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Appendix A - Historical Background <br /> PACIFIC MINI-MART <br /> 4511 Pacific Avenue, Stockton, California <br />' installation of the additional ground water monitoring wells <br /> A vapor extraction test was conducted in December 1993 Since that time, ground water has risen <br /> from approximately 55 feet bsg to as high as 30 feet bsg,reducing the vertical extent of the vadose <br /> zone open to the screened interval of the vapor extraction well The rise of ground water elevation <br /> has also eliminated most of the coarse-grained soil from the vadose zone, leaving predominantly <br /> fine-grained soil in contact with the reduced open screened interval of the vapor extraction well <br /> These changes can potentially drastically reduce the zone of influence of the vapor extraction well(s) <br />' and reduce the concentrations of hydrocarbon vapor recovered by the extraction process <br /> On 29 and 30 April and 01 May 1998, seven probe borings (B 13 through B 19) were advanced off- <br /> site of the subject property to collect soil and grab ground water samples as part of on-going <br /> assessment of the release of fuel hydrocarbons from the former UST facility TPH-g, TPH-d and <br /> BTEX were not detected in any of the soil samples analyzed,however, MTBE was detected at 180 <br /> micrograms per kilogram (pg/kg) in the soil sample from boring B16 at a depth of 40 feet bsg <br /> TPH-g was not detected in any of the grab water samples collected,but TPH-d was detected in seven <br /> of the eight grab water samples at concentrations as high as 1,200 µg/l Various BTEX compounds <br /> iwere detected in the grab water samples from borings B13, B14 and B17 at concentrations as high <br /> as 1 4 micrograms per liter (µg/l), benzene was detected only in the sample collected from boring <br /> B 13 at a depth of 60 feet bsg, at a concentration of 0 61 µg/l In addition, MTBE was detected in <br /> seven of the eight grab ground water samples collected at a maximum concentration of 1,400 µg/l <br /> in sample B 16-H20 TBA was detected in sample B 13-H2OB at a concentration of 16 dig/l <br /> On 20 March 2001, ground water extraction well EW-1 was installed at the site for performance of <br /> a ground water pumping test At the regulatory directive of the EHD a twelve-hour aquifer pump test <br /> was performed on 27 March 2001 to assess the general ground water aquifer characteristics and to <br /> assess aquifer response to ground water extraction at a constant pumping rate utilizing well EW-1 <br /> for ground water extraction and wells MW-1, MW-2, MW-4, MW-5 and MW-6 and vapor well <br /> VW-I as observation wells Three ground water samples were collected from the extracted ground <br /> water and purged ground water was containerized in an on-site 6,500-gallon poly tank The <br /> implications from the March 2001 aquifer ground water pumping test are <br /> • Ground water draw-down of at least 11 15 feet was observed in extraction well EW-1 <br /> following 700 minutes of continuous pumping (5 GPM), ground water draw-down was <br /> observed in well MW-5 (located 15 feet to the east ) at I 1 feet,well MW-4 (located 60 feet <br /> toward the southeast) at 0 1 feet, well MW-6 (located 50 feet toward the north-northwest) <br /> at 0 12 feet and in well vapor well VW-1 (located 60 feet toward the west) at 0 06 feet <br /> • Utilizing a semi-logarithmic plot of ground water draw-down vs observation well distance <br /> • to pumping well, a best-fit line can be utilized to project a radius of influence of <br /> approximately 65 feet at 5 GPM Utilizing the Distance-Drawdown Method,a transmissivity <br /> Advanced GeoEnvironmental,Inc <br />