Large differences in peak oxygen uptake do not independently alter changes in core temperature and sweating during exercise
- 1 September 2011
- journal article
- research article
- Published by American Physiological Society in American Journal of Physiology-Regulatory, Integrative and Comparative Physiology
- Vol. 301 (3), R832-R841
- https://doi.org/10.1152/ajpregu.00257.2011
Abstract
The independent influence of peak oxygen uptake (V̇o2 peak) on changes in thermoregulatory responses during exercise in a neutral climate has not been previously isolated because of complex interactions between V̇o2 peak, metabolic heat production (Hprod), body mass, and body surface area (BSA). It was hypothesized that V̇o2 peak does not independently alter changes in core temperature and sweating during exercise. Fourteen males, 7 high (HI) V̇o2 peak: 60.1 ± 4.5 ml·kg−1·min−1; 7 low (LO) V̇o2 peak: 40.3 ± 2.9 ml·kg−1·min−1 matched for body mass (HI: 78.2 ± 6.1 kg; LO: 78.7 ± 7.1 kg) and BSA (HI: 1.97 ± 0.08 m2; LO: 1.94 ± 0.08 m2), cycled for 60-min at 1) a fixed heat production (FHP trial) and 2) a relative exercise intensity of 60% V̇o2 peak (REL trial) at 24.8 ± 0.6°C, 26 ± 10% RH. In the FHP trial, Hprod was similar between the HI (542 ± 38 W, 7.0 ± 0.6 W/kg or 275 ± 25 W/m2) and LO (535 ± 39 W, 6.9 ± 0.9 W/kg or 277 ± 29 W/m2) groups, while changes in rectal (Tre: HI: 0.87 ± 0.15°C, LO: 0.87 ± 0.18°C, P = 1.00) and aural canal (Tau: HI: 0.70 ± 0.12°C, LO: 0.74 ± 0.21°C, P = 0.65) temperature, whole-body sweat loss (WBSL) (HI: 434 ± 80 ml, LO: 440 ± 41 ml; P = 0.86), and steady-state local sweating (LSRback) ( P = 0.40) were all similar despite relative exercise intensity being different (HI: 39.7 ± 4.2%, LO: 57.6 ± 8.0% V̇o2 peak; P = 0.001). At 60% V̇o2 peak, Hprod was greater in the HI (834 ± 77 W, 10.7 ± 1.3 W/kg or 423 ± 44 W/m2) compared with LO (600 ± 90 W, 7.7 ± 1.4 W/kg or 310 ± 50 W/m2) group (all P < 0.001), as were changes in Tre (HI: 1.43 ± 0.28°C, LO: 0.89 ± 0.19°C; P = 0.001) and Tau (HI: 1.11 ± 0.21°C, LO: 0.66 ± 0.14°C; P < 0.001), and WBSL between 0 and 15, 15 and 30, 30 and 45, and 45 and 60 min (all P < 0.01), and LSRback ( P = 0.02). The absolute esophageal temperature (Tes) onset for sudomotor activity was ∼0.3°C lower ( P < 0.05) in the HI group, but the change in Tes from preexercise values before sweating onset was similar between groups. Sudomotor thermosensitivity during exercise were similar in both FHP ( P = 0.22) and REL ( P = 0.77) trials. In conclusion, changes in core temperature and sweating during exercise in a neutral climate are determined by Hprod, mass, and BSA, not V̇o2 peak.Keywords
This publication has 43 references indexed in Scilit:
- The impact of obesity on physiological responses during prolonged exerciseInternational Journal of Obesity, 2011
- Thermoregulation in multiple sclerosisJournal of Applied Physiology, 2010
- Comparison of heat dissipation response between Malaysian and Japanese males during exercise in humid heat stressInternational Journal of Biometeorology, 2010
- Exercise in a hot environment: the skin circulationScandinavian Journal of Medicine & Science in Sports, 2010
- Experimental Physiology –Research Paper: Sex differences in the effects of physical training on sweat gland responses during a graded exerciseExperimental Physiology, 2010
- Greater Exercise Sweating in Obese Women with Polycystic Ovary Syndrome Compared with Obese ControlsMedicine & Science in Sports & Exercise, 2010
- Critical environmental limits for exercising heat-acclimated lean and obese boysEuropean Journal of Applied Physiology, 2009
- Enhanced heat loss responses induced by short‐term endurance training in exercising womenExperimental Physiology, 2008
- Thermoregulation during exercise in the heat in children: old concepts revisitedJournal of Applied Physiology, 2008
- Specific Genetic Markers of Endurance Performance and &OV0312;o2maxExercise and Sport Sciences Reviews, 2001