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Eckert Cold Storage Company <br /> ' 757 Moffat Blvd, Manteca, California November 26, 1997 <br /> Underground Tank Investigation, Continued Phase I Report of Findings Page: 6 <br /> the fans occasionally prograded over the axial area of the trough in response to major <br /> ' climatic changes in the Sierras. This has resulted in a predominance of fine grained silts <br /> and clays in the subsurface of the area. <br /> 5.0 Soil Conditions <br /> ' The lithology at this site is characterized as thinly bedded silty sands, well-graded sands, silts <br /> and clays(Figures 4 & 5). Saturated sands below the water table became very fluid ("heaved", <br /> ' "flowed", "caved") and made well installation very difficult. <br /> Laboratory analysis of soil samples detected BTEX and Gasoline contamination in the soils <br /> ' above the water table in borings MW-1, 2 and 3. All soil samples for MW-4 tested "ND" <br /> (Table 1 & Appendix A). TEPH (for Kerosene, Diesel and Motor Oil) tested "ND" (None <br /> Detected) in all soil samples. <br /> 60 Hydrology <br /> ' California and the Federal Government have mandated that virtually all groundwater is <br /> ' beneficial for current or future use unless it can be demonstrated that no beneficial use is <br /> known. <br /> ' This aquifer is considered to be of beneficial use and as a result, must be protected from <br /> contamination. Those identified uses include agriculture and industrial, as well as <br /> potential use for animal or human consumption. <br /> 7.0 Groundwater Conditions <br /> ' Analyses of the six monitoring wells MW-1, 3, 4, 5, 6 & 7 (MW-2 was damaged and is used <br /> for water levels, only) show that contaminants are present in MW-1, 3, 6&7. <br /> tAll the wells were resurveyed after the addition of MW-5, 6 & 7. (Appendix F). Gradient was <br /> calculated from the wells and is also shown as Figure 11. The predominant direction is N490W <br /> ' at 0.00233 fl/ft (Figure 11). The surface of the site is paved, but the area to the east is open <br /> residential property. Recharge from surface precipitation is the probable cause of the steep <br /> gradient to the west. <br /> All groundwater samples collected during this event were non-detectable for the oxygenated <br /> ' compounds by EPA Method 8260. <br />