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WASTEWATER RECLAMATION REQUIREMENTS 2 <br /> MUSCO OLIVE PRODUCTS, INC. AND <br /> THE STUDLEY COMPANY <br /> WASTEWATER DISCHARGE TO LAND <br /> SAN JOAQUIN COUNTY <br /> 8. Soils at the facility are predominately clay,clayey silt, and silty clay. Two thirds of the <br /> western portion of the facility is located on materials from the Pliocene period which <br /> consist of sedimentary deposits of the Tulare and Laguna formations. The other one third <br /> (eastern) is situated on Pleistocene nonmarine sediments. Surface soils are of the <br /> Ambrose Clay Formation (Calla-Carbona Complex, Carbona Clay Loam)consisting of <br /> dark brown or dark grayish-brown strongly developed secondary material from <br /> sandstones, shales, and other sedimentary rocks and tend to have low permeability rates. <br /> The nearest active Holocene fault is the Greenville Fault, which is 4.5 miles away. <br /> 9. Evaporation at the site is greater than 100 inches per year, while rainfall is less than 15 <br /> inches per year. <br /> 10. Ground water monitoring well W2 was constructed to monitor perched ground water <br /> downgradient of the facility's surface impoundments. Perched ground water is <br /> encountered at 29 feet below ground surface(bgs). Additional monitoring wells, <br /> constructed adjacent to the surface impoundment, were constructed to 90 feet bgs and did <br /> not encounter ground water. The Discharger has indicated that the perched ground water <br /> zone does not extend beneath the entire site as verified by surface and subsurface soil <br /> conditions explored by boring and backhoe test pits as described in RWQCB Water <br /> Quality Monitoring Program report,dated 21 December 1992. <br /> 11. Ground water samples collected in 1985 from W2 contained 920 mg/L TDS, 32 mg/L <br /> chloride, and 264 mg/L sodium. The monitoring well went dry in January 1987 shortly <br /> after operations began, but is still examined for a return of the aquifer. <br /> 12. The Musco Olive#1 production well encountered artesian water at 250 feet bgs with a <br /> static head at 50 feet bgs. Based on a single sampling event in February 1996, water <br /> quality for this well showed chloride(514 mg/L), sulfate (400 mg/L), sodium (477 mg/L), <br /> total dissolved solids (1,434 mg/L), electrical conductivity (2240µmhos/cm), and a pH of <br /> 7.8. This well will be monitored for background water quality. <br /> 13. Five existing production water wells downgradient of the site were sampled on <br /> 22 November 1985. The wells are dispersed approximately 3000-5000 feet from the <br /> facility and were drilled to depths ranging from 193 to 607 feet. The Musco Olive#1 and <br /> W2(on-site shallow well) were also sampled for background water quality. Accumulative <br /> results of sampling showed a mean and standard deviation for TDS of 1219 mg/L and <br /> 363 mg/L, respectively. Chloride results showed the mean at 211 mg/L and standard <br /> deviation of 130 mg/L. Other parameters/constituents of concern include sulfate, nitrate, <br /> iron, manganese, and electrical conductivity. <br /> 14. The beneficial uses of ground water beneath the facility are municipal and domestic <br /> supply, agricultural irrigation, stock watering, industrial process supply, and industrial <br /> service supply. <br /> 15. Surface water runoff from the upper parcel goes under culverts in the railroad <br /> embankments. It then commingles with the surface water runoff on the lower parcel. <br /> This water combines into one stream channel which passes diagonally through the lower <br /> site and exits the facility and flows under Highway 580 near the lined ponds into an <br /> unnamed, dry creek bed. <br />