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| Values are valid only on day of printing. | |
Measurement of the freezing point of urine is the most widely used
principle in osmometers. The extent of lowering below 0 degrees C
(the freezing point of water) is a function of the concentration of
substances dissolved in the urine. By definition, 1 milliosmole per
kilogram lowers the freezing point 0.001858 degrees C. It has been
observed that one may cool water to as low as -40 degrees C and
still have liquid water provided that no ice crystals, dust or other
contaminants are present and that the water is not agitated (super-
cooling). Vigorous agitation results in rapid freezing of the super-
cooled solution (seeding). When the solution freezes, it quickly
warms to its freezing point and the temperature remains constant
for a relatively long period of time. (In Clinical Diagnosis and
Management by Laboratory Methods. 20th edition. Edited by JB
Henry. Philadelphia, PA, WB Saunders Company, 2001)

