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17 January 2020 AdvancedCeo <br /> Project No. 19-4964 An Employee Owned Company <br /> Page 9 of 14 <br /> 7.1. CHEMICAL AND PHYSICAL PROPERTIES OF SITE SOILS <br /> The dominant soil composition in the general area of the property was inferred from <br /> information provided by the United States Department of Agriculture's Soil Geographic <br /> Database (USDASGD). The USDASGD soil survey indicates the soil type for the property <br /> is predominantly composed of Honcut sandy loam having 0 to 2 percent slopes (#175). <br /> The Honcut sandy loam land complex is composed of alluvium derived from granitic rock <br /> sources and is dominated by sandy loam. Soils are described as well drained; with a <br /> moderate to high permeability; and salinity of less than 2.0 millimhos per centimeter <br /> (mmhos/cm). Sands in the Honcut sandy loam complex typically have the same chemical <br /> properties between surface grade and 60 inches bsg. <br /> 7.2. MASS TRANSPORT PROPERTIES OF UNDERLYING SITE SOILS <br /> The percolation test and dominant soil type at the site indicates that the soils are semi- <br /> permeable to permeable and have moderate water storage. These soils will allow <br /> moderate to high infiltration of water through the surface soils. The longer the effluent <br /> remains near the surface, the more treatment is enhanced due to natural processes within <br /> the soil. If the permeable soils exist to the depth of the groundwater table, it is possible <br /> that surface contaminants may be transported fairly rapidly. <br /> 8.0. GROUNDWATER ANALYSIS <br /> The subject property is supplied with potable water by the onsite domestic water well <br /> located to the south of the existing residence (Figure 2). A groundwater sample was <br /> collected from the well and analyzed for nitrates as part of this study. <br /> 8.1. DESCRIPTION OF LOCAL GROUNDWATER <br /> According to the San Joaquin County Flood Control and Water Conservation District's <br /> Lines of Equal Depth to Groundwater Fall 2018 and the DWR Water Data Library, depth <br /> to groundwater at the site is approximately 20 to 25 bsg. Groundwater flow direction <br /> locally appears to be toward the southwest. Groundwater was not encountered in the 42- <br /> inch deep percolation test hole on 10 January 2020. <br /> 8.2. EXISTING OR POTENTIAL GROUNDWATER CONTAMINATION <br /> The immediately adjacent and outlying land use for the parcel is residential, <br /> governmental, and agricultural. Potential groundwater contamination can occur from <br /> several sources including leaking underground storage tanks, septic systems, agricultural <br /> activities, dairies, and stormwater infiltration. <br />