What is Serum Osmolarity?
Serum osmolarity (or osmolality when directly measured) is the concentration of all osmotically active particles dissolved in blood—primarily sodium, chloride, bicarbonate, potassium, glucose, and urea—expressed as milliosmoles per liter (mOsm/L for osmolarity) or per kilogram of water (mOsm/kg for osmolality). 1, 2
Core Definition and Components
Serum osmolality represents the sum of concentrations of all osmotically active solutes in blood, with sodium and its associated anions (chloride and bicarbonate) being the dominant contributors under normal physiological conditions. 1, 2
The major five osmoles contributing to plasma osmolality are sodium chloride, sodium bicarbonate, glucose, urea, and potassium. 3
Under normal conditions, serum sodium concentration is the single most important determinant of serum osmolality, accounting for the majority of osmotic activity. 2
Normal Range and Clinical Thresholds
The normal range of serum osmolality is 275-295 mOsm/kg of water. 4, 5, 3
A serum osmolality >300 mOsm/kg indicates low-intake dehydration and serves as the action threshold requiring immediate intervention, particularly in older adults. 1, 6
When using calculated osmolarity (rather than direct measurement), an action threshold of >295 mmol/L should be used for screening purposes. 1, 4
Measurement Methods
Direct Measurement (Gold Standard)
Directly measured serum or plasma osmolality using the delta-cryoscopic method is the reference standard and primary indicator of hydration status, carrying a Grade B recommendation with 94% consensus from ESPEN guidelines. 1, 4
Direct measurement is far superior to calculated values and should be prioritized whenever available. 4
Calculated Osmolarity (When Direct Measurement Unavailable)
When direct osmolality measurement is not available, use the formula: Osmolarity = 1.86 × (Na⁺ + K⁺) + 1.15 × glucose + urea + 14 (all measured in mmol/L). 1, 4
A simpler formula for rapid mental calculation is: Osmolarity = 2[Na⁺] + glucose (mg/dL)/18 + BUN (mg/dL)/2.8, which is the simplest and best formula for bedside estimation. 3, 7
Calculated osmolarity can introduce systematic bias, overestimating osmolality in lower ranges and underestimating it in higher ranges, particularly in hyperosmolar states. 8
Clinical Significance and Interpretation
Hyperosmolality (>300 mOsm/kg)
Elevated serum osmolality >300 mOsm/kg is associated with increased risk of mortality and a doubling of 4-year disability risk in older adults. 1
Hyperosmolality indicates low-intake dehydration and serves as the key physiological trigger for protective mechanisms like thirst and urinary concentration. 1, 6
Critical Interpretation Caveats
Interpretation of raised serum osmolality depends on verifying that serum glucose and urea are within normal range, as these can independently elevate osmolality and must be normalized before attributing elevation to dehydration. 1, 6, 5
In low-intake dehydration, it is common that despite raised serum osmolality (>300 mOsm/kg), none of the major individual components (sodium, potassium, urea, or glucose) are elevated outside their normal ranges—the general fluid concentration leads to the overall increase. 1
For hyperglycemia, corrected serum sodium should be increased by 1.6 mEq/L for each 100 mg/dL glucose above 100 mg/dL to account for osmotic water shift. 4
Osmolarity vs. Osmolality: Technical Distinction
Osmolarity is defined as milliosmoles of solutes per liter of solution (mOsm/L). 3
Osmolality is milliosmoles of solutes per kilogram of water in the solution (mOsm/kg), calculated by dividing osmolarity by plasma water content. 3
In clinical practice, the terms are often used interchangeably, though osmolality (measured directly) is the more precise physiological parameter. 1, 3
Effective Osmolality (Tonicity)
Effective osmolality (tonicity) is created only by solutes capable of creating an osmotic gradient across cell membranes (sodium and glucose), excluding freely permeable solutes like urea. 2
The formula for effective osmolality is: Eosm = 2[Na⁺] + glucose/18, with a normal range of 275-295 mOsm/kg of water. 3
Blood tonicity exerts its main effects on brain cells, and abnormalities can cause neurologic symptoms ranging from mild signs to life-threatening convulsions or death. 2
Osmolal Gap
The osmolal gap is the difference between measured osmolality and calculated osmolarity, with a normal range of 0 ± 2 mOsm/L. 3, 9
An increased osmolal gap suggests the presence of unmeasured solutes not included in standard calculations, such as toxic alcohols (methanol, ethylene glycol), mannitol, or other exogenous substances. 2, 9