Introduction, Characteristics and some localities of Brackish Water on earth

Water generally can be classified into three categories that is Fresh water, Brackish Water and Marine water. Fresh water is defined as the Water Which is enclosed by the earth crust and Salinity is less then 0.5 ppt and Marine water is that Water which encloses the earth crust and salinity is more then 35ppt. While Brackish water is piquant and briny than fresh water but not as salty as marine water. Brackish water has a wide range of salinity that is 0.5 to 30ppt.It can be created by combining fresh and salt water, as in estuaries, as well as by some human activities, most notably the construction of coastal marshland. Brackish water has a salty, disagreeable taste and a higher salinity (500–17,000 mg/l) than fresh water. But it is not as salty as marine water (30,000–40,000 mg/l). Water is classified primarily based on its salinity level, TDS, and conductivity. Conductivity, TDS, salinity of fresh water and marine water is 150-500 µs/cm, 1000 mg/l, 500 mg/l and 46,000-72,000 µs/cm, 30,000-40,000 mg/l, 35,000-40,000 mg/l respectively. Conductivity, TDS, and salinity of brackish water is 1000-46,000 µs/cm, 1000-5000 mg/l, and 500-17,000 mg/l respectively.

Brackish water habitats are dynamic. The salinity is influenced by the amount of freshwater that enters from rivers or rain, the tide, and evaporation rate. As a result, many fish species in brackish water environments can tolerate fluctuations in salinity. Brackish water is another significant  source of aquatic life. Due to the tidal regime, brackish water is naturally present in estuaries, river deltas, lagoons in all over the world. Depending on the tide phase and the amount of fresh water discharged into the sea through the river, the salinity of the water in such ecosystems fluctuates dramatically, ranging from zero to 35 ppt. According to theory, brackish water has a specific gravity of 1.005 to 1.010 and contains between 0.5 and 30 grammes of salt per liter, which is more commonly expressed as 0.5 to 30 parts per thousand of salt. As a result, brackish water is a broad term that refers to a variety of salinity regimes. Estuaries, lakes, man-made pools, streams, aquifers, and underground water in different countries of the world are all places where brackish water can be found. Man-made sources of brackish water include dikes, which are walls constructed to restrict the flow of water from rivers and oceans, and the pools and streams that arise from purposefully flooding marshes for prawn farming. Lastly, deep fossil aquifers underground contain brackish groundwater. Because of ancient oceans, saltwater intrusion in coastal locations, or excessive mineral absorption when water percolates into the earth, groundwater can become brackish. 

water

LOCATION OF BRACKISH WATER IN THE WORLD

Salinity (PPT)NameTypeCountriesReference
3.40–3.60World OceanOceanWorldwidePérez and Chebude (2017)
1.00-1.20Sea of AzovMediterranean SeaUkraineRussiaGuinness world record
1.14Sarygamysh LakeSalt LakeTurkmenistanUzbekistanAladin and Plotnikov (2004)
35.0GarabogazkölLagoonTurkmenistanHammer, U.T. (1986)
32.4Lake Tuz (Tuz Gölü)Salt LakeTurkeyAlmardini et al. (2015)
2.30Lake VanSalt LakeTurkeySusan et al 2018
3.00–4.00Lake NatronSalt LakeTanzaniaUNESCO
3.80Mediterranean SeaMediterranean SeaSouthern EuropeLevantNorth AfricaWhite et al. (2014)
40.0Lake RetbaSalt LakeSenegalRussian Nature Reserved
9.50Lake TechirghiolSalt LakeRomaniaLacu Sarat
3.40Lough HyneMarine lakeRepublic of IrelandObservation on Lacu Sarat
0.8 1.0Baltic SeaMarginal seaNorthern EuropeEncyclopedia Britannica Online
2.80–3.20Beaufort SeaMarginal seaNorth of Alaska and CanadaThe Canadian Encyclopedia
0.59Issyk KulSalt LakeKyrgyzstanCentral AsiaDotsika et al. (2004)
33.7Dead SeaSalt LakeIsraelJordanWest BankSchutte et al. (2020)
8.50–28.0Lake UrmiaSalt LakeIranSouth-central Oregon
3.17Chilika LakeLagoonIndiaLacul Techirghiol
15.3Lake PikrolimniSalt LakeGreeceWillever (2016)
31.7Great Salt Lake, North ArmSalt LakeGreat BasinUtahUnited StatesSuosaari et al. (2016)
14.2Great Salt Lake, South ArmSalt LakeGreat BasinUtah, United StatesThe Salton Sea Authority
12.0Lake AbertSalt LakeGreat BasinOregon, United StatesEl-Serehy et al. (2018)
8.80Mono LakeSalt LakeGreat BasinCalifornia, United StatesScience Learning Hub
4.40Salton SeaSalt LakeGreat BasinCalifornia, United StatesAnati (1999)
43.3Gaet’ale PondSalt LakeEthiopiaAquatic Resource Management
3.60–4.10Red SeaMediterranean SeaEgyptSudanArabian PeninsulaHorn of AfricaOcean Salinity
4.10–4.50Great Bitter LakeSalt LakeEgyptFloods of Lake Eyre
1.25Caspian SeaSalt LakeEastern Europe/ Western AsiaMarine Nature Reserved
34.8Lake AssalSalt LakeDjiboutiHorn of Africa
1.40Qinghai LakeSalt LakeChinaRepublic of China
18.0Little Manitou LakeSalt LakeCanadaCanadian Reserved Centre
30.0Lake SaratSalt LakeBrailaRomaniaFacts about Romania
2.20Sea of MarmaraMediterranean SeaBetween the Balkan Peninsula and the Anatolian peninsulaSea of Marmara
1.30–2.30Black SeaMediterranean SeaBetween Europe and Asia – Balkan PeninsulaEastern EuropeAnatoliaCaucasusSea of Marmara
6.60Hamelin PoolLagoonAustraliaIndian Journal of Marine Sciences
3.50+Lake EyreEndorheic lakeAustraliaIndian Journal of Marine Sciences
30.0Lake BaskunchakSalt LakeAstrakhan OblastRussiaThe Black Sea Environment
33.8Don Juan PondSalt LakeAntarcticaNational Oceanographic Centre
0.00-14.6Lake Vandameromictic lakeAntarcticaNational Oceanographic Centre

Leave a Comment

Your email address will not be published. Required fields are marked *

Scroll to Top