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results of the U S Department of Agriculture investigation are presented as Figure 9 <br /> The 521 North Cherokee Lane site is underlain by the Kingdon fine sandy loam and the Tokay fine sandy <br /> loam(USDA, 1992) The Kingdon fine sandy loam is a very deep,moderately well drained,nearly level soil <br /> on low fan terraces of the Mokelumne River Permeability is moderate in the Kingdon fine sandy loam and <br /> most of the areas where the soil is present are used for irrigated crops,orchards,or vineyards The Tokay fine <br /> sandy loam is a very deep, well drained, nearly level soil on low fan terraces of the Mokelumne River <br /> Permeability is moderately rapid in the Tokay soil Most areas are used for irrigated crops, orchards, or <br /> vineyards <br /> 4 1 3 Regional Hydrology <br /> Past Investigations Past hydgeologic investigations conducted in this area have included Piper and others, <br /> 1939,Thomasson and others, 1960, Olmstead and Davis, 1961, Brice, 1977,and Page, 1986 Alt available <br /> geologic and hydrogeologic data available from other hydrogeological investigations at soil and groundwater <br /> contamination investigation sites in the Lodi area were reviewed <br />• Surface Waters The principal surface water body located near the site vicinity is the Mokelumne River which <br /> is part of the contributing drainage system of the San Joaquin-Sacramento Delta area Beneficial uses of <br /> tributary rivers of the Delta include agricultural water supply, domestic water supply, aquatic habitat, and <br /> recreation Water quality in the Delta and its mayor tributaries has been studied for many years Primary <br /> regulatory agency concerns are impacts from nutrients and pesticides in agricultural drainage and their effects <br /> on aquatic species (U S Geological Survey, 1996, 1998) Metals such as selenium are also a concern In <br /> general, water quality in the minor sloughs and irrigation ditches is poorer because of the concentration of <br /> constituents from agricultural runoff and the lack of flushing or mixing with water from higher quality <br /> sources Water within the smaller Delta tributaries, such as the Mokelurnne River, tends to be of higher <br /> quality because agricultural runoff is a smaller proportion of the total flow(U S Geological Survey, 1998) <br /> Mokelumne River The Mokelumne River originates in the Central Sierra Nevada in Alpine County, <br /> approximately 130 miles east-northeast of Lodi The river is fed by numerous tributary streams and receives <br /> runoff from a 627-square-mile watershed area upstream of Comanche and Pardee Reservoirs(U S Geological <br /> Survey, 1995) These two reservoirs,approximately 15 and 35 miles east of Lodi,respectively,are used for <br /> flood control,storage,and recreation Downstream of Comanche Reservoir, the Mokelumne River meanders <br /> Ma,nSD 1Enwronmen1a11PanoarTexacolReportslSAR1203 wpd Page 19 <br />