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LUCCA WINERY <br /> SOIL SUITABILITY & NITRATE LOADING STUDY MAY 2013 <br /> Table 2 Percolation Test Results for the Disposal Area <br /> Percolation Test Results for the Disposal Area with Corresponding <br /> Application Rates in Gallons / Ft2/ Day <br /> Sample Depth <br /> Below Ground Percolation Rate (min/in) Application Rate (gallons/ft2/day) <br /> Surface ft <br /> 3.0 1.9 1.200 <br /> 7.0 6.7 0.971 <br /> Application Rate adapted from California State Water Resources Control Board Guidelines for the <br /> Design of Sewage Systems and is based on the Perc Rate. <br /> D. Groundwater Information <br /> NLS§ 2.1, SSS§ 4.1, 4.3. Groundwater depths and elevations throughout San Joaquin <br /> County are illustrated on maps published by the County Flood Control and Water <br /> Conservation District. The most recent Groundwater Report for the County (Spring <br /> 2011) provides groundwater elevations in wells within the South San Joaquin Irrigation <br /> District (SSJID). The following is a summary of the wells monitored by the County <br /> within SSJID: <br /> In Well "P", State Well ID 01S09E34A001M, depth to water in the early 1970's <br /> was around 57 feet. In 2011, depth to water was approximately 75 feet below <br /> ground surface. Based upon the trend line for the hydrograph, the average <br /> annual decline in depth to water for the well is 0.4 ft/year. <br /> • In Well "T", State Well ID 01S08E27A001M, depth to water in 1964 was around <br /> 40 feet. In 2011, depth to water was approximately 67 feet below ground surface. <br /> Based upon the trend line for the hydrograph, the average annual decline in <br /> depth to water for the well is 0.8 ft/year. <br /> The nearest well to the site Well °V", State Well ID 02S08E08A001 M, depth to <br /> water in the early 1990's was around 43 feet. In 2011, depth to water was <br /> approximately 44 feet below ground surface. Based upon the trend line for the <br /> hydrograph, there appears to be a general trend of increasing water levels. The <br /> trend provides an approximate increase in water level of 0.1 feet/year. This <br /> increase is potentially due to local groundwater pumping is not prevalent and <br /> _ surface water irrigation is mostly utilized. <br /> The existing on-site domestic well was constructed in early 1997. The drillers log <br /> identified the depth to water level to be 32 feet below ground surface. Upon review of <br /> Well "V", depth to water in 1997 was approximately 37 feet. <br /> Cross Sections across the county were developed for the 2011 report. Cross-sections <br /> ran along Highway 4, 99 and Jack Tone Road. Based upon the trends of groundwater in <br /> the area, the directional flow is generally in a northwesterly direction toward the San <br /> Page 15 <br />