Byron/Braidwood Nuclear Stations, Updated Final Safety Analysis Report

Total Page:16

File Type:pdf, Size:1020Kb

Byron/Braidwood Nuclear Stations, Updated Final Safety Analysis Report BRAIDWOOD-UFSAR CHAPTER 2.0 - SITE CHARACTERISTICS TABLE OF CONTENTS PAGE 2.0 SITE CHARACTERISTICS 2.1-1 2.1 GEOGRAPHY AND DEMOGRAPHY 2.1-1 2.1.1 Site Location and Description 2.1-1 2.1.1.1 Specification of Location 2.1-1 2.1.1.2 Site Area Map 2.1-1 2.1.1.3 Boundaries for Establishing Effluent Release Limits 2.1-2 2.1.2 Exclusion Area Authority and Control 2.1-3 2.1.2.1 Authority 2.1-3 2.1.2.2 Control of Activities Unrelated to Plant Operation 2.1-3 2.1.2.3 Arrangements for Traffic Control 2.1-3 2.1.2.4 Abandonment or Relocation of Roads 2.1-3 2.1.3 Population Distribution 2.1-4 2.1.3.1 Population Within 10 Miles 2.1-5 2.1.3.2 Population Between 10 and 50 Miles 2.1-5 2.1.3.3 Transient Population 2.1-6 2.1.3.4 Low Population Zone 2.1-7 2.1.3.5 Population Center 2.1-8 2.1.3.6 Population Density 2.1-9 2.1.4 References 2.1-9 2.2 NEARBY INDUSTRIAL, TRANSPORTATION, AND MILITARY FACILITIES 2.2-1 2.2.1 Locations and Routes 2.2-1 2.2.2 Descriptions 2.2-3 2.2.2.1 Description of Facilities 2.2-3 2.2.2.2 Description of Products and Materials 2.2-3 2.2.2.3 Pipelines 2.2-3 2.2.2.4 Waterways 2.2-4 2.2.2.5 Airports 2.2-4 2.2.2.6 Projections of Industrial Growth 2.2-5 2.2.3 Evaluation of Potential Accidents 2.2-5 2.2.3.1 Determination of Design Basis Events 2.2-5 2.2.3.1.1 Explosions 2.2-5 2.2.3.1.2 Flammable Vapor Clouds (Delayed Ignition) 2.2-6 2.2.3.1.3 Toxic Chemicals 2.2-7 2.2.3.1.4 Fires 2.2-7 2.2.3.1.5 Collisions with Intake Structure 2.2-7 2.2.3.1.6 Liquid Spills 2.2-7 2.2.4 References 2.2-7 2.0-i REVISION 9 – DECEMBER 2002 BRAIDWOOD-UFSAR TABLE OF CONTENTS (Cont’d) PAGE 2.3 METEOROLOGY 2.3-1 2.3.1 Regional Climatology 2.3-1 2.3.1.1 General Climate 2.3-1 2.3.1.2 Regional Meteorological Conditions for Design and Operating Bases 2.3-4 2.3.1.2.1 Thunderstorms, Hail, and Lightning 2.3-4 2.3.1.2.2 Tornadoes and Severe Winds 2.3-6 2.3.1.2.3 Heavy Snow and Severe Glaze Storms 2.3-8 2.3.1.2.4 Ultimate Heat Sink Design 2.3-9 2.3.1.2.5 Inversions and High Air Pollution Potential 2.3-10 2.3.2 Local Meteorology 2.3-12 2.3.2.1 Normal and Extreme Values of Meteorological Parameters 2.3-12 2.3.2.1.1 Winds 2.3-12 2.3.2.1.2 Temperatures 2.3-15 2.3.2.1.3 Atmospheric Moisture 2.3-16 2.3.2.1.3.1 Relative Humidity 2.3-16 2.3.2.1.3.2 Dew-Point Temperature 2.3-17 2.3.2.1.4 Precipitation 2.3-18 2.3.2.1.4.1 Precipitation Measured as Water Equivalent 2.3-18 2.3.2.1.4.2 Precipitation Measured as Snow or Ice Pellets 2.3-20 2.3.2.1.5 Fog 2.3-20 2.3.2.1.6 Atmospheric Stability 2.3-21 2.3.2.2 Potential Influence of the Plant and Its Facilities on Local Meteorology 2.3-24 2.3.2.3 Topographical Description 2.3-26 2.3.3 Onsite Meteorological Measurements Program 2.3-26 2.3.4 Short-Term (Accident) Diffusion Estimates 2.3-33 2.3.4.1 Objective 2.3-33 2.3.4.2 Calculations (For use with TID-14844 based dose analyses) 2.3-33 2.3.5 Long-Term (Routine) Diffusion Estimates (For TID- 14844 based dose analyses) 2.3-35 2.3.5.1 Objective (For TID-14844 based dose analyses) 2.3-35 2.3.5.2 Calculations (For TID-14844 based dose analyses) 2.3-35 2.3.5.2.1 Joint Frequency Distribution of Wind Direction, Wind Speed and Stability (For TID- 14844 based dose analyses) 2.3-36 2.3.5.2.2 Effective Release Height (For TID-14844 based dose analyses) 2.3-38 2.3.5.2.3 Annual Average Atmospheric Dilution Factor (For TID-14844 based dose analyses) 2.3-40 2.3.6 Short-term (Accident) Diffusion Estimates (Alternative Source Term /Q Analysis) 2.3-42 2.3.6.1 Objective 2.3-42 2.3.6.2 Meteorological Data 2.3-42 2.3.6.3 Calculation of /Q at the EAB and LPZ 2.3-42 2.0-ii REVISION 12 – DECEMBER 2008 BRAIDWOOD-UFSAR TABLE OF CONTENTS (Cont’d) 2.3.6.3.1 PAVAN Meteorological Database 2.3-42b 2.3.6.3.2 PAVAN Model Input Parameters 2.3-42c 2.3.6.3.3 PAVAN EAB and LPZ χ/Q 2.3-42c 2.3.6.4 Calculation of χ/Q at the Control Room Intakes 2.3-42d 2.3.6.4.1 ARCON96 Model Analysis 2.3-42d 2.3.6.4.1.1 ARCON96 Meteorological Database 2.3-42f 2.3.6.4.1.2 ARCON96 Input Parameters 2.3-42f 2.3.6.4.1.3 ARCON96 Control Room Intake χ/Q 2.3-43 2.0-iia REVISION 12 – DECEMBER 2008 BRAIDWOOD-UFSAR TABLE OF CONTENTS (Cont’d) PAGE 2.3.7 References 2.3-43 2.4 HYDROLOGIC ENGINEERING 2.4-1 2.4.1 Hydrologic Description 2.4-1 2.4.1.1 Site and Facilities 2.4-1 2.4.1.2 Hydrosphere 2.4-2 2.4.2 Floods 2.4-4 2.4.2.1 Flood History 2.4-4 2.4.2.2 Flood Design Considerations 2.4-4 2.4.2.3 Effects of Local Intense Precipitation 2.4-5 2.4.3 Probable Maximum Floods (PMF) on Steams and Rivers 2.4-8 2.4.3.1 Probable Maximum Precipitation (PMP) on the Kankakee River, the Mazon River, and Crane and Granary Creeks 2.4-9 2.4.3.2 Precipitation Losses on the Kankakee River, the Mazon River, and Crane and Granary Creeks 2.4-9 2.4.3.3 Runoff and Stream Course Models for the Kankakee River, the Mazon River, and Crane and Granary Creeks 2.4-10 2.4.3.4 Probable Maximum Flood Flow on the Kankakee River, the Mazon River, and Crane and Granary Creeks 2.4-10 2.4.3.5 Water Level Determination for the Kankakee River, the Mazon River, and Crane And Granary Creeks 2.4-11 2.4.3.6 Coincident Wind Wave Activity 2.4-13 2.4.4 Potential Dam Failures, Seismically Induced 2.4-13 2.4.5 Probable Maximum Surge and Seiche Flooding 2.4-13 2.4.6 Probable Maximum Tsunami Flooding 2.4-13 2.4.7 Ice Effects 2.4-13 2.4.8 Cooling Water Canals and Reservoirs 2.4-14 2.4.8.1 Pipelines 2.4-14 2.4.8.2 Cooling Pond 2.4-14 2.4.8.2.1 Probable Maximum Precipitation on the Pond 2.4-14 2.4.8.2.2 Precipitation Losses 2.4-15 2.4.8.2.3 Runoff Model 2.4-15 2.4.8.2.4 Probable Maximum Flood Flow for Cooling Pond 2.4-16 2.4.8.2.5 Water Level Determinations 2.4-16 2.4.8.2.6 Coincident Wind Wave Activity 2.4-16 2.4.9 Channel Diversions 2.4-18 2.4.10 Flooding Protection Requirements 2.4-19 2.4.11 Low Water Considerations 2.4-20 2.4.11.1 Low Flow in Rivers 2.4-20 2.4.11.2 Low Water Resulting from Surges, Seiches, or Tsunami 2.4-20 2.0-iii REVISION 12 - DECEMBER 2008 BRAIDWOOD-UFSAR TABLE OF CONTENTS (Cont’d) PAGE 2.4.11.3 Historical Low Flow 2.4-20 2.4.11.4 Future Controls 2.4-20 2.4.11.5 Plant Requirements 2.4-21 2.4.11.6 Heat Sink Dependability Requirements 2.4-22 2.4.12 Dispersion, Dilution, and Travel Times of Accidental Releases of Liquid Effluents In Surface Water 2.4-24 2.4.13 Groundwater 2.4-25 2.4.13.1 Description and Onsite Use 2.4-25 2.4.13.1.1 Onsite Use 2.4-25 2.4.13.1.2 Site and Regional Conditions 2.4-25 2.4.13.2 Sources 2.4-28 2.4.13.2.1 Present and Future Groundwater Use 2.4-28 2.4.13.2.2 Site Hydrogeologic Conditions 2.4-29 2.4.13.2.2.1 Permeability 2.4-29 2.4.13.2.2.2 Groundwater Levels 2.4-30 2.4.13.2.3 Effects of Seepage from Cooling Pond 2.4-31 2.4.13.2.4 Seepage from the Essential Service Cooling Pond 2.4-32 2.4.13.3 Accident Effects 2.4-32 2.4.13.4 Monitoring 2.4-33 2.4.13.5 Design Bases for Subsurface Hydrostatic Loading 2.4-34 2.4.14 Technical Specification and Emergency Operating Requirements 2.4-34 2.4.14.1 Probable Maximum Flood Level 2.4-34 2.4.14.2 Flood Protection Measures 2.4-35 2.4.14.3 Emergency Protective Measures 2.4-35 2.4.15 References 2.4-35 2.4.15.1 References Cited in Text 2.4-35 2.4.15.2 Alphabetical List of References Not Cited in Text 2.4-37 2.5 GEOLOGY, SEISMOLOGY, AND GEOTECHNICAL ENGINEERING 2.5-1 2.5.1 Basic Geologic and Seismic Data 2.5-1 2.5.1.1 Regional Geology 2.5-1 2.5.1.1.1 Regional Geologic History 2.5-1 2.5.1.1.1.1 General 2.5-1 2.5.1.1.1.2 Precambrian (Earlier than Approximately 600 Million Years B.P.) 2.5-2 2.5.1.1.1.3 Cambrain (Approximately 500 to Approximately 600 Million Year B.P.) 2.5-2 2.5.1.1.1.4 Ordovician (430 + 10 to Approximately 500 Million Years B.P.) 2.5-3 2.5.1.1.1.5 Silurian (400 + 10 to 430 + 10 Million Years B.P.) 2.5-4 2.0-iv BRAIDWOOD-UFSAR TABLE OF CONTENTS (Cont’d) PAGE 2.5.1.1.1.6 Devonian (340 + 10 to 400 + 10 Million Years B.P.) 2.5-4 2.5.1.1.1.7 Mississippian (320 + 10 to 340 + 10 Million Years B.P.) 2.5-4 2.5.1.1.1.8 Pennsylvanian (270 + 5 to 320 + 10 Million Years B.P.) 2.5-5 2.5.1.1.1.9 Permian (225 + 5 to 270 + 5 Million Years B.P.) 2.5-5 2.5.1.1.1.10 Triassic (190 + 5 to 225 + 5 Million Years B.P.) 2.5-5 2.5.1.1.1.11 Jurassic (135 + 5 to 190 + 5 Million Years B.P.) 2.5-5 2.5.1.1.1.12 Cretaceous (65 + 2 to 135 + 5 Million Years B.P.) 2.5-5 2.5.1.1.1.13 Quaternary (Present to 2 + 1 Million Years B.P.) 2.5-6 2.5.1.1.2 Physiography 2.5-6 2.5.1.1.3 Stratigraphy 2.5-7 2.5.1.1.3.1 Soil Units 2.5-7 2.5.1.1.3.2 Rock Units 2.5-8 2.5.1.1.4 Structures 2.5-8 2.5.1.1.4.1 Folding 2.5-8 2.5.1.1.4.1.1 Illinois Basin 2.5-8 2.5.1.1.4.1.2 Wisconsin Arch and Kankakee Arch 2.5-9 2.5.1.1.4.1.3 LaSalle Anticlinal Belt 2.5-9 2.5.1.1.4.1.4 Ashton Arch 2.5-9 2.5.1.1.4.1.5 Herscher Dome 2.5-10 2.5.1.1.4.1.6 Downs Anticline 2.5-10 2.5.1.1.4.1.7 Mattoon Anticline 2.5-10 2.5.1.1.4.1.8 Tuscola Anticline 2.5-10 2.5.1.1.4.1.9 Murdock Syncline 2.5-10 2.5.1.1.4.1.10 Marshall Syncline 2.5-10 2.5.1.1.4.1.11 Folded Structures Associated with the Plum River Fault Zone 2.5-11 2.5.1.1.4.1.12 Louden Anticline 2.5-11 2.5.1.1.4.1.13 Salem Anticline 2.5-11 2.5.1.1.4.1.14 Clay City Anticline 2.5-11 2.5.1.1.4.1.15 DuQuoin Monocline 2.5-11 2.5.1.1.4.1.16 Mississippi River Arch 2.5-12 2.5.1.1.4.1.17 Pittsfield and Lincoln Anticlines 2.5-12 2.5.1.1.4.1.18 Mineral Point and Meekers Grove Anticlines 2.5-12 2.5.1.1.4.1.19 Baraboo, Fond du Lac, and Waterloo Synclines 2.5-12 2.5.1.1.4.1.20 Leesville Anticline 2.5-12 2.5.1.1.4.1.21 Michigan Basin 2.5-13 2.5.1.1.4.1.22 Structural Contour Maps 2.5-13 2.5.1.1.4.2 Faulting 2.5-14 2.0-v BRAIDWOOD-UFSAR TABLE OF CONTENTS (Cont’d) PAGE 2.5.1.1.4.2.1 Sandwich Fault Zone and Plum River Fault Zone 2.5-14 2.5.1.1.4.2.2 Chicago Area Faults 2.5-14 2.5.1.1.4.2.2.1 Chicago Area Basement Fault Zone 2.5-14 2.5.1.1.4.2.2.2 Chicago Area Minor Faults 2.5-14 2.5.1.1.4.2.3 Oglesby and Tuscola Faults 2.5-15 2.5.1.1.4.2.4 Centralia Fault 2.5-15 2.5.1.1.4.2.5 Cap Au Gres Faulted Flexure 2.5-15 2.5.1.1.4.2.6 Mifflin Fault 2.5-15 2.5.1.1.4.2.7 Postulated Wisconsin Faults 2.5-16 2.5.1.1.4.2.8 Mt.
Recommended publications
  • Stratographic Coloumn of Iowa
    Iowa Stratographic Column November 4, 2013 QUATERNARY Holocene Series DeForest Formation Camp Creek Member Roberts Creek Member Turton Submember Mullenix Submember Gunder Formation Hatcher Submember Watkins Submember Corrington Formation Flack Formation Woden Formation West Okoboji Formation Pleistocene Series Wisconsinan Episode Peoria Formation Silt Facies Sand Facies Dows Formation Pilot Knob Member Lake Mills Member Morgan Member Alden Member Noah Creek Formation Sheldon Creek Formation Roxana/Pisgah Formation Illinoian Episode Loveland Formation Glasford Formation Kellerville Memeber Pre-Illinoian Wolf Creek Formation Hickory Hills Member Aurora Memeber Winthrop Memeber Alburnett Formation A glacial tills Lava Creek B Volcanic Ash B glacial tills Mesa Falls Volcanic Ash Huckleberry Ridge Volcanic Ash C glacial tills TERTIARY Salt & Pepper sands CRETACEOUS "Manson" Group "upper Colorado" Group Niobrara Formation Fort Benton ("lower Colorado ") Group Carlile Shale Greenhorn Limestone Graneros Shale Dakota Formation Woodbury Member Nishnabotna Member Windrow Formation Ostrander Member Iron Hill Member JURASSIC Fort Dodge Formation PENNSYLVANIAN (subsystem of Carboniferous System) Wabaunsee Group Wood Siding Formation Root Formation French Creek Shale Jim Creek Limestone Friedrich Shale Stotler Formation Grandhaven Limestone Dry Shale Dover Limestone Pillsbury Formation Nyman Coal Zeandale Formation Maple Hill Limestone Wamego Shale Tarkio Limestone Willard Shale Emporia Formation Elmont Limestone Harveyville Shale Reading Limestone Auburn
    [Show full text]
  • Rock Stratigraphy of the Silurian System in Northeastern and Northwestern Illinois
    2UJ?. *& "1 479 S 14.GS: CIR479 STATE OF ILLINOIS c. 1 DEPARTMENT OF REGISTRATION AND EDUCATION Rock Stratigraphy of the Silurian System in Northeastern and Northwestern Illinois H. B. Willman GEOLOGICAL ILLINOIS ""SURVEY * 10RM* APR 3H986 ILLINOIS STATE GEOLOGICAL SURVEY John C. Frye, Chief Urbano, IL 61801 CIRCULAR 479 1973 CONTENTS Page Abstract 1 Introduction 1 Time-stratigraphic classification 3 Alexandrian Series 5 Niagaran Series 5 Cayugan Series 6 Regional correlations 6 Northeastern Illinois 6 Development of the classification 9 Wilhelmi Formation 12 Schweizer Member 13 Birds Member 13 Elwood Formation 14 Kankakee Formation 15 Drummond Member 17 Offerman Member 17 Troutman Member 18 Plaines Member 18 Joliet Formation 19 Brandon Bridge Member 20 Markgraf Member 21 Romeo Member 22 Sugar Run Formation . „ 22 Racine Formation 24 Northwestern Illinois 26 Development of the classification 29 Mosalem Formation 31 Tete des Morts Formation 33 Blanding Formation 35 Sweeney Formation 36 Marcus Formation 3 7 Racine Formation 39 References 40 GEOLOGIC SECTIONS Northeastern Illinois 45 Northwestern Illinois 52 FIGURES Figure 1 - Distribution of Silurian rocks in Illinois 2 2 - Classification of Silurian rocks in northeastern and northwestern Illinois 4 3 - Correlation of the Silurian formations in Illinois and adjacent states 7 - CM 4 Distribution of Silurian rocks in northeastern Illinois (modified from State Geologic Map) 8 - lis. 5 Silurian strata in northeastern Illinois 10 ^- 6 - Development of the classification of the Silurian System in |§ northeastern Illinois 11 7 - Distribution of Silurian rocks in northwestern Illinois (modified ;0 from State Geologic Map) 2 7 8 - Silurian strata in northwestern Illinois 28 o 9 - Development of the classification of the Silurian System in CO northwestern Illinois 30 10 - Index to stratigraphic units described in the geologic sections • • 46 ROCK STRATIGRAPHY OF THE SILURIAN SYSTEM IN NORTHEASTERN AND NORTHWESTERN ILLINOIS H.
    [Show full text]
  • Deep Oil Possibilities of the Illinois Basin
    s Ccc 36? STATE OF ILLINOIS DEPARTMENT OF REGISTRATION AND EDUCATION DEEP OIL POSSIBILITIES OF THE ILLINOIS BASIN Alfred H. Bell Elwood Atherton T. C. Buschbach David H. Swann ILLINOIS STATE GEOLOGICAL SURVEY John C. Frye, Chief URBANA CIRCULAR 368 1964 . DEEP OIL POSSIBILITIES OF THE ILLINOIS BASIN Alfred H. Bell, Elwood Atherton, T. C. Buschbach, and David H. Swann ABSTRACT The Middle Ordovician and younger rocks of the Illinois Basin, which have yielded 3 billion barrels of oil, are underlain by a larger volume of virtually untested Lower Ordovician and Cambrian rocks. Within the region that has supplied 99 percent of the oil, where the top of the Middle Ordovician (Trenton) is more than 1,000 feet be- low sea level, less than 8 inches of hole have been drilled per cubic mile of the older rocks. Even this drilling has been near the edges; and in the central area, which has yielded five- sixths of the oil, only one inch of test hole has been drilled per cubic mile of Lower Ordovician and Cambrian. Yet drilling depths are not excessive, ranging from 6,000 to 14,000 feet to the Precambrian. More production may be found in the Middle Ordovician Galena Limestone (Trenton), thus extending the present productive regions. In addition, new production may be found in narrow, dolomitized fracture zones in the tight limestone facies on the north flank of the basin . The underlying Platteville Limestone is finer grained and offers fewer possibilities. The Joachim Dolomite oil- shows occur in tight sandstone bodies that should have commercial porosity in some re- gions.
    [Show full text]
  • Geology and Oil Production in the Tuscola Area, Illinois
    124 KUItOfS GEOLOGICAL S SURVEY LIBRARY 14.GS: 4^ ^ CIR 424 :. 1 STATE OF ILLINOIS DEPARTMENT OF REGISTRATION AND EDUCATION Geology and Oil Production in the Tuscola Area, Illinois H. M. Bristol Ronald Prescott ILLINOIS STATE GEOLOGICAL SURVEY John C. Frye, Chief URBANA CIRCULAR 424 1968 Digitized by the Internet Archive in 2012 with funding from University of Illinois Urbana-Champaign http://archive.org/details/geologyoilproduc424bris GEOLOGY AND OIL PRODUCTION IN THE TUSCOLA AREA, ILLINOIS H. M. Bristol and Ronald Prescott ABSTRACT The Tuscola Anticline, in east-central Illinois, lies astride the complex LaSalle Anticlinal Belt and dips steeply westward into the Fairfield Basin and gradually eastward into the Murdock Syncline. The anticline is broken into two structural highs, the Hayes Dome and the Shaw Dome. Pleistocene sediments, 50 to 250 feet thick, cover the area. Pennsylvanian sediments cover much of the area, thinning to expose an inlier of Mississippian, Devonian, and Silurian rock north of Tuscola. The basal Cambrian for- mation, the Mt. Simon Sandstone, is penetrated by only two wells. Oil production from the Kimmswick (Trenton) com- menced in 1962 from the R. D. Ernest No. 1 Schweighart well, near Hayes, and as of January 1, 1968, approximately 30 wells were producing oil. Cumulative oil production as of January 1, 1968, is approximately 94,000 barrels. The potential pay zone is confined to the upper 5 to 100 feet of structure and to the upper 125 feet of the Kimmswick, whose permeability ranges from 0.1 to 2. millidarcys, av- eraging 0.6, and whose porosity ranges from 2 to 12 per- cent.
    [Show full text]
  • Braidwood-Ufsar
    BRAIDWOOD-UFSAR CHAPTER 2.0 - SITE CHARACTERISTICS TABLE OF CONTENTS PAGE 2.0 SITE CHARACTERISTICS 2.1-1 2.1 GEOGRAPHY AND DEMOGRAPHY 2.1-1 2.1.1 Site Location and Description 2.1-1 2.1.1.1 Specification of Location 2.1-1 2.1.1.2 Site Area Map 2.1-1 2.1.1.3 Boundaries for Establishing Effluent Release Limits 2.1-2 2.1.2 Exclusion Area Authority and Control 2.1-3 2.1.2.1 Authority 2.1-3 2.1.2.2 Control of Activities Unrelated to Plant Operation 2.1-3 2.1.2.3 Arrangements for Traffic Control 2.1-3 2.1.2.4 Abandonment or Relocation of Roads 2.1-3 2.1.3 Population Distribution 2.1-4 2.1.3.1 Population Within 10 Miles 2.1-5 2.1.3.2 Population Between 10 and 50 Miles 2.1-5 2.1.3.3 Transient Population 2.1-6 2.1.3.4 Low Population Zone 2.1-7 2.1.3.5 Population Center 2.1-8 2.1.3.6 Population Density 2.1-9 2.1.4 References 2.1-9 2.2 NEARBY INDUSTRIAL, TRANSPORTATION, AND MILITARY FACILITIES 2.2-1 2.2.1 Locations and Routes 2.2-1 2.2.2 Descriptions 2.2-3 2.2.2.1 Description of Facilities 2.2-3 2.2.2.2 Description of Products and Materials 2.2-3 2.2.2.3 Pipelines 2.2-3 2.2.2.4 Waterways 2.2-4 2.2.2.5 Airports 2.2-4 2.2.2.6 Projections of Industrial Growth 2.2-5 2.2.3 Evaluation of Potential Accidents 2.2-5 2.2.3.1 Determination of Design Basis Events 2.2-5 2.2.3.1.1 Explosions 2.2-5 2.2.3.1.2 Flammable Vapor Clouds (Delayed Ignition) 2.2-6 2.2.3.1.3 Toxic Chemicals 2.2-7 2.2.3.1.4 Fires 2.2-7 2.2.3.1.5 Collisions with Intake Structure 2.2-7 2.2.3.1.6 Liquid Spills 2.2-7 2.2.4 References 2.2-7 2.0-i REVISION 9 – DECEMBER 2002 BRAIDWOOD-UFSAR TABLE
    [Show full text]
  • IGS 2015B-Maquoketa Group
    ,QGLDQD*HRORJLFDO6XUYH\ $ERXW8V_,*66WDII_6LWH0DS_6LJQ,Q ,*6:HEVLWHIGS Website Search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
    [Show full text]
  • Technical Report : Illinois Natural Areas Inventory
    illliii'p ]i i iiiilffl,'isiPSi fJi J! ! tUl! on or '"'^" before ,he La.es. Da.e !;S;ed ^1" .H.'W I .') 2001 MAR JUL 14 ^4 I 3 2003 AUG 1 8 1994 JIOV J^;.; 'J 4 M J! J OCT 9 1996 14 m 1 3 Wr1337 2007 JUL 1 8 DEC 07 1997 »r! I 1997 APR 91998 MAR 1811393 LI6I—O-l09« ILLINOIS NATURAL AREAS INVENTORY TECHNICAL REPORT UNIVERSITY OF AT L . _ .-AIGN BOOKSIAQKa TECHNICAL REPORT ILLINOIS NATURAL AREAS INVENTORY performed under contract to the ILLINOIS DEPARTMENT OF CONSERVATION by the DEPARTMENT OF LANDSCAPE ARCHITECTURE UNIVERSITY OF ILLINOIS • URBANA-CHAMPAIGN and the NATURAL LAND INSTITUTE ROCKFORD, ILLINOIS This study was conducted for the State of Illinois pursuant to Contract #50-75-226 of the Illinois De- partment of Conservation. The study was financed in part through a planning grant from the Heritage Conservation and Recreation Service, U.S. Depart- ment of the Interior, under provisions of the Land and Water Conservation Fund Act of 1965 (PL 88-578). Illinois Department of Conservation personnel re- sponsible for preparing the Request for Proposals and coordinating the work included John Schweg- man, contract liaison officer, and Dr. Edward Hoff- man, Dr. Robert Lee, Marlin Bowles, and Robert Schanzle. Published November 1978 Illinois Natural Areas Inventory, Urbana For additional Information Natural Areas Section Illinois Department of Conservation 605 Stratton Building Springfield, Illinois 62706 Dv\ '^^ Thf Illinois Natural Areas hwfutory u'os a 3-year project to find and describe natural areas for the Illinois Department of Consen'ation.
    [Show full text]
  • Presented to the Uníversity of Manítoba Ín Partial Fulfillment of the Requírements for the Degree of Master of Science
    UPPERMOST ORDOVICIAN AND LOI^IERMOST SILURIAN STRATIGRAPHY AND SOLITARY RUGOSE CORALS OF THE EAST-CENTRAL UNITED STATES Robert J. McAuleY A thesis presented to the Uníversity of Manítoba ín Partial fulfillment of the requírements for the degree of Master of Science I^linnipeg, Manítoba 1985 UPPERMOST ORDOVICIAN AND LOWERMOST SILURIAN STRATIGRAPHY AND SOLITARY RUGOSE CORALS OF THE EAST-CENTRAL UNITED STATES BY ROBERT J. MCAULEY A tlresis st¡bmitted to the Faculty of Graduate Studies of the University of Ma¡litoba in partial fulfìll¡ne¡rt of the requiretttettts of the degree of MASTER OF SCIENCE o 1985 Permission has been grartted to the LIBRARY OF THE UNIVER- SITY OF MANITOBA to lend or sell copies of this thesis. to the NATIONAL LIBRARY OF CANADA to microfilnr this thesis and to lend or sell copies of the film, and UNIVERSITY MICROFILMS to publish an abstract of this thesis. The author reserves other publicatiolt rights, altd neitlter tlte thesis nor extensive ext¡acts from it may be printed or other- wise reproduced without the author's written perntissiott. l_ CONTENTS 1 Abs trac t Introduc tíon 4 Abbrevíations and RePositories 8 9 Acknowledgments Stratígraphic Sections and Collectíons 10 Eastern I.^Jísconsin 11 l1 Northeastern Illinoís . Eastern lowa 13 i3 Nor thr¿estern I11inoís T4 Northeastern Missourí . Southeastern Míssouri 15 16 Eastern Oklahoma I6 South-central Oklahoma StratígraPhY and SolitarY Rugose Corals 18 South-central Oklahoma 18 1B Lí thos tra tigraPhY Biota 23 24 Age of units Depositional envíronments 25 26 Northeastern Oklahoma LithostratígraPhY .. 26 26 Bio ta 26 Age of uníts 29 Depo sitional environments Southern Illínois and Southeastern 1l- Missouri 30 30 Lí thos tra tigraPhY 30 Bío ta Age of uníts 36 Depositíonal envíronments' 3l Northeastern Míssourí and 38 üles t-central Illinois 3B Li tho s tra tigraPhY Biota ..
    [Show full text]
  • Geology for Planning in St. Clair County, Illinois
    465 � JSGS-- -OIL & 6AS s SECJIGN--=fltES 14.GS: STATE OF ILLINOIS CIR465 c.4 DEPARTMENT OF REGISTRATION AND ED UCATION GEOLOGY FOR PLANNING IN ST. CLAIR COUNTY, ILLINOIS Alan M. Jacobs, compiler ILLINOIS ST ATE GEOLOGIC AL SURVEY John C. Frye, Chief Urbana, IL 61801 CIRCULAR 465 1971 GEOLOGY FOR PLANNING IN ST. CLAIR COUNTY, ILLINOIS Alan M. Jacobs, compiler ABSTRACT St. Clair County lies in southwestern Illinois across the Mississippi River from St. Louis, Missouri . One-fifth of the total land surface of 673 square miles is on flood­ plains of the Mississippi and Kaskaskia Rivers and Silver Creek. The floodplains are underlain by as much as 120 feet of gravel, sand, silt, and clay. The remaining fo ur­ fifths of the land surface is on uplands that contain flat or dissected plains, low ridges and mound-shaped hills, about 20 square miles of strip mines , and an area of karst topog­ raphy. The uplands are underlain by as much as 75 feet of till and sand and gravel, and generally 12 to 3 0 feet of loess and related silt; however, near the Mississippi River bluffs there are more than 100 feet of loes s and related silt. These deposits have been redistributed into spoil piles in the strip mines. Ben<ilath these deposits or cropping out in places are gently sloping beds of limestone, shale, sand­ stone, siltstone, clay stone, and coal. Thinly layered, frac­ tured limestone underlies the area of karst topography. Mineral and water resources are abundant in the county . Limestone of the St.
    [Show full text]
  • Upper Ordovician) at Wequiock Creek, Eastern Wisconsin
    ~rnooij~~~mij~rnoo~ ~oorn~rn~rn~~ rnoo~~rnrn~rn~~ Number 35 September, 1980 Stratigraphy and Paleontology of the Maquoketa Group (Upper Ordovician) at Wequiock Creek, Eastern Wisconsin Paul A. Sivon Department of Geology University of Illinois Urbana, Illinois REVIEW COMMITTEE FOR THIS CONTRIBUTION: T.N. Bayer, Winona State College University, Winona Minnesota M.E. Ostrom, Wisconsin Geological Survey, Madison, Wisconsin Peter Sheehan, Milwaukee Public Museum· ISBN :0-89326-016-4 Milwaukee Public Museum Press Published by the Order of the Board of Trustees Milwaukee Public Museum Accepted for publication July, 1980 Stratigraphy and Paleontology of the Maquoketa Group (Upper Ordovician) at Wequiock Creek, Eastern Wisconsin Paul A. Sivon Department of Geology University of Illinois Urbana, Illinois Abstract: The Maquoketa Group (Upper Ordovician) is poorly exposed in eastern Wisconsin. The most extensive exposure is found along Wequiock Creek, about 10 kilometers north of Green Bay. There the selection includes a small part of the upper Scales Shale and good exposures of the Fort Atkinson Limestone and Brainard Shale. The exposed Scales Shale is 2.4 m of clay, uniform in appearance and containing no apparent fossils. Limestone and dolomite dominate the 3.9 m thick Fort Atkinson Limestone. The carbonate beds alternate with layers of dolomitic shale that contain little to no fauna. The shales represent times of peak terrigenous clastic deposition in a quiet water environment. The car- bonates are predominantly biogenic dolomite and biomicrite. Biotic succession within single carbonate beds includes replacement of a strophomenid-Lepidocyclus dominated bottom community by a trep- ostome bryozoan-Plaesiomys-Lepidocyclus dominated community. Transported echinoderm and cryptostome bryozoan biocalcarenites are common.
    [Show full text]
  • Dolomite Resources of Boone and De Kalb Counties
    View metadata, citation and similar papersbrought at core.ac.uk to you by CORE nUNOfS SSOLOCrCAL provided by Illinois Digital... SURVEY tlBRARY STATE OF ILLINOIS DEPARTMENT OF REGISTRATION AND EDUCATION DOLOMITE RESOURCES OF BOONE AND DE KALB COUNTIES James C. Bradbur/ ILLINOIS STATE GEOLOGICAL SURVEY John C. Frye, Chief URBANA CIRCULAR 379 1965 Digitized by the Internet Archive in 2012 with funding from University of Illinois Urbana-Champaign http://archive.org/details/dolomiteresource379brad DOLOMITE RESOURCES OF BOONE AND DE KALB COUNTIES James C. Bradbury ABSTRACT The dolomite resources of Boone and DeKalb Counties are of interest because of their location near the greater Chicago area. As natural exposures are rare and quarries are limited chiefly to one area within the two counties, much of the information on the distribution and character of the dolomite formations must come from drill records. Maps in this report show distribution of bedrock formations, depth to bedrock, and depth to and thickness of dolomites. Chemical analyses of samples from active and abandoned quarries are presented. Three or more dolomite rock units up to 300 or more feet in thickness are present in the area. Places where each of the carbonate units may be found with relatively thin overburden are suggested. INTRODUCTION The limestone resources of Boone and DeKalb Counties in north-central Illinois are of interest because of their location near the western margin of the Chicago metropolitan area (fig. 1). Widespread deposits of glacial drift and a lack of pronounced topographic relief generally result in a scarcity of outcrops. Thus, although there are several quarries, both active and abandoned, they are mostly limited to a narrow belt in western Boone County.
    [Show full text]
  • Paleozoic Lithostratigraphic Nomenclature for Minnesota
    MINNESOTA GEOLOGICAL SURVEY PRISCILLA C. GREW, Director PALEOZOIC LITHOSTRATIGRAPHIC NOMENCLATURE FOR MINNESOTA John H. Mossier Report of Investigations 36 ISSN 0076-9177 UNIVERSITY OF MINNESOTA Saint Paul - 1987 PALEOZOIC LITHOSTRATIGRAPHIC NOMENCLATURE FOR MINNESOTA CONTENTS Abstract. Structural and sedimentological framework • Cambrian System • 2 Mt. Simon Sandstone. 2 Eau Claire Formation • 6 Galesville Sandstone • 8 Ironton Sandstone. 9 Franconia Formation. 9 St. Lawrence Formation. 11 Jordan Standstone. 12 Ordovician System. 13 Prairie du Chien Group. 14 Oneota Dolomite. 14 Shakopee Formation. 15 St. Peter Sandstone. 17 Glenwood Formation. 17 Platteville Formation. 18 Decorah Shale. 19 Galena Group • 22 Cummings ville Formation. 22 Prosser Limestone. 23 Stewartville Formation • 24 Dubuque Formation. 24 Maquoketa Formation. 25 Devonian System • 25 Spillville Formation • 26 Wapsipinicon Formation 26 Cedar Valley Formation • 26 Northwestern Minnesota. 28 Winnipeg Formation • 28 Red River Formation. 29 Acknowledgments • 30 References cited. 30 Appendix--Principal gamma logs used to construct the composite gamma log illustrated on Plate 1. 36 ILLUSTRATIONS Plate 1 • Paleozoic lithostratigraphic nomenclature for Minnesota • .in pocket Figure 1. Paleogeographic maps of southeastern Minnesota • 3 2. Map showing locations of outcrops, type sections, and cores, southeastern t1innesota • 4 3. Upper Cambrian stratigraphic nomenclature 7 iii Figure 4. Lower Ordovician stratigraphic nomenclature • • • • 14 5. Upper Ordovician stratigraphic nomenclature 20 6. Middle Devonian stratigraphic nomenclature. • • . • • 27 7. Map showing locations of cores and cuttings in northwestern Minnesota • • • • • • • • • • • • • • • • • • 29 TABLE Table 1. Representative cores in Upper Cambrian formations •••••• 5 The University of Minnesota is committed to the policy that all persons shall have equal access to its programs, facilities, and employment without regard to race, religion, color, sex, national orgin, handicap, age, veteran status, or sexual orientation.
    [Show full text]