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Lodi -Quartefly Groundwater Monitoring Page 2 <br /> The three groundwater monitoring wells were installed approximately ten feet into the <br /> groundwater aquifer. The well locations are provided in Figure 1. Groundwater was encountered <br /> at a depth of 50 feet BGS during drilling activities. The screened interval consists of 2-inch <br /> diameter Schedule 20 PVC casing (0.02 slot) that extends from the end of hole to five feet above <br /> the groundwater surface. Blank 2-inch diameter Schedule 20 PVC casing extends from the <br /> screened interval to the ground surface. The sand pack (#2 grade) extends from the bottom of <br /> the boring to five feet above the screened interval. A pelletized bentonite seal (2 feet thick) lies <br /> directly above the sand pack. The remainder of the annular space is filled with grout. A locking <br /> end cap was placed at the top of each casing. The wells are protected at the ground surface with <br /> flush mounted steel Christy boxes set in concrete. <br /> Twenty-four hours after the third well was installed, five casing volumes of water were purged <br /> from monitoring well SRK-MW1, while well SRK-MW2 and SRK-MW3 were bailed dry after <br /> lfour casing volumes were purged. The casing volumes were based on actual static water level <br /> measurements made on the day of sampling. The wells were purged using a teflon bailer and <br /> dedicated nylon rope. The bailer was thoroughly cleaned before purging each well using non- <br /> phosphate soap followed by a deionized water rinse. All water purged from each was placed in <br /> 55-gallon, closed-top drum. No petroleum odors or iridescent sheen were observed in water <br /> evacuated from any of the monitoring wells. <br /> 2.0 SCOPE OF SERVICES <br /> The scope for this phase of work included: <br /> • Property survey to accurately locate the position and elevation of the monitor wells. <br /> ' • Purging and sampling the wells according to PHS/EHD guidelines. <br /> ' • Shipping the groundwater samples under correct chain-of-custody procedures to a <br /> California licensed Laboratory for analyses. <br /> ' • Determining the localized groundwater gradient by measuring the static water level <br /> relative to the top of casing. <br /> i3.0 GROUNDWATER GRADIENT <br /> SRK retained the services of Cella Barr Associates to provide elevations at the top of well heads <br /> relative to a known datum, and the locations of the wells relative to on-site structures. This <br /> information is provided on Figure 1 (located in the pocket at the back of this report). Static <br /> water levels were measured on April 6, 1992, using a Solinst Water Level Indicator. Copies of <br /> the static water levels are provided in Table 1. <br /> zsn+-ra�orcr va.z. <br /> Steffen Robertson and Kirsten <br />