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Of the Elk River M\ *° Ll | Minnesota M I Nuclear-Reactor Site

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Of the Elk River M\ *° Ll | Minnesota M I Nuclear-Reactor Site I Geology and Hydrology iH | of the Elk River m\ *° ll | Minnesota m I Nuclear-Reactor Site GEOLOGICAL SURVEY BULLETIN 1133-C Prepared in cooperation with the U.S. Atomic Energy Commission iid a W Geology and Hydrology of the Elk River Minnesota Nuclear-Reactor Site By R. F. NORVITCH, ROBERT SCHNEIDER, and R. G. GODFREY STUDIES OF SITES FOR NUCLEAR-ENERGY FACILITIES GEOLOGICAL SURVEY BULLETIN 1133-C Prepared in cooperation with the U.S. Atomic Energy Commission UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON = 1963 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington 25, D.G. CONTENTS Page Abstract_______._________.________...______... Cl Introduction.. ________________________________________________ 1 Acknowledgments. ___-_____-___________-__-__________--_--_-_----. 2 Location.________________________________________________________ 2 Geology__________________________________________-_--__-_ 2 Bedrock formations.__________-________.__-________-_--__-_- 2 Glacial deposits and alluvium___________________________________ 3 Topography. ___________________________ _ 4 Hydrology _____________________ _ _ 4 Surface water______.___._________________-_______.________ 4 Ground water____-_-_______-_______-_-_-__--________-_-------- 6 Aquifers________________ __________________ 6 Natural recharge, discharge, and movement_________________ 7 Artificial discharge_______________________________________ 8 Quality of water_____________________________________ 9 Course of accidentally spilled wastes____------------_----_-__-___-__- 9 Surface____________________________________________________ 9 Subsurface__________________________________________________ 16 Conclusions____________________________________________ 17 Well logs and soil borings_______________________________________ 18 References cited____________________________________________ _ 25 ILLUSTRATIONS [Plates land 2 In pocket] PLATE 1. Map of Elk River area, Minnesota, showing generalized distribution of surficial deposits, location of wells, and altitude of the water table. 2. Map of Rural Cooperative Power Association plant area, Elk River, Minn., showing approximate location of drain­ age lines, location of test borings, and geologic section A-A'. Page FIGURE 1. Map of Mississippi River and tributaries_ _.,__._.. C8 2, 3. Average velocity-discharge relation graphs of Mississippi River at Elk River and near Anoka_____._____ 12-13 4. Distribution of concentration of a contaminant at Fridley, Minn. ________________________________. 15 IV CONTENTS TABLES Page TABLE 1. Principal formations penetrated by wells in the vicinity of Elk River, Minn__________________________ C3 2. Chemical analyses of ground water at Elk River and Coon Rapids, Minn., and of Mississippi River water at Fridley, Minn.______________________________ 10 3. Well logs._______._________________.____ 18 4. Logs of soil borings________-_________-_-____________ 22 STUDIES OF SITES FOR NUCLEAR-ENERGY FACILITIES GEOLOGY AND HYDROLOGY OF THE ELK RIVER, MINNESOTA, NUCLEAR-REACTOR SITE By E. F. NORVITCH, EGBERT SCHNEIDER, and E. G. GODFREY ABSTRACT The Elk River, Minn., nuclear-reactor site is on the east bluff of the Mississippi River about 35 miles northwest of Minneapolis and St. Paul. The area is underlain by about 70 to 180 feet of glacial drift, including at the top as much as 120 feet of outwash deposits (valley train) of the glacial Mississippi River. The underlying Cambrian bedrock consists of marine sedimentary forma­ tions including artesian sandstone aquifers. A hypothetically spilled liquid at the reactor site could follow one or both of two courses, thus: (1) It could flow over the land surface and through an arti­ ficial drainage system to the river in a matter of minutes; (2) part or nearly all of it could seep downward to the water table and then move laterally to the river. The time required might range from a few weeks to a year, or perhaps more. The St. Paul and Minneapolis water-supply intakes, 21 and 25 miles down­ stream, respectively, are the most critical points to be considered in the event of an accidental spill. Based on streamflow and velocity data for the Mississippi River near Anoka, the time required for the maximum concentration of a con­ taminant to travel from the reactor site to the St. Paul intake was computed to be about 8 hours, at the median annual maximum daily discharge. For this dis­ charge, the maximum concentration at the intake would be about 0.0026 micro- curie per cubic foot for the release of 1 curie of activity into the river near the reactor site. INTRODUCTION The objective of this report is to determine the geologic and hydro- logic conditions that would affect the movement of a hypothetically spilled liquid at the Elk Eiver, Minn., nuclear-reactor site and to evaluate the possibility of such a spill reaching a major water facility downstream along the Mississippi Eiver. The report was prepared by the U.S. Geological Survey for the Atomic Energy Commission. The study was under the direct super­ vision of Eobert Schneider, district geologist, Ground Water Branch, St. Paul, Minn. Leon E. Sawyer, district engineer, Surface Water Branch, compiled most of the streamflow data for the Mississippi Eiver. Cl C2 STUDIES OF SITES FOB NUCLEAR-ENERGY FACILITIES The study involved collection of well data and a reconnaissance of the geology. Water-level altitudes were determined with an aneroid barometer, and most of the surficial geology was mapped directly from aerial photographs. No topographic quadrangle map of the area is available. Eegional ground-water conditions of the Elk River area have been described by Thiel (1947), and the surficial glacial history was studied by Cooper (1935). ACKNOWLEDGMENTS The following well drillers furnished well logs and gave oral informa­ tion on ground-water conditions in the area: McAlpine Bros., Dayton, Minn.; McAlpine Bros., Eogers, Minn.; and Kate Thomas, Elk River, Minn. Special thanks are due E. J. Nelson, Rural Cooperative Power Association plant superintendent; R. W. Anderson, Platting Engineer of Anoka County; and Richard Halter, Superintendent of Utilities, village of Elk River, for their cooperation. LOCATION The area under investigation may be approximately encompassed by a circle of 2-mile radius centering at the Rural Cooperative Power Association steampower plant at Elk River, Minn. (pi. 1), where the nuclear reactor is located. The plant is on the east bluff of the Mis­ sissippi River about one-quarter mile southeast of the village of Elk River. The village is about 35 miles northwest of Minneapolis and St. Paul at the confluence of the Elk and Mississippi Rivers in south­ eastern Sherburne County. The area is traversed by State Highways 101 and 218 and U.S. Highways 169, 52, and 10. The Great Northern and Northern Pacific Railways serve the area and their main tracks are directly east of the plant site. Additional information was compiled on major water facilities located downstream along the Mississippi River as far south as the Minneapolis municipal water-supply intake at Fridley, Minn. (fig. 1). GEOLOGY BEDROCK FORMATIONS The deepest wells in the Elk River area penetrate sandstone, shale, siltstone, and dolomite of the St. Croixan series. (See table 1.) The formations below the St. Croixan rocks are unknown; but to the south, in the Minneapolis-St. Paul area, the St. Croixan series is underlain by about 1,000 to 2,500 feet of Preeambrian sandstone and shale, the sediments for which may have been derived from eroded Preeambrian lava flows (Schwartz, 1936, p. 24, 81). The flows are not present at NUCLEAR-REACTOR SITE, ELK RIVER, MINN. C3 TABLE 1. Principal formations penetrated by wells in the vicinity of Elk River, Minn. Approxi­ System Series Formation mate Physical Water-bearing thickness characteristics properties (feet) Recent Alluvium and lake (?) Clay, silt, sand, Undetermined. deposits gravel, and marl. Heterogeneous, un- Yields small sup­ sorted deposits con­ plies to a few taining sand and domestic wells. Till gravel in lenses and irregularly shaped Quaternary bodies; material ranges in size from Pleistocene Glacial 70-180 clay to boulders. drift Poorly to well May yield small stratified and to large supplies. Out wash sorted deposits ranging in size from clay to gravel. Friable sandstone Sandstone beds predominates; yield large sup­ some dolomite, plies under high Cambrian St. Croixan Undifierentiated 500± shale, and silt- heads. A large stone. number of flow­ ing wells are completed in the sandstones. the Twin Cities but are exposed in the gorge of the St. Croix River at Taylors Falls, Minn., about 35 miles to the northeast. The oldest rock in the Minneapolis-St. Paul area is Precambrian granite whose upper surface is about 1,350 feet below sea level. Regionally the bedrock strata are on the northwest run of a shallow structural basin whose center is near the Mississippi River in Min­ neapolis (Schwartz, 1936, p. 88). The basin is slightly elongated northeast-southwest and is formed by rocks of Cambrian and Ordo- vician age, including several important artesian aquifers. Faults have been mapped at Hastings, Minn., about 45 miles southeast of Elk River, and in the St. Croix River valley about 40 miles east of Elk River; the possibility of subsequent earth movements of any great magnitude in this region probably is very remote. [GLACIAL DEPOSITS AND ALLUVIUM During
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