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02 March 2020 AdvancedGeo <br /> Project No. 20-5001 AnEmployee-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 Jacktone clay having 0 to 2 percent slopes (#180). The <br /> Jacktone clay land complex is composed of alluvium derived from mixed rock sources. <br /> Soils are described as somewhat poorly drained; with a very low permeability; and salinity <br /> of less than 2.0 millimhos per centimeter (mmhos/cm). The Jacktone clay complex <br /> typically have the same chemical properties between surface grade and 37 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 and have low water storage. These soils will allow low infiltration of water <br /> through the surface soils. The longer the effluent remains near the surface, the more <br /> treatment is enhanced due to natural processes within the soil. If the permeable soils exist <br /> to the depth of the groundwater table, it is possible that surface contaminants may be <br /> transported fairly rapidly. <br /> 8.0. GROUNDWATER ANALYSIS <br /> There is currently no potable water source supplied to the subject property. A domestic <br /> water well is planned to be installed to the east of the proposed residence and will provide <br /> potable water to the residence and property. <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 75 feet bsg. Between 2011 and 2018, depth <br /> to groundwater at the site has fluctuated between 75 and 85 feet bsg. Groundwater flow <br /> direction locally appears to be toward the west-southwest. Groundwater was not <br /> encountered in the 42-inch deep percolation test hole advanced on 06 February 2020. <br /> 8.2. EXISTING OR POTENTIAL GROUNDWATER CONTAMINATION <br /> The immediately adjacent and outlying land use for the parcel is residential and <br /> commercial. Potential groundwater contamination can occur from several sources <br /> including leaking underground storage tanks, septic systems, agricultural activities, <br /> dairies, and stormwater infiltration. <br />