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David Wang, P.E. , Chief <br /> Page 2 <br /> March 6, 1991 <br /> Evaluation of environmental conditions at DDRW Sharpe began with <br /> the 1980 USATHAMA installation assessment. Since that time <br /> Battele Laboratories (1983) and ESE (through the present) have been <br /> contracted to determine the types and extent of contamination <br /> resulting from past activities. Early studies focused on ground <br /> water contamination consisting primarily of volatile organic <br /> compounds (VOC) . <br /> Agencies regulating the remedial activities at DDRW Sharpe (the <br /> Department, the U.S. Environmental Protection Agency, and the <br /> California Regional Water Quality Control Board) entered into a <br /> Federal Facilities Agreement (FFA) with the Army. The purpose of <br /> the FFA is to establish a framework for DDRW Sharpe ' s installation <br /> restoration program. A fundamental ingredient of the FFA is the <br /> schedule of deliverable documents which it serves to channel work <br /> efforts towards a successful conclusion for the installation <br /> restoration program. <br /> An important schedule component is the RI Report that is the <br /> subject of this memorandum. The RI Report compiles the scientific <br /> data that will be the foundation for more interpretive documents <br /> that will follow, primarily the Risk Assessment and FS . <br /> RI REPORT CONTENTS <br /> The RI Report summarizes all data gathered from 1980 to the <br /> present. The data gathered in support of this Report consists of: <br /> o more than 3 , 500 ground water samples, many analyzed for more <br /> than 30 different constituents. ; <br /> o approximately 1, 800 soil gas samples; <br /> 0 over 500 soil samples; and <br /> 0 200 air samples <br /> REPORTED RI FINDINGS <br /> ESE' s findings are summarized in the following section of the <br /> memorandum. They are presented here without interpretation by the <br /> Department. <br /> GROUND WATER CONCLUSIONS: <br /> o The geology beneath DDRW Sharpe is a complex of interbeded <br /> sand, silt, and clays. Individual lithologic units tend to be <br /> discontinuous over distance. <br />