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
WATER RESOURCES TECHNICAL REPORT−−In the UAS, these increases will significantly help to further minimize the alreadylow potential that exists for coastal landward flow.In the LAS, these increases will significantly help to decrease the severe overdraftconditions and water quality degradation that exist in the LAS <strong>of</strong> the southern<strong>Oxnard</strong> Plain. Water levels will approach 80 feet above sea level along the injectionwells during the winter injection period. Annually, these water levels will cycle fromthis high during injection to approximately near sea level during the remainingnoninjection period (see Scenario 2c hydrograph for coastal well 32Q04 [Figure 6-27]). The year-round average gradient will be significantly above sea level and willbe sufficient to create seaward flow and reverse the seawater intrusion alongsouthern <strong>Oxnard</strong> Plain coastal area.• Moderate to large decline in groundwater elevations would occur in the vicinity <strong>of</strong> the<strong>City</strong> Water Yard in the UAS and LAS as a result <strong>of</strong> extracting 20,366 AFY (80 percent) <strong>of</strong>the 25,458 AFY <strong>of</strong> direct injection and in-lieu recharge from the <strong>City</strong> Water Yard wells:two LAS wells (Nos. 20 and 21), two UAS wells (Nos. 22 and 23), and three new UASwells. Water levels would decrease up to 40 feet in the UAS and up to 15 feet in the LASin the vicinity <strong>of</strong> the <strong>City</strong> Water Yard, and decreased up to 20 feet in the UAS and up to10 feet across the northern <strong>Oxnard</strong> Plain. These water level decreases will result in thefollowing:−−In the UAS, these moderate to large 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 decline in groundwater elevations in the Forebay area as a result <strong>of</strong> extracting5,092 AFY (20 percent) <strong>of</strong> the 25,458 AFY <strong>of</strong> direct injection in-lieu recharge from theUWCD El Rio wellfield. Water levels decreased up to 20 feet in the UAS and up to10 feet in the LAS. The water level decline in the LAS is mostly due to interference fromdrawdown at the <strong>City</strong> Water Yard. These water level decreases will result in thefollowing:−−In the UAS, these moderate declines will not interfere with pumping operations atthe Forebay spreading grounds. However, combined with the declines from <strong>City</strong>Water Yard extractions, these moderate declines will contribute to the increasedpotential to induce brief periods <strong>of</strong> coastal landward flow during extended, drierclimatic periods (see Scenario 2c hydrograph for coastal well 05G02, which twicebriefly drops below sea level 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.W112003002SCO LW1458.DOC/ 033390002 92
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CONTENTS6.2.2 Base Case and Phase 1
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CONTENTSFiguresSection 1.0 - Introd
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AcronymsACPAFYASRAWTFBasin PlanbgsB
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1.0 IntroductionThis Technical Repo
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WATER RESOURCES TECHNICAL REPORT•
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SANTA BARBARACOUNTYSanta BarbaraVEN
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WATER RESOURCES TECHNICAL REPORT2.2
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WATER RESOURCES TECHNICAL REPORTof
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WATER RESOURCES TECHNICAL REPORTThe
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WATER RESOURCES TECHNICAL REPORTres
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Figure 2-1Groundwater Basins and th
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Figure 2-3Groundwater Basins andUWC
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604020Precipitation (inches)0-20189
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Note: Generalized surficial geology
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(a) Groundwater Elevation Monitorin
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Figure 2-11DWR 1976Schematic CrossS
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02N22W12R01S02N22W22M04SVineyard Av
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Figure 2-15USGS Groundwater LevelHy
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Figure 2-17USGS Groundwater LevelHy
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(a) Groundwater Elevations, LAS, Sp
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(a) Total Dissolved Solids, UAS, 20
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(a) Chloride Concentrations, Oxnard
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Figure 2-25Subsidence onthe Oxnard
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WATER RESOURCES TECHNICAL REPORTAgr
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WATER RESOURCES TECHNICAL REPORTout
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TABLE 3-2City Blended Water Quality
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TABLE 3-4Agricultural Water Supply
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Figure 3-1NNo ScaleOxnard Plain Wat
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Figure 3-3Santa Clara RiverFlow and
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Figure 3-5Agriculture andPumping al
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Figure 3-7Agriculture and Pumpingal
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50,00045,00040,00035,000Supply and
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Acre-Feet6,0005,0004,0003,0002,0001
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WATER RESOURCES TECHNICAL REPORT4.1
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