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Diamond Pet Food&Ripon Cogeneration July 12,2013 <br /> Second-Quarter 2013 Groundwater Monitoring Report Page 4 of 5 <br /> HYDROGEOLOGIC SETTING <br /> Geology and hydrogeology of the site and vicinity have been described in detail in previous <br /> reports.2 Briefly, the DP/Cogen site is located in the East San Joaquin Groundwater Basin and <br /> is underlain by a sequence of Tertiary- and Quaternary-aged continental deposits of the Tulare <br /> Formation. These deposits consist of interbedded sands/gravels and silts/clays or mixtures <br /> thereof. <br /> Four distinct aquifers or zones have been identified beneath the site and have been designated <br /> by L&A as the semiperched, upper, intermediate, and lower zones. The semiperched zone is <br /> unconfined and occurs from approximately 35 to 60 feet below ground surface (bgs). All other <br /> zones are semiconfined to confined. The upper zone occurs from approximately 85 to 110 feet <br /> bgs, the intermediate zone from 140 to 225 feet bgs, and the lower zone from 240 to greater <br /> than 300 feet bgs. Permeability in the aquifer zones has been estimated at approximately 525 <br /> gpd/ft2; permeability in the confining layers has been estimated at 3.5 gpd/ft2.3 <br /> Groundwater movement in the semiperched and upper semiconfined zones in the vicinity of <br /> Ripon is generally to the west.4 North of Ripon, groundwater moves to the north. Southwest of <br /> Ripon, on the southwest side of the San Joaquin River, groundwater also moves to the north, <br /> towards the river. <br /> GROUNDWATER MONITORING <br /> DEPTH TO GROUNDWATER <br /> The depth to groundwater was measured in all wells prior to purging and sampling using an <br /> Actat Model 300 electric well probe. The depth to groundwater was recorded to the nearest <br /> 0.01 foot(Table 2; Figure 2). <br /> PURGING PROCEDURES <br /> Wells were purged and sampled with a 12-volt PVC submersible pump. Groundwater was <br /> purged from each well until three well volumes of water had been removed from the wells or <br /> until the field parameters of conductivity and pH had stabilized. Purge water was discharged <br /> directly to the ground and allowed to infiltrate or evaporate. <br /> SAMPLE COLLECTION <br /> Each groundwater sample was collected in appropriate sample bottles provided by the analytical <br /> laboratory,placed on ice in a cooler with a chain-of-custody form, and shipped under chain-of- <br /> custody to BC Laboratories, Inc. in Bakersfield, California for analyses. <br /> FIELD ANALYSES <br /> L&A performed field analyses for temperature, conductivity, and pH on groundwater samples <br /> using a Hanna Combo pH/conductivity meter and a LaMotte 2020 turbidity meter. All meters <br /> were field calibrated with standardized solutions before use. <br /> 2 L&A,May 5, 1992,Impacts on Receiving Waters from Discharge at the Simpson Paper Company Facility, <br /> Ripon, California. <br /> 'Ibid., P.27. <br /> 'Ibid., Fig. 3. <br /> 10107.04 Task 2 Lawrence&Associates <br /> W.ICLIENTSIDiamond Pet Foods1010107.01-Groundwater MonitoringlGroundwater Monitoring1201312Q201312nd quarter 2013.docx <br />