Blood Osmolality Equation:
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Blood osmolality is a measure of the concentration of dissolved particles in blood. It helps assess the body's water balance and electrolyte status, and is particularly important in evaluating dehydration, overhydration, and various metabolic disorders.
The calculator uses the blood osmolality equation:
Where:
Explanation: This equation calculates the approximate osmolality of blood based on its major osmotic components. The factors 18 and 2.8 convert glucose and BUN to osmotically equivalent units.
Details: Blood osmolality measurement is crucial for diagnosing and managing fluid and electrolyte disorders, diabetes insipidus, syndrome of inappropriate antidiuretic hormone secretion (SIADH), and monitoring response to treatment in various clinical conditions.
Tips: Enter sodium concentration in mEq/L, glucose in mg/dL, and BUN in mg/dL. All values must be valid (sodium > 0, glucose and BUN ≥ 0).
Q1: What is the normal range for blood osmolality?
A: Normal blood osmolality ranges from 275 to 295 mOsm/kg. Values outside this range may indicate fluid or electrolyte imbalances.
Q2: How does this calculated osmolality compare to measured osmolality?
A: Calculated osmolality provides a good estimate but may differ from measured osmolality by 10-20 mOsm/kg due to unmeasured osmoles such as ethanol, methanol, or other toxins.
Q3: When is osmolality testing typically ordered?
A: Osmolality testing is often ordered when evaluating patients with altered mental status, suspected poisoning, fluid imbalance, or disorders of antidiuretic hormone regulation.
Q4: What is the osmolar gap and why is it important?
A: The osmolar gap is the difference between measured and calculated osmolality. A gap greater than 10-15 mOsm/kg suggests the presence of unmeasured osmotically active substances, often toxins like alcohols.
Q5: Are there limitations to this calculation?
A: This calculation does not account for all osmotically active substances in blood. Other electrolytes, proteins, and abnormal substances can affect actual osmolality.