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FFB. S01LPHYSICAL CHARACTERISTICS AND ANALYTICAL TEST RESULTSStates Department of Agriculture -Soil Conservation Service (USDA-SCS)indicates the on-siteist of a Capay Clay-Urban Land Complex (#122). This correlates with the average clay soilesults of 38% from the samples analyzed from the future filter bed soil. <br /> SS§5.2 a surface and subsurface soil investigation and testing began with three( 15-fo t deep borings 7 <br /> drill d wi a truck-mounted drill rig: One boring near the center of the Future Filter rea, one boring in <br /> the Ex' mg Leachfieldarea, and one boring near the center of the Reserve.Leach ie d area. The Existing <br /> Leachfield area is presumably directly west of the office building, where there appeared to be a"green <br /> stripe"in the lawn area signifying a potential leachiine. The soil boring was drilled next to this green stripe. <br /> Soil samples were taken every five feet for chemical and physical a lysis. In addition; soil samples were <br /> also taken from two shallow percolation test borings at the 24�and 366 ch depths from the future filter bed. <br /> These three deep borings provided: 1.)A profile of the underlying soil characteristics, 2.)Depth to <br /> groundwater, which was found to be approximately I 1 feet below grade, 3.) Saturated formation(first <br /> aquifer)material type, analyzed to be predominately a clay soil type, and 4.)A water table sample for <br /> analysis,which is discussed on Page 7. No rust mottling was observed in any of the borings that would be <br /> indicative of seasonal soil saturation caused by a dramatic rise in the water table elevation. As discussed <br /> below, the water table has apparently risen t 8 feet below gr nd surface(bgs)from on-site monitoring <br /> well data. <br /> NLS§ 1.1, 1.2 As the noted on the SOIL ANALYSIS REPORTS,chemical analyses of the soil samples <br /> quantify s eral constituents that will influence nitrate loading from this project. The important parameters <br /> for nitrate loading assessment are the organic matter,pH cation exchange capaei (CE ,clay content <br /> percentage, along with nitrate-nitrogen�ontent and Total Kjeldahl Nitrogen`(TKN)content.TION measures <br /> the organic and ammonia fractions of nitrogen. It was tested for two reasons: 1.)To determine any increase <br /> in TKN concentrations under the existing Leachfield for comparison with the other two sample sites, and 2.) <br /> To establish a baseline in the event soil under the future filter bed is ever tested for a monitoring program. <br /> There was no significant difference among the three soil samples for TKN. <br /> As noted,the organic matter in the soil is expectedly low. This suggests a very low potential for future <br /> nitrate-nitrogen loading from indigenous nitrogen soil content. Since septic effluent is composed <br /> predominately of ammonium(NH4), the pH, along with the CEC, are significant influences on ammonium <br /> molecules. The pH of the soil is moderately alkaline which may slightly inhibit ammonium formation and <br /> stability, and may create a small propensity for ammonia(NH,)formation. The CEC measures the ability of <br /> the soil to theoretically trap and hold ammonium molecules. Cation Exchange Capacities of the soil <br /> samples are in the high teens and twenties,which suggests there is some potential for the retention of <br /> ammonium molecules for microbial uptake, and suppression of nitrification. <br /> The Standard Penetration Test(SPT)results illustrated ' Table 1 are the number of blows required to drive <br /> a standard two-inch O.D. split spoon sampler one foot indisturbed soil with a 140-pound weight falling <br /> 30 inches. Relative condition of clay soils from this procedure can be classified as soft,medium, stiff, very <br /> stiff and hard. As observed,only two of the SPT tests show a very stiff clay soil, while the remaining soil is <br /> classified as stiff. These two tests classifying the soil as stiff were found in the future filter bed area. <br /> Consequently, it was decided to drill two additional 15 ft deep borings south of the existing entrance <br /> driveway to test for not only for this very stiff clay stratum,but also for more permeable strata(borings <br /> could not be drilled to the north because of railroad tracks). The very stiff stratum was not encountered to <br /> the south of the proposed filter bed location, signifying this stratum is intermittent. Strata with greater <br /> permeability(e.g., sand, silty sand)were also not encountered. <br /> 3 <br /> Chesney Consulting <br />