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L <br /> March 24,2005 <br /> NOA Project Number: E05025A <br /> ` The presence of nitrates is not uncommon in shallow ground water aquifers in San Joaquin County <br /> and other parts of the Central Valley. Nitrate in ground water occurs as a result of the application <br /> of fertilizers,livestock waste, and untreated septic tank waste. Nitrate is mobile and often <br /> accumulates in the shallow ground water zones. <br /> In the early 1900s,natural levels of nitrate in ground water were measured in forty-three (43) wells <br /> throughout the Sacramento Valley by Bryan (1923). It was thought that ground water at that time <br /> was close to"natural" conditions. Based on the work by Bryan,it is estimated that under"natural" <br /> conditions,ground water concentration containing nitrate is no more then about 13.5 mg/L-NO3 (3 <br /> mg/L-N). Areas having 24.75 mg/L-NO3 (5.5 mg/L-N) or more are those in which nitrate <br /> concentrations may be increasing (Hull, 1984). <br /> DBCP is a nematocide and soil fumigant for vegetables and grapes. It is thought to cause health <br /> problems consisting of kidney damage,liver damage,and cancer. The use of DBCP was <br /> discontinued in 1979.The Environmental Protection Agency (EPA) set the maximum contaminant <br /> limit(MCL) at 0.2 parts per billion (ppb) because the EPA believes that given present technology <br /> and resources, this is the lowest level to which water systems can reasonably be required to remove <br /> this contaminant should it occur in drinking water. <br /> 6. 4.5 Well Water Sample Collection, Handling, and Transportation <br /> The samples were collected in a clean plastic container, then decanted into clean,glass vials. The <br /> samples were then transported on ice and remanded under chain of custody to Precision Enviro- <br /> Tech,Stockton. <br /> ` 4.6 Chain of Custody <br /> The Chain of Custody document s have been included in the appendix of this report. <br /> 5.0 SOIL PROFILE AND GEOLOGIC INFORMATION <br /> The Site is depicted on the Geologic Map of the San Francisco-San Jose Quadrangle,as within a region of <br /> Quaternary Modesto Formation. Quaternary Modesto Formation is a unit of arkosic alluvium <br /> forming Mokelumne River terraces and alluvial fan;chiefly sand with minor gravel and silt;probably <br /> glacial outwash (Plate 7). <br /> The surface and near surface soils located at the Site are reported by the San Joaquin County Soil Survey <br /> to be composed of the Delhi fine sand, 0-5% slopes,Delhi loamy sand,0-2% slopes,Timor loamy <br /> I sand, 0-2% slopes,Tinnin loamy coarse sand,0-2%slopes and the Veritas fine sandy loam, 0-2% <br /> slopes (Plate 8). Table 5 presents some selected properties of the soils: <br /> 6 <br />