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IT Corporation <br /> 757 Arnold Drive, Suite D <br /> Martinez, CA 94553-6526 <br /> lot Tf-1 925 370 3990 <br /> 1W 'i <br /> ^ 'i Fax 925 370 3991 <br />' <br /> Vrxarqoup A Member of The IT Group <br /> AL <br /> yr <br /> Mr Bob DeNinno <br /> The Southland Corporation <br /> 10220 S W Greenburg Road, Suite 470 <br /> Portland OR 97233 <br /> Subject First Quarter 1999 Monitoring and Sampling Report <br /> Former Southland Store No,20632 <br /> 4627 DaVnci Drive <br />' Stockton, California <br /> IT Corporation Project 102483 <br />' Dear Mr DeNinno <br /> This First Quarter 1999 Monitoring and Sampling Report presents the results of monitoring and sampling <br />' activities performed by IT Corporation, Inc (Fluor Daniel GTI) at the subject site (Figures 1 and 2. <br /> Attachment 1) on February 17, 1999 A summary of activities conducted during this reporting period is <br /> provided below <br /> Depth to water DT was gauged in four site-related groundwater monitoring wells MW-1 <br /> DeP ( tM 9 g 9 g . ( , <br /> MW-2, MW-3 and MW-5) <br />' ■ Groundwater samples were collected from the four monitoring wells and submitted to a <br /> California-certified laboratory for analysis of benzene,toluene, ethylbenzene, and total xylenes <br />' (BTEX), total petroleum hydrocarbons-as-gasoline (TPH-G), and the oxygenates methyl-tert- <br /> butyl-ether(MTBE),tert-butanol (TBA), diisopropyl ether(DIPS),ethyl-tert-butyl ether(ETBE), <br /> and tert-amyl-methyl ether{TAME) <br /> ' Groundwater Monitoring Data <br /> Groundwater monitoring of the four wells was performed on February 17, 1999 Before monitoring,the <br /> well caps were opened to allow the water in each well to stabilize to atmospheric pressure The DTW <br /> ' was measured to the nearest 0 01 foot from the top of the well casing using an ORS environmental <br /> Equipment INTERFACE PROBE TM Well Monitoring System <br /> A potentiometric surface map was prepared using the groundwater elevation data collected on February <br /> 17, 1999 (Figure 2) Based on the groundwater elevation data, groundwater flow is toward the south at a <br /> gradient of 0 002 ft/ft The groundwater monitoring results from the February 17, 1999 monitoring and <br />