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%Supplemental Information <br /> Report Of Waste Discharge <br /> 8200 N. Highway 99,Stockton, CA <br /> Page 3 of 6 <br /> 6. The proposed extraction system is an interim remediation system. A final remediation <br /> system, consisting of groundwater extraction/treatment and/or ozone injection, will be <br /> proposed after the interim system can be evaluated for effectiveness. At minimum, we <br /> expect groundwater extraction to continue for at Ieast 6-12 months before a final <br /> remediation plan is submitted. <br /> 7. The nearest known water user is located 350 feet north (cross-gradient) of the proposed <br /> extraction well and the proposed discharge area. Since domestic wells in the area are <br /> generally completed at depths greater than 120 feet, we do not expect any nearby water <br /> users to be directly affected by groundwater extraction or treatment system discharge, given <br /> the required effluent limitations. <br /> 8. According the Soil Survey of San Joaquin County, California, (USDA, Soil Conservation <br /> Service, 1992) the area of discharge is located within Soil Map Unit 180-Jacktone clay. <br /> According to the reference, the rate of water intake in irrigated areas is 0.1 inch per hour. <br /> Assuming a discharge area of 40 by 100 feet, this corresponds to approximately 250 gallons <br /> per hour, or more than 4 gpm. We anticipate extracting an average of up to 2 gpm from well <br /> MW 1. <br /> C. Groundwater Monitoring Program <br /> Groundwater monitoring wells at the site are currently sampled on a quarterly basis. The existing <br /> schedule will be adopted for the groundwater monitoring program. <br /> Measurement of the Depth to Groundwater in Monitoring Wells <br /> The depth of the groundwater surface in each monitoring well will be measured from the top of the <br /> well casing to the nearest 0.01 foot with a Solinst or similar electronic water-level indicator. The well <br /> will be vented to the atmosphere before obtaining depth-to-water measurements. Venting will be <br /> conducted to allow the groundwater to equilibrate to barometric pressure. These measurements are <br /> utilized with recorded well casing elevations to evaluate the elevation of the groundwater surface in <br /> each well and the slope of the groundwater surface across the site, if enough data points are available. <br /> Sampling of Groundwater Monitoring Wells <br /> The static water level in each well will be measured to the nearest 0.01 foot with a Solinst or similar <br /> electronic water-level indicator cleaned with a laboratory-grade detergent and deionized water before <br /> use in each well. A clean bailer will be used to obtain a sample from the surface of the water in the <br /> well for subjective analysis of hydrocarbons, if appropriate. The sample will be retrieved and <br /> examined for floating product, sheen, color, and clarity. <br /> Approximately 3 to 5 well volumes will be purged from each well using a submersible pump or a <br /> Teflon bailer to allow sampling of representative formation water. All downhole equipment/materials <br /> are decontaminated before use in each well. The wells are purged until pH, temperature, and electrical <br /> GAG ROUN DZEITULEB t J RGIReports\%vork plan\W DRSu pplementil.doc <br />