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� 1 >I <br /> Ms Vicky McCartney <br /> May 23, 2005 <br /> Page 3 of 6 <br /> • <br /> Semi-Annual Groundwater Sampling Event <br /> On March 31, 2005 monitoring wells MW 1 through MW3 were monitored and sampled <br /> Groundwater elevations were calculated by measuring the depth to groundwater in each well and <br /> subtracting from the respective wellhead elevation Groundwater elevations at the site rose an <br /> average of 4 17 feet since last monitored on July 12, 2004 The average hydraulic gradient across <br /> the site was approximately 0 01 ft/ft (50 feet per mile) Groundwater flowed in a northeasterly <br /> direction A potentiometric surface map is depicted on Figure 3 Groundwater monitoring data <br /> are summarized in Table 1 Monitoring data sheets are included in Attachment C <br /> Prior to sampling, monitoring wells MW 1 through MW3 were purged of a minimum of three <br /> well casing volumes During the purging process, temperature, pH and electrical conductivity <br /> parameters were measured Samples were collected after parameter stabilization, and 100% <br /> water level recovery Groundwater samples were delivered under chain of custody protocol to <br /> Argon Laboratories (ELAP #2359) for analysis of TPHg, BTEX, and gasoline oxygenate <br /> additives including 1,2-DCA Purge water was contained in a properly labeled DOT-approved <br /> 55-gallon drum The drum is currently being stored onsite Purge logs are included in <br /> Attachment C o <br /> RESULTS OF INVESTIGATION - <br /> 5 <br /> Subsurface Conditions _ Z, <br /> �J <br /> Soils encountered in the borings consisted primarily of silt and clay Two sand zones were also <br /> identified, one in the unsaturated zone and the second in the saturated zone The shallower sando <br /> was encountered in borings SBA, SBB and SBG This silty sand interval is approximately 5-10 <br /> feet thick and terminates at a depth between approximately 20-30 feet The deeper silty sand was <br /> present between the depths of approximately 43-48 feet in borings SBA and SBB and from <br /> approximately 48 feet to total depth of 52 feet in boring SBF Groundwater was encountered in <br /> the deeper sand <br /> No hydrocarbon odors or elevated PID readings were observed in soil borings SBB, SBC, SBD, <br /> SBE, SBF, and SBG In boring SBA, located down gradient of the former UST, slightly elevated <br /> PID readings were recorded from the 45 (35 3 parts per million [ppm]) and 50 (38 6 ppm) foot <br /> samples Hydrocarbon odors were not observed in soil samples collected in boring SBA <br /> Groundwater-saturated soils were first noted in the borings at depths between approximately 45 <br /> and 50 feet Water levels rose in the temporary well casings to depths between 33 feet and 41 <br /> feet bgs In borings SBC and SBD saturated soils were encountered at 5 feet bgs as a result of <br /> heavy precipitation Boring logs describing the hthology are included in Attachment B <br /> G\GROUNDZE\W E\SAR\2005\1SAR05bonngreportdoe <br />