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3.2 Tidal Study Conclusions <br /> k <br /> Based on an interpretation of these results, hydraulic communication exists between the <br /> unconfined aquifer being monitored fat the site and nearby tidally influenced water bodies such <br /> as the Stockton Deep Water Channel. However, the results also indicate the tidal effect on <br /> groundwater elevations is minimal and does not impact the groundwater gradient direction at the <br /> site. Because the results of the tidal study indicate only minimal tidal fluctuation of groundwater <br /> beneath the site, it is WESTON'sopinion that this initial tidal study has adequately characterized <br /> the tidal influence on the site and no additional tidal evaluation is necessary. <br /> I II <br /> i <br /> 1 L <br /> 1 <br /> I <br /> jp <br /> 1 <br /> i <br /> I <br /> h <br /> k <br /> I II S r <br /> RFTS/ESMUDRPr.W5 <br /> P Ourm <br />