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Inflow to the pond consists primarily of diversions of water from the wastewater treatment <br /> plant. These diversions originate from two main sources in the Tracy area: Leprino Foods <br /> and Heinz USA. Diversions to the holding ponds may either be Industrial Raw Influent <br /> (mainly from Heinz USA, but possibly including small quantities of domestic sewage) that <br /> has not been treated, or Industrial Primary Effluent that has undergone primary treatment <br /> at the Wastewater Treatment Plant. Both of these diversions occur mainly during the can- <br /> ning season that emends from July through October each year, and are measured by the City <br /> with flowmeters and totalizers. Another potential source of water to the ponds is from pre- <br /> cipitation, which is expected to be a relatively minor source of water during the canning <br /> season. <br /> Outflow from the ponds may potentially occur in two ways: by evaporation from the surface <br /> of the ponds; and by infiltration through the base of the ponds. During the canning season, <br /> when temperatures are high and humidity is low, evaporation should be a relatively <br /> significant loss. Of course, the volume of water lost through infiltration is unknown and is <br /> the object of this study. <br /> The change in storage is the volume of water contained in the holding ponds at the end of <br /> the study minus the volume of water contained in the holding ponds at the beginning of the <br /> study. As might be expected, a large decrease in the volume of water stored in the ponds <br /> must be accounted for by either evaporation or infiltration. <br /> The relationship presented above may therefore be expanded as follows : <br /> I,,,f1 + P = Eo + O�F, + (Vz - V1) <br /> where: <br /> I,urf = volume of water pumped into the ponds <br /> P = volume of precipitation onto the ponds <br /> Eo = volume of water evaporated <br /> OSE, = volume of water infiltrated through the base of the ponds <br /> V, = volume of water in the ponds at the end of the measurement period <br /> V1 = volume of water in the ponds at the beginning of the measurement period <br /> The relationship may be rearranged to solve for 0.,: <br /> O,nF = I,urf + P - Eo - (VZ - V1) <br /> Thus, if each of the variables on the right side of the equation are measured, then the <br /> volume of water infiltrating through the base of the ponds may be calculated. I,., will be <br /> measured using a flowmeter with a totalizer that will calculate the volume of water <br /> discharged through the pipe. The City will record the volume of water pumped through the <br /> pipe at the beginning and end of the measuring period. P and Eo may be estimated by <br /> obtaining data from the City's weather station. <br /> SAC/SAC36357/041.WP5 12 - 8/94 <br />