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I Blaes Environmental Management Inc 3RD Qtr 2003 Groundwater Monitoring Report <br /> 002-70950-04 U-Haul#709-50 <br /> I <br /> S4.0 CONCLUSIONS <br /> Blaes Environmental conducted the groundwater monitoring and sampling event for the Third Quarter <br /> 2003 at U-Haul Facility #709-50 in Stockton, California on September 8 through 11, 2003 Average <br /> groundwater levels recorded in September 2003 were more than 10 feet lower than those recorded during <br /> the May 2003 monitoring event Groundwater was not encountered in the "A"horizon <br /> I Based on theoundwater level measurements from the middle "B" w ' <br /> gr ells and the Farmer Harry's Auto <br /> Mart monitoring wells, the groundwater surface map for September 2003 indicates a flow direction <br /> toward the southeast across the northern portion of the site and a flow direction radiating southwest to <br /> northwest from a high point centered near the southern part of the intersection of Wilson Way and <br /> Sangumetti Lane across the southern portion of the site <br /> Analytical results of groundwater samples collected in September 2003 from both "B" and "C" casing <br /> wells indicated the presence of hydrocarbons in groundwater beneath both the U-Haul Facility and the <br /> Former Harry's Auto Mart Facility Results of samples collected from the "B" casing wells revealed that <br /> the main portion of the U-Haul hydrocarbon plume is located around wells MW-2B, MW 3B, and MW- <br /> 4B The main portion of the Farmer Harry's Auto hydrocarbon plume is located beneath HA MW-1 <br /> I Results of samples collected from the "C" casing wells revealed higher hydrocarbon concentrations near <br /> wells MW-2C and MW-4C Based on the September 2003 analytical results, there appears to be limited <br /> communication between the "B" and "C" horizons The LNAPL such as TPH and BTEX, appears to be <br /> concentrated in the "B" horizon while the heavier DNAPL such as 1,2 DCA, has penetrated more <br /> extensively into the "C"horizon <br /> I <br /> I <br /> I <br /> 11 <br /> I <br />