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ABSTRACT & POWERPOINT PRESENTATION The Increasing Role of Storm Water for Groundwater Recharge in the Central Basin, Los Angeles Coastal Plain, Southern California Ted Johnson Chief Hydrogeologist Water Replenishment District of Southern California Lakewood, California Managed Aquifer Recharge Symposium January 25-26, 2011 Irvine, California Symposium Organizers: National Water Research Institute Orange County Water District Water Research Foundation www.nwri-usa.org/rechargesymposium2011.htm
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ABSTRACT & POWERPOINT PRESENTATION

The Increasing Role of Storm Water for Groundwater Recharge in the Central Basin, Los Angeles Coastal Plain,

Southern California

Ted Johnson Chief Hydrogeologist

Water Replenishment District of Southern California Lakewood, California

Managed Aquifer Recharge Symposium January 25-26, 2011 Irvine, California Symposium Organizers:

• National Water Research Institute • Orange County Water District • Water Research Foundation

www.nwri-usa.org/rechargesymposium2011.htm

The Increasing Role of Storm Water for Groundwater Recharge in the Central Basin, Los Angeles Coastal Plain, Southern California By: Ted Johnson1 and Michael Gagan2

Managed aquifer recharge utilizing captured storm water has been practiced in the Montebello Forebay region of the Central Basin since 1938, when the Rio Hondo and San Gabriel Coastal Spreading Grounds were opened by the Los Angeles County Flood Control District (LACFCD). These facilities receive controlled releases of precipitation from upstream dams in addition to uncontrolled runoff from the San Gabriel River, Rio Hondo Channel, and their tributaries. The Rio Hondo facility has 430 wetted acres with 20 shallow ponds that percolate on average 400 cubic feet per second (cfs) and can hold a maximum of 3,700 acre feet (af). The San Gabriel facility has a spreading grounds and an unlined river channel. The spreading grounds are 96 wetted acres with 3 shallow ponds that percolate on average 75 cfs and can hold up to 550 af. The unlined river channel, which utilizes inflatable rubber dams to contain the water, is 308 wetted acres and can also average a 75 cfs infiltration rate with a storage capacity of 1,000 af. Imported water (starting in 1953) and recycled water (starting in 1962) are also spread at these facilities, and together with the storm water provide the supplemental groundwater recharge necessary to make-up the pumping overdraft in the Central Basin. Since 1938, a total of 7,335,063 af have been recharged at these two facilities, including 2,895,086 af of storm water (39%), 1,510,880 af of recycled water (21%) and 2,929,098 af of imported and other makeup water (40%). The Water Replenishment District of Southern California (WRD) buys the imported and recycled water for recharge to help maintain the reservoir supply. However, the availability of imported water for recharge is becoming more limited due to drought and judicial constraints. Surplus seasonal water WRD has relied upon for nearly 50 years has not been available since May 2007. Additionally, the price of imported water continues to rise. In April 2007, the price to WRD was $285/af. In January 2011 it will be $495/af if seasonal water is available or $638/af if it is not. As a result, WRD and LACFCD have embarked on projects to capture more storm water to reduce the volume of imported water needed for groundwater recharge. Two new rubber dams built on the San Gabriel River capture an additional 3,600 af/year (afy). Infrastructure located behind the Whittier Narrows Dam was removed to increase the footprint of the water conservation pool and increase storm water recharge by another 3,000 afy, with the potential for 1,100 afy more. A pipeline was constructed between the two spreading facilities to enhance operational flexibility to capture another 1,300 afy. And, a new groundwater production facility in concept phase would lower the water table and allow capture of an additional 17,000 afy. Collectively, these innovative projects will capture enough new storm water to offset much of the imported water demand for groundwater recharge.

1 Water Replenishment District of Southern California, 562-275-4240, [email protected]

2 Kindel Gagan, 213-624-1550, [email protected]

The Increasing Role of Storm Water The Increasing Role of Storm Water for Groundwater Recharge in the for Groundwater Recharge in the

Central Basin, Los Angeles Coastal Central Basin, Los Angeles Coastal Plain, Southern CaliforniaPlain, Southern California

Ted Johnson, Michael GaganTed Johnson, Michael GaganWater Replenishment District of Southern CaliforniaWater Replenishment District of Southern California

NWRI Managed Aquifer Recharge, January 26, 2011NWRI Managed Aquifer Recharge, January 26, 2011

USGS

5,800% increase 5,800% increase in 100 yearsin 100 years

But LA is DryBut LA is Dry

Receives only 15 inches (38 cm) rainfall / yr.

Rivers are dry except after infrequent storms or wastewater treatment plant discharges.

San Gabriel River (typically dry)San Gabriel River (typically dry) Treated Sewage Effluent in San Gabriel RiverTreated Sewage Effluent in San Gabriel River

Imported River Water: From Northern California & Colorado River (majority).

Groundwater from wells that tap the local aquifers.

Recycled Municipal Wastewater: From local sewage treatment plants and water reclamation plants.

So Where does LA get its Water?So Where does LA get its Water?

San Gabriel ValleySan Gabriel Valley

Coyote Hills

Palos Verdes Hills

Puente Hills

Merced Hills

Santa Monica Mtns

Long BeachLong Beach

San Gabriel RiverLos Angeles River

Los Los AngelesAngeles

San Gabriel MtnsSan Gabriel Mtns

Pacific Ocean

Newport-Inglewood Uplift

Newport-InglewoodUplift

~2.5 Million People Area = ~270 mi2

Focus on one basinFocus on one basin……The Central Groundwater BasinThe Central Groundwater Basin

E

E’

Geology of the Los Angeles BasinGeology of the Los Angeles Basin

USGS

Thick waterThick water--bearing sediments bearing sediments in the Central Basinin the Central Basin

Thick section of Late Pliocene to Recent water-bearing sediments (> 3,000 feet thick in some places).

Sediments deposited during active faulting and folding.

From Wright (1991)

Understanding of deep structure from 1000s of oil wells.

Central Basin

Aquifers

Over 300 Groundwater Production Over 300 Groundwater Production Wells Extracting over 200,000 afyWells Extracting over 200,000 afy

Historical Groundwater OverdraftHistorical Groundwater OverdraftGroundwater pumping Double Safe Yield (1900 – 1960).

Central Basin Key Well 2S/13W-10A01

-120

-100

-80

-60

-40

-20

0

20

40

60

80

100

1935

1940

1945

1950

1955

1960

1965

1970

1975

1980

1985

1990

1995

2000

2005

2010

Gro

undw

ater

Ele

vatio

n(fe

et fr

om s

ea le

vel)

Plunging Water Levels (10 feet per year)

Loss of Groundwater Supply

Wells going Dry

Seawater Intrusion

Groundwater Management Groundwater Management Solutions for Central BasinSolutions for Central Basin

Reduce Pumping: Adjudication in 1966 reduced pumping to 217,367 acre feet per year (but still greater than natural Safe Yield).

Managed Aquifer Recharge: Supplement storm water recharge with recycled and imported water (WRD founded 1959).

Seawater Barrier: LA County installed Alamitos Seawater Barrier 1964 to control seawater intrusion.

Managed Aquifer Recharge in Managed Aquifer Recharge in the Montebello Forebaythe Montebello Forebay

USGS

Montebello Forebay

Forebay(unconfined aquifers)

Surface Recharge Spreading Basin

Bedrock

(Pico Formation)

Pressure Area (confined aquifers)

Aquifer

Aquifer

Aquifer

Ocean

Replenishment at Spreading Grounds (Recharge Ponds) Replenishment at Spreading Replenishment at Spreading Grounds (Recharge Ponds)Grounds (Recharge Ponds)

San Gabriel San Gabriel spreading spreading groundsgrounds

Rio Hondo Rio Hondo spreading spreading

groundsgrounds

Spreading GroundsSpreading GroundsOwned and Operated by Los Angeles County Flood Control District. Started 1938.

Rio Hondo Spreading grounds• 20 ponds• 430 wetted acres• 400 cfs infiltration rate• 3,700 af storage

San Gabriel Spreading Grounds• 3 ponds + river channel• 400 wetted acres• 150 cfs infiltration rate• 1,550 af storage

Water entering Water entering spreading groundsspreading grounds

Full basinFull basin

Dry and groomed basinDry and groomed basin

Spreading Water SourcesSpreading Water Sources

Rainfall / Storm water Rainfall / Storm water capture ~ 54,000 capture ~ 54,000 afyafy

Imported River Water Imported River Water ~ 21,000 ~ 21,000 afyafy

Recycled Wastewater Recycled Wastewater (tertiary treated) ~ (tertiary treated) ~ 50,000 50,000 afyafy

Historical Spreading AmountsHistorical Spreading AmountsRainfall / Storm water Rainfall / Storm water capture ~ 2.9 capture ~ 2.9 mafmaf since since 1938. 1938.

Imported River Water ~ 2.9 Imported River Water ~ 2.9 mafmaf since 1953.since 1953.

Recycled Wastewater ~ 1.5 Recycled Wastewater ~ 1.5 mafmaf since 1962.since 1962.

Total Recharge 7.3 Total Recharge 7.3 mafmaf..

Central Basin Key Well 2S/13W-10A01

-120

-100

-80

-60

-40

-20

0

20

40

60

80

100

1935

1940

1945

1950

1955

1960

1965

1970

1975

1980

1985

1990

1995

2000

2005

2010

Gro

undw

ater

Ele

vatio

n(fe

et fr

om s

ea le

vel)

Results of Groundwater Management Results of Groundwater Management

Rising Water Rising Water Levels & Levels & Drought Drought ProtectionProtection

Current Challenges Current Challenges ……Loss of WRD historical Loss of WRD historical imported replenishment imported replenishment water due to drought, legal, water due to drought, legal, & environmental factors.& environmental factors.

Price for next level (Tier) of Price for next level (Tier) of imported water 29% higher imported water 29% higher ($638/af vs. $495/af).($638/af vs. $495/af).

Searching for other sources Searching for other sources for groundwater recharge.for groundwater recharge.

More recycled waterMore recycled waterConservationConservationMore storm water captureMore storm water capture

Dam up the river (temporarily)Dam up the river (temporarily)Inflatable rubber dams are Inflatable rubber dams are proven technology to halt proven technology to halt river flow and promote river flow and promote infiltration.infiltration.

2 new dams in 2008 in San 2 new dams in 2008 in San Gabriel River. Joint project Gabriel River. Joint project between WRD/LADPW.between WRD/LADPW.

3,600 3,600 afyafy more storm water more storm water capture and infiltration.capture and infiltration.

Project cost: $4.2 millionProject cost: $4.2 million

Increase Conservation Pool Increase Conservation Pool behind the Whittier Narrows Dambehind the Whittier Narrows Dam

WND is flood control project WND is flood control project built by Army Corps 1957.built by Army Corps 1957.

Oil wells behind dam limited Oil wells behind dam limited water storage capability water storage capability (conservation pool). (conservation pool).

WRD/LADPW project to WRD/LADPW project to remove oil wells.remove oil wells.

Conservation pool increased Conservation pool increased allowing 3,000 allowing 3,000 afyafy more more storm water capturestorm water capture

Interconnection PipelineInterconnection Pipeline

TwoTwo--way pipeline (78way pipeline (78””diamdiam, 1.2 mi) to divert , 1.2 mi) to divert flows between Rio Hondo flows between Rio Hondo and San Gabriel.and San Gabriel.

WRD/LACDPW project WRD/LACDPW project will go online March 2011. will go online March 2011.

Will increase storm water Will increase storm water capture by 1,300 capture by 1,300 afyafy, also , also more recharge flexibility.more recharge flexibility.

Cost $7.6 millionCost $7.6 million

Rio Hon

do

San

Gabr

iel

Create More Vadose ZoneCreate More Vadose Zone

Shallow water table limits Shallow water table limits storm water recharge. storm water recharge.

Concept to install pumping Concept to install pumping wells to drawdown water wells to drawdown water table, exposing more table, exposing more vadose zone, and freeing vadose zone, and freeing up more room for storm up more room for storm water capture / recharge.water capture / recharge.

Modeling shows 17,000 Modeling shows 17,000 afyafy more storm water can more storm water can be captured. be captured.

Low Impact Developments (LIDS)Low Impact Developments (LIDS)

Set of approaches to reduce runoff Set of approaches to reduce runoff and pollutants from reaching surface and pollutants from reaching surface waterways, and promote recharge.waterways, and promote recharge.•• BioswalesBioswales

•• Porous PavementPorous Pavement

•• Dry wellsDry wells

•• Rain HarvestingRain Harvesting

•• Smart LandscapingSmart Landscaping

Elmer Avenue site, Elmer Avenue site, LA and SG Rivers LA and SG Rivers Watershed Council Watershed Council

SummarySummaryImported water for MAR in Imported water for MAR in Central Basin is becoming more Central Basin is becoming more challenging. challenging.

One solution is to increase One solution is to increase storm water conservation storm water conservation through innovative projects.through innovative projects.

New Rubber dams, New New Rubber dams, New Pipelines, Increased Pipelines, Increased Conservation Pools and Vadose Conservation Pools and Vadose Zones, and Zones, and LIDsLIDs are all being are all being constructed to increase storm constructed to increase storm water recharge.water recharge.

Thank Thank You!You!


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