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Prior to the ROW acquisition, Kaldveer Associates (Kaldveer) performed a soil quality <br /> investigation for CalTrans on the eastern portion of the site shown on Figure 2. <br /> Based on the results of the DHS and Kaldveer sampling, the Superior Court ordered the owners <br /> of the property to conduct a soil investigation. <br /> 4_0 Hydrogeological Setting <br /> The site is located in the east central portion of Stockton, at the southwest corner of Miner <br /> Avenue and State Highway 99, in a mixed light industrial and residential area. The elevation <br /> of the site is approximately 26 feet above sea level. The ground surface in this area generally <br /> slopes gently to the west at about 5 feet per mile. <br /> The nearest surface water bodies are ephemeral and include the Stockton Diverting Canal, <br /> located a little less than one mile to the northeast, and Mormon Slough, located about 6,000 feet <br /> to the south. <br /> Based on published data, the current depth to groundwater beneath the site is estimated to be <br /> approximately 65 feet. Historical high groundwater (Spring 1986) is estimated to have been <br /> about 50 feet below grade. Groundwater flow in the site vicinity is expected to be generally <br /> easterly towards a large pumping depression on the east side of Stockton. <br /> As described by Kaldveer, the surface soil at the site consists of dark brown to black, organic <br /> rich clay from the surface to a depth of approximately 2-3 feet. Underlying this unit is a brown <br /> silty clay/clayey silt to a depth of approximately 7-8 feet. Beneath the brown clay, a red-orange <br /> silt is present to 10 feet, the maximum depth explored. <br /> Based on the boring advanced by hollow stem auger (HSA) by Ground Zero in February 1997, <br /> the uppermost three feet of soil at the site generally consisted of dark brown to black organic <br /> rich clay. Underlying this unit, brown silty clays and silts were found to a depth of 41 feet, the <br /> maximum depth explored. Groundwater was not encountered, however streaks of saturated clay <br /> were observed between the depths of 20 and 28.5 feet. The saturated streaks in this boring are <br /> attributed to the proximity of a septic system seepage pit. <br /> 5.0 Investigation by Kaldveer <br /> In June 1991,Kaldveer drilled 33 exploratory soil borings in the ROW acquisition area to depths <br /> of 10 feet below ground surface (bgs). Soil borings were located in a grid-like pattern, but some <br /> were moved to locations of apparent staining. Three near-surface soil samples collected by <br /> hand, and a total of 66 soil samples collected from the borings at depths of 1 and 4.5 feet bgs <br /> were submitted to a CalTrans-approved laboratory. Selected samples were analyzed for total <br /> recoverable petroleum hydrocarbons (TRPH), total petroleum hydrocarbons as gasoline and <br /> rays\torts\summary 2 <br />