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T <br /> Undisturbed soil samples were collected at least every 5-feet as drilling <br /> progressed for lithologic and hydrogeologic description and for possible <br /> chemical analysis. Soil samples were collected continuously below 30-feet <br /> bgs. The samples were collected by driving a split-barrel sampler lined <br /> with 6-inch diameter brass tubes using repeated blows from a 140-1b <br /> hammer dropped 30-inches. Selective soil samples were immediately <br /> trimmed, sealed with Teflon tape and plastic end caps, labeled, and stored <br /> on ice for transport to Kiff Analytical, LLC of Davis, California under chain <br /> of custody. Soil from the remaining tubes was described by the site <br /> geologist using the Unified Soil Classification System (USCS) and was <br /> screened for volatile compounds using an organic vapor meter (OVM). <br /> The soil was screened by emptying soil from one of the sample tubes into <br /> a plastic bag. The bag was then sealed and placed in the sun f o r <br /> approximately 10 minutes. After the volatile compounds were allowed to <br /> volatilize, the OVM measured the vapor in the bag through a small hole <br /> punched in the bag. OVM readings are used as a screening tool only, <br /> since the procedures are not as rigorous as those used in the laboratory. <br /> The OVM readings are listed on the boring logs presented in Appendix D. <br /> Drilling equipment was cleaned with a TSP solution between sampling <br /> intervals to prevent potential cross-contamination. <br /> 5 .3 Monitoring Well Construction <br /> Monitoring well MW-6 as constructed in the boring with 2-inch <br /> diameter, 0.0 ch slott flush-threaded, Schedule 40 PVC well screen <br /> and blank casing. The well is screened between 39-feet bgs and 44-feet <br /> bgs to monitor the targeted water-bearing zone. The well casing was <br /> lowered through the augers and #2112 filter pack sand was placed in t h e <br /> annular space between the well casing and the borehole from the b o t t o m <br /> of the boring to 2-feet above the well screen. A 3-foot thick hydrated <br /> bentonite layer separates the sand from the ovcrl}irtg ccillent surface seal. <br /> The wellhead is secured with a locking wellplug beneath an at-rade <br /> traffic-rated well box. Well construction details are shown on the boring <br /> log in Appendix D. <br /> 5 .4 Monitoring Well D-Lyelopmen <br /> On August 20, 2001, ASE associate geologist Erik Paddleford developed <br /> monitoring well MW-6 using two episodes of surge-block agitation a n d <br /> submersible pump evacuation. Over ten well casing volumes of water <br /> were removed from the well during development, and evacuation <br /> 574 West Grant Line Road CAP — January 2002 <br /> -6- <br />