Laserfiche WebLink
}�, <br /> L A letter from the Sane Joaquin County Public Health Services - Environmental Health <br /> Division (PHS/EHD) dated March 7, 1994, stated that ",the former underground storage <br /> tank(s) cannot be recommended for final closure without further investigation to determine <br /> the full.extent of the soil and/or groundwater problem." In response to the letter from the <br /> PHS/EHD, GeoAudit was retained to assess soil and groundwater conditions at the site. <br /> 2.3 Initial Investigation <br /> I <br /> On April 27 and 28, 1994, eight soil borings were drilled �at they site. Three of the borings <br /> were completed as 2-inch groundwater monitoring wells. Soil samples were collected at five- <br /> foot intervals during drilling. A total of fourteen soil sampies were submitted to a state- <br /> certified laboratory for analysis. Total petroleum hydro4rbons (TPH as gasoline) were <br /> detected in ten samples at concentrations as great as 3,8001ppm (134-20); TPH as diesel was <br /> detected in twelve samples at concentrations as great as 9,000 pphi'(138-20). During drilling, <br /> L <br /> groundwater was encountered at a depth of approximately 20 feet.- <br /> i ; <br /> After installation, groundwater depth was measured and samples were collected from each <br /> L well. The hydraulic gradient was calculated to be 0.0006 Ift/ft, directed S 40° W. TPH as <br /> gasoline was detected in MW1, MW2 and MW3 at concentrations of 1,700 µg/L (ppb), <br /> 14,000 ppb and 2,600 ppb, respectively; TPH as diesel was detected in MW1, MW2 and <br /> MW3 at concentrations of 2,400 ppb, 9,200 ppb and 6,9aD0 ppb, respectively. Analytical <br /> results of all groundwater samples are included in Table �. <br /> y <br /> 3.0 PROCEDURES � 1 <br /> L 3.1 Monitoring Well Purge Procedures <br /> .I <br /> On August 5, 1994, groundwater monitoring procedures were performed at the referenced <br /> site. The depth to groundwater was measured in each well relati,a to the top of the casing <br /> using a Solinst water level meter (Table 1). The relative groundwater elevations and <br /> hydraulic gradient were calculated from these data. <br /> After water levels were measured, a 2-stage purge pump .I as used to purge each well of <br /> approximately 7 gallons of water to stabilize temperature, pH, and conductivity (Appendix <br /> A). Measurements were obtained using an ICM Water Analyzer1V1ode1 #52200. The purge <br /> water was stored on-site in 55-gallon DOT-approved drums.I.After,purging each well, a water <br /> sample was collected from each well using a new disposable plastic bailer. The samples were <br /> collected in 40-m1 EPA vials and Niter amber bottles. <br /> 1 <br /> Rip"P- <br /> r k �_QRS/A.91/92i-5 'i <br /> i ,3 <br />