Desalination and the Impacts of Ocean Salinity: Sea Salt, Brine and Seawater Intrusion

Desalination: Meaning, Methods and Why Salinity Makes It Necessary

Salinity and the Need for Desalination: Scale and Energy Use

The need for desalination comes from the salinity of the ocean, the amount of salt in grams dissolved in 1,000 grams of seawater. The salinity of seawater differs from sea to sea, but its average of about 35 parts per thousand is far too high for drinking or irrigation, so a coastal city can lie on the sea and still run short of water. Removing the salt leaves a concentrated salty by-product called brine, which every plant must dispose of.

With recycled waste water, desalination is one of the few sources of water that do not depend on rainfall, which is why cities that face failed monsoons or have no river of their own turn to it. Its scale has grown fast. By 2020 the world had over 16,800 operating plants with a capacity of roughly 97 million cubic metres a day, and projects already contracted would raise that beyond 114 million.

Energy is the main cost of desalination, because pulling salt out of water takes work. The energy needed has fallen sharply, from 20 to 30 kilowatt-hours per cubic metre in 1970 to about 3 in 2018, a tenfold improvement, yet in 2016 desalination still used about a quarter of all the energy consumed by the water sector.

Desalination Process: Reverse Osmosis, Multi-Stage Flash and Multi-Effect Distillation

All desalination works in one of two ways. It either separates the water from the salt with a membrane, or it turns the water into vapour and condenses it, leaving the salt behind. The membrane method depends on osmosis. In osmosis, water moves on its own through a semi-permeable membrane from the side with less dissolved salt to the side with more, tending to equalise the two.

A desalination plant pushes the water the other way by reverse osmosis. High pressure is applied to the salty side, greater than the osmotic pressure, so that water molecules are forced through the membrane while the salt is held back on the pressurised side. The purified water collects on the far side. Because it needs no heating, reverse osmosis uses far less energy than distillation, and almost all new desalination plants now use it.

The thermal methods work the other way, taking the water out of the salt as vapour, and three of them are in use.

• Multi-stage flash distillation (MSF): Heated seawater flows through a series of chambers, up to 30 stages, each at a lower pressure, so part of it flashes into steam in every stage; the steam is condensed into fresh water. MSF plants produce about 26 per cent of the world's desalinated water.
• Multi-effect distillation (MED): Seawater is sprayed on tubes heated by steam; the vapour it gives off heats the next stage, so each stage reuses the energy of the one before, at a lower temperature and pressure.
• Low temperature thermal desalination (LTTD): A vacuum lets warm seawater evaporate at its own temperature, and cold deep seawater condenses the vapour; it needs no fuel to heat the water.

Low Temperature Thermal Desalination: Kavaratti and the Lakshadweep Plants

LTTD, the method used in Lakshadweep, rests on a simple fact of physics. Water boils at a lower temperature when the pressure is low. Vacuum pumps lower the pressure in a chamber until warm surface seawater evaporates at its own temperature. Cold water pumped up from the deep sea, from depths of as much as 600 metres, runs through coils and condenses the vapour, and that condensate is the fresh water. In principle the water evaporates with a temperature difference of as little as 8 °C between the two waters; a working plant needs more.

India's National Institute of Ocean Technology (NIOT), an autonomous institute of the Ministry of Earth Sciences, studied LTTD from 2004 and opened its first plant in 2005 at Kavaratti in Lakshadweep. That plant makes 1 lakh litres of drinking water a day, using deep seawater at 7 to 15 °C, at a capital cost of about ₹5 crore. Agatti and Minicoy followed, each also at 1 lakh litres a day. NIOT then tried the method on the mainland coast and with a new source of warm water, and more island plants were planned.

• 2007: An experimental floating plant off the coast of Chennai, with a capacity of 10 lakh litres a day.
• 2009: A smaller plant at the North Chennai Thermal Power Station, using the power plant's warm cooling water instead of warm surface seawater.
• 2022: The Ministry of Home Affairs, through the Lakshadweep administration, had entrusted NIOT with six more plants of 1.5 lakh litres a day each, at Amini, Androth, Chetlat, Kadmat, Kalpeni and Kiltan, at a total cost of ₹187.75 crore.

LTTD suits Lakshadweep for a reason of geography. The plants need a temperature difference of about 15 °C between surface seawater and deep seawater close to the shore, and around India such a difference close to the shore is known only near the Lakshadweep coasts. That is why the LTTD plants that supply drinking water are on the islands, while Chennai's large plants use reverse osmosis.

Desalination Plants in India and the Limits of Desalination

Chennai's Desalination Plants: Minjur, Nemmeli and Perur

Chennai is India's clearest case for desalination. The city has no perennial river to draw on; its reservoirs fill mainly from the north-east monsoon, and whenever that monsoon fails the city runs short of water. As a drought-proofing measure the government invested in desalination plants on the Bay of Bengal coast; all of them are seawater reverse osmosis (SWRO) plants.

Perur, at 400 MLD, will be the largest of the four. Minjur was built on a Design, Build, Own, Operate and Transfer basis; the first Nemmeli plant cost ₹805.08 crore, met in full by the Central Government, and the second is funded by KfW, the German development agency, and the Atal Mission for Rejuvenation and Urban Transformation (AMRUT).

Desalination is also spreading beyond city water supply. Gujarat's 2026 policy for data centres offers financial assistance for captive desalination plants to meet the sector's high demand for water.

Costs and Limits of Desalination: Energy, Price and Security

Desalination solves a water problem by creating an energy problem. Even at about 3 kilowatt-hours per cubic metre, a large plant needs a steady supply of power, and where that power comes from coal or gas, every litre of fresh water adds to carbon emissions; plants are increasingly paired with solar and wind power, and LTTD avoids fuel altogether by using the ocean's own temperature difference. Three further limits follow.

• Cost of the water: Desalinated water costs more than water from rivers, aquifers, recycling or conservation, so a city uses it as a supplement and a drought reserve rather than as its first source.
• Brine: Every plant returns a salty waste stream to the sea, which can harm marine life around the outfall.
• Concentration of risk: A city or country that draws most of its drinking water from a few plants depends on their safety.

Brine Discharge: The Environmental Cost of Desalination

Effects of Brine on Marine Life and Their Remedies

Every desalination plant splits seawater into two streams, fresh water for people and a concentrated brine that carries all the salt that was removed. Desalination plants worldwide discharge around 142 million cubic metres of brine a day, more than the volume of fresh water they produce; coastal plants return it to the sea.

The harm comes from three properties of that brine. It is saltier than the sea, so it is denser, and it sinks to the sea floor and spreads along it instead of mixing, raising the salinity around the outfall above what bottom-dwelling plants and animals can bear. It is often warmer than the sea. And it carries residues of the chemicals used to clean the membranes and stop scaling and fouling, with heavy metals from corrosion, especially in thermal plants.

Plants reduce this harm in three ways.

• Dilution: The brine is mixed with another outflow, such as a power plant's cooling water or a treated waste-water outfall, so that it is less salty when it reaches the sea.
• Dispersal: Spreading the discharge and siting outfalls where currents carry it away keeps the brine from pooling in one place; some plants are even mounted on ships so that the brine never builds up at a single spot.
• Reuse: Brine can be a resource; its high salt content gives a steeper salt gradient than seawater, and a company in Denmark is building a commercial osmotic power plant that runs on high-salinity brine.

Sea Salt and Marine Minerals

Salt Production in India: Gujarat, Rajasthan and Tamil Nadu

India is the third-largest producer of common salt in the world, after China and the United States, with about 266 lakh tonnes produced in 2021‑22. Most of it is sea salt, made by the solar evaporation of seawater; sea salt makes up about 80 per cent of the country's output. The rest comes from inland brines, such as the subsoil brine of the Little Rann of Kutch and the salt lakes of Rajasthan.

Gujarat dominates, with 85 per cent of the output, followed by Rajasthan and Tamil Nadu with about 6 per cent each. Because salt is made by the sun, weather decides the harvest, and Gujarat's dry coast and the flats of the Rann suit it. Private producers made 97.12 per cent of the salt in 2021‑22. India achieved self-sufficiency in salt in 1953, after meeting its shortfall through imports at the time of Independence, and now exports it, mainly to China, the Republic of Korea, Japan and Qatar.

• A Union subject: Salt is Item 58 of the Union List in the Seventh Schedule of the Constitution, so the Central Government controls its manufacture, supply and distribution.
• The regulator: The Salt Commissioner's Organisation in Jaipur, an attached office of the Department for Promotion of Industry and Internal Trade, monitors production, quality, prices and supply.
• Annual requirement: About 63 lakh tonnes a year of edible salt, which includes salt for cattle, and 118 lakh tonnes for industry; consumption is about 14 kg a person a year, counting edible and industrial salt.
• Rock salt: Scanty in India; the only resources, about 127.8 lakh tonnes, lie at Mandi in Himachal Pradesh.

Solar Salt Pans: From the Rann of Kutch to Ongole

A salt pan is a shallow, wide pond in which seawater or brine is left for the sun to evaporate until the salt crystallises and can be raked up. The pans are separated by low banks called levees. The water's colour changes with its salinity, because different algae and microbes thrive at each stage, from green through orange to deep red. The salt pans also give waterbirds a place to feed and rest, though building them can destroy mangroves and mudflats.

Salt-making on the Indian coast is very old. The Harappan site of Padri on the Saurashtra coast is interpreted as a centre that specialised in sea-salt production in about 2200 to 2000 BCE. Today the work follows the seasons. In the Little Rann of Kutch, the monsoon fills the ground with salt water; after it recedes in October, workers pump the brine into shallow fields where it evaporates in the sun, and over six to seven months they produce most of India's inland salt.

Magnesium, Bromine and Other Minerals from Seawater

Seawater holds more than common salt. Magnesium is the second most abundant cation in it, about one-eighth of the mass of the sodium ions, which makes seawater and sea salt commercial sources of the metal. Adding lime precipitates magnesium hydroxide, which is turned into magnesium chloride and then into the metal by electrolysis. Bromine makes up about 65 parts per million of seawater, far more than in rocks, because the oceans have gathered it by long leaching; Israel and Jordan are its main producers.

In India these minerals come mostly from the salt works themselves, which recover gypsum, bromine, magnesium chloride, magnesium sulphate, ammonium bicarbonate, soda ash, caustic soda and sodium bicarbonate as by-products of making salt.

Seawater Intrusion in the Coastal Aquifers of India

Salt Wedge Beneath the Coast and the Ghyben-Herzberg Relation

Along many coasts the groundwater is turning salty through seawater intrusion, also called salinity ingress. It is the movement of saline water into the fresh groundwater of coastal aquifers. It happens because seawater, with its dissolved salts, is denser than fresh water. Along the coast, fresh groundwater flowing towards the sea meets saline groundwater pushing in from the ocean, and the denser salt water slides inland beneath the fresh water as a wedge, with a zone of mixing between the two.

Normally the wedge stays near the coast, because the fresh water stands higher inland and its weight holds the salt water back. The Ghyben-Herzberg relation puts a number on that balance. Fresh water has a density of about 1.000 grams per cubic centimetre and seawater about 1.025, so for every metre that fresh groundwater stands above sea level, the fresh water extends about 40 metres below sea level.

Causes of Seawater Intrusion in India: Over-Pumping, Tides and Sea-Level Rise

Seawater intrusion in India has both natural and human causes, and the human ones have made it spread. The main cause is the over-extraction of groundwater. When coastal wells draw water faster than rain can replace it, the fresh water table falls, its pressure drops, and the denser seawater moves inland. A well that sits over the salt wedge can also pull salt water up from below, a process called upconing. Six causes are at work along India's coast.

• Pumping for farms, towns and industry: Wells for all three lower the water table; in the Vasai-Virar area near Mumbai, the pumping that drives the intrusion is mainly for irrigation.
• A seasonal reverse gradient: On the Gujarat coast the water table falls before the monsoon, and near the shore the slope of the water table reverses, so seawater flows landward; after the monsoon the gradient turns back and fresh groundwater discharges into the Arabian Sea.
• Tidal ingress: High tides flood low-lying marshy land, and the salt water seeps down into the upper aquifers; creeks carry it inland.
• Canals and channels: Navigation, drainage and agricultural channels give salt water a path inland, and drainage lowers the fresh water table.
• Salt pans: Brine from salt pans and the canals that feed them adds salt to nearby groundwater.
• Sea-level rise and storm surges: A higher sea pushes the wedge further inland, and cyclone surges flood the coast with seawater.

The problem is most conspicuous in Gujarat and Tamil Nadu. In Gujarat it runs along the Mangrol, Chorwad and Porbandar belt of the Saurashtra coast. In Tamil Nadu the affected areas include Minjur north of Chennai, the Tiruvanmiyur to Kovalam tract, the Cuddalore coast and the districts of Ramanathapuram, Nagapattinam, Thanjavur, Tiruvarur and Thoothukudi. At Minjur the interface between fresh and salt water lay about 3.5 km inland in 1972; by 2022 it had moved about 15 km inland. Elsewhere the problem is local, with isolated pockets in Maharashtra, Ullal and Baindur on the Karnataka coast, seasonal tidal ingress in Kerala, and naturally saline groundwater in coastal Odisha and the Sundarbans.

Remedial Measures for Seawater Intrusion: Recharge, Barriers and Regulation

Because the cause is a falling fresh water table, the remedies aim to raise it again, to block the paths salt water takes, and to control pumping. Water is a State subject in India, so the States carry most of this work, while the Centre supports conservation, rainwater harvesting and monitoring through the Central Ground Water Board; the National Water Policy, 2012, calls for interventions to tackle salinity.

• Artificial recharge: Rainwater harvesting and other recharge works put water back into the aquifer and raise the fresh water table that holds the salt water back.
• Regulating extraction: Gujarat has declared parts of its coast dark zones, where groundwater is over-exploited and new wells are restricted, to curb over-pumping, and has encouraged micro-irrigation to cut the demand for groundwater.
• Barriers against the sea: Kerala has installed tidal regulators in major inlets to keep seawater out of its backwaters; Karnataka is building vented dams and salt water exclusion dams in coastal rivers and rejuvenating its kharlands, the coastal paddy lands reclaimed from tidal marshes.
• Coast-wide planning: Gujarat's High Level Committees on salinity ingress in Saurashtra and Kutch drew up and costed works to arrest the ingress and push the saline front back towards the sea.
• Alternative supply: Desalinated water, as in Chennai, reduces the pressure on coastal aquifers.

Salinity Gradient Energy: Osmotic Power Where Rivers Meet the Sea

Osmotic Power: Pressure Retarded Osmosis and Reverse Electrodialysis

Where a river flows into the sea, fresh water and salt water mix, and the difference in their salt content holds energy that is normally lost. Osmotic power, also called salinity gradient power or blue energy, is the attempt to capture it. The idea goes back to 1954; the method of pressure retarded osmosis was invented by Sidney Loeb in Israel in 1973, partly while watching the Jordan River flow into the Dead Sea.

• Pressure retarded osmosis (PRO): Fresh water passes by osmosis through a membrane into a chamber of pressurised seawater; the rising volume and pressure drive a turbine.
• Reverse electrodialysis (RED): Alternating anion and cation exchange membranes between river and seawater generate electricity directly, in effect a salt battery.

The technology has worked in laboratories, but not yet at a profit. Norway's Statkraft opened the world's first prototype osmotic power plant on the Oslo fjord on 24 November 2009. It produced only about 4 kilowatts, and in January 2014 Statkraft announced that it would not continue, having found the salt gradient between river and sea too small to be economic with existing membranes. Higher gradients exist in desalination brines and geothermal brines, so the future of osmotic power may lie beside desalination plants rather than at river mouths.

Sources

• NCERT: Fundamentals of Physical Geography (Class XI), Chapter 12, Water (Oceans)
• NOAA National Ocean Service: Why is the ocean salty?
• Wikipedia: Desalination
• Wikipedia: Reverse osmosis
• Wikipedia: Osmosis
• Wikipedia: Multi-stage flash distillation
• Wikipedia: Multiple-effect distillation
• Wikipedia: Low-temperature thermal desalination
• Wikipedia: Saltwater intrusion
• Wikipedia: Salt evaporation pond
• Wikipedia: Little Rann of Kutch
• Wikipedia: Salt March
• Wikipedia: Magnesium
• Wikipedia: Bromine
• Wikipedia: Osmotic power
• PIB, Ministry of Earth Sciences: Indigenous technology for conversion of sea water to potable water (21 July 2022)
• PIB, Ministry of Jal Shakti: Salinity in Coastal Areas (21 March 2022)
• Central Ground Water Board: Overview of ground water quality
• Indian Bureau of Mines: Indian Minerals Yearbook 2022, Salt
• Chennai Metropolitan Water Supply and Sewerage Board: Annual Performance Report
• Chennai Metropolitan Water Supply and Sewerage Board: 150 MLD SWRO desalination plant, Nemmeli
• Chennai Metropolitan Water Supply and Sewerage Board: 400 MLD SWRO desalination plant, Perur
• The Hindu: Gujarat unveils Data Centre Policy (Delhi, 10 July 2026)
• The Hindu: U.S. targets bridges in Iran as attacks widen (Delhi, 18 July 2026)
• The Hindu: The Cauvery delta and the Mettur dam (Delhi, 22 August 2026)
• The Hindu: The salt pans of Ongole (Delhi, 20 September 2026)
• UPSC: Civil Services Examination previous question papers