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} <br /> 5.2 Depth to Groundwater _ <br /> The normal seasonal rise in the water table continued during the quarter (Table 1) A rise of <br />' approximately 4 feet took place, bringing the water to its highest level in more than 6 years <br /> 5.3 Groundwater Gradient,and Flow Direction <br /> As in most previous quarters, groundwater flow is east-southeastward, with a prominent trough <br /> beneath the Apache building (Figure 5) <br /> 5.4 Groundwater Contamination <br /> Despite the rise in the static water level, benzene and TPH-g concentrations in MW-5 have declined <br /> to their lowest levels in more than 2 years (Table 2) In fact, benzene was not detected for the first <br />' time However, low concentrations of benzene, toluene, and xylene were detected in MW-4 <br /> Previously, no contaminants had been detected in any samples from this well Hence, the laboratory <br /> result is probably in error, and may be due to improper cleaning of lab equipment after a previous <br />' sample <br /> As expected, gasoline and BTEX were detected at moderate concentrations in VE-1 "deep" <br />' Concentrations have risen since this well was sampled in May 1996, and are about the same as <br /> when this well was sampled in February 1996 <br /> 5.0 CONCLUSIONS <br /> ' Based on long-term trends m the concentration of hydrocarbon vapors being withdrawn from the <br /> extraction wells, it is clear that the vapor extraction system has been successful in lowering the <br /> concentration of gasoline liquids in the soil Quantitative laboratory data indicate that <br /> concentrations in the shallow well vapor stream have declined from a high of 4,800 ppmv in <br /> November 1994 to a few hundred ppmv at the present time, and field measurements show a similar <br /> ' decline Fewer laboratory data are available for the deep zone, but concentrations decreased from <br /> 22,600 ppmv in November 1994 to 5,290 ppmv in September 1995, a reduction of more than 75% <br /> PID data show a steep decline in concentrations from December '1994 to July 1995, but at least <br /> ' some of this decline is due to a rise in the water table, reducing the air flow through the deep zone <br /> It is also apparent from Figures 3 and 4 that PID readings on field samples usually exceed the <br /> ' laboratory results of tedlar bag samples The disparity is probably attributable to the differences in <br /> equipment <br /> ' The total volume of vapor that has been extracted since July of 1994 is approximately 62,000,000, <br /> cubic feet The calculated weight of extracted hydrocarbons exceeded 15,000 pounds as of <br /> December 1996, which is roughly equivalent to 2,300 gallons of gasoline <br /> 6 <br />