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Soil Suitability/ Nitrate Loading Study Irerracon Jeremy Winery ■ Lodi, CA May 7, 2019 ■ Terracon Project No. NA197008 1.4 Groundwater Information 1.4.1 Groundwater Depth and Gradient Groundwater was not encountered within our geotechnical or percolation test borings which were excavated between 3.5 feet below grade surface (bgs) and 25 feet bgs. According to the San Joaquin County Flood Control and Water Conservation District Groundwater Report (SJCWCD) Lines of Equal Depth to Groundwater Spring and Fall 2015 to 2016, groundwater depth lies between approximately 120 and 130 feet bgs. Based on a review of Department of Water Resources (DWR) Well Completion Report dated 2015 for the adjoining northern property, depth of the static water level measured at 90 feet bgs. The groundwater flow direction and the depth to shallow, unconfined groundwater, if present, would likely vary depending upon seasonal variations in rainfall and other hydrogeological features. Without the benefit of on-site groundwater monitoring wells surveyed to a datum, groundwater depth and flow direction beneath the site cannot be directly ascertained. 1.4.2 Potential Groundwater Contamination Issues Potential groundwater contamination can occur from a number of sources including historical petroleum hydrocarbon use, agricultural activities, dairies, septic systems, and storm water infiltration. As per EHD requirements nitrate as N and 1,2-dibromo-3-chloropropane (DBCP) have been included as part of the SSS discussion. Identifying potential groundwater contamination other than nitrates and DBCP is beyond the scope of work for this report. The presence of nitrates is not uncommon in shallow groundwater aquifers in San Joaquin County and other parts of the Central Valley. Nitrate in groundwater occurs as a result of the application of fertilizers, livestock waste, and untreated septic tank waste. Nitrate is mobile and often accumulates in the shallow groundwater zones. In the early 1900s, natural levels of nitrate in groundwater were measured in forty-three (43)wells throughout the Sacramento Valley by Kirk Bryan (1923). It was thought that groundwater at that time was close to "natural" conditions. Based on the work by Bryan, it is estimated that under "natural" conditions, groundwater concentration containing nitrate is no more than about 13.5 milligrams per liter (mg/L) nitrate (NO3) or (3 mg/L-N). Areas having 24.75 mg/L-NO3 (5.5 mg/L- N) or more are those in which nitrate concentrations may be increasing (Hull, 1984). DBCP (dibromochloropropane) is a nematocide and soil fumigant for vegetables and grapes. It is thought to cause health problems consisting of kidney damage, liver damage, and cancer. The use of DBCP was discontinued in 1979. Based on a review of the DWR Water Data Library, from the 1950s to 1970s a groundwater well station depicted approximately 0.25 miles west of the site, was analyzed for various constituents Responsive ■ Resourceful ■ Reliable 7