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SOIL INFORMATION <br /> NLS§ 1.1. The UC Davis Soil Web Map indicates the Map Unit to be a Veritas fine sandy loam <br /> (4266), with Grangeville, Bisgani, Madera and Tinnen fine sandy loams soils compose the <br /> remaining portions of the subject soils. <br /> During the percolation test boring procedure, soil samples were retrieved from the 3 ft, 8 ft and 25 <br /> ft depths for physical and chemical analyses. The attached texture analysis reveals the underlying <br /> soils consists of a clay loam and sandy clay loam. The clay content percentage of the on-site soils <br /> can be considered high enough to promote denitrification potential. <br /> NLS§ 1.2. As noted on the attached Soil Analysis Report,the chemical analyses conducted <br /> quantifies several constituents that influence nitrate loading for this project. The important <br /> parameters for nitrate loading assessment are the organic matter percentage,pH, cation exchange <br /> capacity(CEC),the magnesium/calcium cation saturation percentages, and the nitrate-nitrogen <br /> content of the soil. <br /> SSS§2.1. The organic matter is low at 1.3% and 1.1% at the 3 ft and 8 ft depths, and decreases to <br /> 0.5%at the 25 ft depth. These OM concentrations suggest there is a low potential for future <br /> nitrate forming from organic matter, but sufficient for denitrification potential. Since septic <br /> effluent is composed predominately of ammonium(NH4),the pH, along with the CEC, have <br /> significant influence on ammonium molecules. The magnesium saturation percentage is high in the <br /> shallow soils and has the potential of detaining infiltration and percolation. <br /> The pH of the soil is alkaline which may have the effect of promoting ammonia formation and not <br /> ammonium formation. The CEC measures the ability of the soil to theoretically trap and hold <br /> ammonium molecules and was measured at 27.6 meq/100 g,which is a comparatively high value. <br /> This suggests a high potential for the retention of ammonium molecules that may form for microbial <br /> assimilation within the soil environment. The nitrate-nitrogen concentrations exhibit interesting <br /> results: The NO3-N concentration at the 3 ft depth is 3 ppm, increases to 6 ppm at the 8 ft depth and <br /> then decreases to 3 ppm at the 25 ft depth,thus indicating a possible significant denitrification <br /> potential. <br /> NLS§3.3. Table 1 below summarizes the analyzed soil physical and chemical characteristics <br /> from the retrieved soil sample. <br /> Page -2- <br /> Chesney Consulting <br />