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IT Corporation <br /> 100,3 lint Chicago lliriir�,r� <br /> Cfmrord. (A 01520-112r) <br /> . Tel, 1)2-i.288.118'18 <br /> f-dx. 925.288.C1888 <br /> the <br /> (Wpigroup- <br /> 1 1f,-rnbr r..f The IT l:r,rrrp <br /> January 6, 2000 <br /> Mr. Bob DeNinno <br /> 7-Eleven, Inc. <br /> 10220 SW Greenburg Road, Suite 470 <br /> Portland, Oregon 97223 <br /> ' Subject, Fourth Quarter 1999 Monitor and Sampling Report <br /> 7-Eleven Store No. 14117 <br /> ' 2725 Country Club Boulevard <br /> Stockton, California <br /> IT Project No. 779966 <br /> ' Dear Mr. DeNinno: <br /> This Fourth Quarter 1999 Monitoring and Sampling Report presents the results of activities performed by <br /> the IT Corporation at the subject site (Figure 1, Attachment 1) on November 24, 1999. A summary of <br /> activities conducted during this reporting period is provided below. <br /> Depth to water (DTW) was gauged in four site-related groundwater monitoring wells (MW-1 <br /> through MW-4). <br /> Groundwater samples were collected from the groundwater monitoring wells and submitted to <br /> a California-certified laboratory for analysis for benzene, toluene, ethylbenzene and xylenes <br /> (BTEX), total petroleum hydrocarbons-as-gasoline (TPH-G), and the oxygenates, methyl-tert- <br /> butyl-ether (MTBF), tert-butanol (TBA), diisopropyl ether (DIPE), ethyl-tert-butyl ether (ETRE), <br /> and tert--amylmethyl ether (TAME). <br /> Groundwater Monitoring Data <br /> Groundwater monitoring was performed on November 24, 1999. Before monitoring, the well caps were <br /> ' opened to allow the water in each well to stabilize to atmospheric pressure. The DTW was measured to <br /> the nearest 0.01 foot from the top of the well casing using an interface probe. <br /> ' Monitoring results from the November 24. 1999 monitoring and sampling event are presented in Table i A <br /> j potentiometric surface map was generated using top of casing elevations and DTW data collected on <br /> November 24. 1999 (Figure 2). Based on the monitoring data. the estimated groundwater flow is <br /> ' dominantly toward the south at a gradient 0 02 foot per foot Field data sheets are included in <br /> Attachment 3 <br />