The Salt Wedge and Delta’s Agricultural Water Supply
“The ‘salt wedge’ is a phenomenon that occurs in all tidal estuaries of the world. Salty and dense ocean water entering the river mouth forms an underlying wedge beneath the lighter fresh water that is exiting. Water that is high in salinity can reduce or destroy crop yields, affect aquatic ecosystems and damage infrastructure. The distance that the salt wedge extends up the river changes with the tides and the seasons,” wrote John Ter Borg.