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Mase II Environmental Site Assessment <br />Heritage Square <br />Page 2 <br />underground storage tank (UST, TK2) located east of the Women's Center of San Joaquin County <br />(Women's Center) building. This structure is adjacent to the Heritage Square building. TK2 is situated <br />south of the back entrance stairs to the Women's Center and is located entirely within the parcel owned <br />by the Women's Center. The backhoe was used to expose the top of TK2, which measured three feet wide <br />by ten feet long and is approximately 500 gallons in volume. A shovel handle was lowered inside TK2, <br />and the contents appeared to be a diesel -type of fuel and not a black viscous fluid. <br />Cruz Brothers locating service was used to trace the fuel lines north of the geotechnical borehole to inside <br />the Heritage Square building and back outside to a second UST (TKI) located north of the building. A <br />black viscous fluid was present on the stick used to check the contents of TKI. The dimensions of TKI <br />were not investigated at this time The fuel lines were also traced to an old natural gas-fired boiler located <br />inside the Heritage Square building. <br />On May 22 and 23, 2002, Condor collected one soil sample from beneath TK2 located on the east side of <br />the building and eight soil samples from beneath the fuel lines outside of the building. The samples were <br />analyzed for total lead, kerosene, diesel, and motor oil, and for the same volatile hydrocarbons as the <br />sample collected at the time of the geotechnical borehole advancement. The sample from beneath the tank <br />was also analyzed for semi -volatile hydrocarbons by EPA Method 8270D. The laboratory analyses of the <br />soil sample from beneath the tank detected diesel at a concentration of 3,800 milligrams per kilogram <br />(mg/kg). Volatile hydrocarbons were detected at concentrations similar to those detected in the soil <br />sample collected at the time of the geotechnical borehole advancement. Total lead was detected in each <br />soil sample collected from beneath the piping and TK2 at concentrations below the PRG for residential <br />sites and the TTLC. Based on the results from the laboratory analysis, the viscosity of the product present <br />in the pipe, the proximity of the underground piping to both an existing boiler and twoUSTs, and the <br />apparent age of the boiler, Condor suspected that the former tanks stored bunker or diesel type <br />hydrocarbon fuel. Visual inspection of the contents of TKI confirmed that the UST stored World War II - <br />era bunker oil, a motor oil -like heavy hydrocarbon. Additional information regarding the backhoe work, <br />the investigation and removal of the underground piping, and the soil sampling procedures and analytical <br />results for the piping trenches is available in the "Underground Pipe Investigation and Removal Report," <br />dated June 24, 2002, and prepared by Condor. <br />During the course of performing fieldwork at the site, Condor located an abandoned water well on the <br />east side of the Heritage Square building (Figure 3). A sensitive receptor survey performed by Condor for <br />an adjacent site did not identify any existing state or county records for the well, and the construction <br />details of the well are not known. <br />Condor was retained by David and Marianne Warwick in cooperation with SUSD to further investigate <br />the site for potential subsurface hydrocarbon contamination in association with the one on-site UST <br />(TKI) and the one off-site UST (TK2) in close proximity to the site that were previously unidentified. <br />Condor submitted a Work Plan dated June 5, 2002 to the San Joaquin County Environmental Health <br />Department (EHD) outlining our proposed work for the site. Ms. MargaretLagorio of EHD gave a verbal <br />approval of the Work Plan on June 7, 2002 <br />3.0 LOCAL GEOLOGY <br />The local geology underlying the subject site consists primarily of medium to stiff tight clay with lenses <br />of sandy to silty clay. The sandy to silty clays become more prominent with depth, but individual layers <br />are characterized by limited horizontal extent. According to published geologic maps, surface deposits <br />underlying the site consist of eolian sands belonging to the upper member of the Modesto Formation. <br />CONDOR <br />