Journal of Applied Physiology · 1979 · 266 citations · 0 references
Electrolyte DisorderPhysical ActivitySocial SciencesPlasma OsmolalityMetabolic SyndromePhysiological ResearchKinesiologyBody CompositionStressExerciseApplied PhysiologyStress BiomarkersHealth SciencesMechanobiologyHigh AltitudeRed Cell VolumeHuman PhysiologyExercise SciencePrior DehydrationPhysiologyExercise PhysiologyStress PhysiologyPlasma VolumeMetabolism
Our purpose was 1) to test the hypothesis that in man there is a range of plasma osmolality within which the red cell volume (RCV) and mean corpuscular volume (MCV) remain essentially constant and 2) to determine the upper limit of this range. During a variety of stresses--submaximal and maximal exercise, heat and altitude exposure, +Gz acceleration, and tilting--changes in plasma osmolality between -1 and +13 mosmol/kg resulted in essentially no change in the regression of percent change in plasma volume (PV) calculated from a change in hematocrit (Hct) on that calculated from a change in Hct + hemoglobin (Hb), i.e., the RCV and MCV were constant. Factors that do not influence RCV are the level of metabolism, heat exposure at rest, and short-term orthostasis (heat-to-foot acceleration). Factors that may influence RCV are exposure to high altitude and long-term orthostasis (head-up tilting). Factors that definitely influence RCV are prior dehydration and extended (greater than 2 h) periods of stress. Thus, either the Hct or the Hct + Hb equations can be used to calculate percent changes in PV under short-term (less than 2 h) periods of stress when the change in plasma osmolality is less than 13 mosmol/kg.