Composition Variety Complicates Processing Plans for US Shale Gas By: Keith Bullin Phd Peter Krouskop Phd Bryan Research and Engineering Inc
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Deconstructing the Fayetteville Lessons from a Mature Shale Play
Deconstructing the Fayetteville ©Lessons Kimmeridge 2015 from - Deconstructing a Mature the Fayetteville Shale Play June 20151 Introduction The Fayetteville shale gas play lies in the eastern Arkoma Basin, east of the historic oil and gas fields in the central and western parts of the Basin. As one of the most mature, well-developed and well-understood shale gas plays, it offers an unparalleled dataset on which we can look back and review how closely what we “thought we knew” matches “what we now know”, and what lessons there are to be learned in the development of shales and the distribution of the cores of these plays. As we have previously noted (see Figure 1), identifying the core of a shale play is akin to building a Venn diagram based on a number of geological factors. By revisiting the Fayetteville we can rebuild this diagram and overlay it on what is now a vast database of historical wells to see whether it matched expectations, and if not, why not. The data also allows us to review how the development of the play changed (lateral length, completion, etc.) and the variance in performance Figure 1: Schematic of gradational overlap of geologic between operators presents valuable lessons in attributes that define the core of an unconventional whether success is all about the rocks, or whether resource play operator knowledge/insight can make good rocks bad or vice versa. © Kimmeridge 2015 - Deconstructing the Fayetteville 2 Background The Fayetteville shale lies in the eastern Arkoma Basin and ranges in depth from outcrop in the north to 9,000’ at the southern end of the play, with drill depths primarily between 3,000’ and 6,000’. -
Modern Shale Gas Development in the United States: a Primer
U.S. Department of Energy • Office of Fossil Energy National Energy Technology Laboratory April 2009 DISCLAIMER This report was prepared as an account of work sponsored by an agency of the United States Government. Neither the United States Government nor any agency thereof, nor any of their employees, makes any warranty, expressed or implied, or assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed, or represents that its use would not infringe upon privately owned rights. Reference herein to any specific commercial product, process, or service by trade name, trademark, manufacturer, or otherwise does not necessarily constitute or imply its endorsement, recommendation, or favoring by the United States Government or any agency thereof. The views and opinions of authors expressed herein do not necessarily state or reflect those of the United States Government or any agency thereof. Modern Shale Gas Development in the United States: A Primer Work Performed Under DE-FG26-04NT15455 Prepared for U.S. Department of Energy Office of Fossil Energy and National Energy Technology Laboratory Prepared by Ground Water Protection Council Oklahoma City, OK 73142 405-516-4972 www.gwpc.org and ALL Consulting Tulsa, OK 74119 918-382-7581 www.all-llc.com April 2009 MODERN SHALE GAS DEVELOPMENT IN THE UNITED STATES: A PRIMER ACKNOWLEDGMENTS This material is based upon work supported by the U.S. Department of Energy, Office of Fossil Energy, National Energy Technology Laboratory (NETL) under Award Number DE‐FG26‐ 04NT15455. Mr. Robert Vagnetti and Ms. Sandra McSurdy, NETL Project Managers, provided oversight and technical guidance. -
Hydraulic Fracturing in the Barnett Shale
Hydraulic Fracturing in the Barnett Shale Samantha Fuchs GIS in Water Resources Dr. David Maidment University of Texas at Austin Fall 2015 Table of Contents I. Introduction ......................................................................................................................3 II. Barnett Shale i. Geologic and Geographic Information ..............................................................6 ii. Shale Gas Production.........................................................................................7 III. Water Resources i. Major Texas Aquifers ......................................................................................11 ii. Groundwater Wells ..........................................................................................13 IV. Population and Land Cover .........................................................................................14 V. Conclusion ....................................................................................................................16 VI. References....................................................................................................................17 2 I. Introduction Hydraulic Fracturing, or fracking, is a process by which natural gas is extracted from shale rock. It is a well-stimulation technique where fluid is injected into deep rock formations to fracture it. The fracking fluid contains a mixture of chemical components with different purposes. Proppants like sand are used in the fluid to hold fractures in the rock open once the hydraulic -
Blending Hydrogen Into Natural Gas Pipeline Networks: a Review of Key Issues
Blending Hydrogen into Natural Gas Pipeline Networks: A Review of Key Issues M. W. Melaina, O. Antonia, and M. Penev NREL is a national laboratory of the U.S. Department of Energy, Office of Energy Efficiency & Renewable Energy, operated by the Alliance for Sustainable Energy, LLC. Technical Report NREL/TP-5600-51995 March 2013 Contract No. DE-AC36-08GO28308 Blending Hydrogen into Natural Gas Pipeline Networks: A Review of Key Issues M. W. Melaina, O. Antonia, and M. Penev Prepared under Task No. HT12.2010 NREL is a national laboratory of the U.S. Department of Energy, Office of Energy Efficiency & Renewable Energy, operated by the Alliance for Sustainable Energy, LLC. National Renewable Energy Laboratory Technical Report 15013 Denver West Parkway NREL/TP-5600-51995 Golden, Colorado 80401 March 2013 303-275-3000 • www.nrel.gov Contract No. DE-AC36-08GO28308 NOTICE This report was prepared as an account of work sponsored by an agency of the United States government. Neither the United States government nor any agency thereof, nor any of their employees, makes any warranty, express or implied, or assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed, or represents that its use would not infringe privately owned rights. Reference herein to any specific commercial product, process, or service by trade name, trademark, manufacturer, or otherwise does not necessarily constitute or imply its endorsement, recommendation, or favoring by the United States government or any agency thereof. The views and opinions of authors expressed herein do not necessarily state or reflect those of the United States government or any agency thereof. -
Assessing Undiscovered Resources of the Barnett-Paleozoic Total Petroleum System, Bend Arch–Fort Worth Basin Province, Texas* by Richard M
Assessing Undiscovered Resources of the Barnett-Paleozoic Total Petroleum System, Bend Arch–Fort Worth Basin Province, Texas* By Richard M. Pollastro1, Ronald J. Hill1, Daniel M. Jarvie2, and Mitchell E. Henry1 Search and Discovery Article #10034 (2003) *Online adaptation of presentation at AAPG Southwest Section Meeting, Fort Worth, TX, March, 2003 (www.southwestsection.org) 1U.S. Geological Survey, Denver, CO 2Humble Geochemical Services, Humble, TX ABSTRACT Organic-rich Barnett Shale (Mississippian-Pennsylvanian) is the primary source rock for oil and gas that is produced from Paleozoic reservoir rocks in the Bend Arch–Fort Worth Basin Province. Areal distribution and geochemical typing of hydrocarbons in this mature petroleum province indicates generation and expulsion from the Barnett at a depocenter coincident with a paleoaxis of the Fort Worth Basin. Barnett-sourced hydrocarbons migrated westward into reservoir rocks of the Bend Arch and Eastern shelf; however, some oil and gas was possibly sourced by a composite Woodford-Barnett total petroleum system of the Midland Basin from the west. Current U.S. Geological assessments of undiscovered oil and gas are performed using the total petroleum system (TPS) concept. The TPS is composed of mature source rock, known accumulations, and area(s) of undiscovered hydrocarbon potential. The TPS is subdivided into assessment units based on similar geologic characteristics, accumulation type (conventional or continuous), and hydrocarbon type (oil and (or) gas). Assessment of the Barnett-Paleozoic TPS focuses on the continuous (unconventional) Barnett accumulation where gas and some oil are produced from organic-rich siliceous shale in the northeast portion of the Fort Worth Basin. Assessment units are also identified for mature conventional plays in Paleozoic carbonate and clastic reservoir rocks, such as the Chappel Limestone pinnacle reefs and Bend Group conglomerate, respectively. -
Atmospheric Gases Student Handout Atmospheric Gases
Atmospheric Gases Student Handout Atmospheric Gases Driving Question: What is our atmosphere made of? In this activity you will: 1. Explore the variety and ratio of compounds and elements that make up the Earth’s atmosphere. 2. Understand volumetric measurements of gases in the atmosphere. 3. Visually depict the composition of the atmosphere. Background Information: Understanding Concentration Measurements In this activity, we will investigate the gas composition of our planet’s atmosphere. We use percentages to represent units of gas composition. A percent (%) is equivalent to 1 part out of 100 equal units. 1% = 1 part out of 100 For smaller concentrations scientists use parts per million (ppm) to represent concentrations of gases (or pollutants) in the atmosphere). One ppm is equivalent to 1 part out of 1,000,000 if the volume being measured is separated into 1,000,000 equal units. 1 ppm = 1 part out of 1,000,000 In this activity, you will use graph paper to represent the concentration of different gases in the atmosphere. Copyright © 2011 Environmental Literacy and Inquiry Working Group at Lehigh University Atmospheric Gases Student Handout 2 Here are some examples to help visualize parts per million: The common unit mg/liter is equal to ppm concentration Four drops of ink in a 55-gallon barrel of water would produce an "ink concentration" of 1 ppm. 1 12-oz can of soda pop in a 30-meter swimming pool 1 3-oz chocolate bar on a football field Atmospheric Composition Activity You will be creating a graphic model of the atmosphere composition using the Atmospheric Composition of Clean Dry Air activity sheet. -
Tracer Applications of Noble Gas Radionuclides in the Geosciences
To be published in Earth-Science Reviews Tracer Applications of Noble Gas Radionuclides in the Geosciences (August 20, 2013) Z.-T. Lua,b, P. Schlosserc,d, W.M. Smethie Jr.c, N.C. Sturchioe, T.P. Fischerf, B.M. Kennedyg, R. Purtscherth, J.P. Severinghausi, D.K. Solomonj, T. Tanhuak, R. Yokochie,l a Physics Division, Argonne National Laboratory, Argonne, Illinois, USA b Department of Physics and Enrico Fermi Institute, University of Chicago, Chicago, USA c Lamont-Doherty Earth Observatory, Columbia University, Palisades, New York, USA d Department of Earth and Environmental Sciences and Department of Earth and Environmental Engineering, Columbia University, New York, USA e Department of Earth and Environmental Sciences, University of Illinois at Chicago, Chicago, IL, USA f Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, USA g Center for Isotope Geochemistry, Lawrence Berkeley National Laboratory, Berkeley, USA h Climate and Environmental Physics, Physics Institute, University of Bern, Bern, Switzerland i Scripps Institution of Oceanography, University of California, San Diego, USA j Department of Geology and Geophysics, University of Utah, Salt Lake City, USA k GEOMAR Helmholtz Center for Ocean Research Kiel, Marine Biogeochemistry, Kiel, Germany l Department of Geophysical Sciences, University of Chicago, Chicago, USA Abstract 81 85 39 Noble gas radionuclides, including Kr (t1/2 = 229,000 yr), Kr (t1/2 = 10.8 yr), and Ar (t1/2 = 269 yr), possess nearly ideal chemical and physical properties for studies of earth and environmental processes. Recent advances in Atom Trap Trace Analysis (ATTA), a laser-based atom counting method, have enabled routine measurements of the radiokrypton isotopes, as well as the demonstration of the ability to measure 39Ar in environmental samples. -
A Comparative Study of the Mississippian Barnett Shale, Fort Worth Basin, and Devonian Marcellus Shale, Appalachian Basin
DOE/NETL-2011/1478 A Comparative Study of the Mississippian Barnett Shale, Fort Worth Basin, and Devonian Marcellus Shale, Appalachian Basin U.S. DEPARTMENT OF ENERGY DISCLAIMER This report was prepared as an account of work sponsored by an agency of the United States Government. Neither the United States Government nor any agency thereof, nor any of their employees, makes any warranty, expressed or implied, or assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed, or represents that its use would not infringe upon privately owned rights. Reference herein to any specific commercial product, process, or service by trade name, trademark, manufacturer, or otherwise does not necessarily constitute or imply its endorsement, recommendation, or favoring by the United States Government or any agency thereof. The views and opinions of authors expressed herein do not necessarily state or reflect those of the United States Government or any agency thereof. ACKNOWLEDGMENTS The authors greatly thank Daniel J. Soeder (U.S. Department of Energy) who kindly reviewed the manuscript. His criticisms, suggestions, and support significantly improved the content, and we are deeply grateful. Cover. Top left: The Barnett Shale exposed on the Llano uplift near San Saba, Texas. Top right: The Marcellus Shale exposed in the Valley and Ridge Province near Keyser, West Virginia. Photographs by Kathy R. Bruner, U.S. Department of Energy (USDOE), National Energy Technology Laboratory (NETL). Bottom: Horizontal Marcellus Shale well in Greene County, Pennsylvania producing gas at 10 million cubic feet per day at about 3,000 pounds per square inch. -
Study Develops Fayetteville Shale Reserves, Production Forecast John Browning Katie Smye a Study of Reserve and Production Potential for the Fayette- Scott W
Study develops Fayetteville Shale reserves, production forecast John Browning Katie Smye A study of reserve and production potential for the Fayette- Scott W. Tinker Susan Horvath ville Shale in north central Arkansas forecasts a cumulative Svetlana Ikonnikova Tad Patzek 18 tcf of economically recoverable reserves by 2050, with Gürcan Gülen Frank Male production declining to about 400 bcf/year by 2030 from Eric Potter Forrest Roberts the current peak of about 950 bcf/year. Qilong Fu Carl Grote The forecast suggests the formation will continue to be a The University of Texas major contributor to U.S. natural gas production. Austin The Bureau of Economic Geology (BEG) at The University In this cross section of the Fayetteville Shale, the pay zone is identified by lines correlated between logs. Shaded areas of density-log porosity (DPhi) curve represent DPhi values less than 5%. The map shows the location of the cross section. TECHNOLOGY 1 FAYETTEVILLE POROSITY * THICKNESS (PHI*H) FIG. 2 Contours,2 density porosity-ft Stone 5 8 11 14 17 20 23 26 29 32 35 38 41 44 47 50 Batesville Van Buren Cleburne Independence Pope Conway Faulkner Area shown White Conway 0 Miles 25 Arkansas 0 Km 40 1With 60° NE trend bias to reect fault trends. 2Porosity is net from density logs (DPhi). of Texas at Austin conducted the study, integrating engineer- sient flow model for the first 3-5 years, resulting in decline ing, geology, and economics into a numerical model that al- rates inversely proportional to the square root of time, later lows for scenario testing on the basis of an array of technical shifting to exponential decline as a result of interfracture and economic parameters. -
U.S. Shale Gas
U.S. Shale Gas An Unconventional Resource. Unconventional Challenges. WHITE PAPER U.S. Shale Gas An Unconventional Resource . Unconventional Challenges . Executive Summary Current increasing demand and lagging supply mean high prices for both oil and gas, making exploitation of North American unconventional gas plays suddenly far more lucrative for producers. One of the most important such plays to emerge has been U.S. shale gas, with current recoverable reserves conservatively estimated at 500 to 1,000 trillion cubic feet. Hydraulic fracturing and horizontal drilling are the key enabling technologies that first made recovery of shale gas economically viable with their introduction in the Barnett Shale of Texas during the 1990s. However, a comparison of the currently hottest shale plays makes it clear that, after two decades of development and several iterations of the learning curve, best practices are application-dependent and must evolve locally. That said, a review of current trends in these hot plays indicates that, in many cases, the impact of high-drilling density required to develop continuous gas accumulations can be minimized through early and better identification of the accumulation type and size, well- designed access and transportation networks, and cooperative planning and construction efforts, when possible. U.S. Shale Gas Geographic Potential Across the U.S., from the West Coast to the Northeast, some 19 geographic basins are recognized sources of shale gas, where an estimated 35,000 wells were drilled in 2006. Presently, significant commercial gas shale production occurs in the Barnett Shale in the Fort Worth Basin, Lewis Shale in the San Juan Basin, Antrim Shale in the Michigan Basin, Marcellus Shale and others in the Appalachian Basin, and New Albany Shale in the Illinois Basin. -
Bossier Bossier
CENTER FOR ENERGY STUDIES BOSSIER - HAYNESVILLE SHALE: NORTH LOUISIANA SALT BASIN D. A. GODDARD, E. A. MANCINI, S. C. TALUKAR & M. HORN Louisiana State University Baton Rouge , Louisiana 1 OVERVIEW Regional Geological Setting Total Organic Carbon & RockRock--EvalEval Pyrolisis Kerogen Petrography Thin Section Petrography Naturally Fractured Shale Reservoirs Conclusions 2 Gulf Coast Interior Basins Gulf Coast Interior Salt Basins Mancini and Puckett, 2005 3 TYPE LOG 4 Type Wells 5 Bossier Parish Wells 6 BossierBossier--HaynesvilleHaynesville samples in NLSB . (LA Parish) Sample (Serial #) OP/Well Name Core Interval Depth-Ft (Jackson) 10,944 (162291) AMOCO Davis Bros. Bossier Fm. 10, 945 10,948 Haynesville Fm. 12,804 12,956 12,976 (164798) AMOCO CZ 5-7 (Winn) 15,601 Bossier Fm. 15, 608 Haynesville Fm. 16,413 16,418 16,431 16,432 (166680) EXXON Pardee (Winn) 16195 Bossier Fm. 16, 200 16,400 (107545) Venzina Green #1 (Union) 9,347 Bossier Fm. 9,357 9,372 7 8 Bossier -Haynesville samples in Vernon Field Serial. # Operator Well Field Sec TWP RGE Parish Sample Depth- Ft 224274 Anadarko Fisher 16 #1 Vernon 16 16N 02W Jackson 13,175 13,770 226742 Anadarko Davis Bros 29 Vernon 29 16N 02W Jackson 14,035 15,120 231813 Anadarko Beasley 9 #2 Vernon 9 16N 02W Jackson 11,348 232316 Anadarko StewtHarrison Vernon 34 16N 03W Jackson 11,805 34 #2 9 Modified from Structuremaps.com 10 11 12 13 Analytical results of Total Organic Carbon, RockRock--EvalEval PyrolysisPyrolysis,, and Vitrinite Reflectance (Ro) in the NLSB. Depth % TOC Wt S1 S2 S3 Well Sample (Ft) % mg/g mg/g mg/g Tmax HI OI S1/TOC PI TAI Ro AMOCO DAVIS Cotton V. -
Shallow Groundwater Quality and Geochemistry in the Fayetteville Shale Gas-Production Area, North-Central Arkansas, 2011
Prepared in cooperation with (in alphabetical order) the Arkansas Natural Resources Commission, Arkansas Oil and Gas Commission, Duke University, Faulkner County, Shirley Community Development Corporation, and the University of Arkansas at Fayetteville, and the U.S. Geological Survey Groundwater Resources Program Shallow Groundwater Quality and Geochemistry in the Fayetteville Shale Gas-Production Area, North-Central Arkansas, 2011 Scientific Investigations Report 2012–5273 U.S. Department of the Interior U.S. Geological Survey Cover: Left, Drilling rig and equipment used in the Fayetteville Shale gas-production area, north-central Arkansas. Right, Pond with synthetic liner used to store water at shale gas-production facility in the Fayetteville Shale area, north-central Arkansas. Bottom, Freshwater pond and distribution lines for source water used in drilling and hydrofracturing in the Fayetteville Shale gas-production area, north-central Arkansas. All photographs by Timothy M. Kresse, U.S. Geological Survey. Shallow Groundwater Quality and Geochemistry in the Fayetteville Shale Gas-Production Area, North-Central Arkansas, 2011 By Timothy M. Kresse, Nathaniel R. Warner, Phillip D. Hays, Adrian Down, Avner Vengosh, Robert B. Jackson Prepared in cooperation with (in alphabetical order) the Arkansas Natural Resources Commission, Arkansas Oil and Gas Commission, Duke University, Faulkner County, Shirley Community Development Corporation, and the University of Arkansas at Fayetteville, and the U.S. Geological Survey Groundwater Resources Program Scientific Investigations Report 2012–5273 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior KEN SALAZAR, Secretary U.S. Geological Survey Marcia K. McNutt, Director U.S. Geological Survey, Reston, Virginia: 2012 This and other USGS information products are available at http://store.usgs.gov/ U.S.