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Salt Caverns &Their Use for Disposal of Oil Field Wastes
An Introduction to Salt Caverns & Their Use for Disposal of Oil Field Wastes An Introduction to Salt Caverns & Their Use for Disposal of Oil Field Wastes Table of Contents What Are Salt Caverns? ........................................................................................... 2 Why Are Salt Caverns Important? ............................................................................ 2 Where Are Salt Deposits and Caverns Found? ......................................................... 3 How Are Caverns Formed?...................................................................................... 4 How Are Caverns Used? .......................................................................................... 5 What Types of Wastes Are Considered to Be Oil Field Wastes? ......................................................................... 6 What Are the Legal Requirements Governing Disposal of Oil Field Wastes into Salt Caverns? ....................................... 7 Are NOW or NORM Wastes Currently Being Disposed of into Caverns?.............................................................. 8 How Are Wastes Put into Caverns? .......................................................................... 9 What Types of Monitoring Are Appropriate for Disposal Caverns?........................................................................ 10 What Happens to the Cavern When It Is Full? ........................................................ 11 What Would Happen if Caverns Leak? .................................................................. -
Bureau of Economic Geology
BUREAU OF ECONOMIC GEOLOGY THE UNIVERSITY OF TEXAS AT AUSTIN W. L. FISHER, DIRECTOR PHASE III: EXAMINATION OF TEXAS SALT DOMES AS POTENTIAL SITES FOR PERMANENT STORAGE . OF TOXIC CHEMICAL WASTE Prepared by S. J. Seni, E. W. Collins, H. S. Hamlin, W. F. Mullican Ill, and D. A. Smith Assisted by L. Falconer and T. Walter Report prepared for the Texas Water Commission under Interagency Contract No. IAC(84-85)-2203 Bureau of Economic Geology W. L. Fisher, Director The University of Texas at Austin University Station, Box X Austin, Texas 78713 November 1985 CONTENTS INTRODUCTION. 1 RECOMMENDATIONS AND CONCLUSIONS, by S. J. Seni • 1 REFERENCES 5 TOPICAL SUMMARIES OF RESEARCH REPORTS, by S. J. Seni 7 Subsidence and Collapse 7 Structural Patterns Around Texas Salt Domes 9 Cap Rock. 10 Cap-Rock Hydrology 13 ACKNOWLEDGMENTS. 15 RESEARCH REPORTS* 17 Subsidence over Texas Salt Domes, by W. F. Mullican III 18 Statistical Analysis of Structure in the Houston Diapir Province, by W. F. Mullican III . 73 Petrography and Structure of Cap Rock with Emphasis on Core from Boling Salt Dome, Texas, by S. J. Seni . · 114 Geology and Hydrogeology, Barbers Hill Salt Dome, Texas, by H. S. Hamlin . · 181 Hydraulics of Cap Rock, Barbers Hill Salt Dome, Texas, by D. A. Smith • 236 Review of the Geology and Plio-Pleistocene to Post-Pleistocene Deformation at Damon Mound Salt Dome, Texas, by E. C. Collins. 275 APPENDIX A. List of domes and codes . 308 * All figures, tables, and references are listed within individual research reports. i i INTRODUCTION This report presents the results of final Phase III research in order to better quantify selected issues associated with permanent storage of toxic chemical wastes in solution mined caverns in salt. -
HGS Bulletin Volume 35 No.9 (May 1993)
May 1993 BULLETIN Volume 35 Number 9 THE GREAT $10.00 "EXPERIMENTAL" EVENING MEETING (See Ad, Page 8, and Meeting Survey, Page 9) * * * HGS JOBS HOTLINE (713)785-9729 * * * IN THIS ISSUE... - South Australia - The southern continental margin.. ........... Page 12 - Can I eat the seafood? .......................................... Page 18 - Estimating reservoir size from seismic .......................... Page 22 - Micromagnetics ................................................ Page 24 - Another party heard from.. ..................................... Page 31 - New happenings at the Houston Museum of Natural Science ..... Page 34 - A collector's guide to vintage oil & gas books ..................... Page 36 - Selecting "The Right" workstation .............................. Page 44 AND MORE! See Centerfold for May Calendar and Geoevents. Non-Exclusive 2D/3D .. , ,\.! , HOUSTON GEOLOGICAL SOCIETY 7171 Harwin. Suite 31 4 Houston. Texas 77036-2190 (713) 785-6402 Fax: (713) 785-0553 Office Hours: 7 a.m. .4 p.m. - EXECUTIVE BOARD - President ....................................................................Patrick T . (Pat) Gordon. Consultant President-Elect ...........................................................John M . Biancardi. Vicksburg Production Vice President .........................................................Dwight (Clint) Moore. Anadarko Petroleum Secretary ........................................................... .Jeannie Fisher Mallick. Excalibur Consultina Treasurer ................................................................. -
THE. PALESTINE SALT DOME, ANDERSON COUNTY, TEXAS. By
THE. PALESTINE SALT DOME, ANDERSON COUNTY, TEXAS. By OLIVER B. HOPKINS. INTRODUCTION. The Palestine salt dome has been known for many years, having been described briefly by Penrose* in 1890 and by Dumble 2 in 1891. The dome was recognized through the occurrence of salt, which was obtained here in small quantities prior to 1890. The production of salt lapsed for many years, but recently the industry has been re vived- and a modern plant producing a large quantity of salt of vari ous grades has been established. There are no conspicuous indica tions of oil or gas here, and so far no deep test wells for oil have been put down. The discovery of tarry oil in a deep well on the Keechi dome, 6 miles north of the Palestine dome, has stimulated interest in the oil possibilities of the' domes of this area and has led to the leas ing of the- lands on and around them. The writer spent one week' in October, 1916, in studying the geology of this dome and the surrounding area. He wishes to offer grateful acknowledgment to Judge O. C. Funderburk, of Palestine, for assistance in the field, and to Mr. A. L. Bowers, president of the Palestine Salt & Coal Co., for information relating to the drilling of salt wells. L. W. Stephenson, of the Geological Survey, studied the Cretaceous fossils from the area, and to him the writer is indebted for much of the information concerning the age of the formations present. LOCATION. The Palestine salt dome is in Anderson County, eastern Texas, 6 miles south of west of Palestine. -
October 1990 HOUSTON GEOLOGICAL SOCIETY BULLETIN Vol
October, 1990 BULLETIN 1 HOUSTON GEOLOGICAL SOCIETY t 7 dume 33 rmber 2 CHECK OUT THE CARBONATE FIELD TRIP! Seepage12 GCAGS CONVENTION See pages 8 & 40 HGS SHRIMP PEEL See page 32 IN THIS ISSUEoo. - Deep Oil Prospects in Trinidad .................................. Page 16 - RCRA: A Historical Perspective ................................. Page 22 - Re-evaluating the Potential of Old Plays ........................ Page 25 - Energy and Destiny: We Must Control Both ..................... Page 29 - Chainsaws and Computers ..................................... Page 42 PL US MORE! (For October Events, see page 1 and Geoevents section, page 33) E rom mne-wem to Atlas Wireline Services I Founded in 1932 as Lane-Wells Co., Atlas 0 Wlreline conveyance servioes - br extended- Wiline Services is now a division of Western reach, horizontal, and difficult-to-service Atlas International, offuing comprehensive wells wireline services worldwide. We've continually tl Global services - a single service from one enhanced our capabilities to offer the latest in location in 1932 to over 100 services from digital data acquisition, analysis, and compietion 80 worldwide locations services for every stage in the life of a well: -. -. Openhole senices - pipe recovery to CBILm 7 ATLAB (Circumferential Borehole Imaging Log) WIREUNE Westam Atlam 0 Cased hde services - perforating to pulsed b'iteirnational P.O. Box 1407 neutron logging Houston. Texas 77251-1407 Produdion 0 bgg@ scnices-injection Open Hole Sewices (713) 972-5739 operations to geothermal services Cased Hole Services (7 13) 972-5766 7he Atlas Advmtage HGS OCTOBER EVENTS MEETINGS OCTOBER 8,1990 (Dinner Meeting) "Evaluation of Untested Stratigraphic Traps in a Pleistocene Canyon-Fill Complex, Offshore Louisiana" Jim Geitgey (see page 10) Westin Oaks Hotel, 5011 Westheimer Social Period 5:30 p.m., Dinner and Meeting 6:30 p.m. -
Salt Tectonics Topics
Salt Tectonics Topics Salt Deposition Salt Movement Diapir Structures Imaging Link to faulting Composition of Salt Domes Salt Deposition Restricted marine basins Mostly halite Minor traces of gypsum or anhydrite Often the two are interbedded and folded Bonneville Salt Flats, Utah Gypsum, Ca(SO ).2H 0 4 2 Halite, NaCl Salt moves driven by buoyancy Sequential Stages of a Salt Diapir •Salt density= 2 g/ cm3 •Salt undergoes no compaction •Mechanically weak - viscous •Shale Density is initially 40% water •Initial Density = 1.8 g/ cm3 •Water expelled during compaction • Final Density = 2.4 g/ cm3 Salt at the Surface Salt Structures -Iran Salt Glacier - Iran Gulf of Gulf of Mexico Mexico Salt Variety of Salt Structures Internal flow of salt Jackson et al. 1990 Detection of Salt Domes Gravity Gravity surveys • Find gravity lows • Low density Seismic Imaging GM-SYS™ Profile model of salt structure integrating seismic reflection, FTG gravity, and magnetic data (EarthExplorer, 2009). Seismic Image of a Salt Dome Geosoft GmsYs-3D model of a salt body embedded in a 3D density volume (Earth Explorer, 2009)_ 3D Seismic Interpretation of Salt Sandbox Experiment Relationship between salt dome and normal faulting Structures http://www.beg.utexas.edu/indassoc/agl/animations/AGL95-MM-001/index.html GUGLIELMO, G., Jr., , B. C. VENDEVILLE, D. D. SCHULTZ-ELA, and M. P. A. JACKSON Bureau of Economic Geology, The University of Texas at Austin, Extension Above Salt Diapir Salt Structures vs. Tectonic Structures •Caused by movement of salt, not by plate -
Salt-Influenced Normal Faulting Related to Salt-Dissolution And
SALT-INFLUENCED NORMAL FAULTING RELATED TO SALT-DISSOLUTION AND EXTENSIONAL TECTONICS: 3D SEISMIC ANALYSIS AND 2D NUMERICAL MODELING OF THE SALT VALLEY SALT WALL, UTAH AND DANISH CENTRAL GRABEN, NORTH SEA by Mohammad Naqi Copyright by Mohammad Naqi 2016 All Rights Reserved i A thesis submitted to the Faculty and the Board of Trustees of the Colorado School of Mines in partial fulfillment of the requirements for the degree of Doctor of Philosophy (Geology). Golden, Colorado Date _________________________ Signed: _______________________ Mohammad Naqi Signed: _______________________ Dr. Bruce Trudgill Thesis Advisor Golden, Colorado Date _________________________ Signed: _______________________ Dr. M. Stephen Enders Professor and Department Head Department of Geology and Geological Engineering ii ABSTRACT The northeastern Paradox basin is characterized by a series of salt cored anticlines (salt walls) trending NW-SE. The crestal areas of the salt cored anticlines are breached and cut by faults, forming downthrown valleys, created by the subsidence of the crestal overburden. There has been a prolonged debate on the causative mechanism of subsidence of the anticline crests. Some researchers, based on field observations favor salt-dissolution of the salt forming the core of the anticlines as the main mechanism for the crestal subsidence. Others based on physical modeling favor extensional tectonics as the main mechanism that triggered subsidence. A wider variety of salt structural styles are present in the Danish Salt Dome Province of the Danish Central Graben, ranging from salt diapirs that penetrate their overlying sedimentary cover, to gentle, non-penetrating salt-cored anticlines. Salt structures present as pillows (e.g. the Kraka salt pillow), diapirs (e.g. -
Salt-Dome Locations in the Gulf Coastal Plain, South-Central United States
SALT-DOME LOCATIONS IN THE GULF COASTAL PLAIN, SOUTH-CENTRAL UNITED STATES By Jeffery D. Beckman and Alex K. Williamson U.S. GEOLOGICAL SURVEY WATER-RESOURCES INVESTIGATIONS REPORT 90-4060 A Contribution of the Regional Aquifer-Systems Analysis Program AUSTIN, TEXAS 1990 DEPARTMENT OF THE INTERIOR MANUEL LUJAN, JR., Secretary UNITED STATES GEOLOGICAL SURVEY Dallas L. Peck, Director For more information Copies of this report can be write to: purchased from: Project Chief U.S. Geological Survey U.S. Geological Survey Books and Open-File Reports Section Gulf Coast RASA Box 25425, Federal Center N. Shore Plaza Bldg., Rm. 104 Denver, CO 80225-5425 55 N. Interregional Hwy. Austin, Texas 78702 CONTENTS Page Abstract...................................................... 1 Introduction.................................................. 1 Purpose and scope............................................. 3 Discrepancies between references .............................. 4 Salt-dome locations and method of compilation................. 4 Dome names .................................................... 6 Dome name coding system....................................... 18 Data description.............................................. 18 Summary....................................................... 19 References cited.............................................. 20 ILLUSTRATIONS Plate 1. Salt-dome locations in the Gulf of Mexico Coastal Plain, south-central United States and the adjacent Continental Shelf In pocket Page » Figure 1. Gulf Coast Regional Aquifer-System -
Descriptive Model of Salt-Dome Sulfur and Contained-Sulfur Model For
U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY Descriptive Model of Salt-Dome Sulfur and Contained-Sulfur Model for Salt-Dome Sulfur by Keith R. Long Open-File Report 92-0403 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards or with the North American Stratigraphic Code. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. 1992 Introduction Salt-dome sulfur deposits are biogenic sulfur deposits that form in the anhydrite-gypsum caprocks of salt domes. They differ from other biogenic sulfur deposits due to the restrictions imposed upon their size and occurrence by the size and location of the host salt-dome caprocks. Biogenic sulfur deposits that occur within bedded evaporites contain as much as 500 million tonnes of sulfur (Long, 1992), considerably larger than the largest known salt-dome sulfur deposit which contains 89 million tonnes of sulfur. The factors which control the distribution of sulfur in salt-dome caprocks are very different from those which control sulfur deposits in bedded evaporites. Salt-domes are distinct geologic bodies that are easy to detect and delineate by geophysical methods. Sulfur, if present, is limited to the caprock. These elementary criteria render exploration and assessment of salt domes for sulfur quite strait forward. Biogenic sulfur deposits that occur in bedded evaporites, however, are controlled by a variety of structural and stratigraphic relationships that are more difficult to recognize and utilize in exploration and mineral resource assessment. -
Salt Densities and Velocities with Application to Gulf of Mexico Salt Domes
Salt densities and velocities with application to Gulf of Mexico salt domes Salt densities and velocities with application to Gulf of Mexico salt domes Jingjing Zong∗, Suleyman Coskun, Robert R. Stewart, Nikolay Dyaur, and Michael T. Myers, University of Houston SUMMARY complicated structures such as salt bodies. We study the densties and elastic properties of rock salt from benchtop ultrasonic measurements, log data analysis in the ULTRASONIC LAB MEASUREMENTS Gulf Coast regions, and seismic survey designs, acquisition and interpretations over salt domes. The ultrasonic pulse-transmission method is often used to find In the lab, we analyzed the composition, density, velocity, and velocities in geologic materials (Vernik and Liu, 1997; Stew- stress effects of a variety of rock salt samples. The tested sam- art et al., 2012). We conduct transmission traveltime recording ples are from very different environment. Salt samples from by using vertical or horizontal pulse transducers (0.5-1 MHz) the Gulf of Mexico region are largely isotropic with mixed as sources and receivers (Figure 1). The tested samples are orientations of micro-cracks and crystal aggregates. The Zi- collected from various locations (Figure 2): Gulf of Mexico paquira,´ colombia samples show velocity and density varia- region (the Hockley salt mine, TX and the Bayou Corne salt tions from their lamination of alternating layers of relatively dome, Louisiana), the Zipaquira´ Salt Mine, Colombia and the pure halite and argillaceous halite. The Goderich, Canada Goderich salt mine, Ontario. From the X-ray powder diffrac- halite crystals display distinct cubic anisotropy, with the elas- tion (XRD) and inductively coupled plasma-mass spectrome- tic constants calculated as: C11=48.7, C44=13.1 and C12=11.9. -
North American Geology
DEPARTMENT OF THE INTERIOR ALBERT B. FALL, Secretary UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, Director 0 Bulletin 731 BIBLIOGRAPHY OF NORTH AMERICAN GEOLOGY FOR 1919-1920 BY JOHN M. NICKLES WASHINGTON GOVERNMENT PRINTING OFFICE 1922 CONTENTS. Page. Introduction ________ ___ ___ 1 Serials examined ___ __ _____ _ _____ _____ __ ____ _ ___ 3 Bibliography _________ _______ _ _______ __ ___ 9 Index _ __ _ _ __i. __ 147 Lists _______ _ ______________ _________________ 241 Chemical analyses _ ____ __ ___ _____ ___ 241 Mineral analyses _ _ ___ _ ____ _ ________ 242 Minerals described __ ____ __ __ _ __________ ___ 242 Rocks described ___ _ ____ __ ___ ____ _ ___ 244 Geologic formations described. ___ __ _ ______ _____ _ __ _ 241 ' BIBLIOGRAPHY 0¥ NORTH AMERICAN GEOLOGY FOB 1919-1920. By JOHN M. NICKLES. INTRODUCTION. The bibliography of North American geology, including paleon tology. petrologj7, and mineralogy, for the years 1919 and 1920 con tains publications on the geology of the Continent of North America and adjacent islands and on Panama and the Hawaiian Islands. It includes textbooks and papers of general character by American au thors, .but not those by foreign authors, except papers that appear in American publications. The papers, with full title and medium of publication and explana tory note if the title is not fully self-explanatory, are listed under the names of their authors, which are arranged in alphabetic order. The author list is followed by an index to the literature listed. The bibliography of North American geology is comprised in the following bulletins of the United States Geological Survey: No. -
Underground Hydrocarbon Storage in Texas
UNDERGROUND HYDROCARBON STORAGE IN TEXAS Tim George McGinnis, Lochridge & Kilgore, L.L.P. [email protected] March 30, 2007 Underground Hydrocarbon Storage in Texas Topics: • Industry Overview • Geology • Ownership • Regulation 1 Industry Overview • Underground hydrocarbon storage has become an increasingly vital link in the Texas economy. 2 • Although a vital link, underground hydrocarbon storage reservoirs and caverns have often been treated as “step-children” of the petroleum, pipeline, and petrochemical industries. 3 • Historically, underground hydrocarbon storage facilities have often been regarded as just big underground “tanks.” • Unfortunately, underground hydrocarbon storage has most often received public attention from leaks, fires, or explosions: 4 • Mont Belvieu – casing leak, explosion, and fires in the 1980s • Brenham – cavern overflow and explosion in 1992 • Moss Bluff – leak and fire in 2004 5 All Forms Of Commercial Hydrocarbons Are Stored Underground • Natural Gas • Crude Oil • NGL and LPG • Hydrogen 6 In Texas, Operators Utilize Three Types Of Underground Formations For Hydrocarbon Storage • Caverns leached in salt domes • Caverns leached in bedded salt • Oil and gas reservoirs, either depleted or partially depleted 7 Texas Underground Storage Reservoirs And Caverns Contain Huge Volumes Of Stored Hydrocarbons • Crude Oil – Hundreds of Millions of Barrels • NGL and LPG — Hundreds of Millions of Barrels • Natural Gas – Hundreds of Bcf 8 Crude Oil Underground Storage • The Department of Energy’s Strategic Petroleum Reserve stores crude oil in two Texas salt domes. – Bryan Mound Salt Dome in Brazoria County – Big Hill Salt Dome in Jefferson County 9 • SPR has two other storage facilities in Louisiana, and a 5th site has been selected in Mississippi.