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March 13,2000 <br /> Job Number: LG00-067 <br /> Page 5 <br /> Based on the work by Bryan it is estimated that under"natural"conditions, ground water <br /> concentration of nitrate is no more then about 3 mg/1-N. Areas having 5.5 mg/1-N or more are <br /> �. those in which nitrate concentrations may be increasing. 3 <br /> DBCP is a nematocide and soil fumigant for vegetables, and grapes. It is thought to cause <br /> health problems consisting of kidney damage,liver damage, and cancer. The use of DBCP was <br /> discontinued in 1979. <br /> VL GEOLOGY, SOILS,AND PERCOLATION TEST <br /> The surficial sediment of the site and surrounding area is reported to be the lower member <br /> of the Pleistocene age (about 11,000 to 2 million years ago) Modesto Formation that consists of <br /> tan and light gray gravely sand, silt, and clay." The Modesto Formation was mapped in the Lodi <br /> area by Atwater 5(Plate 6). Shown on the Atwater's geologic map is a dense stipple pattern that <br /> represents a deposit of loose sand that is probably wind blown(eolian). The light stipple pattern <br /> on the map represents probable river deposits(fluvial). Atwater noted in a shallow boring located <br /> along Kingdon Road the wind blown sand was 3.5 feet thick and was overlying compact silty sand <br /> and sandy silt(Plate 6). The surface sand thickness was found to be about 1 foot within the soil <br /> boring at the proposed project location. <br /> The surface and near surface soils located at the proposed project location are reported to <br /> be the Devries sandy loam(Plate 7). The Devries sandy loam is described by the Soil Survey <br /> report as "moderately deep to a hard pan and somewhat poorly drained. Typically, the surface <br /> layer is a grayish brown sandy loam about 13 inches thick. The upper part of the subsoil is light <br /> gray, mottled sandy loam about 15 inches thick. The lower part to a depth of 80 inches is a light <br /> gray,indurated hardpan. In some areas the surface layer is a fine sandy loam or loam. <br /> Permeability is moderately rapid in the Devries soil. Runoff is slow and the hazard of water <br /> s Hull,L.C., 1984,Geochemistry of Ground Water in the Sacramento Valley,California: U.S. Geological <br /> Survey Professional Paper 1401-B. <br /> Helley,E.J.,and Harwood,D.S., 1985, Geologic Map of the Late Cenozoic Deposits of the Sacramento <br /> Valley and Northern Sierran Foothills, California.U.S. Geological Survey miscellaneous field studies map MF- <br /> 1790, scale 1:62,500, 5 sheets. <br /> 5 Atwater,B.F., 1982,Geologic Maps of the Sacramento-San Joaquin Delta,California. U.S. Geological <br /> Survey miscellaneous field studies map MF-1401, scale 1:24,000,20 sheets. <br /> ra � <br /> � e <br /> V <br />