Saltwater Intrusion and Drought Salinity Barriers

West False River drought barrier

A photo of the West False River emergency drought barrier.

The Sacramento-San Joaquin Delta (Delta) is influenced by tides from the San Francisco Bay with flood tides pushing ocean water upstream. However, if saltwater were to intrude too far inland and enter the central Delta, fresh water supplies would be compromised. This would impact Delta agriculture, local municipal supplies, and the natural environment. Additionally, California’s primary water delivery system, which supplies water to 27 million Californians and supports the world’s fifth largest economy, would be threatened.

 
Generally, flows from the Sacramento and San Joaquin Rivers keep tidal saltwater out of the central Delta. However, during periods of extreme drought, the natural upstream flows combined with water releases from upstream reservoirs provides inadequate flows necessary to prevent salty ocean water from moving into the central Delta and through the Delta.  The prevention of saltwater intrusion requires intervention and presents a tough water management challenge.  Data from past installations have demonstrated that drought salinity barriers significantly minimize saltwater intrusion.

A drought salinity barrier is a physical obstacle which could be constructed in one or more strategic Delta channels to:

  • Effectively prevent tidal saltwater intrusion into the Delta
  • Protect water quality and prevent contamination of Delta water, including water for Delta agriculture and municipal supplies
  • Reduce the amount of water released from upstream reservoirs during a drought which preserves stored water for future needs.   

This map shows the locations of the current West False River drought salinity barrier and the potential North Delta drought salinity barriers. The current West False River drought salinity barrier is located near the mouth of the West False River where it flows into the San Joaquin River. The locations of the potential North Delta Drought Salinity Barrier are: 1) Miner Slough site - located in the north Delta just upstream of the Miner Slough Bridge and CA-84N, adjacent to the northwest end of Ryer Island; and 2) the Steamboat Slough site – located 7 miles south-southwest of the Miner Slough site, on the east side of Ryer Island, 1 mile upstream from the southern confluence of Steamboat Slough and the Sacramento River, between Ryer Island and Grand Island.






























Figure 1 - This map shows the locations of the West False River Drought Salinity Barrier near the mouth of the West False River.

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