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Urine Osmolality

Urine osmolality measures the number of osmotically active particles (solutes) in each kilogram of urine water, usually by freezing point depression.

It reflects the kidney's ability to concentrate and dilute urine under the control of antidiuretic hormone (ADH), the renal medullary gradient and the delivery of solute to the collecting duct.

In health, urine osmolality varies from about 50 mOsm/kg (maximally dilute) to 1200 mOsm/kg (maximally concentrated). It is interpreted alongside serum osmolality, sodium, urine sodium and the clinical state of volume.

Urine osmolality has four main uses: to separate causes of hyponatraemia (appropriate suppression of ADH versus inappropriate release), to diagnose and classify polyuria (diabetes insipidus versus primary polydipsia versus solute diuresis), to distinguish prerenal from intrinsic acute kidney injury, and to assess concentrating capacity in chronic kidney disease. Hyponatraemia is the commonest electrolyte disorder in hospital, affecting 15 to 30% of inpatients. Polyuria (over 3 L a day) has a differential that is separated mostly by this test.

Indications. Hyponatraemia or hypernatraemia. Polyuria, polydipsia or nocturia. Suspected diabetes insipidus or syndrome of inappropriate ADH secretion. Acute kidney injury. Assessment of renal concentrating ability. Water deprivation and hypertonic saline testing. Suspected osmotic diuresis from glucose, mannitol or contrast.

Specimen. Random spot urine 5 to 10 mL, preferably a fresh sample not a first morning void unless concentrating ability is being tested. Collected in a plain sterile container. Osmolality is measured within 4 hours or refrigerated, and cloudy specimens are centrifuged. Serum for a paired osmolality and sodium is drawn at the same time.

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