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exist to the depth of the ground -water aquifer, it is possible that any remaining surface contaminants may be transported to the first saturated zone of the aquifer. Because ground water is so deep in the area (116 to 146 feet bgs), there is potential for significant nitrate attenuation before the effluent reaches ground water. Clay -containing soils, like those found on this Site, also tend to inhibit downward movement of nitrate due to adsorption of the nitrate ions to the soil. Sources of Nitrate Dairies, orchards that require fertilization in sandy soils, and septic systems have been found to be the most significant sources of nitrate in ground water. Percolatina Recharae Waters One of the most determinant factors in the Hantzsche and Finnemore equation is the rate of recharge from percolating waters, which mix with the downward -percolating effluent generated by on-site septic systems. In the original Hantzsche and Finnemore paper, "average recharge rate of rainfall" was utilized. Based on San Joaquin County Environmental Health Department policy (personal communication, March 18, 2019), the recharge input for the Hantzsche and Finnemore equation should be derived from average monthly precipitation of rainfall and evapotranspiration rates for the area; the data should be obtained from the California Irrigation Management Information System (CIMIS). Recharge is calculated by first determining whether the average monthly precipitation exceeds average monthly potential evapotranspiration. If so, then the difference is the percolating recharge water into the aquifer. Runoff and stream infiltration drainage are not factored into the calculation. This approach likely under -estimates recharge to the aquifer and, consequently, over-estimates nitrate loading. The Site is located closest to the CIMIS Manteca station. Data from the Manteca station were available for 2014 through 2021; based on the calculation shown, the estimated rate of recharge from percolating waters for the Manteca station is determined to be 3.21 inches (Plate 12). A statistical error of 54 percent is associated with this value. Quality of Rainwater Hantzsche and Finnemore listed 1 mg/L-N as the nitrate concentration of rainwater for their original calculation; in the past, Live Oak has also utilized this value for the nitrate loading calculation. To determine a more accurate local value, Live Oak has collected rainwater during several recent storm events in Lodi. Each sample was collected in a clean, dry, LOGE 2226 Page 9