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biodegradation is not considered in any of the model runs, all three model scenarios represent very <br /> conservative predictions of the potential impacts to the shallow aquifer <br /> 5 3 HYDROLOGIC PARAMETERS <br /> 1 <br /> Hydrologic and soil chemical input and output parameters are shown in Table 9 Hydrologic <br />' parameters include <br /> • Infiltration rate, and <br /> • Depth to groundwater <br /> ' In the Stockton area, the average annual infiltration was assumed to be 20 percent of the annual <br /> rainfall of 15 inches for unpaved conditions However, because the site is capped with asphalt, an <br /> ' infiltration rate of 2 percent of precipitation was assumed As described above, three depths to <br /> groundwater, 35 feet, 54 feet, and 70 feet bgs were considered In all three cases, a groundwater <br /> ' gradient of 0 002 feet per foot and a hydraulic conductivity of 105 cm/sec was assumed This value <br /> of hydraulic conductivity was obtained from the literature for the lower end of the scale for the sandy <br /> silts and silty sands found at the site A low value of hydraulic conductivity was used to be <br /> conservative <br /> ' 5 4 SOIL CHEMICAL PARAMETERS <br /> ' Soil chemical parameters used in the model include the following <br /> • Organic carbon distribution coefficient (K,,,,,), <br /> • Henry's constant (KH), <br /> • The aqueous solubility, <br /> • The free air diffusion coefficient, <br /> • Dry bulk density, <br /> • Total porosity, <br /> • Volumetric water content, and <br /> • Organic carbon fraction <br /> An estimate of 0 5 percent soil organic carbon content was used The volumetric water <br /> content, solubility, free air diffusion coefficient and Henry's constant were obtained from the <br /> literature Soil properties were estimated based on typical values for sandy silts to silty sands <br /> ' SAC116 07 12 AUGUST 1994 <br /> DAMES & MOORE <br />