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Ms Mary Meays Page 3 <br /> January 14, 1993 <br /> trough situated along the southern portion of the site In the afternoon, <br /> water level measurements were elevated in the wells by up to 133 feet and <br /> the potentiometric surface formed a trough centered at MW-5 and oriented <br /> towards the southeast These result are consistent with those obtained during <br /> the previous recent quarters of monitoring <br /> The variability in flow direction and water elevation are probably due to the <br /> influence of tidally induced water level changes in the adjacent Stockton deep <br /> water channel Tidal data for the Stockton area are provided in Table 4 The <br /> difference in water elevations observed between the morning and afternoon <br /> coincide with the fact that the tide was higher when the afternoon <br /> measurements were obtained <br /> The laboratory findings (Table 2) indicate a continued slight decrease in the <br /> concentration of TPH-G and related petroleum compounds at MW-5 The <br /> measured TPH-G concentrations were historically the lowest level observed <br /> (1 8 mg/1) during quarterly monitoring activities BTEX concentrations were <br /> also lower than observed during any previous quarters of monitoring Thus, <br /> a decreasing trend in the concentrations of TPH-G and BTEX compounds has <br /> been established It is likely that the diminished concentrations are a result of <br /> natural microbial degradation of compounds <br /> � MW-4 showed no detectable quantities of TPH-G and BTEX During previous <br /> quarters, TPH-G and BTEX have been oberved at very low concentrations <br /> There have also been quarters in which these compounds were not observed <br /> Thus, it is probable that MW-4 is situated on the margin of the area affected by <br /> gasoline from the UST It is also likely that the diminished concentrations <br /> are a result of natural microbial degradation of compounds <br /> Wells MW-1, MW-2, and MW-3 showed no detectable quantities of TPH-G <br /> and petroleum compounds The absence of TPH-G and related compounds in <br /> these wells is consistent with the results from previous quarterly <br /> investigations <br /> Former Tank Site #2 <br /> Potentiometric surface contours are for Former Tank Site #2 are depicted in <br /> Figures 3 and 4 The contours shown for the measurements taken in both the <br /> morning and afternoon indicate a general southwest gradient In the <br /> afternoon, water level measurements were elevated in wells by up to Q 74 <br /> feet These result are consistent with those obtained during the previous <br /> recent quarters of monitoring <br /> As previously discussed, the variability in water elevation is probably due to <br /> the influence of tidally induced water level changes in the adjacent Stockton <br />