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Adak <br /> ' k' ■ KL EI N F E L D E R <br /> ' 5.3. TASK2-DRILLING OF SOIL BORINGS AND MONITORING WELL INSTALLATION <br /> Four (4) soil borings will be advanced to depths of approximately 30 feet bgs. During the <br /> advancement of the borings, soil samples will be collected at five foot intervals for lithologic <br /> classification. Lithologic classification will be based on the Unified Soil Classification System <br /> (USCS). <br /> After collection, the soil samples will be labeled, logged on a chain-of-custody, and immediately <br /> ' stored in an iced cooler. In an attempt to establish a baseline level for certain analytes in soil, the <br /> soil sample obtained from a depth of 5 feet bgs in each monitoring well boring would be analyzed <br /> for the following: <br /> ' Nitrate (as N) by EPA Method 300.0 <br /> Ammonia(as N) by EPA Method 350.3 <br /> Total Kjeldahl Nitrogen (TKN) by EPA Method 351.2 <br /> ' The samples will be analyzed on a normal laboratory schedule requiring approximately two weeks <br /> (ten working days) for completion unless the optional rush analytical turnaround is requested by the <br /> client at an additional charge. <br /> ' Following completion of the drilling, a 2-inch diameter PVC well will be installed in each of the <br /> borings. The well will be constructed as described in Appendix A. The wells will be surveyed for <br /> well location and elevation above mean sea level(msl) so that subsequent water level sounding data <br /> can be utilized in determining groundwater flow directions and gradient as described in Appendix <br /> A. <br /> ' 5.4. TASK 3 - MONITORING WELL DEVELOPMENT AND SAMPLING <br /> Forty-eight hours after installation, the new wells will be developed to remove sediment-laden <br /> water and to increase the hydraulic radius of each well. Development will be performed as <br /> described in Appendix A. <br /> Water level measurements will be made in the wells prior to development, and at the beginning of <br /> the sampling round prior to purging and sampling the wells. The depth to groundwater will then be <br /> measured in each well according to the protocol described in Appendix A. The depth to <br /> groundwater measurements will then be converted to relative groundwater elevations with respect <br /> to mean sea level or a local benchmark by subtracting them from the surveyed casing elevations. <br /> The resulting groundwater elevations will be used to assess the direction of the groundwater <br /> ' gradient at the time of sampling. This information can then be used to assess which wells represent <br /> upgradient and which wells represent downgradient groundwater conditions. <br /> 20-4587-OI.WPI/201 IP128 Page 7 of 12 <br /> Copyright 2001,Kleinfelder,Inc. May 8,2001 <br />