Effective Serum Osmolality Equation:
From: | To: |
Effective serum osmolality is a measure of the concentration of dissolved particles in blood that affect water movement across cell membranes. It excludes urea as urea freely crosses cell membranes and doesn't contribute to osmotic pressure.
The calculator uses the effective osmolality equation:
Where:
Explanation: The equation accounts for the major osmotically active particles in serum (sodium and glucose) while excluding urea which doesn't affect water movement between compartments.
Details: Effective osmolality is crucial for evaluating disorders of water balance, particularly in conditions like hyperglycemia or hypernatremia. It helps assess the risk of cerebral edema in diabetic ketoacidosis.
Tips: Enter sodium in mEq/L and glucose in mg/dL. Both values must be valid (sodium > 0, glucose ≥ 0). The result is in mOsm/kg.
Q1: What is the normal range for effective osmolality?
A: Normal effective osmolality ranges from 275-295 mOsm/kg. Values outside this range may indicate water balance disorders.
Q2: Why is urea excluded from this calculation?
A: Urea freely crosses cell membranes and doesn't create osmotic gradients that drive water movement between compartments.
Q3: How does hyperglycemia affect osmolality?
A: Elevated glucose increases serum osmolality, drawing water out of cells and potentially causing cellular dehydration.
Q4: What's the difference between measured and calculated osmolality?
A: Measured osmolality includes all solutes, while calculated effective osmolality focuses on those that create osmotic gradients.
Q5: When is this calculation most clinically useful?
A: Particularly valuable in evaluating hyperglycemic states, hypernatremia, and assessing risk for cerebral edema during treatment.