Laserfiche WebLink
Water Sample <br /> Live Oak collected a water sample from the domestic well on the Site on October 18, ( 3� <br /> 2010. The sample was to be analyzed for nitrate and dibromochloropropane (DBCP) 6(_0per 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 DBCPana is, respectively. A trip blank was also utilized. <br /> The sample was placed ice and transported chain of custody to FGL <br /> Environmental, Stockton Results of the tests are forthco <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 Geoloaic_informatiion <br /> The Site is depicted on the Preliminary.geologic map showing Quatemary deposits of <br /> the Lodi Quadrangle, California (Marchand and Atwater, 1979). The Site is depicted <br /> -primarily within the- Riverbank Formation .middle unit, described as "arkosic alluvium <br /> forming Mokelumne River terraces and alluvial fan; chiefly sand; probably glacial <br /> outwash." Portions of the Site also fall within the Riverbank Formation upper unit, <br /> described as "foothilkderived alluvial sand and silt; contains abundant volcanic detritus." <br /> Holocene alluvium, described as channel, levee, and floodplain deposits; chiefly sift <br /> and clay with fine sand along principal drainageways," is present along the north side of <br /> the Site (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 San Joaquin complex, with small areas of Sailboat silt <br /> loam and Bruella sandy loam (Plate 8) (USDA, 2009). The table below presents some <br /> selected properties of these soils. <br /> LOGE1024 Page 4 <br />