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The Basics of a The Basics of a Groundwater Banking Study Groundwater Banking Study An Introduction of the Technical Aspects An Introduction of the Technical Aspects by by John R. Hollenbeck, P.E. John R. Hollenbeck, P.E. San Luis Obispo County Public Works Dept San Luis Obispo County Public Works Dept April 12, 2006 April 12, 2006
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The Basics of a Groundwater Banking Study -

Feb 12, 2022

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Page 1: The Basics of a Groundwater Banking Study -

The Basics of aThe Basics of aGroundwater Banking StudyGroundwater Banking Study

An Introduction of the Technical AspectsAn Introduction of the Technical Aspects

byby

John R. Hollenbeck, P.E.John R. Hollenbeck, P.E.San Luis Obispo County Public Works DeptSan Luis Obispo County Public Works Dept

April 12, 2006April 12, 2006

Page 2: The Basics of a Groundwater Banking Study -

Who is John?Who is John?Born in Atchison, KS, and raised in Born in Atchison, KS, and raised in Atchison Co.Atchison Co.BS & MS Degrees in Civil Engineering BS & MS Degrees in Civil Engineering from Kansas State Universityfrom Kansas State UniversityCareer includesCareer includes

17.5 yrs Black & Veatch17.5 yrs Black & Veatch2 yrs GEI/Bookman2 yrs GEI/Bookman--EdmonstonEdmonston1 yr County of San Luis Obispo 1 yr County of San Luis Obispo (Nacimiento Project Manager)(Nacimiento Project Manager)

Came to CA in June 1994. Reside in Came to CA in June 1994. Reside in Atascadero, CA (Go Greyhounds!)Atascadero, CA (Go Greyhounds!)

GO CATS!

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Basic Success FactorsBasic Success Factors

The single most important success factor in a The single most important success factor in a Conjunctive Use Project is Conjunctive Use Project is TrustTrustPublic involvement and educationPublic involvement and educationThe program is beneficial to the Local The program is beneficial to the Local Community, the District and the Banking Community, the District and the Banking Partners.Partners.PrePre--delivered water raises groundwater levels, delivered water raises groundwater levels, which reduces pumping lift of local wells.which reduces pumping lift of local wells.Maintain flexibility with the infrastructureMaintain flexibility with the infrastructure

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Three Steps of Groundwater Banking Three Steps of Groundwater Banking StudiesStudies

Step 1 Step 1 –– Data Collection & Hydrogeology StudyData Collection & Hydrogeology StudyStep 2 Step 2 –– Physical Facilities Analysis and LayoutPhysical Facilities Analysis and LayoutStep 3 Step 3 –– Institutional and Financial PhaseInstitutional and Financial PhaseOther steps follow if implementation is desired.Other steps follow if implementation is desired.

TodayToday’’s Presentation will focus on a portion of s Presentation will focus on a portion of Step 2 Step 2 –– Method of Banking Water in the GroundMethod of Banking Water in the Ground

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Water Banking ElementsWater Banking Elements

SupplySupply

RechargeRecharge

StorageStorage

RecoveryRecovery

ReturnReturn

ConveyanceConveyance ConveyanceConveyance

Page 6: The Basics of a Groundwater Banking Study -

Methods to Bank Water in the GroundMethods to Bank Water in the Ground

InIn--Lieu RechargeLieu Recharge

Direct RechargeDirect Recharge

Injection WellsInjection Wells

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The Hydrologic Cycle Without The Hydrologic Cycle Without Groundwater BankingGroundwater Banking

Groundwater Basin

Well

Water TablePercolation

PrecipitationTranspiration

EvaporationIrrigation

Natural Recharge

Well

Page 8: The Basics of a Groundwater Banking Study -

Modes of BankingModes of BankingMonetary BankMonetary Bank

Deposit Deposit –– ““PutPut”” Money InMoney In

Withdrawal Withdrawal –– ““TakeTake”” Money OutMoney Out

Fees = Put Fees = Put -- TakeTakeGroundwater BankGroundwater Bank

Deposit Deposit –– ““PutPut”” Water InWater In

Withdrawal Withdrawal –– ““TakeTake”” Water OutWater Out

Losses = Put Losses = Put -- TakeTake

Page 9: The Basics of a Groundwater Banking Study -

Subtle Differences Between Subtle Differences Between Monetary and Groundwater BankingMonetary and Groundwater Banking

Monetary BankingMonetary BankingIf itIf it’’s your money in, then its your money in, then it’’s your money out s your money out (less fee)(less fee)If itIf it’’s OPM in, then its OPM in, then it’’s OPM out (less fee)s OPM out (less fee)

Groundwater BankingGroundwater BankingIf itIf it’’s your water in, then its your water in, then it’’s your water out s your water out (You get to keep the losses!) (You get to keep the losses!) If itIf it’’s OPW in, then its OPW in, then it’’s OPW out s OPW out (You get to keep their losses too!)(You get to keep their losses too!)

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InIn--Lieu RechargeLieu Recharge

Providing imported supply to growers Providing imported supply to growers ““inin--lieulieu””of them pumping directly from the of them pumping directly from the Groundwater BasinGroundwater BasinAmount banked equal to imported supply Amount banked equal to imported supply delivereddeliveredRecharge Sources: Natural Sources (rain, runRecharge Sources: Natural Sources (rain, run--off, etc.) and water from irrigationoff, etc.) and water from irrigation

Page 11: The Basics of a Groundwater Banking Study -

Banking Partners

Well

InIn--Lieu Recharge Lieu Recharge –– The The ““PutPut”” ModeMode

Agricultural Recharge Natural Recharge

Groundwater Basin

Pumping Pum

ping

for A

g us

e

Water Table

Imported Supply (Delivered by

District)

ON (Deposit, or “Put”)

OFF

Well

OFF

(Rising)

Page 12: The Basics of a Groundwater Banking Study -

Banking Partners

Well

InIn--Lieu Recharge Lieu Recharge –– The The ““TakeTake”” ModeMode

Agricultural Recharge Natural Recharge

Groundwater Basin

Pumping Pum

ping

for A

g us

e

Water Table

Imported Supply (Delivered by

District)

OFF

Withdrawal or “Take”

ON ON

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Example of InExample of In--Lieu RechargeLieu RechargeSemitropicSemitropic Water Storage District Water Storage District (Kern Co.)(Kern Co.)

Presently 1MAF of storage with 7 Presently 1MAF of storage with 7 Banking Partners. Banking Partners. New Program Under Construction for New Program Under Construction for additional 0.65MAF of storageadditional 0.65MAF of storageWater from the SWP is delivered to Water from the SWP is delivered to growers during the growers during the ““putput”” (deposit) phase(deposit) phaseDuring the During the ““taketake”” (withdrawal) phase, (withdrawal) phase, water can be direct returned through water can be direct returned through growergrower’’s wells, or through entitlement s wells, or through entitlement exchange to the Banking Partnersexchange to the Banking Partners

Page 14: The Basics of a Groundwater Banking Study -

Direct RechargeDirect Recharge

Storing water by allowing it to percolate into the Storing water by allowing it to percolate into the Groundwater BasinGroundwater BasinRecharge Sources: Natural Sources (rain, runRecharge Sources: Natural Sources (rain, run--off, etc.), water from irrigation, and imported off, etc.), water from irrigation, and imported supplysupply

Page 15: The Basics of a Groundwater Banking Study -

Direct Recharge Direct Recharge –– The The ““PutPut”” ModeMode

Agricultural Recharge

Natural RechargeImported Supply (Percolating)

Pum

ping

for A

g us

e

Water Table

Well

Groundwater Basin

Banking Partners

Well

Pumping

ON (Deposit, or “Put”)

OFF ON

Page 16: The Basics of a Groundwater Banking Study -

Direct Recharge Direct Recharge –– The The ““TakeTake”” ModeMode

Agricultural Recharge

Natural RechargeImported Supply (Percolating)

Pum

ping

for A

g us

e

Water Table

Well

Groundwater Basin

Banking Partners

Well

PumpingON

OFF

Withdrawal or “Take”

ON

Page 17: The Basics of a Groundwater Banking Study -

Example of Direct RechargeExample of Direct Recharge

ArvinArvin--Edison Water Storage District (Kern Co.)Edison Water Storage District (Kern Co.)Presently 250,000 AF of storage with MWDPresently 250,000 AF of storage with MWDWater from the SWP is delivered to spreading ponds Water from the SWP is delivered to spreading ponds (percolation ponds) during the (percolation ponds) during the ““putput”” (deposit) phase(deposit) phaseDuring the During the ““taketake”” (withdrawal) (withdrawal) phase, water can be direct phase, water can be direct returned to the SWP via returned to the SWP via a pipelinea pipeline

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Injection WellsInjection Wells

This Method is often called Aquifer Storage & This Method is often called Aquifer Storage & Recovery (ASR), and the wells are often called Recovery (ASR), and the wells are often called ASR WellsASR WellsGroundwater Basin is recharged by first treating Groundwater Basin is recharged by first treating the water to potable water levels, then inject into the water to potable water levels, then inject into the water table through ASR Wells.the water table through ASR Wells.Recharge Sources: Natural Sources (rain, runRecharge Sources: Natural Sources (rain, run--off, etc.), water from irrigation, and imported off, etc.), water from irrigation, and imported supplysupply

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ASR Wells ASR Wells

Agricultural Recharge Natural Recharge

Banking Partners

Groundwater Basin

New Well “Injection

Well”

Existing Well

Pumping Pum

ping

for A

g us

e

Water Table

Withdrawal

Imported Supply Deposit

ASR Well

“Put” ModeMode“Take”

Page 20: The Basics of a Groundwater Banking Study -

Example of ASR RechargeExample of ASR Recharge

CalleguasCalleguas MWDMWD’’ss Las Las PosasPosas Basin Basin (Ventura Co.)(Ventura Co.)

Presently 300,000 AF of storage with Presently 300,000 AF of storage with MWDMWDWater from the SWP treated at the Jensen Water from the SWP treated at the Jensen WTP, and is delivered to ASR wells WTP, and is delivered to ASR wells during the during the ““putput”” (deposit) phase(deposit) phaseDuring the During the ““taketake”” (withdrawal) phase, the (withdrawal) phase, the ASR wells pump the water out and deliver ASR wells pump the water out and deliver it directly to the local distribution systemit directly to the local distribution system

Page 21: The Basics of a Groundwater Banking Study -

0

10,000

20,000

30,000

40,000

50,000

60,000

0 10 20 30 40 50 60

Time

Gro

undw

ater

Ele

vatio

n

Effect of Banking on Declining Effect of Banking on Declining Groundwater LevelsGroundwater Levels

Before Banking

Deposit

Withdrawal

End Program

Without Banking

Initial Elevation

Point of Overdraft

Losses

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SemitropicSemitropic Water Storage DistrictWater Storage District

Without importing surface water

Surface water imported by State Water Project

With Banking Project

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Effect of Banking on Declining Effect of Banking on Declining Groundwater LevelsGroundwater Levels

The basic effect and benefit of a banking The basic effect and benefit of a banking program is a lengthened time for groundwater program is a lengthened time for groundwater levels to decline due to the introduction of levels to decline due to the introduction of imported water supplies.imported water supplies.

Page 24: The Basics of a Groundwater Banking Study -

Thank You!Thank You!

www.SLOCountyWater.orgwww.SLOCountyWater.orgContact: Courtney Howard, 781Contact: Courtney Howard, 781--10161016Panel DiscussionPanel Discussion

Paavo Ogren, SLO County Paavo Ogren, SLO County John Hollenbeck, SLO CountyJohn Hollenbeck, SLO CountyPaul Sorensen, Paul Sorensen, FugroFugroRon Ron EidEid, Bookman, Bookman--Edmonston/GEIEdmonston/GEI

Page 25: The Basics of a Groundwater Banking Study -

Paul A. SorensenPaul A. SorensenCA Professional GeologistCA Professional Geologist

CA Certified HydrogeologistCA Certified Hydrogeologist

BS DegreeBS Degree--Geology, Geology, UnivUniv of Washingtonof WashingtonMS DegreeMS Degree--Geology, UC Santa BarbaraGeology, UC Santa BarbaraLived in Creston for 21 yearsLived in Creston for 21 yearsCareer includesCareer includes

7 yrs Charlton/Sorensen Intl., Missoula, MT7 yrs Charlton/Sorensen Intl., Missoula, MT5 yrs Earth Sciences Assoc, Palo Alto/SLO5 yrs Earth Sciences Assoc, Palo Alto/SLO10 yrs Fugro West, San Luis Obispo10 yrs Fugro West, San Luis Obispo

Page 26: The Basics of a Groundwater Banking Study -

Paul A. Sorensen Paul A. Sorensen (cont)(cont)

Career HighlightsCareer HighlightsBasin AnalysesBasin Analyses-- Paso Robles Groundwater BasinPaso Robles Groundwater Basin-- KaweahKaweah--DeltaDelta-- Cummings Basin (Tehachapi)Cummings Basin (Tehachapi)-- Bear Valley Basin (Tehachapi)Bear Valley Basin (Tehachapi)-- Goleta BasinGoleta Basin

Active Recharge ProjectsActive Recharge Projects-- Santa Clara Valley Water DistrictSanta Clara Valley Water District-- East Bay Municipal Water DistrictEast Bay Municipal Water District

Drilled more than 400 water wellsDrilled more than 400 water wells

Page 27: The Basics of a Groundwater Banking Study -

Ronald J. Ronald J. EidEid

Raised in southern CaliforniaRaised in southern CaliforniaAttended UC Riverside and UC DavisAttended UC Riverside and UC DavisBS degree in Civil Engineering (1977)BS degree in Civil Engineering (1977)Registered Civil Engineer in CA and AZRegistered Civil Engineer in CA and AZJoined Joined BookmanBookman--Edmonston EngineeringEdmonston Engineering ((Specialists in Water Specialists in Water ResourcesResources) upon graduation) upon graduationResided and worked in Bakersfield office for last 28 Resided and worked in Bakersfield office for last 28 yearsyears

Page 28: The Basics of a Groundwater Banking Study -

Ron Ron EidEid ……

Experience (Planning)Experience (Planning)Surface water hydrologySurface water hydrology

Water supplyWater supplyFlood controlFlood control

Groundwater hydrologyGroundwater hydrologyOpenOpen--channel hydraulicschannel hydraulicsWater rightsWater rightsGroundwater managementGroundwater managementConjunctive useConjunctive use

Page 29: The Basics of a Groundwater Banking Study -

Thank You!Thank You!

www.SLOCountyWater.orgwww.SLOCountyWater.orgContact: Courtney Howard, 781Contact: Courtney Howard, 781--10161016