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2 GROUNDWATER FLOW DIRECTION AND GRADIENT <br /> On June 7, 2002, ASE measured the depth to water in each site <br /> groundwater monitoring well using an electric water level sounder The <br /> surface of the groundwater was also checked for the presence of <br /> free-floating hydrocarbons or sheen using an oil/water interface probe a n d <br /> a product thickness bailer Free-floating hydrocarbons were not observed <br /> in any of the groundwater monitoring wells measured this quarter <br /> Groundwater elevation data is presented as Table One <br /> Groundwater elevation (potentiometric surface) contours are plotted on <br /> Figures 2, 3 and 4 Groundwater in the shallow zone (less than 20-feet <br /> bgs) has historically shown a northern or northwestern flow This quarter, <br /> the groundwater flow direction is primarily to the northwest with a <br /> gradient of approximately 0 0009-feet/foot A shallow zone <br /> potentiometric surface map is presented as Figure 2 <br /> Groundwater in the middle zone (55--70-feet bgs) flows toward the <br /> southwest this quarter at a gradient of approximately 0 0054-feet/foot <br /> The groundwater flow in the deep zone (greater than 100-feet) flows <br /> • toward the southwest this quarter at a gradient of approximately 0 00057 <br /> feet/foot <br /> Potentiometric surface differences in wells adjacent to each other b u t <br /> screened in different zones such as monitoring wells MW-6, MW 7 and <br /> MW-8 show a decreasing hydraulic head with depth, suggesting the <br /> potential for downward groundwater flow <br /> 3 . 0 GROUNDWATER SAMPLE COLLECTION <br /> On June 7, 2002, ASE collected groundwater samples from ten (10) of t h e <br /> site groundwater monitoring wells for analysis The number of wells to be <br /> sampled each quarter was proposed in ASE's letter to the San Joaquin <br /> County PHS-EHD dated September 2, 2001 and approved during a <br /> subsequent telephone conversation with Lori Duncan of the PHS-EHD <br /> Prior to sampling, the site monitoring wells were purged of three well <br /> casing volumes of groundwater using a Grundfos pump and/or dedicated <br /> polyethylene bailers The pH, temperature, and conductivity of the purge <br /> water was monitored during evacuation, and samples were not collected <br /> . until these parameters stabilized Samples were collected from the wells <br /> using dedicated bailers The groundwater samples were decanted from the <br /> Frank's One Stop Quarterly Report — June 2002 Sampling <br /> -2- <br />