Blood osmolality in vitro: dependence on base addition, buffer value, and temperature

Abstract

Blood osmolality (Osm) increases with PCO2 because of CO2 absorption. The influences of NaOH addition, equilibration temperature, and hemoglobin concentration on these respiratory changes of Osm were measured by freezing-point determination in true plasma. Addition of NaOH increases Osm by 2 mosmol X kg H2O-1 X mmol base-1 X l at constant PCO2 due to the osmotic effects of Na+ and produced bicarbonate. Respiratory compensation of the pH change further increases Osm. This contrasts to the respiratory compensation of the osmolar disturbance caused by fixed acid. Raising the equilibration temperature reduces Osm by 0.5 mosmol X kg H2O-1 X degrees C-1 at constant pH mainly caused by a lower absorption coefficient for CO2 and changed pK value for H2CO3. The slope of the linear regression lines between Osm and pH during CO2 equilibration increases with hemoglobin; the value of the quotient delta Osm/delta pH depends directly on the nonbicarbonate buffer value. The use of this quotient for the estimation of the mean nonbicarbonate buffer value of the whole body is suggested. The osmotic effects of therapeutic base infusion should be regarded with caution.