Thirst and artificial heat acclimatization in man

Abstract

The purpose of this study was to investigate the relationship between serum osmotic changes, water intake and water balance in four, fit young men during and after exercise in the heat, before and after artificial heat acclimatization. During exercise, before steady-state conditions were reached, voluntary water intakes generally paralleled but were not proportional to the serum osmotic pressure. In steady-state conditions, drinking was approximately proportional to the effective osmotic pressure of the serum. During the post-exercise recovery period, when serum osmolarity returned to normal levels, water intake also subsided even though there was a total body water (wt) deficit of about 3%. Body weight did not return to control levels until 62 to 86 hr following the exercise. This slow recovery could not be accounted for by a loss of water associated with glycogen utilization during exercise or by sweat electrolyte depletion. In general, the results supported Dill's hypothesis but plasma volume changes, in addition to osmotic factors,are very likely operative in the initiation and satiation of drinking under these conditions. Perhaps slower acting volume control mechanisms mediate the slow recovery of total body water.