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View File - Development Services - City of Oxnard

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WATER RESOURCES TECHNICAL REPORTtwo UAS wells (Nos. 22 and 23), and three UAS wells. Water levels decreased up to20 feet in the UAS and up to 10 feet in the LAS in the vicinity <strong>of</strong> the water yard. Thesewater level decreases will result in the following:−−In the UAS, these small to moderate decreases, combined with the declines from theUWCD El Rio wellfield extractions, will increase the potential to induce brief periods<strong>of</strong> coastal landward flow during extended, drier climatic periods (see Scenario 2chydrograph for coastal well 05G02, which twice briefly drops below sea level forsimulation period [Figure 6-27]).In the LAS, these moderate decreases will increase the moderate potential forlandward flow that exists, particularly during drier years and in the fall when waterlevels are seasonally low.• Moderate to large decline in groundwater elevations in the Forebay area as a result <strong>of</strong>extracting 15,429 AFY (80 percent) <strong>of</strong> the 19,286 AFY <strong>of</strong> in-lieu recharge from the UWCDEl Rio wellfield. Water levels decreased up to 30 feet in the UAS and up to 10 feet in theLAS. The water level decline in the LAS is mostly due to interference from drawdown atthe <strong>City</strong> Water Yard. These water level decreases will result in the following:−−In the UAS, these moderate to large declines may interfere with pumping operationsat the Forebay spreading grounds. Combined with the declines from <strong>City</strong> WaterYard extractions, these declines will contribute to the increased potential to inducebrief periods <strong>of</strong> coastal landward flow during extended, drier climatic periods (seeScenario 2b hydrograph for coastal well 05G02, which twice briefly drops below sealevel for simulation period [Figure 6-27]).In the LAS, these small declines are attributed mostly to drawdown from theextractions at the <strong>City</strong> Water Yard and, consequently, will have no significant effect.These changes will result in the following reductions in overdraft:• For the UAS, the average height above the coastal water level goal will remainapproximately the same, 5.6 feet for Scenario 2b compared to 5.7 feet for the Base Case.• For the LAS, the reduction in overdraft will be 32 percent compared to the Base Case.Scenario 2cScenario 2c results in the following changes relative to the Base Case:• Very large rise in groundwater elevations at the coastal injection wells (seawaterintrusion barrier) as a result <strong>of</strong> injecting 6,172 AFY in this area and a large rise overbroad areas across the southern <strong>Oxnard</strong> Plain and Pleasant Valley areas. This occursmostly in the LAS, as a result <strong>of</strong> delivering 19,286 AFY <strong>of</strong> recycled water to growers(Ocean <strong>View</strong> pipeline, PTP system, PVCWD system) in lieu <strong>of</strong> those growers pumpinggroundwater. Water levels increased up to 80 feet in the LAS along the injection wellsand up to 30 feet in the UAS across the southern <strong>Oxnard</strong> Plain and Pleasant Valley areas.Figures 6-23 and 6-24 show UAS and LAS groundwater elevations, respectively, for thefirst quarter 2020 (winter period) when water levels will be highest from injectionactivities (i.e., injection quarter). These water level increases will result in the following:W112003002SCO LW1458.DOC/ 033390002 91

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