Mancos Shale, Utah By Todd A. Dallegge1 and Charles E. Barker1 Chapter L of Geologic Assessment of Coal in the Colorado Plateau: Arizona, Colorado, New Mexico, and Utah Edited by M.A. Kirschbaum, L.N.R. Roberts, and L.R.H. Biewick U.S. Geological Survey Professional Paper 1625–B* 1 U.S. Geological Survey, Denver, Colorado 80225 * This report, although in the USGS Professional Paper series, is available only on CD-ROM and is not available separately U.S. Department of the Interior U.S. Geological Survey Contents Overview ...................................................................................................................................................... L1 What Is Coal-Bed Methane? ...................................................................................................................... 2 Importance of Coal-Bed Methane Production ........................................................................................ 2 How Much Coal-Bed Methane is Available?........................................................................................... 3 How Do Coal Beds Generate and Store Methane? ................................................................................ 4 Details About Coal Cleat.................................................................................................................... -
Coal Mine Methane Recovery: a Primer
Coal Mine Methane Recovery: A Primer U.S. Environmental Protection Agency July 2019 EPA-430-R-09-013 ACKNOWLEDGEMENTS This report was originally prepared under Task Orders No. 13 and 18 of U.S. Environmental Protection Agency (USEPA) Contract EP-W-05-067 by Advanced Resources, Arlington, USA and updated under Contract EP-BPA-18-0010. This report is a technical document meant for information dissemination and is a compilation and update of five reports previously written for the USEPA. DISCLAIMER This report was prepared for the U.S. Environmental Protection Agency (USEPA). USEPA does not: (a) make any warranty or representation, expressed or implied, with respect to the accuracy, completeness, or usefulness of the information contained in this report, or that the use of any apparatus, method, or process disclosed in this report may not infringe upon privately owned rights; (b) assume any liability with respect to the use of, or damages resulting from the use of, any information, apparatus, method, or process disclosed in this report; or (c) imply endorsement of any technology supplier, product, or process mentioned in this report. ABSTRACT This Coal Mine Methane (CMM) Recovery Primer is an update of the 2009 CMM Primer, which reviewed the major methods of CMM recovery from gassy mines. [USEPA 1999b, 2000, 2001a,b,c] The intended audiences for this Primer are potential investors in CMM projects and project developers seeking an overview of the basic technical details of CMM drainage methods and projects. The report reviews the main pre-mining and post-mining CMM drainage methods with associated costs, water disposal options and in-mine and surface gas collection systems. -
Dinosaur Eggshells from the Lower Maastrichtian St. Mary River Formation of Southern Alberta, Canada
Canadian Journal of Earth Sciences Dinosaur eggshells from the lower Maastrichtian St. Mary River Formation of southern Alberta, Canada Journal: Canadian Journal of Earth Sciences Manuscript ID cjes-2017-0195.R1 Manuscript Type: Article Date Submitted by the Author: 13-Nov-2017 Complete List of Authors: Voris, Jared; University of Calgary, Geoscience; Zelenitsky, Darla; Department of Geoscience, Tanaka, Kohei; Nagoya Daigaku Hakubutsukan; University of Calgary, DepartmentDraft of Geoscience Therrien, François; Royal Tyrrell Museum of Palaeontology, Is the invited manuscript for consideration in a Special N/A Issue? : Keyword: eggshell, dinosaur, Cretaceous, Maastrichtian, Alberta https://mc06.manuscriptcentral.com/cjes-pubs Page 1 of 47 Canadian Journal of Earth Sciences 1 2 3 4 5 6 7 8 9 Dinosaur eggshells from the lower Maastrichtian St. Mary River Formation of southern 10 Alberta, Canada 11 12 Jared T. Voris, Darla K. Zelenitsky,Draft François Therrien, Kohei Tanaka 13 J. T. Voris, D. K. Zelenitsky, and K. Tanaka. Department of Geoscience, University of 14 Calgary, 2500 University Dr. NW, Calgary, AB T2N 1N4, Canada; [email protected], 15 [email protected], [email protected] 16 K. Tanaka. Nagoya University Museum, Nagoya University Furocho, Chikusa-Ku, Nagoya, 17 464-8601, Japan; [email protected] 18 F. Therrien. Royal Tyrrell Museum of Palaeontology, Box 7500, Drumheller, AB T0J 0Y0, 19 Canada.; [email protected] 20 1 https://mc06.manuscriptcentral.com/cjes-pubs Canadian Journal of Earth Sciences Page 2 of 47 1 2 Abstract–North America is known for its rich uppermost Cretaceous record of dinosaur egg 3 remains, although a notable fossil gap exists during the lower Maastrichtian. -
Methane Hydrate Stability and Anthropogenic Climate Change
Biogeosciences, 4, 521–544, 2007 www.biogeosciences.net/4/521/2007/ Biogeosciences © Author(s) 2007. This work is licensed under a Creative Commons License. Methane hydrate stability and anthropogenic climate change D. Archer University of Chicago, Department of the Geophysical Sciences, USA Received: 20 March 2007 – Published in Biogeosciences Discuss.: 3 April 2007 Revised: 14 June 2007 – Accepted: 19 July 2007 – Published: 25 July 2007 Abstract. Methane frozen into hydrate makes up a large 1 Methane in the carbon cycle reservoir of potentially volatile carbon below the sea floor and associated with permafrost soils. This reservoir intu- 1.1 Sources of methane itively seems precarious, because hydrate ice floats in water, and melts at Earth surface conditions. The hydrate reservoir 1.1.1 Juvenile methane is so large that if 10% of the methane were released to the at- Methane, CH , is the most chemically reduced form of car- mosphere within a few years, it would have an impact on the 4 bon. In the atmosphere and in parts of the biosphere con- Earth’s radiation budget equivalent to a factor of 10 increase trolled by the atmosphere, oxidized forms of carbon, such as in atmospheric CO . 2 CO , the carbonate ions in seawater, and CaCO , are most Hydrates are releasing methane to the atmosphere today in 2 3 stable. Methane is therefore a transient species in our at- response to anthropogenic warming, for example along the mosphere; its concentration must be maintained by ongoing Arctic coastline of Siberia. However most of the hydrates release. One source of methane to the atmosphere is the re- are located at depths in soils and ocean sediments where an- duced interior of the Earth, via volcanic gases and hydrother- thropogenic warming and any possible methane release will mal vents. -
Subsurface Characterization of the Pembina-Wabamun Acid-Gas Injection Area
ERCB/AGS Special Report 093 Subsurface Characterization of the Pembina-Wabamun Acid-Gas Injection Area Subsurface Characterization of the Pembina-Wabamun Acid-Gas Injection Area Stefan Bachu Maja Buschkuehle Kristine Haug Karsten Michael Alberta Geological Survey Alberta Energy and Utilities Board ©Her Majesty the Queen in Right of Alberta, 2008 ISBN 978-0-7785-6950-3 The Energy Resources Conservation Board/Alberta Geological Survey (ERCB/AGS) and its employees and contractors make no warranty, guarantee or representation, express or implied, or assume any legal liability regarding the correctness, accuracy, completeness or reliability of this publication. Any digital data and software supplied with this publication are subject to the licence conditions. The data are supplied on the understanding that they are for the sole use of the licensee, and will not be redistributed in any form, in whole or in part, to third parties. Any references to proprietary software in the documentation, and/or any use of proprietary data formats in this release, do not constitute endorsement by the ERCB/AGS of any manufacturer's product. If this product is an ERCB/AGS Special Report, the information is provided as received from the author and has not been edited for conformity to ERCB/AGS standards. When using information from this publication in other publications or presentations, due acknowledgment should be given to the ERCB/AGS. The following reference format is recommended: Bachu, S., Buschkuehle, M., Haug, K., Michael, K. (2008): Subsurface characterization of the Pembina-Wabamun acid-gas injection area; Energy Resources Conservation Board, ERCB/AGS Special Report 093, 60 p. -
3Rd-Order Sequence Stratigraphy and Lithostratigraphy of the Bearpaw–Horseshoe Canyon Transition, Alberta Plains
3rd-order sequence stratigraphy and lithostratigraphy of the Bearpaw–Horseshoe Canyon transition, Alberta plains Ben Hathway, Alberta Geological Survey, Alberta Energy Regulator, Edmonton, Alberta, [email protected] Summary The regional-scale delineation and modelling of upper and lower boundaries and zero edges for the Bearpaw Formation tongues in southern and central Alberta forms an important component of a wider AGS project to construct a digital 3D geological framework for the Alberta subsurface. Core and high-quality wireline logs, generated to a large extent by recent coal-bed methane drilling, permit the establishment of a 3rd-order sequence stratigraphic framework. This provides a context within which lithostratigraphic boundaries of the Bearpaw Formation with laterally equivalent and overlying Horseshoe Canyon and St. Mary River formation strata can be more rigorously mapped. Lower boundaries of the Bearpaw tongues are 3rd-order transgressive, or more proximally, maximum flooding surfaces, and upper boundaries are highly diachronous facies contacts within successive regressive systems tracts. Introduction The complex nature of the intertonguing relationship between Campanian-Maastrichtian (Upper Cretaceous) Bearpaw Formation marine shale and fluviodeltaic nonmarine and shoreline deposits of the Horseshoe Canyon and St. Mary River formations in central and southern Alberta has long been recognized (e.g. Russell, 1932; Irish, 1970). Following earlier work focused on high-resolution, 4th-order sequence analysis of the stratigraphically limited part of the Bearpaw–Horseshoe Canyon transition exposed along the Red Deer River valley (e.g. Rahmani, 1988; Ainsworth, 1994), the first regional sequence stratigraphic study of the succession was undertaken by Catuneanu et al. (1997). In that study increasing and decreasing trends in wireline gamma-ray response were used to delineate up to 11 3rd-order transgressive-regressive (T-R) sequences within the Bearpaw Formation. -
Geologic Methane Seeps Along Boundaries of Arc C Permafrost
Geologic Methane seeps along boundaries of Arc6c permafrost thaws and melng glaciers . Walter Anthony, K.M. , et. al. Nature Geoscience. Vol 5. June 2012. DOI: 10.1038/NGEO1480 Objecves: • This study documents the first evidence of widespread geological methane seepage along boundaries of cryosphere retreat. • The study focused on the release of 14C-depleted methane from abundant gas seeps concentrated along boundaries of permafrost thaw and receding glaciers in Alaska and Greenland. • The authors combined a new method of aerial survey and ground truth to idenfy seep-induced melt-holes in ice covered water bodies in order to quanfy methane seeps in Alaska, to confirm the occurrence of anomalous seeps in Greenland, and to document for the first me the widespread occurrence of 14C- depleted methane seeps along boundaries of permafrost thaw and melng glaciers in the terrestrial Arcc. • Ground surface survey data and in situ measurements (ebullion flux measurements, gas collecon and isotope analyses) were used to map the occurrence of superficial and subcap methane seeps along a north/south transect in Alaska; in West Greenland, seeps were quanfied only by ground survey. • Over 150,000 seeps were mapped in Alaska and Greenland. New Science • Seeps were characterized by anomalously high methane fluxes, and in Alaska by ancient radiocarbon ages and stable isotope values that matched those of coal bed and thermogenic methane accumulaons. • In Greenland, younger seeps were associated with zones of ice-sheet retreat since the Lile Ice Age. • Examinaon of 6,700 lakes across Alaska revealed the occurrence of 77 previously undocumented subcap seep sites containing >150,000 highly ebullient macroseep vents. -
Competition Structured a Late Cretaceous Megaherbivorous Dinosaur Assemblage Jordan C
www.nature.com/scientificreports OPEN Competition structured a Late Cretaceous megaherbivorous dinosaur assemblage Jordan C. Mallon 1,2 Modern megaherbivore community richness is limited by bottom-up controls, such as resource limitation and resultant dietary competition. However, the extent to which these same controls impacted the richness of fossil megaherbivore communities is poorly understood. The present study investigates the matter with reference to the megaherbivorous dinosaur assemblage from the middle to upper Campanian Dinosaur Park Formation of Alberta, Canada. Using a meta-analysis of 21 ecomorphological variables measured across 14 genera, contemporaneous taxa are demonstrably well-separated in ecomorphospace at the family/subfamily level. Moreover, this pattern is persistent through the approximately 1.5 Myr timespan of the formation, despite continual species turnover, indicative of underlying structural principles imposed by long-term ecological competition. After considering the implications of ecomorphology for megaherbivorous dinosaur diet, it is concluded that competition structured comparable megaherbivorous dinosaur communities throughout the Late Cretaceous of western North America. Te question of which mechanisms regulate species coexistence is fundamental to understanding the evolution of biodiversity1. Te standing diversity (richness) of extant megaherbivore (herbivores weighing ≥1,000 kg) com- munities appears to be mainly regulated by bottom-up controls2–4 as these animals are virtually invulnerable to top-down down processes (e.g., predation) when fully grown. Tus, while the young may occasionally succumb to predation, fully-grown African elephants (Loxodonta africana), rhinoceroses (Ceratotherium simum and Diceros bicornis), hippopotamuses (Hippopotamus amphibius), and girafes (Girafa camelopardalis) are rarely targeted by predators, and ofen show indiference to their presence in the wild5.