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Brackish water

earth science Maturity 9-11 Next article →

Brackish water describes a specific type of environment where salinity levels fall between those of freshwater and seawater. It is not a precisely defined condition because the salt concentration can change across different spaces and times. Technically, brackish water contains between 0.5 and 30 grams of salt per litre. This is often expressed as 0.5 to 30 parts per thousand (‰). The specific gravity of this water typically ranges from 1.0004 to 1.0226. If the concentration rises above 30‰, the water is classified as saline. This unique chemistry creates specialized habitats that support distinct biological communities.

One common way brackish water forms is through the mixing of fresh and salt water. This occurs most frequently in estuaries, which are areas where a river meets the sea. In these zones, the salinity levels shift as you move toward the ocean. For example, the River Thames in London demonstrates this transition clearly. Near Battersea, the Thames becomes brackish, and the variety of freshwater fish begins to decrease. By the time the river reaches Gravesend, the conditions become fully marine. This process creates an ecological succession where different species replace one another based on their salt tolerance.

Many animals have evolved to survive these changing conditions. Euryhaline species are organisms that can tolerate a wide range of salinity. In the Thames, marine species like flounder, European seabass, mullet, and smelt become common as salinity rises. Estuaries also serve as vital staging points for migratory fish. Anadromous fish, such as salmon and shad, live in the sea but swim up rivers to spawn. Conversely, catadromous fish, like eels, live in rivers but return to the sea to breed. These habitats also act as nursery grounds where young fish, including herring and plaice, can feed and grow safely.

Another critical brackish habitat is the mangrove swamp, also known as a mangal. These forests often fringe estuaries and lagoons where tides constantly change the salt levels. Mangroves are home to highly specialized residents like mudskippers, which forage on land. Archerfish also live here, spitting at insects to knock them into the water. These swamps provide breeding grounds for snappers, halfbeaks, and tarpon. Beyond fish, animals like the saltwater crocodile and the proboscis monkey rely on these areas. Mangroves also serve as important nesting sites for many bird groups, including herons and kingfishers.

Beyond being biological hubs, these environments serve important physical functions. Mangrove swamps act as buffer zones between the land and the sea. They provide a natural defense against damage from hurricanes and tsunamis. Some large mangrove forests, such as the Sundarbans and Bhitarkanika in the Bay of Bengal, are massive ecosystems. In larger bodies of water, salinity can even cause the water to layer itself. In the Baltic Sea, the denser seawater stays at the bottom while freshwater stays on top. This stratification means cod live in the deep marine layers, while pike stay in the surface waters.

Brackish water is also found in unique geographical locations like the Caspian Sea. As the world's largest lake, the Caspian contains salinity about one-third that of normal seawater. This supports peculiar fauna, including the Caspian seal and the great sturgeon. Hudson Bay is another example, staying brackish due to limited ocean connections and high freshwater runoff. Even inland reservoirs can become brackish, such as Lake Texoma on the U.S. border of Texas and Oklahoma. This lake became brackish because the Red River carries salt from buried deposits upstream. This allows striped bass, a saltwater fish, to live there.

Human activity both creates and utilizes brackish water. Civil engineering projects, such as building dikes, can produce these conditions. Humans also flood coastal marshlands to create brackish pools for farming freshwater prawns. In industry, brackish water is used for cooling power plants and in the oil and gas sectors. It can also be processed for use in agriculture or municipal supplies. Through methods like reverse osmosis or electrodialysis, humans can filter the salt out. This makes the water usable for drinking or livestock, turning a challenging environment into a valuable resource.

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