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T&T Trucking <br /> Subsurface Investigation Results and Site Conceptual Model <br />' No 4_g <br /> 4 2 2 Groundwater Quality <br />' Regionally, the majority of the groundwater in the Eastern San Joaquin basin is characterized by <br /> calcium-magnesium bicarbonate or calcium-sodium bicarbonate types Total dissolved solids <br />' (TDS) range from 30 to 1,632 milligrams per liter (mg/L) and averages about 310 mg/L The <br /> average specific conductance of groundwater ranges within the Eastern San Joaquin basin is 685 <br /> micro-mohs per centimeter (µmhos/cm) Elevated saline groundwater has been intruding from <br /> the Delta eastward toward Stockton Nitrate concentrations are also elevated in areas southeast of <br /> Lodi and Stockton as wells as other County areas (DWR, 2003) General chemistry of the site <br /> groundwater has not been characterized, however, electrical conductance measurements collected <br /> during quarterly purging events range from 800 to 1300 and average approximately 1,000 <br /> µmhos/cm which is consistent with the DWR data for the region <br /> ' 4 2 3 Water Levels <br /> ' Water levels have been measured on a quarterly basis from January 2000 to the present Depth to <br /> groundwater beneath the Site currently ranges from seventy to 71-£t bgs A hydrograph of the <br /> water level elevations for all the wells from August 1998 to December 2003 are presented in <br /> ' Figure 4-4 As shown on Figure 4-4,water levels in all four monitoring wells behave similarly <br /> during the annual hydrologic cycle The highest groundwater levels generally occur during the <br /> spring,responding to precipitation The lowest groundwater levels occur during the fall and early <br /> winter The correlation of water levels between wells indicates a continuous water table condition <br /> and wells are screened across the same water table <br /> ' As shown on Figure 4-4 groundwater levels appear to be decreasing over time This trend is <br /> consistent with regional water levels due to increased groundwater pumping for irrigation and <br /> ' potable water supply <br /> Overall, the hydraulic gradient is primarily flat with periods of very shallow gradients and flow <br /> directions to almost every compass direction The hydraulic gradient across the Site ranges from <br /> ' flat to 0 005-ft/ft to the south-southwest, and there have been two sampling events where a <br /> groundwater divide was calculated (September 1998 and January 2000) with the steeper gradients <br /> occurring during the wetter months <br /> 43 Nature and Extent of Petroleum Hydrocarbons in Soil and Groundwater <br /> This section provides a description and summary of individual constituents of concern detected in <br /> ' CPT HydropunchO samples Constituents include BTEX,TPH-g,TPH-d, and volatile organic <br /> compounds (VOCs) for the fuel oxygenates MtBE, Di-Isopropyl ether (DIPE), ethyl-t-butyl-ether <br /> (ETBE), tert-amyl-methyl-ether (TAME), and tert-butanol Analytical results for CPT <br /> ' groundwater samples are presented in Table 3-2 <br /> • <br /> P\23006\23954 i'1 tru6Ang\C11'1 Summary Report\F[NAI 7&T 1 rucking DOC <br />