EFFECT OF AEROBIC CAPACITY ON SWEAT RATE AND FLUID INTAKE DURING OUTDOOR EXERCISE IN THE HEAT

We measured the aerobic capacity, sweat rate and fluid intake of trained athletes during outdoor exercise and examined the relationship between aerobic capacity and thermoregulatory responses at high ambient temperatures. The maximal aerobic capacity (VO2max) Of the subjects, nine male baseball players of college age, was determined by maximal exercise tests on a cycle ergometer. The subjects practised baseball regularly without drinking fluids from 1330 to 1530 hours. After 30 min rest, they played a baseball game with free access to a sports drink at 15 degrees C from 1600 to 1830 hours. At a mean ambient temperature of 36.7 (SEM 0.2)degrees C, the mean percentage of body mass loss (Delta m(b)) and increase of oral temperature (Delta T-o) from 1330 to 1530 hours was 3.47 (SEM 0.12)% and 0.81 (SEM 0.14)degrees C, respectively. The sweat loss from 1330 to 1830 hours was 56.53 (SEM 1.56)ml . kg(-1) of body mass (m(b)) while the mean fluid consumption was 44.78 (SEM 2.39)ml . kg(-1) of m(b), With recovery of 76.08 (SEM 2.81)% of sweat loss. The VO2max was significantly inversely correlated with Delta m(b), fluid intake and rehydration amount, but showed no correlation with Delta T-o. These results would suggest that at a given exercise intensity in subjects with a higher aerobic capacity body temperature is maintained with a lower sweating rate than that in subjects with a lower aerobic capacity.