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MAR. -30' 95 (THU) 16: 16 NOLTE & ASSOC, SACTO TEL:916 641 9222 P 005 <br /> i Mr. Jim Hamrick <br /> July 14, 1994 <br /> Page 3 <br /> as it collects on the surface. The oil is removed and disposed of by an oil recycling firm_ <br /> The process water is reused and consumed within the facility while the excess process water <br /> flows by gravity to the wastewater evaporation ponds_ The process water is used to cool the <br /> cutting blades that shear the molten glass into globules used to mold the glass bottles. The <br /> process water is a mixture of the plant water supply and a product named Biosol Blue. The <br /> Biosol Blue is considered to be in the triglycerides chemical family and is mixed to 1 to 600 <br /> dilution ratio with the plant water supply . A Material Safety Data Sheet (MSDS) ror Biosol <br /> Blue is presented in Appendix B, The product water from the reverse osmosis system is used <br /> and consumed within the facility. <br /> E10STING CONDITIONS <br /> A review of the U.S. Depa,rtmerit of Agriculture Soil Conservation Service (SCS) soil survey <br /> for San Joaquin County indicates that the soil at the Owens-Brockway Glass Containers <br /> facility consists of either a Capay clay Or a Stomar clay loam. The clean water soil <br /> permeability at a depth of 92 inches for the Capay clay is 0.06 to 0.2 inch/hour, while the <br /> Stomar clay loam is 0.2 to 0.6 inch/hour. The Capay soil is suited to irrigated crops such as <br /> alfalfa, pasture crops, sugar beets and tomatoes, and the Stomar soil is suited for irrigated <br /> crops or orchards. <br /> Ground water <br /> A review was performed of the UNITED S'TA'PES DEPARTMENT Of THE INTERIOR <br /> GEOLOGICAL SURVEY Water Resources Division, Geology.-Hydrology and Water <br /> _Quality of the Tracy-Dos Palos Area San Joaquin Valley, California, August 1971 by <br /> William R. Hotchkiss and Gary O_ Balding. This report states that the ground water <br /> reservoirs for the Tracy-Dos Palos area is divided into three water-bearing zones, the lower <br /> section, the upper section and a shallow water zone. The lower section, the deepest water <br /> bearing zone, is bounded by consolidated deposits at the bottom of the section and an <br /> impermeable confining strata called Corocoran Clay Member at the top of the section. The <br /> upper section, ranges from a depth of 25 ft to the Corocoran Clay Member, The shallow <br /> water zone is generally within 25 ft of the land surface. Contour maps from the report, of <br /> the area around the Owens-Brockway Glass Containers facility, show the shallow water zone <br /> is approximately 10 ft from the land surface, The Corocoran Clay Member, an impermeable <br /> confining strata, is approximately 50 ft below the land surface. <br /> poen.d+ssr.cures ice_ <br />