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Calculation of Alkalinity Requirement for Nitrification <br /> The nitrate-nitrogen loading from the wastewater effluent and the indigenous soil nitrogen is <br /> contingent upon the environmental factors required for nitrification to occur. These conditions <br /> include soil pore-space oxygen content, soil temperature, pH, electrical conductivity, organic <br /> matter, cation exchange capacity, and alkalinity. Alkalinity in wastewater effluent is derived from <br /> the City of Tracy well water, in addition to the introduction of wastes. Nitrification consumes <br /> approximately 7.1 mg of alkalinity for every mg of ammonia-nitrogen (NH4-N) oxidized. <br /> Nitrification of the Total Kjeldahl Nitrogen(TKN) concentration of 146 mg/L, from a septic tank <br /> sample that serves the existing Holly Commerce Center as discussed below, would require: 146 <br /> mg/L NH4-N x 7.1 mg CaCO3 = 1,037 mg/L alkalinity. The alkalinity concentration in the City <br /> water is unknown. The level found in the water table was 15 mg/L. Therefore,there is an <br /> insufficient alkalinity concentration for complete nitrification to readily proceed without the <br /> introduction of wastes and the alkalinity that may be derived from the soil environment. <br /> E. SURFACE WATER INFORMATION <br /> Storm water drainage management will be by on-site retention as engineered by Siegfried. <br /> Rainwater storage will theoretically provide a water table dilution effect to percolating wastewater <br /> effluent although this effect is indeterminable since the water table elevation and directional flow is <br /> variable throughout the entire project site. As referenced in the next Section, rainfall.in comparison <br /> to evapotranspiration is minimal. <br /> Climatic Data: Rainfall versus Evapotranspiration <br /> NLS§3.2. It is generally and scientifically accepted that when precipitation exceeds <br /> evapotranspiration(Eto), deep percolation of surface rainwater may occur. Evapotranspiration <br /> refers to water evaporation that takes place both at the soil surface and transpiration by plants. <br /> The following Table illustrates rainfall and evapotranspiration for the Tracy area. Precipitation data <br /> was obtained from the Soil Survey of San Joaquin County. The conservative "2 years in 10"data <br /> was used and not the "average rainfall"data. . <br /> TABLE 4 <br /> PRECIPITATION AND Eto DATA FOR TRACY, CA <br /> Month 2 Years in 10 will have more Eto Average Potential Deep <br /> precipitation than: (in/mo) (in/mo) (in/day) Percolation(in/mo) <br /> January 2.93 1.55 0.05 1.38 <br /> February 2.21 2.24 0.08 -- <br /> March 2.38 3.72 0.12 - <br /> April 1.51 5.10 0.17 <br /> May 0.71 6.82 0.22 -- <br /> Page -5- <br /> Chesney Consulting <br />