Osmotic Pressure of Seawater Calculator

Find the osmotic pressure of seawater from salinity and temperature, or the brine pressure and minimum energy a desalination plant must overcome at a chosen recovery.

🌊 Osmotic Pressure of Seawater Calculator
Salinity (S)
g/kg
070
Temperature
°C
040
Feed salinity
g/kg
060
Recovery
%
090
Temperature
°C
040
Osmotic pressure
—
Pressure (bar)
—
Pressure (atm)
—
Pressure (psi)
—
Equivalent water head
—
Total ion molality
—
Water activity
—
Water density
—

Minimum applied pressure
—
Brine salinity
—
Brine osmotic pressure
—
Brine pressure (bar)
—
Feed osmotic pressure
—
Ideal minimum energy
—
Ideal energy (MJ/m³)
—

🌊 What is the Osmotic Pressure of Seawater?

The osmotic pressure of seawater is the pressure that would have to be applied to seawater to stop pure water flowing into it through a semipermeable membrane. Dissolved salts lower the chemical potential of the water, so fresh water tends to move toward the saltier side. For open ocean water with a salinity of 35 g/kg at 25 °C the effect is equal to about 2.6 MPa (roughly 26 bar or 374 psi), which is the same as the pressure at the bottom of a freshwater column more than 250 m tall. Reverse osmosis desalination works by pushing the seawater harder than this so that water crosses the membrane the wrong way and the salt is left behind.

The number matters in several places. Desalination engineers use it to size high pressure pumps and to decide how much of the feed can be recovered as fresh water before the brine becomes too salty. Marine biologists use it to understand why fish, algae and bacteria must regulate their internal salts, and why a freshwater organism swells and bursts in the ocean. Oceanographers meet it through the water activity of seawater, which sets its vapour pressure and the rate of evaporation. Chemists use the same ideas to relate salinity, molality and freezing point.

Seawater is not an ideal solution, and this is the most common misunderstanding. The simple van 't Hoff equation treats every dissolved particle as independent, but sea salt is a concentrated mixture of charged ions (mainly sodium, chloride, magnesium, sulfate, calcium and potassium) that attract each other. The osmotic coefficient φ corrects for this. For sea salt it is about 0.90 at salinity 35 and 25 °C, so the real pressure is roughly 10 percent below the ideal value. Also note that the pressure to drive reverse osmosis in practice is much larger than the osmotic pressure of the feed, because the brine is concentrated as water is removed and a driving force is needed for flux.

This calculator has two modes. The Seawater mode converts salinity and temperature into osmotic pressure in MPa, bar, atm and psi, together with the equivalent head of water, the total ion molality and the water activity. The Desalination mode takes the feed salinity, recovery and temperature, computes the brine salinity for a fully rejecting membrane, and reports the minimum applied pressure and an approximate lower bound for the specific energy. For the general van 't Hoff equation with arbitrary solutes see the osmotic pressure calculator, and for cells and membranes see the biological membranes version.

📐 Formula

Π  =  φ · m · ρw · R · T   with   m  =  S / [ M · (1 − S/1000) ]
Π = osmotic pressure (Pa); divide by 106 for MPa, 105 for bar, 101,325 for atm and 6,894.76 for psi
φ = osmotic coefficient of sea salt, held constant at 0.902 (value at S = 35 and 25 °C; approximate elsewhere)
m = total molality of dissolved particles (mol per kg of water); S = salinity in g/kg and M = 31.4 g/mol, the mean molar mass of sea salt per dissolved particle, so m = 1.155 mol/kg at S = 35
ρw = density of pure water at the given temperature (997.1 kg/m³ at 25 °C), R = 8.314462618 J/(mol K) and T = absolute temperature in kelvin
Equivalent form: Π = −(R T / Vw) ln(aw) with ln(aw) = −φ Mw m, where Mw = 0.018015 kg/mol. Head = Π / (ρw g) with g = 9.80665 m/s².
Desalination mode: brine salinity Sb = Sf / (1 − r) for a fully rejecting membrane at recovery r. Minimum applied pressure = Π(Sb). Ideal specific energy W = (1/r) ∫0r Π(Sf/(1 − x)) dx, evaluated numerically (Simpson's rule), an approximate lower bound of pressure times permeate volume. 1 kWh = 3.6 MJ.
Example: S = 35 g/kg at 25 °C gives m = 1.155 mol/kg and Π = 0.902 × 1.155 × 997.1 × 8.3145 × 298.15 = 2.575 MPa.

📖 How to Use This Calculator

Steps

1
Choose a mode. Pick Seawater to get the osmotic pressure from salinity and temperature, or Desalination to find the brine pressure and ideal energy at a chosen recovery.
2
Enter salinity and temperature. Type the salinity in g/kg and the water temperature in °C. In Desalination mode also enter the feed salinity and the recovery as a percentage.
3
Read the pressure and the chart. Results show MPa, bar, atm, psi and metres of water, or the brine salinity, minimum applied pressure and specific energy. The chart marks your value with a dashed guide and a dot, and shows the typical S = 35 line or the roughly 83 bar element rating.

💡 Example Calculations

Example 1 — Open Ocean Seawater

S = 35 g/kg at 25 °C

1
m = 35 / (31.4 × (1 − 0.035)) = 1.155 mol/kg and the water density is 997.08 kg/m³
2
Π = 0.902 × 1.155 × 997.08 × 8.3145 × 298.15 = 2.575 MPa = 25.75 bar = 25.42 atm = 374 psi
3
Head = 2.575×106 / (997.08 × 9.80665) = 263 m of water, and the water activity is 0.9814
Osmotic pressure = 2.575 MPa (25.75 bar)
Try this example →

Example 2 — Red Sea Surface Water

S = 38 g/kg at 28 °C

1
m = 38 / (31.4 × 0.962) = 1.258 mol/kg
2
Π = 0.902 × 1.258 × 996.26 × 8.3145 × 301.15 = 2.831 MPa = 28.31 bar
3
Head = 290 m of water, water activity = 0.9798
Osmotic pressure = 2.831 MPa (28.31 bar)
Try this example →

Example 3 — Brackish Estuary Water

S = 10 g/kg at 10 °C

1
m = 10 / (31.4 × 0.99) = 0.322 mol/kg
2
Π = 0.902 × 0.3217 × 999.73 × 8.3145 × 283.15 = 0.683 MPa = 6.83 bar = 99 psi
3
Head = 70 m of water. Brackish water RO therefore runs at far lower pressures than seawater RO
Osmotic pressure = 0.683 MPa (6.83 bar)
Try this example →

Example 4 — SWRO Plant at 50 Percent Recovery

Feed 35 g/kg, recovery 50 percent, 25 °C

1
Brine salinity = 35 / (1 − 0.5) = 70 g/kg, and the feed osmotic pressure is 25.8 bar
2
Brine osmotic pressure = 5.344 MPa = 53.4 bar, which is the minimum applied pressure at the brine end
3
Ideal specific energy = (1/0.5) ∫ Π dx = 3.629 MJ/m³ = 1.008 kWh/m³, close to the 1.06 kWh/m³ thermodynamic minimum cited for seawater at 50 percent recovery
Minimum pressure = 53.4 bar, ideal energy = 1.008 kWh/m³
Try this example →

Example 5 — Warm Gulf Water at 45 Percent Recovery

Feed 38 g/kg, recovery 45 percent, 28 °C

1
Brine salinity = 38 / 0.55 = 69.1 g/kg and the feed osmotic pressure is 28.3 bar
2
Brine osmotic pressure = 5.318 MPa = 53.2 bar, still well under the roughly 83 bar element rating
3
Ideal specific energy = 1.060 kWh/m³. Real plants add pump, membrane and pressure drop losses and use perhaps 2.5 to 4 kWh/m³
Minimum pressure = 53.2 bar, ideal energy = 1.060 kWh/m³
Try this example →

❓ Frequently Asked Questions

What is the osmotic pressure of seawater?+
About 2.6 MPa (26 bar, 374 psi) for open ocean water at salinity 35 g/kg and 25 °C with this calculator's model. Commonly quoted rounded figures are around 27 bar. It is the pressure that must be exceeded to push pure water out of seawater through a membrane.
How do you calculate the osmotic pressure of seawater?+
Use Π = φ × m × ρw × R × T. Here m is the total molality of dissolved ions (about 1.155 mol/kg at S = 35), φ is the osmotic coefficient (about 0.90), ρw is the density of water, R is 8.3145 J/(mol K) and T is absolute temperature.
Why is the osmotic coefficient of seawater less than 1?+
Dissolved ions attract each other, so the water is less free to leave than ideal van 't Hoff theory predicts. The osmotic coefficient measures that departure from ideal behaviour, and for sea salt at 25 °C it is about 0.90.
How much pressure does seawater reverse osmosis need?+
Typical SWRO plants operate at about 55 to 70 bar, well above the 26 bar osmotic pressure of the feed, because the brine becomes about twice as salty at 50 percent recovery and extra pressure is needed to drive a useful flux.
What is the minimum energy to desalinate seawater?+
The thermodynamic minimum for 35 g/kg seawater at 50 percent recovery is about 1.0 to 1.1 kWh per cubic metre of fresh water. This calculator gives 1.008 kWh/m³ at 25 °C. Practical SWRO uses roughly 2.5 to 4 kWh/m³.
How does recovery affect the pressure needed?+
Recovery sets the brine salinity: Sbrine = Sfeed / (1 − recovery). At 50 percent recovery the brine is twice as salty as the feed, so its osmotic pressure and the minimum applied pressure roughly double to about 53 bar.
Does temperature change the osmotic pressure of seawater?+
Yes, slightly. Osmotic pressure is proportional to absolute temperature, so 35 g/kg seawater has about 2.37 MPa at 0 °C and about 2.58 MPa at 25 °C, an increase of roughly 9 percent.
What is osmotic pressure in metres of water?+
Dividing by ρw g converts pressure to a water column. At 2.575 MPa the head is about 263 m of water, which is why a membrane must be held back against a pressure equal to a column of freshwater more than 250 m tall.
What is the difference between this and the van 't Hoff osmotic pressure calculator?+
The generic van 't Hoff equation assumes ideal behaviour. Seawater is a concentrated mixed electrolyte, so this calculator adds a measured osmotic coefficient and uses the total sea salt molality derived from salinity. See the osmotic pressure calculator for the generic form.
What happens to the osmotic pressure in the brine?+
The brine from a desalination plant has higher salinity, so a higher osmotic pressure. At 70 g/kg it is about 5.3 MPa (53 bar), twice the feed value. This is the pressure the membrane must overcome at the end of the module.
Is the 83 bar limit a hard limit?+
It is a typical rating for seawater RO elements and vessels (about 1200 psi), though some sources quote 82 bar. Check the manufacturer datasheet, since the actual limit depends on the element.
How accurate is a constant osmotic coefficient?+
The coefficient of sea salt changes a few percent with salinity and temperature, and this calculator holds it at 0.902. Expect agreement within a few percent of measured values between about 10 and 50 g/kg. Outside that range the result is flagged as approximate.

What is the osmotic pressure of seawater?

About 2.6 MPa (26 bar, 374 psi) for open ocean water at salinity 35 g/kg and 25 degrees C with this calculator's model. Commonly quoted rounded figures are around 27 bar. It is the pressure that must be exceeded to push pure water out of seawater through a membrane.

How do you calculate the osmotic pressure of seawater?

Use Pi = phi x m x rho_w x R x T. Here m is the total molality of dissolved ions (about 1.155 mol/kg at S = 35), phi is the osmotic coefficient (about 0.90), rho_w is the density of water, R is 8.3145 J/(mol K) and T is absolute temperature.

Why is the osmotic coefficient of seawater less than 1?

Dissolved ions attract each other, so the water is less free to leave than ideal van 't Hoff theory predicts. The osmotic coefficient measures that departure from ideal behaviour, and for sea salt at 25 degrees C it is about 0.90.

How much pressure does seawater reverse osmosis need?

Typical SWRO plants operate at about 55 to 70 bar, well above the 26 bar osmotic pressure of the feed, because the brine becomes about twice as salty at 50 percent recovery and extra pressure is needed to drive a useful flux.

What is the minimum energy to desalinate seawater?

The thermodynamic minimum for 35 g/kg seawater at 50 percent recovery is about 1.0 to 1.1 kWh per cubic metre of fresh water. This calculator gives 1.008 kWh/m3 at 25 degrees C. Practical SWRO uses roughly 2.5 to 4 kWh/m3.

How does recovery affect the pressure needed?

Recovery sets the brine salinity: S_brine = S_feed / (1 - recovery). At 50 percent recovery the brine is twice as salty as the feed, so its osmotic pressure and the minimum applied pressure roughly double to about 53 bar.

Does temperature change the osmotic pressure of seawater?

Yes, slightly. Osmotic pressure is proportional to absolute temperature, so 35 g/kg seawater has about 2.37 MPa at 0 degrees C and about 2.58 MPa at 25 degrees C, an increase of roughly 9 percent.

What is osmotic pressure in metres of water?

Dividing by rho_w x g converts pressure to a water column. At 2.575 MPa the head is about 263 m of water, which is why a membrane must be held back against a pressure equal to a column of freshwater more than 250 m tall.

What is the difference between this and the van 't Hoff osmotic pressure calculator?

The generic van 't Hoff equation assumes ideal behaviour. Seawater is a concentrated mixed electrolyte, so this calculator adds a measured osmotic coefficient and uses the total sea salt molality derived from salinity.

What happens to the osmotic pressure in the brine?

The brine from a desalination plant has higher salinity, so a higher osmotic pressure. At 70 g/kg it is about 5.3 MPa (53 bar), twice the feed value. This is the pressure the membrane must overcome at the end of the module.

Is the 83 bar limit a hard limit?

It is a typical rating for seawater RO elements and vessels (about 1200 psi), though some sources quote 82 bar. Check the manufacturer datasheet, since the actual limit depends on the element.