Osmolarity Calculator

Calculate osmolarity from solute concentrations and Van t Hoff factors.
Supports up to 4 solutes.
Compare to plasma osmolarity and understand osmotic pressure.

Osmolarity

Osmolarity is the total concentration of solute particles in a solution, expressed in osmoles per liter (Osm/L or mOsm/L).

Formula for one solute:

Osmolarity = i × M

For multiple solutes:

Osmolarity = Σ(iₙ × Mₙ) = i₁M₁ + i₂M₂ + i₃M₃ + ...

Where:

  • i = Van’t Hoff factor (number of particles per formula unit)
  • M = molar concentration (mol/L)

Osmolarity vs Osmolality:

  • Osmolarity = osmoles per liter of solution (Osm/L), more common in lab
  • Osmolality = osmoles per kg of solvent (Osm/kg), used clinically, independent of temperature

For dilute aqueous solutions, osmolarity ≈ osmolality.

Clinical reference values:

Fluid Osmolarity
Normal plasma 285 to 295 mOsm/L
Isotonic saline (0.9% NaCl) ~308 mOsm/L
D5W (5% dextrose) ~252 mOsm/L
Urine (normal) 50 to 1,200 mOsm/L
Seawater ~1,000 mOsm/L

Tonicity (clinical):

  • Isotonic: same osmolarity as plasma (~285-295 mOsm/L), no net water movement
  • Hypotonic: lower osmolarity, cells swell (water enters)
  • Hypertonic: higher osmolarity, cells shrink (water leaves)

Where this calculator draws the isotonic line

Plasma itself measures 285-295 mOsm/L, but the fluids a clinician calls isotonic run a little wider than that. Normal saline is 308 mOsm/L and lactated Ringer’s is 273, and both bags are labeled isotonic.

So the verdict below uses a working band of 285 to 310 mOsm/L, which keeps 0.9% saline inside it. Below 285 the result is reported as hypotonic, above 310 as hypertonic. If you need the strict physiological range rather than the practical one, compare your number against 285-295 by eye.

Osmotic pressure:

π = i × M × R × T

Where R = 0.08206 L·atm/(mol·K) and T is temperature in Kelvin. For plasma at 290 mOsm/L and 37 °C: π ≈ 7.4 atm (~5,600 mmHg). Saline at 308 comes out slightly higher, as the worked example below shows.

Serum osmolarity estimation (clinical formula): Serum Osm ≈ 2[Na⁺] + [glucose]/18 + [BUN]/2.8 (concentrations in mEq/L and mg/dL)

Common i values:

Solute i
Glucose (non-electrolyte) 1
Urea 1
NaCl (dilute) 2
KCl 2
MgCl₂ 3
Na₂SO₄ 3
CaCl₂ 3

Osmolarity or osmolality?

The two words differ by one letter and by their denominator. Osmolarity is osmoles per liter of solution; osmolality is osmoles per kilogram of solvent. Clinical laboratories measure osmolality, because it is what a freezing-point osmometer actually determines and because it does not shift with temperature. Textbooks and IV bag labels usually quote osmolarity.

For dilute body fluids the two are close enough to swap in conversation, since a liter of plasma is nearly a kilogram of water. They diverge when a solution carries a lot of protein or lipid, which is exactly the situation where the distinction starts to matter clinically.

Reading the tonicity verdict

Tonicity is not the same as osmolarity, and this is worth holding onto. Osmolarity counts every dissolved particle; tonicity counts only the ones that cannot cross the cell membrane. A urea solution can be high in osmolarity yet effectively hypotonic, because urea diffuses into the cell and stops pulling water outward. That is why 5% dextrose is treated as isotonic in the bag and hypotonic in the patient: once the glucose is metabolized, what remains is free water.

Worked example: 0.9% saline

Sodium chloride at 0.154 mol/L with i = 2 is the one worth committing to memory, because it is the reference every other IV fluid is compared against.

Osmolarity = 2 × 0.154 = 0.308 Osm/L = 308 mOsm/L, which lands inside the working isotonic band.

At body temperature, osmotic pressure π = 0.308 × 0.08206 × 310.15 = 7.839 atm, or about 5,958 mmHg. That is about fifty times a systolic blood pressure reading, and it is the force a red blood cell membrane is holding back at all times. It is also why an accidental infusion of pure water is so destructive: with nothing outside to balance it, water floods in and the cells burst.


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This calculator runs entirely in your browser, so the numbers you enter stay on your device. The math behind it is written by hand and tested against worked examples and standard references before the page goes live.

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