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� W ..n T'�".?PPaa��• .r A �` � �� ��• 'mss R i. . �� ,-�S�e m 'as'sxF'�—"a�__e,�ss�y3- ���.�5 -_ <br /> %-���• � -, � hf :ham _A � �x -/M �'l�w. � }. <br /> i <br /> }iLEItiFEL1)Eti <br /> o Based on the observed geologic conditions, the wells were screened with 2-inch <br /> inside diameter, flush threaded joint, schedule 40, ASThI F-480 PVC pipe with <br /> 0.020-inch factory-cut slots. <br /> o In general, the wells were screened from 5 feet above to 15 feet below first <br /> encountered ground water. <br /> o The annular space between the screen aad the wall of the boring was backfilled <br /> — with clean x112 Lonestar Industries Monterey sand to approximately 2 feet <br /> above the slotted sections. The annular space above the 2112 sand was then <br /> nilcd an additional foot with clean 0130 L.onestar Industries sand. This was <br /> done to prevent benioritc, pellets from leaching into the slotted screen. The <br /> screen and sand filter pack size were selected in the field based on the geologic <br /> conditions encountered in each boring. <br /> o A 3-foot bentonite plug was placed above the sand pack to provic'e a seal against <br /> cement/bentonite grout infiltration. <br /> -� o The remaining annular space was filled with cement/bentonite grout to the <br /> surface. The grout was inplaced under pressure through 1.25-inch diameter <br /> tremmie pipe. <br /> o Each well was secured inside a locking well cover. <br /> WATER LEVEL MEASUREMENTS <br /> Water level measurements were made in three monitoring wells located at the site. <br /> Measurement protocol was as follows: <br /> 1. The water level probe was decontaminated in a trisodium phosphate wash, <br /> �• followed by a distilled water rinse, prior to use in each well. <br /> 2. Water level measurements were made using a conductivity based water level <br /> indicator. Depth-to-water was measured from the north rim of the PVC well <br /> casing to the nearest 0.01 foot. <br /> FIS-91-62 <br /> Copyright 1991 Kleinfelder, Inc. <br />