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r^ <br /> IT CORPORAVON <br /> 3.1 GROUND WATER GRADIENT <br /> As only two piezometric elevations were known, the ground water gradient <br /> underlying the site could not be determined Three wells (MW-1, MW-8, <br /> and MW-9) have reached the water ;,able at the site. However, the pro- <br /> duct in MW-8 has depressed t"ie mater table to beneath the bottom of the <br /> well, making it impossible ;:o determ;s,e the true piezometric surface in <br /> this well. <br /> 3.2 WELLS LOCATED NEAR SITE <br /> Figure 3.1 shows the location of irrigation and domestic wells in the <br /> vicinity of the station. The data presented are from Well Drillers <br /> r <br /> Reports submitted to the California Department of Water Resources <br /> ` (DWR). Table 3.2, which accompanies Figure 3.1, shows information <br /> regarding each well plotted. The well number presented is the nunber on `r <br /> the Water Well Drillers report. Theapproximate elevation of the well <br /> is presented next and, in most cases, is simply an interpreted elevation <br /> from the topographic map for the area. The approximate distance of the <br /> well from the station is indicated. The next column indicates whether <br /> the well is for domestic or irrigation purposes. The depth of the well <br /> and the depth of the surface seal are presented followed by the screen <br /> interval. The surface seal is the cement grout that is intended to pro- <br /> tect the well from contamination migrating down the well bore from the <br /> land surface. The screen interval is the actual length of well that is <br /> open to `lccept water from the ground. Finally, an indication of whether <br /> � at well is active ol• inactive is made along with the year the well was <br /> drilled. Active wells will tend to draw contamination toward them where <br /> an inactive well will be passive. <br /> The station has a low potential for contaminating any wells, as there is <br /> only orie well within a half mile radius of the site. The well screen <br /> data indicate that txo of the wells are very deep and thus are not li!:e— <br /> ly to b : in an aquifer that has any.-direct connection with the shallow <br /> aquifer that would be contaminated by a hydrocarbon spill. <br /> ii t�� is <br /> ,• r - <br /> i.il(t <br /> 6 <br />