Candas V, Libert J P, Vogt J J
J Appl Physiol Respir Environ Exerc Physiol. 1979 Mar;46(3):522-8. doi: 10.1152/jappl.1979.46.3.522.
Rates of evaporation and sweating were recorded for three acclimatized male subjects in hot humid conditions, the ambient parameters of which were set so that the various imposed evaporative rates required the same skin wettedness at different levels of sweating. Rectal and skin temperatures were measured. Results showed that during steady state occurring during the 2nd h of exposure each subject reached the required evaporative rate by means of increases in skin wettedness regardless of the level of sweating; the sweat evaporative efficiency, defined as the ratio between evaporative rate and sweat rate, decreased as skin wettedness increased, in a range between 0.74 and 1.0 Sweat efficiency fell to 0.67 for fully wet skin. The body temperatures did not increase with time if skin wettedness was less than unity. Evaporative heat transfer coefficient (he), maximum evaporative capacity, and wettedness were estimated on the basis of the observed decrease of sweat efficiency. The relationship between skin wettedness and sweat efficiency was interpreted as a combined effect of differences in local he as well as in local sweat rates.
在炎热潮湿的环境中,记录了三名适应环境的男性受试者的蒸发速率和出汗速率,环境参数设置为使得不同的强制蒸发速率在不同出汗水平下需要相同的皮肤湿润度。测量了直肠温度和皮肤温度。结果表明,在暴露的第2小时出现的稳态期间,每个受试者通过增加皮肤湿润度达到所需的蒸发速率,而不管出汗水平如何;汗液蒸发效率定义为蒸发速率与出汗速率之比,随着皮肤湿润度的增加而降低,范围在0.74至1.0之间。对于完全湿润的皮肤,汗液效率降至0.67。如果皮肤湿润度小于1,体温不会随时间升高。基于观察到的汗液效率下降,估算了蒸发传热系数(he)、最大蒸发能力和湿润度。皮肤湿润度与汗液效率之间的关系被解释为局部he差异和局部出汗速率差异的综合影响。