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Soil Suitability Nitrate Loading Study <br /> Manteca Unified School District <br /> 2414"Street,French Camp,CA <br /> Page 5 <br /> Modesto Formation Holocene alluvial fan deposits. The geologic distribution of near-surface deposits in <br /> the vicinity of the site is shown in Figure 5 (Appendix A). <br /> The subsurface soils encountered at the French Camp Elementary School Site consist of unconsolidated <br /> alluvium to the maximum depth explored of 51.5 feet bgs,as logged during drilling of geotechnical borings <br /> in April 2019. Shallow soils consist generally of lean clean to a depth of approximately 2.5 feet bgs, <br /> underlain by silt to approximately 9.5 feet, and lean to fat clay from approximately 9.5 feet bgs to <br /> approximately 24 feet, bgs. Groundwater was initially encountered at approximately 26 feet bgs within a <br /> sandy silt/silty sand zone, but rose to a depth of approximately 20.5 feet within the hollow stem augers. <br /> 1.5.1 Site Map Showing Location,with Dimensions,of the Soil Profile Pit on the Parcel <br /> See Figure 2, Appendix A. <br /> 1.5.2 Description of Soil Profile Pit Including Depth and Dimensions <br /> See Table 3, below. <br /> Table 3 <br /> Descri tion of Soil Profile/Test Holes <br /> Test Holes Diameter in Depth Interval ft Soil Type Soil Class USCS <br /> 2 4 0-3 Jacktone Clay CL <br /> 1 4 0-3 Leach Line Fill CL-ML <br /> 1.5.3 Soil Lithology <br /> Condor classified shallow soil as lean clay(CL)pursuant to the Unified Soil Classification System(USCS). <br /> Shallow soil in the proposed project area was classified by the U.S. Department of Agriculture, Natural <br /> Resource Conservation Service(MRCS)as Jacktone Clay,whose general properties are 0 to 2 percent slope, <br /> somewhat poorly drained, with high runoff. Pertinent information from the NRCS soil survey report are <br /> included in Appendix E. <br /> 1.5.4 Discussion of Soil Lithology as Related to Future Onsite Septic Uses <br /> In general, soil description and classification which indicate slow percolation rates for septic system <br /> effluent. The clayey soil with relatively slow percolation generally promotes denitrification of the septic <br /> system effluent. It should also be noted that the school has already been permitted for three previous septic <br /> tanks and associated leach lines and leach lines additions (summarized in Section 1.3.2 above), although <br /> one of the previously permitted tanks is no longer in use and has been filled. <br /> 1.6 PERCOLATION TEST INFORMATION SECTION <br /> 1.6.1 Site Map Showing the Location of the Percolation Test Holes <br /> See Section 1.5.2 and Figure 2, Appendix A. <br /> 1.6.2 Number of Shallow and Deep Percolation Tests was Performed for Each Parcel <br /> Two shallow percolation tests were performed on the Site at a depth of 3 feet bgs in the area of the proposed <br /> leach field. <br /> rill= CONDOR <br />