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The Particle Size Analysis, and Nitrogen Contents for the two tested soil samples are summarized m <br /> the following Table: <br /> SOIL ANALYSIS <br /> DEPTH SAND% SILT% CLAY% USDAIUSCS 5NITRATE-N <br /> SOIL TEXTURES NT <br /> 10 Ft 32% 32% 36% Clay Loam/Sllty Lean Clay m <br /> 25 Ft 28% 36% 36% Clay Loam/Silty Lean Clay 11 ppm <br /> As noted, the nitrate-nitrogen concentration decreased 39% from the 10-foot depth where there is 18 <br /> ppm NO3 N down to 11 ppm NO3 N at the 25-foot depth. These nitrate-nitrogen concentrations are <br /> medium-to-low. The decrease in concentration with increasing depth indicate that denitrification <br /> may be occurring. This will contribute a lower concentration of nitrate in percolating vadose zone <br /> water down to the zone of saturation. <br /> Additional soil parameters that were tested which pertain to nitrate loading assessment originating <br /> from septic system effluent include: The organic matter content,pH, cation exchange capacity <br /> (CEC), clay content percentage, and soluble salts. Considering the property soils have not been <br /> under agricultural production for many years,the organic matter content in these soils is low, also <br /> contributing a low estimated nitrogen release (ENR). <br /> The significance of cation exchange becomes important when the chemistry of septic effluent is <br /> analyzed. Nitrogen in septic tank effluent consists of approximately 75%N as the ammonium ion <br /> form and 25%N in the organic form. If the ammonium ion is bound and eventually used, <br /> nitrification cannot occur. Consequently, the pH, along with the CEC, have significant influence on <br /> ammonium molecules. The CEC measures the ability of the soil to theoretically trap and hold <br /> ammonium molecules. The two soil samples indicate a comparatively high CEC of 28 meq/100 g at <br /> the 10-foot depth and 27 meq/100 g at the 23-foot depth. This suggests there is a greater potential <br /> for the retention of ammonium molecules by microbial uptake and suppression of nitrification. In <br /> addition, the soil pH is alkaline which also promotes denitrification. <br /> Nitrification is an aerobic reaction accomplished predominately by autotrophic bacteria. Both the <br /> shallow and deeper subsurface soils possess sufficient clay content to_bind the ammani>w ions and <br /> to create microsites within the clay lattices that are anaerobic thus forcing denitrificatigm. <br /> 6o C. PERCOLATION TEST RESULTS <br /> As noted in the Introduction, a new effluent disposal area south of the existing office building was <br /> determined by Mr. David Lagorio. Consequently,percolation testing was done in this area, as <br /> denoted on the attached Site Plan. There are no domestic wells to the south of the subject property <br /> that were within 100 feet of the south property border, and therefore not within 150 feet of the future <br /> effluent disposal area. <br /> 4 <br /> Chesney Consulting <br />