The Process of Developing a Co2 Test Injection: Experience to Date and Best Practice
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Analyses of Natural Gases, 2005–2007 Technical Note 427
Analyses of Natural Gases, 2005–2007 D.L. Driskill December 2008 Technical Note 427 U.S. Department of the Interior Bureau of Land Management BLM/NM/ST-08/007+3700 This document is also available on the Amarillo Field Office Web site at http://www.blm.gov/nm/st/en/prog/energy/helium.html Production services provided by the NOC Information and Publishing Services Section Analyses of Natural Gases, 2005–2007 December 2008 D.L. Driskill Geologist Bureau of Land Management Amarillo Field Office Amarillo, Texas Technical Note 427 U.S. Department of the Interior Bureau of Land Management Analyses of Natural Gases, 2005–2007 Technical Note 427 Suggested citation: Driskill, D.L. 2008. Analyses of Natural Gases, 2005–2007, Technical Note 427. Bureau of Land Management. Denver, Colorado. BLM/NM/ST-08/007+3700. 199 pp. ii Contents Page Abstract ...................................................................................................................................................1 Introduction .............................................................................................................................................3 Tables ......................................................................................................................................................5 Geologic Provinces of the United States ............................................................................................5 Figure 1 - Geologic Provinces of the United States ..........................................................................12 -
Xerox University Microfilms
information t o u s e r s This material was produced from a microfilm copy of the original document. While the most advanced technological means to photograph and reproduce this document have been used, the quality is heavily dependent upon the quality of the original submitted. The following explanation of techniques is provided to help you understand markings or patterns which may appear on this reproduction. 1.The sign or "target” for pages apparently lacking from the document photographed is "Missing Page(s)". If it was possible to obtain the missing page(s) or section, they are spliced into the film along with adjacent pages. This may have necessitated cutting thru an image and duplicating adjacent pages to insure you complete continuity. 2. When an image on the film is obliterated with a large round black mark, it is an indication that the photographer suspected that the copy may have moved during exposure and thus cause a blurred image. You will find a good image of the page in the adjacent frame. 3. When a map, drawing or chart, etc., was part of the material being photographed the photographer followed a definite method in "sectioning" the material. It is customary to begin photoing at the upper left hand corner of a large sheet and to continue photoing from left to right in equal sections with a small overlap. If necessary, sectioning is continued again - beginning below the first row and continuing on until complete. 4. The majority of usefs indicate that the textual content is of greatest value, however, a somewhat higher quality reproduction could be made from "photographs" if essential to the understanding of the dissertation. -
The Silurian of Central Kentucky, U.S.A.: Stratigraphy, Palaeoenvironments and Palaeoecology
The Silurian of central Kentucky, U.S.A.: Stratigraphy, palaeoenvironments and palaeoecology FRANK R. ETTENSOHN, R. THOMAS LIERMAN, CHARLES E. MASON, WILLIAM M. ANDREWS, R. TODD HENDRICKS, DANIEL J. PHELPS & LAWRENCE A. GORDON ETTENSOHN, F.R., LIERMAN, R.T., MASON, C.E., ANDREWS, W.M., HENDRICKS, R.T., PHELPS, D.J. & GORDON, L.A., 2013:04:26. The Silurian of central Kentucky, U.S.A.: Stratigraphy, palaeoenvironments and palaeoecology. Memoirs of the Association of Australasian Palaeontologists 44, 159-189. ISSN 0810-8889. Silurian rocks in Kentucky are exposed on the eastern and western flanks of the Cincinnati Arch, a large-wavelength cratonic structure separating the Appalachian foreland basin from the intracratonic Illinois Basin. The Cincinnati Arch area experienced uplift during latest Ordovician-early Silurian time, so that the exposed Silurian section is relatively thin due to onlap and post- Silurian erosional truncation on the arch. On both flanks of the arch, dolomitic carbonates predominate, but the section on the eastern side reflects a more shale-rich ramp that faced eastern Appalachian source areas. In the Silurian section on the western side of the arch, which apparently developed across a platform-like isolation-accommodation zone, shales are rare except dur- ing some highstand episodes, and rocks in the area reflect deposition across a broad, low-gradient shelf area, interrupted by structurally controlled topographic breaks. Using the progression of interpreted depositional environments and nearshore faunal communities, a relative sea-level curve, which parallels those of previous workers, was generated for the section in Kentucky. While the curve clearly shows the influence of glacial eustasy, distinct indications of the far-field, flexural influence of Taconian and Salinic tectonism are also present. -
View of Pa Element, OSU 41751, X 28, Collection
INFORMATION TO USERS The most advanced technology has been used to photo graph and reproduce this manuscript from the microfilm master. UMI films the original text directly from the copy submitted. Thus, some dissertation copies are in typewriter face, while others may be from a computer printer. 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 copyrighted material had to be removed, a note will indicate the deletion. Oversize materials (e.g., maps, drawings, charts) are re produced by sectioning the original, beginning at the upper left-hand comer and continuing from left to right in equal sections with small overlaps. Each oversize page is available as one exposure on a standard 35 mm slide or as a 17" x 23" black and white photographic print for an additional charge. Photographs included in the original manuscript have been reproduced xerographically in this copy. 35 mm slides or 6" x 9" black and white photographic prints are available for any photographs or illustrations appearing in this copy for an additional charge. Contact UMI directly to order. Accessing theUMI World’s Information since 1938 300 North Zeeb Road, Ann Arbor, Ml 48106-1346 USA Order Number 8820S06 Taxonomy and biostratigraphic significance of Wenlockian and Ludlovian (Silurian) conodonts in the midcontinent outcrop area, North America Kleffner, Mark Alan, Ph.D. The Ohio State University, 1988 UMI 300 N. Zeeb Rd. Ann Arbor, MI 48106 PLEASE NOTE: In all cases this material has been filmed in the best possible way from the available copy. -
Silurian Rocks in the Subsurface of Northwestern Ohio
STATE OF OHIO DEPARTMENT OF NATURAL RESOURCES DIVISION OF GEOLOGICAL SURVEY Horace R. Coli ins, Chief LIBRARJ BUREAU OF GEOLOGY TALLAHASSEE, FLORIDA Report of Investigations No. 100 SILURIAN ROCKS IN THE SUBSURFACE OF NORTHWESTERN OHIO by Adriaan Janssens Columbus 1977 SCIENTIFIC AND TECHNICAL STAFF 8DNRDEPARTMENT OF OF THE NATURAL RESOURCES DIVISION OF GEOLOGICAL SURVEY ADMINISTRATION Horace R. Collins, MS, State Geologist and Division Chief Richard A. Struble, PhD, Geologist and Assistant Chief William J. Buschman, Jr., BS, Administrative Geologist Barbara J. Adams, Office Manager REGIONAL GEOLOGY SUBSURFACE GEOLOGY Robert G. Van Horn, MS, Geologist and Section Head Adriaan Janssens, PhD, Geologist and Section Head Richard W. Carlton, PhD, Geologist Charles R. Grapes II, BS, Geologist Michael L. Couchot, MS, Geologist Frank L. Majchszak, MS, Geologist Douglas L. Crowell, MS, Geologist James Wooten, Geology Technician Richard M. DeLong, MS, Geologist Garry E. Yates, Geology Technician Michael C. Hansen, MS, Geologist Linda C. Gearheart, Clerk Dennis N. Hull, MS, Geologist Brenda L. Rinderle, Office Machine Operator Michele L. Risser, BA , Geologist Joel D. Vormelker, MS, Geologist LAKE ERIE GEOCHEMISTRY LABORATORY Charles H. Carter, PhD, Geologist and Section Head D. Joe Benson, PhD, Geologist David A. Stith, MS, Geologist and Section Head Donald E. Guy, Jr., BA, Geologist George Botoman, MS, Geologist Dale L. Liebenthal, Boat Captain Norman F. Knapp, PhD, Chemist Thomas J. Feldkamp, BS, Geology Technician E. Lorraine Thomas, Laboratory Technician Marjorie L. VanVooren, Typist TECHNICAL PUBLICATIONS Jean Simmons Brown, MS, Geologist/Editor and Section Head Cartography Philip J. Celnar, BFA, Cartography Supervisor R. Anne Berry, BFA, Cartographer James A. Brown, Cartographer Donald R. -
Geology of Ohio—The Silurian
A Quarterly Publication of the Division of Geological Survey Spring 1998 GEOLOGY OF OHIO—THE SILURIAN by Michael C. Hansen he Silurian Period occurred more than 400 million years ago in the middle of the Paleo- Tzoic Era. During this 30-million-year-long span, the climate and depositional environments were different than in any other span of time in Siberia Ohio’s geologic history. Sedimentary rocks of the Silurian System dominate the bedrock surface of Laurentia (North America) China the western half of Ohio, although their exposures are limited because thick glacial sediments cover all but the southernmost portion of the outcrop area. Baltica Australia Silurian rocks in Ohio are primarily carbonates— Ohio limestones and dolomites—and the many quarries in these rocks in western Ohio indicate their impor- tance. Silurian rocks in the subsurface of eastern Ohio contain extensive deposits of salt and accu- Africa mulations of natural gas and oil. In local areas in the Antarctica South America India western half of Ohio, magnificent scenery in the form of caves, cliffs, and waterfalls are unexpected Continental configuration during Silurian time (modified from C. R. Scotese and others, 1979, benefits of Silurian rocks. Paleozoic base maps, Journal of Geology, v. 87, fig. 14). The Silurian System was named by Roderick Impey Murchison, a Scotsman who eventually be- came the director of the Geological Survey of Great Britain. He first studied these rocks in Wales and NY named them after a Celtic tribe, the Silures. His MI monumental work, The Silurian System, was pub- platform/ lished in 1838. The lower part of Murchison’s Sil- pinnacle reef urian System overlapped with the upper part of PA Adam Sedgwick’s Cambrian System, a matter which became a great dispute between these two promi- OHIO nent geologists. -
Hydrogeologic Framework of Bedrock Units and Initial Salinity Distribution for a Simulation of Groundwater Flow for the Lake Michigan Basin
National Water Availability and Use Pilot Program Hydrogeologic Framework of Bedrock Units and Initial Salinity Distribution for a Simulation of Groundwater Flow for the Lake Michigan Basin Scientific Investigations Report 2009–5060 U.S. Department of the Interior U.S. Geological Survey Cover image: Three-dimensional rendering of surficial topography and hydrogeologic layers beneath the Lake Michigan Basin. (Image by David Lampe, U.S. Geological Survey.) Hydrogeologic Framework of Bedrock Units and Initial Salinity Distribution for a Simulation of Groundwater Flow for the Lake Michigan Basin By David C. Lampe National Water Availability and Use Pilot Program Scientific Investigations Report 2009–5060 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior KEN SALAZAR, Secretary U.S. Geological Survey Suzette M. Kimball, Acting Director U.S. Geological Survey, Reston, Virginia: 2009 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment, visit http://www.usgs.gov or call 1-888-ASK-USGS For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod To order this and other USGS information products, visit http://store.usgs.gov 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 materials contained within this report. Suggested citation: Lampe, D.C., 2009, Hydrogeologic framework of bedrock units and initial salinity distribution for a simulation of ground- water flow for the Lake Michigan Basin: U.S. -
Stratigraphic Framework of Cambrian and Ordovician FEET Tuscar 3000 6000 Rocks Across the Appalachian Basin from Pennsylvania to Tennessee
U.S. DEPARTMENT OF THE INTERIOR MISCELLANEOUS INVESTIGATIONS SERIES MAP I-2264 U.S. GEOL.OGICAL SURVEY ROME TROUGH ALLEGHENY STRUCTURAL FRONT SSEE OHIO -- WEST VIRGINIA HINGE ZONE D'D' Thrust fault underlying Broadtop Imbricate thrust fault in Broadtop Thrust fault underlying Bergton-Crab block of Shumaker and others (1985); block of Shumaker and others (1985); Run block of Shumaker and others 15-20 mi shortening (Jacobeen and 1-5 mi shortening (Shumaker and oth- (1985); 4-5 mi shortening (Shumaker ers, 1985) and others, 1985) A-A' Kanes, 1975; Shumaker and others, 7t 1985) 6t Exxon No. 1 Bean 8t Shell Oil Company 4 Hardy Co., W. Va Shell Oil Company No. 1 Whetzel NW Tie with No. 1 Greenland Lodge Rockingham Co., Va. Occidental Petroleum Corp. Grant Co., W. Va. (Restored to original D data) unpub. Ryder, (R.T. No. 1 Burley position; bed thick- (Restored to original position about (Restored to original position; Marshall Co., W., Va nesses not corrected 25-30 mi southwest of Allegheny struc- bed thicknesses not corrected 3 5 for dip) tural front (Shumaker and others, 1985)) 2 McCormick Phillips Petroleum Company for dip) FEET FEET Parker and Chapman FEET 2000 5000 No. 1 Birney No. A-1 Finch 0 1 No. 1 Troyer Harrison Co., Ohio Marion Co., W., Va DISCUSSION Deep Well Pollution Control Corp. Holmes Co., Ohio LOWER FEET No. D-1 Empire Reeves Steel Div. FEET SILURIAN 5000 VIRGINIA INTRODUCTION Richland Co., Ohio FEET 10,000 Tuscarora Sandstone WEST VIRGINIA 2000 WEST VIRGINIA FEET PENNSYLVANIA Cross section D-D’ featured in this map is the second in a series of restored stratigraphic cross WEST VIRGINIA 0 PENNSYLVANIA Tuscarora Sandstone ora Sandstone sections drawn by the author to show the stratigraphic framework of Cambrian and Ordovician FEET Tuscar 3000 6000 rocks across the Appalachian basin from Pennsylvania to Tennessee. -
OFR 2011-1, Central Ohio Geology Core Outcrop Workshop II
DEPARTMENT OF NATURAL RESOURCES DIVISION OF GEOLOGICAL SURVEY Lawrence H. Wickstrom, Chief Open-File Report 2011-1 Central Ohio’s Geology in Core and Outcrop Workshop II Hosted by Ohio Department of Natural Resources Division of Geological Survey Sponsored by Ohio Geological Society Horace R. Collins Laboratory Delaware, Ohio April 20, 2011 Ohio Department of Natural Resources Division of Geological Survey 2045 Morse Road, Bldg. C-1 Columbus, Ohio 43229-6693 2011 Agenda 9:00–9:05 A.M. Welcome 9:05–9:30 A.M. Geological Survey’s geohazards and geologic mapping programs 9:30–10:00 A.M. Central Ohio geology 10:00–10:15 A.M. Break 10:15–11:00 A.M. Group A exercise: The utility of Geological Survey map products Group B exercise: Core description 101; anatomy of a fact sheet 11:00–11:45 A.M. Group A exercise: Core description 101; anatomy of a fact sheet Group B exercise: The utility of Geological Survey map products 11:45–12:30 P.M. Lunch provided 12:30–2:00 P.M. Group A exercise: Soil Classifi cations—Unifi ed, AASHTO, USDA, ODOT’s version of AASHTO, and Rock Mass Classifi cation ASTM Group B exercise: Utility of fact sheets in fi eld-like settings; group discussion 2:00–2:15 P.M. Break 2:15–3:45 P.M. Group A exercise: Utility of fact sheets in fi eld-like settings; group discussion Group B exercise: Soil Classifi cations—Unifi ed, AASHTO, USDA, ODOT’s version of AASHTO, and Rock Mass Classifi cation ASTM 3:45–4:00 P.M. -
Ohio Geology 1999, No. 2
A Quarterly Publication of the Division of Geological Survey 1999, No. 2 MAPPING OHIO’S KARST TERRAIN by Dennis N. Hull n southern Highland County, some landown- ing a severe threat to potable water supplies. Be- ers watch anxiously as lawns and farm lots cause of such risks, many of the nation’s state I slowly sag into the earth, causing birdfeeders, geological surveys and the U.S. Geological Survey swing sets, clothesline posts, fence posts, and out- are actively mapping and characterizing the nation’s buildings to tilt out-of-plumb. In Columbus, city karst regions. engineers struggle to contain the rapidly escalating The Ohio Geological Survey recently released cost of a multimillion-dollar tunneling project that Digital Chart and Map Series (DCMS) 24, Known is delayed by the unanticipated presence of an and probable karst in Ohio, a color, plot-on-demand, ancient buried valley and ancient caverns filled 1:500,000-scale digital map that depicts areas of with sticky red clay. In north-central Ohio, rural probable karst and locations of documented karst residents from Bellevue to Castalia are frustrated features. Plotted on a county/township base, the by a maze of subterranean passageways that allow map includes generalized bedrock-geology infor- pesticides, fertilizers, herbicides, and animal wastes mation for areas of probable karst. to move unabated from fields into underlying aqui- fers. Children might easily imagine that some rock- eating Stygian monster from Star Wars has been loosed upon the state to wreak such havoc. Geolo- gists, however, quickly recognize that the common factor in all these problems is karst. -
Scottslawn Road Widening Geotechnical Report
Geotechnical Exploration Report Scottslawn Road Improvements Marysville, Union County, Ohio Prepared for GPD Group 1801 Watermark Drive, Suite 210 Columbus, Ohio 43215 John Xu, P.E. Senior Project Manager Prepared by Professional Service Industries, Inc. 4960 Vulcan Avenue Columbus, Ohio 43228 Paul S. Hundley, P.E. February 21, 2018 Regional Engineer/Principal Consultant PSI Project No. 01021257 PSI Project Number: 01021257 Scottslawn Road Improvements February 21, 2018 Page 1 TABLE OF CONTENTS 1 EXECUTIVE SUMMARY ......................................................................................................................... 2 2 INTRODUCTION ................................................................................................................................... 3 2.1 PROJECT DESCRIPTION ..................................................................................................................... 3 2.2 PROJECT AUTHORIZATION ............................................................................................................... 3 2.3 SCOPE OF SERVICES ......................................................................................................................... 3 3 GEOLOGY AND OBSERVATION OF THE PROJECT .................................................................................... 4 3.1 SITE RECONNAISSANCE .................................................................................................................... 4 3.2 GENERAL GEOLOGY OF THE SITE .................................................................................................... -
Ohio Karst Areas
STATE OF OHIO DEPARTMENT OF NATURAL RESOURCES DIVISION OF GEOLOGICAL SURVEY Ted Strickland, Governor Sean D. Logan, Director Larry Wickstrom, Chief OHIO KARST AREAS ASHTABULA LAKE WILLIAMS FULTON LUCAS GEAUGA OTTAWA TRUMBULL HENRY CUYAHOGA SANDUSKY DEFIANCE ERIE WOOD LORAIN PORTAGE PAULDING HURON MEDINA SUMMIT SENECA PUTNAM HANCOCK MAHONING ASHLAND VAN WERT WYANDOT CRAWFORD RICHL AND WAYNE STARK COLUMBIANA ALLEN HARDIN MERCER CARROLL MARION AUGLAIZE HOLMES MORROW TUSCARAWAS JEFFERSON LOGAN KNOX SHELBY UNION COSHOCTON HARRISON DELAWARE DARKE LICKING CHAMPAIGN MIAMI GUERNSEY MUSKINGUM BELMONT FRANKLIN MADISON CLARK PREBLE FAIRFIELD PERRY MONTGOMERY NOBLE MONROE GREENE PICKAWAY MORGAN FAYETTE HOCKING BUTLER WARREN WASHINGTON CLINTON ROSS ATHENS HIGHLAND VINTON HAMILTON CLERMONT PIKE MEIGS JACKSON BROWN ADAMS GALLIA SCIOTO 0 10 20 30 40 miles LAWRENCE 0 10 20 30 40 50 kilometers EXPLANATION Silurian- and Devonian-age carbonate bedrock overlain by less than 20 feet of glacial drift and/or alluvium Probable karst areas Silurian- and Devonian-age carbonate bedrock overlain Area not known to by more than 20 feet of glacial drift and/or alluvium contain karst features Interbedded Ordovician-age limestone and shale overlain Wisconsinan by less than 20 feet of glacial drift and/or alluvium Glacial Margin Illinoian Interbedded Ordovician-age limestone and shale overlain Glacial Margin by more than 20 feet of glacial drift and/or alluvium OHIO KARST AREAS Karst is a landform that develops on or in limestone, dolomite, or gyp- sinan glacial border in southern Highland and Adams Counties, where sum by dissolution and that is characterized by the presence of character- highly dissected ridges capped by Silurian carbonate rocks rise 150 to 200 istic features such as sinkholes, underground (or internal) drainage through feet above surrounding drainage.