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k <br /> Geological Tec vda lac. Page 5 <br /> • Groundwater Monitoring Report <br /> Project No. 750.2 <br /> December 20,2001 <br /> $ • The remaining wells were found to be free of contaminants, which is consistent with <br /> other events. <br /> ` • Vertical groundwater gradient was calculated and determined to be downward and r <br /> greater than the horizontal gradient of the water table, suggesting that the contaminants <br /> in the water table may be transported to deeper depths in the subsurface. <br /> • Oxidation-Reduction Potential measurements (Table 4) are positive for all the wells, <br /> suggesting that the volume of contaminants leaching into groundwater is minimal and <br /> that biodegradation of the contaminants is at a rate sufficient enough to beep the <br /> BTEX/TPH-G plume in a small area around the source without depleting the oxygen to <br /> a level to slow the reaction process. <br /> Recommendations: <br /> • Quarterly groundwater monitoring will continue at the site. The next event will occur <br /> by February 28, 2002. <br /> • A Vadose Zone Remediation - Corrective Action Plan has been approved by San <br /> Joaquin County PHS/EHD and the USTCFP. The soil vapor extraction system is in the <br /> process of being installed and should be completed by early January 2002. <br /> 3.0 LIMITATIONS <br /> +' This report was prepared in accordance with the accepted standards and practices of the <br /> field of environmental geology, groundwater hydrology and good business practices. it <br /> should be recognized that definition and evaluation of environmental conditions is a <br /> a difficult and an inexact science. Judgments leading to conclusions and recommendations <br /> are generally made with an incomplete knowledge of the site-specific conditions present. <br /> The tasks proposed and completed during this project were reviewed and approved by the <br /> local regulatory agency for compliance with the law. No warranty, expressed or implied, is <br /> I made, i <br /> I <br /> t <br /> k <br /> 1 <br />