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Mr.M. Scott Mansholt—CEMC <br /> First Quarter 2006 Groundwater Monitoring and Sampling Report April 18,2006 <br /> US Can-Welty Road Page 3 of 5 <br /> GROUNDWATER MONITORING AND SAMPLING <br /> MONITORING <br /> On February 14, 2006, depth to water(DTW)was measured in wells MW-3 through MW-5 and <br /> WFSMW-1 using a hydrocarbon/water interface probe. DTW in these wells ranged from 32.67 <br /> feet below top of casing(btoc)in MW-5 to 36.20 feet btoc in WFSMW-1. The approximate <br /> groundwater flow direction beneath the site is to the east at a calculated gradient of approximately <br /> 0.001 ft/ft. Cumulative DTW measurements, groundwater elevations, and product thickness are <br /> presented in Table 1. A map showing the potentiometric surface is presented on Figure 3. Field <br /> data sheets are included in Attachment A. <br /> SAMPLING <br /> Following DTW measurements,groundwater samples were collected from wells MW-3,MW-5, <br /> and WFSMW-1 on February 14,2006. Well MW-4 was purged dry using a low-flow <br /> submersible pump and was not sampled because there was insufficient groundwater recovery in <br /> the well for sample collection. Well MW-3 was purged of only one well casing volume of water <br /> because of slow recharge in the well. Well WFSMW-1 was purged of approximately four casing <br /> volumes. Well MW-5 was redeveloped and was purged of approximately 25 gallons or 12 casing <br /> volumes. The wells were purged using a low-flow submersible pump. In these wells,pH, <br /> specific conductance, dissolved oxygen,turbidity,and temperature water-quality parameters were <br /> recorded. After water-quality parameters stabilized(i.e., a minimum of three consecutive <br /> readings with values within 10 percent for each parameter), groundwater samples were collected. <br /> The TPHd with silica gel-cleanup result for the sample collected from MW-3 on February 14, <br /> 2006(22,000 gg/L)appeared anomalous and significantly higher than the TPHd result(1,500 <br /> gg/L). The laboratory noted that the normal reporting limit(50 gg/L) could not be obtained for <br /> the TPHd analysis with silica-gel cleanup because of sample matrix interference observed during <br /> extraction. The surrogate quality control did not meet quality control requirements for the TPHd <br /> with silica gel-cleanup analysis. PAH concentrations detected in the sample collected on <br /> February 14,2006 from MW-3 were four to eight times greater than historical results. Because of <br /> potential matrix effects due to sediments in the samples collected on February 14,2006, and the <br /> anomalous TPHd with silica gel-cleanup result,MW-3 was re-sampled on March 30,2006. No <br /> samples were collected from MW-1 and MW-2 due to the presence of SPO in these wells. Field <br /> data sheets are included as Attachment A. <br /> GROUNDWATER ANALYTICAL RESULTS <br /> Groundwater samples were collected on February 14 and March 30,2006. All samples were <br /> collected using a low-flow submersible pump using new polyethylene tubing through which <br /> groundwater was extracted. As discussed in the above paragraph,MW-3 was re-sampled on <br /> March 30,2006 and the samples where analyzed for TPHd and PAHs. Laboratory-provided <br /> bottles were used to preserve the samples. The bottles were labeled, sealed, and placed <br /> immediately into an ice-cooled chest for delivery to Lancaster Laboratories,Inc. (Lancaster), <br /> under SAIC chain-of-custody protocol. Lancaster is a California State-certified laboratory <br /> (ELAP#2116). <br /> The samples were analyzed for the following: <br /> • TPHd: CIO—C25,using U.S. Environmental Protection Agency(EPA)Method 8015M and <br /> TPHd with silica-gel preparation for samples with detectable concentrations of TPHd <br /> using EPA Method 8015M; <br /> • TPHg: C6—Clo,using EPA Method 8015M; <br />