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First Quarter 2002 Monitoring and Sampling Report 2 <br /> 7-Eleven Inc Store No 17334,4501 North Pershing Avenue, Stockton,CA April 22,2002 <br />' on evaluations of site assessment and feasibility testing needs and access-related drilling conditions <br /> Results and specific assessment steps will be submitted under separate cover <br />' Geolo IH dro Bolo <br /> 9Y Y g 9Y <br /> 1 The relatively level site is located at an elevation of approximately 8 feet above mean sea level The site <br /> is underlain by Quaternary alluvial deposits assigned to the Modesto Formation (Fluor Daniel GTI, <br /> Additional Site Assessment Report, January 15, 1998) Materials encountered during previous drilling at <br /> the site generally consisted of clayey silt and sandy silt to approximately 24 feet below ground surface <br /> (bgs), followed by interbedded clayey silt and silty fine sand to maximum exploratory drilling depths <br />' ranging from 35 to 40 feet bgs <br /> The depth to groundwater in MW-9 has ranged from 30 feet bgs in 1990 to 20 feet bgs in 1996 Depth to <br />' groundwater for the current quarter ranged between 15 59 to 16 72 feet below grade Seasonal water <br /> table fluctuations average 2 to 3 feet Historically, groundwater flow direction at the subject site and <br /> adjacent facilities has been to the northeast <br /> Sensitive Receptors <br /> Previous reports on sensitive receptors indicate that there are no public supply wells within 4000 feet <br /> downgradient of the site The nearest crossgradient/upgradient water supply well is of unreported status <br />' and lies about 1,500 feet away Other wells within 2000 feet of the site are not in hydraulic communication <br /> with shallow groundwater at the site <br />' Groundwater Monitoring Data <br />' Before monitoring, the well caps were opened to allow the water in each well to stabilize to atmospheric <br /> pressure The DTW was measured to the nearest 0 01 foot from the top of the well casing using an <br /> interface probe, and the resulting data was used to prepare a potentiometric surface map (Attachment 1, <br />' Figure 2) Based on the potentiometric surface map, groundwater flow is toward the northeast at an <br /> approximate gradient of about 0 005 foot per foot, consistent with historic measurements Groundwater <br />' monitoring results for the quarter and historical monitoring results are presented in Tables 1 and 2, <br /> respectively (Attachment 2) Field data sheets are included in Attachment 3 <br /> I <br />' Monitoring Well Sampling and Analytical Results <br /> Quarterly groundwater samples were collected after purging at least 4 well-casing volumes of groundwater <br />' from each monitoring well, unless the well was purged dry The groundwater samples were collected <br /> using disposable bailers Groundwater samples were placed in analysis-specific containers with analysis- <br /> 17334Q21 QMR DOC <br /> 1 <br />