Laserfiche WebLink
Geologiut 'ecknks Inc. Page 4 <br /> ' Groundwater Monitoring Report <br /> Project No.989.2 <br /> April 25, 2002 <br /> 2.2 Laboratory Analyses <br /> ' The groundwater samples collected on March 14, 2002, were delivered to Sherwood Labs <br /> (Department of Health Services Certification No. 1400), of Hilmar, California, for the <br /> 1 following analyses: <br /> • Benzene, toluene, ethylbenzene and xylene (BTEX by EPA method 8020) <br /> • Gasoline range petroleum hydrocarbons (TPH-Gasoline by EPA method 8015(m)) <br /> ' Fuel oxygenate suite (MTBE, D1PE, ETBE, TAME, and TBA by EPA method 8260) <br /> • <br /> 1,2-Dibromoethane and 1,2-Dichloro ethane (1,2 DCA and EDB by EPA method 8260) <br /> ' The fuel oxygenates, 1,2 DCA and EDB samples were submitted to Entech Analytical Labs <br /> of Santa Clara, California (DHS # 2346). <br /> ' A Chain of Custody was completed for all samples collected and tracked to ensure sample <br /> integrity. Laboratory data sheets with detection limits are included in Appendix C. <br /> ' The laboratory data were submitted electronically to GeoTracker as required under AB2886 <br /> on March 29, 2002. The confirmation number for the electronic submittal is 1641162216. <br /> 3.0 FINDINGS AND DISCUSSION <br /> ' 3.1 Hydrology of Site <br /> ' On March 14, 2002, the depth to groundwater was measured in all of the wells prior to <br /> purging. Depths to groundwater ranged from a high of 7.53-feet below the top of casing to <br /> a low of 8.86-feet below the top of casing. The average depth to water was 8.35-feet below <br /> tthe top of casing. The wells are screened at 5-feet bgs and groundwater surface continues to <br /> be below the tops of the screens in the 6 monitoring wells. Groundwater elevations were <br /> calculated and are summarized in Table 2 of Appendix A. <br /> I <br /> Site-specific groundwater gradient was calculated using MW-1, MW-3 and MW-6, and <br /> ' found to be N 17°W at 0.0049 ft/ft. The calculated groundwater gradient is displayed on the <br /> groundwater gradient map, Figure 3. Previous groundwater gradient calculations show a <br /> consistent bearing of north-northwest. The bearings have been measured between N050W <br /> ' and N45°W and the slope averages 0.0062 ft/ft. Groundwater bearing and slope are <br /> summarized in Table 2 of Appendix A and are plotted on a Rose Diagram, Figure 4. <br />