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„ r • <br /> • <br /> packed with number 3 sand to approximately 1 to 2 feet above the slotted interval. A surged and <br /> refilled bentonite plug will be added above the sand pack to prevent cement from entering the well pack. <br /> The remaining annulus will be backfilled to grade with a slurry of cement and bentonite powder. <br /> The monitoring wells will be protected with a traffic-rated, cast-aluminum utility box equipped with a <br /> PVC skirt. The box has a watertight seal to protect against surface-water infiltration and must be <br /> opened with a special wrench. The design of this box discourages vandalism and reduces the possibility <br /> of accidental disturbance of the well. <br /> Well Development and Samoling <br /> ERI will wait a minimum of 24 hours before development of the monitoring wells to allow the grout to <br /> seal. Initially, a water sample will be collected for subjective analysis before development of the <br /> monitoring wells. This sample will be collected from near the water surface in the well with a Teflon® <br /> bailer cleaned with a laboratory-grade detergent and deionized water. The wells will be developed with <br /> a surge block and pump. Well development will continue until the discharge water is clear of silt and <br /> sand. Clay-size sediments derived from the screened portion of the formation cannot be eliminated by <br /> well development. After the well has been allowed to stabilize, the well will be checked for floating <br /> product using an interface probe. The thickness of any product detected in the well will be recorded. If <br /> floating product is encountered in the well, the well will not be purged, and the water will not be <br /> sampled for chemical analysis. Product will be bailed from the well and stored in appropriately labeled <br /> drums onsite. ERI will apprise Unocal of appropriate recycling options for product bailed from well. <br /> If no floating product is detected after development, the well will be purged of stagnant water and a <br /> sample will be collected for laboratory analysis. The well will be purged of approximately 3 to 5 well <br /> volumes of water with a submersible pump, or until pH, conductivity, and temperature of the purged <br /> water have stabilized. Water purged from the wells will be stored in labeled, 55-gallon, steel drums <br /> approved for this use by the Department of Transportation until suitable recycling options can be <br /> selected based on laboratory analysis. ERI will coordinate with Unocal for disposal of the purged <br /> water. <br /> The wells will be allowed to recover to at least 80 percent of static conditions, and a sample of the <br /> formation water will be collected with a new disposable Teflon®bailer. The water will be transferred <br /> slowly from the bailer to laboratory-cleaned, 1-liter amber bottles and 40-milliliter glass vials for <br /> analyses by the laboratory. The glass vials will contain hydrochloric acid as a preservative. The <br /> sampler will check to see if headspace is present. If headspace is present, the sampler will collect more <br /> samples until none is present. Chain of Custody Records will be initiated in the field by the geologist, <br /> updated throughout handling of the samples, and sent along with the samples to the laboratory. Copies <br /> of Chain of Custody Records will be included in our final report. <br /> Gradient Evaluation <br /> ERI will evaluate the direction of flow and gradient at the site. The elevation of the top of each well <br /> casing will be measured relative to mean sea level by a licensed land surveyor. Water-depth <br /> measurements will be made from the top of the casing in the well to the nearest 0.01 foot with an <br /> electronic water-level indicator. The well will be vented to atmosphere for a minimum of 0.5 to 1 hour <br /> before obtaining depth-to-water measurements. Venting is conducted to allow the groundwater to <br /> equilibrate with barometric pressure. These data will be combined to evaluate the relative elevation of <br /> the groundwater surface in each well and the slope of the groundwater surface across the site. <br />