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phase If 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 (TK1) located north of the building. A <br /> black viscous fluid was present on the stick used to check the contents of TK1. The dimensions of TK1 <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 two USTs, 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 TK1 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 .lnvestigation 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 /> (TK1) 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 Alan 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 /> o CONDOR <br />