Laboratory of Exercise Physiology, School of Physical Education, Physical Therapy and Occupational Therapy, Department of Physical Education, Federal University of Minas Gerais, Brazil.
J Physiol Anthropol. 2010;29(1):1-12. doi: 10.2114/jpa2.29.1.
To evaluate the effects of heat acclimation on sweat rate redistribution and thermodynamic parameters, 9 tropical native volunteers were submitted to 11 days of exercise-heat exposures (40+/-0 degrees C and 45.1+/-0.2% relative humidity). Sudomotor function was evaluated by measuring total and local (forehead, chest, arm, forearm, and thigh) sweat rates, local sweat sodium concentration, and mean skin and rectal temperatures. We also calculated heat production (H), heat storage (S), heat exchange by radiation (R) and by convection (C), evaporated sweat (E(sw)), sweating efficiency (eta(sw)), skin wettedness (w(sk)), and the ratio between the heat storage and the sum of heat production and heat gains by radiation and convection (S/(H+R+C)). The heat acclimation increased the whole-body sweat rate and reduced the mean skin temperature. There were changes in the local sweat rate patterns: on the arm, forearm, and thigh it increased significantly from day 1 to day 11 (all p<0.05) and the sweat rates from the forehead and the chest showed a small nonsignificant increase (p=0.34 and 0.17, respectively). The relative increase of local sweat rates on day 11 was not different among the sites; however, when comparing the limbs (arm, forearm, and thigh) with the trunk (forehead and chest), there was a significant higher increase in the limbs (32+/-5%) in comparison to the trunk (11+/-2%, p=0.001). After the heat acclimation period we observed higher w(sk) and E(sw) and reduced S/(H+R+C), meaning greater thermoregulatory efficiency. The increase in the limb sweat rate, but not the increase in the trunk sweat rate, correlated with the increased w(sk), E(sw), and reduced S/(H+R+C) (p<0.05 to all). Altogether, it can be concluded that heat acclimation increased the limbs' sweat rates in tropical natives and that this increase led to increased loss of heat through evaporation of sweat and this higher sweat evaporation was related to higher thermoregulatory efficiency.
为了评估热适应对汗率再分布和热力学参数的影响,9 名热带本地人志愿者接受了 11 天的运动-热暴露(40+/-0°C 和 45.1+/-0.2%相对湿度)。通过测量全身和局部(额、胸、臂、前臂和大腿)汗率、局部汗钠浓度、平均皮肤和直肠温度来评估汗分泌功能。我们还计算了产热(H)、储热(S)、辐射(R)和对流(C)的热交换、蒸发的汗水(E(sw))、出汗效率(eta(sw))、皮肤湿润度(w(sk))以及储热与产热和辐射和对流热增益之和的比值(S/(H+R+C))。热适应增加了全身汗率,降低了平均皮肤温度。局部汗率模式发生了变化:手臂、前臂和大腿的汗率从第 1 天到第 11 天显著增加(均 p<0.05),额部和胸部的汗率略有增加但无统计学意义(分别为 p=0.34 和 0.17)。第 11 天各部位局部汗率的相对增加无差异;然而,当比较四肢(手臂、前臂和大腿)与躯干(额部和胸部)时,四肢的增加明显更高(32+/-5%)与躯干(11+/-2%,p=0.001)。热适应期后,我们观察到更高的 w(sk)和 E(sw),以及更低的 S/(H+R+C),这意味着更高的体温调节效率。四肢汗率的增加,但不是躯干汗率的增加,与 w(sk)、E(sw)的增加和 S/(H+R+C)的降低相关(均 p<0.05)。总之,可以得出结论,热适应增加了热带本地人四肢的汗率,这种增加导致通过汗水蒸发散失更多热量,而更高的汗水蒸发与更高的体温调节效率有关。