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13 August 2021 AdvancedGeo <br />Project No. 21-6530 AnfmployeeawoedCompony <br />Page 8 of 14. <br />6.6. POTENTIAL PROBLEMS PREDICTED <br />On site soils within the shallow percolation test hole demonstrated an adequate <br />percolation rate. <br />6.7. PERCOLATION TEST FINDINGS <br />The shallow percolation test performed provided a satisfactory percolation test rate. The <br />percolation rate of 5.68 minutes per inch was calculated from data collected during the <br />four-hour percolation test; the final reading over the four-hour period was used to <br />calculate the percolation rate. The use of the proposed septic system should follow the <br />San Joaquin County On-site Wastewater Treatment Standards. <br />7.0. CHEMICAL AND PHYSICAL PROPERTIES OF SOIL <br />Soil chemical properties were supplied by regionally sourced material for the surrounding <br />area. <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 Galt clay having 0 to 1 percent slopes (#160). The Galt <br />clay is composed of alluvium derived from mixed rock sources. Soils are described as <br />somewhat poorly drained, with a moderately low permeability, and salinity ranging from <br />0.2 to 0.5 millimhos per centimeter (mmhos/cm). The Galt clay typically features clay from <br />0 to 32 inches bsg and cemented soils from 32 to 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 and have moderate water storage. These soils will allow moderate infiltration <br />of water through the surface soils. The longer the effluent remains near the surface, the <br />more treatment is enhanced due to natural processes within the soil. If the permeable <br />soils exist to the depth of the groundwater table, it is possible that surface contaminants <br />may be transported fairly rapidly. <br />