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ttp <br /> time, calculations cannot be performed to estimate nitrogen concentrations. Similarly, grams <br /> of N/capita/day cannot be used since the customers are not living on-site. Therefore, the <br /> scientific literature indicates an average N concentration of 62 mg NIL of discharged effluent <br /> based upon several studies. It is our opinion that this is reliable data. The N in this figure of <br /> 62 mg'N/L is referred to as Total Kjeldahl Nitrogen (TKN) concentrations, which is organic <br /> N plus ammonia. These studies were based upon household effluent _ thus the dilemma: will <br /> the effluent from the restrooms at the Open Air Mall be equivalent to the N composition of <br /> household effluent? Logically, with respect to N alone, we are assuming that it will be. <br /> If we project a daily wastewater flow of 30,000 gals, the N Ioading will be approximately 7 <br /> - kg N/day, or 1,092 kg N/yr. This effluent.N is approximately 75% ammonium ions and 25% <br /> organic N. Upon discharge to the soil, N may undergo mineralization, nitrification, adsorption, <br /> biological uptake, denitrification or eventual volatilization. Consequently, we must only look <br /> at nitrification occurring on the total N loading rates to arrive at potential nitrate impacts. It <br /> must be emphasized that there are numerous factors which lead to the production of nitrates <br /> from sewage effluent. There have been several mathematical models formulated to assist in <br /> explaining the various processes in the soil environment for nitrate production, although they <br /> are extremely complex. <br /> A discussion of various soil tests performed, and the characteristics of the subsurface soils <br /> under the project site will attempt to assess the potential for nitrate (NO3) production. <br /> Nitrification and denitrification are the two main processes controlling NO3 formation and <br /> ultimate NO, concentration. Nitrification is dependant upon the transformation of ammonium <br /> (NH4) ions to nitrate ions under aerobic conditions by bacterial functions. <br /> The soil parameters-analyzed included clay content, organic matter (OM) content, cation <br /> exchange capacity (CEC), and pH. Composites were made from the two 25 ft seepage pit test <br /> boring sites. One composite was from the five ft depth and the other from the 25 ft depth. <br /> The Soil Analysis Report results can be found in the Appendix: <br /> Clay content was measured by the hydrometer method (ASTM D-422) and found to be a <br /> relatively high average of 33% for all four sample locations. High clay content translates to <br /> lower oxygen content of the subsurface soils. Under anaerobic conditions, denitrification is <br /> enhanced. <br /> 10 <br /> Valfey Ag*search <br />