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San Joaquin County - Public Works <br />1810 E. Hazelton Avenue, Stockton, CA <br />Site Background through February 2017 <br />Page 2 of 5 <br />On May 20, 2005, Ramage Environmental published Well Installation and Groundwater Monitoring <br />Report, which documented the installation of one additional groundwater monitoring well (MW-7) and <br />two remedial feasibility test wells (SVE-1A/B/C and AS-1/SVE-2B). <br />Ramage Environmental continued to conduct quarterly groundwater sampling and publishing <br />groundwater monitoring reports through the second quarter of 2010. <br />All measurements and data dated prior to June 2010 were provided by Ramage Environmental. Condor <br />Earth Technologies, Inc. (Condor) is not responsible for the accuracy and completeness of information <br />collected and developed by others. <br />On April 29, 2011, Condor collected field inspection samples, groundwater parameters, and groundwater <br />samples from MW-1 through MW-7 for the second quarter 2011 semi-annual groundwater monitoring <br />event. Between May 14, 2010, and April 29, 2011, the groundwater surface in the seven monitoring wells <br />rose an average of 2.15 feet, the groundwater gradient decreased from 0.0024 feet per foot (ft/ft) to <br />0.0018 ft/ft, and the direction of groundwater flow remained toward the northeast. The groundwater flow <br />direction and gradient appear to be consistent with recent historical trends. <br />Between May 14, 2010, and April 29, 2011, the concentrations of gasoline compounds in groundwater <br />were generally similar in MW-1 and generally decreased in MW-2 and MW-4. The concentration of <br />methyl tertiary-butyl ether (MTBE) in the down-gradient well MW-4 decreased from 29.8 micrograms <br />per liter (4/1) to 29 lag/l. The concentration of MTBE in MW-4 has decreased in each of the last seven <br />sampling events. <br />Gasoline hydrocarbons were concentrated near MW-1 and decreased in concentration with distance from <br />the source area. The lateral extents of TPH-G and benzene appeared to be defined by the four perimeter <br />wells MW-3, MW-4, MW-5 and MW-7 and the lateral extent of MTBE in groundwater appeared to be <br />mostly defined, except in the down-gradient direction. <br />Condor recommended that the remedial feasibility testing and vertical investigation tasks be completed. <br />Condor also recommended that groundwater monitoring continue under the following revised semi- <br />annual schedule: MW-1, MW-2, and MW-4 (semi-annually), MW-6 (annually), and MW-3, MW-5, and <br />MW-7 (every two years). <br />On June 9 and 10, 2011, Condor conducted an air sparge and soil vapor extraction pilot test with the <br />approval and oversight of the San Joaquin County Environmental Health Department (SJCEHD). The <br />two-day test included soil vapor extraction tests at the wells SVE-1A, SVE-1B, and SVE-2B, a longer <br />term test at MW-1, and an air sparge and soil vapor extraction test at MW-1. The results of the SVE pilot <br />test indicated that vapor extraction flow rates of 63 to 81 scfm can be achieved and maintained with <br />equipment similar to that used in the test. Condor estimated the radius of influence for SVE wells was <br />approximately 50 feet. The hydrocarbon extraction rate was highest at MW-1 (10 pounds per hour), and <br />SVE-1B had the highest extraction rate (2.5 pounds per hour) among the SVE wells. Condor estimates the <br />radius of influence for air sparge well AS-1 is approximately 30 feet. The air sparge pilot test did not <br />indicate that air sparging would increase the SVE hydrocarbon extraction rate, but it did indicate that air <br />sparging would be effective for decreasing groundwater hydrocarbon concentrations in the vicinity of the <br />air sparge well. The results of the pilot test were included in the Air Sparge/ Soil Vapor Extraction Pilot <br />Test Report June 2011, dated January 20, 2012. <br />Between April 29, 2011, and November 3, 2011, the groundwater surface in the seven monitoring wells <br />raised an average of 0.82 feet, the groundwater gradient remained unchanged at 0.0018 ft/ft, and the