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' Site Investigation Report for the <br /> Former UST Locations at Stockton AASF <br /> California Army National Guard <br /> 1.3 Physiographic Setting <br /> Approximately 90% of the land surface within the AASF is paved. Some grasses exist throughout the <br /> area; landscaping and maintenance is performed to reduce vegetation around aircraft locations. The <br /> ' site has been graded and modified to promote surface drainage into storm drain inlets(Figure 1-2). <br /> Catch basins collect rainwater and divert the runoff to the north through underground pipes into the <br /> adjacent airport/Stockton storm/sewer water system. The system drains approximately 1.5 miles <br /> ' north of the site into Little John Creek,then into French Camp Slough, and finally into the San <br /> Joaquin River(Versar, Inc., 2004). <br /> ' 1.4 Geology <br /> 1.4.1 The site lies within the Sacramento Valley which is composed of unconsolidated Quaternary <br /> sediments from alluvial and lake deposits. The Sierra Nevada Mountains to the east are a source of <br /> ' the alluvium deposits as a result of erosion. Also contributing to the deposits are the Sacramento <br /> Valley Coast Ranges to the west. Both ranges consist of a wide variety of rocks and granite,which <br /> are metamorphic (ranging widely in age and composition) and sedimentary. In addition,the Stockton <br /> ' Fault, which trends northeast-southwest, is located within the city limits, as well as the Midland Fault <br /> Zone (trending north), located approximately 25 miles northwest of the site(Versar, Inc., 2004). <br /> ' 1.4.2 Depth-to-groundwater in the vicinity of the site is estimated to be approximately 37 to 44 feet <br /> bgs. The groundwater gradient is 0.004 feet/foot(Versar,Inc., 2004),however,the gradient cannot <br /> be accurately measured based on data from only three closely spaced wells. Based on the limited <br /> ' data, groundwater flow is estimated to be toward the north; this conclusion is based on the historical <br /> groundwater measurements collected from the three existing AASF monitoring wells. <br /> ' 1.4.3 Based on the 12 soil borings drilled and sampled by URS in March 2008,vadose zone soils <br /> from beneath the surface fill to groundwater consist of interlayered silty clays,clayey silts, and silty <br /> and clayey sands (soil boring logs are shown in Appendix A). <br /> ' 2.0 AREAS OF POTENTIAL ENVIRONMENTAL CONCERN <br /> 2.1 The areas of potential environmental concern at the AASF, in regard to this site investigation, <br /> are the locations of the two former 20,000-gallon USTs and the three former 5,000-gallon USTs and <br /> associated piping and fuel dispensers. <br /> 2.2 Review of the preliminary assessment/site investigation update report indicates that Versar,Inc., <br /> has conducted a preliminary assessment and site investigations of the Stockton facility(including the <br /> AASF). This site investigation is a continuation of those investigations, and is intended to determine <br /> the extent of contamination at the AASF. Contaminants of potential concern associated with this area <br /> include TPH-D,TPH-G, BTEX, oxygenates,and lead. VOCs were also detected in both soil and <br /> groundwater during the URS investigation; however,no potential source areas for VOCs have been <br /> identified during previous AASF site investigations. <br /> 3.0 CONCEPTUAL SITE MODEL <br /> ' This subsection presents details of the previous investigations of the area of the two former 20,000- <br /> gallon USTs at the Stockton AASF, the nature and extent of petroleum impacts, and migration <br /> potential.The following information describes the investigations nearby/adjacent to the three former <br /> KAWprocess\00251\CA ARNG\Stockton AASF SI\FINAL\SI Rpt.doc 3 June 2008 <br />