Salinity Gradients in Estuaries
Speaker: Indian English
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Estuaries represent a dynamic transition between freshwater rivers and the open sea. Because seawater is denser than river water, it often slides along the bottom to form what oceanographers call a salt wedge. The exact shape and of this boundary depends on both tidal forces and river . During periods of heavy rainfall, freshwater pushes the marine layer outward, whereas summer droughts allow salty water to penetrate much further inland. Organisms living in these zones must possess remarkable physiological mechanisms to fluctuations in osmotic pressure. Consequently, the biodiversity of an estuary reflects the ability of resident species to constant environmental change.