solving seawater intrusion in the central and west coast ... · proven deterrent to intrusion for...

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Solving Seawater Intrusion in the Central and West Coast Basins of Coastal Los Angeles County….for Now Ted Johnson, PG. CHG. Chief Hydrogeologist Water Replenishment District of Southern California [email protected]

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Page 1: Solving Seawater Intrusion in the Central and West Coast ... · proven deterrent to intrusion for over 60 years. Steep inland gradients caused by groundwater pumping are the main

Solving Seawater Intrusion in the

Central and West Coast Basins of

Coastal Los Angeles County….for Now

Ted Johnson, PG. CHG.Chief Hydrogeologist

Water Replenishment Districtof Southern California

[email protected]

Page 2: Solving Seawater Intrusion in the Central and West Coast ... · proven deterrent to intrusion for over 60 years. Steep inland gradients caused by groundwater pumping are the main

5,700% increase in 110 years

LA County Population Growth

Page 3: Solving Seawater Intrusion in the Central and West Coast ... · proven deterrent to intrusion for over 60 years. Steep inland gradients caused by groundwater pumping are the main

1930s – 1950s Pumping Double

Natural Replenishment

160 foot drop (49 m)

50 foot drop (15 m)

Unsustainable.Severe Overdraft.Wells Went Dry.

Seawater Intrusion.Great threat to local

water supply.

Page 4: Solving Seawater Intrusion in the Central and West Coast ... · proven deterrent to intrusion for over 60 years. Steep inland gradients caused by groundwater pumping are the main

With Population Growth Came Groundwater Pumping Greater than Natural Replenishment… Overdraft and Seawater Intrusion

Page 5: Solving Seawater Intrusion in the Central and West Coast ... · proven deterrent to intrusion for over 60 years. Steep inland gradients caused by groundwater pumping are the main

By 1950s, groundwater was belowsea level in half of the basins,resulting in Sea Water Intrusion

Several miles inland along the Coast

Page 6: Solving Seawater Intrusion in the Central and West Coast ... · proven deterrent to intrusion for over 60 years. Steep inland gradients caused by groundwater pumping are the main

Silverado Aquifer

Lower San Pedro Aquifer

Pico Formation (“bedrock”)

200 ft. Sand Aquifer

Modified from DWR 1961, Cross Section E-E’

West East

Paci

fic O

cean

Sea Water Intrusion

1000

ft

(300

m)

Drinking Water Wells

Page 7: Solving Seawater Intrusion in the Central and West Coast ... · proven deterrent to intrusion for over 60 years. Steep inland gradients caused by groundwater pumping are the main

All coastal aquifers likely have minor seawater intrusion, even if not in overdraft

But heavy pumping can increase rate and distance of intrusion.

Seawater intrusion barriers can block the inflow of salt water and replenish the basins with fresh water

Page 8: Solving Seawater Intrusion in the Central and West Coast ... · proven deterrent to intrusion for over 60 years. Steep inland gradients caused by groundwater pumping are the main

Initial Barrier Tests 1952 - 1954

Page 9: Solving Seawater Intrusion in the Central and West Coast ... · proven deterrent to intrusion for over 60 years. Steep inland gradients caused by groundwater pumping are the main

Merged Silverado & 400 ft Gravel Aquifers

Lower San Pedro Aquifer

Silverado

400 ft. Gravel

Pico Formation (“bedrock”)

200 ft. Sand Aquifer

Modified from DWR 1961, Cross Section E-E’

West East

Seawater Barrier Wells

Injection Wells Build up pressure to overcome intrusion

Injected water also replenishes aquifers

Paci

fic O

cean

Page 10: Solving Seawater Intrusion in the Central and West Coast ... · proven deterrent to intrusion for over 60 years. Steep inland gradients caused by groundwater pumping are the main

West CoastBasin Barrier Project

1950sDominguez GapBarrier Project

1970s

Alamitos GapBarrier Project

1960s

Sea Water Barrier Wells - LACFCD

Nearly 300 injection wells, 16 mile overall length

Page 11: Solving Seawater Intrusion in the Central and West Coast ... · proven deterrent to intrusion for over 60 years. Steep inland gradients caused by groundwater pumping are the main

Water for the Barriers

n Treated Drinking Water (potable) from MWD (imported water): Ø Exclusive source 1953 – 1995.Ø Partial Source 1995 – Present.Ø 1.5 Million acre-feet to date.

n Advanced Treated Recycled Water:Ø Since 1995 at West Coast Barrier

(WBMWD).Ø Since 2005 at Alamitos Barrier (WRD). Ø Since 2006 at Dominguez Barrier (City

of LA). Ø 184,000 acre-feet to date.

n Goal is to move towards 100% recycled water at all three barriers (Water Independence Now–WIN).

Page 12: Solving Seawater Intrusion in the Central and West Coast ... · proven deterrent to intrusion for over 60 years. Steep inland gradients caused by groundwater pumping are the main

Secondary or Tertiary Wastewater

Advanced Treated Recycled Water for Barriers

To

Barriers

Advanced Oxidation

H2O2 Ultra Violet

Light Reverse Osmosis

Microfiltration

Page 13: Solving Seawater Intrusion in the Central and West Coast ... · proven deterrent to intrusion for over 60 years. Steep inland gradients caused by groundwater pumping are the main

Barrier Injection Amounts & Costs

n Injection Amounts (2016-17 estimate):n Potable Water: 6,260 afn Recycled Water: 26,040 af (81%)

32,300 af n Total Cost of Water:

n Potable Water: $ 8.5 million ($1360/af)n Recycled Water: $18.4 million ($ 707/af)

$26.9 million

Page 14: Solving Seawater Intrusion in the Central and West Coast ... · proven deterrent to intrusion for over 60 years. Steep inland gradients caused by groundwater pumping are the main

San Gabriel Valley

Palos Verdes Hills

Santa Monica Mtns

Long Beach

Los Angeles

San Gabriel Mtns

Pacific Ocean

San Fernando Valley

Torrance Carson

Going to 100% Recycled at Barriers

West Coast Barrier: Permitted for 100%

Dominguez Gap Barrier: Permitted for 50%. Moving towards 100% 2017

Alamitos Barrier: Permitted 100%

Page 15: Solving Seawater Intrusion in the Central and West Coast ... · proven deterrent to intrusion for over 60 years. Steep inland gradients caused by groundwater pumping are the main

Seawater Barrier Models

Page 16: Solving Seawater Intrusion in the Central and West Coast ... · proven deterrent to intrusion for over 60 years. Steep inland gradients caused by groundwater pumping are the main

Summaryn Seawater barrier injection wells have been a

proven deterrent to intrusion for over 60 years. Steep inland gradients caused by groundwater pumping are the main driver for the intrusion.

n Recycled water is an effective injection source for the barriers to offset the need for potable water use.

n WRD’s goal is to have the barriers at 100% recycled water in 2017.

n Impact of increased pumping and/or sea level rise may require additional injection and/or additional wells. Modeling can help predict the impacts.

Page 17: Solving Seawater Intrusion in the Central and West Coast ... · proven deterrent to intrusion for over 60 years. Steep inland gradients caused by groundwater pumping are the main

Thank You