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Environmental Labs of Milpitas, California. Those soil filled liners were sealed with Teflon <br /> paper and plastic endcaps, labeled and logged onto a chain-of-custody form. The samples <br /> were placed on ice in a chilled ice chest and the "third party" left the site to take the samples <br /> directly to Priority Labs. Copies of the analytical data and chain-of-custody documentation <br /> are presented in Appendix A. <br /> SAMPLING - GROUNDWATER FIELD METHODS <br /> One groundwater sample was collected from the groundwater which had flooded the excavation. <br /> This sample was collected in a new one-liter bottle attached to the end of an aluminum pole <br /> with a stainless steel hose clamp, displacing the surface sediment, then lowering the bottle <br /> into the water, carefully bailing a sample to the edge of the open pit. The water sample was <br /> then carefully poured into the appropriate laboratory prepared container with minimum <br /> cavitation and headspace. The container was sealed, labeled and logged onto a chain-of- <br /> custody form. The samples were taken by the "third party" to Priority Environmental Labs, <br /> Inc. for analysis. Copies of the analytical data and chain-of-custody documentation are <br /> presented in Appendix A. <br /> SUBSURFACE CONDITIONS <br /> The site is either a natural land formation in the Old River or reclaimed land from the <br /> Sacramento-San Joaquin Delta. The island area in the delta is typically composed of alluvial <br /> river sediment of sand, clay and organic soils (peat) and organic muds. At the time the <br /> Wright representative observed the empty 3 to 4 foot deep excavation on November 11, 1995, <br /> it was dry. Later, on March 29, 1996, the pit had filled with about 18-24 inches of water. <br /> Depth to groundwater is assumed to occur at about 3 feet below grade in undisturbed <br /> sediments. The excavation was about 6.5 feet deep into the soil, which appeared to contain <br /> organic sediment with thin interbeds of sand. The sediment and soil are highly organic, and <br /> may approach 100%reduced organic matter in various stages of compaction, and may exhaust <br /> methane and other decomposition gases upon exposure to air. <br /> CHEMICAL ANALYTICAL METHODS AND RESULTS <br /> One water sample and ten soil samples were sent to Priority Environmental labs for chemical <br /> analysis. The samples were analyzed for Total Petroleum Hydrocarbons as Gasoline and as <br /> Diesel (TPHG, TPHD), Benzene, Toluene, Ethylbenzene and Xylene (BTEX), Methyl-Tertiary- <br /> Butyl-Ether (MTBE) and Lead using EPA Methods 5030/8015, 8020 and 7420. The results are <br /> presented in Tables 1 and 2 below. <br /> SOIL DISPOSAL SITE RESTORATION <br /> Soil from the tank excavation was stockpiled on and covered with plastic at the site by both <br /> representatives of the Estate and Wright personnel. On April 22, 1996 a Generator's Waste <br /> Profile Sheet was forwarded along with the analytical data to Altamont Landfill and Resource <br /> Recovery Facility in Livermore, CA (Altamont). On April 23, 1996 Altamont notified Wright <br /> that it would accept the soil for disposal as Class II cover. The soil was disposed of at <br /> Altamont on June 12, 1996. A copy of the soil profile acceptance letter and weight tickets <br /> from Altamont are provided in Appendix D. <br />