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I <br /> 1 <br /> Mr Nuel Henderson <br /> Page 5 of 9 <br /> Groundwater Sampling <br /> ' Water Ievels in new wells MW1313, MW15A through MW15C, MW16A and MW16B were <br /> monitored on January 30, 2003 Water level data are summarized in Table 2 <br /> 1 The new wells were purged and sampled on January 30 and 31, 2003 Prior to sampling, at least <br /> three well casing volumes of groundwater were purged from each new well During the purging <br /> ' process temperature, pH, and electrical conductivity parameters were measured Purging <br /> continued until these parameters had stabilized Groundwater samples were collected from each <br /> well subsequent to parameter stabilization and a minimum of 80% recovery to pre-purge levels <br /> ' using a disposable bailer The samples were transferred to the appropriate containers, sealed, <br /> labeled, and immediately placed in an ice chest cooled to a temperature of approximately 40C <br /> The samples were transported to Argon under chain of custody protocol for the analysis of TPHg, <br /> ' BTEX, gasoline oxygenates, EDB and 1,2 DCA using the appropriate EPA methods <br /> ' RESULTS <br /> Soil Lithology <br /> '• Well MW13 was deepened and renamed MW13B Soil logging was initiated at a depth of 75 <br /> feet bgs At intervals of 75-76 5180 feet bgs and 76 5/80-815 feet bgs, soil in well MW13B was <br /> ' identified as silty clay and well-graded sand with clay,respectively <br /> Except for two sand beds identified at 415/45 feet bgs to 46 5150 feet bgs ("A Sand"), and 60 <br /> ' feet bgs to 75 feet bgs ("B Sand"), silts and clays were the predominant soil types classified in <br /> wells MW16A and MW16B <br /> ' In well MW15A, a poorly-graded sand with clay was identified from 36 5140 — 46 5150 feet bgs <br /> This is believed to correlate to the A Sand in the wells further west The B Sand was logged in <br /> well MW 1513 between the depths of 60 feet and total depth of 81 5 feet The mud-rotary drill <br /> ' cuttings returned in well MW15C indicated the B Sand to be present between approximately 60 <br /> and 78 feet The A Sand was not noted to be present in this well Beneath the B Sand in well <br /> MW15, fine-grained materials were present to total depth of 121 feet except for two very thin <br /> ' sand beds a four-inch thick sand stringer at a depth of 106 feet and a one-foot thick clayey sand <br /> at 118-119 feet <br /> ' Boring logs for the new wells are included in Attachment A <br /> ' 11GZA_FSIVOL_MATA1GROUNDZE1ROEKICLOSURE"Repwfts\Add_HSA Mud wells doc <br /> I <br />