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WASTE DISCHARGE REQUIREMENTS -6- <br />FORWARD INCORPORATED <br />WASTE MANAGEMENT FACILITY <br />CLASS II LANDFILLS CLASS III LANDFILLS <br />CLASS II SURFACE IMPOUNDMENT <br />CLASS II LAND TREATMENT UNIT <br />CLOSURE OF CLASS I LANDFILL <br />SAN JOAQUIN COUNTY <br />penetration into the clay layer. The culvert drainage system is designed <br />to gather runoff from the vegetative layer and route the water into a <br />holding pond. <br />25. Findings 15 through 24 indicate the water quality will be adequately <br />protected during the closure and post -closure maintenance period. <br />Therefore, the Board finds that the Discharger has satisfied the <br />requirements of Section 2510(b) and approves the proposed engineered <br />alternative to Section 2531(b)(1) for the in-place closure of WMU A. <br />TOW"Tt'20111FITAff <br />26. Land within 1,000 feet of the site is used for agriculture. <br />27. The Forward Landfill is underlain by the Victor Formation. This is a <br />heterogeneous formation composed of fan and flood plain deposits derived <br />from Sierra granitics, metamorphics, and volcanics. Geologic materials <br />immediately under the WMUs are lenticular clay, silt, sand, and minor <br />amounts of gravel. Some of the lenses of clay, silt, and sand appear to <br />be laterally continuous between monitoring wells over a distance of up to <br />1,800 feet. Others are discontinuous across the site. The lenses range <br />from a few inches to approximately 20 feet in thickness. Based on <br />geological cross-sections submitted with the Report of Waste Discharge, <br />over 50 percent of the material within 60 Feet of the ground surface is <br />coarse grained soil (Bureau of Reclamation, Unified Soil Classification). <br />28. The shallow ground water beneath the site is contained in the Victor <br />Formation and recent alluvium. Generally, these sediments have moderate <br />permeabilities with locally high permeabilities in the sandy and gravelly <br />lenses. Ground water in the Victor Formation is unconfined and flows in <br />a north -northeasterly direction beneath the site. The ground water table <br />is 30-40 Feet below the bottom of the WMUs. The quality of this water is <br />suitable for domestic or agricultural use. <br />29. Low levels (0.2 to 3.0 Ng/1) of volatile organic compounds (VOCs) have been <br />found in several monitoring wells (MWs) at the facility between June 1988 <br />and February 1989. MW -5 was sampled once before it went dry in June 1988 <br />and it contained chloroethane, 1,1-dichloroethane, 1,1-dichloroethene, <br />1,1,1 -trichloroethane, trichloroethene, d i bromoch I oromethane, and benzene. <br />Samples from MW -5A, the replacement well for MW -5, contained 1,1- <br />dichloroethane, 1,1,1 -trichloroethane and trichloroethene. Other wells <br />