Effective Osmolality Equation:
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The effective osmolality equation estimates plasma osmolality primarily based on sodium concentration. It provides a quick assessment of body fluid tonicity and is useful in evaluating hydration status and electrolyte balance.
The calculator uses the effective osmolality equation:
Where:
Explanation: The equation doubles the sodium concentration to estimate effective osmolality, as sodium is the primary extracellular osmole.
Details: Effective osmolality calculation is important for assessing fluid balance, diagnosing dehydration or overhydration, and evaluating electrolyte disorders.
Tips: Enter sodium concentration in mEq/L. The value must be valid (sodium > 0).
Q1: Why use 2 × Na for osmolality calculation?
A: Sodium and its accompanying anions (mainly chloride and bicarbonate) account for approximately 95% of extracellular fluid osmolality, making this a reliable estimate.
Q2: What are normal osmolality values?
A: Normal plasma osmolality ranges from 275-295 mOsm/kg. Values outside this range may indicate fluid or electrolyte imbalances.
Q3: When should osmolality be measured?
A: Osmolality should be assessed when evaluating dehydration, hypernatremia, hyponatremia, or suspected poisoning with osmotically active substances.
Q4: Are there limitations to this equation?
A: This simplified equation does not account for other osmotically active substances like glucose, urea, or ethanol, which may be significant in certain clinical situations.
Q5: How does this differ from calculated osmolality?
A: Calculated osmolality typically includes glucose and urea (2Na + glucose/18 + BUN/2.8), while effective osmolality focuses only on osmotically active particles that don't cross cell membranes easily.