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22 August 2000 <br /> . AGE-NC Project No 99-0592 <br /> Page 2 of 4 <br /> 2 2 COLLECTION AND ANALYSIS OF GROUND WATER SAMPLES <br />' A water sample was collected from monitoring well MW-1 using a new disposable bailer after <br /> P <br /> allowing the well to achieve a minimum 80%recovery of the pre-purge water volume Additionally, <br />' a water sample was collected from domestic well DW-I after the well purge valve was opened and <br /> water was allowed to run for more than 30 minutes, allowing the pump to turn on The samples were <br /> transferred into laboratory-supplied 40-ml,EPA-approved VOA vials containing 0 5 ml 18% <br />' hydrochloric acid as a sample preservative The sample vials were then labeled with the monitoring <br /> well or domestic well designation, date, time of sampling and the sampler's Initials The samples <br />' were transported In a chilled container under chain of custody to McCampbell Analytical, Inc <br /> (MAI),a California Department ofHealth Services(DHS)-certified analytical laboratory for analysis <br /> The samples were analyzed for <br />' 0 Total petroleum hydrocarbons quantified 'as gasoline (TPH-g) In accordance with EPA <br /> Method 5030/8015-Modified, <br />' 0 Volatile aromatic compounds, Including benzene, toluene, ethylbenzene, and total xylenes <br /> (BTEX)with methyl tertiary butyl ether(MTBE)in accordance with EPA Method 8020,and <br />' • 0 Fuel oxygenates,Including tertiary butanol(TBA),di-isopropyl ether(DIPE),ethyl tert-butyl <br /> ether(ETBE),tert-amyl methyl ether(TAME),and MTBE In accordance with EPA Method <br /> 8260M <br /> I <br />' 30 FINDINGS <br /> Hydrocarbon-Impact to ground water was Inferred from laboratory analysis and field observations <br /> Ground water elevation was determined by subtracting the measured depth-to-water from the <br /> surveyed casing elevation <br /> I3 1 GROUND WATER ELEVATION AND GRADIENT <br />' Ground water elevation decreased 2 22 feet to 55 18 feet below the top of the well casing In MW-1 Lt`1 <br /> since the 15 February 2000 monitoring event Ground water elevation data are presented on Table <br /> 1 Monitoring data from MW-1 was combined with monitoring well data from an adjacent site to <br /> I determine the ground water flow direction Ground water flow direction was Inferred to be <br /> northwesterly with a gradient of 0 005 ft/ft The flow direction has significantly changed compared <br /> to previous monitonng events The flow direction has rotated approximately 100 degrees to the west <br /> Figure 4 - Ground Water Elevation depicts the contours for June 2000 The gradient map was <br /> expanded to Include data from monitoring wells,located at 3535 East Cherokee Road <br />' Advanced GeoEnvironrnental,Inc <br />