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October 13, 2004 <br /> ` NOA Project Number: E040109A <br /> drilling of two percolation test holes to a depth of 25 feet on September 17,2004. <br /> ✓4.2 Potential Ground Water Contamination Issues <br /> Identifying potential ground-water contamination sources was not part of the scope of work for the <br /> soil suitability study. Potential ground-water contamination can occur from a number of sources <br /> which often include leaky underground storage tanks,agricultural activities, dairies, septic systems, <br /> 60 and storm water infiltration. Any past agricultural activities and the present use of septic systems in <br /> the area should be considered potential ground-water contamination sources. <br /> 4.3 Water Sample Location <br /> One domestic well exists on the Site. No records of these wells were found during file review at <br /> EHD on October 4, 2004,presumably because the well was recently developed. <br /> Three water samples were collected at the well head of the on-site domestic water well on October <br /> 1, 2004 by Mr.Angel Chavez of our office. The locations of the well and water sample are indicated <br /> in Plate 1. <br /> /4.4 Water Sample Constituents <br /> The water sample was analyzed for nitrate and DBCP. Nitrate was found at m /L-N3iOell <br /> belo_ a maximum contaminant level (MCL) set by the US EPA of 45 mg/L-NO3. DBCP was <br /> of detectedn the water sample. The analytical reports prepared by Precision Enviro-Tech can be <br /> found in the appendix of this report. <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 /> i 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 /> ion 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 /> 5 <br />