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								        									S  E  C  0  R
<br />			Smith Canal is located approximately 1,300 feet south of the site, and the Calaveras
<br />			River is located approximately 3,500 feet north of the site   Both of these surface water
<br />			bodies are channeled, flow generally to the southwest, and drain into the Stockton Deep
<br />			Water  Channel  (GRI,  Groundwater Monitoring  Well,  CPT,  and  Ozone  Microsparge
<br />			System Installation Report, May 9, 2003)
<br />			MONITORING AND SAMPLING
<br />			The current monitoring well network consists of 12 wells (MW-1 and MW-3 through MW-
<br />			13) that are sampled quarterly   Wells MW-1, MW-3 through MW-10, MW-12, and MW-
<br />			13 are screened in the shallow water-bearing zone, and well MW-11 is screened in the
<br />			intermediate water-bearing zone   Groundwater samples were collected by TRC from
<br />			each of the wells on November 11, 2005
<br />			The groundwater samples were submitted to Severn Trent Laboratories, Inc  (STL) for
<br />			analysis of gasoline range organics (GRO), BTEX, fuel oxygenates (MtBE, TBA, tertiary
<br />			amyl methyl ether (TAME], DIPE, ethyl tertiary butyl ether [EtBE], and ethanol), 1,2-DCA,
<br />			and ethylene dibromfde (EDB) by EPA Method 8260B  Groundwater samples from wells
<br />			MW-3 and MW-7 were additionally analyzed for acetone by EPA Method 82608   Due to
<br />			a laboratory oversight, the groundwater samples from wells MW-3 and MW-7 were not
<br />			analyzed for tertiary butyl formate and tertiary butyl  acetate by EPA Method 8260B
<br />			Results are discussed below and are summarized in TRC's Quarterly Monitoring Report,
<br />			October Through December 2005 dated December 27, 2005 (Attachment 1)
<br />			Groundwater  monitoring  and  sampling   activities  at  the  site  were  performed   in
<br />			conjunction with those performed by Blaine Tech Services (BTS) at the nearby Shell
<br />			Service Station,  located at 1267 Country Club Boulevard    During the November 11,
<br />			2005 coordinated sampling event, split samples were collected by TRC from Shell wells
<br />			S-1 through S-4, and TRC obtained permission to sample off-site Shell wells S-5 and S-
<br />			6   These samples were submitted to STL for analysis of GRO, BTEX, fuel oxygenates
<br />			(MtBE, TAME,  DIPE,  EtBE, TBA,  and ethanol),  1,2-DCA, and EDB by EPA Method
<br />			8260B
<br />			DISCUSSION
<br />			During the fourth quarter 2005, depth to groundwater ranged between 14 63 and 19 21
<br />			feet bgs, which was in range of historical levels    Historical groundwater depths have
<br />			been reported between 11 40 feet and 32 14 feet bgs  The direction of groundwater flow
<br />			was toward the north at a hydraulic gradient of 0 002 foot per foot (ft/ft), which is also
<br />			consistent with the north to northeast groundwater flow direction reported over previous
<br />			quarters
<br />			The highest concentrations of petroleum hydrocarbons have historically been detected in
<br />			on-site wells MW-3 and MW-7   Concentrations of GRO and benzene were reported at
<br />			site  maximum  concentrations  of  180,000  pg/L  (MW-7)  and  472   pg/L  (MW-3),
<br />			respectively,  during  2001,  concentrations within  these wells and  other on-site wells
<br />			MW-1,  MW-4,  and  MW-6  have  since declined  over time    Petroleum  hydrocarbon
<br />			concentrations have generally not been detected at or above laboratory MRLs in wells
<br />			MW-5,  and  MW-8  through  MW-10,  MW-12,  and  MW-13     Well  MW-11,  which  is
<br />   •      	screened in a deeper water-bearing zone beneath the site, has occasionally contained
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