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that the high concentration at 65 feet was not due to simple vertical migration Perhaps it is due to <br /> lateral migration within groundwater, or to lateral nugration along the top of the Riverbank hardpan <br /> followed by a"spillover" effect north of the termination of the hardpan Lateral contaminant migration <br /> is examined further in the next section <br /> 5.4 Lateral Extent of Soil Contamination <br /> Figure 10 vividly illustrates that the margins of the diesel plume are nearly vertical within the silt bed <br /> above the Modesto channel, but below 35 feet the plume spreads out very abruptly within the upper <br /> part of the channel This lateral spreading with depth is best seen in a series of isocon maps at various <br /> depths (Figures 11-15) <br /> Figure 11 shows the extent of diesel contamination at a depth of 35 feet, dust below the base of the <br /> excavation At this depth, the shape of the plume bears no relation to the geometry of the Modesto <br /> channel A high concentration was detected in GT-1, and although the sample at 35 feet in GT4 was <br /> not analyzed, a concentration near 8,000 mg/kg is estimated to have been present, based on a PID <br /> reading of 200 ppm and the concentration of 14,600 mg/kg at 40 feet The concentrations reported by <br /> SEMCO in three samples at the base of the excavation are lower than expected, but have been <br /> incorporated into Figure 11 for completeness <br /> The extent of diesel contamination at 45 feet, in the lower part of the Modesto channel, is depicted in <br /> Figure 12 The areal extent of contamination is considerably greater than at 3 5 feet, and the plume has <br />. become slightly elongated in a northeast-southwest direction <br /> With increasing depth, the diesel plume begins to narrow in a north-south direction and lengthen in an <br /> east-west direction, with the long axis subparallel to the axis of the Modesto channel At 50 feet, <br /> concentrations in excess of 20,000 mg/kg may be present along the was of the channel (Figure 13) <br /> i <br /> In contrast, gasoline concentrations between 45 and 50 feet define a plume that resembles the diesel <br /> plume at 35 feet (Figure 14) This probably indicates that a smaller volume of gasoline was released, <br /> and therefore the gasoline plume did not become ponded along the axis of the Modesto channel <br /> The diesel plume reaches its maximum elongation at a depth of 55 feet (Figures 10 and 15) At this <br /> depth, the contamination is contained in either the basal silt bed of the Modesto Formation or in the <br /> silty to clayey sand of the uppermost Riverbank Formation <br /> 5.5 Volume of Contaminated Soil <br /> Figures 11-15 can be used to estimate the volume of contaminated soil and other parameters The <br /> volume is calculated by summing the volume at successive depth intervals Due to the irregular shape <br /> of the plume,the area enclosed by the zero line on each map has been divided into smaller squares, and <br /> then the area of each square has been multiplied by the thickness of the interval to obtain the volume <br /> 13 <br />