Urine specific gravity (USG) and osmolality are measures of the solute concentration in urine and are used to assess the ability of the renal tubules to concentrate or dilute the glomerular filtrate.
Urine specific gravity is a measurement of the density of urine compared to pure water. For routine clinical purposes, USG is determined using a refractometer (refractive index generally correlates well with USG). The USG is influenced by the number of molecules in urine, as well as their molecular weight and size, therefore it only approximates solute concentration. It is also affected by temperature, with urine density decreasing with increasing temperatures. The presence of large amounts of protein and glucose will alter the USG and should be considered when interpreting USG results. The following substances will increase the USG by 0.001 units.
Urine osmolality is directly related to the number of particles in solution and is unaffected by molecular weight and size. Osmolality can be measured by freezing point depression (technique used at Cornell University) and changes in vapor pressure. Urine osmolality can be approximated from the USG, by multiplying the last 2 digits of the USG by 36. Knowledge of urinary solute concentration is essential for proper interpretation of BUN and serum creatinine, which are indicators of glomerular filtration rate. The USG is very useful for identifying the cause of azotemia. The interpretation of several urine chemical parameters also is influenced by the specific gravity of the specimen. Why does this make sense? In addition, urinary constituents (erythrocytes, leukocytes and casts) can lyse in dilute urine (USG < 1.008), affecting interpretation of the urine sediment results.
Last Updated: Friday, January 15th 1999 |