Salt lake

A salt lake or saline lake is a landlocked body of water that has a concentration of salts (typically sodium chloride) and other dissolved minerals significantly higher than most lakes (often defined as at least three grams of salt per litre). In some cases, salt lakes have a higher concentration of salt than sea water; such lakes can also be termed hypersaline lakes. An alkalic salt lake that has a high content of carbonate is sometimes termed a soda lake.^{[citation needed]}

One saline lake classification differentiates between:

subsaline: 0.5–3‰ (0.05-0.3%)
hyposaline: 3–20‰ (0.3-2%)
mesosaline: 20–50‰ (2-5%)
hypersaline: greater than 50‰ (5%)^[1]

Properties[]

Salton lake in Iran with salt mounds

Salt lakes form when the water flowing into the lake, containing salt or minerals, cannot leave because the lake is endorheic (terminal). The water then evaporates, leaving behind any dissolved salts and thus increasing its salinity, making a salt lake an excellent place for salt production. High salinity can also lead to halophilic flora and fauna in and around the lake; sometimes, in fact, the result may be an absence or near absence of multicellular life in the salt lake.

If the amount of water flowing into a lake is less than the amount evaporated, the lake will eventually disappear and leave a dry lake (also called playa or salt flat).^{[citation needed]}

Brine lakes consist of water that has reached salt saturation or near saturation (brine), and may also be heavily saturated with other materials.^{[citation needed]}

Most brine lakes develop as a result of high evaporation rates in an arid climate with a lack of an outlet to the ocean. The high salt content in these bodies of water may come from minerals deposited from the surrounding land. Another source for the salt may be that the body of water was formerly connected to the ocean. While the water evaporates from the lake, the salt remains. Eventually, the body of water will become brine.^{[citation needed]}

Because of the density of brine, swimmers are more buoyant in brine than in fresh or ordinary salt water. Examples of such brine lakes are the Dead Sea and the Great Salt Lake.^{[citation needed]}

Bodies of brine may also form on the ocean floor at cold seeps. These are sometimes called brine lakes, but are more frequently referred to as brine pools. It is possible to observe waves on the surface of these bodies.^[2]

Man-made bodies of brine are created for edible salt production. These can be referred to as brine ponds.^{[citation needed]}

List[]

Astronaut's photo of Bakhtegan and Maharloo salt lakes near Shiraz, Iran. Salt lakes are particularly common in Iran.

Lake Elton, Russia

Mono Lake, United States

Salt transport by a camel train on Lake Karum in Ethiopia.

Note: Some of the following are also partly fresh and/or brackish water.

References[]

^ Hammer, U. T. (1986). Saline Lake Ecosystems of the World. Springer. pp. 14–15. ISBN 90-6193-535-0. Retrieved 5 June 2020.
^ "NOAA Ocean Explorer: Expedition to the Deep Slope: May 31 Log". www.oceanexplorer.noaa.gov. Retrieved 30 March 2018.

External links[]

Media related to Salt lakes at Wikimedia Commons

[1] Hammer, U. T. (1986). Saline Lake Ecosystems of the World. Springer. pp. 14–15. ISBN 90-6193-535-0. Retrieved 5 June 2020.

[2] "NOAA Ocean Explorer: Expedition to the Deep Slope: May 31 Log". www.oceanexplorer.noaa.gov. Retrieved 30 March 2018.

[1]

[2]

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Salt lake

Contents

Properties[]

List[]

See also[]

References[]

External links[]

Water salinity
Part of a series on

Salinity levels
Fresh water (< 0.05%) Brackish water (0.05–3%) Saline water (3–5%) Brine (> 5% up to 26%-28% max)
Bodies of water
Seawater Salt lake Hypersaline lake Salt pan Brine pool Bodies by salinity
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