Laserfiche WebLink
Executive Summary <br /> The fate and transport model VLEACH(Version 2 2 0 2) was used to predict future groundwater <br /> impacts from MTBE+impacted soils previously detected beneath the subject site Cambria used <br /> site specific data to calibrate the model Site specific parameters that are most sensitive to the <br /> model output include MTBE concentrations,area, depth to groundwater,fraction organic carbon, <br /> soil texture,and soil water content Published data were used for MTBE chemical parameters <br /> The VLEACH model was run using maximum soil MTBE concentrations that were detected in <br /> soil samples collected during August 1996 A fine-grained silt loam soil was used as the <br /> representative soil profile covering an estimated area of 176 feet2 The VLEACH model output <br /> predicts that the highest MTBE groundwater concentrations will occur after 1 year and <br /> concentrations will be reduced by over 50% after 10 years After 57 years, the model predicts <br /> that MTBE concentrations will fall below state and federal regulatory levels for drmkuig water <br /> These findings agree reasonably well with the actual groundwater analytical data collected from <br /> • well MW-1, located closest to the MTBE source, where the highest MTBE concentrations were ' at <br /> observed 2 to 3 years following soil sample collection The actual data also indicate that MTBE' 7 <br /> groundwater concentrations fell below regulatory Ievels in the first quarter 2004 or <br /> approximately 8 years following soil sample collection. These findings are significantly less <br /> than the predicted timeframe of 57 years because the initial conditions used in the model <br /> overestimate the actual MTBE mass between the depths of 9 and 14 fbg Consequently, the <br /> modeled MTBE concentrations require a longer period of time to leach from the soil profile and <br /> attenuate in groundwater The site characteristics and modeling results supporting this <br /> conclusion are discussed in detail below <br /> Site Characteristics <br /> Soil Types: Soils beneath the subject site are classified primarily as fine-grained soils (silt and <br /> clay) with lesser amounts of coarse-grained sediments (sands) to the total explored depth of 45 <br /> fbg Soil samples collected from well boring MW-1 were classified as sandy silt(AM)from the <br /> near surface to a depth of approximately 10 fbg The ML contained approximately 10% clay, <br /> 70% silt, and 20% fine sand Soils beneath 10 fbg and extending to a depth of approximately <br /> 23 S fbg contained approximately 25% clay, 65% silt, and 10% fine to medium sand and were <br /> classified as clayey silt (MH) Below the clayey silt layer, sandy silt and silty sands (SM) were <br /> . encountered to the total depth of 32 fbg r <br />