Laserfiche WebLink
• Soil Profile and Geologic Information <br /> The Site is mapped on the Geologic map of California: San Jose Sheet (Rogers, 1966). <br /> It is depicted within a map unit of Pleistocene nonmarine deposits (Plate 7). <br /> The surface and near surface soils located at the Site are reported by the Web Soil <br /> Survey (USDA, 2016) to be composed of the San Joaquin complex (Plate 8). The table <br /> 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 /> San Joaquin 0-16 Loam; CL-ML ML <2 5.6-6.5 0.6-2.0 Severe: <br /> complex, 16-26 Clay loam, clay; CL <2 6.1-7.8 <0.06 cemented <br /> 0-1% 26-60 Indurated pan, peres <br /> slopes, 241 slow) <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 May 23 through June 3, 2016, Live Oak excavated soil borings on the two proposed <br /> parcel of the Site for the purpose of conducting percolation tests. A shallow boring was <br /> excavated on Parcel 1; both shallow and deep borings were excavated on Parcel 2. <br /> The borings were four inches in diameter, 3.30, 3.40, and 14.50 feet deep, and were <br /> excavated by hand auger (Table 2). The locations of the borings are indicated on Plate <br /> 9. <br /> The soil in the borings was similar to that described by the Soil Survey. At location P1, <br /> sandy clay was encountered to a depth of 2.5 feet, followed by clayey sand to the full <br /> depth of the boring (3.4 feet). At location P2, sandy clay was encountered to a depth of <br /> 10 feet, followed by clayey sand to a depth of 13 feet, followed by sandy clay to the full <br /> depth of the boring (14.50 feet). The soil logs are presented on Plates 10 and 11. <br /> Discussion of Soil Lithology <br /> Based on the soil observed in the borings, there appears to be moderate potential for <br /> percolation at the test locations. Sandy soils generally have a much greater potential <br /> for percolation than fine-grained or cemented soils. However, a percolation test is the <br /> only accepted method for determining the suitability of the soils for a septic disposal <br /> area. Percolation test results are discussed in the following section. <br /> • <br /> LOGE 1608 Page 4 <br />