Question

Why is the ocean salty?

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Answer

Because rivers have been carrying dissolved minerals into the sea for billions of years, and the salt has nowhere to go.

The main source is rock weathering. Rain is slightly acidic — atmospheric carbon dioxide dissolves in it to form weak carbonic acid. As it falls on land and flows over rock, it slowly dissolves minerals, carrying ions including sodium, chloride, calcium and magnesium into rivers and eventually the sea.

Why the ocean accumulates it and rivers do not. This is the crucial part. Water leaves the ocean almost exclusively by evaporation, and evaporation takes only the water — the dissolved salts stay behind. Rivers are constantly flushed; the ocean is a terminal destination with no outflow. Over geological time, salt concentrates.

A second source is hydrothermal vents on the ocean floor, where seawater percolates through hot volcanic rock, dissolving minerals and returning them. Underwater volcanism contributes too.

Why it is not getting steadily saltier. Ocean salinity has been roughly stable for a very long time, because salts are also removed — deposited as sediment, incorporated into marine organisms' shells and skeletons, precipitated in evaporite deposits, and absorbed into new seafloor rock. Input and output are approximately balanced.

Why sodium chloride dominates. Different ions have different residence times in seawater. Calcium is rapidly taken up by organisms building shells, so it does not accumulate. Sodium and chloride are less readily removed by biological processes, so they build up and account for the overwhelming majority of dissolved salt — around 85%.

Salinity averages about 3.5%, or 35 grams per litre, but varies: higher where evaporation is strong and rainfall low, lower near river mouths and melting ice.

Some inland lakes are far saltier. The Dead Sea and Great Salt Lake have no outflow at all, so they concentrate salt much further.

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