Laserfiche WebLink
Boyett Petroleum <br /> 419 Main Street, Manteca, California <br /> Quarterly Groundwater Sampling Report <br />' December, 1999 <br /> Narrative <br /> ' On December 10, 1999, GeoAnalytical Laboratories, Inc., conducted field measurements, <br /> well pumping and groundwater sampling on four (4) groundwater monitoring wells <br /> ' located at this site (Figures I and 2). <br /> Groundwater elevations were taken from four (4) wells prior to pumping (Table 1 & <br /> ' Appendix B). Monitoring wells MW-1 through MW-4 were evacuated by means of a <br /> steam-cleaned, stainless steel bladder type pump. During the three (3) volume pump <br /> down of each well, samples were collected to measure field pH, electrical conductivity and <br /> ' temperature (Table 3 & Appendix B). Once stability was achieved, a minimum of three <br /> (3) well volumes were removed and samples were collected with a disposable bailer. The <br /> samples were then labeled and placed in an ice chest cooled with Blue Ice®. <br /> lie <br /> The samples were then logged on a Chain of Custody (Appendix A) and transported to the <br /> State-certified laboratory, GeoAnalytical Laboratory Inc., in Modesto, California. The <br /> analysis requeSted for the four (4) water samples was EPA method 602 for BTX&E <br /> (Benzene, Toluene, Xylene, and Ethyl-Benzene) and MTBE (Methyl Tertiary Butyl Ether) <br /> and EPA method GCFID (5030/Luft) for gasoline. MTBE contamination was confirmed <br /> ' by EPA method 8260. The analytes and concentrations detected are listed in Table 2 of <br /> this report. <br /> Groundwater Gradient <br /> The water level measurements from three (3) monitoring wells (MW-1, MW-2, MW-3) <br /> were used to construct a groundwater gradient map (Figure 3). This quarter, the <br /> ' groundwater gradient trend is North 60° West with a downward slope of 0.001 ft/ft. <br /> Since the sampling event on September 27, 1999, the groundwater has risen an average of <br /> 0.63 feet or 7.56 inches. Historical groundwater gradient maps are provided for reference <br /> ' in Appendix C. <br /> k ' <br />