Laserfiche WebLink
i <br /> IIn n <br /> Water Sample <br /> A water sample was collected from the domestic well on the Site on October 21, 2009 <br /> by David Welch. The sample was to be analyzed for Nitrate and dibromochloropropane <br /> (DBCP) per San Joaquin County Environmental Health Department policy. <br /> As required by the laboratory, the sample was collected in a plastic container and two <br /> glass vials for nitrate and DBCP analysis, respectively. A trip blank was also utilized. <br /> The sample was placed on ice and transported under chain of custody to FGL <br /> Environmental, Stockton. Results of the tests are forthcoming. <br /> Nitrate is commonly detected in shallow ground water aquifers of the Central Valley. <br /> Application of fertilizers, livestock waste, and untreated septic tank waste can all <br /> contribute to nitrate in ground water. Nitrate is mobile and tends to accumulate in <br /> shallow ground water zones. Based on work in the Sacramento Valley from the early <br /> 1900s, it is estimated that under "natural" conditions, ground water contains nitrate at <br /> concentrations no more then about 13.5 mg/L-NO3 (3 mg/L-N). Nitrate may be <br /> increasing in areas with concentrations of 24.75 mg/L-NO3 (5.5 mg/L-N) or more (Hull, <br /> 1984). <br /> DBCP is a nematocide and soil fumigant for vegetables and grapes. It is known to <br /> cause male reproductive effects and is classified as a probable human carcinogen. <br /> Most domestic use of DBCP was discontinued in 1977 through 1979. The US EPA set <br /> the MCL at 0.2 parts per billion (ppb) because it believes that given present technology <br /> and resources, this is the lowest level to which water systems can reasonably be <br /> required to remove this contaminant should it occur in drinking water. The Maximum <br /> Contaminant Level Goal (MCLG) for DBCP is zero. <br /> Soil Profile and Geologic Information <br /> The Site is depicted on the Preliminary Geologic map of Cenozoic Deposits of the <br /> Bellota Quadrangle, California (Marchand and Atwater, 1979). A map unit of the <br /> Riverbank Formation middle member is depicted on the Site. This map unit represents <br /> "arkosic alluvium forming Mokelumne River river terraces and alluvial fans; chiefly sand; <br /> probably glacial outwash" (Plate 7). <br /> The surface and near surface soils located at the Site are reported by the USDA Web <br /> Soil Survey to be composed of Bruella sandy loam, 0 to 2 percent slopes, Bruella sandy <br /> loam, hard substratum, 0 to 2 percent slopes, and San Joaquin loam, thick surface, 0 to <br /> 2 percent slopes (Plate 8) (USDA, 2009). The table below presents some selected <br /> properties of these soils: <br /> C7 <br /> LOGE0915 Page 4 <br />