Laserfiche WebLink
into the slotted PVC tube. Groundwater was brought to the surface within the Teflon tube by <br /> moving the Teflon tube up and down in a piston-like motion. <br /> A second boring (B4-2) was drilled to a total depth of 18.0 feet bgs and was located <br /> approximately 10 feet away from the southern edge of the former tank (Figure 2). Soil <br /> samples were collected at depths of 12 and 17 feet for laboratory analysis. Samples were <br /> collected using a 2-foot long, 1-inch diameter, Large-Bore Soil Sampler equipped with a clear <br /> acetate plastic liner. A groundwater sample was collected after the boring had been advanced <br /> to the total depth of 18 feet bgs using the method described above. Based on the lack of field <br /> evidence of PHC-impacted soil or groundwater, Margaret Lagorio and Carol Oz of PHS/EHD <br /> decided that the third boring planned for the site was unnecessary and provided verbal <br /> authorization to complete the investigation with two borings. Both borings were subsequently <br /> grouted to the surface with neat cement per PHS/EHD guidelines. " <br /> Soil and groundwater samples were placed in an ice-cooled chest and submitted under chain-of- <br /> custody procedures to BSK Analytical Laboratories (BSK), a California DHS-certified r <br /> laboratory for PHC analyses. Samples were analyzed for BTEX, TPHg, and MTBE using <br /> EPA Methods 8020/8015. The Work Plan stated that EPA Method 200.8 would be used for -- <br /> analysis of lead in soil and water samples. This method uses inductively coupled plasma and <br /> mass spectrometry (ICP/MS) as the analytical technique and is typically used on low turbidity <br /> drinking water samples. However, due to the high turbidity in water samples collected during <br /> this investigation, BSK performed lead analyses for water samples using EPA Method 200.7. <br /> Soil samples were analyzed using EPA Method 6010. Both these methods use ICP as the <br /> analytical technique. According to BSK, these ICP methods provide the same detection limits <br /> as the ICP/MS method while offering the advantage of being able to accommodate analysis of <br /> turbid water samples. This change in analytical method for lead analysis was conveyed to -- <br /> Carol Oz. <br /> 4.0 INVESTIGATION FINDINGS <br /> Findings of the investigation, including geologic and hydrologic characteristics, and analytical <br /> results of the soil and groundwater samples, are discussed in the following sections. <br /> 4 <br /> 98I MWVRPTS1s4USTINV.RPT <br />