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Mohr-Fry Ranches <br /> 950 Industrial Drive Stockton California <br /> Groundwater Sampling Report <br /> AuguA 1994 <br /> Narrative <br /> On August 4, 1994, WBF, Inc, in conjunction with HKM Groundwater, conducted field <br /> measurements, well pumping and groundwater sampling on three groundwater monitoring wells <br />' located at this site(Figure 2) <br /> All samphng equipment, including the bailer and cables used by sampling personnel, was disassembled <br />' and steam-cleaned prior to commencement of samphng These procedures were followed between <br /> each well, sampling point, and at the end of the sampling day De-ionized or organic-free water <br /> (provided by the laboratory)was introduced into the bailer as a final stage of cleaning This water was <br />' then gently poured into sample vials to be used as bailer blanks These bailer blanks were not tested <br /> unless their corresponding samples contained contaminants <br /> Immediately prior to sampling, water levels and well depth measurements were taken in all wells at the <br /> site Each well was evacuated using a stainless steel bladder pump which does not introduce air into <br /> the water column The pH, temperature and electrical conductivity of the water were monitored as the <br />' wells were evacuated (Table 2) These parameters are noted on the Field Logs (Appendix B) <br /> Instruments calibrated to known standards were used to monitor these parameters At least three (3) <br /> well volumes were evacuated from each well, and more, if necessary, until the above parameters were <br />' stabilized Once stability was achieved, the samples were collected, labeled and chilled in an ice chest <br /> with Blue Ice <br />' The samples were carefully poured from a Teflon bailer into half gallon plastic containers and clean <br /> glass vials with Teflon-tuned screw caps provided by the laboratory Care was taken to ensure that no <br />' air space existed in the vials by inverting to check for bubbles and re-sampling if necessary The <br /> samples were analyzed or extracted within 14 days according to their EPA methods <br />' A travel blank provided by the laboratory accompanied the sample vials from the tune they were picked <br /> up from the lab to the time they were returned to the laboratory This travel blank was only analyzed if <br /> the samples contained contaminants The travel blank and sample vials were then logged on a Chain of <br />' Custody Record and dehvered to GeoAnalyhcal, Inc, a State certified laboratory in Modesto, <br /> Cahfonua The analysis requested for the water samples were EPA method 602 for BTX&E <br /> compounds, and EPA method GCFID 3510 for Diesel The analytical results are listed m Table 3 of <br />' this report <br /> Groundwater elevations from 8/4/94 were used to construct a groundwater gradient map and calculate <br /> the gradient at 0 0016 ft/ft at N 14°W(Figure 3) Monthly water level readings were conducted since <br /> 1 <br />