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" comparison to the low density housing and indicates the shallow soils in the area are not conducive <br /> to acceptable management of sewage effluent over long periods of time. This is primarily attributed <br /> to the tight, silty soils at the leachline depth. <br /> [3] SOIL PROFILE AND PERCOLATION TESTING <br /> One shallow percolation test was conducted on Parcel 1 according to San Joaquin County <br /> Department of Environmental Health regulations. No perc test was performed on the Designated <br /> Remainder per Department regulations. The perc test location is illustrated on the attached Parcel <br /> Map. Percolation test results can be found on the Field Test Data Sheet in the Appendix. <br /> Perc test results indicate a comparatively fast percolation after the four hour test period. Soil <br /> structures consists of a tight sandy silt (SM) throughout the shallow soil profile. No hardpan <br /> _ layer was encountered. The boring was pre-saturated the total depth, 24 hrs prior to starting the <br /> perc test to induce worst-case saturated soil conditions. <br /> Percolation test results indicate a perc rate of 7.1 min/in for Parcel 1. Considering the soil type, <br /> this rate can be considered favorable. It is our opinion that the material at the test depth of 42 <br /> inches is of sufficient porosity to allow water infiltration and percolation. However, repeated <br /> saturations from septic effluent in conjunction with the propensity of the soil to build up a biomat, <br /> leads to leachline failures as evidenced by the repairs. <br /> [4] LOCAL GROUNDWATER AND SURFACE WATER INFORMATION <br /> The static water table depth, or the zone of saturation is located at approximately 55 feet below grade <br /> from the sounding of a domestic well on Ohm Road. The 1996 "Lines of Equal Depth" published by <br /> " the San Joaquin County Flood Control District does not reference the static water table depths in this <br /> area. It is possible there may be perched water table conditions under the subject property at a higher <br /> elevation than the static water level and this should be investigated if seepage pits are ever installed. <br /> There is no potential for septic impact to any surface waters, providing applicable distance <br /> requirements are followed. The property is not in the flood plain. <br /> Analysis of water drawn from the domestic well at the farm labor residences near the intersection of <br /> Ohm Road and Koster Road indicates a nitrate concentration of 22 ppm NO3. The Maximum <br /> Contaminant Level (MCL) for NO3 in drinking water is 45 ppm. The pesticides DBCP and EDB <br /> were not detected(ND). A nitrate concentration of 22 ppm indicates the underlying shallow aquifers <br /> have been moderately impacted from nitrogen contributors, such as agricultural operations, septic <br /> systems or rainfall. No well logs were available in the area to verify if clay layers may have helped <br /> attenuate the downward migration of nitrate molecules. <br /> 2 <br />