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10, MEMO <br /> F <br /> 2021899-7004 <br /> - Lammersville School District 9 <br /> July 16; 1990 <br /> observations,one sample from each boring was selected for laboratory analysis. Samples were preserved <br /> manifest to GTE C L Environmental Laboratories, <br /> on ice and delivered with the appropriate Chain-of-Custody <br /> Inc. (GTEL),a State-certified laboratory,in Concord,California. The soil samples obtained from the three <br /> borings (MW-6, MW-7 and MVv8) were analyzed for TAH-G and BTEX using U. S. Environmental <br /> Protection Agency (EPA) Methods 50301801518020. <br /> 5.5 MONITORING WELL INSTALLATION MW-7, and MW-8}to provide <br /> -- The three soil borings were completed as monitoring wells(MW-6, <br /> groundwater sampling points east of the site. The wells were installed to a total depth of 20 feet and were <br /> _ constructed of 15 fret of 0.020-inch, machine-slotted PVC screen threaded to blank PVC; casing to the <br /> surface. The annular space from the bottom of the wells to approximately 1 foot above the slotted interval <br /> was filled with number 2112 grain-size sand. The wells were then sealad with approximately 2 feet of <br /> bentonite,overlain by sand-cement grout to the surface. The drilling and construction of the yells, and <br /> placement of the annular seals,was inspected by Mr.Gregory Lyon of the SJCPHS-END. <br /> re installed to provide access to all the wells. <br /> Lacking caps and traffic-rated street boxes we <br /> Specific well construction details,which are shown on the drill logs, are included in Appendix ll. <br /> 5.6 GROUNDWATER MONITORING <br /> On June 19, 1990,the wells were dEvelcped using bailing and surging techniques to remove fine <br /> particulates and to accelerate proper settling of the sand pack. Groundwater collected during well <br /> development was stored on site in DOT-approved containers for disposal or remediation at a later date, <br /> depending on the results of laboratory analyses. <br /> On June 21,1990,depth to groundwater was measured to determine static water table elevations <br /> �ocarbons[Table 4). Prior to monitoring,all eight <br /> and the presence of any separate-phase petroleum hyd <br /> levation control. An arbitrary datum of 100 feet was use <br /> wells were surveyed to grade level for ed far <br /> elevation control, using MWA as a benchmark. The depth to water was measured using an interface <br /> at <br /> uishes between <br /> _ probe, consisting of a dual optical sensor and electrical conductivity probe,witthe <br /> s iveysr results lts to determine <br /> water and petroleum products. The monitoring data was combs <br /> the water table elevation in each of the monitoring wells. Figura 3 presents a Potentiometric Surface Map <br /> drocarbons <br /> of the water tableelevationsmeasured on June 21,-1990--.-Noseparate-please petroleum y were measured on the groundwater surface, �- <br /> GROUNDWATER <br /> TECHNOLOGY.INC. <br />