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Hydrology of buried crystalline rock at Savannah River Plant near Aiken, South Carolina

Technical Report ·
DOI:https://doi.org/10.2172/5251507· OSTI ID:5251507
The purpose of this report is to present the results of hydrologic investigations that were made on buried crystalline rock at the Savannah River Plant in connection with an investigation of the feasibility of storing high-level radioactive waste in artificially excavated chambers in the rock. The methods pursued in this investigation may be applicable to other investigations of low permeability metamorphic and igneous rocks. Fractures occurring in single boreholes were investigated by core inspection, geophysical logs, packer tests, and in-hole tracer tests. The correlation of fractures between holes was based on the rapidity of water level response to hydraulic activities in nearby wells and on an in-hole tracer test conducted in one boring while a nearby boring was being pumped. Values for hydraulic conductivity and other hydraulic parameters were determined from laboratory tests, packer tests, pumping tests, a two-well tracer test, and a numerical model that duplicated the results of a year-long pumping test. Dispersivity of the fractured crystalline rock was determined using a two-well tracer test. Water geochemistry and isotropic composition were evaluated. The age of the water was determined to be about 840,000 years. The average velocity of regional flow in crystalline rock is about 0.2 ft/y.
Research Organization:
Department of Energy, Aiken, SC (USA). Savannah River Operations Office
DOE Contract Number:
AC09-76SR00001
OSTI ID:
5251507
Report Number(s):
DOE/SR-WM-79-2
Country of Publication:
United States
Language:
English