Morris Nathan B, Coombs Geoff, Jay Ollie
1School of Human Kinetics, University of Ottawa, Ottawa, ON, CANADA; and 2Thermal Ergonomics Laboratory, Exercise and Sports Science, Faculty of Health Sciences, University of Sydney, NSW, AUSTRALIA.
Med Sci Sports Exerc. 2016 Jan;48(1):114-22. doi: 10.1249/MSS.0000000000000746.
To compare the reductions in evaporative heat loss from the skin (Esk) to internal heat loss (Hfluid) induced by ice slurry (ICE) ingestion relative to 37 °C fluid and the accompanying body temperature and local thermoeffector responses during exercise in warm, dry conditions (33.5 °C ± 1.4 °C; 23.7% ± 2.6% relative humidity [RH]).
Nine men cycled at approximately 55% VO2peak for 75 min and ingested 3.2 mL · kg(-1) aliquots of 37 °C fluid or ICE after 15, 30, and 45 min of exercise. Metabolic heat production (M-W), rectal temperature (Tre), mean skin temperature (Tsk), whole-body sweat loss (WBSL), local sweat rate (LSR), and skin blood flow (SkBF) were measured throughout. Net heat loss (HLnet) and heat storage (S) were estimated using partitional calorimetry.
Relative to the 37 °C trial, M-W was similar (P = 0.81) with ICE ingestion; however, the 200 ± 20 kJ greater Hfluid (P < 0.001) with ICE ingestion was overcompensated by a 381 ± 199-kJ lower Esk (P < 0.001). Net heat loss (HLnet) was consequently 131 ± 120 kJ lower (P = 0.01) and S was greater (P = 0.05) with ICE ingestion compared with 37 °C fluid ingestion. Concurrently, LSR and WBSL were lower by 0.16 ± 0.14 mg · min(-1) · cm(-2) (P < 0.01) and 191 ± 122 g (P < 0.001), respectively, and SkBF tended to be lower (P = 0.06) by 5.4%maxAU ± 13.4%maxAU in the ICE trial. Changes in Tre and Tsk were similar throughout exercise with ICE compared to 37 °C fluid ingestion.
Relative to 37 °C, ICE ingestion caused disproportionately greater reductions in Esk relative to Hfluid, resulting in a lower HLnet and greater S. Mechanistically, LSR and possibly SkBF were suppressed independently of Tre or Tsk, reaffirming the concept of human abdominal thermoreception. From a heat balance perspective, recommendations for ICE ingestion during exercise in warm, dry conditions should be reconsidered.
比较在温暖干燥环境(33.5℃±1.4℃;相对湿度[RH]为23.7%±2.6%)中运动时,摄入冰浆(ICE)相对于37℃液体所引起的皮肤蒸发散热(Esk)减少量与内部热量散失(Hfluid),以及伴随的体温和局部热效应反应。
9名男性以约55%的最大摄氧量进行75分钟的骑行运动,并在运动15、30和45分钟后分别摄入3.2 mL·kg⁻¹的37℃液体或ICE。全程测量代谢产热(M-W)、直肠温度(Tre)、平均皮肤温度(Tsk)、全身汗液流失(WBSL)、局部出汗率(LSR)和皮肤血流量(SkBF)。使用分区量热法估算净热量散失(HLnet)和热量储存(S)。
相对于37℃的试验,摄入ICE时M-W相似(P = 0.81);然而,摄入ICE时Hfluid增加200±20 kJ(P < 0.001),而Esk降低381±199 kJ(P < 0.001),这一减少量超过了前者。因此,与摄入37℃液体相比,摄入ICE时净热量散失(HLnet)降低了131±120 kJ(P = 0.01),且S更高(P = 0.05)。同时,在ICE试验中,LSR和WBSL分别降低了0.16±0.14 mg·min⁻¹·cm⁻²(P < 0.01)和191±122 g(P < 0.001),SkBF有降低趋势(P = 0.06),降低幅度为5.4%maxAU±13.4%maxAU。与摄入37℃液体相比,在整个运动过程中,摄入ICE时Tre和Tsk的变化相似。
相对于37℃,摄入ICE导致Esk相对于Hfluid的减少比例更大,从而使HLnet更低,S更高。从机制上讲,LSR以及可能的SkBF独立于Tre或Tsk受到抑制,再次证实了人体腹部温度感受的概念。从热平衡的角度来看,对于在温暖干燥环境中运动时摄入ICE的建议应重新考虑。