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Soil Profile and Geologic Information <br /> The Site is mapped on the Geologic Map of California: San Jose sheet (Rodgers, 1966). <br /> It is depicted within map units of Great Valley fan deposits and Pleistocene nonmarine <br /> material (Plate 7). <br /> The surface and near surface soils located at the Site are reported by the Soil Survey of <br /> San Joaquin County, California (USDA, 1992) to be composed of Capay clay (Plate 8). <br /> The table below presents some selected properties of this soil: <br /> Table 1. Selected Properties of On-Site Soils (USDA, 1992) <br /> Soil Name Depth Unified Soil Salinity Soil Perme- Septic tank <br /> and Map (in) Classification mmhos/cm Reaction ability absorption <br /> Symbol pH (in/hr) fields <br /> Capay Clay, 0-20: Clay: CH, CL <2 6.6 - 8.4 0.06 - 0-2 Severe: <br /> 0-2% 20-60: Clay, silty clay: CL, CH <2 6.6 - 8-4 0-06-0.2 peres slowly <br /> slopes, 118 <br /> Capay Clay, 0-20: Clay; CH, CL <4 6.6- 8.4 0.06 - 0.2 Severe: <br /> wet, 0-2% 20-44: Clay, silty clay: CH, CL <4 6.6 - 8.4 0.06 - 0.2 peres slowly <br /> slopes, 121 44-60: Silty clay loam. clay <4 6.6 - 8.4 0.06- 0.2 <br /> loam: CL <br /> Note: The table descriptions do not necessarily reflect site-specific soil properties. See description of the map unit for <br /> composition and behavior characteristics of the map unit. <br /> Soil Borings <br /> On March 31, 2015, Live Oak excavated a shallow soil boring on the proposed <br /> homesite parcel the Site for the purpose of conducting a percolation test. The boring <br /> was four inches in diameter, 3.45 feet deep, and was excavated by hand auger (Table <br /> 2). The location of the boring is indicated on Plate 9. <br /> The soil in the boring was similar to that described by the Soil Survey. Clay was <br /> encountered to a depth of 2.5 feet, followed by clay with sand to the full depth of the <br /> hole. The soil log is presented on Plate 10. <br /> Discussion of Soil Lithology <br /> Based on the soil observed in the boring, there appears to be moderate potential for <br /> percolation in the shallow soil zone at the test location. Sandy soils generally have a <br /> much greater potential for percolation than fine-grained or cemented soils. However, a <br /> percolation test is the only accepted method for determining the suitability of the soils <br /> for a septic disposal area. Percolation test results are discussed in the following <br /> section. <br /> LOGE 1502 Page 5 <br />